R/V Professor Bogorov Cruise report: Cruise 37 POSETIV - Paramushir-Okhotsk Sea Expedition to Investigate Venting, Vladivostok - Vladivostok, September 23 - October 22, 1994

Since the discovery of fluid venting in the late seventies the processes involved in the marine geochemical cycle, especially those of fluid and gas flux through the sediment-water interface have become a new and exciting area of interest and research. Today numerous vent fields have been discovered...

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Other Authors: Gaedicke, Christoph, Baranov, Boris, Lelikov, Evgeniy
Format: Report
Language:English
Published: GEOMAR Forschungszentrum für marine Geowissenschaften 1995
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/23580/
https://oceanrep.geomar.de/id/eprint/23580/1/GEOMAR%20Report%2042.pdf
https://doi.org/10.3289/GEOMAR_REP_42_1995
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spelling ftoceanrep:oai:oceanrep.geomar.de:23580 2023-05-15T17:52:42+02:00 R/V Professor Bogorov Cruise report: Cruise 37 POSETIV - Paramushir-Okhotsk Sea Expedition to Investigate Venting, Vladivostok - Vladivostok, September 23 - October 22, 1994 Gaedicke, Christoph Baranov, Boris Lelikov, Evgeniy 1995 text https://oceanrep.geomar.de/id/eprint/23580/ https://oceanrep.geomar.de/id/eprint/23580/1/GEOMAR%20Report%2042.pdf https://doi.org/10.3289/GEOMAR_REP_42_1995 en eng GEOMAR Forschungszentrum für marine Geowissenschaften https://oceanrep.geomar.de/id/eprint/23580/1/GEOMAR%20Report%2042.pdf Gaedicke, C., Baranov, B. and Lelikov, E., eds. (1995) R/V Professor Bogorov Cruise report: Cruise 37 POSETIV - Paramushir-Okhotsk Sea Expedition to Investigate Venting, Vladivostok - Vladivostok, September 23 - October 22, 1994. Open Access . GEOMAR-Report, 042 . GEOMAR Forschungszentrum für marine Geowissenschaften, Kiel, 94 pp. DOI 10.3289/GEOMAR_REP_42_1995 <https://doi.org/10.3289/GEOMAR_REP_42_1995>. doi:10.3289/GEOMAR_REP_42_1995 cc_by info:eu-repo/semantics/openAccess Report NonPeerReviewed 1995 ftoceanrep https://doi.org/10.3289/GEOMAR_REP_42_1995 2023-04-07T15:12:24Z Since the discovery of fluid venting in the late seventies the processes involved in the marine geochemical cycle, especially those of fluid and gas flux through the sediment-water interface have become a new and exciting area of interest and research. Today numerous vent fields have been discovered and described. Special benthic communities which include molluscs with bacterial symbiotes and polychaete worms are related to fluid discharge onto the sea-floor. The main scientific objectives have been to qualify and quantify the amount of water and gas discharge at the sea-floor in order to estimate the role of these sources to the global biogeochemical cycle of elements. Thus the mapping of vent fields and the description of related geological structures such as the bottom-simulating reflector (BSR) were among the first steps of investigation. The BSR is a acoustically detectable horizon in the sedimentary column. Above this horizon gas hydrates of methane (and sometimes higher order hydrocarbons) and water occur in varying amounts in an ice like condition. The depth of the BSR below the sea-floor depends on physico-chemical parameters such as temperature and pressure, as well as the chemical composition of the fluids. The BSR occurs widely in the area of investigation. To evaluate fully the nature and origin of vent phenomena, thought to be related to tectonic processes in the forearc and backarc region of island arcs, multidisciplinary research is necessary. From September 23 to October 22, 1994 a joint expedition with scientists from the Pacific Oceanological Institute (POI), Vladivostok/Russia, the Shirshov Institute of Oceanology, Moscow/ Russia, the Institute for Marine Geology and Geophysics (IMG&G), Yuzhno-Sakhalinsk/Russia, the Research Centre for Marine Geoscience (GEOMAR), Kiel/Germany and the Netherlands Institute for Marine Research (NIOZ), Texel/The Netherlands was carried out on board the Research Vessel Professor Bogorov during her 37th cruise. The Expedition was the principle part of the ... Report okhotsk sea OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Okhotsk Pacific
