{"id":16,"date":"2015-03-09T12:22:13","date_gmt":"2015-03-09T16:22:13","guid":{"rendered":"https:\/\/grad.biology.ualberta.ca\/paleobotany\/?page_id=16"},"modified":"2020-05-12T17:03:14","modified_gmt":"2020-05-12T23:03:14","slug":"lab-2-pt-2","status":"publish","type":"page","link":"https:\/\/grad.biology.ualberta.ca\/paleobotany\/?page_id=16","title":{"rendered":"Lab 02 pt 2 Algae, fungi and bryophyts"},"content":{"rendered":"<div id=\"attachment_229\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3966-L3-2.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-229\" class=\"size-medium wp-image-229\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3966-L3-2-300x200.jpg\" alt=\"Water biscuit Age Pennsylvanian.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3966-L3-2-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3966-L3-2-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3966-L3-2-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-229\" class=\"wp-caption-text\">L3-2: Water biscuit<br \/>Age Pennsylvanian.<\/p><\/div>\n<div id=\"attachment_228\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3969-L3-3.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-228\" class=\"size-medium wp-image-228\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3969-L3-3-300x200.jpg\" alt=\"Water biscuit or Boghead Coal from Transvaal. Age Permian.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3969-L3-3-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3969-L3-3-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3969-L3-3-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-228\" class=\"wp-caption-text\">L3-3: Water biscuit or Boghead Coal from Transvaal. Age Permian.<\/p><\/div>\n<div id=\"attachment_227\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3972-L3-4.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-227\" class=\"size-medium wp-image-227\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3972-L3-4-300x200.jpg\" alt=\"Cryptozoon fragment from New York. Age Precambrian.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3972-L3-4-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3972-L3-4-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3972-L3-4-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-227\" class=\"wp-caption-text\">L3-4: Cryptozoon fragment from New York. Age Precambrian.<\/p><\/div>\n<div id=\"attachment_226\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3974-L3-5.-JPG.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-226\" class=\"size-medium wp-image-226\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3974-L3-5.-JPG-300x200.jpg\" alt=\"Algal limestone from Belt Series (Newlandia). From Glacier National Park. Age Precambrian.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3974-L3-5.-JPG-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3974-L3-5.-JPG-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3974-L3-5.-JPG-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-226\" class=\"wp-caption-text\">L3-5: Algal limestone from Belt Series (Newlandia). From Glacier National Park. Age Precambrian.<\/p><\/div>\n<div id=\"attachment_225\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3976-L3-6.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-225\" class=\"size-medium wp-image-225\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3976-L3-6-300x200.jpg\" alt=\"Collenia (alga limestone) from Jasper.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3976-L3-6-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3976-L3-6-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3976-L3-6-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-225\" class=\"wp-caption-text\">L3-6: Collenia (algae limestone) from Jasper.<\/p><\/div>\n<div id=\"attachment_224\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3977-L3-7.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-224\" class=\"size-medium wp-image-224\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3977-L3-7-300x200.jpg\" alt=\"Oolitic limestone Bluegreen alga ? Age Mississippian.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3977-L3-7-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3977-L3-7-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3977-L3-7-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-224\" class=\"wp-caption-text\">L3-7: Oolitic limestone Bluegreen algae ?<br \/>Age Mississippian.<\/p><\/div>\n<div id=\"attachment_223\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3979-L3-8.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-223\" class=\"size-medium wp-image-223\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3979-L3-8-300x200.jpg\" alt=\"Oolitic limeston Bluegreen alga. Age Mississippian\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3979-L3-8-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3979-L3-8-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3979-L3-8-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-223\" class=\"wp-caption-text\">L3-11: Oolitic limeston Bluegreen algae.<br \/>Age Mississippian<\/p><\/div>\n<div id=\"attachment_222\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3981-L3-8.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-222\" class=\"size-medium wp-image-222\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3981-L3-8-300x200.jpg\" alt=\"Oolitic sand formed by blue green alga Chroococcus from the Persian Gulf.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3981-L3-8-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3981-L3-8-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3981-L3-8-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-222\" class=\"wp-caption-text\">L3-8: Oolitic sand formed by blue green algae Chroococcus from the Persian Gulf.<\/p><\/div>\n<div id=\"attachment_221\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3982-L3-15.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-221\" class=\"size-medium wp-image-221\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3982-L3-15-300x200.jpg\" alt=\"Receptaculites (Chorophyta) in Tindle Limestone from Manitoba. Age Ordovician.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3982-L3-15-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3982-L3-15-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3982-L3-15-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-221\" class=\"wp-caption-text\">L3-12: Receptaculites in Tindle Limestone from Manitoba. Age Ordovician.