Odontoscelis (Odontoscelis) fuliginosa (Linnaeus, 1761)
publication ID |
https://doi.org/ 10.5281/zenodo.5342454 |
persistent identifier |
https://treatment.plazi.org/id/038E87F4-FFB5-FFEB-FE88-FE67FC6CED02 |
treatment provided by |
Felipe |
scientific name |
Odontoscelis (Odontoscelis) fuliginosa (Linnaeus, 1761) |
status |
sensu lato |
Odontoscelis (Odontoscelis) fuliginosa (Linnaeus, 1761) sensu lato
Material examined. GILAN: Deylaman , 1 specimen, 16.-20.vii.1996 ; Manjil , 1 specimen, 16.v.-14.vi.1995. ARDABIL: Khalkhal – Kivi, 1 specimen, 4.viii.1996 .
Comments. In mountain steppes. Holopalaearctic. DANILOVITSH (1975) recognized a variability in the structure of the aedeagus in different populations. GÖLLNER- SCHEIDING (1986) mentioned that in most populations both aedeagal processes (Fig. 2A-C) are long and gracile. DANILOVITSH (1975) pointed out that the second aedeagal process is considerably shorter and broader in populations from northern Iran and Turkmenistan. In a male from Deylaman the aedeagus is similar to Fig. 2D. A large material is needed to decide whether these populations represent
Fig. 2. Lateral view of aedeagus (ap1, ap2 = aedeagal processes).A-D – Odontoscelis fuliginosa (Linnaeus, 1761) : A – Germany, Thüringen; B – Bulgaria; C – Kazakhstan; D – Iran, Gorgana. E – O. montandoni Kis, 1979 , Egypt (A-C after GÖLLNER- SCHEIDING (1986); D-E after DANILOVITSH (1975)).
separate species. KIS (1979) already proved that populations from North Africa with a peculiar shape of the second process (Fig. 2E), which were regarded as a form of O. fuliginosa by DANILOVITSH (1975), belong to a separate species O. montandoni Kis, 1979 .
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