Mid‐ Weichselian interstadial in Kolari, western Finnish Lapland
F innish L apland is known as an area where numerous sites with sediments from P leistocene glacial and interglacial periods occur. Recent sedimentological observations and dating call for reinterpretation of the record, which shows a complicated M id‐ W eichselian ice‐sheet evolution within the ice...
| Published in: | Boreas |
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| Main Authors: | , , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Wiley
2014
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1111/bor.12060 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fbor.12060 https://onlinelibrary.wiley.com/doi/pdf/10.1111/bor.12060 |
| Summary: | F innish L apland is known as an area where numerous sites with sediments from P leistocene glacial and interglacial periods occur. Recent sedimentological observations and dating call for reinterpretation of the record, which shows a complicated M id‐ W eichselian ice‐sheet evolution within the ice‐divide zone. Here, a large, previously unstudied section from a former H annukainen iron mine was investigated sedimentologically and dated with optically stimulated luminescence ( OSL ). Ten sedimentary units were identified displaying a variety of depositional environments (glacial, glaciolacustrine, fluvial and aeolian). They are all – except for the lowermost, deeply weathered till – interpreted to be of M id‐ or L ate W eichselian/ H olocene age. Five OSL samples from fluvial sediments give ages ranging from 55 to 35 ka, indicating two MIS 3 ice‐free intervals of unknown duration. The M id‐ W eichselian interstadial was interrupted by a re‐advance event, which occurred later than 35 ka and caused glaciotectonic deformation, folding and stacking of older sediments. This new evidence emphasizes the importance of the K olari area when unravelling the complex L ate P leistocene glacial history of northern F inland and adjacent regions. |
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