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Palaeoecology of a marine impact crater in the Ordovician sea
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences. Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences. Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences, Palaeobiology. Paleobiologi.
Paleobiologi.
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences. Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences. Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences, Palaeobiology. Paleobiologi.
2005 (English)In: Palaeontological Association 49th Annual Meeting: University of Oxford, 2005Conference paper, Published paper (Other scientific)
Abstract [en]

Palaeoecology of a marine impact crater in the Ordovician sea

Åsa Frisk1, Maurits Lindström2 and Lars Holmer1

1Department of Earth Sciences, Palaeobiology, Uppsala University, Sweden

2Department of Geology and Geochemistry, Stockholm University, Sweden

The aftermath of marine impacts, in particular the patterns of faunal recovery in and around marine craters, are poorly understood. In the Ordovician Baltoscandian epicontinental sea a bolide impact resulted in the Tvären crater. At present it is located in the Stockholm archipelago, Sweden, where drillings in 1991 resulted in two drill cores.

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2005.
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URN: urn:nbn:se:uu:diva-75218OAI: oai:DiVA.org:uu-75218DiVA: diva2:103128
Available from: 2006-02-15 Created: 2006-02-15

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