Production-Respiration Relationships at Different Timescales within the Biosphere 2 Coral Reef Biome
Temporal relationships between organic carbon production and respiration are not well understood in coral reef ecosystems. We monitored dissolved oxygen (O2) concentrations within the Biosphere 2 coral reef biome over a 3-yr period (1 January 1997-1 January 2000), to calculate daily rates of gross p...
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description | Temporal relationships between organic carbon production and respiration are not well understood in coral reef ecosystems. We monitored dissolved oxygen (O2) concentrations within the Biosphere 2 coral reef biome over a 3-yr period (1 January 1997-1 January 2000), to calculate daily rates of gross production (P), community respiration (R), and net community production (NCP). P averaged 170 mmol $O_2\>m^{-2}\>d^{-1}$, and R averaged 173 mmol $O_2\>m^{-2}\>d^{-1}$, which yielded a mean NCP of only -3 mmol $O_2\>m^{-2}\>d^{-1}$, or a difference of only 2%. This long-term balance between P and R reflects the closed-system design of the biome. The SD of P, however, was ±56 mmol $O_2\>m^{-2}\>d^{-1}$; that of R was ±47 mmol $O_2\>m^{-2}\>d^{-1}$; and that of NCP was ±26 mmol $O_2\>m^{-2}\>d^{-1}$ or ±15% of mean P. To better resolve the behavior of P, R, and NCP at different timescales, each of these time series were spectrally decomposed into four frequency bands that corresponded to four timescales: 3 months (seasonal to annual). At timescales >1 month, the variance of P was not different from the variance of R. At timescales of |
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J. ; Langdon, Chris</creator><creatorcontrib>Falter, James L. ; Atkinson, M. J. ; Langdon, Chris</creatorcontrib><description>Temporal relationships between organic carbon production and respiration are not well understood in coral reef ecosystems. We monitored dissolved oxygen (O2) concentrations within the Biosphere 2 coral reef biome over a 3-yr period (1 January 1997-1 January 2000), to calculate daily rates of gross production (P), community respiration (R), and net community production (NCP). P averaged 170 mmol $O_2\>m^{-2}\>d^{-1}$, and R averaged 173 mmol $O_2\>m^{-2}\>d^{-1}$, which yielded a mean NCP of only -3 mmol $O_2\>m^{-2}\>d^{-1}$, or a difference of only 2%. This long-term balance between P and R reflects the closed-system design of the biome. The SD of P, however, was ±56 mmol $O_2\>m^{-2}\>d^{-1}$; that of R was ±47 mmol $O_2\>m^{-2}\>d^{-1}$; and that of NCP was ±26 mmol $O_2\>m^{-2}\>d^{-1}$ or ±15% of mean P. To better resolve the behavior of P, R, and NCP at different timescales, each of these time series were spectrally decomposed into four frequency bands that corresponded to four timescales: <1 week, 1 week-1 month, 1-3 months (subseasonal), and >3 months (seasonal to annual). At timescales >1 month, the variance of P was not different from the variance of R. At timescales of <1 month, the variance in P was significantly greater than the variance in R (P < 0.01). Furthermore, the correlation between changes in P and changes in R became weaker with decreasing timescale. We suggest that changes in P and R become well matched at timescales that coincide with the turnover of carbon by the dominant macroalgae within the biome (1-3 months). In addition, we conclude that measurements of NCP based on daily or weekly data sets are not good indicators of the long-term net metabolic performance of coral reefs.</description><identifier>ISSN: 0024-3590</identifier><identifier>EISSN: 1939-5590</identifier><identifier>DOI: 10.4319/lo.2001.46.7.1653</identifier><identifier>CODEN: LIOCAH</identifier><language>eng</language><publisher>Waco, TX: American Society of Limnology and Oceanography</publisher><subject>Animal and plant ecology ; Animal, plant and microbial ecology ; Arcologies ; Biological and medical sciences ; Biomes ; Coral reefs ; Fundamental and applied biological sciences. Psychology ; Marine ; Oceans ; Reefs ; Respiration ; Sea water ; Sea water ecosystems ; Sensors ; Statistical variance ; Synecology ; Time series</subject><ispartof>Limnology and oceanography, 2001-11, Vol.46 (7), p.1653-1660</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><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a5443-fd3c4bb9f7d9e390e03963fe1370867428f12c472fdd6af642960ff09984d1fd3</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/3069089$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/3069089$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,803,1417,1433,27924,27925,45574,45575,46409,46833,58017,58250</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=14150728$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Falter, James L.