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Heterotrophic Bacterial Utilization of Nitrogenous and Nonnitrogenous Substrates, Determined from Ammonia and Oxygen Fluxes
We describe a simple procedure to allow the broad nature of the organic substrates used for planktonic bacterial growth to be determined. The method analyzes the coupled oxygen and ammonia fluxes in terms of the relative proportions of nitrogenous and nonnitrogenous substrates assimilated by the mic...
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Published in: | Limnology and oceanography 2001-11, Vol.46 (7), p.1675-1683 |
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container_title | Limnology and oceanography |
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creator | Rodrigues, Rubina M. N. V. Williams, Peter J. le B. |
description | We describe a simple procedure to allow the broad nature of the organic substrates used for planktonic bacterial growth to be determined. The method analyzes the coupled oxygen and ammonia fluxes in terms of the relative proportions of nitrogenous and nonnitrogenous substrates assimilated by the microheterotrophs. The model uses a stoichiometric equation that requires the knowledge of the respiratory quotient, substrate C/N ratio, cell C/N quota, and bacterial carbon growth yield and the assumption that nitrification was not occurring. We discuss the uncertainties associated with the attribution of values for these constants and illustrate the use and limitations of the approach in the interpretation of field observations on bacterioplankton metabolism in a temperate coastal ecosystem. With the exception of a single observation, we were able to interpret the data using the proposed model. Our findings are that during the spring bloom, nitrogenous substrates made up 40-80% of the total, falling to |
doi_str_mv | 10.4319/lo.2001.46.7.1675 |
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N. V. ; Williams, Peter J. le B.</creator><creatorcontrib>Rodrigues, Rubina M. N. V. ; Williams, Peter J. le B.</creatorcontrib><description>We describe a simple procedure to allow the broad nature of the organic substrates used for planktonic bacterial growth to be determined. The method analyzes the coupled oxygen and ammonia fluxes in terms of the relative proportions of nitrogenous and nonnitrogenous substrates assimilated by the microheterotrophs. The model uses a stoichiometric equation that requires the knowledge of the respiratory quotient, substrate C/N ratio, cell C/N quota, and bacterial carbon growth yield and the assumption that nitrification was not occurring. We discuss the uncertainties associated with the attribution of values for these constants and illustrate the use and limitations of the approach in the interpretation of field observations on bacterioplankton metabolism in a temperate coastal ecosystem. With the exception of a single observation, we were able to interpret the data using the proposed model. Our findings are that during the spring bloom, nitrogenous substrates made up 40-80% of the total, falling to <20% in the postbloom period. Thus, with essentially routine methods for determining oxygen and ammonia fluxes, we have been able to determine a fundamental aspect of the cycling of organic material by the bacterioplankton.</description><identifier>ISSN: 0024-3590</identifier><identifier>EISSN: 1939-5590</identifier><identifier>DOI: 10.4319/lo.2001.46.7.1675</identifier><identifier>CODEN: LIOCAH</identifier><language>eng</language><publisher>Waco, TX: American Society of Limnology and Oceanography</publisher><subject>Amino acids ; Ammonia ; Animal and plant ecology ; Animal, plant and microbial ecology ; Bacteria ; Biochemistry ; Biological and medical sciences ; Fundamental and applied biological sciences. Psychology ; Marine ; Nitrification ; Nitrogen ; Nucleic acids ; organic substances ; Oxygen ; Ratios ; Sea water ; Sea water ecosystems ; Synecology</subject><ispartof>Limnology and oceanography, 2001-11, Vol.46 (7), p.1675-1683</ispartof><rights>Copyright 2001 American Society of Limnology and Oceanography Inc.</rights><rights>2001, by the Association for the Sciences of Limnology and Oceanography, Inc.</rights><rights>2002 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4125-18dd8753d7db7209aa3258fd4c9516a92a4104df8142ecc7917cac9a0697004e3</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27900,27901</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=14150726$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Rodrigues, Rubina M. N. V.</creatorcontrib><creatorcontrib>Williams, Peter J. le B.</creatorcontrib><title>Heterotrophic Bacterial Utilization of Nitrogenous and Nonnitrogenous Substrates, Determined from Ammonia and Oxygen Fluxes</title><title>Limnology and oceanography</title><description>We describe a simple procedure to allow the broad nature of the organic substrates used for planktonic bacterial growth to be determined. The method analyzes the coupled oxygen and ammonia fluxes in terms of the relative proportions of nitrogenous and nonnitrogenous substrates assimilated by the microheterotrophs. The model uses a stoichiometric equation that requires the knowledge of the respiratory quotient, substrate C/N ratio, cell C/N quota, and bacterial carbon growth yield and the assumption that nitrification was not occurring. We discuss the uncertainties associated with the attribution of values for these constants and illustrate the use and limitations of the approach in the interpretation of field observations on bacterioplankton metabolism in a temperate coastal ecosystem. With the exception of a single observation, we were able to interpret the data using the proposed model. Our findings are that during the spring bloom, nitrogenous substrates made up 40-80% of the total, falling to <20% in the postbloom period. Thus, with essentially routine methods for determining oxygen and ammonia fluxes, we have been able to determine a fundamental aspect of the cycling of organic material by the bacterioplankton.