Temperature influence on phytoplankton community growth rates
A large database of field estimates of phytoplankton community growth rates in natural populations was compiled and analyzed to determine the apparent temperature effect on phytoplankton community growth rate. We conducted an ordinary least squares regression to optimize the parameters in two common...
Gespeichert in:
Veröffentlicht in: | Global biogeochemical cycles 2016-04, Vol.30 (4), p.550-559 |
---|---|
Hauptverfasser: | , , , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | 559 |
---|---|
container_issue | 4 |
container_start_page | 550 |
container_title | Global biogeochemical cycles |
container_volume | 30 |
creator | Sherman, Elliot Moore, J. Keith Primeau, Francois Tanouye, David |
description | A large database of field estimates of phytoplankton community growth rates in natural populations was compiled and analyzed to determine the apparent temperature effect on phytoplankton community growth rate. We conducted an ordinary least squares regression to optimize the parameters in two commonly used growth‐temperature relations (Arrhenius and Q10 models). Both equations fit the observational data equally with the optimized parameter values. The optimum apparent Q10 value was 1.47 ± 0.08 (95% confidence interval, CI). Microzooplankton grazing rates closely matched the temperature trends for phytoplankton growth. This likely reflects a dynamic adjustment of biomass and grazing rates by the microzooplankton to match their available food source, illustrating tight coupling of phytoplankton growth and microzooplankton grazing rates. The field‐measured temperature effect and growth rates were compared with estimates from the satellite Carbon‐based Productivity Model (CbPM) and three Earth System Models (ESMs), with model output extracted at the same month and sampling locations as the observations. The optimized, apparent Q10 value calculated for the CbPM was 1.51, with overestimation of growth rates. The apparent Q10 value in the Community Earth System Model (V1.0) was 1.65, with modest underestimation of growth rates. The GFDL‐ESM2M and GFDL‐ESM2G models produced apparent Q10 values of 1.52 and 1.39, respectively. Models with an apparent Q10 that is significantly greater than ~1.5 will overestimate the phytoplankton community growth response to the ongoing climate warming and will have spatial biases in estimated growth rates for the current era.
Key Points
Estimations of Q10 and Arrhenius equation parameters were made using field‐measured phytoplankton community growth rates
The Arrhenius and Q10 equations do an equally good job of estimating the temperature dependence of phytoplankton community growth rates
The optimal apparent Q10 value is 1.5. Models should capture a community growth‐temperature response equal to this value to avoid bias |
doi_str_mv | 10.1002/2015GB005272 |
format | Article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_1790970669</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>4046937001</sourcerecordid><originalsourceid>FETCH-LOGICAL-a5097-929750bb77bbcfd29a793ab573310d1f48c8189a1194f3d9be5c685ee00223a83</originalsourceid><addsrcrecordid>eNp9kD1PwzAQhi0EEqWw8QMisTBQOH_F9sBAKyhIlVjKHDnphaYkcbATVfn3GJUBMTCdTnru7rmXkEsKtxSA3TGgcjkHkEyxIzKhRoiZYUwckwlonc5SxtNTchbCDoAKKc2E3K-x6dDbfvCYVG1ZD9gWmLg26bZj77rath997ArXNENb9WPy7t2-3yZxBMM5OSltHfDip07J29PjevE8W70uXxYPq5mVYFR0MEpCniuV50W5YcYqw20uFecUNrQUutBUG0ujcck3JkdZpFoixqcYt5pPyfVhb-fd54Chz5oqFFhHO3RDyKgy8Q6kqYno1R905wbfRrtIaUVFKiSL1M2BKrwLwWOZdb5qrB8zCtl3ltnvLCPODvi-qnH8l82W8wUDAYp_AVFlc6Q</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1787146452</pqid></control><display><type>article</type><title>Temperature influence on phytoplankton community growth rates</title><source>Wiley Free Content</source><source>Wiley-Blackwell AGU Digital Library</source><source>EZB-FREE-00999 freely available EZB journals</source><source>Wiley Online Library All Journals</source><creator>Sherman, Elliot ; Moore, J. Keith ; Primeau, Francois ; Tanouye, David</creator><creatorcontrib>Sherman, Elliot ; Moore, J. Keith ; Primeau, Francois ; Tanouye, David</creatorcontrib><description>A large database of field estimates of phytoplankton community growth rates in natural populations was compiled and analyzed to determine the apparent temperature effect on phytoplankton community growth rate. We conducted an ordinary least squares regression to optimize the parameters in two commonly used growth‐temperature relations (Arrhenius and Q10 models). Both equations fit the observational data equally with the optimized parameter values. The optimum apparent Q10 