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<metadata xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:dc="http://purl.org/dc/elements/1.1/"><dc:title>Duality of terrestrial subterranean fauna</dc:title><dc:creator>Novak,	Tone	(Avtor)
	</dc:creator><dc:creator>Perc,	Matjaž	(Avtor)
	</dc:creator><dc:creator>Lipovšek Delakorda,	Saška	(Avtor)
	</dc:creator><dc:creator>Janžekovič,	Franc	(Avtor)
	</dc:creator><dc:subject>endemites</dc:subject><dc:subject>superficial subterranean habitats</dc:subject><dc:subject>trogloxenes</dc:subject><dc:subject>troglophiles</dc:subject><dc:subject>troglobionts</dc:subject><dc:description>Terrestrial animals in subterranean habitats are often classified according to their degree of morphological or ecological specialization to the subterranean environment. The commonly held view is that, as distance into a cave increases, the frequency of morphologically specialized, i.e., troglomorphic, species or ecological specialization will increase. We tested this hypothesis for the fauna in 54 caves in Slovenia-the classical land for subterranean biology. We found that there exist two ecologically well separated terrestrial subsurface faunas: one shallow and one deep. 1) The shallow subterranean fauna, adapted to the terrestrial shallow subterranean habitats (SSHs) in the upper 10 m of subsurface strata, is most diverse. It consists of randomly distributed non-troglobionts and a major group of troglobionts adapted to the soil root zone. 2) The deep subterranean fauna is represented by a minor group of troglobionts, adapted to caves. Troglobionts are strictly divided between the two faunas. There is strong evidence that in karstic ecosystems with deep-rooted vegetation this might be a global pattern, or that in these locations only the shallow subterranean fauna exist.</dc:description><dc:date>2012</dc:date><dc:date>2017-08-04 12:12:47</dc:date><dc:type>Članek v reviji</dc:type><dc:identifier>67169</dc:identifier><dc:identifier>ISSN: 0392-6672</dc:identifier><dc:identifier>UDK: 591.9:551.44</dc:identifier><dc:identifier>OceCobissID: 858900</dc:identifier><dc:identifier>COBISS_ID: 19061512</dc:identifier><dc:identifier>DOI: 10.5038/1827-806X.41.2.5</dc:identifier><dc:identifier>ISSN pri članku: 0392-6672</dc:identifier><dc:identifier>NUK URN: URN:SI:UM:DK:P4FEEGFF</dc:identifier><dc:language>sl</dc:language></metadata>
