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High diversity of lichens at 84°S, Queen Maud Mountains, suggests preglacial survival of species in the Ross Sea region, Antarctica

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dc.contributor.author Green, T.G. Allan
dc.contributor.author Sancho, Leopoldo G.
dc.contributor.author Türk, Roman
dc.contributor.author Seppelt, Rodney D.
dc.contributor.author Hogg, Ian D.
dc.date.accessioned 2011-03-29T21:01:29Z
dc.date.available 2011-03-29T21:01:29Z
dc.date.issued 2011
dc.identifier.citation Green, T.G.A., Sancho, L.G., Türk, R., Seppelt, R.D. & Hogg, I.D. (2011). High diversity of lichens at 84°S, Queen Maud Mountains, suggests preglacial survival of species in the Ross Sea region, Antarctica. Polar Biology, available online 09 March 2011. en_NZ
dc.identifier.uri http://hdl.handle.net/10289/5213
dc.description.abstract Investigations of lichens collected in 1959/1960, 1963/1964 and 2003 from near the Beardmore Glacier in the southern Ross Sea region (84 S) have more than doubled the number of known lichen species in the area to around 30. The ranges of 15 species have been extended to 84° S. A lichen diversity hotspot has also been found along Ebony Ridge and its associated peaks where 28 of the species occur, a number equivalent to more northerly sites in the Ross Sea (e.g. Botany Bay 77° S). Furthermore, 6 species had been previously recorded only from the Antarctic Peninsula region. In agreement with previous studies on mites and springtails from the same area, we suggest that these populations represent relicts that predate the present Ross Ice Shelf extension, with a possible age of 2,000,000 years or older. en_NZ
dc.language.iso en
dc.relation.uri http://www.springerlink.com/content/574410k65u578317/ en_NZ
dc.subject relict en_NZ
dc.subject Collembola en_NZ
dc.subject Beardmore Glacier en_NZ
dc.subject mosses en_NZ
dc.subject diversity en_NZ
dc.subject lichens en_NZ
dc.title High diversity of lichens at 84°S, Queen Maud Mountains, suggests preglacial survival of species in the Ross Sea region, Antarctica en_NZ
dc.type Journal Article en_NZ
dc.identifier.doi 10.1007/s00300-011-0982-5 en_NZ


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