Early Eocene Climatic Optimum Pacific deep ocean temperatures from clumped isotope thermometry
- 1Bjerknes Centre for Climate Research and Department of Earth Science, University of Bergen, Bergen, Norway (johanna.marquardt@uib.no)
- 2Present address: Department of Environmental Sciences, University of Basel, Basel, Switzerland
- 3School of Environment, Earth and Ecosystem Sciences, The Open University, Milton Keynes, UK
- 4MARUM – Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany
- 5Department of Earth and Planetary Sciences, University of California, Santa Cruz, CA, USA
Past greenhouse climates provide crucial insights into how the climate system operates under conditions with high atmospheric carbon dioxide concentrations and smaller or absent continental ice sheets, and thus inform projections of future climate. When studying past greenhouse climate states, deep ocean temperatures are often used to estimate global mean temperature (Westerhold et al., 2020), which is needed to determine climate sensitivity and assess the performance of climate models. Additionally, deep ocean temperatures provide insights into past ocean circulation patterns.
The Early Eocene Climatic Optimum (EECO; 53.3 to 49.1 Ma) was characterized by extreme global warmth and elevated atmospheric CO2 concentrations (Hollis et al., 2019a). Currently, our understanding of deep ocean temperatures during the EECO relies primarily on benthic foraminiferal stable oxygen isotopes and Mg/Ca records. These proxies, however, are influenced by factors other than temperature, making robust deep-time temperature reconstructions challenging. Carbonate clumped isotope thermometry, on the other hand, is largely independent of past seawater chemistry and can therefore provide essential new constraints.
Recent clumped isotope-based deep ocean temperature reconstructions from the Atlantic Ocean are substantially warmer during the peak EECO than previous estimates based on stable oxygen isotopes and Mg/Ca records (Meckler et al., 2022). However, it remains to be tested whether these warmer temperatures are a regional signal restricted to the Atlantic Ocean or found globally in the deep ocean. Here we present a record of deep ocean temperatures using clumped isotopes in benthic foraminifera from the Pacific Ocean (ODP Site 1209, ~2300 m paleo-water depth). Our new record spans the interval between 52 Ma to 50.3 Ma, covering the peak EECO and the major shift in benthic foraminiferal stable carbon isotopes around 51 Ma which is observed globally in the deep ocean. Warmer than expected Atlantic as well as Pacific deep ocean temperatures could indicate that EECO global mean temperature was warmer than previously assumed, which would have implications for existing estimates of climate sensitivity.
References
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Meckler, A. N., Sexton, P. F., Piasecki, A. M., Leutert, T. J., Marquardt, J., Ziegler, M., ... & Bernasconi, S. M. (2022). Cenozoic evolution of deep ocean temperature from clumped isotope thermometry. Science, 377(6601), 86-90.
Westerhold, T., Marwan, N., Drury, A. J., Liebrand, D., Agnini, C., Anagnostou, E., ... & Zachos, J. C. (2020). An astronomically dated record of Earth’s climate and its predictability over the last 66 million years. Science, 369(6509), 1383-1387.
How to cite: Marquardt, J., Lypiridou, I., Taylor, V. E., Sexton, P. F., Westerhold, T., Zachos, J. C., and Meckler, A. N.: Early Eocene Climatic Optimum Pacific deep ocean temperatures from clumped isotope thermometry, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-5765, https://doi.org/10.5194/egusphere-egu24-5765, 2024.
