Carbon sequestration and storage in Norwegian Arctic coastal wetlands: Impacts of climate change

Coastal wetlands contain some of the largest stores of pedologic and biotic carbon pools, and climate change is likely to influence the ability of these ecosystems to sequester carbon. Recent studies have attempted to provide data on carbon sequestration in both temperate and tropical coastal wetlan...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:The Science of the total environment 2020-12, Vol.748, p.141343-141343, Article 141343
1. Verfasser: Ward, Raymond D.
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 141343
container_issue
container_start_page 141343
container_title The Science of the total environment
container_volume 748
creator Ward, Raymond D.
description Coastal wetlands contain some of the largest stores of pedologic and biotic carbon pools, and climate change is likely to influence the ability of these ecosystems to sequester carbon. Recent studies have attempted to provide data on carbon sequestration in both temperate and tropical coastal wetlands. Alteration of Arctic wetland carbon sequestration rates is also likely where coastal forcing mechanisms interact directly with these coastal systems. At present there are no data available to provide a detailed understanding of present day and historical carbon sequestration rates within Arctic coastal wetlands. In order to address this knowledge gap, rates of carbon sequestration were assessed within five Arctic coastal wetland sites in Norway. This was undertaken using radiometric dating techniques (210Pb and 137Cs) to establish a geochronology for recent wetland development, and soil carbon stocks were estimated from cores. Average carbon sequestration rates were varied, both between sites and over time, ranging between 19 and 603 g C m2 y−1, and these were correlated with increases in the length of the growing season. Stocks ranged between 3.67 and 13.79 Mg C ha−1, which is very low compared with global average estimations for similar coastal systems, e.g. 250 Mg C ha−1 for temperate salt marshes, 280 Mg C ha−1 for mangroves, and 140 Mg C ha−1 for seagrasses. This is most likely due to isostatic uplift and sediment accretion historically outpacing sea level rise, which results in wetland progradation and thus a continuous formation of new marsh with thin organic soil horizons. However, with increasing rates of sea level rise it is uncertain whether this trend is set to continue or be reversed. [Display omitted] •Arctic coastal wetlands store less carbon than global averages due to thin soils.•Carbon sequestration rates are similar to those of temperate salt marshes.•Extension of the growing season has resulted in increased carbon sequestration.
doi_str_mv 10.1016/j.scitotenv.2020.141343
format Article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_2435755778</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S0048969720348725</els_id><sourcerecordid>2435755778</sourcerecordid><originalsourceid>FETCH-LOGICAL-c397t-f9855d261770c202c821c207be1635641a6900b23da25c6c8e226bc7fe35b8213</originalsourceid><addsrcrecordid>eNqFkE9PwzAMxSMEEmPwGciRS0eStknLbZr4M2mCC5xD6rojU9eMJNvEtydjiCu-WLZ-tt57hFxzNuGMy9vVJICNLuKwmwgm0rbgeZGfkBGvVJ1xJuQpGTFWVFkta3VOLkJYsVSq4iPyPjO-cQMN-LnFEL2JNk1maGmIzpslUjvQZ-f3uLRmoFMP0QIFZ0I0Pd1j7BMb7uh8vTEQA3Udhd6uTUQKH2ZY4iU560wf8Oq3j8nbw_3r7ClbvDzOZ9NFBnmtYtbVVVm2QnKlGCQbUAmeumqQy7yUBTeyZqwReWtECRIqFEI2oDrMyyax-ZjcHP9uvPuxotc2APZJH7pt0KLIS1WWSlUJVUcUvAvBY6c3Pkn2X5ozfchUr_RfpvqQqT5mmi6nx0tMTnYW_YHDAbC1HiHq1tl_f3wDvUCEgw</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2435755778</pqid></control><display><type>article</type><title>Carbon sequestration and storage in Norwegian Arctic coastal wetlands: Impacts of climate change</title><source>Elsevier ScienceDirect Journals Complete</source><creator>Ward, Raymond D.</creator><creatorcontrib>Ward, Raymond D.</creatorcontrib><description>Coastal wetlands contain some of the largest stores of pedologic and biotic carbon pools, and climate change is likely to influence the ability of these ecosystems to sequester carbon. Recent studies have attempted to provide data on carbon sequestration in both temperate and tropical coastal wetlands. Alteration of Arctic wetland carbon sequestration rates is also likely where coastal forcing mechanisms interact directly with these coastal systems. At present there are no data available to provide a detailed understanding of present day and historical carbon sequestration rates within Arctic coastal wetlands. In order to address this knowledge gap, rates of carbon sequestration were assessed within five Arctic coastal wetland sites in Norway. This was undertaken using radiometric dating techniques (210Pb and 137Cs) to establish a geochronology for recent wetland development, and soil carbon stocks