SST Proxies Chilean (ODP Leg 202 Site 1235 and Site 1234) and Angola Margin (ODP Leg 175 Site 1078 and Site 1079)
The TEX86 paleothermometer has been extensively used to reconstruct past sea water temperatures, but it remains unclear which export depths the proxy represents. Here we used a novel approach to better constrain the proxy recording depths by investigating paleotemperature proxies (TEX86, UK'37,...
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.957090 https://doi.org/10.1594/PANGAEA.957090 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.957090 2024-10-06T13:42:29+00:00 SST Proxies Chilean (ODP Leg 202 Site 1235 and Site 1234) and Angola Margin (ODP Leg 175 Site 1078 and Site 1079) Varma, Devika Hättig, Katrin van der Meer, Marcel T J Reichart, Gert-Jan Schouten, Stefan MEDIAN LATITUDE: -24.057369 * MEDIAN LONGITUDE: -30.134710 * SOUTH-BOUND LATITUDE: -36.219210 * WEST-BOUND LONGITUDE: -73.681810 * NORTH-BOUND LATITUDE: -11.920770 * EAST-BOUND LONGITUDE: 13.400250 * DATE/TIME START: 1997-09-03T18:10:00 * DATE/TIME END: 2002-04-18T10:00:00 2023 application/zip, 4 datasets https://doi.pangaea.de/10.1594/PANGAEA.957090 https://doi.org/10.1594/PANGAEA.957090 en eng PANGAEA Varma, Devika; Hättig, Katrin; van der Meer, Marcel T J; Reichart, Gert-Jan; Schouten, Stefan (2023): Constraining Water Depth Influence on Organic Paleotemperature Proxies Using Sedimentary Archives. Paleoceanography and Paleoclimatology, 38(6), e2022PA004533, https://doi.org/10.1029/2022PA004533 https://doi.pangaea.de/10.1594/PANGAEA.957090 https://doi.org/10.1594/PANGAEA.957090 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess Alkenones GDGTs NIOZ_UU NIOZ Royal Netherlands Institute for Sea Research and Utrecht University Ocean Drilling Program ODP OH-GDGTs SST dataset bundled publication 2023 ftpangaea https://doi.org/10.1594/PANGAEA.95709010.1029/2022PA004533 2024-09-11T00:15:18Z The TEX86 paleothermometer has been extensively used to reconstruct past sea water temperatures, but it remains unclear which export depths the proxy represents. Here we used a novel approach to better constrain the proxy recording depths by investigating paleotemperature proxies (TEX86, UK'37, RI-OH and RI-OH') from two pairs of proximal (< 12 km apart) cores from Chilean and Angola margin, respectively. These cores are from steep continental slopes and lower shelves, which leads to a substantial difference in water depth between them despite being closely located. Surprisingly, the deep and the shallow UK'37 records at the Chilean margin shows dissimilarities, in contrast to the similar records from the Angola margin, which may be due to post-depositional alteration at the former sites. In contrast, the TEX86 records were statistically indistinguishable between the sites at both the locations, even though the GDGT [2]/[3] ratio suggests GDGTs derived from potentially different archaeal communities residing at different depths. A short-lived difference between the TEX86 records is observed during the last glacial period at the Angola margin, possibly due to a contribution of Antarctic Intermediate Waters to the deep site. Modelling suggests that the TEX86 source signal at our core sites reaches its peak abundance at water depths shallower than 350 m. The RI-OH and RI-OH' records show similar variability as the TEX86 records, although regional differences in their absolute temperature estimates exist. Our approach using proximal sediment cores at steep slopes appears useful to constrain the export depth of organic proxy signals for paleoreconstructions. Other/Unknown Material Antarc* Antarctic PANGAEA - Data Publisher for Earth & Environmental Science Antarctic ENVELOPE(-73.681810,13.400250,-11.920770,-36.219210) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Alkenones GDGTs NIOZ_UU NIOZ Royal Netherlands Institute for Sea Research and Utrecht University Ocean Drilling Program ODP OH-GDGTs SST |
spellingShingle |
Alkenones GDGTs NIOZ_UU NIOZ Royal Netherlands Institute for Sea Research and Utrecht University Ocean Drilling Program ODP OH-GDGTs SST Varma, Devika Hättig, Katrin van der Meer, Marcel T J Reichart, Gert-Jan Schouten, Stefan SST Proxies Chilean (ODP Leg 202 Site 1235 and Site 1234) and Angola Margin (ODP Leg 175 Site 1078 and Site 1079) |
