The effect of global change on soil phosphatase activity
Soil phosphatase enzymes are produced by plant roots and microorganisms and play a key role in the cycling of phosphorus (P), an often‐limiting element in terrestrial ecosystems. The production of these enzymes in soil is the most important biological strategy for acquiring phosphate ions from organ...
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creator | Margalef, Olga Sardans, Jordi Maspons, Joan Molowny‐Horas, Roberto Fernández‐Martínez, Marcos Janssens, Ivan A. Richter, Andreas Ciais, Philippe Obersteiner, Michael Peñuelas, Josep |
description | Soil phosphatase enzymes are produced by plant roots and microorganisms and play a key role in the cycling of phosphorus (P), an often‐limiting element in terrestrial ecosystems. The production of these enzymes in soil is the most important biological strategy for acquiring phosphate ions from organic molecules. Previous works showed how soil potential phosphatase activity is mainly driven by climatic conditions and soil nitrogen (N) and carbon. Nonetheless, future trends of the activity of these enzymes under global change remain little known. We investigated the influence of some of the main drivers of change on soil phosphatase activity using a meta‐analysis of results from 97 published studies. Our database included a compilation of N and P fertilization experiments, manipulation experiments with increased atmospheric CO2 concentration, warming, and drought, and studies comparing invaded and non‐invaded ecosystems. Our results indicate that N fertilization leads to higher phosphatase activity, whereas P fertilization has the opposite effect. The rise of atmospheric CO2 levels or the arrival of invasive species also exhibits positive response ratios on the activity of soil phosphatases. However, the occurrence of recurrent drought episodes decreases the activity of soil phosphatases. Our analysis did not reveal statistically significant effects of warming on soil phosphatase activity. In general, soil enzymatic changes in the reviewed experiments depended on the initial nutrient and water status of the ecosystems. The observed patterns evidence that future soil phosphatase activity will not only depend on present‐day soil conditions but also on potential compensations or amplifications among the different drivers of global change. The responses of soil phosphatases to the global change drivers reported in this study and the consideration of cost–benefit approaches based on the connection of the P and N cycle will be useful for a better estimation of phosphatase production in carbon (C)–N–P models.
We investigated the influence of the main drivers of global change on soil phosphatase activity using a meta‐analysis of results from 97 published studies. Our models indicated that an increased fertilization with nitrogen or atmospheric CO2, or the arrival of invasive species may all lead to higher phosphatase activities in the soil. Excessive phosphorus fertilization or increased drought, in contrast, typically decreases the activities of these enzymes. Warm |
doi_str_mv | 10.1111/gcb.15832 |
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We investigated the influence of the main drivers of global change on soil phosphatase activity using a meta‐analysis of results from 97 published studies. Our models indicated that an increased fertilization with nitrogen or atmospheric CO2, or the arrival of invasive species may all lead to higher phosphatase activities in the soil. Excessive phosphorus fertilization or increased drought, in contrast, typically decreases the activities of these enzymes. Warming was not found to induce consistent responses, depending on water and nutrient availability. The responses reported in this study are useful for a better estimation of phosphatase production in carbon–nitrogen–phosphorus models.</description><identifier>ISSN: 1354-1013</identifier><identifier>EISSN: 1365-2486</identifier><identifier>DOI: 10.1111/gcb.15832</identifier><identifier>PMID: 34383341</identifier><language>eng</language><publisher>Oxford: Blackwell Publishing Ltd</publisher><subject>atmospheric CO2 increment experiment ; Atmospheric models ; Biological fertilization ; Carbon dioxide ; Carbon dioxide concentration ; Climatic conditions ; Drought ; Ecosystems ; Environmental Sciences ; Enzymes ; Experiments ; Fertilization ; global change ; Global Changes ; Introduced species ; Invasive species ; Meta-analysis ; Microorganisms ; N and P fertilization ; Nitrogen ; Nutrient status ; Organic chemistry ; Phosphatase ; Phosphates ; Phosphorus ; phosphorus cycle ; Plant roots ; Soil ; Soil analysis ; Soil conditions ; soil phosphatase activity ; Soils ; Statistical analysis ; Terrestrial