(Table 1) Age determination of sediments from the Campbell Plateau ...

Campbell Plateau occupies a key position in the southwest Pacific sector of the Southern Ocean. The plateau confines and steers the Antarctic Circumpolar Current (ACC) along its flanks, isolating the Subantarctic plateau from cold polar waters. Oxygen and carbon isotope records from Campbell Plateau...

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Bibliographic Details
Main Authors: Neil, Helen L, Carter, Lionel, Morris, Michele
Format: Dataset
Language:English
Published: PANGAEA 2013
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.821375
https://doi.pangaea.de/10.1594/PANGAEA.821375
id ftdatacite:10.1594/pangaea.821375
record_format openpolar
spelling ftdatacite:10.1594/pangaea.821375 2024-09-30T14:24:29+00:00 (Table 1) Age determination of sediments from the Campbell Plateau ... Neil, Helen L Carter, Lionel Morris, Michele 2013 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.821375 https://doi.pangaea.de/10.1594/PANGAEA.821375 en eng PANGAEA https://dx.doi.org/10.1029/2003pa000975 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label DEPTH, sediment/rock Age, dated Age, dated standard deviation Kasten corer TAN3034 Tangaroa Supplementary Dataset Dataset dataset 2013 ftdatacite https://doi.org/10.1594/pangaea.82137510.1029/2003pa000975 2024-09-02T08:42:43Z Campbell Plateau occupies a key position in the southwest Pacific sector of the Southern Ocean. The plateau confines and steers the Antarctic Circumpolar Current (ACC) along its flanks, isolating the Subantarctic plateau from cold polar waters. Oxygen and carbon isotope records from Campbell Plateau cores provide new records of water mass stratification for the past 130 kyr. During glacial climes, strengthening of the Subantarctic Front (SAF) caused waters over the plateau flanks to be deeply mixed and ~3°C cooler. Waters of the plateau interior remained stratified and isolated from the cold southern waters. In the west, waters cooled markedly (~4°C) owing to reduced entrainment of Tasman Sea water. Marked cooling also occurred north of Campbell Plateau under increased entrainment of polar water by a branch of the SAF. The ACC remained along the flanks of Campbell Plateau during the last interglacial, when interior waters were stratified and warmer by ~1°C than now. ... : Supplement to: Neil, Helen L; Carter, Lionel; Morris, Michele (2004): Thermal isolation of Campbell Plateau, New Zealand, by the Antarctic Circumpolar Current over the past 130 kyr. Paleoceanography, 19(4), PA4008 ... Dataset Antarc* Antarctic Southern Ocean DataCite Antarctic Campbell Plateau ENVELOPE(171.000,171.000,-50.667,-50.667) New Zealand Pacific Southern Ocean The Antarctic
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Event label
DEPTH, sediment/rock
Age, dated
Age, dated standard deviation
Kasten corer
TAN3034
Tangaroa
spellingShingle Event label
DEPTH, sediment/rock
Age, dated
Age, dated standard deviation
Kasten corer
TAN3034
Tangaroa
Neil, Helen L
Carter, Lionel
Morris, Michele
(Table 1) Age determination of sediments from the Campbell Plateau ...
topic_facet Event label
DEPTH, sediment/rock
Age, dated
Age, dated standard deviation
Kasten corer
TAN3034
Tangaroa
description Campbell Plateau occupies a key position in the southwest Pacific sector of the Southern Ocean. The plateau confines and steers the Antarctic Circumpolar Current (ACC) along its flanks, isolating the Subantarctic plateau from cold polar waters. Oxygen and carbon isotope records from Campbell Plateau cores provide new records of water mass stratification for the past 130 kyr. During glacial climes, strengthening of the Subantarctic Front (SAF) caused waters over the plateau flanks to be deeply mixed and ~3°C cooler. Waters of the plateau interior remained stratified and isolated from the cold southern waters. In the west, waters cooled markedly (~4°C) owing to reduced entrainment of Tasman Sea water. Marked cooling also occurred north of Campbell Plateau under increased entrainment of polar water by a branch of the SAF. The ACC remained along the flanks of Campbell Plateau during the last interglacial, when interior waters were stratified and warmer by ~1°C than now. ... : Supplement to: Neil, Helen L; Carter, Lionel; Morris, Michele (2004): Thermal isolation of Campbell Plateau, New Zealand, by the Antarctic Circumpolar Current over the past 130 kyr. Paleoceanography, 19(4), PA4008 ...
format Dataset
author Neil, Helen L
Carter, Lionel
Morris, Michele
author_facet Neil, Helen L
Carter, Lionel
Morris, Michele
author_sort Neil, Helen L
title (Table 1) Age determination of sediments from the Campbell Plateau ...
title_short (Table 1) Age determination of sediments from the Campbell Plateau ...
title_full (Table 1) Age determination of sediments from the Campbell Plateau ...
title_fullStr (Table 1) Age determination of sediments from the Campbell Plateau ...
title_full_unstemmed (Table 1) Age determination of sediments from the Campbell Plateau ...
title_sort (table 1) age determination of sediments from the campbell plateau ...
publisher PANGAEA
publishDate 2013
url https://dx.doi.org/10.1594/pangaea.821375
https://doi.pangaea.de/10.1594/PANGAEA.821375
long_lat ENVELOPE(171.000,171.000,-50.667,-50.667)
geographic Antarctic
Campbell Plateau
New Zealand
Pacific
Southern Ocean
The Antarctic
geographic_facet Antarctic
Campbell Plateau
New Zealand
Pacific
Southern Ocean
The Antarctic
genre Antarc*
Antarctic
Southern Ocean
genre_facet Antarc*
Antarctic
Southern Ocean
op_relation https://dx.doi.org/10.1029/2003pa000975
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.82137510.1029/2003pa000975
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