{"id":267,"date":"2016-03-22T23:31:42","date_gmt":"2016-03-23T05:31:42","guid":{"rendered":"https:\/\/grad.biology.ualberta.ca\/paleobotany\/?page_id=267"},"modified":"2020-05-23T14:52:46","modified_gmt":"2020-05-23T20:52:46","slug":"lab-10-cordaites-and-conifers","status":"publish","type":"page","link":"https:\/\/grad.biology.ualberta.ca\/paleobotany\/?page_id=267","title":{"rendered":"Lab 10 Cordaites and Conifers"},"content":{"rendered":"<div id=\"attachment_997\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5714-L16-1.jpg\" rel=\"attachment wp-att-997\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-997\" class=\"size-medium wp-image-997\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5714-L16-1-300x200.jpg\" alt=\"Cordaites. Peel, stem x.s young stem w\/no septation. From Iowa.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5714-L16-1-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5714-L16-1-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5714-L16-1-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5714-L16-1-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-997\" class=\"wp-caption-text\">L16-1: Cordaites.<br \/>Peel, stem x.s young stem w\/no septation. From Iowa.<\/p><\/div>\n<div id=\"attachment_998\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5715-L16-2.jpg\" rel=\"attachment wp-att-998\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-998\" class=\"size-medium wp-image-998\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5715-L16-2-300x200.jpg\" alt=\"Cordaites. Peels, stem x.s. young stem showing septation. Note trave in 2nd wood on P844. From N.A. Age M. Pennsylvanian.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5715-L16-2-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5715-L16-2-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5715-L16-2-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5715-L16-2-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-998\" class=\"wp-caption-text\">L16-2: Cordaites.<br \/>Peels, stem x.s. young stem showing septation. Note trace in 2nd wood on P844. From N.A. Age M. Pennsylvanian.<\/p><\/div>\n<div id=\"attachment_1000\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5717-L16-2.jpg\" rel=\"attachment wp-att-1000\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1000\" class=\"size-medium wp-image-1000\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5717-L16-2-300x200.jpg\" alt=\"Cordaites. Peels, stem x.s. young stem showing septation. Note trave in 2nd wood on P844. From N.A. Age M. Pennsylvanian.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5717-L16-2-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5717-L16-2-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5717-L16-2-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5717-L16-2-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1000\" class=\"wp-caption-text\">L16-2: Cordaites.<br \/>Peels, stem x.s. young stem showing septation. Note trace in 2nd wood on P844. From N.A. Age M. Pennsylvanian.<\/p><\/div>\n<div id=\"attachment_1001\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5718-L16-2.jpg\" rel=\"attachment wp-att-1001\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1001\" class=\"size-medium wp-image-1001\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5718-L16-2-300x200.jpg\" alt=\"Cordaites. Peels, stem x.s. young stem showing septation. Note trave in 2nd wood on P844. From N.A. Age M. Pennsylvanian.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5718-L16-2-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5718-L16-2-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5718-L16-2-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5718-L16-2-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1001\" class=\"wp-caption-text\">L16-2: Cordaites.<br \/>Peels, stem x.s. young stem showing septation. Note trace in 2nd wood on P844. From N.A. Age M. Pennsylvanian.<\/p><\/div>\n<div id=\"attachment_1002\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5719-L16-2.jpg\" rel=\"attachment wp-att-1002\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1002\" class=\"size-medium wp-image-1002\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5719-L16-2-300x200.jpg\" alt=\"Cordaites. Peels, stem x.s. young stem showing septation. Note trave in 2nd wood on P844. From N.A. Age M. Pennsylvanian.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5719-L16-2-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5719-L16-2-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5719-L16-2-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5719-L16-2-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1002\" class=\"wp-caption-text\">L16-2: Cordaites.<br \/>Peels, stem x.s. young stem showing septation. Note trace in 2nd wood on P844. From N.A. Age M. Pennsylvanian.<\/p><\/div>\n<div id=\"attachment_1003\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5720-L16-3.jpg\" rel=\"attachment wp-att-1003\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1003\" class=\"size-medium wp-image-1003\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5720-L16-3-300x200.jpg\" alt=\"Cordaites. Peels, stem x.s. Age Pennsylvanian. \" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5720-L16-3-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5720-L16-3-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5720-L16-3-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5720-L16-3-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1003\" class=\"wp-caption-text\">L16-3: Cordaites.<br \/>Peels, stem x.s. Age Pennsylvanian.<\/p><\/div>\n<div id=\"attachment_1004\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5721-L16-3.jpg\" rel=\"attachment wp-att-1004\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1004\" class=\"size-medium wp-image-1004\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5721-L16-3-300x200.jpg\" alt=\"Cordaites. Peels, stem x.s. Age Pennsylvanian. \" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5721-L16-3-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5721-L16-3-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5721-L16-3-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5721-L16-3-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1004\" class=\"wp-caption-text\">L16-3: Cordaites.<br \/>Peels, stem x.s. Age Pennsylvanian.<\/p><\/div>\n<div id=\"attachment_1005\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5722-L16-4.jpg\" rel=\"attachment wp-att-1005\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1005\" class=\"size-medium wp-image-1005\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5722-L16-4-300x200.jpg\" alt=\"Cordaites. L.s. septate pith. Age Pennsylvanian. \" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5722-L16-4-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5722-L16-4-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5722-L16-4-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5722-L16-4-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1005\" class=\"wp-caption-text\">L16-4: Cordaites.<br \/>L.s. septate pith. Age Pennsylvanian.<\/p><\/div>\n<div id=\"attachment_1006\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5723-L16-5.jpg\" rel=\"attachment wp-att-1006\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1006\" class=\"size-medium wp-image-1006\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5723-L16-5-300x200.jpg\" alt=\"Cordaites. l.s. stem.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5723-L16-5-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5723-L16-5-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5723-L16-5-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5723-L16-5-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1006\" class=\"wp-caption-text\">L16-5: Cordaites.<br \/>l.s. stem.<\/p><\/div>\n<div id=\"attachment_1008\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5725-L16-6.jpg\" rel=\"attachment wp-att-1008\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1008\" class=\"size-medium wp-image-1008\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5725-L16-6-300x200.jpg\" alt=\"Cordaites. Stem x.s. From Iowa. Age M. Pennsylvanian. \" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5725-L16-6-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5725-L16-6-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5725-L16-6-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5725-L16-6-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1008\" class=\"wp-caption-text\">L16-6: Cordaites.<br \/>Stem x.s. From Iowa. Age M. Pennsylvanian.<\/p><\/div>\n<div id=\"attachment_1009\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5726-L16-7.jpg\" rel=\"attachment wp-att-1009\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1009\" class=\"size-medium wp-image-1009\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5726-L16-7-300x200.jpg\" alt=\"no info\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5726-L16-7-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5726-L16-7-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5726-L16-7-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5726-L16-7-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1009\" class=\"wp-caption-text\">L16-8: Artisia sp. pith cast of Cordaites<\/p><\/div>\n<div id=\"attachment_1011\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5728-L16-9.jpg\" rel=\"attachment wp-att-1011\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1011\" class=\"size-medium wp-image-1011\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5728-L16-9-300x200.jpg\" alt=\"Cordaites. Leaf tip, note parallel venation (looks like a moncot leaf). From Mazon Creek. Age U. Pennsylvanian. \" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5728-L16-9-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5728-L16-9-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5728-L16-9-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5728-L16-9-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1011\" class=\"wp-caption-text\">L16-9: Cordaites.<br \/>Leaf tip, note parallel venation (looks like a moncot leaf). From Mazon Creek. Age U. Pennsylvanian.<\/p><\/div>\n<div id=\"attachment_1013\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5730-L16-10.jpg\" rel=\"attachment wp-att-1013\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1013\" class=\"size-medium wp-image-1013\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5730-L16-10-300x200.jpg\" alt=\"Cordaites leaf. Collected by R. Stockey. From Knoxville, Tennesee. Age Pennsylvanian. \" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5730-L16-10-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5730-L16-10-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5730-L16-10-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5730-L16-10-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1013\" class=\"wp-caption-text\">L16-10: Cordaites leaf.<br \/>Collected by R. Stockey. From Knoxville, Tennesee. Age Pennsylvanian.