Continuous sterane and phytane δ13C record reveals a substantial pCO2 decline since the mid-Miocene
Witkowski, C.R.; von der Heydt, A.S.; Valdes, P.J.; van der Meer, M.T.J.; Schouten, S.; Sinninghe Damsté, J.S. (2024). Continuous sterane and phytane δ13C record reveals a substantial pCO2 decline since the mid-Miocene. Nature Comm. 15(1): 5192. https://dx.doi.org/10.1038/s41467-024-47676-9 In: Nature Communications. Nature Publishing Group: London. ISSN 2041-1723; e-ISSN 2041-1723, more |   |
| Author keywords | Carbon cycle; Palaeoclimate |
| Authors | | Top | - Witkowski, C.R., more
- von der Heydt, A.S.
- Valdes, P.J.
| - van der Meer, M.T.J., more
- Schouten, S., more
- Sinninghe Damsté, J.S., more
| |
| Abstract | Constraining the relationship between temperature and atmospheric concentrations of carbon dioxide (pCO2) is essential to model near-future climate. Here, we reconstruct pCO2 values over the past 15 million years (Myr), providing a series of analogues for possible near-future temperatures and pCO2, from a single continuous site (DSDP Site 467, California coast). We reconstruct pCO2 values using sterane and phytane, compounds that many phytoplankton produce and then become fossilised in sediment. From 15.0-0.3 Myr ago, our reconstructed pCO2 values steadily decline from 650 ± 150 to 280 ± 75 ppmv, mirroring global temperature decline. Using our new range of pCO2 values, we calculate average Earth system sensitivity and equilibrium climate sensitivity, resulting in 13.9 °C and 7.2 °C per doubling of pCO2, respectively. These values are significantly higher than IPCC global warming estimations, consistent or higher than some recent state-of-the-art climate models, and consistent with other proxy-based estimates. |
|
