2007
DOI: 10.1016/j.flora.2007.05.005
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Slowest to fastest: Extreme range in lichen growth rates supports their use as an indicator of climate change in Antarctica

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Cited by 100 publications
(86 citation statements)
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References 33 publications
(41 reference statements)
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“…The use of lichens in dating rock surfaces is well known (see below) and is based on temporal changes in lichen surface areas in response to climate and environment. Present trends of climate warming will have major consequences for lichens, with the known geographical ranges of both individual taxa and lichen communities either increasing or declining (see, e.g., Nash & Olafsen 1995;Insarov et al 1999;Lange & Green 2005;Aptroot & van Herk 2007;Ellis & Coppins 2007;Sancho et al 2007;Binder & Ellis 2008).…”
Section: Climate Changementioning
confidence: 99%
“…The use of lichens in dating rock surfaces is well known (see below) and is based on temporal changes in lichen surface areas in response to climate and environment. Present trends of climate warming will have major consequences for lichens, with the known geographical ranges of both individual taxa and lichen communities either increasing or declining (see, e.g., Nash & Olafsen 1995;Insarov et al 1999;Lange & Green 2005;Aptroot & van Herk 2007;Ellis & Coppins 2007;Sancho et al 2007;Binder & Ellis 2008).…”
Section: Climate Changementioning
confidence: 99%
“…The bryoflora is likely to be the most sensitive vegetation component to target for this purpose, as growth rates (mean 0.6-1.3 mm y -1 ; Clarke et al 2012) are greater than that of lichens (<0.1 mm y -1 ; Sancho et al 2007), which are impractically slow. Whilst previous investigations of vegetation distributions in the Windmill Islands, have examined broadscale patterns (over meters to kilometres; e.g.…”
Section: Introductionmentioning
confidence: 99%
“…ese ndings can be related with the human impacts in the area, to decreasing diversity along the two summer seasons (Victoria & Pereira, 2007). For Sancho et al (2007) these changes can be a climate change indicator, because that lichen species found in the studied region are susceptible to extreme temperature variation, increasing or decreasing their growth (Sancho et al, 2007), but the fast development and death of the foliose muscicolous lichen cannot be discarded, as certain types of foliose lichens are among the fastest-growing species which have the ability to grow up to one centimeter per year, and this growth rate is unusual in most lichen species (Bednarik, 2004).…”
Section: Discussionmentioning
confidence: 98%