<HashMap><database>biostudies-literature</database><scores/><additional><omics_type>Unknown</omics_type><volume>16(1)</volume><submitter>Mejia LM</submitter><pubmed_abstract>Accurate predictions of the future climate response to CO&lt;sub>2&lt;/sub> 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 paradig</pubmed_abstract><journal>Nature communications</journal><pagination>10981</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC12689775</full_dataset_link><repository>biostudies-literature</repository><pubmed_title>Coccolith clumped isotopes reveal modest rather than extreme northern high latitude amplification during the Miocene.</pubmed_title><pmcid>PMC12689775</pmcid><pubmed_authors>Jaggi M</pubmed_authors><pubmed_authors>Stoll H</pubmed_authors><pubmed_authors>Mejia LM</pubmed_authors><pubmed_authors>Perez-Huerta A</pubmed_authors><pubmed_authors>Zhang H</pubmed_authors><pubmed_authors>Bernasconi SM</pubmed_authors><pubmed_authors>Taylor VE</pubmed_authors><pubmed_authors>Fernandez A</pubmed_authors><pubmed_authors>Guitian J</pubmed_authors></additional><is_claimable>false</is_claimable><name>Coccolith clumped isotopes reveal modest rather than extreme northern high latitude amplification during the Miocene.</name><description>Accurate predictions of the future climate response to CO&lt;sub>2&lt;/sub> 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 paradig</description><dates><release>2025-01-01T00:00:00Z</release><publication>2025 Dec</publication><modification>2026-06-05T23:47:28.029Z</modification><creation>2026-05-23T03:13:52.661Z</creation></dates><accession>S-EPMC12689775</accession><cross_references><pubmed>41365867</pubmed><doi>10.1038/s41467-025-65954-y</doi></cross_references></HashMap>