<\/p><\/div>\n<div id=\"attachment_220\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3983-L3-16.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-220\" class=\"size-medium wp-image-220\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3983-L3-16-300x200.jpg\" alt=\"Prototaxites southnorthii Age Devonian.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3983-L3-16-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3983-L3-16-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3983-L3-16-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-220\" class=\"wp-caption-text\">L3-16: Prototaxites southnorthii<br \/>Age Devonian.<\/p><\/div>\n<div id=\"attachment_217\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3990-L3-19.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-217\" class=\"size-medium wp-image-217\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3990-L3-19-300x200.jpg\" alt=\"Protosalvinia (Foerstia) from New Albany Shale, Ohio. Age Upper Devonian.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3990-L3-19-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3990-L3-19-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3990-L3-19-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-217\" class=\"wp-caption-text\">L3-19: Protosalvinia (Foerstia) from New Albany Shale, Ohio. Age Upper Devonian.<\/p><\/div>\n<div id=\"attachment_216\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3992-L3-20.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-216\" class=\"size-medium wp-image-216\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3992-L3-20-300x200.jpg\" alt=\"Protosalvinia (Foerstia) From New Albany Shale, Ohio. Age Upper Devonian.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3992-L3-20-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3992-L3-20-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3992-L3-20-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-216\" class=\"wp-caption-text\">L3-20: Protosalvinia (Foerstia) From New Albany Shale, Ohio. Age Upper Devonian.<\/p><\/div>\n<div id=\"attachment_215\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3993-L3-22.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-215\" class=\"size-medium wp-image-215\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3993-L3-22-300x200.jpg\" alt=\"Corallina - moderne calcareous red algae, Rhodophyta.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3993-L3-22-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3993-L3-22-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3993-L3-22-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-215\" class=\"wp-caption-text\">L3-25: Corallina &#8211; moderne calcareous red algae, Rhodophyta.<\/p><\/div>\n<div id=\"attachment_214\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3996-L3-24.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-214\" class=\"size-medium wp-image-214\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3996-L3-24-300x200.jpg\" alt=\"Solenopora (fissil red Algae)\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3996-L3-24-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3996-L3-24-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3996-L3-24-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-214\" class=\"wp-caption-text\">L3-24: Solenopora (fossil red Algae). P637\/P638.\u00a0<\/p><\/div>\n<div id=\"attachment_213\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3997-L3-25.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-213\" class=\"size-medium wp-image-213\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3997-L3-25-300x200.jpg\" alt=\"Algae Compression?\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3997-L3-25-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3997-L3-25-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3997-L3-25-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-213\" class=\"wp-caption-text\">L3-27: Algae Compression?<\/p><\/div>\n<div id=\"attachment_212\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3998-L3-26.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-212\" class=\"size-medium wp-image-212\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3998-L3-26-300x200.jpg\" alt=\"Halimeda ?\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3998-L3-26-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3998-L3-26-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_3998-L3-26-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-212\" class=\"wp-caption-text\">Halimeda ?<\/p><\/div>\n<div id=\"attachment_211\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4002-L3-27.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-211\" class=\"size-medium wp-image-211\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4002-L3-27-300x200.jpg\" alt=\"Algae compression.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4002-L3-27-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4002-L3-27-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4002-L3-27-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-211\" class=\"wp-caption-text\">L3-30: Algae compression.<\/p><\/div>\n<div id=\"attachment_210\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4004-L3-31.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-210\" class=\"size-medium wp-image-210\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4004-L3-31-300x200.jpg\" alt=\"Montastrea annularis (Coral). From Stock Island, Florida Key. Age Pleistocene\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4004-L3-31-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4004-L3-31-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4004-L3-31-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-210\" class=\"wp-caption-text\">L3-31: Montastrea annularis (Coral). From Stock Island, Florida Key. Age Pleistocene<\/p><\/div>\n<div id=\"attachment_209\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4007-L3-33.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-209\" class=\"size-medium wp-image-209\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4007-L3-33-300x200.jpg\" alt=\"Agleophyton major and Paleomyces, Rhynie Chert, Scotland. Age LM Devonian.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4007-L3-33-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4007-L3-33-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4007-L3-33-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-209\" class=\"wp-caption-text\">L3-33: Agleophyton major and Paleomyces, Rhynie Chert, Scotland. Age LM Devonian.