The effects of El Niño‐Southern Oscillation events on intertidal seagrass beds over a long‐term timescale
El Niño‐Southern Oscillation (ENSO) events can cause dramatic changes in marine communities. However, we know little as to how ENSO events affect tropical seagrass beds over decadal timescales. Therefore, a diverse array of seagrass (Thalassia hemprichii) habitat types were surveyed once every 3 mon...
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Veröffentlicht in: | Global change biology 2018-10, Vol.24 (10), p.4566-4580 |
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description | El Niño‐Southern Oscillation (ENSO) events can cause dramatic changes in marine communities. However, we know little as to how ENSO events affect tropical seagrass beds over decadal timescales. Therefore, a diverse array of seagrass (Thalassia hemprichii) habitat types were surveyed once every 3 months for 16 years (January 2001 to February 2017) in a tropical intertidal zone that is regularly affected by both ENSO events and anthropogenic nutrient enrichment. La Niña and El Niño events had distinct effects on the biomass and growth of T. hemprichii. During La Niña years, higher (a) precipitation levels and (b) seawater nitrogen concentrations led to increases in seagrass leaf productivity, canopy height, and biomass. However, the latter simultaneously stimulated the growth of periphyton on seagrass leaves; this led to decreases in seagrass cover and shoot density. More frequent La Niña events could, then, eventually lead to either a decline in intertidal seagrass beds or a shift to another, less drought‐resistant seagrass species in those regions already characterized by eutrophication due to local anthropogenic activity.
La Niña and El Niño events had distinct effects on the biomass and growth of the seagrass Thalassia hemprichii. During La Niña years, higher precipitation levels and seawater nitrogen concentrations led to increase in leaf productivity, canopy height, and biomass. However, the latter simultaneously stimulated the growth of periphyton on seagrass leaves; this led to decreases in seagrass cover and shoot density. More frequent La Niña events could, then, eventually lead to either a decline in intertidal seagrass beds or a shift to another, less drought‐resistant seagrass species in those regions already characterized by eutrophication due to local anthropogenic activity. |
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La Niña and El Niño events had distinct effects on the biomass and growth of the seagrass Thalassia hemprichii. During La Niña years, higher precipitation levels and seawater nitrogen concentrations led to increase in leaf productivity, canopy height, and biomass. However, the latter simultaneously stimulated the growth of periphyton on seagrass leaves; this led to decreases in seagrass cover and shoot density. More frequent La Niña events could, then, eventually lead to either a decline in intertidal seagrass beds or a shift to another, less drought‐resistant seagrass species in those regions already characterized by eutrophication due to local anthropogenic activity.</description><identifier>ISSN: 1354-1013</identifier><identifier>EISSN: 1365-2486</identifier><identifier>DOI: 10.1111/gcb.14404</identifier><identifier>PMID: 30030884</identifier><language>eng</language><publisher>England: Blackwell Publishing Ltd</publisher><subject>Anthropogenic factors ; Biomass ; Drought ; Ecosystem ; El Nino ; El Nino phenomena ; El Nino-Southern Oscillation ; ENSO ; Eutrophication ; Grasses ; Halodule uninervis ; Hydrocharitaceae - physiology ; Intertidal environment ; Intertidal zone ; La Nina ; La Niña ; Leaves ; Mineral nutrients ; Nitrogen - analysis ; Nutrient enrichment ; Ocean currents ; Periphyton ; Plant cover ; Plant Leaves ; Sea grasses ; Seawater ; Seawater - chemistry ; Southern Oscillation ; Thalassia hemprichii ; Tropical climate</subject><ispartof>Global change biology, 2018-10, Vol.24 (10), p.4566-4580</ispartof><rights>2018 John Wiley & Sons Ltd</rights><rights>2018 John Wiley & Sons Ltd.</rights><rights>Copyright © 2018 John Wiley & Sons Ltd</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4194-51ca037489642048bf3cdbd860e8a620f406149894cef6668a5b33d3d183aacd3</citedby><cites>FETCH-LOGICAL-c4194-51ca037489642048bf3cdbd860e8a620f406149894cef6668a5b33d3d183aacd3</cites><orcidid>0000-0001-8322-7195 ; 0000-0003-4644-1779</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.14404$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1111%2Fgcb.14404$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1417,27924,27925,45574,45575</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/30030884$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Lin, Hsing‐Juh</creatorcontrib><creatorcontrib>Lee, Chen‐Lu</creatorcontrib><creatorcontrib>Peng, Shang‐En</creatorcontrib><creatorcontrib>Hung, Meng‐Chi</creatorcontrib><creatorcontrib>Liu, Pi‐Jen</creatorcontrib><creatorcontrib>Mayfield, Anderson B.</creatorcontrib><title>The effects of El Niño‐Southern Oscillation events on intertidal seagrass beds over a long‐term timescale</title><title>Global change biology</title><addtitle>Glob Chang Biol</addtitle><description>El Niño‐Southern Oscillation (ENSO) events can cause dramatic changes in marine communities. However, we know little as to how ENSO events affect tropical seagrass beds over decadal timescales. Therefore, a diverse array of seagrass (Thalassia hemprichii) habitat types were surveyed once every 3 months for 16 years (January 2001 to February 2017) in a tropical intertidal zone that is regularly affected by both ENSO events and anthropogenic nutrient enrichment. La Niña and El Niño events had distinct effects on the biomass and growth of T. hemprichii. During La Niña years, higher (a) precipitation levels and (b) seawater nitrogen concentrations led to increases in seagrass leaf productivity, canopy height, and biomass. However, the latter simultaneously stimulated the growth of periphyton on seagrass leaves; this led to decreases in seagrass cover and shoot density. More frequent La Niña events could, then, eventually lead to either a decline in intertidal seagrass beds or a shift to another, less drought‐resistant seagrass species in those regions already characterized by eutrophication due to local anthropogenic activity.
