Lake sediment archives of late Holocene climate variability in Lutzow-Holm Bay, East Antarctica

• Main Author: Rudd, Rachel Claire
• Other Authors: Tyler, Jonathan, Tibby, John, School of Physical Sciences
• Format: Thesis
• Language: English
• Published: 2019
• Subjects: climate; Antarctica; paleolimnology; diatoms; stable isotopes; Antarctic; East Antarctica; Lützow-Holm Bay; The Antarctic; Antarc*; ice core
• Online Access: http://hdl.handle.net/2440/123658

Large fluctuations in year-to-year climate variability have been observed at southern high latitudes over the last 60 years, however short instrumental records make the identification and interpretation of long-term trends difficult. In the Antarctic region, the need for a longer term perspective on climate variability can be addressed using natural archives including ice cores and lake and marine sediments. Lakes in coastal ice-free regions sit at the boundary of the continent and the oceans, and provide an opportunity to fill a spatial gap between the ice core records constrained to the interior of the continent, and the more extensively studied lower latitudes. This thesis presents records of environmental change spanning 3000 years inferred from the sediments of two lakes, Lake Hamagiku and Lake Naga, in the Lützow-Holm Bay region of East Antarctica. These records of past environmental change are supported by an investigation into the modern relationship between diatom assemblages and their habitats and lake water chemistry. Specific conductivity was found to be the primary factor explaining variations in diatom assemblage, consistent with previous studies. Diatom assemblages were also observed to differ significantly between the lake littoral region and the lake floor deeper than two metres water depth. These modern observations are used in the interpretation of the fossil diatom records to reflect changes in ice cover as a result of regional temperature variations, where longer ice-free conditions result in a greater relative abundance of the taxa inhabiting the lake floor region. Fossil diatom assemblages revealed a coherent and sustained shift in the relative abundance of key taxa at ~1800 cal. yr BP in both lakes, which is interpreted to reflect regional warming, and an associated increase in the duration of ice-free conditions at these sites. Diatom valve concentration, organic carbon and nitrogen concentrations and carbon and nitrogen stable isotope ratios suggest that the climatic shift at this ...