Presenter Information

Paul E. Olsen, Columbia University

Start Date

18-2-2020 4:00 PM

End Date

18-2-2020 5:00 PM

Access Type

Open Access

Abstract

Despite the extremely high levels of atmospheric CO2 (+2000 ppm) in the Late Triassic and earliest Jurassic (~232-199 million years ago), there is evidence of seasonally freezing conditions in the Arctic of that time. This evidence consists of abundant icerafted debris in lake sediments. Based on phylogenetic bracket analysis, dinosaurs at this time were insulated, and could take advantage of the rich Arctic deciduous and evergreen vegetation, even under freezing winter conditions. Transient volcanic winters caused by the eruptions of the Central Atlantic Magmatic Province led to a mass extinction at 201.6 million years ago, at the close of the Triassic, that decimating all medium- to large-sized non-dinosaurian, uninsulated animals on land. In contrast, the insulated dinosaurs, already adapted to cold temperatures, not only survived but underwent a rapid adaptive radiation and ecological expansion in the Jurassic, taking over regions formerly dominated by large uninsulated reptiles.

Biography

Paul Olsen is a paleontologist and stratigrapher. He received a BA in Geology in 1978 and an M. Phil. and Ph.D. in Biology in 1984 at Yale University. His interests and research projects examine patterns of evolution and extinction as a response to and cause of climate change over geological time, especially in continental ecosystems from the age of the dinosaurs. Dr. Olsen is currently Storke Memorial Professor of Earth and Environmental Sciences at Columbia University at Lamont Doherty Earth Observatory. A member of the National Academy of Sciences, he was awarded the Thomas Jefferson Medal for Outstanding Contributions to Natural Science in 2015.

ORCID

0000-0002-5852-6326

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Feb 18th, 4:00 PM Feb 18th, 5:00 PM

Arctic Ice and the Ecological Ascent of the Dinosaurs

Despite the extremely high levels of atmospheric CO2 (+2000 ppm) in the Late Triassic and earliest Jurassic (~232-199 million years ago), there is evidence of seasonally freezing conditions in the Arctic of that time. This evidence consists of abundant icerafted debris in lake sediments. Based on phylogenetic bracket analysis, dinosaurs at this time were insulated, and could take advantage of the rich Arctic deciduous and evergreen vegetation, even under freezing winter conditions. Transient volcanic winters caused by the eruptions of the Central Atlantic Magmatic Province led to a mass extinction at 201.6 million years ago, at the close of the Triassic, that decimating all medium- to large-sized non-dinosaurian, uninsulated animals on land. In contrast, the insulated dinosaurs, already adapted to cold temperatures, not only survived but underwent a rapid adaptive radiation and ecological expansion in the Jurassic, taking over regions formerly dominated by large uninsulated reptiles.