<\/p><\/div>\n<div id=\"attachment_1015\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5732-L16-11.jpg\" rel=\"attachment wp-att-1015\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1015\" class=\"size-medium wp-image-1015\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5732-L16-11-300x200.jpg\" alt=\"Cordaites leaves. From Knoxville, Tennesee. Age Pennsylvanian.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5732-L16-11-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5732-L16-11-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5732-L16-11-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5732-L16-11-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1015\" class=\"wp-caption-text\">L16-11: Cordaites leaves.<br \/>From Knoxville, Tennesee. Age Pennsylvanian.<\/p><\/div>\n<div id=\"attachment_1018\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5735-L16-12.jpg\" rel=\"attachment wp-att-1018\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1018\" class=\"size-medium wp-image-1018\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5735-L16-12-300x200.jpg\" alt=\"Cordaites x.s. Peel, several leaves. Note evenly spaced vascular bundles and the sclerenchyma strands. From N.A. Age M. Pennsylvanian. \" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5735-L16-12-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5735-L16-12-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5735-L16-12-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5735-L16-12-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1018\" class=\"wp-caption-text\">L16-12: Cordaites x.s.<br \/>Peel, several leaves. Note evenly spaced vascular bundles and the sclerenchyma strands. From N.A. Age M. Pennsylvanian.<\/p><\/div>\n<div id=\"attachment_1019\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5736-L16-13.jpg\" rel=\"attachment wp-att-1019\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1019\" class=\"size-medium wp-image-1019\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5736-L16-13-300x200.jpg\" alt=\"Cordaites leaves. Peel, x.s. From West Mineral, Kansas. \" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5736-L16-13-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5736-L16-13-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5736-L16-13-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5736-L16-13-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1019\" class=\"wp-caption-text\">L16-13: Cordaites leaves.<br \/>Peel, x.s. From West Mineral, Kansas.<\/p><\/div>\n<div id=\"attachment_1021\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5738-L16-16.jpg\" rel=\"attachment wp-att-1021\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1021\" class=\"size-medium wp-image-1021\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5738-L16-16-300x200.jpg\" alt=\"Amyelon, x.s. Peel, leaf material. From N.A. \" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5738-L16-16-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5738-L16-16-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5738-L16-16-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5738-L16-16-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1021\" class=\"wp-caption-text\">L16-16: Amyelon, x.s.<br \/>Peel, leaf material. From N.A.<\/p><\/div>\n<div id=\"attachment_1022\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5739-L16-17.jpg\" rel=\"attachment wp-att-1022\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1022\" class=\"size-medium wp-image-1022\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5739-L16-17-300x200.jpg\" alt=\"Amyelon, x.s. Peel showing x.s. diarch root of cordaites. From Given, Iowa. Age M. Pennsylvanian. \" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5739-L16-17-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5739-L16-17-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5739-L16-17-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5739-L16-17-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1022\" class=\"wp-caption-text\">L16-17: Amyelon, x.s.<br \/>Peel showing x.s. diarch root of cordaites. From Given, Iowa. Age M. Pennsylvanian.<\/p><\/div>\n<div id=\"attachment_1023\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5740-L16-18.jpg\" rel=\"attachment wp-att-1023\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1023\" class=\"size-medium wp-image-1023\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5740-L16-18-300x200.jpg\" alt=\"Amyelon, (premnoxylon) x.s. Peels showing root of Cordaites with a pith. From N.A. Age M. Pennsylvanian.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5740-L16-18-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5740-L16-18-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5740-L16-18-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5740-L16-18-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1023\" class=\"wp-caption-text\">L16-18: Amyelon, (premnoxylon) x.s.<br \/>Peels showing root of Cordaites with a pith. From N.A. Age M. Pennsylvanian.<\/p><\/div>\n<div id=\"attachment_1026\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5743-L16-19.jpg\" rel=\"attachment wp-att-1026\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1026\" class=\"size-medium wp-image-1026\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5743-L16-19-300x200.jpg\" alt=\"Amyelon, x.s. Peels showing root of Cordaites.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5743-L16-19-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5743-L16-19-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5743-L16-19-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5743-L16-19-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1026\" class=\"wp-caption-text\">L16-19: Amyelon, x.s.<br \/>Peels showing root of Cordaites.<\/p><\/div>\n<div id=\"attachment_1028\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5745-L16-20.jpg\" rel=\"attachment wp-att-1028\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1028\" class=\"size-medium wp-image-1028\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5745-L16-20-300x200.jpg\" alt=\"Cordaianthus. Compound reproductive unit, find bracts, axillary cones. From Shuler Mine, Iowa. Age U. Pennsylvanian.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5745-L16-20-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5745-L16-20-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5745-L16-20-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5745-L16-20-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1028\" class=\"wp-caption-text\">L16-20: Cordaianthus.<br \/>Compound reproductive unit, find bracts, axillary cones. From Shuler Mine, Iowa. Age U. Pennsylvanian.<\/p><\/div>\n<div id=\"attachment_1031\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5748-L16-21.jpg\" rel=\"attachment wp-att-1031\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1031\" class=\"size-medium wp-image-1031\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5748-L16-21-300x200.jpg\" alt=\"Cordaianthus. From Murphyboro, IL. \" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5748-L16-21-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5748-L16-21-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5748-L16-21-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5748-L16-21-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1031\" class=\"wp-caption-text\">L16-23: Cordaianthus.<br \/>From Murphyboro, IL.<\/p><\/div>\n<div id=\"attachment_1033\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5750-L16-23.jpg\" rel=\"attachment wp-att-1033\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1033\" class=\"size-medium wp-image-1033\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5750-L16-23-300x200.jpg\" alt=\"Cordaianthus. From Murphyboro, IL. \" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5750-L16-23-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5750-L16-23-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5750-L16-23-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5750-L16-23-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1033\" class=\"wp-caption-text\">L16-23: Cordaianthus.<br \/>From Murphyboro, IL.<\/p><\/div>\n<div id=\"attachment_1034\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5751-L16-23.jpg\" rel=\"attachment wp-att-1034\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1034\" class=\"size-medium wp-image-1034\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5751-L16-23-300x200.jpg\" alt=\"Cordaianthus. From Murphyboro, IL. \" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5751-L16-23-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5751-L16-23-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5751-L16-23-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5751-L16-23-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1034\" class=\"wp-caption-text\">L16-23: Cordaianthus.<br \/>From Murphyboro, IL.<\/p><\/div>\n<div id=\"attachment_1037\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5754-L16-24.jpg\" rel=\"attachment wp-att-1037\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1037\" class=\"size-medium wp-image-1037\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5754-L16-24-300x200.jpg\" alt=\"Cordaianthus concinus. Peel. From West Mineral, Kansas. Age M. Pennsylvanian.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5754-L16-24-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5754-L16-24-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5754-L16-24-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5754-L16-24-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1037\" class=\"wp-caption-text\">L16-24: Cordaianthus concinus.<br \/>Peel. From West Mineral, Kansas. Age M. Pennsylvanian.<\/p><\/div>\n<div id=\"attachment_1039\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5756-L16-25.jpg\" rel=\"attachment wp-att-1039\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1039\" class=\"size-medium wp-image-1039\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5756-L16-25-300x200.jpg\" alt=\"Cordaianthus. Peel, showing cones sectioned in various ways w. bractioles &amp; sporangia. From Given, Iowa. Age M. Pennsylvanian. \" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5756-L16-25-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5756-L16-25-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5756-L16-25-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5756-L16-25-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1039\" class=\"wp-caption-text\">L16-25: Cordaianthus.<br \/>Peel, showing cones sectioned in various ways w. bractioles &amp; sporangia. From Given, Iowa. Age M. Pennsylvanian.<\/p><\/div>\n<div id=\"attachment_1040\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5757-L16-26.jpg\" rel=\"attachment wp-att-1040\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1040\" class=\"size-medium wp-image-1040\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5757-L16-26-300x200.jpg\" alt=\"Nucellangium &amp; Cordaianthus. Peel. From Shuler Mine, Iowa. Age U. Pennsylvanian.