T241 The Cretaceous–Paleogene Boundary: From Impact Cratering Processes to Mass Extinction Mechanisms
Wednesday, 13 October 2021
1:30 PM - 5:30 PM
D139/D140
TRANSFORMATIVE EFFECTS OF THE END-CRETACEOUS EVENT ON THE EVOLUTION OF MODERN NEOTROPICAL RAINFORESTS
Paper number: T241-11
Program: Technical Sessions
Time: 3:55 PM – 4:10 PM
Authors
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Germán BayonaCorporacion Geologica Ares, Bogota
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Fabiany HerreraField Museum of Natural History, Chicago, IL
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Scott WingNational Museum of Natural History, Department of Paleobiology, Washington, DC
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Conrad LabandeiraNational Museum of Natural History, Department of Paleobiology, Washington, DC
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L. Alejandro Giraldo CerónSmithsonian Tropical Research Institute, Panama
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Carlos JaramilloSmithsonian Tropical Research Institute, Ancón, Panamá
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Felipe de la ParraInstituto Colombiano del Petróleo, Bucaramanga
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Dayenari Caballero-RodríguezSmithsonian Tropical Research Institute, Ancón, Panamá
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Daniele SilvestroUniversity of Fribourg, Fribourg, Fribourg
Abstract
Maastrichtian rainforests were diverse assemblages of ferns, angiosperms, and conifers that formed open canopies and had diverse plant–insect interactions. Plant diversity declined by 45% at the K/Pg boundary, establishing a long interval (~6 million years) of unusual low plant diversity in the Neotropics. Paleocene plant communities became dominated by angiosperms, whereas conifers became (nearly) regionally extinct. By the mid–late Paleocene, tropical forests resembled modern-aspect rainforests in having closed canopies and a multistratal structure. Despite their low taxonomic diversity, Paleocene rainforests were ecologically diverse and had the same plant-family composition, dominated by legumes, as modern Neotropical rainforests.
The transformation in forest structure and plant composition across the K/Pg boundary likely is a byproduct of the ecological catastrophe at the end-Cretaceous, and indicates fundamental changes in carbon fixation, evapotranspiration and nutrient cycling.
Geological Society of America Abstracts with Programs. Vol. 53, No. 6
doi: 10.1130/abs/2021AM-370862
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