(Table 3) Calibrated deglacial ages for the Amundsen Sea Embayment providing an upper and lower estimate for the minimum age of grounding line retreat ...

AGE = Deglacial age. Dates from Hillenbrand et al. (2013) and Kirshner et al. (2012) were recalibrated using an marine reservoir effect (MRE) correction of 1300 ± 70 years. Also listed are the deglacial ages (1-9) for the western Amundsen Sea Embayment (ASE) (see Table 3 in Smith et al., 2011 for de...

Full description

Bibliographic Details
Main Authors: Smith, James A, Hillenbrand, Claus-Dieter, Kuhn, Gerhard, Klages, Johann Philipp, Graham, Alastair G C, Larter, Robert D, Ehrmann, Werner, Moreton, Steven Grahame, Wiers, Steffen, Frederichs, Thomas
Format: Dataset
Language:English
Published: PANGAEA 2014
Subjects:
Event label
Identification
LATITUDE
LONGITUDE
Distance
Distance to landmark
AGE
Age, minimum/young
Age, maximum/old
Reference/source
Vibro corer
Gravity corer
Piston corer
Kasten corer
Gravity corer Kiel type
JR20060109
JR20080221
NBP9902
OSO0910
ANT-XXIII/4
ANT-XXVI/3
James Clark Ross
Nathaniel B. Palmer
Oden
Polarstern
Amundsen Sea
Online Access:https://dx.doi.org/10.1594/pangaea.835463
https://doi.pangaea.de/10.1594/PANGAEA.835463
Description
Summary:AGE = Deglacial age. Dates from Hillenbrand et al. (2013) and Kirshner et al. (2012) were recalibrated using an marine reservoir effect (MRE) correction of 1300 ± 70 years. Also listed are the deglacial ages (1-9) for the western Amundsen Sea Embayment (ASE) (see Table 3 in Smith et al., 2011 for details). ...

Similar Items