Articles | Volume 16, issue 4
https://doi.org/10.5194/cp-16-1451-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-16-1451-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
07 Aug 2020
Research article |
| 07 Aug 2020
| 07 Aug 2020
Sea surface temperature in the Indian sector of the Southern Ocean over the Late Glacial and Holocene
Lisa Claire Orme
CORRESPONDING AUTHOR
Norwegian Polar Institute, Tromsø, 9296, Norway
ICARUS, Department of Geography, Maynooth University, Maynooth,
Ireland
Xavier Crosta
UMR 5805 EPOC, Université de Bordeaux, Bordeaux, France
Arto Miettinen
Norwegian Polar Institute, Tromsø, 9296, Norway
Ecosystems and Environment Research Programme, University of Helsinki, Helsinki, Finland
Dmitry V. Divine
Norwegian Polar Institute, Tromsø, 9296, Norway
Katrine Husum
Norwegian Polar Institute, Tromsø, 9296, Norway
Elisabeth Isaksson
Norwegian Polar Institute, Tromsø, 9296, Norway
Lukas Wacker
Department of Physics, ETH Zürich, 8093 Zurich, Switzerland
Rahul Mohan
National Centre for Polar and Ocean Research (NCPOR), Ministry of
Earth Sciences, Vasco-da-Gama, Goa 403804, India
Olivier Ther
UMR 5805 EPOC, Université de Bordeaux, Bordeaux, France
Minoru Ikehara
Center for Advanced Marine Core Research, Kochi University, Nankoku, 783-8502, Japan
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Cited
13 citations as recorded by crossref.
- Climate-driven redox changes in the southern Scotia Sea over the last 35 kyr: Insights from sedimentary sulfur isotope J. Kim et al. 10.1016/j.palaeo.2024.112086
- Paleoproductivity and deep-sea oxygenation in Cosmonaut Sea since the last glacial maximum: impact on atmospheric CO2 L. Hu et al. 10.3389/fmars.2023.1215048
- Diatom based reconstruction of climate evolution through the Last Glacial Maximum to Holocene in the Cosmonaut Sea, East Antarctica Q. Li et al. 10.1016/j.dsr2.2021.104960
- Variety and Distribution of Diatom-Based Sea Ice Proxies in Antarctic Marine Sediments of the Past 2000 Years C. Allen & Z. Weich 10.3390/geosciences12080282
- New cosmogenic nuclide constraints on Late Glacial and Holocene glacier fluctuations in the sub-Antarctic Indian Ocean (Kerguelen Islands, 49°S) J. Charton et al. 10.1016/j.quascirev.2022.107461
- Synergic role of frontal migration and silicic acid concentration in driving diatom productivity in the Indian sector of the Southern Ocean over the past 350 ka S. Shukla et al. 10.1016/j.marmicro.2023.102245
- A Meta‐Analysis of Studies Attributing Significance to Solar Irradiance R. Vachula & A. Cheung 10.1029/2022EA002466
- Seasonally Resolved Holocene Sea Ice Variability Inferred From South Pole Ice Core Chemistry D. Winski et al. 10.1029/2020GL091602
- The Plata plume water penetration into the southwestern Atlantic shelf during the Holocene G. Bonifatto et al. 10.1007/s00367-024-00767-4
- Multi-decadal trends in Antarctic sea-ice extent driven by ENSO–SAM over the last 2,000 years X. Crosta et al. 10.1038/s41561-021-00697-1
- Sea Surface Temperature Changes Reflected by Diatoms in the P6-10 Core from 1893 to 2013 from Prydz Bay, Antarctica Y. Huang et al. 10.3390/jmse11071428
- Antarctic Polar Front migrations in the Kerguelen Plateau region, Southern Ocean, over the past 360 kyrs M. Civel-Mazens et al. 10.1016/j.gloplacha.2021.103526
- Holocene changes in the position of the Southern Hemisphere Westerlies recorded by long-distance transport of pollen to the Kerguelen Islands M. Zwier et al. 10.1016/j.quascirev.2024.108595
13 citations as recorded by crossref.
- Climate-driven redox changes in the southern Scotia Sea over the last 35 kyr: Insights from sedimentary sulfur isotope J. Kim et al. 10.1016/j.palaeo.2024.112086
- Paleoproductivity and deep-sea oxygenation in Cosmonaut Sea since the last glacial maximum: impact on atmospheric CO2 L. Hu et al. 10.3389/fmars.2023.1215048
- Diatom based reconstruction of climate evolution through the Last Glacial Maximum to Holocene in the Cosmonaut Sea, East Antarctica Q. Li et al. 10.1016/j.dsr2.2021.104960
- Variety and Distribution of Diatom-Based Sea Ice Proxies in Antarctic Marine Sediments of the Past 2000 Years C. Allen & Z. Weich 10.3390/geosciences12080282
- New cosmogenic nuclide constraints on Late Glacial and Holocene glacier fluctuations in the sub-Antarctic Indian Ocean (Kerguelen Islands, 49°S) J. Charton et al. 10.1016/j.quascirev.2022.107461
- Synergic role of frontal migration and silicic acid concentration in driving diatom productivity in the Indian sector of the Southern Ocean over the past 350 ka S. Shukla et al. 10.1016/j.marmicro.2023.102245
- A Meta‐Analysis of Studies Attributing Significance to Solar Irradiance R. Vachula & A. Cheung 10.1029/2022EA002466
- Seasonally Resolved Holocene Sea Ice Variability Inferred From South Pole Ice Core Chemistry D. Winski et al. 10.1029/2020GL091602
- The Plata plume water penetration into the southwestern Atlantic shelf during the Holocene G. Bonifatto et al. 10.1007/s00367-024-00767-4
- Multi-decadal trends in Antarctic sea-ice extent driven by ENSO–SAM over the last 2,000 years X. Crosta et al. 10.1038/s41561-021-00697-1
- Sea Surface Temperature Changes Reflected by Diatoms in the P6-10 Core from 1893 to 2013 from Prydz Bay, Antarctica Y. Huang et al. 10.3390/jmse11071428
- Antarctic Polar Front migrations in the Kerguelen Plateau region, Southern Ocean, over the past 360 kyrs M. Civel-Mazens et al. 10.1016/j.gloplacha.2021.103526
- Holocene changes in the position of the Southern Hemisphere Westerlies recorded by long-distance transport of pollen to the Kerguelen Islands M. Zwier et al. 10.1016/j.quascirev.2024.108595
Latest update: 23 Apr 2024
Short summary
A record of past sea temperature in the Indian sector of the Southern Ocean, spanning the last 14 200 years, has been developed by analysis of fossil diatoms in marine sediment. During the late deglaciation the reconstructed temperature changes were highly similar to those over Antarctica, most likely due to a reorganisation of global ocean and atmospheric circulation. During the last 11 600 years temperatures gradually cooled and became increasingly variable.
A record of past sea temperature in the Indian sector of the Southern Ocean, spanning the last...
