Clumped isotope evidence for Early Jurassic extreme polar warmth and high climate sensitivity
Periods of high atmospheric CO2 levels during the Cretaceous–early Paleogene (∼ 140 to 34 Myr ago) were marked by very high polar temperatures and reduced latitudinal gradients relative to the Holocene. These features represent a challenge for most climate models, implying either higher-than-predict...
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ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00060293 2023-05-15T14:58:38+02:00 Clumped isotope evidence for Early Jurassic extreme polar warmth and high climate sensitivity Letulle, Thomas Suan, Guillaume Daëron, Mathieu Rogov, Mikhail Lécuyer, Christophe Vinçon-Laugier, Arnauld Reynard, Bruno Montagnac, Gilles Lutikov, Oleg Schlögl, Jan 2022-03 electronic https://doi.org/10.5194/cp-18-435-2022 https://noa.gwlb.de/receive/cop_mods_00060293 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00059938/cp-18-435-2022.pdf https://cp.copernicus.org/articles/18/435/2022/cp-18-435-2022.pdf eng eng Copernicus Publications Climate of the Past -- http://www.copernicus.org/EGU/cp/cp/published_papers.html -- http://www.bibliothek.uni-regensburg.de/ezeit/?2217985 -- 1814-9332 https://doi.org/10.5194/cp-18-435-2022 https://noa.gwlb.de/receive/cop_mods_00060293 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00059938/cp-18-435-2022.pdf https://cp.copernicus.org/articles/18/435/2022/cp-18-435-2022.pdf https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess CC-BY article Verlagsveröffentlichung article Text doc-type:article 2022 ftnonlinearchiv https://doi.org/10.5194/cp-18-435-2022 2022-03-07T00:09:02Z Periods of high atmospheric CO2 levels during the Cretaceous–early Paleogene (∼ 140 to 34 Myr ago) were marked by very high polar temperatures and reduced latitudinal gradients relative to the Holocene. These features represent a challenge for most climate models, implying either higher-than-predicted climate sensitivity to atmospheric CO2 or systematic biases or misinterpretations in proxy data. Here, we present a reconstruction of marine temperatures at polar (> 80∘) and middle (∼ 40∘) paleolatitudes during the Early Jurassic (∼ 180 Myr ago) based on the clumped isotope (Δ47) and oxygen isotope (δ18Oc) analyses of shallow buried pristine mollusc shells. Reconstructed calcification temperatures range from ∼ 8 to ∼ 18 ∘C in the Toarcian Arctic and from ∼ 24 to ∼ 28 ∘C in Pliensbachian mid-paleolatitudes. These polar temperatures were ∼ 10–20 ∘C higher than present along with reduced latitudinal gradients. Reconstructed seawater oxygen isotope values (δ18Ow) of −1.5 ‰ to 0.5 ‰ VSMOW and of −5 ‰ to −2.5 ‰ VSMOW at middle and polar paleolatitudes, respectively, point to a significant freshwater contribution in Arctic regions. These data highlight the risk of assuming the same δ18Osw value for δ18O-derived temperature from different oceanic regions. These findings provide critical new constraints for model simulations of Jurassic temperatures and δ18Osw values and suggest that high climate sensitivity has been a hallmark of greenhouse climates for at least 180 Myr. Article in Journal/Newspaper Arctic Niedersächsisches Online-Archiv NOA Arctic Climate of the Past 18 3 435 448 |
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Niedersächsisches Online-Archiv NOA |
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article Verlagsveröffentlichung Letulle, Thomas Suan, Guillaume Daëron, Mathieu Rogov, Mikhail Lécuyer, Christophe Vinçon-Laugier, Arnauld Reynard, Bruno Montagnac, Gilles Lutikov, Oleg Schlögl, Jan Clumped isotope evidence for Early Jurassic extreme polar warmth and high climate sensitivity |
topic_facet |
