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General Information:
Citation:
Johnson, J. S.
,
Schaefer, J. M.
,
Schimmelpfennig, I.
,
Smith, J. A.
,
Bentley, M. J.
,
Fogwill, C. J.
and
Gohl, K. 
ORCID: https://orcid.org/0000-0002-9558-2116
(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.
.
ORCID: https://orcid.org/0000-0002-9558-2116
(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.
.
Cite this page as:
hdl:10013/epic.38044
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Further Details:
Item Type:
Conference
Authors:
Johnson, J. S.
;
Schaefer, J. M.
;
Schimmelpfennig, I.
;
Smith, J. A.
;
Bentley, M. J.
;
Fogwill, C. J.
;
Gohl, Karsten
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
Eprint ID:
24901