Late quaternary palaeoceanography of the circumpolar deep water from the South Tasman Rise
We use sediment cores from the South Tasman Rise (STR) to reconstruct deepwater circulation in the southwest Pacific sector of the Southern Ocean. Sediment cores MD972106 (45° 09′ S, 146° 17′ E, 3310 m water depth) and GC34 (45° 06′ S, 147° 45′ E, 4002 m water depth) preserve records covering the la...
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Language: | English |
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John Wiley & Sons
2006
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Online Access: | https://espace.library.uq.edu.au/view/UQ:730251 |
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ftunivqespace:oai:espace.library.uq.edu.au:UQ:730251 2023-05-15T18:24:35+02:00 Late quaternary palaeoceanography of the circumpolar deep water from the South Tasman Rise Moy, Andrew D. Howard, William R. Gagan, Michael K. 2006-10-01 https://espace.library.uq.edu.au/view/UQ:730251 eng eng John Wiley & Sons doi:10.1002/jqs.1067 issn:0267-8179 issn:1099-1417 orcid:0000-0002-8279-323X Earth and Planetary Sciences (miscellaneous) Palaeontology Arts and Humanities (miscellaneous) 1201 Arts and Humanities (miscellaneous) 1901 Earth and Planetary Sciences (miscellaneous) 1911 Palaeontology Journal Article 2006 ftunivqespace https://doi.org/10.1002/jqs.1067 2020-08-06T08:38:38Z We use sediment cores from the South Tasman Rise (STR) to reconstruct deepwater circulation in the southwest Pacific sector of the Southern Ocean. Sediment cores MD972106 (45° 09′ S, 146° 17′ E, 3310 m water depth) and GC34 (45° 06′ S, 147° 45′ E, 4002 m water depth) preserve records covering the last 160 k yr, with chronology controlled by calibrated accelerator mass spectrometry radiocarbon dates and benthic foraminiferal δO tied to SPECMAP. The STIR benthic foraminiferal δC records provide new δC values for Southern Ocean deep water spanning the last 160 kyr at sites unlikely to be affected by variations in productivity. The records establish that glacial benthic foraminifera (Cibicidoides spp.) δC values are lower relative to interglacial values and are comparable to previous glacial benthic δC records in the Indian and Pacific sectors of the Southern Ocean. Comparisons of the benthic foraminiferal δ C time series at the STR are made with the equatorial Pacific (V19-30 and Site 846) and the equatorial Atlantic (GeoB1115). The similarity of benthic δC records at the STR to the equatorial Pacific suggest the Southern Ocean deep-water mass closely tracked those of the deep Pacific, and the presence of a δC gradient between the STR and the equatorial Atlantic suggests there was continual production of northern source deep water over the past 160 k yr. Article in Journal/Newspaper Southern Ocean The University of Queensland: UQ eSpace Indian Pacific South Tasman Rise ENVELOPE(148.000,148.000,-47.500,-47.500) Southern Ocean Journal of Quaternary Science 21 7 763 777 |
institution |
Open Polar |
collection |
The University of Queensland: UQ eSpace |
op_collection_id |
ftunivqespace |
language |
English |
topic |
Earth and Planetary Sciences (miscellaneous) Palaeontology Arts and Humanities (miscellaneous) 1201 Arts and Humanities (miscellaneous) 1901 Earth and Planetary Sciences (miscellaneous) 1911 Palaeontology |
spellingShingle |
Earth and Planetary Sciences (miscellaneous) Palaeontology Arts and Humanities (miscellaneous) 1201 Arts and Humanities (miscellaneous) 1901 Earth and Planetary Sciences (miscellaneous) 1911 Palaeontology Moy, Andrew D. Howard, William R. Gagan, Michael K. Late quaternary palaeoceanography of the circumpolar deep water from the South Tasman Rise |
topic_facet |
Earth and Planetary Sciences (miscellaneous) Palaeontology Arts and Humanities (miscellaneous) 1201 Arts and Humanities (miscellaneous) 1901 Earth and Planetary Sciences (miscellaneous) 1911 Palaeontology |
description |
We use sediment cores from the South Tasman Rise (STR) to reconstruct deepwater circulation in the southwest Pacific sector of the Southern Ocean. Sediment cores MD972106 (45° 09′ S, 146° 17′ E, 3310 m water depth) and GC34 (45° 06′ S, 147° 45′ E, 4002 m water depth) preserve records covering the last 160 k yr, with chronology controlled by calibrated accelerator mass spectrometry radiocarbon dates and benthic foraminiferal δO tied to SPECMAP. The STIR benthic foraminiferal δC records provide new δC values for Southern Ocean deep water spanning the last 160 kyr at sites unlikely to be affected by variations in productivity. The records establish that glacial benthic foraminifera (Cibicidoides spp.) δC values are lower relative to interglacial values and are comparable to previous glacial benthic δC records in the Indian and Pacific sectors of the Southern Ocean. Comparisons of the benthic foraminiferal δ C time series at the STR are made with the equatorial Pacific (V19-30 and Site 846) and the equatorial Atlantic (GeoB1115). The similarity of benthic δC records at the STR to the equatorial Pacific suggest the Southern Ocean deep-water mass closely tracked those of the deep Pacific, and the presence of a δC gradient between the STR and the equatorial Atlantic suggests there was continual production of northern source deep water over the past 160 k yr. |
format |
Article in Journal/Newspaper |
author |
Moy, Andrew D. Howard, William R. Gagan, Michael K. |
author_facet |
Moy, Andrew D. Howard, William R. Gagan, Michael K. |
author_sort |
Moy, Andrew D. |
title |
Late quaternary palaeoceanography of the circumpolar deep water from the South Tasman Rise |
title_short |
Late quaternary palaeoceanography of the circumpolar deep water from the South Tasman Rise |
title_full |
Late quaternary palaeoceanography of the circumpolar deep water from the South Tasman Rise |
title_fullStr |
Late quaternary palaeoceanography of the circumpolar deep water from the South Tasman Rise |
title_full_unstemmed |
Late quaternary palaeoceanography of the circumpolar deep water from the South Tasman Rise |
title_sort |
late quaternary palaeoceanography of the circumpolar deep water from the south tasman rise |
publisher |
John Wiley & Sons |
publishDate |
2006 |
url |
https://espace.library.uq.edu.au/view/UQ:730251 |
long_lat |
ENVELOPE(148.000,148.000,-47.500,-47.500) |
geographic |
Indian Pacific South Tasman Rise Southern Ocean |
geographic_facet |
Indian Pacific South Tasman Rise Southern Ocean |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_relation |
doi:10.1002/jqs.1067 issn:0267-8179 issn:1099-1417 orcid:0000-0002-8279-323X |
op_doi |
https://doi.org/10.1002/jqs.1067 |
container_title |
Journal of Quaternary Science |
container_volume |
21 |
container_issue |
7 |
container_start_page |
763 |
op_container_end_page |
777 |
_version_ |
1766205260301336576 |