Sea ice changes in the southwest Pacific sector of the Southern Ocean during the last 140 000 years

• Published in: Climate of the Past
• Main Authors: J. Jones, K. E. Kohfeld, H. Bostock, X. Crosta, M. Liston, G. Dunbar, Z. Chase, A. Leventer, H. Anderson, G. Jacobsen
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2022
• Subjects: Environmental pollution; TD172-193.5; Environmental protection; TD169-171.8; Environmental sciences; GE1-350; Antarctic; Southern Ocean; Pacific; Antarc*; Sea ice
• Online Access: https://doi.org/10.5194/cp-18-465-2022; https://doaj.org/article/66b4bc061f7a483bb4792ddeedef1dc1

Sea ice expansion in the Southern Ocean is believed to have contributed to glacial–interglacial atmospheric CO 2 variability by inhibiting air–sea gas exchange and influencing the ocean's meridional overturning circulation. However, limited data on past sea ice coverage over the last 140 ka (a complete glacial cycle) have hindered our ability to link sea ice expansion to oceanic processes that affect atmospheric CO 2 concentration. Assessments of past sea ice coverage using diatom assemblages have primarily focused on the Last Glacial Maximum ( ∼21 ka) to Holocene, with few quantitative reconstructions extending to the onset of glacial Termination II ( ∼135 ka). Here we provide new estimates of winter sea ice concentrations (WSIC) and summer sea surface temperatures (SSST) for a full glacial–interglacial cycle from the southwestern Pacific sector of the Southern Ocean using the modern analog technique (MAT) on fossil diatom assemblages from deep-sea core TAN1302-96. We examine how the timing of changes in sea ice coverage relates to ocean circulation changes and previously proposed mechanisms of early glacial CO 2 drawdown. We then place SSST estimates within the context of regional SSST records to better understand how these surface temperature changes may be influencing oceanic CO 2 uptake. We find that winter sea ice was absent over the core site during the early glacial period until MIS 4 ( ∼65 ka), suggesting that sea ice may not have been a major contributor to early glacial CO 2 drawdown. Sea ice expansion throughout the glacial–interglacial cycle, however, appears to coincide with observed regional reductions in Antarctic Intermediate Water production and subduction, suggesting that sea ice may have influenced intermediate ocean circulation changes. We observe an early glacial (MIS 5d) weakening of meridional SST gradients between 42 and 59 ∘ S throughout the region, which may have contributed to early reductions in atmospheric CO 2 concentrations through its impact on air–sea gas exchange.