Geochemical composition and radiocarbon ages of cores from Lago Fugnano, Tierra del Fuego

• Main Authors: Waldmann, Nicolas D, Ariztegui, Daniel, Anselmetti, Flavio S, Austin, James A Jr, Moy, Christopher M, Stern, C, Recasens, Cristina, Dunbar, Robert B
• Format: Other/Unknown Material
• Language: English
• Published: PANGAEA 2010
• Subjects: International Polar Year (2007-2008); IPY; Antarc*; Antarctic; ice core; International Polar Year; Tierra del Fuego
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.840656; https://doi.org/10.1594/PANGAEA.840656

Recent advances in the chronology and the palaeoclimatic understanding of Antarctic ice core records point towards a larger heterogeneity of latitudinal climate fluctuations than previously thought. Thus, realistic palaeoclimate reconstructions rely in the development of a tight array of well-constrained records with a dense latitudinal coverage. Climatic records from southernmost South America are critical cornerstones to link these Antarctic palaeoclimatic archives with their South American counterparts. At 54° S on the Island of Tierra del Fuego, Lago Fagnano is located in one of the most substantially and extensively glaciated regions of southernmost South America during the Late Pleistocene. This elongated lake is the largest (~110km long) and non-ice covered lake at high southern latitudes. A multi-proxy study of selected cores allows the characterisation of a Holocene sedimentary record. Detailed petrophysical, sedimentological and geochemical studies of a complete lacustrine laminated sequence reveal variations in major and trace elements, as well as organic content, suggesting high variability in environmental conditions. Comparison of these results with other regional records allows the identification of major known late Holocene climatic intervals and the proposal for a time for the onset of the Southern Westerlies in Tierra del Fuego. These results improve our understanding of the forcing mechanisms behind climate change in southernmost Patagonia.