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5757-L16-26-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5757-L16-26-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5757-L16-26-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5757-L16-26-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1040\" class=\"wp-caption-text\">L16-26: Nucellangium &amp; Cordaianthus.<br \/>Peel. From Shuler Mine, Iowa. Age U. Pennsylvanian.<\/p><\/div>\n<div id=\"attachment_1043\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5761-L16-27.jpg\" rel=\"attachment wp-att-1043\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1043\" class=\"size-medium wp-image-1043\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5761-L16-27-300x200.jpg\" alt=\"Cardiocarpus spinatus. Peel. From West Mineral, Kansas. Age M. Pennsylvanian.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5761-L16-27-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5761-L16-27-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5761-L16-27-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5761-L16-27-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1043\" class=\"wp-caption-text\">L16-27: Cardiocarpus spinatus.<br \/>Peel. From West Mineral, Kansas. Age M. Pennsylvanian.<\/p><\/div>\n<div id=\"attachment_1044\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5762-L16-28.jpg\" rel=\"attachment wp-att-1044\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1044\" class=\"size-medium wp-image-1044\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5762-L16-28-300x200.jpg\" alt=\"Cardiocarpus spinatus. Peel.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5762-L16-28-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5762-L16-28-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5762-L16-28-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5762-L16-28-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1044\" class=\"wp-caption-text\">L16-28: Cardiocarpus spinatus.<br \/>Peel.<\/p><\/div>\n<div id=\"attachment_1046\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5764-L16-29.jpg\" rel=\"attachment wp-att-1046\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1046\" class=\"size-medium wp-image-1046\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5764-L16-29-300x200.jpg\" alt=\"Cardiocarpus. Peel, showing bilateral symmetry. From Given, Iowa. \" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5764-L16-29-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5764-L16-29-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5764-L16-29-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5764-L16-29-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1046\" class=\"wp-caption-text\">L16-29: Cardiocarpus.<br \/>Peel, showing bilateral symmetry. From Given, Iowa.<\/p><\/div>\n<div id=\"attachment_1047\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5765-L16-30.jpg\" rel=\"attachment wp-att-1047\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1047\" class=\"size-medium wp-image-1047\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5765-L16-30-300x200.jpg\" alt=\"Cardiocarups spinatus. Peel. From West Mineral, Kansas. Age M. Pennsylvanian.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5765-L16-30-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5765-L16-30-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5765-L16-30-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5765-L16-30-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1047\" class=\"wp-caption-text\">L16-30: Cardiocarups spinatus.<br \/>Peel. From West Mineral, Kansas. Age M. Pennsylvanian.<\/p><\/div>\n<div id=\"attachment_1049\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5767-L16-31.jpg\" rel=\"attachment wp-att-1049\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1049\" class=\"size-medium wp-image-1049\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5767-L16-31-300x200.jpg\" alt=\"Cardiocarups spinatus. From What Cheer, Iowa.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5767-L16-31-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5767-L16-31-768x512.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5767-L16-31-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/IMG_5767-L16-31-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1049\" class=\"wp-caption-text\">L16-31: Cardiocarups spinatus.<br \/>From What Cheer, Iowa.<\/p><\/div>\n<div id=\"attachment_1050\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5562-L17-1.jpg\" rel=\"attachment wp-att-1050\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1050\" class=\"size-medium wp-image-1050\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5562-L17-1-300x199.jpg\" alt=\"Walchia (piniformis?) \" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5562-L17-1-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5562-L17-1-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5562-L17-1-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5562-L17-1-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1050\" class=\"wp-caption-text\">L17-1: Walchia (piniformis?)<\/p><\/div>\n<div id=\"attachment_1051\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5565-L17-3.jpg\" rel=\"attachment wp-att-1051\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1051\" class=\"size-medium wp-image-1051\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5565-L17-3-300x199.jpg\" alt=\"Plagiophyllum diffusum. From York Haven, PA. Age L.Triassic. \" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5565-L17-3-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5565-L17-3-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5565-L17-3-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5565-L17-3-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1051\" class=\"wp-caption-text\">L17-3: Plagiophyllum diffusum.<br \/>From York Haven, PA. Age L.Triassic.<\/p><\/div>\n<div id=\"attachment_1052\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5569-L17-4.jpg\" rel=\"attachment wp-att-1052\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1052\" class=\"size-medium wp-image-1052\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5569-L17-4-300x199.jpg\" alt=\"Plagiophyllum diffusum. From York Haven, PA. Age L.Triassic.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5569-L17-4-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5569-L17-4-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5569-L17-4-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5569-L17-4-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1052\" class=\"wp-caption-text\">L17-3: Plagiophyllum diffusum.<br \/>From York Haven, PA. Age L.Triassic.<\/p><\/div>\n<div id=\"attachment_1053\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5570-L17-4.jpg\" rel=\"attachment wp-att-1053\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1053\" class=\"size-medium wp-image-1053\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5570-L17-4-300x199.jpg\" alt=\"Plagiophyllum diffusum. From York Haven, PA. Age L.Triassic.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5570-L17-4-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5570-L17-4-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5570-L17-4-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5570-L17-4-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1053\" class=\"wp-caption-text\">L17-4: Plagiophyllum diffusum.<br \/>From York Haven, PA. Age L.Triassic.<\/p><\/div>\n<div id=\"attachment_1054\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5571-L17-4.jpg\" rel=\"attachment wp-att-1054\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1054\" class=\"size-medium wp-image-1054\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5571-L17-4-300x199.jpg\" alt=\"Plagiophyllum diffusum. From York Haven, PA. Age L.Triassic.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5571-L17-4-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5571-L17-4-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5571-L17-4-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5571-L17-4-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1054\" class=\"wp-caption-text\">L17-4: Plagiophyllum diffusum.<br \/>From York Haven, PA. Age L.Triassic.<\/p><\/div>\n<div id=\"attachment_1058\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5576-L17-5.jpg\" rel=\"attachment wp-att-1058\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1058\" class=\"size-medium wp-image-1058\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5576-L17-5-300x199.jpg\" alt=\"Missing info.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5576-L17-5-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5576-L17-5-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5576-L17-5-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5576-L17-5-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1058\" class=\"wp-caption-text\">L17-6: Dinophyton, pin-wheel from York Haven, Pa. Age Triassic.<\/p><\/div>\n<div id=\"attachment_1060\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5579-L17-7.jpg\" rel=\"attachment wp-att-1060\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1060\" class=\"size-medium wp-image-1060\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5579-L17-7-300x199.jpg\" alt=\"Glyptolepis. From York Haven, PA. Age Triassic.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5579-L17-7-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5579-L17-7-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5579-L17-7-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5579-L17-7-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1060\" class=\"wp-caption-text\">L17-7: Glyptolepis.<br \/>From York Haven, PA. Age Triassic.<\/p><\/div>\n<div id=\"attachment_1062\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5581-L17-9.jpg\" rel=\"attachment wp-att-1062\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1062\" class=\"size-medium wp-image-1062\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5581-L17-9-300x199.jpg\" alt=\"Araucaria longifolia. From Wyoming. Rock Sprins Fm. Age U. Cretaceous.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5581-L17-9-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5581-L17-9-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5581-L17-9-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5581-L17-9-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1062\" class=\"wp-caption-text\">L17-9: Araucaria longifolia.<br \/>From Wyoming. Rock Sprins Fm. Age U. Cretaceous.<\/p><\/div>\n<div id=\"attachment_1066\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5586-L17-10.jpg\" rel=\"attachment wp-att-1066\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1066\" class=\"size-medium wp-image-1066\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5586-L17-10-300x199.jpg\" alt=\"Araucaria ? From New Mexico. Kirtland Fm. Age U. Cretaceous.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5586-L17-10-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5586-L17-10-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5586-L17-10-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5586-L17-10-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1066\" class=\"wp-caption-text\">L17-10: Araucaria ?