Organic geochemical characteristics of time-series settling particles in northern South China Sea and their implications
Abstract Organic carbon, total nitrogen, amino acids, sugars, and chlorophyll were determined in < 1 mm fractions of the samples collected by successive large aperture time-series sediment traps (Honjo-Mark M) in northern South China Sea during September 1987 to October 1988. The ratio of C/N and...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Jianfang, Chen [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
1998 |
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| Anmerkung: |
© Institute of Geochemistry, Chinese Academy of Sciences 1998 |
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| Übergeordnetes Werk: |
Enthalten in: Chinese journal of geochemistry - Science in China Press, 1985, 17(1998), 3 vom: Juli, Seite 275-283 |
|---|---|
| Übergeordnetes Werk: |
volume:17 ; year:1998 ; number:3 ; month:07 ; pages:275-283 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF02834604 |
|---|
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| 520 | |a Abstract Organic carbon, total nitrogen, amino acids, sugars, and chlorophyll were determined in < 1 mm fractions of the samples collected by successive large aperture time-series sediment traps (Honjo-Mark M) in northern South China Sea during September 1987 to October 1988. The ratio of C/N and the relative abundance of amino acids and sugars show that organic matter in the settling particles from northern South China Sea is derived mainly from marine plantkon (especially phytoplankton). The organic carbon fluxes in our sediment traps are lower than those in other sediment traps. But the relative contents of $ C_{org} $/total particulate matter are generally similar to those in the Panama Basin, Arabian Sea and Subarctic Pacific. It is suggested that monsoon-caused changes of physical and chemical conditions in the upper euphotic layer would control the fluxes of organic matter as well as its composition and transport in northern South China Sea. | ||
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10.1007/BF02834604 doi (DE-627)OLC2088099913 (DE-He213)BF02834604-p DE-627 ger DE-627 rakwb eng 550 540 VZ 13 ssgn Jianfang, Chen verfasserin aut Organic geochemical characteristics of time-series settling particles in northern South China Sea and their implications 1998 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institute of Geochemistry, Chinese Academy of Sciences 1998 Abstract Organic carbon, total nitrogen, amino acids, sugars, and chlorophyll were determined in < 1 mm fractions of the samples collected by successive large aperture time-series sediment traps (Honjo-Mark M) in northern South China Sea during September 1987 to October 1988. The ratio of C/N and the relative abundance of amino acids and sugars show that organic matter in the settling particles from northern South China Sea is derived mainly from marine plantkon (especially phytoplankton). The organic carbon fluxes in our sediment traps are lower than those in other sediment traps. But the relative contents of $ C_{org} $/total particulate matter are generally similar to those in the Panama Basin, Arabian Sea and Subarctic Pacific. It is suggested that monsoon-caused changes of physical and chemical conditions in the upper euphotic layer would control the fluxes of organic matter as well as its composition and transport in northern South China Sea. Luqiang, Xu aut Lianfu, Zheng aut Wong, How-Kin aut Jennerjahn, Tim aut Enthalten in Chinese journal of geochemistry Science in China Press, 1985 17(1998), 3 vom: Juli, Seite 275-283 (DE-627)130963208 (DE-600)1066729-5 (DE-576)077051459 1000-9426 nnns volume:17 year:1998 number:3 month:07 pages:275-283 https://doi.org/10.1007/BF02834604 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_4012 AR 17 1998 3 07 275-283 |
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10.1007/BF02834604 doi (DE-627)OLC2088099913 (DE-He213)BF02834604-p DE-627 ger DE-627 rakwb eng 550 540 VZ 13 ssgn Jianfang, Chen verfasserin aut Organic geochemical characteristics of time-series settling particles in northern South China Sea and their implications 1998 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institute of Geochemistry, Chinese Academy of Sciences 1998 Abstract Organic carbon, total nitrogen, amino acids, sugars, and chlorophyll were determined in < 1 mm fractions of the samples collected by successive large aperture time-series sediment traps (Honjo-Mark M) in northern South China Sea during September 1987 to October 1988. The ratio of C/N and the relative abundance of amino acids and sugars show that organic matter in the settling particles from northern South China Sea is derived mainly from marine plantkon (especially phytoplankton). The