</description><subject>Amino acids</subject><subject>Ammonia</subject><subject>Animal and plant ecology</subject><subject>Animal, plant and microbial ecology</subject><subject>Bacteria</subject><subject>Biochemistry</subject><subject>Biological and medical sciences</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>Marine</subject><subject>Nitrification</subject><subject>Nitrogen</subject><subject>Nucleic acids</subject><subject>organic substances</subject><subject>Oxygen</subject><subject>Ratios</subject><subject>Sea water</subject><subject>Sea water ecosystems</subject><subject>Synecology</subject><issn>0024-3590</issn><issn>1939-5590</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2001</creationdate><recordtype>article</recordtype><recordid>eNqFkTtvFDEURi0EEkvCD4hE4QZEwQx-e1xQJCEPpNVuQVJbjscDjjz2Ys-KLPx5POwq0KWyfXXOd698ATjBqGUUq48htQQh3DLRyhYLyZ-BBVZUNZwr9BwsECKsofX-Erwq5R4hpDjnC_D72k0upymnzXdv4Zmx9elNgLeTD_6XmXyKMA1w5SvyzcW0LdDEHq5SjP-Vvm7vypTN5MoH-HlOHH10PRxyGuHpOKbozV9t_bCrBrwM2wdXjsGLwYTiXh_OI3B7eXFzft0s11dfzk-XjWWY8AZ3fd9JTnvZ30mClDGU8G7omVUcC6OIYRixfugwI85aqbC0xiqDhJIIMUePwLt97ianH1tXJj36Yl0IJro6vMYdYaITtILvnwCxqk1Y11UU71GbUynZDXqT_WjyTmOk543okPS8Ec2ElnreSHXeHuJNsSYM2UTryz-RYY4kEZX7tOd--uB2Twfr5Wo9V5iQhz5v9v59mVJ-9Gn9EKQw_QPjvajn</recordid><startdate>200111</startdate><enddate>200111</enddate><creator>Rodrigues, Rubina M. 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V. ; Williams, Peter J. le B.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4125-18dd8753d7db7209aa3258fd4c9516a92a4104df8142ecc7917cac9a0697004e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2001</creationdate><topic>Amino acids</topic><topic>Ammonia</topic><topic>Animal and plant ecology</topic><topic>Animal, plant and microbial ecology</topic><topic>Bacteria</topic><topic>Biochemistry</topic><topic>Biological and medical sciences</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>Marine</topic><topic>Nitrification</topic><topic>Nitrogen</topic><topic>Nucleic acids</topic><topic>organic substances</topic><topic>Oxygen</topic><topic>Ratios</topic><topic>Sea water</topic><topic>Sea water ecosystems</topic><topic>Synecology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Rodrigues, Rubina M. N. V.</creatorcontrib><creatorcontrib>Williams, Peter J. le B.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Aqualine</collection><collection>Bacteriology Abstracts (Microbiology B)</collection><collection>Ecology Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Oceanic Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><jtitle>Limnology and oceanography</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Rodrigues, Rubina M. N. V.</au><au>Williams, Peter J. le B.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Heterotrophic Bacterial Utilization of Nitrogenous and Nonnitrogenous Substrates, Determined from Ammonia and Oxygen Fluxes</atitle><jtitle>Limnology and oceanography</jtitle><date>2001-11</date><risdate>2001</risdate><volume>46</volume><issue>7</issue><spage>1675</spage><epage>1683</epage><pages>1675-1683</pages><issn>0024-3590</issn><eissn>1939-5590</eissn><coden>LIOCAH</coden><abstract>We describe a simple procedure to allow the broad nature of the organic substrates used for planktonic bacterial growth to be determined. The method analyzes the coupled oxygen and ammonia fluxes in terms of the relative proportions of nitrogenous and nonnitrogenous substrates assimilated by the microheterotrophs. The model uses a stoichiometric equation that requires the knowledge of the respiratory quotient, substrate C/N ratio, cell C/N quota, and bacterial carbon growth yield and the assumption that nitrification was not occurring. We discuss the uncertainties associated with the attribution of values for these constants and illustrate the use and limitations of the approach in the interpretation of field observations on bacterioplankton metabolism in a temperate coastal ecosystem. With the exception of a single observation, we were able to interpret the data using the proposed model. Our findings are that during the spring bloom, nitrogenous substrates made up 40-80% of the total, falling to <20% in the postbloom period. Thus, with essentially routine methods for determining oxygen and ammonia fluxes, we have been able to determine a fundamental aspect of the cycling of organic material by the bacterioplankton.</abstract><cop>Waco, TX</cop><pub>American Society of Limnology and Oceanography</pub><doi>10.4319/lo.2001.46.7.1675</doi><tpages>9</tpages></addata></record> |
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subjects | Amino acids Ammonia Animal and plant ecology Animal, plant and microbial ecology Bacteria Biochemistry Biological and medical sciences Fundamental and applied biological sciences. Psychology Marine Nitrification Nitrogen Nucleic acids organic substances Oxygen Ratios Sea water Sea water ecosystems Synecology |
title | Heterotrophic Bacterial Utilization of Nitrogenous and Nonnitrogenous Substrates, Determined from Ammonia and Oxygen Fluxes |
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