Deglacial to postglacial palaeoenvironments of the Celtic Sea: lacustrine conditions versus a continuous marine sequence

Author:

Furze Mark F. A.1,Scourse James D.2,Pieńkowski Anna J.2,Marret Fabienne3,Hobbs William O.4,Carter Rosemary A.2,Long Brian T.2

Affiliation:

1. Earth & Planetary Sciences Division; Department of Physical Sciences; MacEwan University; Edmonton AB Canada T5J 4S2

2. School of Ocean Sciences; College of Natural Sciences; Bangor University; Menai Bridge LL59 5AB UK

3. School of Environmental Sciences; University of Liverpool; Liverpool L69 7ZT UK

4. St. Croix Watershed Research Station; Science Museum of Minnesota; 16910 152nd Street North Marine St. Croix MN 55047 USA

Publisher

Wiley

Subject

Geology,Archeology,Ecology, Evolution, Behavior and Systematics

Reference159 articles.

1. The surficial geology of the Canadian eastern Arctic and Polar continental shelves;Andrews;Continental Shelf Research,1991

2. Appeltans , W. Bouchet , P. Boxshall , G. A. Fauchald , K. Gordon , D. P. Hoeksema , B. W. Poore , G. C. B. van Soest , R. W. M. Stöhr , S. Walter , T. C. Costello , M.J. 2011 World register of marine species http://www.marinespecies.org

3. Foraminifera from the Irish Sea glacigenic deposits at Aberdaron, western Lleyn, North Wales: palaeoenvironmental implications;Austin;Journal of Quaternary Science,1992

4. Evolution of seasonal stratification in the Celtic Sea during the Holocene;Austin;Journal of the Geological Society of London,1997

5. Dinoflagellate cysts in Upper Quaternary sediments from southwestern Norway and potential correlations with the oceanic record;Bakken;Boreas,1986

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