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Development of anoxia during the Holocene fresh-brackish water transition in the Baltic Sea
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences.
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2001 (English)In: MARINE GEOLOGY, ISSN 0025-3227, Vol. 177, no 3-4, 221-242 p.Article in journal (Refereed) Published
Abstract [en]

One of the most pronounced environmental changes during the Holocene Baltic Sea history was the transition from the freshwater Ancylus Lake to the brackish water Litorina Sea. The establishment of brackish conditions during this transition (the A/L) was c

Place, publisher, year, edition, pages
ELSEVIER SCIENCE BV , 2001. Vol. 177, no 3-4, 221-242 p.
Keyword [en]
laminated sediments; Baltic Sea; paleoredox; paleosalinity; diatom stratigraphy; SEDIMENTARY ORGANIC-MATTER; EARLY DIAGENESIS; GOTLAND DEEP; LAMINATED SEDIMENTS; INTERSTITIAL WATER; MARINE-SEDIMENTS; REDOX CONDITIONS; RICH SEDIMENTS; LEVEL RECORD; BLACK-S
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Geology
Identifiers
URN: urn:nbn:se:uu:diva-37881OAI: oai:DiVA.org:uu-37881DiVA: diva2:65780
Note
Addresses: Sohlenius G, Swedish Univ Agr Sci, Dept Soil Sci, POB 7014, S-75007 Uppsala, Sweden. Swedish Univ Agr Sci, Dept Soil Sci, S-75007 Uppsala, Sweden. Baltic Sea Res Inst, D-18119 Rostock, Germany. Uppsala Univ, Dept Earth Sci, S-75236 Uppsala, SweAvailable from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-14

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