Organic Carbon and Carbonate System in the Bottom Sediments of Shallow Bights of the Peter the Great Bay (Sea of Japan)
Abstract—The diagenesis of organic matter (OM) is studied in bottom sediments taken in February, 2018 from therapeutic mud deposits of the Uglovoi Bay and Voevoda and Ekspeditsiya bights (Peter the Great Bay, Sea of Japan). The carbonate system of bottom sediments and pore water were analyzed for th...
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| Autor*in: |
Tishchenko, P. Ya. [verfasserIn] |
|---|
| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2020 |
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| Anmerkung: |
© Pleiades Publishing, Ltd. 2020 |
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| Übergeordnetes Werk: |
Enthalten in: Geochemistry international - Pleiades Publishing, 1964, 58(2020), 6 vom: Juni, Seite 704-718 |
|---|---|
| Übergeordnetes Werk: |
volume:58 ; year:2020 ; number:6 ; month:06 ; pages:704-718 |
| Links: |
|---|
| DOI / URN: |
10.1134/S0016702920050109 |
|---|
| Katalog-ID: |
OLC2062989180 |
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| 520 | |a Abstract—The diagenesis of organic matter (OM) is studied in bottom sediments taken in February, 2018 from therapeutic mud deposits of the Uglovoi Bay and Voevoda and Ekspeditsiya bights (Peter the Great Bay, Sea of Japan). The carbonate system of bottom sediments and pore water were analyzed for the contents of nutrients, dissolved organic carbon, humic substance, and concentrations of sulfates and chlorides. The concentrations of organic carbon, chlorophyll-a, humic and fulvic acids, and mobile sulfide species are measured in a solid phase of sediment. Underwater photographing shows that sampling localities are covered by Zostera marina meadows in the Voevoda and Ekspeditsiya bights and by diatom mats in Uglovoi Bay. The proportions between dissolved inorganic carbon and alkalinity, as well as data on sulfate–chlorine ratios and mobile sulfide species indicate that the OM degradation in bottom sediments is mainly controlled by sulfate reduction. The Uglovoi Bay and Voevoda and Ekspeditsii bights are characterized by different values of bioturbation coefficients: 3.0, 107.6, and 14.5 $ cm^{2} $/day, respectively. The estimated fluxes of organic carbon from water into sediment and of dissolved inorganic carbon from sediment into water significantly differ. The disbalance between organic and inorganic carbons can be caused by the following reasons: (a) ignored $ CO_{2} $ flux released by marine organisms from bottom sediments through their siphonal system; (b) partial OM consumption in food with its subsequent deposition in it. | ||
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| 700 | 1 | |a Sagalaev, S. G. |4 aut | |
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| 700 | 1 | |a Tibenko, E. Yu. |4 aut | |
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10.1134/S0016702920050109 doi (DE-627)OLC2062989180 (DE-He213)S0016702920050109-p DE-627 ger DE-627 rakwb eng 550 VZ Tishchenko, P. Ya. verfasserin aut Organic Carbon and Carbonate System in the Bottom Sediments of Shallow Bights of the Peter the Great Bay (Sea of Japan) 2020 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2020 Abstract—The diagenesis of organic matter (OM) is studied in bottom sediments taken in February, 2018 from therapeutic mud deposits of the Uglovoi Bay and Voevoda and Ekspeditsiya bights (Peter the Great Bay, Sea of Japan). The carbonate system of bottom sediments and pore water were analyzed for the contents of nutrients, dissolved organic carbon, humic substance, and concentrations of sulfates and chlorides. The concentrations of organic carbon, chlorophyll-a, humic and fulvic acids, and mobile sulfide species are measured in a solid phase of sediment. Underwater photographing shows that sampling localities are covered by Zostera marina meadows in the Voevoda and Ekspeditsiya bights and by diatom mats in Uglovoi Bay. The proportions between dissolved inorganic carbon and alkalinity, as well as data on sulfate–chlorine ratios and mobile sulfide species indicate that the OM degradation in bottom sediments is mainly controlled by sulfate reduction. The Uglovoi Bay and Voevoda and Ekspeditsii bights are characterized by different values of bioturbation coefficients: 3.0, 107.6, and 14.5 $ cm^{2} $/day, respectively. The estimated fluxes of organic carbon from water into