Cyphonethes biseriatus ( Verhoeff, 1900 )

Karaman, Ivo M. & Horvatović, Mladen, 2018, Revision of the genera Cyphonethes Verhoeff, 1926 and Titanethes Schioedte, 1849 (Isopoda: Oniscoidea: Trichoniscidae) with a description of a new genus and three new taxa, Zootaxa 4459 (2), pp. 261-284: 263-265

publication ID

https://doi.org/10.11646/zootaxa.4459.2.3

publication LSID

lsid:zoobank.org:pub:49F5AF2B-E795-404B-A946-2C00DB6011B2

persistent identifier

http://treatment.plazi.org/id/40481448-675D-FF9F-FF28-FB332455FEA3

treatment provided by

Plazi

scientific name

Cyphonethes biseriatus ( Verhoeff, 1900 )
status

comb. nov.

Cyphonethes biseriatus ( Verhoeff, 1900)  comb. nov.

Figs 1–2 View Figure

Titanethes biseriatus: Tabacaru, 1996 

Titanethes biseriatus: Schmalfuss, 2003 

Microtitanethes licodrensis: Pljakić, 1977  syn. nov.

Microtitanethes licodrensis: Tabacaru, 1996 

Microtitanethes licodrensis: Schmalfuss, 2003 

Material examined: Serbia: Krupanj, Lipenovići, Lukića pećina cave, 7.4.2008, leg. I. Karaman & M. Horvatović, 1♀  ; ibid. 24.5.2008, leg. I. Karaman & M. Horvatović, 1♂  ; Sjenica, Vranjina pećina cave, 4♂, 7♀  ; Sjenica, 17.4.1973  , 1♂, 3♀. Montenegro: Rožaje , Bać  , vrelo (fountainhead), 2.8.1972, leg. M. Pljakić, 2♀; ibid. 13.2.1974  , leg. M. Pljakić, 3♂, 2♀. Bosnia and Herzegovina: Republika Srpska, East Herzegovina, Fatničko polje, Lepirnica cave, 18.6.2003  , leg. I. Karaman, 2♂, 3♀. Macedonia: Skopska Crna Gora Mt, Banjani, Monastery Sveti Ilija, 17.4. 2000  , leg. I. Karaman, 1♀; Skopska Crna Gora Mt, Blace, Fuše špela cave, 27.2.2007, leg. I. Karaman, 11♂, 28♀  ; Skopje, Rašće, Dona Dupka cave, 7.10.2009, leg. I. Karaman, 1♀.

Diagnosis. Medium sized species (up to 4.4 mm long) without tegumental sexual gland-piliferous organ. Cephalon with three rows of small and low tubercles; Pereon tergites smooth with two transversal rows of small, low tubercles. Exopodite of pleopod 1 with widely rounded distal margin ( Fig. 1 View Figure ); medial margin of pleopod 2 exopodite with distinct curvature toward its distal end ( Fig. 2 View Figure ).

Remarks. The distribution of these species includes an unusually wide area of the central part of the Balkan Peninsula, where it occurs only sporadically ( Fig. 3 View Figure ), in isolated and mutually remote karstic regions. The species is described on the basis of a single female specimen from a cave in the vicinity of the town of Trebinje in the eastern part of Herzegovina. Strouhal (1939c) mentioned two additional cave localities in the wider surroundings of Trebinje from which three female specimens of this species were collected. According to the position of the localities and listed fauna of the remaining cave isopods, we believe that these findings are reliable and that certainly relate to this species. In any case the species is recognizable in the local fauna of cave isopods by two transversal rows of tubercles on pereon tergites and by its body dimensions. Over our long term biospeleological investigations on terrestrial isopods on the terrain of Eastern Herzegovina (including Trebinje vicinity and a cave that could be the Vučja pećina cave—locus typicus of C. biseriatus  ) we found this species only on one occasion, in a cave located about 35 km north of Trebinje. This best illustrates the fact that C. biseriatus  is very rare. However, the fact that adults of C. biseriatus  by size resemble juvenile specimens of the genus Alpioniscus  and Cyphonethes herzegowinensis  (that are otherwise frequent and numerous in the caves of this area) should not be neglected. Therefore, during the selective collection of cave isopods they could easily be overlooked.