La Niña and El Niño events had distinct effects on the biomass and growth of the seagrass Thalassia hemprichii. During La Niña years, higher precipitation levels and seawater nitrogen concentrations led to increase in leaf productivity, canopy height, and biomass. However, the latter simultaneously stimulated the growth of periphyton on seagrass leaves; this led to decreases in seagrass cover and shoot density. More frequent La Niña events could, then, eventually lead to either a decline in intertidal seagrass beds or a shift to another, less drought‐resistant seagrass species in those regions already characterized by eutrophication due to local anthropogenic activity.</description><subject>Anthropogenic factors</subject><subject>Biomass</subject><subject>Drought</subject><subject>Ecosystem</subject><subject>El Nino</subject><subject>El Nino phenomena</subject><subject>El Nino-Southern Oscillation</subject><subject>ENSO</subject><subject>Eutrophication</subject><subject>Grasses</subject><subject>Halodule uninervis</subject><subject>Hydrocharitaceae - physiology</subject><subject>Intertidal environment</subject><subject>Intertidal zone</subject><subject>La Nina</subject><subject>La Niña</subject><subject>Leaves</subject><subject>Mineral nutrients</subject><subject>Nitrogen - analysis</subject><subject>Nutrient enrichment</subject><subject>Ocean currents</subject><subject>Periphyton</subject><subject>Plant cover</subject><subject>Plant Leaves</subject><subject>Sea grasses</subject><subject>Seawater</subject><subject>Seawater - chemistry</subject><subject>Southern Oscillation</subject><subject>Thalassia hemprichii</subject><subject>Tropical climate</subject><issn>1354-1013</issn><issn>1365-2486</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><sourceid>EIF</sourceid><recordid>eNp10U1O3DAYBmCrKuoA7YILVJa6KYuA_-JxlmU0_EgIFqVry3G-DB4lNrUTqtlxBK7CGbgJJ8HDQBdIeONP8qNXtl-E9ig5oHkdLmx9QIUg4hPaplyWBRNKfl7PpSgooXyCdlJaEkI4I_ILmvA8EaXENvJX14ChbcEOCYcWzzt84R4fwtPd_e8wDtcQPb5M1nWdGVzwGG7Br6XHzg8QB9eYDicwi2hSwjU0-ewWIja4C36RUzLq8eB6SNZ08BVttaZL8O1130V_judXs9Pi_PLkbPbrvLCCVqIoqTWET4WqpGBEqLrltqkbJQkoIxlpBZFUVKoSFloppTJlzXnDG6q4Mbbhu-jnJvcmhr8jpEH3LlnIr_AQxqQZmXLOBGEs0x_v6DKM0efbaUZpNlNRlVntb5SNIaUIrb6JrjdxpSnR6xJ0LkG_lJDt99fEse6h-S_ffj2Dww345zpYfZykT2ZHm8hnUV6SKw</recordid><startdate>201810</startdate><enddate>201810</enddate><creator>Lin, Hsing‐Juh</creator><creator>Lee, Chen‐Lu</creator><creator>Peng, Shang‐En</creator><creator>Hung, Meng‐Chi</creator><creator>Liu, Pi‐Jen</creator><creator>Mayfield, Anderson B.</creator><general>Blackwell Publishing Ltd</general><scope>CGR</scope><scope>CUY</scope><scope>CVF</scope><scope>ECM</scope><scope>EIF</scope><scope>NPM</scope><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>7X8</scope><orcidid>https://orcid.org/0000-0001-8322-7195</orcidid><orcidid>https://orcid.org/0000-0003-4644-1779</orcidid></search><sort><creationdate>201810</creationdate><title>The effects of El Niño‐Southern Oscillation events on intertidal seagrass beds over a long‐term timescale</title><author>Lin, Hsing‐Juh ; Lee, Chen‐Lu ; Peng, Shang‐En ; Hung, Meng‐Chi ; Liu, Pi‐Jen ; Mayfield, Anderson B.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4194-51ca037489642048bf3cdbd860e8a620f406149894cef6668a5b33d3d183aacd3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>Anthropogenic factors</topic><topic>Biomass</topic><topic>Drought</topic><topic>Ecosystem</topic><topic>El Nino</topic><topic>El Nino phenomena</topic><topic>El Nino-Southern Oscillation</topic><topic>ENSO</topic><topic>Eutrophication</topic><topic>Grasses</topic><topic>Halodule uninervis</topic><topic>Hydrocharitaceae - physiology</topic><topic>Intertidal environment</topic><topic>Intertidal zone</topic><topic>La Nina</topic><topic>La Niña</topic><topic>Leaves</topic><topic>Mineral nutrients</topic><topic>Nitrogen - analysis</topic><topic>Nutrient enrichment</topic><topic>Ocean currents</topic><topic>Periphyton</topic><topic>Plant cover</topic><topic>Plant Leaves</topic><topic>Sea grasses</topic><topic>Seawater</topic><topic>Seawater - chemistry</topic><topic>Southern Oscillation</topic><topic>Thalassia hemprichii</topic><topic>Tropical climate</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Lin, Hsing‐Juh</creatorcontrib><creatorcontrib>Lee, Chen‐Lu</creatorcontrib><creatorcontrib>Peng, Shang‐En</creatorcontrib><creatorcontrib>Hung, Meng‐Chi</creatorcontrib><creatorcontrib>Liu, Pi‐Jen</creatorcontrib><creatorcontrib>Mayfield, Anderson B.