Late Holocene sedimentation in coastal areas of the northwestern Ross Sea (Antarctica).

• Main Authors: E. Colizza, F. Finocchiaro, G. Kuhn, L. Langone, R. Melis, K. Mezgec, M. Severi, R. Traversi, R. Udisti, M. Braida, STENNI, Barbara
• Other Authors: European Geosciences Union, E., Colizza, F., Finocchiaro, G., Kuhn, L., Langone, R., Meli, K., Mezgec, M., Severi, R., Traversi, R., Udisti, Stenni, Barbara, M., Braida
• Format: Conference Object
• Language: English
• Published: Copernicus Publications 2013
• Subjects: Marine core; Antarctica; Western Ross Sea; geochemistry; sediments; Antarctic; Ross Sea; Hallett; Cape Hallett; Wood Bay; Antarc*; Ice Shelf
• Online Access: http://hdl.handle.net/10278/42749

Sediment cores and box cores collected in two coastal areas of the northwestern Ross Sea (Antarctica) highlight the possibility of studying the Late Holocene period in detail. In this work we propose a study on two box cores and two gravity cores collected in the Cape Hallett and Wood Bay areas during the 2005 PNRA oceanographic cruise. The two sites are feed by Eastern Antarctic Ice Shelf (EAIS) and previous studies have highlighted a complex postglacial sedimentary sequence, also influenced by local morphology. This study is performed within the framework of the PNRA-ESF PolarCLIMATE HOLOCLIP (Holocene climate variability at high-southern latitudes: an integrated perspective) Project. The data set includes: magnetic susceptibility, X-ray analyses, 210Pb, 14C dating, diatoms and foraminifera assemblages, organic carbon, and grain-size analyses. Furthermore XRF core scanner analyses, colour analysis from digital images, and major, minor and trace element concentration analyses (ICP-AES) are performed. Data show that the box core and upper core sediments represent a very recent sedimentation in which it is possible to observe the parameter variability probably linked to climate variability/changes: these variation will be compared with isotopic record form ice cores collected form the same Antarctic sector.