Elevated NH sub(4) super(+) in a neutrally buoyant hydrothermal plume
Anomalously high concentrations of NH sub(4) super(+) in hydrothermal vent discharge fluids were tracked in the resulting neutrally buoyant plume over the unsedimented Endeavour Segment, Juan de Fuca Ridge. Vertical profiles of NH sub(4) super(+) concentrations showed plume depth ( similar to 2025 m...
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Veröffentlicht in: | Deep-sea research. Part I, Oceanographic research papers Oceanographic research papers, 1998-11, Vol.45 (11), p.1891-1902 |
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container_title | Deep-sea research. Part I, Oceanographic research papers |
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creator | Cowen, J P Wen, Xiyuan Jones, R D Thomson, R E |
description | Anomalously high concentrations of NH sub(4) super(+) in hydrothermal vent discharge fluids were tracked in the resulting neutrally buoyant plume over the unsedimented Endeavour Segment, Juan de Fuca Ridge. Vertical profiles of NH sub(4) super(+) concentrations showed plume depth ( similar to 2025 m) maxima of nearly 400 nM over the Endeavour Segment's main vent field, on the same order as most subsurface NH sub(4) super(+) maxima. Plume NH sub(4) super(+) values decreased to just above background deep water values (50-70 nM) in older plume water at a station 15 km southwest of the vent field, although most of the plume NH sub(4) super(+) appears to be transported beyond the ridge axial valley. Preliminary net specific NH sub(4) super(+) removal rates determined within the plume maximum (0.04-0.13 d super(-1)) and corresponding turnover times (8-28 d) are similar to values for CH sub(4) oxidation rates. The data suggest that NH sub(4) super(+) may be a significant substrate for in situ chemolithotrophic production of organic matter in the Endeavour Segment hydrothermal plume. |
doi_str_mv | 10.1016/S0967-0637(98)00032-6 |
format | Article |
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Vertical profiles of NH sub(4) super(+) concentrations showed plume depth ( similar to 2025 m) maxima of nearly 400 nM over the Endeavour Segment's main vent field, on the same order as most subsurface NH sub(4) super(+) maxima. Plume NH sub(4) super(+) values decreased to just above background deep water values (50-70 nM) in older plume water at a station 15 km southwest of the vent field, although most of the plume NH sub(4) super(+) appears to be transported beyond the ridge axial valley. Preliminary net specific NH sub(4) super(+) removal rates determined within the plume maximum (0.04-0.13 d super(-1)) and corresponding turnover times (8-28 d) are similar to values for CH sub(4) oxidation rates. The data suggest that NH sub(4) super(+) may be a significant substrate for in situ chemolithotrophic production of organic matter in the Endeavour Segment hydrothermal plume.</description><identifier>ISSN: 0967-0637</identifier><identifier>DOI: 10.1016/S0967-0637(98)00032-6</identifier><language>eng</language><subject>Marine</subject><ispartof>Deep-sea research. 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Vertical profiles of NH sub(4) super(+) concentrations showed plume depth ( similar to 2025 m) maxima of nearly 400 nM over the Endeavour Segment's main vent field, on the same order as most subsurface NH sub(4) super(+) maxima. Plume NH sub(4) super(+) values decreased to just above background deep water values (50-70 nM) in older plume water at a station 15 km southwest of the vent field, although most of the plume NH sub(4) super(+) appears to be transported beyond the ridge axial valley. Preliminary net specific NH sub(4) super(+) removal rates determined within the plume maximum (0.04-0.13 d super(-1)) and corresponding turnover times (8-28 d) are similar to values for CH sub(4) oxidation rates. 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Part I, Oceanographic research papers</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Cowen, J P</au><au>Wen, Xiyuan</au><au>Jones, R D</au><au>Thomson, R E</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Elevated NH sub(4) super(+) in a neutrally buoyant hydrothermal plume</atitle><jtitle>Deep-sea research. Part I, Oceanographic research papers</jtitle><date>1998-11-01</date><risdate>1998</risdate><volume>45</volume><issue>11</issue><spage>1891</spage><epage>1902</epage><pages>1891-1902</pages><issn>0967-0637</issn><abstract>Anomalously high concentrations of NH sub(4) super(+) in hydrothermal vent discharge fluids were tracked in the resulting neutrally buoyant plume over the unsedimented Endeavour Segment, Juan de Fuca Ridge. Vertical profiles of NH sub(4) super(+) concentrations showed plume depth ( similar to 2025 m) maxima of nearly 400 nM over the Endeavour Segment's main vent field, on the same order as most subsurface NH sub(4) super(+) maxima. Plume NH sub(4) super(+) values decreased to just above background deep water values (50-70 nM) in older plume water at a station 15 km southwest of the vent field, although most of the plume NH sub(4) super(+) appears to be transported beyond the ridge axial valley. Preliminary net specific NH sub(4) super(+) removal rates determined within the plume maximum (0.04-0.13 d super(-1)) and corresponding turnover times (8-28 d) are similar to values for CH sub(4) oxidation rates. The data suggest that NH sub(4) super(+) may be a significant substrate for in situ chemolithotrophic production of organic matter in the Endeavour Segment hydrothermal plume.</abstract><doi>10.1016/S0967-0637(98)00032-6</doi><tpages>12</tpages></addata></record> |
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title | Elevated NH sub(4) super(+) in a neutrally buoyant hydrothermal plume |
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