SST reconstruction from sediment cores M125-55-7/8
The western tropical Atlantic (WTA) supplies warm and saline waters to the upper-limb of the Atlantic Meridional Overturning Circulation (AMOC) and may store excess heat and salinity during periods of AMOC slowdown. Since previous sea surface temperature (SST) reconstructions from the WTA typically...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.905301 2023-05-15T18:01:09+02:00 SST reconstruction from sediment cores M125-55-7/8 Hou, Alicia Meng Xiao Bahr, André Schmidt, Stefan Strebl, Cornelia Albuquerque, Ana Luiza Spadano Chiessi, Cristiano Mazur Friedrich, Oliver LATITUDE: -20.363500 * LONGITUDE: -38.623200 * DATE/TIME START: 2016-03-31T19:46:00 * DATE/TIME END: 2016-03-31T21:45:00 2019-08-27 application/zip, 6 datasets https://doi.pangaea.de/10.1594/PANGAEA.905301 https://doi.org/10.1594/PANGAEA.905301 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.905301 https://doi.org/10.1594/PANGAEA.905301 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Hou, Alicia Meng Xiao; Bahr, André; Schmidt, Stefan; Strebl, Cornelia; Albuquerque, Ana Luiza Spadano; Chiessi, Cristiano Mazur; Friedrich, Oliver (2020): Forcing of western tropical South Atlantic sea surface temperature across three glacial-interglacial cycles. Global and Planetary Change, 188, 103150, https://doi.org/10.1016/j.gloplacha.2020.103150 M125 M125_445-7 M125-55-7 Meteor (1986) PC Piston corer SAMBA South Atlantic Ocean Dataset 2019 ftpangaea https://doi.org/10.1594/PANGAEA.905301 https://doi.org/10.1016/j.gloplacha.2020.103150 2023-01-20T07:34:23Z The western tropical Atlantic (WTA) supplies warm and saline waters to the upper-limb of the Atlantic Meridional Overturning Circulation (AMOC) and may store excess heat and salinity during periods of AMOC slowdown. Since previous sea surface temperature (SST) reconstructions from the WTA typically focus on the Last Glacial Maximum and the last deglaciation, additional long-term records spanning several glacial-interglacial transitions are needed in order to elucidate the drivers of long-term WTA SST variability. We performed stable isotope and Mg/Ca analyses on the surface-dwelling planktonic foraminifera Globigerinoides ruber(pink) on a sediment core from the southern WTA to reconstruct surface-ocean changes over the past 322 kyr. We evaluate the relative importance of atmospheric pCO2 concentration, AMOC strength, and trade-wind intensity in driving the thermal evolution of the WTA across multiple glacial-interglacial cycles. Our SST record indicates that CO2 is the primary driver of glacial-interglacial SST variations in the southern WTA, however, its influence was strongly diminished during Marine Isotope Stage 6. A relatively stable cross-equatorial heat distribution over the past 322 kyr suggests that glacial-interglacial variations in AMOC strength did not drive past WTA SST changes at these timescales. The zonal SST contrast within the (sub)tropical South Atlantic displayed a clear glacial-interglacial mode of variability, which we attribute to low-frequency fluctuations in the strength of the southeast trade winds. Based on these findings, we hypothesize that increasing the concentration of greenhouse gases derived from anthropogenic activities may cause the southern WTA to become warmer and thermally homogenous, which may subsequently impact continental moisture-availability over tropical South America. Dataset Planktonic foraminifera South Atlantic Ocean PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-38.623200,-38.623200,-20.363500,-20.363500) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
M125 M125_445-7 M125-55-7 Meteor (1986) PC Piston corer SAMBA South Atlantic Ocean |
spellingShingle |
M125 M125_445-7 M125-55-7 Meteor (1986) PC Piston corer SAMBA South Atlantic Ocean Hou, Alicia Meng Xiao Bahr, André Schmidt, Stefan Strebl, Cornelia Albuquerque, Ana Luiza Spadano Chiessi, Cristiano Mazur Friedrich, Oliver SST reconstruction from sediment cores M125-55-7/8 |
