hdl:10013/epic.38044
Pine Island Glacier reached current limits by the mid-Holocene evidence from exposure dating
Johnson, J. S., Schaefer, J. M., Schimmelpfennig, I., Smith, J. A., Bentley, M. J., Fogwill, C. J. and Gohl, Karsten
ORCID: https://orcid.org/0000-0002-9558-2116
;

Contact
Karsten.Gohl [ at ] awi.de
Abstract
Item Type
Conference
(Poster)
Authors
Johnson, J. S., Schaefer, J. M., Schimmelpfennig, I., Smith, J. A., Bentley, M. J., Fogwill, C. J. and Gohl, Karsten
ORCID: https://orcid.org/0000-0002-9558-2116
;

Divisions
Programs
Helmholtz Research Programs > PACES I (2009-2013) > TOPIC 3: Lessons from the Past
Helmholtz Research Programs > PACES I (2009-2013) > TOPIC 3: Lessons from the Past > WP 3.2: Tectonic, Climate and Biosphere Development from Greenhouse to Icehouse
Helmholtz Research Programs > PACES I (2009-2013) > TOPIC 3: Lessons from the Past > WP 3.2: Tectonic, Climate and Biosphere Development from Greenhouse to Icehouse
Peer revision
Not peer-reviewed
Publication Status
Published
Event Details
11th International Symposium of Antarctic Earth Sciences (ISAES), EdinburghJuly 2011..
Eprint ID
24901
Cite as
Johnson, J. S.
,
Schaefer, J. M.
,
Schimmelpfennig, I.
,
Smith, J. A.
,
Bentley, M. J.
,
Fogwill, C. J.
and
Gohl, K.
(2011):
Pine Island Glacier reached current limits by the mid-Holocene evidence from exposure dating
,
11th International Symposium of Antarctic Earth Sciences (ISAES), EdinburghJuly 2011.
.
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