Vertical flux and lithologic material in the Ross Sea ...

As part of the USJGOFS-AESOPS program, we deployed an array of moored sediment traps and determined the composition and vertical flux of particulate matter through the water column of the continental shelf environment of the Ross Sea. We deployed two moorings, with two traps each. One mooring was lo...

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Main Authors: Collier, Robert W, Dymond, Jack R, Honjo, Susumu, Manganini, Steven J, Francois, Roger, Dunbar, Robert G
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2000
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.787551
https://doi.pangaea.de/10.1594/PANGAEA.787551
id ftdatacite:10.1594/pangaea.787551
record_format openpolar
spelling ftdatacite:10.1594/pangaea.787551 2024-09-15T17:41:01+00:00 Vertical flux and lithologic material in the Ross Sea ... Collier, Robert W Dymond, Jack R Honjo, Susumu Manganini, Steven J Francois, Roger Dunbar, Robert G 2000 application/zip https://dx.doi.org/10.1594/pangaea.787551 https://doi.pangaea.de/10.1594/PANGAEA.787551 en eng PANGAEA https://dx.doi.org/10.1016/s0967-0645(00)00076-x Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Antarctic Environments Southern Ocean Process Study AESOPS article Collection Supplementary Publication Series of Datasets 2000 ftdatacite https://doi.org/10.1594/pangaea.78755110.1016/s0967-0645(00)00076-x 2024-08-01T10:51:52Z As part of the USJGOFS-AESOPS program, we deployed an array of moored sediment traps and determined the composition and vertical flux of particulate matter through the water column of the continental shelf environment of the Ross Sea. We deployed two moorings, with two traps each. One mooring was located in the southcentral Ross Sea along the line of AESOPS process studies; the other mooring was located in the northcentral Ross Sea. The flux in the southern Ross Sea was generally double that in the north, and there was a significant increase in flux into the deep traps indicating horizontal transport and possible focusing of particulate matter. The particles are primarily biogenic although lithogenic contributions can increase to over 30% of the flux in the near-bottom trap nearer to the ice shelf. The fluxes collected by the traps were generally low but within the range of previous observations. Several unique observations stand out from these data: (1) The export of organic matter to 200 m during the ... : Supplement to: Collier, Robert W; Dymond, Jack R; Honjo, Susumu; Manganini, Steven J; Francois, Roger; Dunbar, Robert G (2000): The vertical flux of biogenic and lithogenic material in the Ross Sea: moored sediment trap observations 1996-1998. Deep Sea Research Part II: Topical Studies in Oceanography, 47(15-16), 3491-3520 ... Article in Journal/Newspaper Antarc* Antarctic Ice Shelf Ross Sea Southern Ocean DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Antarctic Environments Southern Ocean Process Study AESOPS
spellingShingle Antarctic Environments Southern Ocean Process Study AESOPS
Collier, Robert W
Dymond, Jack R
Honjo, Susumu
Manganini, Steven J
Francois, Roger
Dunbar, Robert G
Vertical flux and lithologic material in the Ross Sea ...
topic_facet Antarctic Environments Southern Ocean Process Study AESOPS
description As part of the USJGOFS-AESOPS program, we deployed an array of moored sediment traps and determined the composition and vertical flux of particulate matter through the water column of the continental shelf environment of the Ross Sea. We deployed two moorings, with two traps each. One mooring was located in the southcentral Ross Sea along the line of AESOPS process studies; the other mooring was located in the northcentral Ross Sea. The flux in the southern Ross Sea was generally double that in the north, and there was a significant increase in flux into the deep traps indicating horizontal transport and possible focusing of particulate matter. The particles are primarily biogenic although lithogenic contributions can increase to over 30% of the flux in the near-bottom trap nearer to the ice shelf. The fluxes collected by the traps were generally low but within the range of previous observations. Several unique observations stand out from these data: (1) The export of organic matter to 200 m during the ... : Supplement to: Collier, Robert W; Dymond, Jack R; Honjo, Susumu; Manganini, Steven J; Francois, Roger; Dunbar, Robert G (2000): The vertical flux of biogenic and lithogenic material in the Ross Sea: moored sediment trap observations 1996-1998. Deep Sea Research Part II: Topical Studies in Oceanography, 47(15-16), 3491-3520 ...
format Article in Journal/Newspaper
author Collier, Robert W
Dymond, Jack R
Honjo, Susumu
Manganini, Steven J
Francois, Roger
Dunbar, Robert G
author_facet Collier, Robert W
Dymond, Jack R
Honjo, Susumu
Manganini, Steven J
Francois, Roger
Dunbar, Robert G
author_sort Collier, Robert W
title Vertical flux and lithologic material in the Ross Sea ...
title_short Vertical flux and lithologic material in the Ross Sea ...
title_full Vertical flux and lithologic material in the Ross Sea ...
title_fullStr Vertical flux and lithologic material in the Ross Sea ...
title_full_unstemmed Vertical flux and lithologic material in the Ross Sea ...
title_sort vertical flux and lithologic material in the ross sea ...
publisher PANGAEA
publishDate 2000
url https://dx.doi.org/10.1594/pangaea.787551
https://doi.pangaea.de/10.1594/PANGAEA.787551
genre Antarc*
Antarctic
Ice Shelf
Ross Sea
Southern Ocean
genre_facet Antarc*
Antarctic
Ice Shelf
Ross Sea
Southern Ocean
op_relation https://dx.doi.org/10.1016/s0967-0645(00)00076-x
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.78755110.1016/s0967-0645(00)00076-x
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