sediment and of dissolved inorganic carbon from sediment into water significantly differ. The disbalance between organic and inorganic carbons can be caused by the following reasons: (a) ignored $ CO_{2} $ flux released by marine organisms from bottom sediments through their siphonal system; (b) partial OM consumption in food with its subsequent deposition in it. Medvedev, E. V. aut Barabanshchikov, Yu. A. aut Pavlova, G. Yu. aut Sagalaev, S. G. aut Tishchenko, P. P. aut Shvetsova, M. G. aut Shkirnikova, E. M. aut Ulanova, O. A. aut Tibenko, E. Yu. aut Orekhova, N. A. aut Enthalten in Geochemistry international Pleiades Publishing, 1964 58(2020), 6 vom: Juni, Seite 704-718 (DE-627)12960321X (DE-600)241677-3 (DE-576)01509703X 0016-7029 nnns volume:58 year:2020 number:6 month:06 pages:704-718 https://doi.org/10.1134/S0016702920050109 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO AR 58 2020 6 06 704-718 |
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10.1134/S0016702920050109 doi (DE-627)OLC2062989180 (DE-He213)S0016702920050109-p DE-627 ger DE-627 rakwb eng 550 VZ Tishchenko, P. Ya. verfasserin aut Organic Carbon and Carbonate System in the Bottom Sediments of Shallow Bights of the Peter the Great Bay (Sea of Japan) 2020 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2020 Abstract—The diagenesis of organic matter (OM) is studied in bottom sediments taken in February, 2018 from therapeutic mud deposits of the Uglovoi Bay and Voevoda and Ekspeditsiya bights (Peter the Great Bay, Sea of Japan). The carbonate system of bottom sediments and pore water were analyzed for the contents of nutrients, dissolved organic carbon, humic substance, and concentrations of sulfates and chlorides. The concentrations of organic carbon, chlorophyll-a, humic and fulvic acids, and mobile sulfide species are measured in a solid phase of sediment. Underwater photographing shows that sampling localities are covered by Zostera marina meadows in the Voevoda and Ekspeditsiya bights and by diatom mats in Uglovoi Bay. The proportions between dissolved inorganic carbon and alkalinity, as well as data on sulfate–chlorine ratios and mobile sulfide species indicate that the OM degradation in bottom sediments is mainly controlled by sulfate reduction. The Uglovoi Bay and Voevoda and Ekspeditsii bights are characterized by different values of bioturbation coefficients: 3.0, 107.6, and 14.5 $ cm^{2} $/day, respectively. The estimated fluxes of organic carbon from water into sediment and of dissolved inorganic carbon from sediment into water significantly differ. The disbalance between organic and inorganic carbons can be caused by the following reasons: (a) ignored $ CO_{2} $ flux released by marine organisms from bottom sediments through their siphonal system; (b) partial OM consumption in food with its subsequent deposition in it. Medvedev, E. V. aut Barabanshchikov, Yu. A. aut Pavlova, G. Yu. aut Sagalaev, S. G. aut Tishchenko, P. P. aut Shvetsova, M. G. aut Shkirnikova, E. M. aut Ulanova, O. A. aut Tibenko, E. Yu. aut Orekhova, N. A. aut Enthalten in Geochemistry international Pleiades Publishing, 1964 58(2020), 6 vom: Juni, Seite 704-718 (DE-627)12960321X (DE-600)241677-3 (DE-576)01509703X 0016-7029 nnns volume:58 year:2020 number:6 month:06 pages:704-718 https://doi.org/10.1134/S0016702920050109 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO AR 58 2020 6 06 704-718 |
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10.1134/S0016702920050109 doi (DE-627)OLC2062989180 (DE-He213)S0016702920050109-p DE-627 ger DE-627 rakwb eng 550 VZ Tishchenko, P. Ya. verfasserin aut Organic Carbon and Carbonate System in the Bottom Sediments of Shallow Bights of the Peter the Great Bay (Sea of Japan) 2020 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2020 Abstract—The diagenesis of organic matter (OM) is studied in bottom sediments taken in February, 2018 from therapeutic mud deposits of the Uglovoi Bay and Voevoda and Ekspeditsiya bights (Peter the Great Bay, Sea of Japan). The carbonate system of bottom sediments and pore water were analyzed for the contents of nutrients, dissolved organic carbon, humic substance, and concentrations of sulfates and chlorides. The concentrations of organic carbon, chlorophyll-a, humic and fulvic acids, and mobile sulfide species are measured in a solid phase of sediment. Underwater photographing shows that sampling localities are covered by Zostera marina meadows in