hdl:10013/epic.12618
The d13C in benthic foraminiferal tests of Fontbotia wuellerstorfi (Schwager) relative to d13C of dissolved inorganic carbon in Southern Ocean deep water: implications for glacial ocean circulation models
Mackensen, Andreas 
ORCID: https://orcid.org/0000-0002-5024-4455, Hubberten, Hans-Wolfgang, Bickert, T., Fischer, G. and Fütterer, Dieter
;
ORCID: https://orcid.org/0000-0002-5024-4455, Hubberten, Hans-Wolfgang, Bickert, T., Fischer, G. and Fütterer, Dieter
;
Contact
amackensen [ at ] awi-bremerhaven.de
Abstract
Item Type
Article
Authors
Mackensen, Andreas ORCID: https://orcid.org/0000-0002-5024-4455, Hubberten, Hans-Wolfgang, Bickert, T., Fischer, G. and Fütterer, Dieter
;
ORCID: https://orcid.org/0000-0002-5024-4455, Hubberten, Hans-Wolfgang, Bickert, T., Fischer, G. and Fütterer, Dieter
;
Divisions
AWI Organizations > Geosciences > Marine Geology and Paleontology
AWI Organizations > Geosciences > Permafrost Research
AWI Organizations > Geosciences > Permafrost Research
Programs
Publication Status
Published
Eprint ID
2027
Cite as
Mackensen, A.
,
Hubberten, H. W.
,
Bickert, T.
,
Fischer, G.
and
Fütterer, D.
(1993):
The d13C in benthic foraminiferal tests of Fontbotia wuellerstorfi (Schwager) relative to d13C of dissolved inorganic carbon in Southern Ocean deep water: implications for glacial ocean circulation models
,
Paleoceanography,
8
(5),
pp. 587-610
.
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