Troglophilus neglectus, VLASINENSIS

Karaman, Ivo, Hammouti, Nasera, Pavićević, Dragan, Kiefer, Andreas, Horvatović, Mladen & Seitz, Alfred, 2011, The genus Troglophilus Krauss, 1879 (Orthoptera: Rhaphidophoridae) in the west Balkans, Zoological Journal of the Linnean Society 163 (4), pp. 1035-1063 : 1043-1045

publication ID

https://doi.org/ 10.1111/j.1096-3642.2011.00738.x

persistent identifier

https://treatment.plazi.org/id/03F75E0E-FFD3-FFA8-FCF4-FAE1FC7BF8B6

treatment provided by

Valdenar

scientific name

Troglophilus neglectus
status

 

TROGLOPHILUS NEGLECTUS VLASINENSIS View in CoL : HARZ, 1969

Material examined: See Appendix.

Diagnosis: Medium to large sized species. Male body length ranges between 13.5– 20 mm; females, 14–24 mm. Body colour dark brown, light brown to light green marbled. Males tenth tergite with narrow, partially square, medial lobe which is divided by a central deep depression in two triangular-shaped lobes ( Fig. 6A–D View Figure 6 ). Female tenth abdominal tergite with two paramedial, sharp spine-like protrusions ( Fig. 6E–F View Figure 6 ). The titillator distally protruded with abruptly narrowed obtuse tip ( Fig. 7A View Figure 7 ); in lateral view, distally voluminous ( Fig. 7B View Figure 7 ). The ovipositor short and wide, length ranges between 8–11 mm; the widest point is in its proximal third ( Fig. 12I View Figure 12 ), ventral margin almost straight.

Distribution: This species is widely distributed over a large part of the Balkans ( Fig. 8 View Figure 8 ) and neighbouring parts of Austria and Italy. We can roughly distinguish two relatively compact units of its distribution range. The first one extends from northern parts of Macedonia and southern parts of Serbia to northeast Serbia and western-most parts of Bulgaria. The southern distribution borders are still not clear; it is possible that the species is present in Albania as well.

The second unit comprises western-most parts of the Balkans and neighbouring regions of Austria and Italy. The species is present in western Bosnia, in Croatia from northern Dalmatia to the north and west, and widely in Slovenia. The eastern-most area of this unit of the species distribution range is in Slavonia and western Bosnia. However, the distribution pattern in Bosnia is still unclear. The species is not present in western parts of Serbia, in Montenegro, in Herzegovina, and in south and central Dalmatia. It seems that it is absent from east Bosnia too. Southern populations appear only at higher altitudes. There are no data on the sympatric appearance of this species with other Troglophilus species in the eastern unit of its distribution range. In the western unit, sympatry with T. cavicola is very common.

Remarks: The citation of this species from the Imanthia Cave near Nousa in Greece most probably refers to the species T. zorae sp. nov. This was concluded according to the illustration of a male tenth tergite in Maran (1958).

Morphological characteristics of T. neglectus vlasinensis from south-east Serbia, used for differentiation in Maran (1958), are in the boundaries of the variability of T. neglectus . Troglophilus neglectus neglectus and T. neglectus vlasinensis share the same haplotype, T neg HT1, which also suggests synonymization of these taxa.

After examination of a large number of specimens, we can say with certainty that the populations of T. neglectus in eastern Serbia are parthenogenetic. We suppose that it is the same in the neighbouring parts of Bulgaria where this species is present. As females dominate in the material from the south populations, this led us to the supposition that parthenogenetic populations also prevail in these areas (the only males were collected from a cave north of Skopje). The assumption that the marginal populations are often parthenogenetic imposes a conclusion that these areas were secondarily inhabited from the west. However, in keeping with the recent distribution, we conclude quite the opposite. The primary distribution range of this species must be related to the southern parts of Serbia and neighbouring areas. The explanation for such an opinion is given in the Discussion.

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Tavera, Department of Geology and Geophysics

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