ecosystems</subject><ispartof>Global change biology, 2021-11, Vol.27 (22), p.5989-6003</ispartof><rights>2021 John Wiley & Sons Ltd</rights><rights>Copyright © 2021 John Wiley & Sons Ltd</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4302-13f353ef3173b0f086fb86f364e47302b49770999c9b467bbcb09f524ad90cdd3</citedby><cites>FETCH-LOGICAL-c4302-13f353ef3173b0f086fb86f364e47302b49770999c9b467bbcb09f524ad90cdd3</cites><orcidid>0000-0003-2286-8727 ; 0000-0002-5705-1787 ; 0000-0003-2478-0219 ; 0000-0002-5661-3610 ; 0000-0003-3282-4808 ; 0000-0001-6981-2769 ; 0000-0002-7215-0150 ; 0000-0001-8560-4943 ; 0000-0002-3036-3182 ; 0000-0003-2626-6379</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1111%2Fgcb.15832$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1111%2Fgcb.15832$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>230,314,776,780,881,1411,27901,27902,45550,45551</link.rule.ids><backlink>$$Uhttps://hal.science/hal-03434930$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Margalef, Olga</creatorcontrib><creatorcontrib>Sardans, Jordi</creatorcontrib><creatorcontrib>Maspons, Joan</creatorcontrib><creatorcontrib>Molowny‐Horas, Roberto</creatorcontrib><creatorcontrib>Fernández‐Martínez, Marcos</creatorcontrib><creatorcontrib>Janssens, Ivan A.</creatorcontrib><creatorcontrib>Richter, Andreas</creatorcontrib><creatorcontrib>Ciais, Philippe</creatorcontrib><creatorcontrib>Obersteiner, Michael</creatorcontrib><creatorcontrib>Peñuelas, Josep</creatorcontrib><title>The effect of global change on soil phosphatase activity</title><title>Global change biology</title><description>Soil phosphatase enzymes are produced by plant roots and microorganisms and play a key role in the cycling of phosphorus (P), an often‐limiting element in terrestrial ecosystems. The production of these enzymes in soil is the most important biological strategy for acquiring phosphate ions from organic molecules. Previous works showed how soil potential phosphatase activity is mainly driven by climatic conditions and soil nitrogen (N) and carbon. Nonetheless, future trends of the activity of these enzymes under global change remain little known. We investigated the influence of some of the main drivers of change on soil phosphatase activity using a meta‐analysis of results from 97 published studies. Our database included a compilation of N and P fertilization experiments, manipulation experiments with increased atmospheric CO2 concentration, warming, and drought, and studies comparing invaded and non‐invaded ecosystems. Our results indicate that N fertilization leads to higher phosphatase activity, whereas P fertilization has the opposite effect. The rise of atmospheric CO2 levels or the arrival of invasive species also exhibits positive response ratios on the activity of soil phosphatases. However, the occurrence of recurrent drought episodes decreases the activity of soil phosphatases. Our analysis did not reveal statistically significant effects of warming on soil phosphatase activity. In general, soil enzymatic changes in the reviewed experiments depended on the initial nutrient and water status of the ecosystems. The observed patterns evidence that future soil phosphatase activity will not only depend on present‐day soil conditions but also on potential compensations or amplifications among the different drivers of global change. The responses of soil phosphatases to the global change drivers reported in this study and the consideration of cost–benefit approaches based on the connection of the P and N cycle will be useful for a better estimation of phosphatase production in carbon (C)–N–P models.
We investigated the influence of the main drivers of global change on soil phosphatase activity using a meta‐analysis of results from 97 published studies. Our models indicated that an increased fertilization with nitrogen or atmospheric CO2, or the arrival of invasive species may all lead to higher phosphatase activities in the soil. Excessive phosphorus fertilization or increased drought, in contrast, typically decreases the activities of these enzymes. Warming was not found to induce consistent responses, depending on water and nutrient availability. The responses reported in this study are useful for a better estimation of phosphatase production in carbon–nitrogen–phosphorus models.