Clay mineralogy on five NBP cores ...

During 2006, the SHALDRIL program recovered cores of Eocene through Pliocene material at four locations in the northwestern Weddell Sea, each representing a key period in the evolution of the Antarctic Peninsula ice cap. The recovered cores are not continuous, yet they provide a record of climate ch...

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Main Authors: Wellner, Julia S, Anderson, John B, Ehrmann, Werner, Weaver, Fred M, Kirshner, Alexandra E, Livsey, Daniel, Simms, Alexander R
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2012
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.777615
https://doi.pangaea.de/10.1594/PANGAEA.777615
id ftdatacite:10.1594/pangaea.777615
record_format openpolar
spelling ftdatacite:10.1594/pangaea.777615 2024-09-15T17:46:26+00:00 Clay mineralogy on five NBP cores ... Wellner, Julia S Anderson, John B Ehrmann, Werner Weaver, Fred M Kirshner, Alexandra E Livsey, Daniel Simms, Alexander R 2012 application/zip https://dx.doi.org/10.1594/pangaea.777615 https://doi.pangaea.de/10.1594/PANGAEA.777615 en eng PANGAEA https://dx.doi.org/10.1029/2010sp001047 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig NBP0602A Nathaniel B. Palmer article Collection Supplementary Publication Series of Datasets 2012 ftdatacite https://doi.org/10.1594/pangaea.77761510.1029/2010sp001047 2024-08-01T10:52:43Z During 2006, the SHALDRIL program recovered cores of Eocene through Pliocene material at four locations in the northwestern Weddell Sea, each representing a key period in the evolution of the Antarctic Peninsula ice cap. The recovered cores are not continuous, yet they provide a record of climate change with samples from the late Eocene, late Oligocene, middle Miocene, and early Pliocene and represent the only series of samples recovered from the northwestern Weddell Sea and spanning the Cenozoic and the initial growth of the peninsula ice cap. Late Eocene sediments sampled in the James Ross Basin are typically characterized by very dark greenish-gray muddy fine sand with some preserved burrowing and are interpreted to represent a shallow water continental shelf setting. Rare dropstones, primarily of well-cemented sandstones and minor ice-rafted material consisting of angular grains with glacially influenced surface features record the onset of mountain glaciation, the earliest such evidence in the region. ... : Supplement to: Wellner, Julia S; Anderson, John B; Ehrmann, Werner; Weaver, Fred M; Kirshner, Alexandra E; Livsey, Daniel; Simms, Alexander R (2011): History of an evolving ice sheet as recorded in SHALDRIL cores from the Northwestern Weddell Sea, Antarctica. In: Anderson, J.B. & Wellner, J.S. (eds.), Tectonic, Climatic, and Cryospheric Evolution of the Antarctic Peninsula, American Geophysical Union Special Publications, 63, 131-151 ... Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Antarctica Ice cap Ice Sheet Weddell Sea DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Drilling/drill rig
NBP0602A
Nathaniel B. Palmer
spellingShingle Drilling/drill rig
NBP0602A
Nathaniel B. Palmer
Wellner, Julia S
Anderson, John B
Ehrmann, Werner
Weaver, Fred M
Kirshner, Alexandra E
Livsey, Daniel
Simms, Alexander R
Clay mineralogy on five NBP cores ...
topic_facet Drilling/drill rig
NBP0602A
Nathaniel B. Palmer
description During 2006, the SHALDRIL program recovered cores of Eocene through Pliocene material at four locations in the northwestern Weddell Sea, each representing a key period in the evolution of the Antarctic Peninsula ice cap. The recovered cores are not continuous, yet they provide a record of climate change with samples from the late Eocene, late Oligocene, middle Miocene, and early Pliocene and represent the only series of samples recovered from the northwestern Weddell Sea and spanning the Cenozoic and the initial growth of the peninsula ice cap. Late Eocene sediments sampled in the James Ross Basin are typically characterized by very dark greenish-gray muddy fine sand with some preserved burrowing and are interpreted to represent a shallow water continental shelf setting. Rare dropstones, primarily of well-cemented sandstones and minor ice-rafted material consisting of angular grains with glacially influenced surface features record the onset of mountain glaciation, the earliest such evidence in the region. ... : Supplement to: Wellner, Julia S; Anderson, John B; Ehrmann, Werner; Weaver, Fred M; Kirshner, Alexandra E; Livsey, Daniel; Simms, Alexander R (2011): History of an evolving ice sheet as recorded in SHALDRIL cores from the Northwestern Weddell Sea, Antarctica. In: Anderson, J.B. & Wellner, J.S. (eds.), Tectonic, Climatic, and Cryospheric Evolution of the Antarctic Peninsula, American Geophysical Union Special Publications, 63, 131-151 ...
format Article in Journal/Newspaper
author Wellner, Julia S
Anderson, John B
Ehrmann, Werner
Weaver, Fred M
Kirshner, Alexandra E
Livsey, Daniel
Simms, Alexander R
author_facet Wellner, Julia S
Anderson, John B
Ehrmann, Werner
Weaver, Fred M
Kirshner, Alexandra E
Livsey, Daniel
Simms, Alexander R
author_sort Wellner, Julia S
title Clay mineralogy on five NBP cores ...
title_short Clay mineralogy on five NBP cores ...
title_full Clay mineralogy on five NBP cores ...
title_fullStr Clay mineralogy on five NBP cores ...
title_full_unstemmed Clay mineralogy on five NBP cores ...
title_sort clay mineralogy on five nbp cores ...
publisher PANGAEA
publishDate 2012
url https://dx.doi.org/10.1594/pangaea.777615
https://doi.pangaea.de/10.1594/PANGAEA.777615
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Ice cap
Ice Sheet
Weddell Sea
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Ice cap
Ice Sheet
Weddell Sea
op_relation https://dx.doi.org/10.1029/2010sp001047
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.77761510.1029/2010sp001047
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