topic_facet |
Alkenones GDGTs NIOZ_UU NIOZ Royal Netherlands Institute for Sea Research and Utrecht University Ocean Drilling Program ODP OH-GDGTs SST |
description |
The TEX86 paleothermometer has been extensively used to reconstruct past sea water temperatures, but it remains unclear which export depths the proxy represents. Here we used a novel approach to better constrain the proxy recording depths by investigating paleotemperature proxies (TEX86, UK'37, RI-OH and RI-OH') from two pairs of proximal (< 12 km apart) cores from Chilean and Angola margin, respectively. These cores are from steep continental slopes and lower shelves, which leads to a substantial difference in water depth between them despite being closely located. Surprisingly, the deep and the shallow UK'37 records at the Chilean margin shows dissimilarities, in contrast to the similar records from the Angola margin, which may be due to post-depositional alteration at the former sites. In contrast, the TEX86 records were statistically indistinguishable between the sites at both the locations, even though the GDGT [2]/[3] ratio suggests GDGTs derived from potentially different archaeal communities residing at different depths. A short-lived difference between the TEX86 records is observed during the last glacial period at the Angola margin, possibly due to a contribution of Antarctic Intermediate Waters to the deep site. Modelling suggests that the TEX86 source signal at our core sites reaches its peak abundance at water depths shallower than 350 m. The RI-OH and RI-OH' records show similar variability as the TEX86 records, although regional differences in their absolute temperature estimates exist. Our approach using proximal sediment cores at steep slopes appears useful to constrain the export depth of organic proxy signals for paleoreconstructions. |
format |
Other/Unknown Material |
author |
Varma, Devika Hättig, Katrin van der Meer, Marcel T J Reichart, Gert-Jan Schouten, Stefan |
author_facet |
Varma, Devika Hättig, Katrin van der Meer, Marcel T J Reichart, Gert-Jan Schouten, Stefan |
author_sort |
Varma, Devika |
title |
SST Proxies Chilean (ODP Leg 202 Site 1235 and Site 1234) and Angola Margin (ODP Leg 175 Site 1078 and Site 1079) |
title_short |
SST Proxies Chilean (ODP Leg 202 Site 1235 and Site 1234) and Angola Margin (ODP Leg 175 Site 1078 and Site 1079) |
title_full |
SST Proxies Chilean (ODP Leg 202 Site 1235 and Site 1234) and Angola Margin (ODP Leg 175 Site 1078 and Site 1079) |
title_fullStr |
SST Proxies Chilean (ODP Leg 202 Site 1235 and Site 1234) and Angola Margin (ODP Leg 175 Site 1078 and Site 1079) |
title_full_unstemmed |
SST Proxies Chilean (ODP Leg 202 Site 1235 and Site 1234) and Angola Margin (ODP Leg 175 Site 1078 and Site 1079) |
title_sort |
sst proxies chilean (odp leg 202 site 1235 and site 1234) and angola margin (odp leg 175 site 1078 and site 1079) |
publisher |
PANGAEA |
publishDate |
2023 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.957090 https://doi.org/10.1594/PANGAEA.957090 |
op_coverage |
MEDIAN LATITUDE: -24.057369 * MEDIAN LONGITUDE: -30.134710 * SOUTH-BOUND LATITUDE: -36.219210 * WEST-BOUND LONGITUDE: -73.681810 * NORTH-BOUND LATITUDE: -11.920770 * EAST-BOUND LONGITUDE: 13.400250 * DATE/TIME START: 1997-09-03T18:10:00 * DATE/TIME END: 2002-04-18T10:00:00 |
long_lat |
ENVELOPE(-73.681810,13.400250,-11.920770,-36.219210) |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_relation |
Varma, Devika; Hättig, Katrin; van der Meer, Marcel T J; Reichart, Gert-Jan; Schouten, Stefan (2023): Constraining Water Depth Influence on Organic Paleotemperature Proxies Using Sedimentary Archives. Paleoceanography and Paleoclimatology, 38(6), e2022PA004533, https://doi.org/10.1029/2022PA004533 https://doi.pangaea.de/10.1594/PANGAEA.957090 https://doi.org/10.1594/PANGAEA.957090 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.95709010.1029/2022PA004533 |
_version_ |
1812175692463341568 |