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...

Full description

Bibliographic Details
Published in:Climate of the Past
Main Authors: Letulle, Thomas, Suan, Guillaume, Daëron, Mathieu, Rogov, Mikhail, Lécuyer, Christophe, Vinçon-Laugier, Arnauld, Reynard, Bruno, Montagnac, Gilles, Lutikov, Oleg, Schlögl, Jan
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2022
Subjects:
article
Verlagsveröffentlichung
Arctic
Online Access: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
Description
Summary: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.

Similar Items