</creatorcontrib><collection>Medline</collection><collection>MEDLINE</collection><collection>MEDLINE (Ovid)</collection><collection>MEDLINE</collection><collection>MEDLINE</collection><collection>PubMed</collection><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>MEDLINE - Academic</collection><jtitle>Global change biology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Lin, Hsing‐Juh</au><au>Lee, Chen‐Lu</au><au>Peng, Shang‐En</au><au>Hung, Meng‐Chi</au><au>Liu, Pi‐Jen</au><au>Mayfield, Anderson B.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The effects of El Niño‐Southern Oscillation events on intertidal seagrass beds over a long‐term timescale</atitle><jtitle>Global change biology</jtitle><addtitle>Glob Chang Biol</addtitle><date>2018-10</date><risdate>2018</risdate><volume>24</volume><issue>10</issue><spage>4566</spage><epage>4580</epage><pages>4566-4580</pages><issn>1354-1013</issn><eissn>1365-2486</eissn><abstract>El Niño‐Southern Oscillation (ENSO) events can cause dramatic changes in marine communities. However, we know little as to how ENSO events affect tropical seagrass beds over decadal timescales. Therefore, a diverse array of seagrass (Thalassia hemprichii) habitat types were surveyed once every 3 months for 16 years (January 2001 to February 2017) in a tropical intertidal zone that is regularly affected by both ENSO events and anthropogenic nutrient enrichment. La Niña and El Niño events had distinct effects on the biomass and growth of T. hemprichii. During La Niña years, higher (a) precipitation levels and (b) seawater nitrogen concentrations led to increases in seagrass leaf productivity, canopy height, and biomass. However, the latter simultaneously stimulated the growth of periphyton on seagrass leaves; this led to decreases in seagrass cover and shoot density. More frequent La Niña events could, then, eventually lead to either a decline in intertidal seagrass beds or a shift to another, less drought‐resistant seagrass species in those regions already characterized by eutrophication due to local anthropogenic activity.
La Niña and El Niño events had distinct effects on the biomass and growth of the seagrass Thalassia hemprichii. During La Niña years, higher precipitation levels and seawater nitrogen concentrations led to increase in leaf productivity, canopy height, and biomass. However, the latter simultaneously stimulated the growth of periphyton on seagrass leaves; this led to decreases in seagrass cover and shoot density. More frequent La Niña events could, then, eventually lead to either a decline in intertidal seagrass beds or a shift to another, less drought‐resistant seagrass species in those regions already characterized by eutrophication due to local anthropogenic activity.</abstract><cop>England</cop><pub>Blackwell Publishing Ltd</pub><pmid>30030884</pmid><doi>10.1111/gcb.14404</doi><tpages>16</tpages><orcidid>https://orcid.org/0000-0001-8322-7195</orcidid><orcidid>https://orcid.org/0000-0003-4644-1779</orcidid></addata></record> |
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subjects | Anthropogenic factors Biomass Drought Ecosystem El Nino El Nino phenomena El Nino-Southern Oscillation ENSO Eutrophication Grasses Halodule uninervis Hydrocharitaceae - physiology Intertidal environment Intertidal zone La Nina La Niña Leaves Mineral nutrients Nitrogen - analysis Nutrient enrichment Ocean currents Periphyton Plant cover Plant Leaves Sea grasses Seawater Seawater - chemistry Southern Oscillation Thalassia hemprichii Tropical climate |
title | The effects of El Niño‐Southern Oscillation events on intertidal seagrass beds over a long‐term timescale |
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