article Verlagsveröffentlichung |
description |
Periods of high atmospheric CO2 levels during the Cretaceous–early Paleogene (∼ 140 to 34 Myr ago) were marked by very high polar temperatures and reduced latitudinal gradients relative to the Holocene. These features represent a challenge for most climate models, implying either higher-than-predicted climate sensitivity to atmospheric CO2 or systematic biases or misinterpretations in proxy data. Here, we present a reconstruction of marine temperatures at polar (> 80∘) and middle (∼ 40∘) paleolatitudes during the Early Jurassic (∼ 180 Myr ago) based on the clumped isotope (Δ47) and oxygen isotope (δ18Oc) analyses of shallow buried pristine mollusc shells. Reconstructed calcification temperatures range from ∼ 8 to ∼ 18 ∘C in the Toarcian Arctic and from ∼ 24 to ∼ 28 ∘C in Pliensbachian mid-paleolatitudes. These polar temperatures were ∼ 10–20 ∘C higher than present along with reduced latitudinal gradients. Reconstructed seawater oxygen isotope values (δ18Ow) of −1.5 ‰ to 0.5 ‰ VSMOW and of −5 ‰ to −2.5 ‰ VSMOW at middle and polar paleolatitudes, respectively, point to a significant freshwater contribution in Arctic regions. These data highlight the risk of assuming the same δ18Osw value for δ18O-derived temperature from different oceanic regions. These findings provide critical new constraints for model simulations of Jurassic temperatures and δ18Osw values and suggest that high climate sensitivity has been a hallmark of greenhouse climates for at least 180 Myr. |
format |
Article in Journal/Newspaper |
author |
Letulle, Thomas Suan, Guillaume Daëron, Mathieu Rogov, Mikhail Lécuyer, Christophe Vinçon-Laugier, Arnauld Reynard, Bruno Montagnac, Gilles Lutikov, Oleg Schlögl, Jan |
author_facet |
Letulle, Thomas Suan, Guillaume Daëron, Mathieu Rogov, Mikhail Lécuyer, Christophe Vinçon-Laugier, Arnauld Reynard, Bruno Montagnac, Gilles Lutikov, Oleg Schlögl, Jan |
author_sort |
Letulle, Thomas |
title |
Clumped isotope evidence for Early Jurassic extreme polar warmth and high climate sensitivity |
title_short |
Clumped isotope evidence for Early Jurassic extreme polar warmth and high climate sensitivity |
title_full |
Clumped isotope evidence for Early Jurassic extreme polar warmth and high climate sensitivity |
title_fullStr |
Clumped isotope evidence for Early Jurassic extreme polar warmth and high climate sensitivity |
title_full_unstemmed |
Clumped isotope evidence for Early Jurassic extreme polar warmth and high climate sensitivity |
title_sort |
clumped isotope evidence for early jurassic extreme polar warmth and high climate sensitivity |
publisher |
Copernicus Publications |
publishDate |
2022 |
url |
https://doi.org/10.5194/cp-18-435-2022 https://noa.gwlb.de/receive/cop_mods_00060293 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00059938/cp-18-435-2022.pdf https://cp.copernicus.org/articles/18/435/2022/cp-18-435-2022.pdf |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
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Arctic |
op_relation |
Climate of the Past -- http://www.copernicus.org/EGU/cp/cp/published_papers.html -- http://www.bibliothek.uni-regensburg.de/ezeit/?2217985 -- 1814-9332 https://doi.org/10.5194/cp-18-435-2022 https://noa.gwlb.de/receive/cop_mods_00060293 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00059938/cp-18-435-2022.pdf https://cp.copernicus.org/articles/18/435/2022/cp-18-435-2022.pdf |
op_rights |
https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.5194/cp-18-435-2022 |
container_title |
Climate of the Past |
container_volume |
18 |
container_issue |
3 |
container_start_page |
435 |
op_container_end_page |
448 |
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1766330764444565504 |