Products of the early diagenesis of sediments as a source of energy in the food chain of the Gonchocoele bottom community (Bivalvia) near gas-hydrate seeps off Paramushir Island, Sea of Okhotsk.
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dc.contributor.author | Strizhov, Valentin P | |
dc.contributor.author | Kuznetsov, Alexey P | |
dc.contributor.author | Gurina, N V | |
dc.coverage.spatial | LATITUDE: 50.515000 * LONGITUDE: 155.301667 * MINIMUM DEPTH, sediment/rock: 0.025 m * MAXIMUM DEPTH, sediment/rock: 1.850 m | |
dc.date.accessioned | 2019-11-23T11:53:58Z | |
dc.date.available | 2019-11-23T11:53:58Z | |
dc.date.issued | 1990-04-04 | |
dc.identifier | https://doi.pangaea.de/10.1594/PANGAEA.758912 | |
dc.identifier | https://doi.org/10.1594/PANGAEA.758912 | |
dc.identifier.citation | Strizhov, Valentin P; Kuznetsov, Alexey P; Gurina, N V (1990): Products of the early diagenesis of sediments as a source of energy in the food chain of the Gonchocoele bottom community (Bivalvia) near gas-hydrate seeps off Paramushir Island, Sea of Okhotsk. Oceanology, 30(4), 490-494 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/7352 | |
dc.description.abstract | Isotopic analysis of organic matter from bottom sediments and soft tissues of bivalve Conchocoele from a community near the gas-hydrate seep off the Paramushir Island indicates that the intramolecular energy of energy-rich compounds H2S and methane, which are products of early diagenesis, is used for chemical synthesis by free-living symbiotic sulfur-oxidizing, sulfur reducing, and methane-oxidizing bacteria in the community. | |
dc.format | text/tab-separated-values, 56 data points | |
dc.language.iso | en | |
dc.publisher | PANGAEA | |
dc.rights | CC-BY-3.0: Creative Commons Attribution 3.0 Unported | |
dc.rights | Access constraints: unrestricted | |
dc.source | Supplement to: Strizhov, Valentin P; Kuznetsov, Alexey P; Gurina, N V (1990): Products of the early diagenesis of sediments as a source of energy in the food chain of the Gonchocoele bottom community (Bivalvia) near gas-hydrate seeps off Paramushir Island, Sea of Okhotsk. Oceanology, 30(4), 490-494 | |
dc.subject | AMK11A-1391 | |
dc.subject | Archive of Ocean Data | |
dc.subject | ARCOD | |
dc.subject | DEPTH, sediment/rock | |
dc.subject | Mass spectrometry | |
dc.subject | MULT | |
dc.subject | Sulfur bound in sulfate | |
dc.subject | Sulfur of pyrite | |
dc.subject | Wet chemistry | |
dc.subject | δ13C, organic carbon | |
dc.subject | δ34S, FeS2 | |
dc.subject | δ34S, sulfate | |
dc.title | Products of the early diagenesis of sediments as a source of energy in the food chain of the Gonchocoele bottom community (Bivalvia) near gas-hydrate seeps off Paramushir Island, Sea of Okhotsk. | |
dc.title.alternative | (Table 2) Concentrations and isotopic compositions of pyrite and sulfate sulfur in argillaceous sediments outside the gas hydrate seep zone, Sea of Okhotsk | |
dc.type | Dataset |
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