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Southern Ocean and atmospheric CO2 in a warm world - unravelling CO2 sinks in the Southern Ocean during the last interglacial climate state (Project acronym: SOCO)

Subject Area Palaeontology
Term from 2017 to 2020
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 329606761
 
Final Report Year 2021

Final Report Abstract

The project SOCO aimed at assessing carbon cycling and ocean circulation changes in the Atlantic, Indian and Pacific sectors of Southern Ocean during the last interglacial climate period, with particular emphasis on its climatic optimum Marine Isotope Stage 5e as it is considered a potential climate analog of future global climate change. The project specifically targeted resolving biological, dynamical and physical control mechanisms of variations in Southern Ocean carbon storage and ocean circulation changes in the Southern Ocean by applying a multi-proxy approach to our study sediment cores. Through reconstructions of deep-ocean oxygenation, carbon storage, export production, bottom water corrosivity, sea ice dynamics and water mass origin, we were able to disclose three key aspects of Southern Ocean dynamics during the last interglacial climate interval: First, the last peak interglacial was characterized by recurrent perturbations in AABW formation that were likely related to warming of CDW by ~2°C above Holocene levels. This in turn might have been caused by ice shelf melting primarily in the Weddell Sea, signifying the impact of destabilizations of the Antarctic ice sheet through Southern Ocean processes on global sea level. Second, ocean circulation dynamics in the Southern Ocean during the last peak interglacial overall significantly differed from the Holocene; specifically, the global deep ocean was filled by more southern-sourced water masses during the last peak interglacial, which also altered the ocean’s capacity to store and release carbon during that time. Lastly, the Southern Ocean is a significant carbon sink as the Earth system transitions into a glacial climate state, yet processes in the Indian and Pacific sectors diverge from those in the Atlantic sector. While dust-driven export production and wind-driven upwelling determine carbon storage in the Atlantic sector, the deep-ocean respired carbon in the Indian and Pacific sectors are primarily influenced by physical and dynamical processes. The project successfully dealt with unexpected scientific surprises (e.g., previous misalignments of core chronologies based on low-resolution data) and setbacks (e.g., contamination issues), primarily by means of adjusting the publication strategy and performing alternative and complementary proxy analyses. The work highlights the importance of Southern Ocean processes in driving CO2,atm changes and Antarctic ice sheet stability during peak climate conditions and interglacial-glacial climate transitions. Yet, it also emphasizes the spatial heterogeneity and temporal differences of carbon cycle variations and ocean circulation changes across the Southern Ocean that was previously underappreciated. Many questions remain to be resolved, such as the character and quantitative impact of latitudinal variations in Southern Ocean– atmosphere gas exchange on CO2,atm levels and other ocean regions, as well as the character and consequences of marine carbon cycling in the Southern Ocean during other warmer-thanpresent day climate intervals such as MIS11 or the mid-Pliocene Warm Period.

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