Authigenic uranium, mass accumulation rates, benthic δ¹³C and SST during the last interglacial period of ODP Site 177-1094 ...

Southern Ocean sediments reveal a spike in authigenic uranium 127,000 years ago, within the last interglacial, reflecting decreased oxygenation of deep water by Antarctic Bottom Water (AABW). Unlike ice age reductions in AABW, the interglacial stagnation event appears decoupled from open ocean condi...

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Main Authors: Hayes, Christopher T, Martínez‐García, Alfredo, Hasenfratz, Albin, Jaccard, Samuel L, Hodell, David A, Sigman, Daniel M, Haug, Gerald H, Anderson, Robert F
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2014
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.839454
https://doi.pangaea.de/10.1594/PANGAEA.839454
id ftdatacite:10.1594/pangaea.839454
record_format openpolar
spelling ftdatacite:10.1594/pangaea.839454 2024-09-15T17:41:16+00:00 Authigenic uranium, mass accumulation rates, benthic δ¹³C and SST during the last interglacial period of ODP Site 177-1094 ... Hayes, Christopher T Martínez‐García, Alfredo Hasenfratz, Albin Jaccard, Samuel L Hodell, David A Sigman, Daniel M Haug, Gerald H Anderson, Robert F 2014 application/zip https://dx.doi.org/10.1594/pangaea.839454 https://doi.pangaea.de/10.1594/PANGAEA.839454 en eng PANGAEA https://dx.doi.org/10.1126/science.1256620 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Composite Core Leg177 Joides Resolution Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 2014 ftdatacite https://doi.org/10.1594/pangaea.83945410.1126/science.1256620 2024-08-01T10:53:32Z Southern Ocean sediments reveal a spike in authigenic uranium 127,000 years ago, within the last interglacial, reflecting decreased oxygenation of deep water by Antarctic Bottom Water (AABW). Unlike ice age reductions in AABW, the interglacial stagnation event appears decoupled from open ocean conditions and may have resulted from coastal freshening due to mass loss from the Antarctic ice sheet. AABW reduction coincided with increased North Atlantic Deep Water (NADW) formation, and the subsequent reinvigoration in AABW coincided with reduced NADW formation. Thus, alternation of deep water formation between the Antarctic and the North Atlantic, believed to characterize ice ages, apparently also occurs in warm climates. ... : Supplement to: Hayes, Christopher T; Martínez‐García, Alfredo; Hasenfratz, Albin; Jaccard, Samuel L; Hodell, David A; Sigman, Daniel M; Haug, Gerald H; Anderson, Robert F (2014): A stagnation event in the deep South Atlantic during the last interglacial period. Science, 346(6216), 1514-1517 ... Article in Journal/Newspaper Antarc* Antarctic Ice Sheet NADW North Atlantic Deep Water North Atlantic Southern Ocean DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Composite Core
Leg177
Joides Resolution
Ocean Drilling Program ODP
spellingShingle Composite Core
Leg177
Joides Resolution
Ocean Drilling Program ODP
Hayes, Christopher T
Martínez‐García, Alfredo
Hasenfratz, Albin
Jaccard, Samuel L
Hodell, David A
Sigman, Daniel M
Haug, Gerald H
Anderson, Robert F
Authigenic uranium, mass accumulation rates, benthic δ¹³C and SST during the last interglacial period of ODP Site 177-1094 ...
topic_facet Composite Core
Leg177
Joides Resolution
Ocean Drilling Program ODP
description Southern Ocean sediments reveal a spike in authigenic uranium 127,000 years ago, within the last interglacial, reflecting decreased oxygenation of deep water by Antarctic Bottom Water (AABW). Unlike ice age reductions in AABW, the interglacial stagnation event appears decoupled from open ocean conditions and may have resulted from coastal freshening due to mass loss from the Antarctic ice sheet. AABW reduction coincided with increased North Atlantic Deep Water (NADW) formation, and the subsequent reinvigoration in AABW coincided with reduced NADW formation. Thus, alternation of deep water formation between the Antarctic and the North Atlantic, believed to characterize ice ages, apparently also occurs in warm climates. ... : Supplement to: Hayes, Christopher T; Martínez‐García, Alfredo; Hasenfratz, Albin; Jaccard, Samuel L; Hodell, David A; Sigman, Daniel M; Haug, Gerald H; Anderson, Robert F (2014): A stagnation event in the deep South Atlantic during the last interglacial period. Science, 346(6216), 1514-1517 ...
format Article in Journal/Newspaper
author Hayes, Christopher T
Martínez‐García, Alfredo
Hasenfratz, Albin
Jaccard, Samuel L
Hodell, David A
Sigman, Daniel M
Haug, Gerald H
Anderson, Robert F
author_facet Hayes, Christopher T
Martínez‐García, Alfredo
Hasenfratz, Albin
Jaccard, Samuel L
Hodell, David A
Sigman, Daniel M
Haug, Gerald H
Anderson, Robert F
author_sort Hayes, Christopher T
title Authigenic uranium, mass accumulation rates, benthic δ¹³C and SST during the last interglacial period of ODP Site 177-1094 ...
title_short Authigenic uranium, mass accumulation rates, benthic δ¹³C and SST during the last interglacial period of ODP Site 177-1094 ...
title_full Authigenic uranium, mass accumulation rates, benthic δ¹³C and SST during the last interglacial period of ODP Site 177-1094 ...
title_fullStr Authigenic uranium, mass accumulation rates, benthic δ¹³C and SST during the last interglacial period of ODP Site 177-1094 ...
title_full_unstemmed Authigenic uranium, mass accumulation rates, benthic δ¹³C and SST during the last interglacial period of ODP Site 177-1094 ...
title_sort authigenic uranium, mass accumulation rates, benthic δ¹³c and sst during the last interglacial period of odp site 177-1094 ...
publisher PANGAEA
publishDate 2014
url https://dx.doi.org/10.1594/pangaea.839454
https://doi.pangaea.de/10.1594/PANGAEA.839454
genre Antarc*
Antarctic
Ice Sheet
NADW
North Atlantic Deep Water
North Atlantic
Southern Ocean
genre_facet Antarc*
Antarctic
Ice Sheet
NADW
North Atlantic Deep Water
North Atlantic
Southern Ocean
op_relation https://dx.doi.org/10.1126/science.1256620
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.83945410.1126/science.1256620
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