Aeolian transport and deposition of plant wax n-alkanes across the tropical North Atlantic Ocean ...

Long chain n-alkanes are terrestrial higher plant biomarkers used to reconstruct continental paleoclimatic and paleohydrological conditions with marine sedimentary archives. Latitudinal variation in their concentration and distribution in marine sediments relatively close to the continent has been w...

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Main Authors: Schreuder, Laura T, Stuut, Jan-Berend W, Korte, Laura F, Sinninghe Damsté, Jaap S, Schouten, Stefan
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2017
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.882501
https://doi.pangaea.de/10.1594/PANGAEA.882501
id ftdatacite:10.1594/pangaea.882501
record_format openpolar
spelling ftdatacite:10.1594/pangaea.882501 2024-09-15T18:21:33+00:00 Aeolian transport and deposition of plant wax n-alkanes across the tropical North Atlantic Ocean ... Schreuder, Laura T Stuut, Jan-Berend W Korte, Laura F Sinninghe Damsté, Jaap S Schouten, Stefan 2017 application/zip https://dx.doi.org/10.1594/pangaea.882501 https://doi.pangaea.de/10.1594/PANGAEA.882501 en eng PANGAEA https://dx.doi.org/10.1016/j.orggeochem.2017.10.010 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University NIOZ_UU article Collection Supplementary Publication Series of Datasets 2017 ftdatacite https://doi.org/10.1594/pangaea.88250110.1016/j.orggeochem.2017.10.010 2024-08-01T10:53:02Z Long chain n-alkanes are terrestrial higher plant biomarkers used to reconstruct continental paleoclimatic and paleohydrological conditions with marine sedimentary archives. Latitudinal variation in their concentration and distribution in marine sediments relatively close to the continent has been widely studied, but little is known on how far this continental signal extends into the ocean. Furthermore, no studies have examined the seasonal variation in the deposition of these biomarkers in marine sediments. Here we studied longitudinal variation in the composition of long chain n-alkanes and two other terrestrial higher plant biomarkers (long chain n-alkanols and long chain fatty acids) in atmospheric particles, as well as longitudinal and seasonal variation in long chain n-alkanes in sinking particles in the ocean at different water depths and in surface sediments, all collected along a 12°N transect across the tropical North Atlantic Ocean. The highest abundance of all three biomarker classes was closest ... : Supplement to: Schreuder, Laura T; Stuut, Jan-Berend W; Korte, Laura F; Sinninghe Damsté, Jaap S; Schouten, Stefan (2018): Aeolian transport and deposition of plant wax n -alkanes across the tropical North Atlantic Ocean. Organic Geochemistry, 115, 113-123 ... Article in Journal/Newspaper North Atlantic DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University NIOZ_UU
spellingShingle NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University NIOZ_UU
Schreuder, Laura T
Stuut, Jan-Berend W
Korte, Laura F
Sinninghe Damsté, Jaap S
Schouten, Stefan
Aeolian transport and deposition of plant wax n-alkanes across the tropical North Atlantic Ocean ...
topic_facet NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University NIOZ_UU
description Long chain n-alkanes are terrestrial higher plant biomarkers used to reconstruct continental paleoclimatic and paleohydrological conditions with marine sedimentary archives. Latitudinal variation in their concentration and distribution in marine sediments relatively close to the continent has been widely studied, but little is known on how far this continental signal extends into the ocean. Furthermore, no studies have examined the seasonal variation in the deposition of these biomarkers in marine sediments. Here we studied longitudinal variation in the composition of long chain n-alkanes and two other terrestrial higher plant biomarkers (long chain n-alkanols and long chain fatty acids) in atmospheric particles, as well as longitudinal and seasonal variation in long chain n-alkanes in sinking particles in the ocean at different water depths and in surface sediments, all collected along a 12°N transect across the tropical North Atlantic Ocean. The highest abundance of all three biomarker classes was closest ... : Supplement to: Schreuder, Laura T; Stuut, Jan-Berend W; Korte, Laura F; Sinninghe Damsté, Jaap S; Schouten, Stefan (2018): Aeolian transport and deposition of plant wax n -alkanes across the tropical North Atlantic Ocean. Organic Geochemistry, 115, 113-123 ...
format Article in Journal/Newspaper
author Schreuder, Laura T
Stuut, Jan-Berend W
Korte, Laura F
Sinninghe Damsté, Jaap S
Schouten, Stefan
author_facet Schreuder, Laura T
Stuut, Jan-Berend W
Korte, Laura F
Sinninghe Damsté, Jaap S
Schouten, Stefan
author_sort Schreuder, Laura T
title Aeolian transport and deposition of plant wax n-alkanes across the tropical North Atlantic Ocean ...
title_short Aeolian transport and deposition of plant wax n-alkanes across the tropical North Atlantic Ocean ...
title_full Aeolian transport and deposition of plant wax n-alkanes across the tropical North Atlantic Ocean ...
title_fullStr Aeolian transport and deposition of plant wax n-alkanes across the tropical North Atlantic Ocean ...
title_full_unstemmed Aeolian transport and deposition of plant wax n-alkanes across the tropical North Atlantic Ocean ...
title_sort aeolian transport and deposition of plant wax n-alkanes across the tropical north atlantic ocean ...
publisher PANGAEA
publishDate 2017
url https://dx.doi.org/10.1594/pangaea.882501
https://doi.pangaea.de/10.1594/PANGAEA.882501
genre North Atlantic
genre_facet North Atlantic
op_relation https://dx.doi.org/10.1016/j.orggeochem.2017.10.010
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.88250110.1016/j.orggeochem.2017.10.010
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