the Expedition ARKTIS-XIX/4 of the research vessel POLARSTERN ...
the Expedition ARKTIS-XIX/4 of the research vessel POLARSTERN ...
the Expedition ARKTIS-XIX/4 of the research vessel POLARSTERN ...
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6 Quaternary geological and biological studies on Store<br />
Koldewey and on Geographical Society Ø<br />
Ole Bennike, Holger Cremer, Lena Håkansson, Nadja Hultzsch, Martin Klug,<br />
Svenja Kobabe, Bernd Wagner<br />
Only a few studies were carried out so far to reconstruct <strong>the</strong> Late Quaternary and<br />
Holocene environmental history <strong>of</strong> north eastern Greenland. Therefore, <strong>the</strong> extent<br />
and <strong>the</strong> thickness <strong>of</strong> <strong>the</strong> ice shield and <strong>the</strong> outlet glaciers during <strong>the</strong> Last Glacial<br />
Maximum (LGM) are still under discussion. According to <strong>the</strong> past investigations, <strong>the</strong><br />
deglaciation from <strong>the</strong> shelves started in eastern and north eastern Greenland<br />
somewhen between 16 and 14 ka BP (Funder 1989, 1998). The ice retreat was<br />
interrupted by several standstills or readvances and reached <strong>the</strong> present outer coast<br />
at c. 9-11 ka BP. This was indicated by marine-sedimentological studies,<br />
geomorphological investigations, <strong>the</strong> findings <strong>of</strong> fossils, and <strong>the</strong> study <strong>of</strong> lake<br />
sediments. All lake sediment records from <strong>the</strong> outer coast <strong>of</strong> East Greenland, for<br />
example, are younger than 10 ka BP (Wagner et al. 2000, Wagner & Melles 2001,<br />
Bennike & Björck 2002, Wagner & Melles 2002), and no older lacustrine sediment<br />
sequences have been recovered so far from this part <strong>of</strong> Greenland. However, it was<br />
also suggested that parts <strong>of</strong> <strong>the</strong> outer coast have been ice free during <strong>the</strong> LGM. This<br />
was traced back to <strong>the</strong> findings <strong>of</strong> pre-Holocene shells, for example on Store<br />
Koldewey in Nor<strong>the</strong>ast Greenland (Hjort 1981) or on <strong>the</strong> north eastern Geographical<br />
Society Ø in central East Greenland (Funder & Hjort 1973, Hjort 1981).<br />
In order to better understand <strong>the</strong> past environmental and climatic history <strong>of</strong> East and<br />
Nor<strong>the</strong>ast Greenland, extensive studies including palaeolimnological work,<br />
Quaternary geological work, and <strong>the</strong> investigation <strong>of</strong> <strong>the</strong> recent existing lakes and<br />
soils were carried out on Store Koldewey and Geographical Society Ø during <strong>the</strong><br />
expedition ARK <strong>XIX</strong>/4.<br />
Geographical<br />
Society Ø<br />
Store<br />
Koldewey<br />
Fig. 6-1: Map <strong>of</strong> East and<br />
Nor<strong>the</strong>ast Greenland. The<br />
during <strong>the</strong> field season 2003<br />
studied islands are encircled.<br />
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