Alkenone in surface sediments of the Nordic seas and the North Atlantic ...
Alkenone sediment data from the Nordic seas and North Atlantic are compared to those from Sikes et al. (1997) for the Southern Ocean to evaluate further UK37 and UK37' as proxies to estimate cold temperatures (<10°C) and the effect of salinity and temperature in the relative abundance of 37:...
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ftdatacite:10.1594/pangaea.857436 2024-09-09T19:54:05+00:00 Alkenone in surface sediments of the Nordic seas and the North Atlantic ... Rosell-Melé, Antoni 1998 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.857436 https://doi.pangaea.de/10.1594/PANGAEA.857436 en eng PANGAEA https://dx.doi.org/10.1029/98pa02355 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label Latitude of event Longitude of event Elevation of event DEPTH, sediment/rock Alkenone, C374 peak area Alkenone, C373 peak area Alkenone, C372 peak area Alkenone, C374 Giant box corer Bottle, Niskin Piston corer Kiel type Gravity corer Kiel type Kasten corer CTD/Rosette POS119 M7/2 M7/3 M7/4 M7/5 M21/5 Poseidon Meteor 1986 Dataset dataset Supplementary Dataset 1998 ftdatacite https://doi.org/10.1594/pangaea.85743610.1029/98pa02355 2024-07-03T13:11:36Z Alkenone sediment data from the Nordic seas and North Atlantic are compared to those from Sikes et al. (1997) for the Southern Ocean to evaluate further UK37 and UK37' as proxies to estimate cold temperatures (<10°C) and the effect of salinity and temperature in the relative abundance of 37:4 to the total abundance of C37 alkenones (37:4%). UK37 and UK37' are found to be equally viable as proxies, but there are significant regional differences in their cold temperature dependence. The measurement of 37:4% in cores from the North Atlantic region can be used to identify situations when UK37' is not a reliable paleothermometer. Variations in salinity are probably responsible for changes in the sedimentary record of 37:4%, and a preliminary calibration has been obtained for 37:4%=f(salinity). This new relationship should be further confirmed through field or laboratory experiments, but it paves the way to derive a molecular proxy to reconstruct paleosalinity in surface waters. ... : Supplement to: Rosell-Melé, Antoni (1998): Interhemispheric appraisal of the value of alkenone indices as temperature and salinity proxies in high-latitude locations. Paleoceanography, 13(6), 694-703 ... Dataset Nordic Seas North Atlantic Southern Ocean DataCite Southern Ocean |
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Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Event label Latitude of event Longitude of event Elevation of event DEPTH, sediment/rock Alkenone, C374 peak area Alkenone, C373 peak area Alkenone, C372 peak area Alkenone, C374 Giant box corer Bottle, Niskin Piston corer Kiel type Gravity corer Kiel type Kasten corer CTD/Rosette POS119 M7/2 M7/3 M7/4 M7/5 M21/5 Poseidon Meteor 1986 |
spellingShingle |
Event label Latitude of event Longitude of event Elevation of event DEPTH, sediment/rock Alkenone, C374 peak area Alkenone, C373 peak area Alkenone, C372 peak area Alkenone, C374 Giant box corer Bottle, Niskin Piston corer Kiel type Gravity corer Kiel type Kasten corer CTD/Rosette POS119 M7/2 M7/3 M7/4 M7/5 M21/5 Poseidon Meteor 1986 Rosell-Melé, Antoni Alkenone in surface sediments of the Nordic seas and the North Atlantic ... |
topic_facet |
Event label Latitude of event Longitude of event Elevation of event DEPTH, sediment/rock Alkenone, C374 peak area Alkenone, C373 peak area Alkenone, C372 peak area Alkenone, C374 Giant box corer Bottle, Niskin Piston corer Kiel type Gravity corer Kiel type Kasten corer CTD/Rosette POS119 M7/2 M7/3 M7/4 M7/5 M21/5 Poseidon Meteor 1986 |
description |
Alkenone sediment data from the Nordic seas and North Atlantic are compared to those from Sikes et al. (1997) for the Southern Ocean to evaluate further UK37 and UK37' as proxies to estimate cold temperatures (<10°C) and the effect of salinity and temperature in the relative abundance of 37:4 to the total abundance of C37 alkenones (37:4%). UK37 and UK37' are found to be equally viable as proxies, but there are significant regional differences in their cold temperature dependence. The measurement of 37:4% in cores from the North Atlantic region can be used to identify situations when UK37' is not a reliable paleothermometer. Variations in salinity are probably responsible for changes in the sedimentary record of 37:4%, and a preliminary calibration has been obtained for 37:4%=f(salinity). This new relationship should be further confirmed through field or laboratory experiments, but it paves the way to derive a molecular proxy to reconstruct paleosalinity in surface waters. ... : Supplement to: Rosell-Melé, Antoni (1998): Interhemispheric appraisal of the value of alkenone indices as temperature and salinity proxies in high-latitude locations. Paleoceanography, 13(6), 694-703 ... |
format |
Dataset |
author |
Rosell-Melé, Antoni |
author_facet |
Rosell-Melé, Antoni |
author_sort |
Rosell-Melé, Antoni |
title |
Alkenone in surface sediments of the Nordic seas and the North Atlantic ... |
title_short |
Alkenone in surface sediments of the Nordic seas and the North Atlantic ... |
title_full |
Alkenone in surface sediments of the Nordic seas and the North Atlantic ... |
title_fullStr |
Alkenone in surface sediments of the Nordic seas and the North Atlantic ... |
title_full_unstemmed |
Alkenone in surface sediments of the Nordic seas and the North Atlantic ... |
title_sort |
alkenone in surface sediments of the nordic seas and the north atlantic ... |
publisher |
PANGAEA |
publishDate |
1998 |
url |
https://dx.doi.org/10.1594/pangaea.857436 https://doi.pangaea.de/10.1594/PANGAEA.857436 |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
Nordic Seas North Atlantic Southern Ocean |
genre_facet |
Nordic Seas North Atlantic Southern Ocean |
op_relation |
https://dx.doi.org/10.1029/98pa02355 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.85743610.1029/98pa02355 |
_version_ |
1809923517186048000 |