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
AWI Organizations > Geosciences > Geophysics
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
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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