organic carbon fluxes in our sediment traps are lower than those in other sediment traps. But the relative contents of $ C_{org} $/total particulate matter are generally similar to those in the Panama Basin, Arabian Sea and Subarctic Pacific. It is suggested that monsoon-caused changes of physical and chemical conditions in the upper euphotic layer would control the fluxes of organic matter as well as its composition and transport in northern South China Sea. Luqiang, Xu aut Lianfu, Zheng aut Wong, How-Kin aut Jennerjahn, Tim aut Enthalten in Chinese journal of geochemistry Science in China Press, 1985 17(1998), 3 vom: Juli, Seite 275-283 (DE-627)130963208 (DE-600)1066729-5 (DE-576)077051459 1000-9426 nnns volume:17 year:1998 number:3 month:07 pages:275-283 https://doi.org/10.1007/BF02834604 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_4012 AR 17 1998 3 07 275-283 |
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10.1007/BF02834604 doi (DE-627)OLC2088099913 (DE-He213)BF02834604-p DE-627 ger DE-627 rakwb eng 550 540 VZ 13 ssgn Jianfang, Chen verfasserin aut Organic geochemical characteristics of time-series settling particles in northern South China Sea and their implications 1998 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institute of Geochemistry, Chinese Academy of Sciences 1998 Abstract Organic carbon, total nitrogen, amino acids, sugars, and chlorophyll were determined in < 1 mm fractions of the samples collected by successive large aperture time-series sediment traps (Honjo-Mark M) in northern South China Sea during September 1987 to October 1988. The ratio of C/N and the relative abundance of amino acids and sugars show that organic matter in the settling particles from northern South China Sea is derived mainly from marine plantkon (especially phytoplankton). The organic carbon fluxes in our sediment traps are lower than those in other sediment traps. But the relative contents of $ C_{org} $/total particulate matter are generally similar to those in the Panama Basin, Arabian Sea and Subarctic Pacific. It is suggested that monsoon-caused changes of physical and chemical conditions in the upper euphotic layer would control the fluxes of organic matter as well as its composition and transport in northern South China Sea. Luqiang, Xu aut Lianfu, Zheng aut Wong, How-Kin aut Jennerjahn, Tim aut Enthalten in Chinese journal of geochemistry Science in China Press, 1985 17(1998), 3 vom: Juli, Seite 275-283 (DE-627)130963208 (DE-600)1066729-5 (DE-576)077051459 1000-9426 nnns volume:17 year:1998 number:3 month:07 pages:275-283 https://doi.org/10.1007/BF02834604 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_4012 AR 17 1998 3 07 275-283 |
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10.1007/BF02834604 doi (DE-627)OLC2088099913 (DE-He213)BF02834604-p DE-627 ger DE-627 rakwb eng 550 540 VZ 13 ssgn Jianfang, Chen verfasserin aut Organic geochemical characteristics of time-series settling particles in northern South China Sea and their implications 1998 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institute of Geochemistry, Chinese Academy of Sciences 1998 Abstract Organic carbon, total nitrogen, amino acids, sugars, and chlorophyll were determined in < 1 mm fractions of the samples collected by successive large aperture time-series sediment traps (Honjo-Mark M) in northern South China Sea during September 1987 to October 1988. The ratio of C/N and the relative abundance of amino acids and sugars show that organic matter in the settling particles from northern South China Sea is derived mainly from marine plantkon (especially phytoplankton). The organic carbon fluxes in our sediment traps are lower than those in other sediment traps. But the relative contents of $ C_{org} $/total particulate matter are generally similar to those in the Panama Basin, Arabian Sea and Subarctic Pacific. It is suggested that monsoon-caused changes of physical and chemical conditions in the upper euphotic layer would control the fluxes of organic matter as well as its composition and transport in northern South China Sea. Luqiang, Xu aut Lianfu, Zheng aut Wong, How-Kin aut Jennerjahn, Tim aut Enthalten in Chinese journal of geochemistry Science in China Press, 1985 17(1998), 3 vom: Juli, Seite 275-283 (DE-627)130963208 (DE-600)1066729-5 (DE-576)077051459 1000-9426 nnns volume:17 year:1998 number:3 month:07 pages:275-283 https://doi.org/10.1007/BF02834604 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_4012 AR 17 1998 3 07 275-283 |
