Clumped-isotope-derived climate trends leading up to the end-Cretaceous mass extinction in northwest Europe

Thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geology or Earth and Environmental Sciences, Department of Earth and Environmental Sciences Paleotemperature reconstructions linked to Deccan traps volcanic greenhouse gas emissions and associated feed...

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Main Author: O'Hora, Heidi
Other Authors: Earth and Environmental Sciences, Department of, Ann Arbor
Format: Article in Journal/Newspaper
Language:English
Published: 2021
Subjects:
Online Access:https://hdl.handle.net/2027.42/171489
https://doi.org/10.7302/4001
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spelling ftumdeepblue:oai:deepblue.lib.umich.edu:2027.42/171489 2023-08-20T04:04:50+02:00 Clumped-isotope-derived climate trends leading up to the end-Cretaceous mass extinction in northwest Europe O'Hora, Heidi Earth and Environmental Sciences, Department of Ann Arbor 2021-08 application/pdf https://hdl.handle.net/2027.42/171489 https://doi.org/10.7302/4001 en_US eng https://hdl.handle.net/2027.42/171489 https://dx.doi.org/10.7302/4001 Geological Sciences Science Article 2021 ftumdeepblue https://doi.org/10.7302/4001 2023-07-31T21:09:14Z Thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geology or Earth and Environmental Sciences, Department of Earth and Environmental Sciences Paleotemperature reconstructions linked to Deccan traps volcanic greenhouse gas emissions and associated feedbacks in the lead-up to the end-Cretaceous meteorite impact and extinction document local and global climate trends during a key interval of geologic history. Here, we present a new clumped-isotope-based paleotemperature record derived from fossil bivalves from the Maastrichtian type region, in southeast Netherlands and northeast Belgium. Clumped isotope data documents a mean temperature of 19.2 3.8 C, consistent with other Maastrichtian temperature estimates, and an average seawater δ18O value of -0.2 0.9‰ VSMOW for the region during the latest Cretaceous (67.1–66.0 Ma). A notable temperature increase at ~66.4 Ma is interpreted to be a regional manifestation of the globally-defined Late Maastrichtian Warming Event, linking Deccan Traps volcanic CO2 emissions prior to the end-Cretaceous extinction to climate change in the Maastricht region. Fluctuating seawater δ18O values coinciding with temperature changes suggest alternating influences of warm, salty southern-sourced waters and cooler, fresher northern-sourced waters from the Arctic Ocean. This new paleotemperature record contributes to the understanding of regional and global climate response to large-scale volcanism and ocean circulation changes leading up to a catastrophic mass extinction. http://deepblue.lib.umich.edu/bitstream/2027.42/171489/1/OHora_Heidi_MS_Thesis_2021.pdf c5a42028-499d-4e85-9fdc-dc71e2baca26 Description of OHora_Heidi_MS_Thesis_2021.pdf : MS thesis SELF Article in Journal/Newspaper Arctic Arctic Ocean Climate change University of Michigan: Deep Blue Arctic Arctic Ocean
institution Open Polar
collection University of Michigan: Deep Blue
op_collection_id ftumdeepblue
language English
topic Geological Sciences
Science
spellingShingle Geological Sciences
Science
O'Hora, Heidi
Clumped-isotope-derived climate trends leading up to the end-Cretaceous mass extinction in northwest Europe
topic_facet Geological Sciences
Science
description Thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geology or Earth and Environmental Sciences, Department of Earth and Environmental Sciences Paleotemperature reconstructions linked to Deccan traps volcanic greenhouse gas emissions and associated feedbacks in the lead-up to the end-Cretaceous meteorite impact and extinction document local and global climate trends during a key interval of geologic history. Here, we present a new clumped-isotope-based paleotemperature record derived from fossil bivalves from the Maastrichtian type region, in southeast Netherlands and northeast Belgium. Clumped isotope data documents a mean temperature of 19.2 3.8 C, consistent with other Maastrichtian temperature estimates, and an average seawater δ18O value of -0.2 0.9‰ VSMOW for the region during the latest Cretaceous (67.1–66.0 Ma). A notable temperature increase at ~66.4 Ma is interpreted to be a regional manifestation of the globally-defined Late Maastrichtian Warming Event, linking Deccan Traps volcanic CO2 emissions prior to the end-Cretaceous extinction to climate change in the Maastricht region. Fluctuating seawater δ18O values coinciding with temperature changes suggest alternating influences of warm, salty southern-sourced waters and cooler, fresher northern-sourced waters from the Arctic Ocean. This new paleotemperature record contributes to the understanding of regional and global climate response to large-scale volcanism and ocean circulation changes leading up to a catastrophic mass extinction. http://deepblue.lib.umich.edu/bitstream/2027.42/171489/1/OHora_Heidi_MS_Thesis_2021.pdf c5a42028-499d-4e85-9fdc-dc71e2baca26 Description of OHora_Heidi_MS_Thesis_2021.pdf : MS thesis SELF
author2 Earth and Environmental Sciences, Department of
Ann Arbor
format Article in Journal/Newspaper
author O'Hora, Heidi
author_facet O'Hora, Heidi
author_sort O'Hora, Heidi
title Clumped-isotope-derived climate trends leading up to the end-Cretaceous mass extinction in northwest Europe
title_short Clumped-isotope-derived climate trends leading up to the end-Cretaceous mass extinction in northwest Europe
title_full Clumped-isotope-derived climate trends leading up to the end-Cretaceous mass extinction in northwest Europe
title_fullStr Clumped-isotope-derived climate trends leading up to the end-Cretaceous mass extinction in northwest Europe
title_full_unstemmed Clumped-isotope-derived climate trends leading up to the end-Cretaceous mass extinction in northwest Europe
title_sort clumped-isotope-derived climate trends leading up to the end-cretaceous mass extinction in northwest europe
publishDate 2021
url https://hdl.handle.net/2027.42/171489
https://doi.org/10.7302/4001
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Climate change
genre_facet Arctic
Arctic Ocean
Climate change
op_relation https://hdl.handle.net/2027.42/171489
https://dx.doi.org/10.7302/4001
op_doi https://doi.org/10.7302/4001
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