(Table S3) Possible ties beyond 1215 ka in the slower sedimentation rate age model of IODP Exp302 composite core
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.832425 https://doi.org/10.1594/PANGAEA.832425 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.832425 2023-05-15T14:53:45+02:00 (Table S3) Possible ties beyond 1215 ka in the slower sedimentation rate age model of IODP Exp302 composite core O'Regan, Matthew King, John W Backman, Jan Jakobsson, Martin Pälike, Heiko Moran, Kathryn Heil, Chip Sakamoto, Tatsuhiko Cronin, Thomas M Jordan, Richard William LATITUDE: 87.890000 * LONGITUDE: 137.650000 * MINIMUM DEPTH, sediment/rock: 16.23 m * MAXIMUM DEPTH, sediment/rock: 26.69 m 2008-05-09 text/tab-separated-values, 28 data points https://doi.pangaea.de/10.1594/PANGAEA.832425 https://doi.org/10.1594/PANGAEA.832425 en eng PANGAEA https://doi.org/10.1594/PANGAEA.832427 O'Regan, Matthew; King, John W; Backman, Jan; Jakobsson, Martin; Pälike, Heiko; Moran, Kathryn; Heil, Chip; Sakamoto, Tatsuhiko; Cronin, Thomas M; Jordan, Richard William (2008): Constraints on the Pleistocene chronology of sediments from the Lomonosov Ridge. Paleoceanography, 23(1), PA1S19, https://doi.org/10.1029/2007PA001551 https://doi.pangaea.de/10.1594/PANGAEA.832425 https://doi.org/10.1594/PANGAEA.832425 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY 302-CompSite Age model Arctic Coring Expedition ACEX COMPCORE Composite Core Datum level DEPTH sediment/rock Exp302 Integrated Ocean Drilling Program / International Ocean Discovery Program IODP Vidar Viking Dataset 2008 ftpangaea https://doi.org/10.1594/PANGAEA.832425 https://doi.org/10.1594/PANGAEA.832427 https://doi.org/10.1029/2007PA001551 2023-01-20T09:49:39Z Dataset Arctic PANGAEA - Data Publisher for Earth & Environmental Science Arctic ENVELOPE(137.650000,137.650000,87.890000,87.890000) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
302-CompSite Age model Arctic Coring Expedition ACEX COMPCORE Composite Core Datum level DEPTH sediment/rock Exp302 Integrated Ocean Drilling Program / International Ocean Discovery Program IODP Vidar Viking |
spellingShingle |
302-CompSite Age model Arctic Coring Expedition ACEX COMPCORE Composite Core Datum level DEPTH sediment/rock Exp302 Integrated Ocean Drilling Program / International Ocean Discovery Program IODP Vidar Viking O'Regan, Matthew King, John W Backman, Jan Jakobsson, Martin Pälike, Heiko Moran, Kathryn Heil, Chip Sakamoto, Tatsuhiko Cronin, Thomas M Jordan, Richard William (Table S3) Possible ties beyond 1215 ka in the slower sedimentation rate age model of IODP Exp302 composite core |
topic_facet |
302-CompSite Age model Arctic Coring Expedition ACEX COMPCORE Composite Core Datum level DEPTH sediment/rock Exp302 Integrated Ocean Drilling Program / International Ocean Discovery Program IODP Vidar Viking |
format |
Dataset |
author |
O'Regan, Matthew King, John W Backman, Jan Jakobsson, Martin Pälike, Heiko Moran, Kathryn Heil, Chip Sakamoto, Tatsuhiko Cronin, Thomas M Jordan, Richard William |
author_facet |
O'Regan, Matthew King, John W Backman, Jan Jakobsson, Martin Pälike, Heiko Moran, Kathryn Heil, Chip Sakamoto, Tatsuhiko Cronin, Thomas M Jordan, Richard William |
author_sort |
O'Regan, Matthew |
title |
(Table S3) Possible ties beyond 1215 ka in the slower sedimentation rate age model of IODP Exp302 composite core |
title_short |
(Table S3) Possible ties beyond 1215 ka in the slower sedimentation rate age model of IODP Exp302 composite core |
title_full |
(Table S3) Possible ties beyond 1215 ka in the slower sedimentation rate age model of IODP Exp302 composite core |
title_fullStr |
(Table S3) Possible ties beyond 1215 ka in the slower sedimentation rate age model of IODP Exp302 composite core |
title_full_unstemmed |
(Table S3) Possible ties beyond 1215 ka in the slower sedimentation rate age model of IODP Exp302 composite core |
title_sort |
(table s3) possible ties beyond 1215 ka in the slower sedimentation rate age model of iodp exp302 composite core |
publisher |
PANGAEA |
publishDate |
2008 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.832425 https://doi.org/10.1594/PANGAEA.832425 |
op_coverage |
LATITUDE: 87.890000 * LONGITUDE: 137.650000 * MINIMUM DEPTH, sediment/rock: 16.23 m * MAXIMUM DEPTH, sediment/rock: 26.69 m |
long_lat |
ENVELOPE(137.650000,137.650000,87.890000,87.890000) |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
op_relation |
https://doi.org/10.1594/PANGAEA.832427 O'Regan, Matthew; King, John W; Backman, Jan; Jakobsson, Martin; Pälike, Heiko; Moran, Kathryn; Heil, Chip; Sakamoto, Tatsuhiko; Cronin, Thomas M; Jordan, Richard William (2008): Constraints on the Pleistocene chronology of sediments from the Lomonosov Ridge. Paleoceanography, 23(1), PA1S19, https://doi.org/10.1029/2007PA001551 https://doi.pangaea.de/10.1594/PANGAEA.832425 https://doi.org/10.1594/PANGAEA.832425 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.832425 https://doi.org/10.1594/PANGAEA.832427 https://doi.org/10.1029/2007PA001551 |
_version_ |
1766325343471271936 |