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
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Not peer-reviewed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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