<\/p><\/div>\n<div id=\"attachment_208\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4009-L3-34.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-208\" class=\"size-medium wp-image-208\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4009-L3-34-300x200.jpg\" alt=\"Paleomyces, Rhynie Chert, Scotland. Age LM Devonian.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4009-L3-34-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4009-L3-34-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4009-L3-34-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-208\" class=\"wp-caption-text\">L3-34: Paleomyces, Rhynie Chert, Scotland. Age LM Devonian.<\/p><\/div>\n<div id=\"attachment_207\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4022-L3-36.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-207\" class=\"size-medium wp-image-207\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4022-L3-36-300x200.jpg\" alt=\"Fossil wood from Antarctica with white pocket rot. \" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4022-L3-36-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4022-L3-36-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4022-L3-36-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-207\" class=\"wp-caption-text\">L3-35: Fossil wood from Antarctica with white pocket rot.<\/p><\/div>\n<div id=\"attachment_206\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4021-L3-36.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-206\" class=\"size-medium wp-image-206\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4021-L3-36-300x200.jpg\" alt=\"Fossil wood from Antarctica with white pocket rot. ? Cretaceous.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4021-L3-36-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4021-L3-36-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4021-L3-36-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-206\" class=\"wp-caption-text\">L3-35: Fossil wood from Antarctica with white pocket rot. ? Cretaceous.<\/p><\/div>\n<div id=\"attachment_205\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4010-L3-37.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-205\" class=\"size-medium wp-image-205\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4010-L3-37-300x200.jpg\" alt=\"Moss gametophyte Aulacomnium heterostrichoides from Horsefly, BC. Age M. Eocene.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4010-L3-37-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4010-L3-37-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4010-L3-37-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-205\" class=\"wp-caption-text\">L3-37: Moss gametophyte Aulacomnium heterostrichoides from Horsefly, BC. Age M. Eocene.<\/p><\/div>\n<div id=\"attachment_204\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4012-L3-38.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-204\" class=\"size-medium wp-image-204\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4012-L3-38-300x200.jpg\" alt=\"Fossil Bryophyte, origin unknown.\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4012-L3-38-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4012-L3-38-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4012-L3-38-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-204\" class=\"wp-caption-text\">L3-38: Fossil Bryophyte, origin unknown.<\/p><\/div>\n<div id=\"attachment_203\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4014-L3-39.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-203\" class=\"size-medium wp-image-203\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4014-L3-39-300x200.jpg\" alt=\"Fossil Bryophyte from Genessee. Collected by D. Whighton. Age ?\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4014-L3-39-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4014-L3-39-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4014-L3-39-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-203\" class=\"wp-caption-text\">L3-39: Fossil Bryophyte from Genessee. Collected by D. Whighton.<\/p><\/div>\n<div id=\"attachment_202\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4016-L3-40.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-202\" class=\"size-medium wp-image-202\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4016-L3-40-300x200.jpg\" alt=\"Fossil Bryophyte from Republic School Yard, Klondike Mt. Fm. M. Eocene. Collected by M. Wilson 1976\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4016-L3-40-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4016-L3-40-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4016-L3-40-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-202\" class=\"wp-caption-text\">L3-40: Fossil Bryophyte from Republic School Yard, Klondike Mt. Fm. M. Eocene. Collected by M. Wilson 1976<\/p><\/div>\n<div id=\"attachment_201\" style=\"width: 310px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4018-L3-41.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-201\" class=\"size-medium wp-image-201\" src=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4018-L3-41-300x200.jpg\" alt=\"Fossil Bryophyte from Genessee\" width=\"300\" height=\"200\" srcset=\"https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4018-L3-41-300x200.jpg 300w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4018-L3-41-1024x683.jpg 1024w, https:\/\/grad.biology.ualberta.ca\/paleobotany\/wp-content\/uploads\/sites\/57\/2015\/12\/IMG_4018-L3-41-624x416.jpg 624w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-201\" class=\"wp-caption-text\">L3-41: Fossil Bryophyte from Genessee Alberta. S2724.<\/p><\/div>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>&nbsp;<\/p>\n","protected":false},"author":1614,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-16","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/grad.biology.ualberta.ca\/paleobotany\/index.php?rest_route=\/wp\/v2\/pages\/16","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=16"}],"version-history":[{"count":10,"href":"https:\/\/grad.biology.ualberta.ca\/paleobotany\/index.php?rest_route=\/wp\/v2\/pages\/16\/revisions"}],"predecessor-version":[{"id":1470,"href":"https:\/\/grad.biology.ualberta.ca\/paleobotany\/index.php?rest_route=\/wp\/v2\/pages\/16\/revisions\/1470"}],"wp:attachment":[{"href":"https:\/\/grad.biology.ualberta.ca\/paleobotany\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=16"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}