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Quaternary, Volume 1, Issue 1
2018 June - 8 articles
Cover Story: The flood history of Lake Storsjön (Sweden), based on lithological, geochemical, and mineral magnetic records of a sediment sequence, reveals catchment-scale processes as well as large-scale climatic change during the Holocene.
Since the onset of the neoglacial period (≈4000 cal yr BP), a tree line descent and the increased occurrence of strong snowmelt flood events caused stronger soil erosion. These vegetation/climate shifts are indicated by the more frequent occurrence of black (flood) layers in the sediments. Their peak ≈2600 cal yr BP coincides with a prominent solar minimum and the prevalence of a negative NAO index. View this paper.
Since the onset of the neoglacial period (≈4000 cal yr BP), a tree line descent and the increased occurrence of strong snowmelt flood events caused stronger soil erosion. These vegetation/climate shifts are indicated by the more frequent occurrence of black (flood) layers in the sediments. Their peak ≈2600 cal yr BP coincides with a prominent solar minimum and the prevalence of a negative NAO index. View this paper.
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Quaternary - ISSN 2571-550X