CN of diatom-bound organic matter in surface sediments ...

Treatment of diatom microfossils from Southern Ocean sediments with hot perchloric acid leaves a "diatom-bound" N fraction which is 0-4 per mil lower in d15N than the bulk sediment, typically 3 per mil lower in recent Antarctic diatom ooze. Results from Southern Ocean surface sediments ind...

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Bibliographic Details
Main Authors: Sigman, Daniel M, Altabet, Mark A, Francois, Roger, McCorkle, Daniel C, Gaillard, Jean-Francois
Format: Dataset
Language:English
Published: PANGAEA 1999
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.856899
https://doi.pangaea.de/10.1594/PANGAEA.856899
id ftdatacite:10.1594/pangaea.856899
record_format openpolar
spelling ftdatacite:10.1594/pangaea.856899 2024-01-28T10:01:24+01:00 CN of diatom-bound organic matter in surface sediments ... Sigman, Daniel M Altabet, Mark A Francois, Roger McCorkle, Daniel C Gaillard, Jean-Francois 1999 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.856899 https://doi.pangaea.de/10.1594/PANGAEA.856899 en eng PANGAEA https://dx.doi.org/10.1029/1998pa900018 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 DEPTH, sediment/rock Depth, top/min Depth, bottom/max Carbon/Nitrogen ratio MultiCorer MD75 NBP9604 Marion Dufresne 1972 Nathaniel B. Palmer dataset Dataset Supplementary Dataset 1999 ftdatacite https://doi.org/10.1594/pangaea.85689910.1029/1998pa900018 2024-01-04T23:54:53Z Treatment of diatom microfossils from Southern Ocean sediments with hot perchloric acid leaves a "diatom-bound" N fraction which is 0-4 per mil lower in d15N than the bulk sediment, typically 3 per mil lower in recent Antarctic diatom ooze. Results from Southern Ocean surface sediments indicate that early diagenetic changes in bulk sediment N content and d15N are not reflected in diatom-bound N, suggesting that diatom-bound N is physically protected from early diagenesis by the microfossil matrix. A meridional transect of multicores from the Indian sector of the Southern Ocean shows a northward increase in the d15N of diatom-bound N, suggesting that diatom-bound d15N, like bulk sedimentary d15N, varies with nitrate utilization in the overlying surface waters. The d15N of diatom-bound N is 3-4 per mil higher in glacial age Antarctic sediments than in Holocene sediments, supporting the hypothesis, previously based on bulk sediment d15N, that nitrate utilization in the surface Antarctic was higher during the ... : Supplement to: Sigman, Daniel M; Altabet, Mark A; Francois, Roger; McCorkle, Daniel C; Gaillard, Jean-Francois (1999): The isotopic composition of diatom-bound nitrogen in Southern Ocean sediments. Paleoceanography, 14(2), 118-134 ... Dataset Antarc* Antarctic Southern Ocean DataCite Metadata Store (German National Library of Science and Technology) Antarctic Indian Southern Ocean
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Event label
Latitude of event
Longitude of event
DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Carbon/Nitrogen ratio
MultiCorer
MD75
NBP9604
Marion Dufresne 1972
Nathaniel B. Palmer
spellingShingle Event label
Latitude of event
Longitude of event
DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Carbon/Nitrogen ratio
MultiCorer
MD75
NBP9604
Marion Dufresne 1972
Nathaniel B. Palmer
Sigman, Daniel M
Altabet, Mark A
Francois, Roger
McCorkle, Daniel C
Gaillard, Jean-Francois
CN of diatom-bound organic matter in surface sediments ...
topic_facet Event label
Latitude of event
Longitude of event
DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Carbon/Nitrogen ratio
MultiCorer
MD75
NBP9604
Marion Dufresne 1972
Nathaniel B. Palmer
description Treatment of diatom microfossils from Southern Ocean sediments with hot perchloric acid leaves a "diatom-bound" N fraction which is 0-4 per mil lower in d15N than the bulk sediment, typically 3 per mil lower in recent Antarctic diatom ooze. Results from Southern Ocean surface sediments indicate that early diagenetic changes in bulk sediment N content and d15N are not reflected in diatom-bound N, suggesting that diatom-bound N is physically protected from early diagenesis by the microfossil matrix. A meridional transect of multicores from the Indian sector of the Southern Ocean shows a northward increase in the d15N of diatom-bound N, suggesting that diatom-bound d15N, like bulk sedimentary d15N, varies with nitrate utilization in the overlying surface waters. The d15N of diatom-bound N is 3-4 per mil higher in glacial age Antarctic sediments than in Holocene sediments, supporting the hypothesis, previously based on bulk sediment d15N, that nitrate utilization in the surface Antarctic was higher during the ... : Supplement to: Sigman, Daniel M; Altabet, Mark A; Francois, Roger; McCorkle, Daniel C; Gaillard, Jean-Francois (1999): The isotopic composition of diatom-bound nitrogen in Southern Ocean sediments. Paleoceanography, 14(2), 118-134 ...
format Dataset
author Sigman, Daniel M
Altabet, Mark A
Francois, Roger
McCorkle, Daniel C
Gaillard, Jean-Francois
author_facet Sigman, Daniel M
Altabet, Mark A
Francois, Roger
McCorkle, Daniel C
Gaillard, Jean-Francois
author_sort Sigman, Daniel M
title CN of diatom-bound organic matter in surface sediments ...
title_short CN of diatom-bound organic matter in surface sediments ...
title_full CN of diatom-bound organic matter in surface sediments ...
title_fullStr CN of diatom-bound organic matter in surface sediments ...
title_full_unstemmed CN of diatom-bound organic matter in surface sediments ...
title_sort cn of diatom-bound organic matter in surface sediments ...
publisher PANGAEA
publishDate 1999
url https://dx.doi.org/10.1594/pangaea.856899
https://doi.pangaea.de/10.1594/PANGAEA.856899
geographic Antarctic
Indian
Southern Ocean
geographic_facet Antarctic
Indian
Southern Ocean
genre Antarc*
Antarctic
Southern Ocean
genre_facet Antarc*
Antarctic
Southern Ocean
op_relation https://dx.doi.org/10.1029/1998pa900018
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.85689910.1029/1998pa900018
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