were estimated from cores. Average carbon sequestration rates were varied, both between sites and over time, ranging between 19 and 603 g C m2 y−1, and these were correlated with increases in the length of the growing season. Stocks ranged between 3.67 and 13.79 Mg C ha−1, which is very low compared with global average estimations for similar coastal systems, e.g. 250 Mg C ha−1 for temperate salt marshes, 280 Mg C ha−1 for mangroves, and 140 Mg C ha−1 for seagrasses. This is most likely due to isostatic uplift and sediment accretion historically outpacing sea level rise, which results in wetland progradation and thus a continuous formation of new marsh with thin organic soil horizons. However, with increasing rates of sea level rise it is uncertain whether this trend is set to continue or be reversed. [Display omitted] •Arctic coastal wetlands store less carbon than global averages due to thin soils.•Carbon sequestration rates are similar to those of temperate salt marshes.•Extension of the growing season has resulted in increased carbon sequestration.</description><identifier>ISSN: 0048-9697</identifier><identifier>EISSN: 1879-1026</identifier><identifier>DOI: 10.1016/j.scitotenv.2020.141343</identifier><language>eng</language><publisher>Elsevier B.V</publisher><subject>Blue carbon ; Climate mitigation ; Increased productivity ; Norway ; Salt marshes ; Sediment accretion</subject><ispartof>The Science of the total environment, 2020-12, Vol.748, p.141343-141343, Article 141343</ispartof><rights>2020 Elsevier B.V.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c397t-f9855d261770c202c821c207be1635641a6900b23da25c6c8e226bc7fe35b8213</citedby><cites>FETCH-LOGICAL-c397t-f9855d261770c202c821c207be1635641a6900b23da25c6c8e226bc7fe35b8213</cites><orcidid>0000-0002-7391-5530</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0048969720348725$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,776,780,3537,27901,27902,65534</link.rule.ids></links><search><creatorcontrib>Ward, Raymond D.</creatorcontrib><title>Carbon sequestration and storage in Norwegian Arctic coastal wetlands: Impacts of climate change</title><title>The Science of the total environment</title><description>Coastal wetlands contain some of the largest stores of pedologic and biotic carbon pools, and climate change is likely to influence the ability of these ecosystems to sequester carbon. Recent studies have attempted to provide data on carbon sequestration in both temperate and tropical coastal wetlands. Alteration of Arctic wetland carbon sequestration rates is also likely where coastal forcing mechanisms interact directly with these coastal systems. At present there are no data available to provide a detailed understanding of present day and historical carbon sequestration rates within Arctic coastal wetlands. In order to address this knowledge gap, rates of carbon sequestration were assessed within five Arctic coastal wetland sites in Norway. This was undertaken using radiometric dating techniques (210Pb and 137Cs) to establish a geochronology for recent wetland development, and soil carbon stocks were estimated from cores. Average carbon sequestration rates were varied, both between sites and over time, ranging between 19 and 603 g C m2 y−1, and these were correlated with increases in the length of the growing season. Stocks ranged between 3.67 and 13.79 Mg C ha−1, which is very low compared with global average estimations for similar coastal systems, e.g. 250 Mg C ha−1 for temperate salt marshes, 280 Mg C ha−1 for mangroves, and 140 Mg C ha−1 for seagrasses. This is most likely due to isostatic uplift and sediment accretion historically outpacing sea level rise, which results in wetland progradation and thus a continuous formation of new marsh with thin organic soil horizons. However, with increasing rates of sea level rise it is uncertain whether this trend is set to continue or be reversed. [Display omitted] •Arctic coastal wetlands store less carbon than global averages due to thin soils.•Carbon sequestration rates are similar to those of temperate salt marshes.•Extension of the growing season has resulted in increased carbon sequestration.</description><subject>Blue carbon</subject><subject>Climate mitigation</subject><subject>Increased productivity</subject><subject>Norway</subject><subject>Salt marshes</subject><subject>Sediment accretion</subject><issn>0048-9697</issn><issn>1879-1026</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNqFkE9PwzAMxSMEEmPwGciRS0eStknLbZr4M2mCC5xD6rojU9eMJNvEtydjiCu-WLZ-tt57hFxzNuGMy9vVJICNLuKwmwgm0rbgeZGfkBGvVJ1xJuQpGTFWVFkta3VOLkJYsVSq4iPyPjO-cQMN-LnFEL2JNk1maGmIzpslUjvQZ-f3uLRmoFMP0QIFZ0I0Pd1j7BMb7uh8vTEQA3Udhd6uTUQKH2ZY4iU560wf8Oq3j8nbw_3r7ClbvDzOZ9NFBnmtYtbVVVm2QnKlGCQbUAmeumqQy7yUBTeyZqwReWtECRIqFEI2oDrMyyax-ZjcHP9uvPuxotc2APZJH7pt0KLIS1WWSlUJVUcUvAvBY6c3Pkn2X5ozfchUr_RfpvqQqT5mmi6nx0tMTnYW_YHDAbC1HiHq1tl_f3wDvUCEgw</recordid><startdate>20201215</startdate><enddate>20201215</enddate><creator>Ward, Raymond D.