Chronology and Sedimentary Processes in the Western Ross Sea, Antarctica since the Last Glacial Period

• Published in: Journal of Marine Science and Engineering
• Main Authors: Geng Liu, Zhongshan Shen, Xibin Han, Haifeng Wang, Weiwei Chen, Yi Zhang, Pengyun Ma, Yibing Li, Yun Cai, Pengfei Xue, Huafeng Qin, Chunxia Zhang
• Format: Article in Journal/Newspaper
• Language: English
• Published: MDPI AG 2024
• Subjects: magnetic susceptibility; AMS 14 C; sediment grain size; ice-shelf processes; paleoenvironmental evolution; Naval architecture. Shipbuilding. Marine engineering; VM1-989; Oceanography; GC1-1581; Antarc*; Antarctic; Antarctica; ice core; Ice Sheet; Ice Shelf; Ice Shelves; Ross Ice Shelf; Ross Sea; Sea ice
• Online Access: https://doi.org/10.3390/jmse12020254; https://doaj.org/article/65ad6f216a994a8fab369ce1baf3bc1c

The stability of contemporary ice shelves is under threat due to global warming, and the geological records in the Ross Sea offer such an opportunity to test the linkage between them. However, the absence of calcareous microfossils in the sediments of the Ross Sea results in uncertainties in establishing a precise chronology for studies. Hence, three sediment cores were collected and studied in terms of radiocarbon dating, magnetic susceptibility, and sediment grain size to reconstruct the environmental processes in the Ross Sea since the last glacial period. The main results are as follows: (1) two grain-size components were identified for the studied cores, which can be correlated to ice-shelf and sea-ice transport, respectively; (2) due to old-carbon contamination and an inconsistent carbon reservoir, the radiocarbon dates were generally underestimated, and as an alternative, changes in magnetic susceptibility of the studied cores can be tuned to the ice-core records to establish a reliable age–depth model and; (3) integrating sediment grain-size changes and comparisons with other paleoenvironmental proxies in the Antarctic, a process from a sub-ice sheet in the last glacial period to a sub-ice shelf in the glacial maximum, and, finally, to a glaciomarine state since the last deglacial period was identified in the western Ross Sea. Integrating these findings, the warming processes in the Antarctic were highlighted in the retreat processes of the Ross Ice Shelf in the past.