<br \/>From New Mexico. Kirtland Fm. Age U. Cretaceous.<\/p><\/div>\n<div id=\"attachment_1067\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5588-L17-11.jpg\" rel=\"attachment wp-att-1067\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1067\" class=\"size-medium wp-image-1067\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5588-L17-11-300x199.jpg\" alt=\"Araucaria sphaerocarpa. Peel of holotype from BMNH, showing l.s. of cone Carruthers 1866.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5588-L17-11-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5588-L17-11-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5588-L17-11-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5588-L17-11-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1067\" class=\"wp-caption-text\">L17-11: Araucaria sphaerocarpa.<br \/>Peel of holotype from BMNH, showing l.s. of cone Carruthers 1866.<\/p><\/div>\n<div id=\"attachment_1074\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5595-L17-12.jpg\" rel=\"attachment wp-att-1074\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1074\" class=\"size-medium wp-image-1074\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5595-L17-12-300x199.jpg\" alt=\"Araucaria mirabilis. 1\/4 of a cone. From Cerro Cuadrado, Patagonia. Age Jurassic. \" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5595-L17-12-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5595-L17-12-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5595-L17-12-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5595-L17-12-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1074\" class=\"wp-caption-text\">L17-12: Araucaria mirabilis.<br \/>1\/4 of a cone. From Cerro Cuadrado, Patagonia. Age Jurassic.<\/p><\/div>\n<div id=\"attachment_1076\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5597-L17-12.jpg\" rel=\"attachment wp-att-1076\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1076\" class=\"size-medium wp-image-1076\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5597-L17-12-300x199.jpg\" alt=\"Araucaria mirabilis. 1\/4 of a cone. From Cerro Cuadrado, Patagonia. Age Jurassic. \" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5597-L17-12-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5597-L17-12-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5597-L17-12-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5597-L17-12-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1076\" class=\"wp-caption-text\">L17-12: Araucaria mirabilis.<br \/>1\/4 of a cone. From Cerro Cuadrado, Patagonia. Age Jurassic.<\/p><\/div>\n<div id=\"attachment_1079\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5601-L17-16.jpg\" rel=\"attachment wp-att-1079\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1079\" class=\"size-medium wp-image-1079\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5601-L17-16-300x199.jpg\" alt=\"Pinus. Showing 3 needle fasicle. From Princeton, BC. Age M. Eocene. \" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5601-L17-16-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5601-L17-16-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5601-L17-16-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5601-L17-16-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1079\" class=\"wp-caption-text\">L17-16: Pinus.<br \/>Showing 3 needle fasicle. From Princeton, BC. Age M. Eocene.<\/p><\/div>\n<div id=\"attachment_1080\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5603-L17-17.jpg\" rel=\"attachment wp-att-1080\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1080\" class=\"size-medium wp-image-1080\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5603-L17-17-300x199.jpg\" alt=\"Pinus. showing fasicle of leaves, collected by M. Wilson, 1975. From Smithers, BC. Age M.Eocene. \" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5603-L17-17-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5603-L17-17-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5603-L17-17-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5603-L17-17-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1080\" class=\"wp-caption-text\">L17-17: Pinus.<br \/>showing fasicle of needles, collected by M. Wilson, 1975. From Smithers, BC. Age M.Eocene.<\/p><\/div>\n<div id=\"attachment_1082\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5607-L17-19.jpg\" rel=\"attachment wp-att-1082\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1082\" class=\"size-medium wp-image-1082\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5607-L17-19-300x199.jpg\" alt=\"Pinus leaves. From Princeton, BC. Allenby Fm. Age M. Eocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5607-L17-19-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5607-L17-19-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5607-L17-19-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5607-L17-19-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1082\" class=\"wp-caption-text\">L17-19: Pinus needles.<br \/>From Princeton, BC. Allenby Fm. Age M. Eocene.<\/p><\/div>\n<div id=\"attachment_1085\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5613-L17-23.jpg\" rel=\"attachment wp-att-1085\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1085\" class=\"size-medium wp-image-1085\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5613-L17-23-300x199.jpg\" alt=\"Pinus arnoldii cone. Peels showing different anatomical features. From Princeton, BC. Allenby Fm. Age M. Eocene. \" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5613-L17-23-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5613-L17-23-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5613-L17-23-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5613-L17-23-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1085\" class=\"wp-caption-text\">L17-23: Pinus arnoldii cone.<br \/>Peels showing different anatomical features. From Princeton, BC. Allenby Fm. Age M. Eocene.<\/p><\/div>\n<div id=\"attachment_1086\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5614-L17-23.jpg\" rel=\"attachment wp-att-1086\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1086\" class=\"size-medium wp-image-1086\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5614-L17-23-300x199.jpg\" alt=\"Pinus arnoldii cone. Peels showing different anatomical features. From Princeton, BC. Allenby Fm. Age M. Eocene. \" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5614-L17-23-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5614-L17-23-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5614-L17-23-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5614-L17-23-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1086\" class=\"wp-caption-text\">L17-23: Pinus arnoldii cone.<br \/>Peels showing different anatomical features. From Princeton, BC. Allenby Fm. Age M. Eocene.<\/p><\/div>\n<div id=\"attachment_1087\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5615-L17-23.jpg\" rel=\"attachment wp-att-1087\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1087\" class=\"size-medium wp-image-1087\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5615-L17-23-300x199.jpg\" alt=\"Pinus arnoldii cone. Peels showing different anatomical features. From Princeton, BC. Allenby Fm. Age M. Eocene. \" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5615-L17-23-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5615-L17-23-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5615-L17-23-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5615-L17-23-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1087\" class=\"wp-caption-text\">L17-23: Pinus arnoldii cone.<br \/>Peels showing different anatomical features. From Princeton, BC. Allenby Fm. Age M. Eocene.<\/p><\/div>\n<div id=\"attachment_1088\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5616-L17-23.jpg\" rel=\"attachment wp-att-1088\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1088\" class=\"size-medium wp-image-1088\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5616-L17-23-300x199.jpg\" alt=\"Pinus arnoldii cone. Peels showing different anatomical features. From Princeton, BC. Allenby Fm. Age M. Eocene. \" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5616-L17-23-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5616-L17-23-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5616-L17-23-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/02\/PJC_5616-L17-23-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1088\" class=\"wp-caption-text\">L17-23: Pinus arnoldii cone.<br \/>Peels showing different anatomical features. From Princeton, BC. Allenby Fm. Age M. Eocene.<\/p><\/div>\n<div id=\"attachment_1298\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5619-L17-24.jpg\" rel=\"attachment wp-att-1298\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1298\" class=\"size-medium wp-image-1298\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5619-L17-24-300x199.jpg\" alt=\"Pinus arnoldii cone. From Princeton, BC. Allenby Fm. Age M. Eocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5619-L17-24-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5619-L17-24-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5619-L17-24-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5619-L17-24-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1298\" class=\"wp-caption-text\">L17-24: Pinus arnoldii cone.<br \/>From Princeton, BC. Allenby Fm. Age M. Eocene.<\/p><\/div>\n<div id=\"attachment_1299\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5621-L17-25.jpg\" rel=\"attachment wp-att-1299\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1299\" class=\"size-medium wp-image-1299\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5621-L17-25-300x199.jpg\" alt=\"Conifer cone. From Genesee, AB. Paskapoo Fm.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5621-L17-25-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5621-L17-25-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5621-L17-25-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5621-L17-25-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1299\" class=\"wp-caption-text\">L17-25: Conifer cone.<br \/>From Genesee, AB. Paskapoo Fm.<\/p><\/div>\n<div id=\"attachment_1300\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5622-L17-25.jpg\" rel=\"attachment wp-att-1300\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1300\" class=\"size-medium wp-image-1300\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5622-L17-25-300x199.jpg\" alt=\"Conifer cone. From Genesee, AB. Paskapoo Fm.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5622-L17-25-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5622-L17-25-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5622-L17-25-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5622-L17-25-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1300\" class=\"wp-caption-text\">L17-26: Conifer cone.<br \/>From Genesee, AB. Paskapoo Fm.