value was 1.47 ± 0.08 (95% confidence interval, CI). Microzooplankton grazing rates closely matched the temperature trends for phytoplankton growth. This likely reflects a dynamic adjustment of biomass and grazing rates by the microzooplankton to match their available food source, illustrating tight coupling of phytoplankton growth and microzooplankton grazing rates. The field‐measured temperature effect and growth rates were compared with estimates from the satellite Carbon‐based Productivity Model (CbPM) and three Earth System Models (ESMs), with model output extracted at the same month and sampling locations as the observations. The optimized, apparent Q10 value calculated for the CbPM was 1.51, with overestimation of growth rates. The apparent Q10 value in the Community Earth System Model (V1.0) was 1.65, with modest underestimation of growth rates. The GFDL‐ESM2M and GFDL‐ESM2G models produced apparent Q10 values of 1.52 and 1.39, respectively. Models with an apparent Q10 that is significantly greater than ~1.5 will overestimate the phytoplankton community growth response to the ongoing climate warming and will have spatial biases in estimated growth rates for the current era.
Key Points
Estimations of Q10 and Arrhenius equation parameters were made using field‐measured phytoplankton community growth rates
The Arrhenius and Q10 equations do an equally good job of estimating the temperature dependence of phytoplankton community growth rates
The optimal apparent Q10 value is 1.5. Models should capture a community growth‐temperature response equal to this value to avoid bias</description><identifier>ISSN: 0886-6236</identifier><identifier>EISSN: 1944-9224</identifier><identifier>DOI: 10.1002/2015GB005272</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Algae ; Arrhenius ; Climate change ; Global warming ; Grazing ; Growth rate ; growth rates ; Natural populations ; Ocean temperature ; Phytoplankton ; phytoplankton growth ; Plankton ; Plant growth ; Q10 ; Temperature effects</subject><ispartof>Global biogeochemical cycles, 2016-04, Vol.30 (4), p.550-559</ispartof><rights>2016. American Geophysical Union. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a5097-929750bb77bbcfd29a793ab573310d1f48c8189a1194f3d9be5c685ee00223a83</citedby><cites>FETCH-LOGICAL-a5097-929750bb77bbcfd29a793ab573310d1f48c8189a1194f3d9be5c685ee00223a83</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1002%2F2015GB005272$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1002%2F2015GB005272$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1416,1432,11513,27923,27924,45573,45574,46408,46467,46832,46891</link.rule.ids></links><search><creatorcontrib>Sherman, Elliot</creatorcontrib><creatorcontrib>Moore, J. Keith</creatorcontrib><creatorcontrib>Primeau, Francois</creatorcontrib><creatorcontrib>Tanouye, David</creatorcontrib><title>Temperature influence on phytoplankton community growth rates</title><title>Global biogeochemical cycles</title><description>A large database of field estimates of phytoplankton community growth rates in natural populations was compiled and analyzed to determine the apparent temperature effect on phytoplankton community growth rate. We conducted an ordinary least squares regression to optimize the parameters in two commonly used growth‐temperature relations (Arrhenius and Q10 models). Both equations fit the observational data equally with the optimized parameter values. The optimum apparent Q10 value was 1.47 ± 0.08 (95% confidence interval, CI). Microzooplankton grazing rates closely matched the temperature trends for phytoplankton growth. This likely reflects a dynamic adjustment of biomass and grazing rates by the microzooplankton to match their available food source, illustrating tight coupling of phytoplankton growth and microzooplankton grazing rates. The field‐measured temperature effect and growth rates were compared with estimates from the satellite Carbon‐based Productivity Model (CbPM) and three Earth System Models (ESMs), with model output extracted at the same month and sampling locations as the observations. The optimized, apparent Q10 value calculated for the CbPM was 1.51, with overestimation of growth rates. The apparent Q10 value in the Community Earth System Model (V1.0) was 1.65, with modest underestimation of growth rates. The GFDL‐ESM2M and GFDL‐ESM2G models produced apparent Q10 values of 1.52 and 1.39, respectively. Models with an apparent Q10 that is significantly greater than ~1.5 will overestimate the phytoplankton community growth response to the ongoing climate warming and will have spatial biases in estimated growth rates for the current era.