</description><subject>atmospheric CO2 increment experiment</subject><subject>Atmospheric models</subject><subject>Biological fertilization</subject><subject>Carbon dioxide</subject><subject>Carbon dioxide concentration</subject><subject>Climatic conditions</subject><subject>Drought</subject><subject>Ecosystems</subject><subject>Environmental Sciences</subject><subject>Enzymes</subject><subject>Experiments</subject><subject>Fertilization</subject><subject>global change</subject><subject>Global Changes</subject><subject>Introduced species</subject><subject>Invasive species</subject><subject>Meta-analysis</subject><subject>Microorganisms</subject><subject>N and P fertilization</subject><subject>Nitrogen</subject><subject>Nutrient status</subject><subject>Organic chemistry</subject><subject>Phosphatase</subject><subject>Phosphates</subject><subject>Phosphorus</subject><subject>phosphorus cycle</subject><subject>Plant roots</subject><subject>Soil</subject><subject>Soil analysis</subject><subject>Soil conditions</subject><subject>soil phosphatase activity</subject><subject>Soils</subject><subject>Statistical analysis</subject><subject>Terrestrial ecosystems</subject><issn>1354-1013</issn><issn>1365-2486</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNp1kE1LAzEQhoMotlYP_oOAJw9bJzvZjxxr0VYoeKnnkKRJd8va1M220n9v6kpvDgwzDM-8zLyE3DMYsxhPa6PHLCsxvSBDhnmWpLzML099xhMGDAfkJoQNAGAK-TUZIMcSkbMhKZeVpdY5azrqHV03XquGmkpt15b6LQ2-buiu8mFXqU4FS5Xp6kPdHW_JlVNNsHd_dUQ-Xl-W03myeJ-9TSeLxHCENGHoMEPrkBWowUGZOx0Tc255EQHNRVGAEMIIzfNCa6NBuCzlaiXArFY4Io-9bqUauWvrT9UepVe1nE8W8jSD-AwXCAcW2Yee3bX-a29DJzd-327jeTLNSiZ4xqIFZ0XT-hBa686yDOTJTxn9lL9-RvapZ7_rxh7_B-Vs-txv_ACr_XGd</recordid><startdate>202111</startdate><enddate>202111</enddate><creator>Margalef, Olga</creator><creator>Sardans, Jordi</creator><creator>Maspons, Joan</creator><creator>Molowny‐Horas, Roberto</creator><creator>Fernández‐Martínez, Marcos</creator><creator>Janssens, Ivan A.</creator><creator>Richter, Andreas</creator><creator>Ciais, Philippe</creator><creator>Obersteiner, Michael</creator><creator>Peñuelas, Josep</creator><general>Blackwell Publishing Ltd</general><general>Wiley</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7SN</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H97</scope><scope>L.G</scope><scope>1XC</scope><orcidid>https://orcid.org/0000-0003-2286-8727</orcidid><orcidid>https://orcid.org/0000-0002-5705-1787</orcidid><orcidid>https://orcid.org/0000-0003-2478-0219</orcidid><orcidid>https://orcid.org/0000-0002-5661-3610</orcidid><orcidid>https://orcid.org/0000-0003-3282-4808</orcidid><orcidid>https://orcid.org/0000-0001-6981-2769</orcidid><orcidid>https://orcid.org/0000-0002-7215-0150</orcidid><orcidid>https://orcid.org/0000-0001-8560-4943</orcidid><orcidid>https://orcid.org/0000-0002-3036-3182</orcidid><orcidid>https://orcid.org/0000-0003-2626-6379</orcidid></search><sort><creationdate>202111</creationdate><title>The effect of global change on soil phosphatase activity</title><author>Margalef, Olga ; Sardans, Jordi ; Maspons, Joan ; Molowny‐Horas, Roberto ; Fernández‐Martínez, Marcos ; Janssens, Ivan A. ; Richter, Andreas ; Ciais, Philippe ; Obersteiner, Michael ; Peñuelas, Josep</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4302-13f353ef3173b0f086fb86f364e47302b49770999c9b467bbcb09f524ad90cdd3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>atmospheric CO2 increment experiment</topic><topic>Atmospheric models</topic><topic>Biological fertilization</topic><topic>Carbon dioxide</topic><topic>Carbon dioxide concentration</topic><topic>Climatic conditions</topic><topic>Drought</topic><topic>Ecosystems</topic><topic>Environmental Sciences</topic><topic>Enzymes</topic><topic>Experiments</topic><topic>Fertilization</topic><topic>global change</topic><topic>Global Changes</topic><topic>Introduced species</topic><topic>Invasive species</topic><topic>Meta-analysis</topic><topic>Microorganisms</topic><topic>N and P fertilization</topic><topic>Nitrogen</topic><topic>Nutrient status</topic><topic>Organic chemistry</topic><topic>Phosphatase</topic><topic>Phosphates</topic><topic>Phosphorus</topic><topic>phosphorus cycle</topic><topic>Plant roots</topic><topic>Soil</topic><topic>Soil analysis</topic><topic>Soil conditions</topic><topic>soil phosphatase activity</topic><topic>Soils</topic><topic>Statistical analysis</topic><topic>Terrestrial ecosystems</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Margalef, Olga</creatorcontrib><creatorcontrib>Sardans, Jordi</creatorcontrib><creatorcontrib>Maspons, Joan</creatorcontrib><creatorcontrib>Molowny‐Horas, Roberto</creatorcontrib><creatorcontrib>Fernández‐Martínez, Marcos</creatorcontrib><creatorcontrib>Janssens, Ivan A.</creatorcontrib><creatorcontrib>Richter, Andreas</creatorcontrib><creatorcontrib>Ciais, Philippe</creatorcontrib><creatorcontrib>Obersteiner, Michael</creatorcontrib><creatorcontrib>Peñuelas, Josep</creatorcontrib><collection>CrossRef</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) 3: Aquatic Pollution & Environmental Quality</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Hyper Article en Ligne (HAL)</collection><jtitle>Global change biology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Margalef, Olga</au><au>Sardans, Jordi</au><au>Maspons, Joan</au><au>Molowny‐Horas, Roberto</au><au>Fernández‐Martínez, Marcos</au><au>Janssens, Ivan A.