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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 />

51

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