Key Points
Estimations of Q10 and Arrhenius equation parameters were made using field‐measured phytoplankton community growth rates
The Arrhenius and Q10 equations do an equally good job of estimating the temperature dependence of phytoplankton community growth rates
The optimal apparent Q10 value is 1.5. Models should capture a community growth‐temperature response equal to this value to avoid bias</description><subject>Algae</subject><subject>Arrhenius</subject><subject>Climate change</subject><subject>Global warming</subject><subject>Grazing</subject><subject>Growth rate</subject><subject>growth rates</subject><subject>Natural populations</subject><subject>Ocean temperature</subject><subject>Phytoplankton</subject><subject>phytoplankton growth</subject><subject>Plankton</subject><subject>Plant growth</subject><subject>Q10</subject><subject>Temperature effects</subject><issn>0886-6236</issn><issn>1944-9224</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><recordid>eNp9kD1PwzAQhi0EEqWw8QMisTBQOH_F9sBAKyhIlVjKHDnphaYkcbATVfn3GJUBMTCdTnru7rmXkEsKtxSA3TGgcjkHkEyxIzKhRoiZYUwckwlonc5SxtNTchbCDoAKKc2E3K-x6dDbfvCYVG1ZD9gWmLg26bZj77rath997ArXNENb9WPy7t2-3yZxBMM5OSltHfDip07J29PjevE8W70uXxYPq5mVYFR0MEpCniuV50W5YcYqw20uFecUNrQUutBUG0ujcck3JkdZpFoixqcYt5pPyfVhb-fd54Chz5oqFFhHO3RDyKgy8Q6kqYno1R905wbfRrtIaUVFKiSL1M2BKrwLwWOZdb5qrB8zCtl3ltnvLCPODvi-qnH8l82W8wUDAYp_AVFlc6Q</recordid><startdate>201604</startdate><enddate>201604</enddate><creator>Sherman, Elliot</creator><creator>Moore, J. Keith</creator><creator>Primeau, Francois</creator><creator>Tanouye, David</creator><general>Blackwell Publishing Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7SN</scope><scope>7TG</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>7UA</scope><scope>M7N</scope></search><sort><creationdate>201604</creationdate><title>Temperature influence on phytoplankton community growth rates</title><author>Sherman, Elliot ; Moore, J. Keith ; Primeau, Francois ; Tanouye, David</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a5097-929750bb77bbcfd29a793ab573310d1f48c8189a1194f3d9be5c685ee00223a83</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Algae</topic><topic>Arrhenius</topic><topic>Climate change</topic><topic>Global warming</topic><topic>Grazing</topic><topic>Growth rate</topic><topic>growth rates</topic><topic>Natural populations</topic><topic>Ocean temperature</topic><topic>Phytoplankton</topic><topic>phytoplankton growth</topic><topic>Plankton</topic><topic>Plant growth</topic><topic>Q10</topic><topic>Temperature effects</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Sherman, Elliot</creatorcontrib><creatorcontrib>Moore, J. Keith</creatorcontrib><creatorcontrib>Primeau, Francois</creatorcontrib><creatorcontrib>Tanouye, David</creatorcontrib><collection>CrossRef</collection><collection>Ecology Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Water Resources Abstracts</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><jtitle>Global biogeochemical cycles</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Sherman, Elliot</au><au>Moore, J. Keith</au><au>Primeau, Francois</au><au>Tanouye, David</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Temperature influence on phytoplankton community growth rates</atitle><jtitle>Global biogeochemical cycles</jtitle><date>2016-04</date><risdate>2016</risdate><volume>30</volume><issue>4</issue><spage>550</spage><epage>559</epage><pages>550-559</pages><issn>0886-6236</issn><eissn>1944-9224</eissn><abstract>A