the Voevoda and Ekspeditsiya bights and by diatom mats in Uglovoi Bay. The proportions between dissolved inorganic carbon and alkalinity, as well as data on sulfate–chlorine ratios and mobile sulfide species indicate that the OM degradation in bottom sediments is mainly controlled by sulfate reduction. The Uglovoi Bay and Voevoda and Ekspeditsii bights are characterized by different values of bioturbation coefficients: 3.0, 107.6, and 14.5 $ cm^{2} $/day, respectively. The estimated fluxes of organic carbon from water into sediment and of dissolved inorganic carbon from sediment into water significantly differ. The disbalance between organic and inorganic carbons can be caused by the following reasons: (a) ignored $ CO_{2} $ flux released by marine organisms from bottom sediments through their siphonal system; (b) partial OM consumption in food with its subsequent deposition in it. Medvedev, E. V. aut Barabanshchikov, Yu. A. aut Pavlova, G. Yu. aut Sagalaev, S. G. aut Tishchenko, P. P. aut Shvetsova, M. G. aut Shkirnikova, E. M. aut Ulanova, O. A. aut Tibenko, E. Yu. aut Orekhova, N. A. aut Enthalten in Geochemistry international Pleiades Publishing, 1964 58(2020), 6 vom: Juni, Seite 704-718 (DE-627)12960321X (DE-600)241677-3 (DE-576)01509703X 0016-7029 nnns volume:58 year:2020 number:6 month:06 pages:704-718 https://doi.org/10.1134/S0016702920050109 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO AR 58 2020 6 06 704-718 |
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10.1134/S0016702920050109 doi (DE-627)OLC2062989180 (DE-He213)S0016702920050109-p DE-627 ger DE-627 rakwb eng 550 VZ Tishchenko, P. Ya. verfasserin aut Organic Carbon and Carbonate System in the Bottom Sediments of Shallow Bights of the Peter the Great Bay (Sea of Japan) 2020 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2020 Abstract—The diagenesis of organic matter (OM) is studied in bottom sediments taken in February, 2018 from therapeutic mud deposits of the Uglovoi Bay and Voevoda and Ekspeditsiya bights (Peter the Great Bay, Sea of Japan). The carbonate system of bottom sediments and pore water were analyzed for the contents of nutrients, dissolved organic carbon, humic substance, and concentrations of sulfates and chlorides. The concentrations of organic carbon, chlorophyll-a, humic and fulvic acids, and mobile sulfide species are measured in a solid phase of sediment. Underwater photographing shows that sampling localities are covered by Zostera marina meadows in the Voevoda and Ekspeditsiya bights and by diatom mats in Uglovoi Bay. The proportions between dissolved inorganic carbon and alkalinity, as well as data on sulfate–chlorine ratios and mobile sulfide species indicate that the OM degradation in bottom sediments is mainly controlled by sulfate reduction. The Uglovoi Bay and Voevoda and Ekspeditsii bights are characterized by different values of bioturbation coefficients: 3.0, 107.6, and 14.5 $ cm^{2} $/day, respectively. The estimated fluxes of organic carbon from water into sediment and of dissolved inorganic carbon from sediment into water significantly differ. The disbalance between organic and inorganic carbons can be caused by the following reasons: (a) ignored $ CO_{2} $ flux released by marine organisms from bottom sediments through their siphonal system; (b) partial OM consumption in food with its subsequent deposition in it. Medvedev, E. V. aut Barabanshchikov, Yu. A. aut Pavlova, G. Yu. aut Sagalaev, S. G. aut Tishchenko, P. P. aut Shvetsova, M. G. aut Shkirnikova, E. M. aut Ulanova, O. A. aut Tibenko, E. Yu. aut Orekhova, N. A. aut Enthalten in Geochemistry international Pleiades Publishing, 1964 58(2020), 6 vom: Juni, Seite 704-718 (DE-627)12960321X (DE-600)241677-3 (DE-576)01509703X 0016-7029 nnns volume:58 year:2020 number:6 month:06 pages:704-718 https://doi.org/10.1134/S0016702920050109 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO AR 58 2020 6 06 704-718 |
