Cited by 11Geology and Paleoclimatology ResearchPaleontology and Stratigraphy of FossilsClimate variability and models

Clumped isotope evidence for Early Jurassic extreme polar warmth and high climate sensitivity

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Letulle, Thomas, Suan, Guillaume, Daëron, Mathieu, Rogov, Mikhail, Lécuyer, Christophe, Vinçon-Laugier, Arnauld, Reynard, Bruno, Montagnac, Gilles +2 more·2022·Climate of the Past

Published version of a preprint

Abstract

Periods of high atmospheric CO 2 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 CO 2 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 (Δ 47 ) and oxygen isotope ( δ 18 O c ) 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 ( δ 18 O w ) 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 δ 18 O sw value for δ 18 O-derived temperature from different oceanic regions. These findings provide critical new constraints for model simulations of Jurassic temperatures and δ 18 O sw values and suggest that high climate sensitivity has been a hallmark of greenhouse climates for at least 180 Myr.

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Authors
Letulle, T., Suan, G., Daëron, M., Rogov, M., Lécuyer, C., Vinçon-Laugier, A., Reynard, B., Montagnac, G., Lutikov, O., & Schlögl, J.
Affiliations
  • Lyon 1 Université (FR)
  • Commissariat à l'Énergie Atomique et aux Énergies Alternatives (FR)
  • Russian Academy of Sciences (RU)
Corresponding author
Reynard, Bruno
Venue
Climate of the Past
Published
2022-03-04
Volume
18
Issue
3
Pages
435-448
ISSN
  • 1814-9324 (ISSN-L)
  • 1814-9332
OpenAlex
W4220869237
Cited by
11
References
13
Citations by year
2026: 2 · 2025: 5 · 2024: 3 · 2022: 1
FWCI
0.86
Type
journal article
Language
en
Open access
Locations
  • Climate of the past (publishedVersion, cc-by)
  • HAL (submittedVersion, other-oa)
  • DOAJ (DOAJ: Directory of Open Access Journals) (submittedVersion, cc-by-sa)
Funders
  • Agence Nationale de la Recherche (ANR-18-CE31-0020)
  • Centre National de la Recherche Scientifique (205700)
  • Russian Foundation for Basic Research (21-55-15015)
  • Agentúra na Podporu Výskumu a Vývoja (APVV 17-0555)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
  • Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
Keywords
Lower Jurassic, climate sensitivity, greenhouse microclimate, clumped isotopes, calcification temperature, mollusk shells, seawater oxygen isotopes, latitudinal temperature gradient, Toarcian, Pliensbachian, paleoclimate reconstruction

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