</creatorcontrib><creatorcontrib>Atkinson, M. J.</creatorcontrib><creatorcontrib>Langdon, Chris</creatorcontrib><title>Production-Respiration Relationships at Different Timescales within the Biosphere 2 Coral Reef Biome</title><title>Limnology and oceanography</title><description>Temporal relationships between organic carbon production and respiration are not well understood in coral reef ecosystems. We monitored dissolved oxygen (O2) concentrations within the Biosphere 2 coral reef biome over a 3-yr period (1 January 1997-1 January 2000), to calculate daily rates of gross production (P), community respiration (R), and net community production (NCP). P averaged 170 mmol $O_2\>m^{-2}\>d^{-1}$, and R averaged 173 mmol $O_2\>m^{-2}\>d^{-1}$, which yielded a mean NCP of only -3 mmol $O_2\>m^{-2}\>d^{-1}$, or a difference of only 2%. This long-term balance between P and R reflects the closed-system design of the biome. The SD of P, however, was ±56 mmol $O_2\>m^{-2}\>d^{-1}$; that of R was ±47 mmol $O_2\>m^{-2}\>d^{-1}$; and that of NCP was ±26 mmol $O_2\>m^{-2}\>d^{-1}$ or ±15% of mean P. To better resolve the behavior of P, R, and NCP at different timescales, each of these time series were spectrally decomposed into four frequency bands that corresponded to four timescales: <1 week, 1 week-1 month, 1-3 months (subseasonal), and >3 months (seasonal to annual). At timescales >1 month, the variance of P was not different from the variance of R. At timescales of <1 month, the variance in P was significantly greater than the variance in R (P < 0.01). Furthermore, the correlation between changes in P and changes in R became weaker with decreasing timescale. We suggest that changes in P and R become well matched at timescales that coincide with the turnover of carbon by the dominant macroalgae within the biome (1-3 months). In addition, we conclude that measurements of NCP based on daily or weekly data sets are not good indicators of the long-term net metabolic performance of coral reefs.</description><subject>Animal and plant ecology</subject><subject>Animal, plant and microbial ecology</subject><subject>Arcologies</subject><subject>Biological and medical sciences</subject><subject>Biomes</subject><subject>Coral reefs</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>Marine</subject><subject>Oceans</subject><subject>Reefs</subject><subject>Respiration</subject><subject>Sea water</subject><subject>Sea water ecosystems</subject><subject>Sensors</subject><subject>Statistical variance</subject><subject>Synecology</subject><subject>Time series</subject><issn>0024-3590</issn><issn>1939-5590</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2001</creationdate><recordtype>article</recordtype><recordid>eNqFkE1v1DAURS1UJKaFH4DEwpsiNgnPH3HiRRcwtAVpRFFV1pabPGtceeJgZ1T13xMzo7LsyldP515Lh5D3DGopmP4cYs0BWC1V3dZMNeIVWTEtdNU0Gk7ICoDLSiz5DTnN-QEAdNM0KzL8SnHY97OPY3WLefLJlkxvMfwLeeunTO1Mv3nnMOE40zu_w9zbgJk--nnrRzpvkX71MU_bhaCcrmOyYZlAV847fEteOxsyvju-Z-T31eXd-nu1ubn-sf6yqWwjpajcIHp5f69dO2gUGhCEVsIhEy10qpW8c4z3suVuGJR1SnKtwDnQupMDW9pn5ONhd0rxzx7zbHY-9xiCHTHus2Edl0JxvoCfXgCZZsVWQdkB7VPMOaEzU_I7m54MA1PUmxBNUW-kMq0p6pfO-XHeFlEu2bH3-X9RsgZa3i3cxYF79AGfXh42m5835SJVe_znw6H_kOeYnvsClIZOi78br5-I</recordid><startdate>200111</startdate><enddate>200111</enddate><creator>Falter, James L.</creator><creator>Atkinson, M. J.