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10.1134/S0016702920050109 doi (DE-627)OLC2062989180 (DE-He213)S0016702920050109-p DE-627 ger DE-627 rakwb eng 550 VZ Tishchenko, P. Ya. verfasserin aut Organic Carbon and Carbonate System in the Bottom Sediments of Shallow Bights of the Peter the Great Bay (Sea of Japan) 2020 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2020 Abstract—The diagenesis of organic matter (OM) is studied in bottom sediments taken in February, 2018 from therapeutic mud deposits of the Uglovoi Bay and Voevoda and Ekspeditsiya bights (Peter the Great Bay, Sea of Japan). The carbonate system of bottom sediments and pore water were analyzed for the contents of nutrients, dissolved organic carbon, humic substance, and concentrations of sulfates and chlorides. The concentrations of organic carbon, chlorophyll-a, humic and fulvic acids, and mobile sulfide species are measured in a solid phase of sediment. Underwater photographing shows that sampling localities are covered by Zostera marina meadows in the Voevoda and Ekspeditsiya bights and by diatom mats in Uglovoi Bay. The proportions between dissolved inorganic carbon and alkalinity, as well as data on sulfate–chlorine ratios and mobile sulfide species indicate that the OM degradation in bottom sediments is mainly controlled by sulfate reduction. The Uglovoi Bay and Voevoda and Ekspeditsii bights are characterized by different values of bioturbation coefficients: 3.0, 107.6, and 14.5 $ cm^{2} $/day, respectively. The estimated fluxes of organic carbon from water into sediment and of dissolved inorganic carbon from sediment into water significantly differ. The disbalance between organic and inorganic carbons can be caused by the following reasons: (a) ignored $ CO_{2} $ flux released by marine organisms from bottom sediments through their siphonal system; (b) partial OM consumption in food with its subsequent deposition in it. Medvedev, E. V. aut Barabanshchikov, Yu. A. aut Pavlova, G. Yu. aut Sagalaev, S. G. aut Tishchenko, P. P. aut Shvetsova, M. G. aut Shkirnikova, E. M. aut Ulanova, O. A. aut Tibenko, E. Yu. aut Orekhova, N. A. aut Enthalten in Geochemistry international Pleiades Publishing, 1964 58(2020), 6 vom: Juni, Seite 704-718 (DE-627)12960321X (DE-600)241677-3 (DE-576)01509703X 0016-7029 nnns volume:58 year:2020 number:6 month:06 pages:704-718 https://doi.org/10.1134/S0016702920050109 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO AR 58 2020 6 06 704-718 |
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550 VZ Organic Carbon and Carbonate System in the Bottom Sediments of Shallow Bights of the Peter the Great Bay (Sea of Japan) |
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Organic Carbon and Carbonate System in the Bottom Sediments of Shallow Bights of the Peter the Great Bay (Sea of Japan) |
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Organic Carbon and Carbonate System in the Bottom Sediments of Shallow Bights of the Peter the Great Bay (Sea of Japan) |
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Tishchenko, P. Ya. |
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Tishchenko, P. Ya. Medvedev, E. V. Barabanshchikov, Yu. A. Pavlova, G. Yu. Sagalaev, S. G. Tishchenko, P. P. Shvetsova, M. G. Shkirnikova, E. M. Ulanova, O. A. Tibenko, E. Yu. Orekhova, N. A. |
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Tishchenko, P. Ya. |
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10.1134/S0016702920050109 |
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550 |
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organic carbon and carbonate system in the bottom sediments of shallow bights of the peter the great bay (sea of japan) |
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Organic Carbon and Carbonate System in the Bottom Sediments of Shallow Bights of the Peter the Great Bay (Sea of Japan) |
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Abstract—The diagenesis of organic matter (OM) is studied in bottom sediments taken in February, 2018 from therapeutic mud deposits of the Uglovoi Bay and Voevoda and Ekspeditsiya bights (Peter the Great Bay, Sea of Japan). The carbonate system of bottom sediments and pore water were analyzed for the contents of nutrients, dissolved organic carbon, humic substance, and concentrations of sulfates and chlorides. The concentrations of organic carbon, chlorophyll-a, humic and fulvic acids, and mobile sulfide species are measured in a solid phase of sediment. Underwater photographing shows that sampling localities are covered by Zostera marina meadows in the Voevoda and Ekspeditsiya bights and by diatom mats in Uglovoi Bay. The proportions between dissolved inorganic carbon and alkalinity, as well as data on sulfate–chlorine ratios and mobile sulfide species indicate that the OM degradation in bottom sediments is mainly controlled by sulfate reduction. The Uglovoi Bay and Voevoda and Ekspeditsii bights are characterized by different values of bioturbation coefficients: 3.0, 107.6, and 14.5 $ cm^{2} $/day, respectively. The estimated fluxes of organic carbon from water into sediment and of dissolved inorganic carbon from sediment into water significantly differ. The disbalance between organic and inorganic carbons can be caused by the following reasons: (a) ignored $ CO_{2} $ flux released by marine organisms from bottom sediments through their siphonal system; (b) partial OM consumption in food with its subsequent deposition in it. © Pleiades Publishing, Ltd. 2020 |
