Accurate predictions of the future climate response to CO2 depend on the ability of climate models to simulate past analog warmer climates, like the Miocene. However, one key unresolved issue in paleoclimate modeling is reproducing the pronounced high-latitude warmth and relatively flat latitudinal temperature gradients inferred from proxy records. Here, we use clumped isotope thermometry—a method that sidesteps limitations of conventional proxies—on pure coccolith calcite from a high-latitude North Atlantic site, extending from the Mid Miocene to the Quaternary. Coccolith-derived clumped isotope temperatures are on average ~9 °C lower than alkenone estimates, representing the first proxy dataset to align with Miocene model outputs and calling into question the prevailing paradigm of pronounced high latitude amplification. This record highlights the need to continuously reevaluate proxy interpretations to achieve both reliable trends and absolute temperature values, while providing a more optimistic perspective of future high latitude climate response to CO2 emissions. 

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Modest, not extreme, northern high latitude amplification during the Miocene shown by coccolith clumped isotopes

Modest, not extreme, northern high latitude amplification during the Miocene shown by coccolith clumped isotopes

This is a Preprint and has not been peer reviewed. This is version 2 of this Preprint.

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Authors

Luz Maria Mejia Ramirez, Stefano M. Bernasconi, Alvaro Fernandez, Hongrui Zhang, José Guitián, Madalina Jaggi, Victoria Emma Taylor, Alberto Perez-Huerta, Heather M. Stoll

Abstract

Accurate predictions of the future climate response to CO2 depend on the ability of climate models to simulate past analog warmer climates, like the Miocene. However, one key unresolved issue in paleoclimate modeling is reproducing the pronounced high-latitude warmth and relatively flat latitudinal temperature gradients inferred from proxy records. Here, we use clumped isotope thermometry—a method that sidesteps limitations of conventional proxies—on pure coccolith calcite from a high-latitude North Atlantic site, extending from the Mid Miocene to the Quaternary. Coccolith-derived clumped isotope temperatures are on average ~9 °C lower than alkenone estimates, representing the first proxy dataset to align with Miocene model outputs and calling into question the prevailing paradigm of pronounced high latitude amplification. This record highlights the need to continuously reevaluate proxy interpretations to achieve both reliable trends and absolute temperature values, while providing a more optimistic perspective of future high latitude climate response to CO2 emissions. 

DOI

https://doi.org/10.31223/X59B0N

Subjects

Physical Sciences and Mathematics

Keywords

coccolithophores, clumped isotopes, High Latitude Amplification, Miocene, clumped isotopes, High Latitude Amplification, Miocene

Dates

Published: 2024-12-14 00:55

Last Updated: 2025-04-07 22:07

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License

CC-BY Attribution-No Derivatives 4.0 International

Additional Metadata

Conflict of interest statement:
None

Data Availability (Reason not available):
All data included in the Manuscript or supplemental information