</creator><general>Elsevier B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7X8</scope><orcidid>https://orcid.org/0000-0002-7391-5530</orcidid></search><sort><creationdate>20201215</creationdate><title>Carbon sequestration and storage in Norwegian Arctic coastal wetlands: Impacts of climate change</title><author>Ward, Raymond D.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c397t-f9855d261770c202c821c207be1635641a6900b23da25c6c8e226bc7fe35b8213</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Blue carbon</topic><topic>Climate mitigation</topic><topic>Increased productivity</topic><topic>Norway</topic><topic>Salt marshes</topic><topic>Sediment accretion</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Ward, Raymond D.</creatorcontrib><collection>CrossRef</collection><collection>MEDLINE - Academic</collection><jtitle>The Science of the total environment</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ward, Raymond D.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Carbon sequestration and storage in Norwegian Arctic coastal wetlands: Impacts of climate change</atitle><jtitle>The Science of the total environment</jtitle><date>2020-12-15</date><risdate>2020</risdate><volume>748</volume><spage>141343</spage><epage>141343</epage><pages>141343-141343</pages><artnum>141343</artnum><issn>0048-9697</issn><eissn>1879-1026</eissn><abstract>Coastal wetlands contain some of the largest stores of pedologic and biotic carbon pools, and climate change is likely to influence the ability of these ecosystems to sequester carbon. Recent studies have attempted to provide data on carbon sequestration in both temperate and tropical coastal wetlands. Alteration of Arctic wetland carbon sequestration rates is also likely where coastal forcing mechanisms interact directly with these coastal systems. At present there are no data available to provide a detailed understanding of present day and historical carbon sequestration rates within Arctic coastal wetlands. In order to address this knowledge gap, rates of carbon sequestration were assessed within five Arctic coastal wetland sites in Norway. This was undertaken using radiometric dating techniques (210Pb and 137Cs) to establish a geochronology for recent wetland development, and soil carbon stocks were estimated from cores. Average carbon sequestration rates were varied, both between sites and over time, ranging between 19 and 603 g C m2 y−1, and these were correlated with increases in the length of the growing season. Stocks ranged between 3.67 and 13.79 Mg C ha−1, which is very low compared with global average estimations for similar coastal systems, e.g. 250 Mg C ha−1 for temperate salt marshes, 280 Mg C ha−1 for mangroves, and 140 Mg C ha−1 for seagrasses. This is most likely due to isostatic uplift and sediment accretion historically outpacing sea level rise, which results in wetland progradation and thus a continuous formation of new marsh with thin organic soil horizons. However, with increasing rates of sea level rise it is uncertain whether this trend is set to continue or be reversed. [Display omitted] •Arctic coastal wetlands store less carbon than global averages due to thin soils.•Carbon sequestration rates are similar to those of temperate salt marshes.•Extension of the growing season has resulted in increased carbon sequestration.</abstract><pub>Elsevier B.V</pub><doi>10.1016/j.scitotenv.2020.141343</doi><tpages>1</tpages><orcidid>https://orcid.org/0000-0002-7391-5530</orcidid><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 0048-9697
ispartof The Science of the total environment, 2020-12, Vol.748, p.141343-141343, Article 141343
issn 0048-9697
1879-1026
language eng
recordid cdi_proquest_miscellaneous_2435755778
source Elsevier ScienceDirect Journals Complete
subjects Blue carbon
Climate mitigation
Increased productivity
Norway
Salt marshes
Sediment accretion
title Carbon sequestration and storage in Norwegian Arctic coastal wetlands: Impacts of climate change
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-20T20%3A23%3A40IST&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=Carbon%20sequestration%20and%20storage%20in%20Norwegian%20Arctic%20coastal%20wetlands:%20Impacts%20of%20climate%20change&rft.jtitle=The%20Science%20of%20the%20total%20environment&rft.au=Ward,%20Raymond%20D.&rft.date=2020-12-15&rft.volume=748&rft.spage=141343&rft.epage=141343&rft.pages=141343-141343&rft.artnum=141343&rft.issn=0048-9697&rft.eissn=1879-1026&rft_id=info:doi/10.1016/j.scitotenv.2020.141343&rft_dat=%3Cproquest_cross%3E2435755778%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=2435755778&rft_id=info:pmid/&rft_els_id=S0048969720348725&rfr_iscdi=true