| abstractGer |
Abstract—The diagenesis of organic matter (OM) is studied in bottom sediments taken in February, 2018 from therapeutic mud deposits of the Uglovoi Bay and Voevoda and Ekspeditsiya bights (Peter the Great Bay, Sea of Japan). The carbonate system of bottom sediments and pore water were analyzed for the contents of nutrients, dissolved organic carbon, humic substance, and concentrations of sulfates and chlorides. The concentrations of organic carbon, chlorophyll-a, humic and fulvic acids, and mobile sulfide species are measured in a solid phase of sediment. Underwater photographing shows that sampling localities are covered by Zostera marina meadows in the Voevoda and Ekspeditsiya bights and by diatom mats in Uglovoi Bay. The proportions between dissolved inorganic carbon and alkalinity, as well as data on sulfate–chlorine ratios and mobile sulfide species indicate that the OM degradation in bottom sediments is mainly controlled by sulfate reduction. The Uglovoi Bay and Voevoda and Ekspeditsii bights are characterized by different values of bioturbation coefficients: 3.0, 107.6, and 14.5 $ cm^{2} $/day, respectively. The estimated fluxes of organic carbon from water into sediment and of dissolved inorganic carbon from sediment into water significantly differ. The disbalance between organic and inorganic carbons can be caused by the following reasons: (a) ignored $ CO_{2} $ flux released by marine organisms from bottom sediments through their siphonal system; (b) partial OM consumption in food with its subsequent deposition in it. © Pleiades Publishing, Ltd. 2020 |
| abstract_unstemmed |
Abstract—The diagenesis of organic matter (OM) is studied in bottom sediments taken in February, 2018 from therapeutic mud deposits of the Uglovoi Bay and Voevoda and Ekspeditsiya bights (Peter the Great Bay, Sea of Japan). The carbonate system of bottom sediments and pore water were analyzed for the contents of nutrients, dissolved organic carbon, humic substance, and concentrations of sulfates and chlorides. The concentrations of organic carbon, chlorophyll-a, humic and fulvic acids, and mobile sulfide species are measured in a solid phase of sediment. Underwater photographing shows that sampling localities are covered by Zostera marina meadows in the Voevoda and Ekspeditsiya bights and by diatom mats in Uglovoi Bay. The proportions between dissolved inorganic carbon and alkalinity, as well as data on sulfate–chlorine ratios and mobile sulfide species indicate that the OM degradation in bottom sediments is mainly controlled by sulfate reduction. The Uglovoi Bay and Voevoda and Ekspeditsii bights are characterized by different values of bioturbation coefficients: 3.0, 107.6, and 14.5 $ cm^{2} $/day, respectively. The estimated fluxes of organic carbon from water into sediment and of dissolved inorganic carbon from sediment into water significantly differ. The disbalance between organic and inorganic carbons can be caused by the following reasons: (a) ignored $ CO_{2} $ flux released by marine organisms from bottom sediments through their siphonal system; (b) partial OM consumption in food with its subsequent deposition in it. © Pleiades Publishing, Ltd. 2020 |
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Organic Carbon and Carbonate System in the Bottom Sediments of Shallow Bights of the Peter the Great Bay (Sea of Japan) |
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Medvedev, E. V. Barabanshchikov, Yu. A. Pavlova, G. Yu Sagalaev, S. G. Tishchenko, P. P. Shvetsova, M. G. Shkirnikova, E. M. Ulanova, O. A. Tibenko, E. Yu Orekhova, N. A. |
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Medvedev, E. V. Barabanshchikov, Yu. A. Pavlova, G. Yu Sagalaev, S. G. Tishchenko, P. P. Shvetsova, M. G. Shkirnikova, E. M. Ulanova, O. A. Tibenko, E. Yu Orekhova, N. A. |
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