1987
DOI: 10.5194/gh-42-93-1987
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Zur letzten Eiszeit im alpinen und nordeuropäischen Raum

Abstract: Abstract. On the last Glaciation of the Alps and Fennoscandia. During the Pleistocene the Alps and the Fennoscandian Shield were covered several times with extensive ice caps. During the last Ice Age. the Würm or Weichsel Glaciation, the maximum extent of the glaciers occurred at the end of the Ice Age, as late as 20.000 years ago. The main retreat phases during deglaciation were marked as distinct ice marginal zones and dated between 20,000 and 9,000 BP.

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Cited by 9 publications
(5 citation statements)
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“…graminicola remained ice-free during the Last Glacial Maximum [69], thus the species could have survived at least the last glaciation within the southern edge of Südschwarzwald. Moreover, if its limited occurrence to a single mountain is confirmed, it will suggest that T .…”
Section: Discussionmentioning
confidence: 99%
“…graminicola remained ice-free during the Last Glacial Maximum [69], thus the species could have survived at least the last glaciation within the southern edge of Südschwarzwald. Moreover, if its limited occurrence to a single mountain is confirmed, it will suggest that T .…”
Section: Discussionmentioning
confidence: 99%
“…The longest continuous record of glaciation in the Southern Alps comes from a core drilled from the sea floor about 300 km off the east coast of the South Island. This site, known as Deep Sea Drilling Programme (DSDP) site 594, consists of alternating layers of pelagic sediment derived from free-swimming marine organisms and hemipelagic deposits that consist in part FIGURES 3A AND B (a) Pleistocene glaciation of the Alps, based on Glückert (1987) and Lister et al (1998) of sediments derived from the Southern Alps (Nelson et al 1985). Analysis of the top 100 m of the core has yielded an apparently uninterrupted record of sedimentation that records 12 major periods of alpine glaciation over the last 730,000 years.…”
Section: Southern Alpsmentioning
confidence: 99%
“…Moreover, N. enslini was only found in sites that were not covered by glaciers during the Last Glacial Maximum (Glückert 1987) but are located very close to the border of Quaternary glaciers. A similar distribution was already observed for the N. virei species complex (Foulquier et al 2008) with its main distribution area located west of the Alps and nearly never overlapping with formerly glaciated areas.…”
Section: Discussionmentioning
confidence: 98%