Journal article
2006
APA
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Çıplak, B., & Heller, K. (2006). Morphology, bioacoustics and phylogeography of the Isophya major group (Orthoptera: Tettigoniidae: Phaneropterinae): A species complex occurring in Anatolia and Cyprus.
Chicago/Turabian
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Çıplak, B., and K. Heller. “Morphology, Bioacoustics and Phylogeography of the Isophya Major Group (Orthoptera: Tettigoniidae: Phaneropterinae): A Species Complex Occurring in Anatolia and Cyprus” (2006).
MLA
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Çıplak, B., and K. Heller. Morphology, Bioacoustics and Phylogeography of the Isophya Major Group (Orthoptera: Tettigoniidae: Phaneropterinae): A Species Complex Occurring in Anatolia and Cyprus. 2006.
BibTeX Click to copy
@article{b2006a,
title = {Morphology, bioacoustics and phylogeography of the Isophya major group (Orthoptera: Tettigoniidae: Phaneropterinae): A species complex occurring in Anatolia and Cyprus},
year = {2006},
author = {Çıplak, B. and Heller, K.}
}
The species of the Isophya major-group (Orthoptera: Tettigoniidae: Phaneropterinae), are reviewed. I. major Brunner von Wattenwyl and I. mavromoustakisi Uvarov are redescribed. Two new species are described; Isophya mersinensis Sevgili & Ciplak sp. n. and Isophya salmani Sevgili & Heller sp. n. from south Anatolia. Illustrations of morphology and male calling song are pro- vided and a detailed comparison of the four species in the group is presented. We conclude that these four species constitute a natural group in sharing male cerci with two or more denticles not ordered in a line, a character unique to this species group within the genus. From an evaluation of their morphology and song characteristics, relationships among the species in the group are I. major + (I. mersinensis sp. n. + (I. salmani + I. mavromoustakisi). Based on the the distribution pattern and habitat preference, we concluded that the division of I. salmani and I. mavromoustakisi was a vicariant event resulting from the separation of Cyprus and Anatolia due to reflooding of the Mediterranean after the Messinian salinity crisis at the beginning of the Pliocene, around 5 My ago.