<\/p><\/div>\n<div id=\"attachment_1301\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5624-L17-27.jpg\" rel=\"attachment wp-att-1301\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1301\" class=\"size-medium wp-image-1301\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5624-L17-27-300x199.jpg\" alt=\"Casts of Cone\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5624-L17-27-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5624-L17-27-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5624-L17-27-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5624-L17-27-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1301\" class=\"wp-caption-text\">L17-27: Casts of Cone<\/p><\/div>\n<div id=\"attachment_1302\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5626-L17-28.jpg\" rel=\"attachment wp-att-1302\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1302\" class=\"size-medium wp-image-1302\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5626-L17-28-300x199.jpg\" alt=\"Cones from ?\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5626-L17-28-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5626-L17-28-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5626-L17-28-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5626-L17-28-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1302\" class=\"wp-caption-text\">L17-28: Cones from Auberlam ? Germany. Age Mio-Pliocene.<\/p><\/div>\n<div id=\"attachment_1303\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5627-L17-28.jpg\" rel=\"attachment wp-att-1303\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1303\" class=\"size-medium wp-image-1303\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5627-L17-28-300x199.jpg\" alt=\"Cones from ?\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5627-L17-28-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5627-L17-28-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5627-L17-28-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5627-L17-28-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1303\" class=\"wp-caption-text\">L17-28: Cones from Auberlam ? Germany. Age Mio-Pliocene<\/p><\/div>\n<div id=\"attachment_1304\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5629-L17-29.jpg\" rel=\"attachment wp-att-1304\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1304\" class=\"size-medium wp-image-1304\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5629-L17-29-300x199.jpg\" alt=\"Pinus seed. From BC. Tranquille Fm. Age M. Eocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5629-L17-29-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5629-L17-29-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5629-L17-29-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5629-L17-29-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1304\" class=\"wp-caption-text\">L17-29: Pinus seed.<br \/>From BC. Tranquille Fm. Age M. Eocene.<\/p><\/div>\n<div id=\"attachment_1305\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5631-L17-30.jpg\" rel=\"attachment wp-att-1305\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1305\" class=\"size-medium wp-image-1305\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5631-L17-30-300x199.jpg\" alt=\"Pinaceous seed. From Princeton, BC. Allenby Fm. Age M. Eocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5631-L17-30-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5631-L17-30-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5631-L17-30-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5631-L17-30-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1305\" class=\"wp-caption-text\">L17-30: Pinaceous seed.<br \/>From Princeton, BC. Allenby Fm. Age M. Eocene.<\/p><\/div>\n<div id=\"attachment_1306\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5633-L17-32.jpg\" rel=\"attachment wp-att-1306\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1306\" class=\"size-medium wp-image-1306\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5633-L17-32-300x199.jpg\" alt=\"Picea seed. From Princeton, BC. Age Eocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5633-L17-32-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5633-L17-32-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5633-L17-32-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5633-L17-32-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1306\" class=\"wp-caption-text\">L17-32: Picea seed.<br \/>From Princeton, BC. Age Eocene.<\/p><\/div>\n<div id=\"attachment_1309\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5637-L17-33.jpg\" rel=\"attachment wp-att-1309\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1309\" class=\"size-medium wp-image-1309\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5637-L17-33-300x199.jpg\" alt=\"Abies sp. seed. From Princeton, BC. Age Eocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5637-L17-33-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5637-L17-33-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5637-L17-33-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5637-L17-33-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1309\" class=\"wp-caption-text\">L17-33: Abies sp. seed.<br \/>From Princeton, BC. Age Eocene.<\/p><\/div>\n<div id=\"attachment_1310\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5639-L17-33.jpg\" rel=\"attachment wp-att-1310\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1310\" class=\"size-medium wp-image-1310\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5639-L17-33-300x199.jpg\" alt=\"Abies sp. seed. From Princeton, BC. Age Eocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5639-L17-33-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5639-L17-33-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5639-L17-33-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5639-L17-33-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1310\" class=\"wp-caption-text\">L17-33: Abies sp. seed.<br \/>From Princeton, BC. Age Eocene.<\/p><\/div>\n<div id=\"attachment_1311\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5642-L17-34.jpg\" rel=\"attachment wp-att-1311\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1311\" class=\"size-medium wp-image-1311\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5642-L17-34-300x199.jpg\" alt=\"Pinus pollen cone? From Blakeburn Mine, BC. Age Eocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5642-L17-34-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5642-L17-34-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5642-L17-34-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5642-L17-34-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1311\" class=\"wp-caption-text\">L17-34: Pinus? pollen cone<br \/>From Blakeburn Mine, BC. Age Eocene.<\/p><\/div>\n<div id=\"attachment_1312\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5643-L17-34.jpg\" rel=\"attachment wp-att-1312\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1312\" class=\"size-medium wp-image-1312\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5643-L17-34-300x199.jpg\" alt=\"Pinus pollen cone? From Blakeburn Mine, BC. Age Eocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5643-L17-34-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5643-L17-34-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5643-L17-34-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5643-L17-34-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1312\" class=\"wp-caption-text\">L17-34: Pinus? pollen cone<br \/>From Blakeburn Mine, BC. Age Eocene.<\/p><\/div>\n<div id=\"attachment_1313\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5645-L17-35.jpg\" rel=\"attachment wp-att-1313\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1313\" class=\"size-medium wp-image-1313\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5645-L17-35-300x199.jpg\" alt=\"Pseudolarix americana. From Republic, WA, USA. Klondike Mt. Fm. Age Eocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5645-L17-35-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5645-L17-35-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5645-L17-35-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5645-L17-35-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1313\" class=\"wp-caption-text\">L17-35: Pseudolarix americana.<br \/>From Republic, WA, USA. Klondike Mt. Fm. Age Eocene.<\/p><\/div>\n<div id=\"attachment_1314\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5647-L17-36.jpg\" rel=\"attachment wp-att-1314\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1314\" class=\"size-medium wp-image-1314\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5647-L17-36-300x199.jpg\" alt=\"Elatocladus. From Alberta. Age U. Cretaceous.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5647-L17-36-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5647-L17-36-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5647-L17-36-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5647-L17-36-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1314\" class=\"wp-caption-text\">L17-36: Elatocladus.<br \/>From Alberta. Age U. Cretaceous.<\/p><\/div>\n<div id=\"attachment_1316\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5650-L17-38.jpg\" rel=\"attachment wp-att-1316\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1316\" class=\"size-medium wp-image-1316\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5650-L17-38-300x199.jpg\" alt=\"Cupressinocladus &amp; Glyptostrobus europaeus. Holotype? From Smoky Tower, AB. Paskapoo Fm. Age Paleocene. \" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5650-L17-38-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5650-L17-38-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5650-L17-38-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5650-L17-38-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1316\" class=\"wp-caption-text\">L17-38: Cupressinocladus &amp; Glyptostrobus europaeus.<br \/>Holotype? From Smoky Tower, AB. Paskapoo Fm. Age Paleocene.<\/p><\/div>\n<div id=\"attachment_1324\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5662-L17-39.jpg\" rel=\"attachment wp-att-1324\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1324\" class=\"size-medium wp-image-1324\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5662-L17-39-300x199.jpg\" alt=\"Cupressinocladus. From Alberta. Age Paleocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5662-L17-39-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5662-L17-39-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5662-L17-39-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5662-L17-39-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1324\" class=\"wp-caption-text\">L17-39: Cupressinocladus.<br \/>From Alberta. Age Paleocene.