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description Since the discovery of fluid venting in the late seventies the processes involved in the marine geochemical cycle, especially those of fluid and gas flux through the sediment-water interface have become a new and exciting area of interest and research. Today numerous vent fields have been discovered and described. Special benthic communities which include molluscs with bacterial symbiotes and polychaete worms are related to fluid discharge onto the sea-floor. The main scientific objectives have been to qualify and quantify the amount of water and gas discharge at the sea-floor in order to estimate the role of these sources to the global biogeochemical cycle of elements. Thus the mapping of vent fields and the description of related geological structures such as the bottom-simulating reflector (BSR) were among the first steps of investigation. The BSR is a acoustically detectable horizon in the sedimentary column. Above this horizon gas hydrates of methane (and sometimes higher order hydrocarbons) and water occur in varying amounts in an ice like condition. The depth of the BSR below the sea-floor depends on physico-chemical parameters such as temperature and pressure, as well as the chemical composition of the fluids. The BSR occurs widely in the area of investigation. To evaluate fully the nature and origin of vent phenomena, thought to be related to tectonic processes in the forearc and backarc region of island arcs, multidisciplinary research is necessary. From September 23 to October 22, 1994 a joint expedition with scientists from the Pacific Oceanological Institute (POI), Vladivostok/Russia, the Shirshov Institute of Oceanology, Moscow/ Russia, the Institute for Marine Geology and Geophysics (IMG&G), Yuzhno-Sakhalinsk/Russia, the Research Centre for Marine Geoscience (GEOMAR), Kiel/Germany and the Netherlands Institute for Marine Research (NIOZ), Texel/The Netherlands was carried out on board the Research Vessel Professor Bogorov during her 37th cruise. The Expedition was the principle part of the ...
author2 Gaedicke, Christoph
Baranov, Boris
Lelikov, Evgeniy
format Report
title R/V Professor Bogorov Cruise report: Cruise 37 POSETIV - Paramushir-Okhotsk Sea Expedition to Investigate Venting, Vladivostok - Vladivostok, September 23 - October 22, 1994
spellingShingle R/V Professor Bogorov Cruise report: Cruise 37 POSETIV - Paramushir-Okhotsk Sea Expedition to Investigate Venting, Vladivostok - Vladivostok, September 23 - October 22, 1994
title_short R/V Professor Bogorov Cruise report: Cruise 37 POSETIV - Paramushir-Okhotsk Sea Expedition to Investigate Venting, Vladivostok - Vladivostok, September 23 - October 22, 1994
title_full R/V Professor Bogorov Cruise report: Cruise 37 POSETIV - Paramushir-Okhotsk Sea Expedition to Investigate Venting, Vladivostok - Vladivostok, September 23 - October 22, 1994
title_fullStr R/V Professor Bogorov Cruise report: Cruise 37 POSETIV - Paramushir-Okhotsk Sea Expedition to Investigate Venting, Vladivostok - Vladivostok, September 23 - October 22, 1994
title_full_unstemmed R/V Professor Bogorov Cruise report: Cruise 37 POSETIV - Paramushir-Okhotsk Sea Expedition to Investigate Venting, Vladivostok - Vladivostok, September 23 - October 22, 1994
title_sort r/v professor bogorov cruise report: cruise 37 posetiv - paramushir-okhotsk sea expedition to investigate venting, vladivostok - vladivostok, september 23 - october 22, 1994
publisher GEOMAR Forschungszentrum für marine Geowissenschaften
publishDate 1995
url https://oceanrep.geomar.de/id/eprint/23580/
https://oceanrep.geomar.de/id/eprint/23580/1/GEOMAR%20Report%2042.pdf
https://doi.org/10.3289/GEOMAR_REP_42_1995
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Gaedicke, C., Baranov, B. and Lelikov, E., eds. (1995) R/V Professor Bogorov Cruise report: Cruise 37 POSETIV - Paramushir-Okhotsk Sea Expedition to Investigate Venting, Vladivostok - Vladivostok, September 23 - October 22, 1994. Open Access . GEOMAR-Report, 042 . GEOMAR Forschungszentrum für marine Geowissenschaften, Kiel, 94 pp. DOI 10.3289/GEOMAR_REP_42_1995 <https://doi.org/10.3289/GEOMAR_REP_42_1995>.
doi:10.3289/GEOMAR_REP_42_1995
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op_doi https://doi.org/10.3289/GEOMAR_REP_42_1995
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