The relict mite Rhagidia gelida (Acari, Rhagidiidae) as a biological cryoindicator of periglacial microclimate in European highland screes

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Abstract

The periglacial temperature regime in cool scree slopes located at subalpine altitudes of only 300-600 m a.s.l. in the Czech highlands is described and proved by the occurrence of a relict population of the predatory mite Rhagidia gelida Thorell (Acari, Prostigmata, Rhagidiidae). The mite has a circum-boreal pattern of distribution today, but its disjunct populations have an island-like pattern of distribution in the cool screes in the Czech highlands. R. gelida is univoltine, freezing intolerant, and considered a biological cryoindicator of the periglacial microclimate. As coolness is needed for R. gelida to survive in the cool screes, it is concluded that the scree slope patchy permafrost-like habitats have lasted continuously, perhaps persisting in modified form as paleorefugia, since the Pleistocene. © 2005 Regents of the University of Colorado.

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APA

Zacharda, M., Gude, M., Kraus, S., Hauck, C., Molenda, R., & Růžička, V. (2005). The relict mite Rhagidia gelida (Acari, Rhagidiidae) as a biological cryoindicator of periglacial microclimate in European highland screes. Arctic, Antarctic, and Alpine Research, 37(3), 402–408. https://doi.org/10.1657/1523-0430(2005)037[0402:TRMRGA]2.0.CO;2

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