<\/p><\/div>\n<div id=\"attachment_1319\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5654-L17-40.jpg\" rel=\"attachment wp-att-1319\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1319\" class=\"size-medium wp-image-1319\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5654-L17-40-300x199.jpg\" alt=\"Cupressinocladus. Broken specimen. From Smoky Tower, AB. Age Paleocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5654-L17-40-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5654-L17-40-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5654-L17-40-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5654-L17-40-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1319\" class=\"wp-caption-text\">L17-40: Cupressinocladus.<br \/>Broken specimen. From Smoky Tower, AB. Age Paleocene.<\/p><\/div>\n<div id=\"attachment_1321\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5657-L17-41.jpg\" rel=\"attachment wp-att-1321\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1321\" class=\"size-medium wp-image-1321\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5657-L17-41-300x199.jpg\" alt=\"Cedar family. From McAbee site, BC. Age M. Eocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5657-L17-41-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5657-L17-41-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5657-L17-41-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5657-L17-41-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1321\" class=\"wp-caption-text\">L17-41: Cedar family.<br \/>From McAbee site, BC. Age M. Eocene.<\/p><\/div>\n<div id=\"attachment_1325\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5664-L17-42.jpg\" rel=\"attachment wp-att-1325\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1325\" class=\"size-medium wp-image-1325\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5664-L17-42-300x199.jpg\" alt=\"Taxodioxylon (Metasequoia). From Drumheller, AB. Age U. Cretaceous.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5664-L17-42-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5664-L17-42-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5664-L17-42-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5664-L17-42-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1325\" class=\"wp-caption-text\">L17-42: Taxodioxylon (Metasequoia).<br \/>From Drumheller, AB. Age U. Cretaceous.<\/p><\/div>\n<div id=\"attachment_1328\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5668-L17-43.jpg\" rel=\"attachment wp-att-1328\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1328\" class=\"size-medium wp-image-1328\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5668-L17-43-300x199.jpg\" alt=\"Metasequoia occidentalis. From Smoky Tower, AB. Age Paleocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5668-L17-43-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5668-L17-43-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5668-L17-43-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5668-L17-43-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1328\" class=\"wp-caption-text\">L17-43: Metasequoia occidentalis.<br \/>From Smoky Tower, AB. Age Paleocene.<\/p><\/div>\n<div id=\"attachment_1331\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5672-L17-44.jpg\" rel=\"attachment wp-att-1331\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1331\" class=\"size-medium wp-image-1331\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5672-L17-44-300x199.jpg\" alt=\"Metasequoia occidentalis. From Smoky Tower, AB. Age Paleocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5672-L17-44-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5672-L17-44-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5672-L17-44-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5672-L17-44-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1331\" class=\"wp-caption-text\">L17-44: Metasequoia occidentalis.<br \/>From Smoky Tower, AB. Age Paleocene.<\/p><\/div>\n<div id=\"attachment_1335\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5677L17-45.jpg\" rel=\"attachment wp-att-1335\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1335\" class=\"size-medium wp-image-1335\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5677L17-45-300x199.jpg\" alt=\"Metasequoia occidentalis. From Smoky Tower, AB. Age Paleocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5677L17-45-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5677L17-45-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5677L17-45-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5677L17-45-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1335\" class=\"wp-caption-text\">L17-45: Metasequoia occidentalis.<br \/>From Smoky Tower, AB. Age Paleocene.<\/p><\/div>\n<div id=\"attachment_1337\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5680-L17-46.jpg\" rel=\"attachment wp-att-1337\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1337\" class=\"size-medium wp-image-1337\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5680-L17-46-300x199.jpg\" alt=\"Metasequoia occidentalis. From Genesee, AB. Scollard Fm. Age Paleocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5680-L17-46-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5680-L17-46-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5680-L17-46-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5680-L17-46-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1337\" class=\"wp-caption-text\">L17-46: Metasequoia occidentalis.<br \/>From Genesee, AB. Scollard Fm. Age Paleocene.<\/p><\/div>\n<div id=\"attachment_1338\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5682-L17-47.jpg\" rel=\"attachment wp-att-1338\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1338\" class=\"size-medium wp-image-1338\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5682-L17-47-300x199.jpg\" alt=\"Metasequoia occidentalis. From Genesee, AB. Scollard Fm. Age Paleocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5682-L17-47-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5682-L17-47-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5682-L17-47-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5682-L17-47-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1338\" class=\"wp-caption-text\">L17-47: Metasequoia occidentalis.<br \/>From Genesee, AB. Scollard Fm. Age Paleocene.<\/p><\/div>\n<div id=\"attachment_1339\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5684-L17-48.jpg\" rel=\"attachment wp-att-1339\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1339\" class=\"size-medium wp-image-1339\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5684-L17-48-300x199.jpg\" alt=\"Metasequoia occidentalis. From Genesee, AB. Scollard Fm. Age Paleocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5684-L17-48-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5684-L17-48-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5684-L17-48-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5684-L17-48-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1339\" class=\"wp-caption-text\">L17-48: Metasequoia occidentalis.<br \/>From Genesee, AB. Scollard Fm. Age Paleocene.<\/p><\/div>\n<div id=\"attachment_1343\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5693-L17-49.jpg\" rel=\"attachment wp-att-1343\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1343\" class=\"size-medium wp-image-1343\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5693-L17-49-300x199.jpg\" alt=\"Metasequoia occidentalis. From Genesee, AB. Scollard Fm. Age Paleocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5693-L17-49-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5693-L17-49-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5693-L17-49-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5693-L17-49-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1343\" class=\"wp-caption-text\">L17-49: Metasequoia occidentalis.<br \/>From Genesee, AB. Scollard Fm. Age Paleocene.<\/p><\/div>\n<div id=\"attachment_1346\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5696-L17-50.jpg\" rel=\"attachment wp-att-1346\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1346\" class=\"size-medium wp-image-1346\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5696-L17-50-300x199.jpg\" alt=\"Metasequoia occidentalis. From Genesee, AB. Scollard Fm. Age Paleocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5696-L17-50-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5696-L17-50-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5696-L17-50-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5696-L17-50-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1346\" class=\"wp-caption-text\">L17-50: Metasequoia occidentalis.<br \/>From Genesee, AB. Scollard Fm. Age Paleocene.<\/p><\/div>\n<div id=\"attachment_1348\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5698-L17-51.jpg\" rel=\"attachment wp-att-1348\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1348\" class=\"size-medium wp-image-1348\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5698-L17-51-300x199.jpg\" alt=\"Metasequoia occidentalis. From Genesee, AB. Scollard Fm. Age Paleocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5698-L17-51-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5698-L17-51-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5698-L17-51-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5698-L17-51-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1348\" class=\"wp-caption-text\">L17-51: Metasequoia occidentalis.<br \/>From Genesee, AB. Scollard Fm. Age Paleocene.<\/p><\/div>\n<div id=\"attachment_1352\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5702-L17-52.jpg\" rel=\"attachment wp-att-1352\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1352\" class=\"size-medium wp-image-1352\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5702-L17-52-300x199.jpg\" alt=\"Metasequoia foliage. From Joffre Bridge, AB. Paskapoo Fm. Age Paleocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5702-L17-52-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5702-L17-52-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5702-L17-52-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5702-L17-52-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1352\" class=\"wp-caption-text\">L17-52: Metasequoia foliage.<br \/>From Joffre Bridge, AB. Paskapoo Fm. Age Paleocene.<\/p><\/div>\n<div id=\"attachment_1354\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5704-L17-53.jpg\" rel=\"attachment wp-att-1354\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1354\" class=\"size-medium wp-image-1354\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5704-L17-53-300x199.jpg\" alt=\"Metasequoia leaf. From Joffre Bridge, AB. Paskapoo Fm. Age Paleocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5704-L17-53-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5704-L17-53-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5704-L17-53-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5704-L17-53-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1354\" class=\"wp-caption-text\">L17-53: Metasequoia leaf.<br \/>From Joffre Bridge, AB. Paskapoo Fm. Age Paleocene.