Composition of organic matter in deep-sea holoturians and host bottom sediments from the Kuril-Kamchatka Trench ...

In 5 holothurian species of the Aspidochirota and Elasipoda orders concentration of organic carbon in alimentary canals due to selective feeding on the average is 7 times higher than in host sediments. Concentration decreases from the first section of the alimentary canal to the last. Intestinal con...

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Main Authors: Bordovsky, Oleg K, Sokolova, Maria N, Smirnov, B A, Akhmet'yeva, E A, Zezina, Olga N
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1974
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.754286
https://doi.pangaea.de/10.1594/PANGAEA.754286
id ftdatacite:10.1594/pangaea.754286
record_format openpolar
spelling ftdatacite:10.1594/pangaea.754286 2024-09-15T18:15:54+00:00 Composition of organic matter in deep-sea holoturians and host bottom sediments from the Kuril-Kamchatka Trench ... Bordovsky, Oleg K Sokolova, Maria N Smirnov, B A Akhmet'yeva, E A Zezina, Olga N 1974 application/zip https://dx.doi.org/10.1594/pangaea.754286 https://doi.pangaea.de/10.1594/PANGAEA.754286 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Grab VITYAZ Vityaz ex-Mars Archive of Ocean Data ARCOD article Collection Supplementary Publication Series of Datasets 1974 ftdatacite https://doi.org/10.1594/pangaea.754286 2024-08-01T10:54:44Z In 5 holothurian species of the Aspidochirota and Elasipoda orders concentration of organic carbon in alimentary canals due to selective feeding on the average is 7 times higher than in host sediments. Concentration decreases from the first section of the alimentary canal to the last. Intestinal contents are enriched with bitumens, in which amount of oils and resins increases, while that of asphaltenes slightly decreases from the first section to the last. It is conjectured from analysis of structure and group composition of oil fraction of bitumens that heteroatomic and specifically oxygen-containing rather than purely hydrocarbon compounds have food value. Organic matter in intestines contains 6 to 9 kcal/g. Judging by changes in chemical composition of contents, only a few of these calories are utilized. Hence to assure themselves of energy they need, organisms must continuously pass sedimentary material through their alimentary canals. ... : Supplement to: Bordovsky, Oleg K; Sokolova, Maria N; Smirnov, B A; Akhmet'yeva, E A; Zezina, Olga N (1974): Evaluation of the role of bottom fauna in the transformation of organic matter in sediments (with specific reference to the deep-sea detritus-feeders in the Kuril-Kamchatka Trench). Oceanology, 14, 128-132 ... Article in Journal/Newspaper Kamchatka DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Grab
VITYAZ
Vityaz ex-Mars
Archive of Ocean Data ARCOD
spellingShingle Grab
VITYAZ
Vityaz ex-Mars
Archive of Ocean Data ARCOD
Bordovsky, Oleg K
Sokolova, Maria N
Smirnov, B A
Akhmet'yeva, E A
Zezina, Olga N
Composition of organic matter in deep-sea holoturians and host bottom sediments from the Kuril-Kamchatka Trench ...
topic_facet Grab
VITYAZ
Vityaz ex-Mars
Archive of Ocean Data ARCOD
description In 5 holothurian species of the Aspidochirota and Elasipoda orders concentration of organic carbon in alimentary canals due to selective feeding on the average is 7 times higher than in host sediments. Concentration decreases from the first section of the alimentary canal to the last. Intestinal contents are enriched with bitumens, in which amount of oils and resins increases, while that of asphaltenes slightly decreases from the first section to the last. It is conjectured from analysis of structure and group composition of oil fraction of bitumens that heteroatomic and specifically oxygen-containing rather than purely hydrocarbon compounds have food value. Organic matter in intestines contains 6 to 9 kcal/g. Judging by changes in chemical composition of contents, only a few of these calories are utilized. Hence to assure themselves of energy they need, organisms must continuously pass sedimentary material through their alimentary canals. ... : Supplement to: Bordovsky, Oleg K; Sokolova, Maria N; Smirnov, B A; Akhmet'yeva, E A; Zezina, Olga N (1974): Evaluation of the role of bottom fauna in the transformation of organic matter in sediments (with specific reference to the deep-sea detritus-feeders in the Kuril-Kamchatka Trench). Oceanology, 14, 128-132 ...
format Article in Journal/Newspaper
author Bordovsky, Oleg K
Sokolova, Maria N
Smirnov, B A
Akhmet'yeva, E A
Zezina, Olga N
author_facet Bordovsky, Oleg K
Sokolova, Maria N
Smirnov, B A
Akhmet'yeva, E A
Zezina, Olga N
author_sort Bordovsky, Oleg K
title Composition of organic matter in deep-sea holoturians and host bottom sediments from the Kuril-Kamchatka Trench ...
title_short Composition of organic matter in deep-sea holoturians and host bottom sediments from the Kuril-Kamchatka Trench ...
title_full Composition of organic matter in deep-sea holoturians and host bottom sediments from the Kuril-Kamchatka Trench ...
title_fullStr Composition of organic matter in deep-sea holoturians and host bottom sediments from the Kuril-Kamchatka Trench ...
title_full_unstemmed Composition of organic matter in deep-sea holoturians and host bottom sediments from the Kuril-Kamchatka Trench ...
title_sort composition of organic matter in deep-sea holoturians and host bottom sediments from the kuril-kamchatka trench ...
publisher PANGAEA
publishDate 1974
url https://dx.doi.org/10.1594/pangaea.754286
https://doi.pangaea.de/10.1594/PANGAEA.754286
genre Kamchatka
genre_facet Kamchatka
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.754286
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