Late Cenozoic atmospheric CO2 reconstruction
As the nearest geologic time period, the late Cenozoic witnessed major climate transitions such as the Northern Hemisphere Glaciation and the Mid-Pleistocene Transition, as well as time periods widely recognized as analogs of near-future climate such as the Mid-Miocene Climate Optimum and the Mid-Pliocene Warm Period. However, the role of CO2 in these climate events remain unresolved, mainly due to the lack of high-resolution, high-precision CO2 record.
- Category 1 proxy-derived CO2 estimates over the past 10 million years. Existing records suffer from large uncertainties, low agreements, and data gaps.1
The Chinese Loess Plateau has been receiving eolian dust deposition since the late Oligocene. The paleosols developed on these eolian deposits hold valuable information of the long-term evolution of atmospheric CO2 levels. Leveraging this unique archive, we improved the classic paleosol-CO2 method by developing new constraint on the input parameter and new sampling method, allowing us to reconstruct a continuous Pleistocene CO2 record with high fidelity.
- Pleistocene loess-paleosol sequence on the Chinese Loess Plateau, characterized by light and dark layers formed during glacial and interglacial periods, respectively.2
The results show relatively stable CO2 during the interglacial periods and long-term decline in glacial CO2, highlighting the role of CO2 in the amplification of the glacial cycles and the long-term global cooling. Moreover, our CO2 data suggest increasing climate sensitivity under higher CO2 levels, and overall higher climate sensitivity than model projections, indicating a potentially underestimated future warming.
Related Publications:
- Da J, Zhang Y G, Wang H, et al. An Early Pleistocene atmospheric CO2 record based on pedogenic carbonate from the Chinese loess deposits[J]. Earth and Planetary Science Letters, 2015, 426: 69-75.
- Da J, Zhang Y G, Li G, et al. Low CO2 levels of the entire Pleistocene epoch, Nat. Commun., 10, 4342[EB/OL].(2019)