2008
DOI: 10.3354/cr00768
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Abstract: Warming of the planet has accelerated in recent years and is predicted to continue over the next 50 to 100 yr. Evidence of responses to present warming in marine ecosystems include shifts in the geographic range of species as well as in the composition of pelagic and demersal fish, benthic and intertidal assemblages. Here we provide a review of the changes in geographic distributions and population abundance of species detected on rocky shores of the NE Atlantic over the last 60 yr. This period encompassed the… Show more

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Cited by 226 publications
(184 citation statements)
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“…The presence in Thailand was not mentioned as they were thought to be found around the Mediterranean. In addition, the Chthamalids we found exhibit great variation and this has previously been reported that Chthamalids have high intraspecific variation in external morphology (Helmuth et al 2006;Hawkins et al 2008) and thus using shell morphology is not ideal for taxonomic identification; thus several studies have used other measures for species diagnosis, including opercular plate geometry (Tsang et al 2012), light microscopy and SEM of arthropodal characters (e.g. the number of conical spines and the number of setules of the basal guard setae on cirri and pattern of oral cones) (Miller and Blower 1989;Southward and Newman 2003;Yan and Chan 2004;Tsang et al 2012) and molecular approaches (Tsang et al 2012).…”
Section: Discussionsupporting
confidence: 74%
“…The presence in Thailand was not mentioned as they were thought to be found around the Mediterranean. In addition, the Chthamalids we found exhibit great variation and this has previously been reported that Chthamalids have high intraspecific variation in external morphology (Helmuth et al 2006;Hawkins et al 2008) and thus using shell morphology is not ideal for taxonomic identification; thus several studies have used other measures for species diagnosis, including opercular plate geometry (Tsang et al 2012), light microscopy and SEM of arthropodal characters (e.g. the number of conical spines and the number of setules of the basal guard setae on cirri and pattern of oral cones) (Miller and Blower 1989;Southward and Newman 2003;Yan and Chan 2004;Tsang et al 2012) and molecular approaches (Tsang et al 2012).…”
Section: Discussionsupporting
confidence: 74%
“…Particularly rapid increases were observed along the margins of both the Norwegian and North Seas, at rates varying between ~0.3 and ~0.7 °C per decade. There is a wealth of information associating this warming with poleward shifts in species' geographical ranges, phenology changes to earlier dates in the year, and ecosystem regime changes from cold-water to warm-water assemblages 14,[16][17][18][19][20] . SST has not been increasing homogeneously during the year, but rather changes have been more rapid during spring and autumn (Fig.…”
Section: Global Patternsmentioning
confidence: 99%
“…The continuity of coastlines between the temperate and polar zones facilitates the poleward migration of temperate macrophyte species and is unique to the Arctic Ocean because the Southern Ocean acts as a barrier for dispersal of southern temperate species to Antarctica (Wulff et al, 2009;Jueterbock et al, 2013). Northern Hemisphere intertidal biota are already moving northwards at speeds of up to 50 km per decade (Helmuth et al, 2006;Hawkins et al, 2008;Weslawski et al, 2010), and there are reports of northward range extensions of kelps (Müller et al, 2009 and references therein; Wilce and Dunton, 2014), and new eelgrass meadows in Greenland .…”
Section: Macrophyte-dominated Ecosystems In a Warmer Arcticmentioning
confidence: 99%