{"refrec":{"BRefID":345038,"RR":"<b>Wilson, K.L.; Skinner, M.A.; Lotze, H.K.</b> (2019). Projected 21st‐century distribution of canopy‐forming seaweeds in the Northwest Atlantic with climate change. <i>Diversity Distrib. 25(4)</i>: 582-602. <a href=\"https://dx.doi.org/10.1111/ddi.12897\" target=\"_blank\">https://dx.doi.org/10.1111/ddi.12897</a>","BEntID":341673,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Diversity Distrib. 25(4)</i>: 582-602. <a href=\"https://dx.doi.org/10.1111/ddi.12897\" target=\"_blank\">https://dx.doi.org/10.1111/ddi.12897</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Wilson, K.L.; Skinner, M.A.; Lotze, H.K.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Wilson, K.L.; Skinner, M.A.; Lotze, H.K.","Englishabstract":"Aim</h3>                              <p>Climate change is predicted to alter the distribution and abundance of marine species, including canopy-forming seaweeds which provide important ecosystem functions and services. We asked whether continued warming will affect the distribution of six common canopy-forming species: mid-intertidal fucoids (<i>Ascophyllum nodosum,</i> <i>Fucus vesiculosus</i>), low-intertidal Irish moss (<i>Chondrus crispus</i>), subtidal laminarian kelps (<i>Saccharina latissima,</i> <i>Laminaria digitata</i>) and the invasive <i>Codium fragile</i>.</p>               </section>                        <section class=\"article-section__content\" id=\"ddi12897-sec-0002\">                              <h3 class=\"article-section__sub-title section1\" id=\"ddi12897-sec-0002-title\"> Location</h3>                              <p>Northwest Atlantic.</p>               </section>                        <section class=\"article-section__content\" id=\"ddi12897-sec-0003\">                              <h3 class=\"article-section__sub-title section1\" id=\"ddi12897-sec-0003-title\"> Methods</h3>                              <p>We used occurrence records and the correlative presence-only species distribution model <span class=\"smallCaps\">Maxent</span> to determine present-day distribution. This distribution was compared to each species’ warm-water physiological thresholds indicating areas of stable or reduced growth and mortality. Present-day models were then projected to mid-century (2040–2050) and end-century (2090–2100) using two contrasting carbon emission scenarios (RCP2.6 and 8.5) and two global climate models from CMIP5 based on changes in ocean temperatures.</p>               </section>                        <section class=\"article-section__content\" id=\"ddi12897-sec-0004\">                              <h3 class=\"article-section__sub-title section1\" id=\"ddi12897-sec-0004-title\"> Results</h3>                              <p>Projected range shifts were minimal under low emissions (RCP2.6), but substantial species-specific range shifts were projected under high emissions (RCP8.5), with all species except <i>C.&nbsp;fragile </i>predicted to experience a northward shift in their southern (warm) edge of ≤406&nbsp;km by the year 2100. Northward expansions outweighed southern extirpations for fucoids and <i>C.&nbsp;crispus </i>leading to overall range expansions, while range contractions were projected for kelps and <i>C.&nbsp;fragile. </i>Model projections generally agreed with physiological thresholds but were more conservative suggesting that range shifts for kelps may be underpredicted.</p>               </section>                        <section class=\"article-section__content\" id=\"ddi12897-sec-0005\">                              <h3 class=\"article-section__sub-title section1\" id=\"ddi12897-sec-0005-title\"> Main conclusions</h3>                              <p>Our results highlight the benefits to be gained from strong climate change mitigation (RCP2.6), which would limit changes in rocky shore community distribution and composition. The business-as-usual RCP8.5 scenario projected major range shifts, seaweed community reorganization and transitions in dominant species south of Newfoundland by 2100 (~47°N). As canopy-forming seaweeds provide essential habitat, carbon storage, nutrient cycling and commercial value, understanding their response to continued climate warming is critical to inform coastal management and conservation planning.</p>","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Projected 21st‐century distribution of canopy‐forming seaweeds in the Northwest Atlantic with climate change","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-11 01:32:48.166169","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2019,"MonPub":null,"DateUpdate":"2021-09-20","DateCreate":"2021-09-20","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000463154200008","VABBcode":null,"OpenAcc":1,"DOI":"10.1111/ddi.12897"},"refs":null,"anarec":{"AnaID":345038,"PubliDate":2019,"Pagination":"582-602","XtraPublOfAnaID":null,"ISBN":null,"Volume":"25","Issue":"4","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":99812,"SerRR":"Diversity and Distributions. 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