<\/p><\/div>\n<div id=\"attachment_1357\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5708-L17-54.jpg\" rel=\"attachment wp-att-1357\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1357\" class=\"size-medium wp-image-1357\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5708-L17-54-300x199.jpg\" alt=\"Metasequoia occidentalis. From Battle Bluff, BC. Age M.Eocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5708-L17-54-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5708-L17-54-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5708-L17-54-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5708-L17-54-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1357\" class=\"wp-caption-text\">L17-54: Metasequoia occidentalis.<br \/>From Battle Bluff, BC. Age M.Eocene.<\/p><\/div>\n<div id=\"attachment_1358\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5710-L17-55.jpg\" rel=\"attachment wp-att-1358\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1358\" class=\"size-medium wp-image-1358\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5710-L17-55-300x199.jpg\" alt=\"Metasequoia occidentalis. From Republic, WA, USA. Klondike Mt. Fm. Age M. Eocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5710-L17-55-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5710-L17-55-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5710-L17-55-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5710-L17-55-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1358\" class=\"wp-caption-text\">L17-55: Metasequoia occidentalis.<br \/>From Republic, WA, USA. Klondike Mt. Fm. Age M. Eocene.<\/p><\/div>\n<div id=\"attachment_1404\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5771-L17-56.jpg\" rel=\"attachment wp-att-1404\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1404\" class=\"size-medium wp-image-1404\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5771-L17-56-300x199.jpg\" alt=\"Metasequoia cones. Unknown location.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5771-L17-56-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5771-L17-56-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5771-L17-56-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5771-L17-56-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1404\" class=\"wp-caption-text\">L17-56: Metasequoia cones. From the Drumheller area.<\/p><\/div>\n<div id=\"attachment_1360\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5714-L17-57.jpg\" rel=\"attachment wp-att-1360\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1360\" class=\"size-medium wp-image-1360\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5714-L17-57-300x199.jpg\" alt=\"Taxodiaceae occidentalis. From Drumheller, AB. HSC Fm. Age U. Cretaceous.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5714-L17-57-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5714-L17-57-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5714-L17-57-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5714-L17-57-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1360\" class=\"wp-caption-text\">L17-57: Taxodiaceae occidentalis.<br \/>From Drumheller, AB. HSC Fm. Age U. Cretaceous.<\/p><\/div>\n<div id=\"attachment_1362\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5717-L17-58.jpg\" rel=\"attachment wp-att-1362\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1362\" class=\"size-medium wp-image-1362\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5717-L17-58-300x199.jpg\" alt=\"Metasequoia milleri seed cones. Peels. From Princeton, BC. Allenby Fm. Age M. Eocene. \" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5717-L17-58-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5717-L17-58-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5717-L17-58-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5717-L17-58-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1362\" class=\"wp-caption-text\">L17-58: Metasequoia milleri seed cones.<br \/>Peels. From Princeton, BC. Allenby Fm. Age M. Eocene.<\/p><\/div>\n<div id=\"attachment_1391\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5755-L17-59.jpg\" rel=\"attachment wp-att-1391\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1391\" class=\"size-medium wp-image-1391\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5755-L17-59-300x199.jpg\" alt=\"Taxodiaceae cones. From Drumheller, AB. Horseshoe Canyon Fm. Age U. Cretaceous.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5755-L17-59-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5755-L17-59-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5755-L17-59-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5755-L17-59-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1391\" class=\"wp-caption-text\">L17-59: Taxodiaceae cones.<br \/>From Drumheller, AB. Horseshoe Canyon Fm. Age U. Cretaceous.<\/p><\/div>\n<div id=\"attachment_1369\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5725-L17-60.jpg\" rel=\"attachment wp-att-1369\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1369\" class=\"size-medium wp-image-1369\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5725-L17-60-300x199.jpg\" alt=\"Metasequoia occidentalis cone. From Drumheller, AB. HSC Fm. Age U. Cretaceous.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5725-L17-60-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5725-L17-60-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5725-L17-60-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5725-L17-60-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1369\" class=\"wp-caption-text\">L17-60: Metasequoia occidentalis cone.<br \/>From Drumheller, AB. HSC Fm. Age U. Cretaceous.<\/p><\/div>\n<div id=\"attachment_1371\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5728-L17-61.jpg\" rel=\"attachment wp-att-1371\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1371\" class=\"size-medium wp-image-1371\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5728-L17-61-300x199.jpg\" alt=\"Metasequoia occidentalis cone. From Genesee, AB. Paskapoo Fm. Age Paleocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5728-L17-61-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5728-L17-61-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5728-L17-61-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5728-L17-61-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1371\" class=\"wp-caption-text\">L17-61: Metasequoia occidentalis cone.<br \/>From Genesee, AB. Paskapoo Fm. Age Paleocene.<\/p><\/div>\n<div id=\"attachment_1372\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5730-L17-62a.jpg\" rel=\"attachment wp-att-1372\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1372\" class=\"size-medium wp-image-1372\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5730-L17-62a-300x199.jpg\" alt=\"Metasequoia cones. From Sundance Mine, Lake Wabamun. Scollard Fm. Age Paleocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5730-L17-62a-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5730-L17-62a-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5730-L17-62a-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5730-L17-62a-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1372\" class=\"wp-caption-text\">L17-62a: Metasequoia cones.<br \/>From Sundance Mine, Lake Wabamun. Scollard Fm. Age Paleocene.<\/p><\/div>\n<div id=\"attachment_1379\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5739-L17-63.jpg\" rel=\"attachment wp-att-1379\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1379\" class=\"size-medium wp-image-1379\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5739-L17-63-300x199.jpg\" alt=\"Metasequoia foxii and Paleocarpinus joffrensis. From Joffre Bridge, AB. Age Paleocene. \" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5739-L17-63-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5739-L17-63-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5739-L17-63-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5739-L17-63-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1379\" class=\"wp-caption-text\">L17-63: Metasequoia foxii and Paleocarpinus joffrensis.<br \/>From Joffre Bridge, AB. Age Paleocene.<\/p><\/div>\n<div id=\"attachment_1385\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5746-L17-65.jpg\" rel=\"attachment wp-att-1385\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1385\" class=\"size-medium wp-image-1385\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5746-L17-65-300x199.jpg\" alt=\"Metasequoia foxii. Broken. Coll by Betty Speirs. From Joffre Bridge, AB. Age Paleocene. \" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5746-L17-65-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5746-L17-65-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5746-L17-65-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5746-L17-65-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1385\" class=\"wp-caption-text\">L17-65: Metasequoia foxii.<br \/>Broken. Coll by Betty Speirs. From Joffre Bridge, AB. Age Paleocene.<\/p><\/div>\n<div id=\"attachment_1386\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5748-L17-66.jpg\" rel=\"attachment wp-att-1386\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1386\" class=\"size-medium wp-image-1386\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5748-L17-66-300x199.jpg\" alt=\"Metasequoia foxii. From Joffre Bridge, AB. Age Paleocene. \" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5748-L17-66-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5748-L17-66-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5748-L17-66-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5748-L17-66-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1386\" class=\"wp-caption-text\">L17-66: Metasequoia foxii.<br \/>From Joffre Bridge, AB. Age Paleocene.<\/p><\/div>\n<div id=\"attachment_1388\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5751-L17-68.jpg\" rel=\"attachment wp-att-1388\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1388\" class=\"size-medium wp-image-1388\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5751-L17-68-300x199.jpg\" alt=\"Glyptostrobus sp. From Smoky Tower, AB. Paskapoo Fm. Age Paleocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5751-L17-68-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5751-L17-68-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5751-L17-68-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5751-L17-68-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1388\" class=\"wp-caption-text\">L17-68: Glyptostrobus sp.<br \/>From Smoky Tower, AB. Paskapoo Fm. Age Paleocene.<\/p><\/div>\n<div id=\"attachment_1393\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5758-L17-69.jpg\" rel=\"attachment wp-att-1393\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1393\" class=\"size-medium wp-image-1393\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5758-L17-69-300x199.jpg\" alt=\"Glyptostrobus europaeus. From Smoky Tower, AB. Paskapoo Fm. Age Paleocene. \" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5758-L17-69-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5758-L17-69-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5758-L17-69-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5758-L17-69-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1393\" class=\"wp-caption-text\">L17-69: Glyptostrobus europaeus.