A study of the TEX86 paleothermometer in the water column and sediments of the Santa Barbara Basin, California

Particulate organic matter collected during a 2-year period, as part of an ongoing sediment trap study, and a high-resolution sediment record from 1850 to 1987 A.D. from the Santa Barbara Basin were analyzed for TEX86, a temperature proxy based on marine crenarchaeotal membrane lipids. Highest fluxe...

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Authors: Huguet, Carme|||0000-0001-8025-2010; Schimmelmann, Arndt; Thunell, Robert; Lourens, Lucas J.; Sinninghe Damsté, Jaap S.; Schouten, Stefan
Format: Article
Publication date:2007
Country:España
Institution:Universitat Autònoma de Barcelona
Repository:Dipòsit Digital de Documents de la UAB
Language:English
OAI Identifier:oai:ddd.uab.cat:25432
Online Access:https://ddd.uab.cat/record/25432
https://dx.doi.org/urn:doi:10.1029/2006PA001310
Access Level:Open access
Keyword:Santa Barbara Basin
Paleoclimatology
Marine organic chemistry
Geochemical tracers
Sea surface temperature
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author Huguet, Carme|||0000-0001-8025-2010
author2 Schimmelmann, Arndt
Thunell, Robert
Lourens, Lucas J.
Sinninghe Damsté, Jaap S.
Schouten, Stefan
author2_role author
author
author
author
author
author_browse Huguet, Carme|||0000-0001-8025-2010
Lourens, Lucas J.
Schimmelmann, Arndt
Schouten, Stefan
Sinninghe Damsté, Jaap S.
Thunell, Robert
author_facet Huguet, Carme|||0000-0001-8025-2010
Schimmelmann, Arndt
Thunell, Robert
Lourens, Lucas J.
Sinninghe Damsté, Jaap S.
Schouten, Stefan
author_role author
collection Dipòsit Digital de Documents de la UAB
description Particulate organic matter collected during a 2-year period, as part of an ongoing sediment trap study, and a high-resolution sediment record from 1850 to 1987 A.D. from the Santa Barbara Basin were analyzed for TEX86, a temperature proxy based on marine crenarchaeotal membrane lipids. Highest fluxes of crenarchaeotal lipids in the water column were found in May-June 1996 and from October 1996 to January 1997 and, in general, showed a good correlation with mass fluxes. TEX86 reconstructed temperatures from the sediment trap series ranged from 8 to 11°C and were usually substantially lower than sea surface temperatures (SST), indicating that unlike in previous studies, the TEX86 corresponds to subsurface temperatures, likely between 100 and 150 m. TEX86 temperature variations observed in trap samples were not coupled to changes in SST or deep-water temperatures and only to some degree with crenarchaeotal lipid fluxes. This suggests that a complex combination of different depth origins and seasonal growth periods of Crenarchaeota contributed to the variations in TEX86 signal during the annual cycle. TEX86 temperatures in the two sediment cores studied (8-13°C) were also substantially lower than those of instrumental SST records (14-17.5°C) confirming that TEX86 records a subsurface temperature signal in the Santa Barbara Basin. This result highlights the importance of performing calibration studies using sediment traps and core tops before applying the TEX86 temperature proxy in a given study area.
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oai_identifier_str oai:ddd.uab.cat:25432
publishDate 2007
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spelling A study of the TEX86 paleothermometer in the water column and sediments of the Santa Barbara Basin, California Huguet, Carme|||0000-0001-8025-2010 Schimmelmann, Arndt Thunell, Robert Lourens, Lucas J. Sinninghe Damsté, Jaap S. Schouten, Stefan Santa Barbara Basin Paleoclimatology Marine organic chemistry Geochemical tracers Sea surface temperature Particulate organic matter collected during a 2-year period, as part of an ongoing sediment trap study, and a high-resolution sediment record from 1850 to 1987 A.D. from the Santa Barbara Basin were analyzed for TEX86, a temperature proxy based on marine crenarchaeotal membrane lipids. Highest fluxes of crenarchaeotal lipids in the water column were found in May-June 1996 and from October 1996 to January 1997 and, in general, showed a good correlation with mass fluxes. TEX86 reconstructed temperatures from the sediment trap series ranged from 8 to 11°C and were usually substantially lower than sea surface temperatures (SST), indicating that unlike in previous studies, the TEX86 corresponds to subsurface temperatures, likely between 100 and 150 m. TEX86 temperature variations observed in trap samples were not coupled to changes in SST or deep-water temperatures and only to some degree with crenarchaeotal lipid fluxes. This suggests that a complex combination of different depth origins and seasonal growth periods of Crenarchaeota contributed to the variations in TEX86 signal during the annual cycle. TEX86 temperatures in the two sediment cores studied (8-13°C) were also substantially lower than those of instrumental SST records (14-17.5°C) confirming that TEX86 records a subsurface temperature signal in the Santa Barbara Basin. This result highlights the importance of performing calibration studies using sediment traps and core tops before applying the TEX86 temperature proxy in a given study area. https://ddd.uab.cat/record/25432 https://dx.doi.org/urn:doi:10.1029/2006PA001310
spellingShingle A study of the TEX86 paleothermometer in the water column and sediments of the Santa Barbara Basin, California
Huguet, Carme|||0000-0001-8025-2010
Santa Barbara Basin
Paleoclimatology
Marine organic chemistry
Geochemical tracers
Sea surface temperature
title A study of the TEX86 paleothermometer in the water column and sediments of the Santa Barbara Basin, California
title_full A study of the TEX86 paleothermometer in the water column and sediments of the Santa Barbara Basin, California
title_fullStr A study of the TEX86 paleothermometer in the water column and sediments of the Santa Barbara Basin, California
title_full_unstemmed A study of the TEX86 paleothermometer in the water column and sediments of the Santa Barbara Basin, California
title_short A study of the TEX86 paleothermometer in the water column and sediments of the Santa Barbara Basin, California
title_sort A study of the TEX86 paleothermometer in the water column and sediments of the Santa Barbara Basin, California
topic Santa Barbara Basin
Paleoclimatology
Marine organic chemistry
Geochemical tracers
Sea surface temperature
topic_facet Santa Barbara Basin
Paleoclimatology
Marine organic chemistry
Geochemical tracers
Sea surface temperature
url https://ddd.uab.cat/record/25432
https://dx.doi.org/urn:doi:10.1029/2006PA001310