The role of the Southern Ocean in past global biogeochemical cycling

This thesis describes several recent advances on the role of the Southern Ocean in past global biogeochemical cycling. We focus on the ocean of the Last Glacial Maximum (LGM) and the Pleistocene epoch and apply proxies of long-term climate variability (particularly the deep-sea sediment records of δ\(^{13}\)C and δ\(^{18}\)O). Specifically, we aim to explore how the physical and biogeochemical state of the Southern Ocean influenced past global marine tracer distributions, such that we can better interpret proxy data and improve our understanding of the drivers of long-term climate variability. The focus on the ocean realm is motivated by the large carbon reservoir in the (deep) ocean, which is able to interact with the atmosphere and govern atmospheric pCO\(_2\) on millennial timescales – particularly through Southern Ocean processes. The LGM and Pleistocene represent the most recent glacial extreme and glacial-interglacial cycles, respectively. Therefore, relatively many proxy data are available, and their recorded climate variability is likely indicative of long-term natural climate variability. We applied global ocean models of different complexities (NorESM-OC, HAMOCC2s and TMI) to study the drivers that shape the benthic δ\(^{13}\)C and δ\(^{18}\)O records. Applying these, we studied the role of the Southern Ocean in shaping vertical marine δ\(^{13}\)C gradients (Paper I), as well as its contribution to the δ\(^{18}\)O archive of glacial-interglacial cycles (Paper IV) using idealized model experiments. Besides these, the LGM ocean and its circulation and biological changes are studied to reveal and explore their relative importance in a more complex model setup (NorESM-OC; Papers II and III). A central conclusion of this thesis is that knowledge of the relevant water mass end-member characteristics is fundamental for interpretation of the benthic δ\(^{13}\)C and δ\(^{18}\)O records. We show that Southern source waters (waters originating in the Southern Ocean) have a particularly large potential to influence the records of both δ\(^{13}\)C and δ\(^{18}\)O, through changes in the biogeochemical or physical state of the Southern Ocean. We find that biogeochemical changes in the Southern Ocean (of particularly air-sea gas exchange and nutrient utilisation) have the potential to affect δ\(^{13}\)C globally and with a magnitude relevant for global δ\(^{13}\)C deep-sea records (Paper I). Such major biogeochemical changes are indeed implied by the estimated