</au><au>Richter, Andreas</au><au>Ciais, Philippe</au><au>Obersteiner, Michael</au><au>Peñuelas, Josep</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The effect of global change on soil phosphatase activity</atitle><jtitle>Global change biology</jtitle><date>2021-11</date><risdate>2021</risdate><volume>27</volume><issue>22</issue><spage>5989</spage><epage>6003</epage><pages>5989-6003</pages><issn>1354-1013</issn><eissn>1365-2486</eissn><abstract>Soil phosphatase enzymes are produced by plant roots and microorganisms and play a key role in the cycling of phosphorus (P), an often‐limiting element in terrestrial ecosystems. The production of these enzymes in soil is the most important biological strategy for acquiring phosphate ions from organic molecules. Previous works showed how soil potential phosphatase activity is mainly driven by climatic conditions and soil nitrogen (N) and carbon. Nonetheless, future trends of the activity of these enzymes under global change remain little known. We investigated the influence of some of the main drivers of change on soil phosphatase activity using a meta‐analysis of results from 97 published studies. Our database included a compilation of N and P fertilization experiments, manipulation experiments with increased atmospheric CO2 concentration, warming, and drought, and studies comparing invaded and non‐invaded ecosystems. Our results indicate that N fertilization leads to higher phosphatase activity, whereas P fertilization has the opposite effect. The rise of atmospheric CO2 levels or the arrival of invasive species also exhibits positive response ratios on the activity of soil phosphatases. However, the occurrence of recurrent drought episodes decreases the activity of soil phosphatases. Our analysis did not reveal statistically significant effects of warming on soil phosphatase activity. In general, soil enzymatic changes in the reviewed experiments depended on the initial nutrient and water status of the ecosystems. The observed patterns evidence that future soil phosphatase activity will not only depend on present‐day soil conditions but also on potential compensations or amplifications among the different drivers of global change. The responses of soil phosphatases to the global change drivers reported in this study and the consideration of cost–benefit approaches based on the connection of the P and N cycle will be useful for a better estimation of phosphatase production in carbon (C)–N–P models.
We investigated the influence of the main drivers of global change on soil phosphatase activity using a meta‐analysis of results from 97 published studies. Our models indicated that an increased fertilization with nitrogen or atmospheric CO2, or the arrival of invasive species may all lead to higher phosphatase activities in the soil. Excessive phosphorus fertilization or increased drought, in contrast, typically decreases the activities of these enzymes. Warming was not found to induce consistent responses, depending on water and nutrient availability. The responses reported in this study are useful for a better estimation of phosphatase production in carbon–nitrogen–phosphorus models.</abstract><cop>Oxford</cop><pub>Blackwell Publishing Ltd</pub><pmid>34383341</pmid><doi>10.1111/gcb.15832</doi><tpages>15</tpages><orcidid>https://orcid.org/0000-0003-2286-8727</orcidid><orcidid>https://orcid.org/0000-0002-5705-1787</orcidid><orcidid>https://orcid.org/0000-0003-2478-0219</orcidid><orcidid>https://orcid.org/0000-0002-5661-3610</orcidid><orcidid>https://orcid.org/0000-0003-3282-4808</orcidid><orcidid>https://orcid.org/0000-0001-6981-2769</orcidid><orcidid>https://orcid.org/0000-0002-7215-0150</orcidid><orcidid>https://orcid.org/0000-0001-8560-4943</orcidid><orcidid>https://orcid.org/0000-0002-3036-3182</orcidid><orcidid>https://orcid.org/0000-0003-2626-6379</orcidid></addata></record> |
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subjects | atmospheric CO2 increment experiment Atmospheric models Biological fertilization Carbon dioxide Carbon dioxide concentration Climatic conditions Drought Ecosystems Environmental Sciences Enzymes Experiments Fertilization global change Global Changes Introduced species Invasive species Meta-analysis Microorganisms N and P fertilization Nitrogen Nutrient status Organic chemistry Phosphatase Phosphates Phosphorus phosphorus cycle Plant roots Soil Soil analysis Soil conditions soil phosphatase activity Soils Statistical analysis Terrestrial ecosystems |
title | The effect of global change on soil phosphatase activity |
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