Southern Ocean marine sediment core sea-ice records for the last 150,000 years ...

Antarctic sea ice forms a critical part of the Southern Ocean and global climate system. The behaviour of Antarctic sea ice throughout the last glacial-interglacial (G-IG) cycle (12,000-130,000 years) allows us to investigate the interactions between sea ice and climate under a large range of mean c...

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Bibliographic Details
Main Authors: Chadwick, Matthew, Crosta, Xavier, Esper, Oliver, Kohfeld, Karen E
Format: Dataset
Language:English
Published: PANGAEA 2022
Subjects:
AGE
Online Access:https://dx.doi.org/10.1594/pangaea.943275
https://doi.pangaea.de/10.1594/PANGAEA.943275
id ftdatacite:10.1594/pangaea.943275
record_format openpolar
spelling ftdatacite:10.1594/pangaea.943275 2024-09-30T14:25:25+00:00 Southern Ocean marine sediment core sea-ice records for the last 150,000 years ... Chadwick, Matthew Crosta, Xavier Esper, Oliver Kohfeld, Karen E 2022 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.943275 https://doi.pangaea.de/10.1594/PANGAEA.943275 en eng PANGAEA https://dx.doi.org/10.1016/j.quascirev.2011.04.002 https://dx.doi.org/10.1016/j.quascirev.2016.06.006 https://dx.doi.org/10.1016/s0031-0182(02)00516-3 https://dx.doi.org/10.1016/j.quascirev.2013.02.004 https://dx.doi.org/10.1029/2011pa002264 https://dx.doi.org/10.1029/98pa00339 https://dx.doi.org/10.1016/s0377-8398(03)00072-0 https://dx.doi.org/10.1016/j.palaeo.2014.01.019 https://dx.doi.org/10.1002/2014pa002764 https://dx.doi.org/10.1007/bf02369010 https://dx.doi.org/10.1016/s0031-0182(00)00131-0 https://dx.doi.org/10.1016/j.marmicro.2020.101894 https://dx.doi.org/10.5194/cp-18-465-2022 https://dx.doi.org/10.1016/j.dsr2.2015.03.011 https://dx.doi.org/10.1016/j.quascirev.2019.04.007 https://dx.doi.org/10.1016/j.yqres.2011.11.006 https://dx.doi.org/10.1029/2000pa000599 https://dx.doi.org/10.1002/2014pa002745 https://dx.doi.org/10.1130/g20709.1 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Diatoms Glacial - Interglacial marine sediments Sea ice Southern Ocean Event label DEPTH, sediment/rock AGE Fragilariopsis curta and Fragilariopsis cylindrus Sea ice concentration, winter Sea ice cover duration Reference/source Composite Core Piston corer Piston corer BGR type Gravity corer Kiel type Core Gravity corer Calculated, see references Leg177 ELT27 ANT-XVIII/5a ANT-XXII/4 ANT-XXVI/2 ANT-VI/3 ANT-VIII/3 ANT-IX/4 ANT-X/5 ANT-XI/2 ANT-XI/4 SO136 Joides Resolution Eltanin Polarstern Sonne Past Global Changes - Cycles of Sea-Ice Dynamics in the Earth system PAGES_C-SIDE Dataset dataset 2022 ftdatacite https://doi.org/10.1594/pangaea.94327510.1016/j.quascirev.2011.04.00210.1016/j.quascirev.2016.06.00610.1016/s0031-0182(02)00516-310.1016/j.quascirev.2013.02.00410.1029/2011pa00226410.1029/98pa0033910.1016/s0377-8398(03)00072-010.1016/j.palaeo.2014.01.0191 2024-09-02T08:44:46Z Antarctic sea ice forms a critical part of the Southern Ocean and global climate system. The behaviour of Antarctic sea ice throughout the last glacial-interglacial (G-IG) cycle (12,000-130,000 years) allows us to investigate the interactions between sea ice and climate under a large range of mean climate states. Understanding both temporal and spatial variations in Antarctic sea ice across a G-IG cycle is crucial to better understanding the G-IG regulation of atmospheric CO2, ocean circulation, nutrient cycling and productivity. Published qualitative and quantitative records of G-IG sea-ice, which cover at least 30,000 of the last 150,000 years, are compiled from twenty four marine sediment cores. All records include the combined relative abundances of the two sea-ice related diatoms Fragilariopsis curta and F. cylindrus (FCC). The FCC proxy is a qualitative indicator of winter sea-ice presence (Gersonde and Zielinski, 2000). Fourteen of the core records also have quantitative reconstructions of winter ... Dataset Antarc* Antarctic Sea ice Southern Ocean DataCite Antarctic Southern Ocean
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Diatoms
Glacial - Interglacial
marine sediments
Sea ice
Southern Ocean
Event label
DEPTH, sediment/rock
AGE
Fragilariopsis curta and Fragilariopsis cylindrus
Sea ice concentration, winter
Sea ice cover duration
Reference/source
Composite Core
Piston corer
Piston corer BGR type
Gravity corer Kiel type
Core
Gravity corer
Calculated, see references
Leg177
ELT27
ANT-XVIII/5a
ANT-XXII/4
ANT-XXVI/2
ANT-VI/3
ANT-VIII/3
ANT-IX/4
ANT-X/5
ANT-XI/2
ANT-XI/4
SO136
Joides Resolution
Eltanin
Polarstern
Sonne
Past Global Changes - Cycles of Sea-Ice Dynamics in the Earth system PAGES_C-SIDE
spellingShingle Diatoms
Glacial - Interglacial
marine sediments
Sea ice
Southern Ocean
Event label
DEPTH, sediment/rock
AGE
Fragilariopsis curta and Fragilariopsis cylindrus
Sea ice concentration, winter
Sea ice cover duration
Reference/source
Composite Core
Piston corer
Piston corer BGR type
Gravity corer Kiel type
Core
Gravity corer
Calculated, see references
Leg177
ELT27
ANT-XVIII/5a
ANT-XXII/4
ANT-XXVI/2
ANT-VI/3
ANT-VIII/3
ANT-IX/4
ANT-X/5
ANT-XI/2
ANT-XI/4
SO136
Joides Resolution
Eltanin
Polarstern
Sonne
Past Global Changes - Cycles of Sea-Ice Dynamics in the Earth system PAGES_C-SIDE
Chadwick, Matthew
Crosta, Xavier
Esper, Oliver
Kohfeld, Karen E
Southern Ocean marine sediment core sea-ice records for the last 150,000 years ...
