Marine temperatures underestimated for past greenhouse climate.

ABSTRACT: Understanding the Earth's climate system during past periods of high atmospheric CO₂ is crucial for forecasting climate change under anthropogenically-elevated CO₂. The Mesozoic Era is believed to have coincided with a long-term Greenhouse climate, and many of our temperature reconstructions come from stable isotopes of marine biotic calcite, in particular from belemnites, an extinct group of molluscs with carbonate hard-parts. Yet, temperatures reconstructed from the oxygen isotope composition of belemnites are consistently colder than those derived from other temperature proxies, leading to large uncertainties around Mesozoic sea temperatures. Here we apply clumped isotope palaeothermometry to two distinct carbonate phases from exceptionally well-preserved belemnite

SUBMITTER: Vickers ML 

PROVIDER: S-EPMC8476565 | biostudies-literature | 2021 Sep

REPOSITORIES: biostudies-literature