CONTENT OF ORGANIC MATTER IN THE BOTTOM SEDIMENTS OFF LUTZOW-HOLM BAY COLLECTED BY THE 2nd JAPANESE ANTARCTIC RESEARCH EXPEDITION

The samples investigated were collected off Lutzow-Holm Bay in Antarctica by Dr. T. TORII aboard the "SOYA", research ship of the 2nd Japanese Antarctic Research Expedition (1957-58). The summary of the results is as follows (See the appendix). (1) Organic carbon in dry sediments ranges be...

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Main Authors: Yukio SUGIMURA, Kimio NOGUCHI
Format: Article in Journal/Newspaper
Language:English
Japanese
Published: National Institute of Polar Research 1961
Subjects:
Online Access:https://doi.org/10.15094/00007100
https://doaj.org/article/95ca58f320164e78a5341e9cb8c4cd2f
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spelling ftdoajarticles:oai:doaj.org/article:95ca58f320164e78a5341e9cb8c4cd2f 2023-05-15T13:56:48+02:00 CONTENT OF ORGANIC MATTER IN THE BOTTOM SEDIMENTS OFF LUTZOW-HOLM BAY COLLECTED BY THE 2nd JAPANESE ANTARCTIC RESEARCH EXPEDITION Yukio SUGIMURA Kimio NOGUCHI 1961-03-01T00:00:00Z https://doi.org/10.15094/00007100 https://doaj.org/article/95ca58f320164e78a5341e9cb8c4cd2f EN JA eng jpn National Institute of Polar Research https://doi.org/10.15094/00007100 https://doaj.org/toc/0085-7289 https://doaj.org/toc/2432-079X doi:10.15094/00007100 0085-7289 2432-079X https://doaj.org/article/95ca58f320164e78a5341e9cb8c4cd2f Antarctic Record, Iss 12, Pp 1071-1073 (1961) Geography (General) G1-922 article 1961 ftdoajarticles https://doi.org/10.15094/00007100 2022-12-31T15:59:29Z The samples investigated were collected off Lutzow-Holm Bay in Antarctica by Dr. T. TORII aboard the "SOYA", research ship of the 2nd Japanese Antarctic Research Expedition (1957-58). The summary of the results is as follows (See the appendix). (1) Organic carbon in dry sediments ranges between 0.15 and 0.30% and organic nitrogen varies from 0.014 to 0.032%. However, the value of org. N/org.C, 0.05-0.17, does not differ from the corresponding values for bottom sediments from other ocean floors. (2) Chlorophyll derivatives which express an amount of pheophytin equivalent are 4-17 p.p.m. The values are less than the correspending values for the sediments off California, 18-46 p.p.m. (3) Marine humus, as calculated from the value of organic carbon and TRASK'S factor (1.72), varies from 0.3 to 0.5%. The values much differs from the corresponding values for the sediments of the northern Pacific, the southern Pacific and the Atlantic oceans, 1-1.5%, 0.4-1.0% and 0.3-1.5%. (4) Carbonate content shows that the value owes mostly to foraminiferal residues, as CaCO_3 varies from 2 to 11%. The number of the observations so far made is greatly limited. Therefore, the tendencies described above are only approaches to further investigation. Article in Journal/Newspaper Antarc* Antarctic Antarctica Directory of Open Access Journals: DOAJ Articles Antarctic Pacific Torii ENVELOPE(35.667,35.667,-71.317,-71.317)
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
Japanese
topic Geography (General)
G1-922
spellingShingle Geography (General)
G1-922
Yukio SUGIMURA
Kimio NOGUCHI
CONTENT OF ORGANIC MATTER IN THE BOTTOM SEDIMENTS OFF LUTZOW-HOLM BAY COLLECTED BY THE 2nd JAPANESE ANTARCTIC RESEARCH EXPEDITION
topic_facet Geography (General)
G1-922
description The samples investigated were collected off Lutzow-Holm Bay in Antarctica by Dr. T. TORII aboard the "SOYA", research ship of the 2nd Japanese Antarctic Research Expedition (1957-58). The summary of the results is as follows (See the appendix). (1) Organic carbon in dry sediments ranges between 0.15 and 0.30% and organic nitrogen varies from 0.014 to 0.032%. However, the value of org. N/org.C, 0.05-0.17, does not differ from the corresponding values for bottom sediments from other ocean floors. (2) Chlorophyll derivatives which express an amount of pheophytin equivalent are 4-17 p.p.m. The values are less than the correspending values for the sediments off California, 18-46 p.p.m. (3) Marine humus, as calculated from the value of organic carbon and TRASK'S factor (1.72), varies from 0.3 to 0.5%. The values much differs from the corresponding values for the sediments of the northern Pacific, the southern Pacific and the Atlantic oceans, 1-1.5%, 0.4-1.0% and 0.3-1.5%. (4) Carbonate content shows that the value owes mostly to foraminiferal residues, as CaCO_3 varies from 2 to 11%. The number of the observations so far made is greatly limited. Therefore, the tendencies described above are only approaches to further investigation.
format Article in Journal/Newspaper
author Yukio SUGIMURA
Kimio NOGUCHI
author_facet Yukio SUGIMURA
Kimio NOGUCHI
author_sort Yukio SUGIMURA
title CONTENT OF ORGANIC MATTER IN THE BOTTOM SEDIMENTS OFF LUTZOW-HOLM BAY COLLECTED BY THE 2nd JAPANESE ANTARCTIC RESEARCH EXPEDITION
title_short CONTENT OF ORGANIC MATTER IN THE BOTTOM SEDIMENTS OFF LUTZOW-HOLM BAY COLLECTED BY THE 2nd JAPANESE ANTARCTIC RESEARCH EXPEDITION
title_full CONTENT OF ORGANIC MATTER IN THE BOTTOM SEDIMENTS OFF LUTZOW-HOLM BAY COLLECTED BY THE 2nd JAPANESE ANTARCTIC RESEARCH EXPEDITION
title_fullStr CONTENT OF ORGANIC MATTER IN THE BOTTOM SEDIMENTS OFF LUTZOW-HOLM BAY COLLECTED BY THE 2nd JAPANESE ANTARCTIC RESEARCH EXPEDITION
title_full_unstemmed CONTENT OF ORGANIC MATTER IN THE BOTTOM SEDIMENTS OFF LUTZOW-HOLM BAY COLLECTED BY THE 2nd JAPANESE ANTARCTIC RESEARCH EXPEDITION
title_sort content of organic matter in the bottom sediments off lutzow-holm bay collected by the 2nd japanese antarctic research expedition
publisher National Institute of Polar Research
publishDate 1961
url https://doi.org/10.15094/00007100
https://doaj.org/article/95ca58f320164e78a5341e9cb8c4cd2f
long_lat ENVELOPE(35.667,35.667,-71.317,-71.317)
geographic Antarctic
Pacific
Torii
geographic_facet Antarctic
Pacific
Torii
genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
op_source Antarctic Record, Iss 12, Pp 1071-1073 (1961)
op_relation https://doi.org/10.15094/00007100
https://doaj.org/toc/0085-7289
https://doaj.org/toc/2432-079X
doi:10.15094/00007100
0085-7289
2432-079X
https://doaj.org/article/95ca58f320164e78a5341e9cb8c4cd2f
op_doi https://doi.org/10.15094/00007100
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