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Paleolimnological trends in total organic carbon indicate natural and anthropogenic sources of acidity in Grosser Arbersee, Germany.

Sci. Total Environ. 107, 83-90 (1991)
DOI
Open Access Green as soon as Postprint is submitted to ZB.
In Grosser Arbersee, a cirque lake in the Bavarian Forest (Germany), the acidification chronology since the late-glacial period has been studied paleolimnologically, applying subfossil diatom assemblages. Distinct phases of acidification could be detected, both natural phases via postglacial development of soils and vegetation in the catchment, and anthropogenic phases via mineral acid depositions. Whereas the former phases were accompanied (and most probably caused as well) by increases in organic carbon contents, the latter phases are characterized by losses of organic carbon contents from the lake.
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Publication type Article: Journal article
Document type Scientific Article
Language english
Publication Year 1991
HGF-reported in Year 0
ISSN (print) / ISBN 0048-9697
e-ISSN 1879-1026
Quellenangaben Volume: 107, Issue: , Pages: 83-90 Article Number: , Supplement: ,
Publisher Elsevier
Reviewing status Peer reviewed
Institute(s) Institute of Ecological Chemistry (IOEC)
Scopus ID 0025918843
Erfassungsdatum 1991-12-31