<br \/>From Smoky Tower, AB. Paskapoo Fm. Age Paleocene.<\/p><\/div>\n<div id=\"attachment_1397\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5763-L17-70.jpg\" rel=\"attachment wp-att-1397\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1397\" class=\"size-medium wp-image-1397\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5763-L17-70-300x199.jpg\" alt=\"Glyptostrobus europaeus. From Joffre Bridge, AB. Paskapoo Fm. Age Paleocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5763-L17-70-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5763-L17-70-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5763-L17-70-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5763-L17-70-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1397\" class=\"wp-caption-text\">L17-70: Glyptostrobus europaeus.<br \/>From Joffre Bridge, AB. Paskapoo Fm. Age Paleocene.<\/p><\/div>\n<div id=\"attachment_1419\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5798-L17-71.jpg\" rel=\"attachment wp-att-1419\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1419\" class=\"size-medium wp-image-1419\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5798-L17-71-300x199.jpg\" alt=\"Glyptostrobus sp. Specimen with foliage and pollen cone? From Smithers, BC. Age M.Eocene. \" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5798-L17-71-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5798-L17-71-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5798-L17-71-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5798-L17-71-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1419\" class=\"wp-caption-text\">L17-71: Glyptostrobus sp.<br \/>Specimen with foliage and pollen cone? From Smithers, BC. Age M.Eocene.<\/p><\/div>\n<div id=\"attachment_1405\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5773-L17-72.jpg\" rel=\"attachment wp-att-1405\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1405\" class=\"size-medium wp-image-1405\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5773-L17-72-300x199.jpg\" alt=\"Glyptostrobus sp. From Smithers, BC. Age M.Eocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5773-L17-72-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5773-L17-72-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5773-L17-72-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5773-L17-72-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1405\" class=\"wp-caption-text\">L17-72: Glyptostrobus sp.<br \/>From Smithers, BC. Age M.Eocene.<\/p><\/div>\n<div id=\"attachment_1406\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5776-L17-73.jpg\" rel=\"attachment wp-att-1406\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1406\" class=\"size-medium wp-image-1406\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5776-L17-73-300x199.jpg\" alt=\"Glyptostrobus sp. \" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5776-L17-73-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5776-L17-73-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5776-L17-73-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5776-L17-73-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1406\" class=\"wp-caption-text\">L17-73: Glyptostrobus sp.<\/p><\/div>\n<div id=\"attachment_1409\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5784-L17-74.jpg\" rel=\"attachment wp-att-1409\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1409\" class=\"size-medium wp-image-1409\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5784-L17-74-300x199.jpg\" alt=\"Taxodiophyllum. From China Creek, BC. Age M.Eocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5784-L17-74-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5784-L17-74-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5784-L17-74-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5784-L17-74-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1409\" class=\"wp-caption-text\">L17-74: Taxodiophyllum.<br \/>From China Creek, BC. Age M.Eocene.<\/p><\/div>\n<div id=\"attachment_1407\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5779-L17-75.jpg\" rel=\"attachment wp-att-1407\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1407\" class=\"size-medium wp-image-1407\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5779-L17-75-300x199.jpg\" alt=\"Taxodiophyllum. From Princeton, BC. Age M.Eocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5779-L17-75-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5779-L17-75-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5779-L17-75-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5779-L17-75-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1407\" class=\"wp-caption-text\">L17-75: Taxodiophyllum.<br \/>From Princeton, BC. Age M.Eocene.<\/p><\/div>\n<div id=\"attachment_1422\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5802-L17-76.jpg\" rel=\"attachment wp-att-1422\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1422\" class=\"size-medium wp-image-1422\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5802-L17-76-300x199.jpg\" alt=\"Taxodiaceous cone. From Collawash River, Oregon. Age E.Miocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5802-L17-76-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5802-L17-76-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5802-L17-76-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5802-L17-76-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1422\" class=\"wp-caption-text\">L17-76: Taxodiaceous cone.<br \/>From Collawash River, Oregon. Age E.Miocene.<\/p><\/div>\n<div id=\"attachment_1410\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5786-L17-77.jpg\" rel=\"attachment wp-att-1410\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1410\" class=\"size-medium wp-image-1410\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5786-L17-77-300x199.jpg\" alt=\"Pararaucaria patagonica. Similar to Taxodiaceae. Cerro Cuadrado, Patagonia. Age Jurassic. \" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5786-L17-77-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5786-L17-77-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5786-L17-77-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5786-L17-77-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1410\" class=\"wp-caption-text\">L17-78: Pararaucaria patagonica.<br \/>Similar to Taxodiaceae. Cerro Cuadrado, Patagonia. Age Jurassic.<\/p><\/div>\n<div id=\"attachment_1424\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5805-L17-78.jpg\" rel=\"attachment wp-att-1424\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1424\" class=\"size-medium wp-image-1424\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5805-L17-78-300x199.jpg\" alt=\"Glyptostrobus &amp; Sciatopitophyllum canadense. From Smoky Tower, AB. Paskapoo Fm. Age Paleocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5805-L17-78-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5805-L17-78-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5805-L17-78-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5805-L17-78-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1424\" class=\"wp-caption-text\">L17-79: L17-82: Glyptostrobus &amp; Sciatopitophyllum canadense.<br \/>From Smoky Tower, AB. Paskapoo Fm. Age Paleocene.<\/p><\/div>\n<div id=\"attachment_1428\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5811-L17-82.jpg\" rel=\"attachment wp-att-1428\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1428\" class=\"size-medium wp-image-1428\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5811-L17-82-300x199.jpg\" alt=\"Radial section of a trunk.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5811-L17-82-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5811-L17-82-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5811-L17-82-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5811-L17-82-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1428\" class=\"wp-caption-text\">L17-82: Radial section of a trunk.<\/p><\/div>\n<div id=\"attachment_1417\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5794-L17-83.jpg\" rel=\"attachment wp-att-1417\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1417\" class=\"size-medium wp-image-1417\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5794-L17-83-300x199.jpg\" alt=\"Taxodioxylon sp. From Drumheller, AB. U. Cretaceous.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5794-L17-83-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5794-L17-83-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5794-L17-83-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5794-L17-83-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1417\" class=\"wp-caption-text\">L17-83: Taxodioxylon sp.<br \/>From Drumheller, AB. U. Cretaceous.<\/p><\/div>\n<div id=\"attachment_1431\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5816-L17-87-type.jpg\" rel=\"attachment wp-att-1431\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1431\" class=\"size-medium wp-image-1431\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5816-L17-87-type-300x199.jpg\" alt=\"Sciadopityphyllum canadenses. From Smoky Tower, AB. Paskapoo Fm. Age Paleocene.\" width=\"300\" height=\"199\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5816-L17-87-type-300x199.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5816-L17-87-type-768x510.jpg 768w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5816-L17-87-type-1024x680.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2016\/03\/PJC_5816-L17-87-type-624x414.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-1431\" class=\"wp-caption-text\">L17-87: Sciadopityphyllum canadenses.<br \/>From Smoky Tower, AB. Paskapoo Fm. Age Paleocene.<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"","protected":false},"author":1614,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-267","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/grad.biology.ualberta.ca\/paleobotany\/index.php?rest_route=\/wp\/v2\/pages\/267","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/grad.biology.ualberta.ca\/paleobotany\/index.php?rest_route=\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/grad.biology.ualberta.ca\/paleobotany\/index.php?rest_route=\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/grad.biology.ualberta.ca\/paleobotany\/index.php?rest_route=\/wp\/v2\/users\/1614"}],"replies":[{"embeddable":true,"href":"https:\/\/grad.biology.ualberta.ca\/paleobotany\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=267"}],"version-history":[{"count":9,"href":"https:\/\/grad.biology.ualberta.ca\/paleobotany\/index.php?rest_route=\/wp\/v2\/pages\/267\/revisions"}],"predecessor-version":[{"id":1491,"href":"https:\/\/grad.biology.ualberta.ca\/paleobotany\/index.php?rest_route=\/wp\/v2\/pages\/267\/revisions\/1491"}],"wp:attachment":[{"href":"https:\/\/grad.biology.ualberta.ca\/paleobotany\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=267"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}