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Bibliographic Details
Main Author:	Lein, Alla Yu
Format:	Dataset Open Access
Language:	en
Published:	PANGAEA 2004
Subjects:	14C uptake; AMK11A-1392; AMK11A-1395; Archive of Ocean Data; ARCOD; Elevation of event; Event label; Latitude of event; Longitude of event; Methane, oxidation rate, integrated; Methane formation rate, integrated; MULT; Multiple investigations; Sample type
Online Access:	https://doi.org/10.1594/PANGAEA.785877
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(Table 6.2.2) Rates of anaerobic processes in bottom sediments of the Tajura rift, Gulf of Aden
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Concentrations of dissolved and particulate heavy metals in waters above the northwestern slope of the Paramushir Island (Sea of Okhotsk)
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(Table 3.1.12) Daily production and consumption of methane in bottom sediments of the White Sea
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(Table 5b) Rates of microbial processes in bottom waters of the Kara Sea in September 2007
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(Table 48-1) Rate of methane formation in bottom sediments collected by grabs within the Tajura Rift
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(Table 5) Concentration of methane, rates of its formation and oxidation, as well as rates of sulfate reduction and dark CO2 assimilation in the water column of the White Sea
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(Table 48-2) Rate of methane formation in bottom sediments collected by cores within the Tajura Rift
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(Table 5a) Rates of microbial processes in bottom sediments of the Kara Sea in September 2007
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(Table 3.4.6) Formation of methane and hydrogen sulfide and consumption of methane in the 0-100 cm layer of Chukchi Sea bottom sediments per 1 sq. m
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(Table 3) Methane concentration and oxidation rate in the Kara Sea water column in September 2007
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(Table 4.3.5) Integrated formation- and consumption rates of methane in surface layer bottom sediments of the Batabano Bay
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(Table 9.1.2) Abundance of microorganisms and rates of methane oxidation and carbon dioxide assimilation in waters in the area of the Axial Seamount, Juan de Fuca Ridge
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(Table 3.3.11) Formation and oxidation of metane in bottom sediments from Stations DM49-4404-1 and DM49-4397-1 and methane flux from bottom sediments to water
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(Table 10.4.2) Total abundance of bacteria, CO2 assimilation- and methane oxidation rates in water samples collected within the Rainbow hydrothermal field, in the smoke zone above active hydrothermal vents
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(Table 9.2.1) Abundance of microorganisms and rates of methane oxidation and carbon dioxide assimilation in waters of the Guaymas Basin, Gulf of California
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(Table 9.1.4) Rates of biogeochemical processes in Holocene sediments of the Axial Seamount, Juan de Fuca Ridge
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(Table 4.4.6) Formation- and consumption rates of methane in surface sediment layers of the Benguela Upwelling area per 1 sq. m
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(Table 8.2.6) Integral rate of microbial processes for upper 20 cm of bottom sediments from the Gdansk Bay, Baltic Sea
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(Table 8.3.14) Rates of microbial processes in deposits covered by bacterial mats in the caldera of the Haakon Mosby mud volcano, Norwegian Sea
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(Table 10.4.5) Rates of microbial processes in bacterial foulings on rocks of hydrothermal edifices and in hydrothermal sediments from the Rainbow hydrothermal field
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(Table 10.4.3) Chemical composition, bacteria adundance, and rates of microbial processes in samples of hydrothermal fluids collected within the Rainbow hydrothermal field
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(Table 8.2.4a) Concentration of sulfates and methane, total alkalinity, and rates of microbial processes in bottom waters of the Gdansk Bay, Baltic Sea
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(Table 4) Carbon-14 dioxide assimilation rate in vertical water sections above the Broken Spur and TAG hydrothermal fields
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(Table 4.5.6) Rates of microbial formation and consumption of methane in the upper meter of Upper Holocene bottom sediments from the area adjacent to the Congo River mouth
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(Table 8.3.15) Chemical composition and rates of microbial processes in bottom water in caldera of the Haakon Mosby mud volcano, Norwegian Sea
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(Table 8.2.4b) Concentration of sulfates and methane, total alkalinity, and rates of microbial processes in bottom sediments of the Gdansk Bay, Baltic Sea
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(Table 4b) Geochemical parameters of bottom waters from the Kara Sea in September 2007
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(Table 11) Methane oxidation rates per volume and per 1 sq. m of Barents Sea bottom sediments at Station ASV11-829
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(Table 9.4.4) Rates of microbial processes in hot and warm hydrothermal solutions from the 9°50'N EPR hydrothermal field
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(Table 7) Integrated rates of microbiological processes in upper 30 cm of bottom sediments from the area of the Spitsbergen (Svalbard) Archipelago
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(Table 9) Amount and consumption of methane in Upper Holocene bottom sediments of the Barents Sea
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(Table 5.2.1) Rates of methane formation and sulfate reduction in bottom sediments from the Gulf of California and Pacific Ocean
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(Table 2) Bacterial biomass and productivity in the Kara Sea water column in September 2007
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(Table 3) Total biomass of phytoplankton, biomass of diatoms in plankton, and contribution of the most abundant species to the total biomass of phytoplankton at trap stations in the White Sea in August-September 2007 and in June 2008
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(Table 49) Dark assimilation rate of carbon dioxide in bottom sediments from the Gulf of Aden
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(Table 44-1) Cellulose decomposition rate, abundance of cellulose bacteria, cellulose content, and 14C distribution in products of cellulose decomposition in bottom sediments from grabs collected in the Gulf of Aden
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(Table 44-2) Cellulose decomposition rate, abundance of cellulose bacteria, cellulose content, and 14C distribution in products of cellulose decomposition in bottom sediments from cores collected in the Gulf of Aden
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(Table 11-1) Values of dark carbon dioxide assimilation in supra bottom water and surface layer bottom sediments of the Kara Sea along the section from the Ob River mouth to the Saint Anna Trough in September 2007
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(Table 5) Carbon-14 dioxide assimilation rate in bottom sediments from the Broken Spur and TAG hydrothermal fields
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(Table 7a) Azide, sulfide, ammonium chloride and thiosulfate influences on carbon-14 dioxide assimilation rates in water samples from the Broken Spur and TAG hydrothermal fields
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