Elucidating modern West Antarctic sea surface conditions: An intercomparison of lipid biomarker proxies, instrumental and numerical-model data

• Main Authors: Lamping, Nele, Müller, Juliane, Hefter, Jens, Mollenhauer, Gesine, Haas, Christian, Shi, Xiaoxu, Vorrath, Maria-Elena, Lohmann, Gerrit
• Format: Text
• Language: English
• Published: 2021
• Subjects: Antarctic; Southern Ocean; West Antarctica; Antarc*; Antarctica; Ice Shelf; Ice Shelves; Sea ice
• Online Access: https://doi.org/10.5194/cp-2021-19; https://cp.copernicus.org/preprints/cp-2021-19/

The importance of Southern Ocean sea ice has come into the focus of polar research in the last couple of decades. Especially in West Antarctica, where sea ice has declined, its distribution and evolution play a critical role for the stability of nearby ice shelves. Organic geochemical analyses of marine surface sediments from the West Antarctic continental shelves permit a biomarker-based reconstruction of sea surface conditions in these vulnerable areas. We analysed highly branched isoprenoids (HBIs), such as the sea-ice proxy IPSO 25 and phytoplankton-derived HBI-trienes, but also phytosterols and isoprenoidal glycerol dialkyl glycerol tetraethers (GDGTs), which are established tools for the reconstruction of primary productivity and sea surface temperatures, respectively. The combination of IPSO 25 with a phytoplankton marker results in the semi-quantitative sea-ice index PIPSO 25 , which provides useful reconstructions of sea-ice conditions, avoiding misleading over- or underestimations of sea-ice cover. Comparisons of the biomarker-based sea-ice distribution patterns and GDGT-based temperatures with (1) sea-ice distributions obtained from satellite observations and (2) estimated sea-ice patterns and SSTs deduced from modelled data are in reasonable agreement, but also highlight specific aspects that need to be considered when interpreting biomarker data. We further discuss IPSO 25 concentrations in the vicinity of ice shelves, where elevated values could be related to the occurrence of ice shelf basal melt water and platelet ice under landfast sea ice.