</creator><creator>Langdon, Chris</creator><general>American Society of Limnology and Oceanography</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7SN</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H95</scope><scope>L.G</scope><scope>7TN</scope></search><sort><creationdate>200111</creationdate><title>Production-Respiration Relationships at Different Timescales within the Biosphere 2 Coral Reef Biome</title><author>Falter, James L. ; Atkinson, M. J. ; Langdon, Chris</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a5443-fd3c4bb9f7d9e390e03963fe1370867428f12c472fdd6af642960ff09984d1fd3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2001</creationdate><topic>Animal and plant ecology</topic><topic>Animal, plant and microbial ecology</topic><topic>Arcologies</topic><topic>Biological and medical sciences</topic><topic>Biomes</topic><topic>Coral reefs</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>Marine</topic><topic>Oceans</topic><topic>Reefs</topic><topic>Respiration</topic><topic>Sea water</topic><topic>Sea water ecosystems</topic><topic>Sensors</topic><topic>Statistical variance</topic><topic>Synecology</topic><topic>Time series</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Falter, James L.</creatorcontrib><creatorcontrib>Atkinson, M. J.</creatorcontrib><creatorcontrib>Langdon, Chris</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Aqualine</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><jtitle>Limnology and oceanography</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Falter, James L.</au><au>Atkinson, M. J.</au><au>Langdon, Chris</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Production-Respiration Relationships at Different Timescales within the Biosphere 2 Coral Reef Biome</atitle><jtitle>Limnology and oceanography</jtitle><date>2001-11</date><risdate>2001</risdate><volume>46</volume><issue>7</issue><spage>1653</spage><epage>1660</epage><pages>1653-1660</pages><issn>0024-3590</issn><eissn>1939-5590</eissn><coden>LIOCAH</coden><abstract>Temporal relationships between organic carbon production and respiration are not well understood in coral reef ecosystems. We monitored dissolved oxygen (O2) concentrations within the Biosphere 2 coral reef biome over a 3-yr period (1 January 1997-1 January 2000), to calculate daily rates of gross production (P), community respiration (R), and net community production (NCP). P averaged 170 mmol $O_2\>m^{-2}\>d^{-1}$, and R averaged 173 mmol $O_2\>m^{-2}\>d^{-1}$, which yielded a mean NCP of only -3 mmol $O_2\>m^{-2}\>d^{-1}$, or a difference of only 2%. This long-term balance between P and R reflects the closed-system design of the biome. The SD of P, however, was ±56 mmol $O_2\>m^{-2}\>d^{-1}$; that of R was ±47 mmol $O_2\>m^{-2}\>d^{-1}$; and that of NCP was ±26 mmol $O_2\>m^{-2}\>d^{-1}$ or ±15% of mean P. To better resolve the behavior of P, R, and NCP at different timescales, each of these time series were spectrally decomposed into four frequency bands that corresponded to four timescales: <1 week, 1 week-1 month, 1-3 months (subseasonal), and >3 months (seasonal to annual). At timescales >1 month, the variance of P was not different from the variance of R. At timescales of <1 month, the variance in P was significantly greater than the variance in R (P < 0.01). Furthermore, the correlation between changes in P and changes in R became weaker with decreasing timescale. We suggest that changes in P and R become well matched at timescales that coincide with the turnover of carbon by the dominant macroalgae within the biome (1-3 months). In addition, we conclude that measurements of NCP based on daily or weekly data sets are not good indicators of the long-term net metabolic performance of coral reefs.</abstract><cop>Waco, TX</cop><pub>American Society of Limnology and Oceanography</pub><doi>10.4319/lo.2001.46.7.1653</doi><tpages>8</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Animal and plant ecology Animal, plant and microbial ecology Arcologies Biological and medical sciences Biomes Coral reefs Fundamental and applied biological sciences. Psychology Marine Oceans Reefs Respiration Sea water Sea water ecosystems Sensors Statistical variance Synecology Time series |
title | Production-Respiration Relationships at Different Timescales within the Biosphere 2 Coral Reef Biome |
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