Research Article| September 01, 2000 Microfloral diversity patterns of the late Paleocene–Eocene interval in Colombia, northern South America Carlos A. Jaramillo; Carlos A. Jaramillo 1Paleobotany Laboratory, Florida Museum of Natural History, Gainesville, Florida 32611, USA Search for other works by this author on: GSW Google Scholar David L. Dilcher David L. Dilcher 1Paleobotany Laboratory, Florida Museum of Natural History, Gainesville, Florida 32611, USA Search for other works by this author on: GSW Google Scholar Author and Article Information Carlos A. Jaramillo 1Paleobotany Laboratory, Florida Museum of Natural History, Gainesville, Florida 32611, USA David L. Dilcher 1Paleobotany Laboratory, Florida Museum of Natural History, Gainesville, Florida 32611, USA Publisher: Geological Society of America Received: 27 Mar 2000 Revision Received: 05 Jun 2000 Accepted: 20 Jun 2000 First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (2000) 28 (9): 815–818. https://doi.org/10.1130/0091-7613(2000)28<815:MDPOTL>2.0.CO;2 Article history Received: 27 Mar 2000 Revision Received: 05 Jun 2000 Accepted: 20 Jun 2000 First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Carlos A. Jaramillo, David L. Dilcher; Microfloral diversity patterns of the late Paleocene–Eocene interval in Colombia, northern South America. Geology 2000;; 28 (9): 815–818. doi: https://doi.org/10.1130/0091-7613(2000)28<815:MDPOTL>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract The late Paleocene–early Eocene interval was characterized by a long period of global warming that culminated with the highest temperatures of the Tertiary. This interval was also associated with plant extinctions and a subsequent increase in plant diversity in temperate latitudes. However, tropical regions remain largely unknown. We compare the microfloral diversity of the late Paleocene with the late early to middle Eocene in flood plain, coastal plain, and estuarine facies of a section in the Colombian eastern Andes. Several techniques such as range-through method, rarefaction, bootstrap, detrended correspondence analysis, and Simpson index were used to assess the significance of the diversity pattern observed throughout the section. The microfloral record indicates a distinct, diverse Paleocene flora declining toward the end of the Paleocene, being replaced by a different and much more diverse Eocene flora. It is uncertain, however, how these floral changes correlate with the latest Paleocene thermal maximum and Eocene thermal maximum events. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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