large database of field estimates of phytoplankton community growth rates in natural populations was compiled and analyzed to determine the apparent temperature effect on phytoplankton community growth rate. We conducted an ordinary least squares regression to optimize the parameters in two commonly used growth‐temperature relations (Arrhenius and Q10 models). Both equations fit the observational data equally with the optimized parameter values. The optimum apparent Q10 value was 1.47 ± 0.08 (95% confidence interval, CI). Microzooplankton grazing rates closely matched the temperature trends for phytoplankton growth. This likely reflects a dynamic adjustment of biomass and grazing rates by the microzooplankton to match their available food source, illustrating tight coupling of phytoplankton growth and microzooplankton grazing rates. The field‐measured temperature effect and growth rates were compared with estimates from the satellite Carbon‐based Productivity Model (CbPM) and three Earth System Models (ESMs), with model output extracted at the same month and sampling locations as the observations. The optimized, apparent Q10 value calculated for the CbPM was 1.51, with overestimation of growth rates. The apparent Q10 value in the Community Earth System Model (V1.0) was 1.65, with modest underestimation of growth rates. The GFDL‐ESM2M and GFDL‐ESM2G models produced apparent Q10 values of 1.52 and 1.39, respectively. Models with an apparent Q10 that is significantly greater than ~1.5 will overestimate the phytoplankton community growth response to the ongoing climate warming and will have spatial biases in estimated growth rates for the current era.
Key Points
Estimations of Q10 and Arrhenius equation parameters were made using field‐measured phytoplankton community growth rates
The Arrhenius and Q10 equations do an equally good job of estimating the temperature dependence of phytoplankton community growth rates
The optimal apparent Q10 value is 1.5. Models should capture a community growth‐temperature response equal to this value to avoid bias</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1002/2015GB005272</doi><tpages>10</tpages><oa>free_for_read</oa></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0886-6236 |
ispartof | Global biogeochemical cycles, 2016-04, Vol.30 (4), p.550-559 |
issn | 0886-6236 1944-9224 |
language | eng |
recordid | cdi_proquest_miscellaneous_1790970669 |
source | Wiley Free Content; Wiley-Blackwell AGU Digital Library; EZB-FREE-00999 freely available EZB journals; Wiley Online Library All Journals |
subjects | Algae Arrhenius Climate change Global warming Grazing Growth rate growth rates Natural populations Ocean temperature Phytoplankton phytoplankton growth Plankton Plant growth Q10 Temperature effects |
title | Temperature influence on phytoplankton community growth rates |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-11T07%3A20%3A58IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Temperature%20influence%20on%20phytoplankton%20community%20growth%20rates&rft.jtitle=Global%20biogeochemical%20cycles&rft.au=Sherman,%20Elliot&rft.date=2016-04&rft.volume=30&rft.issue=4&rft.spage=550&rft.epage=559&rft.pages=550-559&rft.issn=0886-6236&rft.eissn=1944-9224&rft_id=info:doi/10.1002/2015GB005272&rft_dat=%3Cproquest_cross%3E4046937001%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1787146452&rft_id=info:pmid/&rfr_iscdi=true |