hdl:10013/epic.10794

Evidence for a steeper Eemian than Holocene sea surface temperature gradient between Arctic to sub-Arctic regions


Bauch, H. A., Erlenkeuser, H., Fahl, Kirsten ORCID: https://orcid.org/0000-0001-9317-4656, Spielhagen, Robert F., Weinelt, M. S., Andruleit, H. and Henrich, R. ;
Contact
hbauch [ at ] geomar.de

Abstract


Item Type
Article
Authors
Bauch, H. A., Erlenkeuser, H., Fahl, Kirsten ORCID: https://orcid.org/0000-0001-9317-4656, Spielhagen, Robert F., Weinelt, M. S., Andruleit, H. and Henrich, R. ;
Divisions
AWI Organizations > Geosciences > Marine Geology and Paleontology
Programs
Basic Research > Helmholtz Independent Research
Publication Status
Published
Eprint ID
203
Cite as
Bauch, H. A. , Erlenkeuser, H. , Fahl, K. , Spielhagen, R. F. , Weinelt, M. S. , Andruleit, H. and Henrich, R. (1999): Evidence for a steeper Eemian than Holocene sea surface temperature gradient between Arctic to sub-Arctic regions , Palaeogeography palaeoclimatology palaeoecology, 145 (1), pp. 95-117 .


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