topic_facet |
M125 M125_445-7 M125-55-7 Meteor (1986) PC Piston corer SAMBA South Atlantic Ocean |
description |
The western tropical Atlantic (WTA) supplies warm and saline waters to the upper-limb of the Atlantic Meridional Overturning Circulation (AMOC) and may store excess heat and salinity during periods of AMOC slowdown. Since previous sea surface temperature (SST) reconstructions from the WTA typically focus on the Last Glacial Maximum and the last deglaciation, additional long-term records spanning several glacial-interglacial transitions are needed in order to elucidate the drivers of long-term WTA SST variability. We performed stable isotope and Mg/Ca analyses on the surface-dwelling planktonic foraminifera Globigerinoides ruber(pink) on a sediment core from the southern WTA to reconstruct surface-ocean changes over the past 322 kyr. We evaluate the relative importance of atmospheric pCO2 concentration, AMOC strength, and trade-wind intensity in driving the thermal evolution of the WTA across multiple glacial-interglacial cycles. Our SST record indicates that CO2 is the primary driver of glacial-interglacial SST variations in the southern WTA, however, its influence was strongly diminished during Marine Isotope Stage 6. A relatively stable cross-equatorial heat distribution over the past 322 kyr suggests that glacial-interglacial variations in AMOC strength did not drive past WTA SST changes at these timescales. The zonal SST contrast within the (sub)tropical South Atlantic displayed a clear glacial-interglacial mode of variability, which we attribute to low-frequency fluctuations in the strength of the southeast trade winds. Based on these findings, we hypothesize that increasing the concentration of greenhouse gases derived from anthropogenic activities may cause the southern WTA to become warmer and thermally homogenous, which may subsequently impact continental moisture-availability over tropical South America. |
format |
Dataset |
author |
Hou, Alicia Meng Xiao Bahr, André Schmidt, Stefan Strebl, Cornelia Albuquerque, Ana Luiza Spadano Chiessi, Cristiano Mazur Friedrich, Oliver |
author_facet |
Hou, Alicia Meng Xiao Bahr, André Schmidt, Stefan Strebl, Cornelia Albuquerque, Ana Luiza Spadano Chiessi, Cristiano Mazur Friedrich, Oliver |
author_sort |
Hou, Alicia Meng Xiao |
title |
SST reconstruction from sediment cores M125-55-7/8 |
title_short |
SST reconstruction from sediment cores M125-55-7/8 |
title_full |
SST reconstruction from sediment cores M125-55-7/8 |
title_fullStr |
SST reconstruction from sediment cores M125-55-7/8 |
title_full_unstemmed |
SST reconstruction from sediment cores M125-55-7/8 |
title_sort |
sst reconstruction from sediment cores m125-55-7/8 |
publisher |
PANGAEA |
publishDate |
2019 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.905301 https://doi.org/10.1594/PANGAEA.905301 |
op_coverage |
LATITUDE: -20.363500 * LONGITUDE: -38.623200 * DATE/TIME START: 2016-03-31T19:46:00 * DATE/TIME END: 2016-03-31T21:45:00 |
long_lat |
ENVELOPE(-38.623200,-38.623200,-20.363500,-20.363500) |
genre |
Planktonic foraminifera South Atlantic Ocean |
genre_facet |
Planktonic foraminifera South Atlantic Ocean |
op_source |
Supplement to: Hou, Alicia Meng Xiao; Bahr, André; Schmidt, Stefan; Strebl, Cornelia; Albuquerque, Ana Luiza Spadano; Chiessi, Cristiano Mazur; Friedrich, Oliver (2020): Forcing of western tropical South Atlantic sea surface temperature across three glacial-interglacial cycles. Global and Planetary Change, 188, 103150, https://doi.org/10.1016/j.gloplacha.2020.103150 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.905301 https://doi.org/10.1594/PANGAEA.905301 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.905301 https://doi.org/10.1016/j.gloplacha.2020.103150 |
_version_ |
1766170513119379456 |