Project Details
Projekt
Interrelations of tectonic deformation and surface erosion with West Antarctic Ice Sheet dynamics
Subject Area
Palaeontology
Term
from 2014 to 2019
Project identifier
Deutsche Forschungsgemeinschaft (DFG) - Project number 258133812
West Antarctica, and particularly the Amundsen Sea area, hosts glaciers with the most pronounced mass losses of the whole continent. Complete collapse of the West Antarctic Ice Sheet would result in a global sea level rise of 3 to 5 m. Apart from climatic and oceanographic changes, ice sheets are influenced by the tectonic and structural history as well as by heat flow patterns of the underlying bedrock. This project plan aims for a better understanding of the long-term geodynamic and paleo-topographic evolution of the Amundsen Sea area, of its heat flow distribution, and of its glacial thinning and retreat history. This will be achieved by applying a combination of geophysical methods, thermochronology, and surface exposure dating. Combining these data sets will provide information on spatial and temporal correlations of geodynamic activity, heat flow patterns, and ice sheet evolution. In more general terms, this project will contribute to a better understanding of relations between lithospheric processes, surface processes, and glacial dynamics. The project is based on Polarstern expedition XXX/3 in February-March 2015. During this expedition, the shallow drilling MeBo device will be deployed, enabling the first drilling campaign in the Amundsen Sea. Cored material will include basement rocks and clastic sediments presumably covering the time from the Cretaceous to the present, offering a unique opportunity for studying the evolution of the Amundsen Sea area.
DFG Programme
Infrastructure Priority Programmes
Subproject of
SPP 1158:
Infrastructure area - Antarctic Research with Comparative Investigations in Arctic Sea Ice Areas
Participating Person
Professor Dr. Frank Lisker