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10.1007/BF02834604 doi (DE-627)OLC2088099913 (DE-He213)BF02834604-p DE-627 ger DE-627 rakwb eng 550 540 VZ 13 ssgn Jianfang, Chen verfasserin aut Organic geochemical characteristics of time-series settling particles in northern South China Sea and their implications 1998 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institute of Geochemistry, Chinese Academy of Sciences 1998 Abstract Organic carbon, total nitrogen, amino acids, sugars, and chlorophyll were determined in < 1 mm fractions of the samples collected by successive large aperture time-series sediment traps (Honjo-Mark M) in northern South China Sea during September 1987 to October 1988. The ratio of C/N and the relative abundance of amino acids and sugars show that organic matter in the settling particles from northern South China Sea is derived mainly from marine plantkon (especially phytoplankton). The organic carbon fluxes in our sediment traps are lower than those in other sediment traps. But the relative contents of $ C_{org} $/total particulate matter are generally similar to those in the Panama Basin, Arabian Sea and Subarctic Pacific. It is suggested that monsoon-caused changes of physical and chemical conditions in the upper euphotic layer would control the fluxes of organic matter as well as its composition and transport in northern South China Sea. Luqiang, Xu aut Lianfu, Zheng aut Wong, How-Kin aut Jennerjahn, Tim aut Enthalten in Chinese journal of geochemistry Science in China Press, 1985 17(1998), 3 vom: Juli, Seite 275-283 (DE-627)130963208 (DE-600)1066729-5 (DE-576)077051459 1000-9426 nnns volume:17 year:1998 number:3 month:07 pages:275-283 https://doi.org/10.1007/BF02834604 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_4012 AR 17 1998 3 07 275-283 |
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Abstract Organic carbon, total nitrogen, amino acids, sugars, and chlorophyll were determined in < 1 mm fractions of the samples collected by successive large aperture time-series sediment traps (Honjo-Mark M) in northern South China Sea during September 1987 to October 1988. The ratio of C/N and the relative abundance of amino acids and sugars show that organic matter in the settling particles from northern South China Sea is derived mainly from marine plantkon (especially phytoplankton). The organic carbon fluxes in our sediment traps are lower than those in other sediment traps. But the relative contents of $ C_{org} $/total particulate matter are generally similar to those in the Panama Basin, Arabian Sea and Subarctic Pacific. It is suggested that monsoon-caused changes of physical and chemical conditions in the upper euphotic layer would control the fluxes of organic matter as well as its composition and transport in northern South China Sea. © Institute of Geochemistry, Chinese Academy of Sciences 1998 |
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Abstract Organic carbon, total nitrogen, amino acids, sugars, and chlorophyll were determined in < 1 mm fractions of the samples collected by successive large aperture time-series sediment traps (Honjo-Mark M) in northern South China Sea during September 1987 to October 1988. The ratio of C/N and the relative abundance of amino acids and sugars show that organic matter in the settling particles from northern South China Sea is derived mainly from marine plantkon (especially phytoplankton). The organic carbon fluxes in our sediment traps are lower than those in other sediment traps. But the relative contents of $ C_{org} $/total particulate matter are generally similar to those in the Panama Basin, Arabian Sea and Subarctic Pacific. It is suggested that monsoon-caused changes of physical and chemical conditions in the upper euphotic layer would control the fluxes of organic matter as well as its composition and transport in northern South China Sea. © Institute of Geochemistry, Chinese Academy of Sciences 1998 |
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Abstract Organic carbon, total nitrogen, amino acids, sugars, and chlorophyll were determined in < 1 mm fractions of the samples collected by successive large aperture time-series sediment traps (Honjo-Mark M) in northern South China Sea during September 1987 to October 1988. The ratio of C/N and the relative abundance of amino acids and sugars show that organic matter in the settling particles from northern South China Sea is derived mainly from marine plantkon (especially phytoplankton). The organic carbon fluxes in our sediment traps are lower than those in other sediment traps. But the relative contents of $ C_{org} $/total particulate matter are generally similar to those in the Panama Basin, Arabian Sea and Subarctic Pacific. It is suggested that monsoon-caused changes of physical and chemical conditions in the upper euphotic layer would control the fluxes of organic matter as well as its composition and transport in northern South China Sea. © Institute of Geochemistry, Chinese Academy of Sciences 1998 |
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