topic_facet Diatoms
Glacial - Interglacial
marine sediments
Sea ice
Southern Ocean
Event label
DEPTH, sediment/rock
AGE
Fragilariopsis curta and Fragilariopsis cylindrus
Sea ice concentration, winter
Sea ice cover duration
Reference/source
Composite Core
Piston corer
Piston corer BGR type
Gravity corer Kiel type
Core
Gravity corer
Calculated, see references
Leg177
ELT27
ANT-XVIII/5a
ANT-XXII/4
ANT-XXVI/2
ANT-VI/3
ANT-VIII/3
ANT-IX/4
ANT-X/5
ANT-XI/2
ANT-XI/4
SO136
Joides Resolution
Eltanin
Polarstern
Sonne
Past Global Changes - Cycles of Sea-Ice Dynamics in the Earth system PAGES_C-SIDE
description Antarctic sea ice forms a critical part of the Southern Ocean and global climate system. The behaviour of Antarctic sea ice throughout the last glacial-interglacial (G-IG) cycle (12,000-130,000 years) allows us to investigate the interactions between sea ice and climate under a large range of mean climate states. Understanding both temporal and spatial variations in Antarctic sea ice across a G-IG cycle is crucial to better understanding the G-IG regulation of atmospheric CO2, ocean circulation, nutrient cycling and productivity. Published qualitative and quantitative records of G-IG sea-ice, which cover at least 30,000 of the last 150,000 years, are compiled from twenty four marine sediment cores. All records include the combined relative abundances of the two sea-ice related diatoms Fragilariopsis curta and F. cylindrus (FCC). The FCC proxy is a qualitative indicator of winter sea-ice presence (Gersonde and Zielinski, 2000). Fourteen of the core records also have quantitative reconstructions of winter ...
format Dataset
author Chadwick, Matthew
Crosta, Xavier
Esper, Oliver
Kohfeld, Karen E
author_facet Chadwick, Matthew
Crosta, Xavier
Esper, Oliver
Kohfeld, Karen E
author_sort Chadwick, Matthew
title Southern Ocean marine sediment core sea-ice records for the last 150,000 years ...
title_short Southern Ocean marine sediment core sea-ice records for the last 150,000 years ...
title_full Southern Ocean marine sediment core sea-ice records for the last 150,000 years ...
title_fullStr Southern Ocean marine sediment core sea-ice records for the last 150,000 years ...
title_full_unstemmed Southern Ocean marine sediment core sea-ice records for the last 150,000 years ...
title_sort southern ocean marine sediment core sea-ice records for the last 150,000 years ...
publisher PANGAEA
publishDate 2022
url https://dx.doi.org/10.1594/pangaea.943275
https://doi.pangaea.de/10.1594/PANGAEA.943275
geographic Antarctic
Southern Ocean
geographic_facet Antarctic
Southern Ocean
genre Antarc*
Antarctic
Sea ice
Southern Ocean
genre_facet Antarc*
Antarctic
Sea ice
Southern Ocean
op_relation https://dx.doi.org/10.1016/j.quascirev.2011.04.002
https://dx.doi.org/10.1016/j.quascirev.2016.06.006
https://dx.doi.org/10.1016/s0031-0182(02)00516-3
https://dx.doi.org/10.1016/j.quascirev.2013.02.004
https://dx.doi.org/10.1029/2011pa002264
https://dx.doi.org/10.1029/98pa00339
https://dx.doi.org/10.1016/s0377-8398(03)00072-0
https://dx.doi.org/10.1016/j.palaeo.2014.01.019
https://dx.doi.org/10.1002/2014pa002764
https://dx.doi.org/10.1007/bf02369010
https://dx.doi.org/10.1016/s0031-0182(00)00131-0
https://dx.doi.org/10.1016/j.marmicro.2020.101894
https://dx.doi.org/10.5194/cp-18-465-2022
https://dx.doi.org/10.1016/j.dsr2.2015.03.011
https://dx.doi.org/10.1016/j.quascirev.2019.04.007
https://dx.doi.org/10.1016/j.yqres.2011.11.006
https://dx.doi.org/10.1029/2000pa000599
https://dx.doi.org/10.1002/2014pa002745
https://dx.doi.org/10.1130/g20709.1
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.1594/pangaea.94327510.1016/j.quascirev.2011.04.00210.1016/j.quascirev.2016.06.00610.1016/s0031-0182(02)00516-310.1016/j.quascirev.2013.02.00410.1029/2011pa00226410.1029/98pa0033910.1016/s0377-8398(03)00072-010.1016/j.palaeo.2014.01.0191
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