Distribution of C. biseriatus  covers territories that do not share congruent fauna, particularly where cryptobionts are concerned. This can be explained only by its possible dispersion during the Pleistocene, when there had to be adequate corridors of substrate saturated with moisture which provided for the expansion of this species, especially to the east. We found specimens of T. biseriatus  , in a small and relatively dry cave in West Serbia (the northernmost point of the species known areal—loc.typ of Microtithanethes licodrensis  syn. nov.), deep in the crevices of cracked clay in a very humid part of the cave. However, the appearance of this species of real troglobite—without pigment and with reduced eyes, its unusual distribution and finding outside caves from the localities of Bać ( Pljakić 1977) and our finding of a specimen on Skopska Crna Gora Mt ( Macedonia), suggest it is more likely to be an element of MSS (Mesovoid Shallow Substratum) fauna with specific requirements for high humidity. Such conditions in the past could have provided littoral along river and stream flows of primarily karstic terrains that most likely allowed wide dispersion of this species (then as epigean), as is the case with the Carpatho- Balkan isopod species Mesoniscus graniger (Frivaldsky, 1865)  . These findings of specimens of this species outside a cave, in an ambient that is more suitable for organisms inhabiting MSS, speaks about the true nature of this species, i.e. it is a species that has relatively recently settled underworld. We mainly found specimens of this species in small numbers and always in the deeper parts of caves where real troglobionts are present.

It is worth noting that in a cave (Kovačevića pećina cave) near the cave with C. biseriatus  in West Serbia (Lukića pećina cave), two interesting troglobite/troglophile species were found ( Kličković et al. 2007): the pselaphid species Bryaxis blacensis (Karaman, 1954)  and the julid diplopod species Apfelbeckia insculpta (L. Koch, 1867)  . Bryaxis blacensis  was described from a cave near Blace at Skopska Crna Gora Mt in Macedonia (close to the cave where we found C. biseriatus  ). The two listed caves, far from each other, are the only known findings of this species up till now. The julid diplopod A. insculpta  is often a characteristic troglophile for south diniaric caves where C. biseriatus  is also present. This finding is the most remote finding of this species to the north; the same holds true for C. biseriatus  . Thus, the mentioned species are connecting distant and faunistically remarkably different regions, as a testimony to past invasions of some faunal elements in certain areas, but also as an expression of the zoogeographical closeness of these regions in the past.

In most cases we found C. biseriatus  sympatrically with other cave isopod species. On the southern part of its distribution (east Herzegovina) it appears together with Cyphonethes herzegowinensis  and some species from the genus Alpioniscus  ( Alpioniscus (I.) heroldii Verhoeff, 1931  or A. (I.) herzegowinensis Verhoeff, 1931  ). In the Dona Dupka cave (Rašće, Macedonia) it appears together with Cyphoniscellus (Vardaroniscus) tetraceratus (Buturović, 1955)  . At localities in Serbia we found them together with the species Mesoniscus graniger  (which was more numerous), that by size and body shape does not differ, so it is possible to overlook the presence of this species when found in mixed populations.

Kingdom

Animalia

Phylum

Arthropoda

Class

Malacostraca

Order

Isopoda

Family

Trichoniscidae

Genus

Cyphonethes

Loc

Cyphonethes biseriatus ( Verhoeff, 1900 )

Karaman, Ivo M. & Horvatović, Mladen 2018

2018
Loc

Titanethes biseriatus

: Schmalfuss 2003

2003
Loc

Microtitanethes licodrensis

: Schmalfuss 2003

2003
Loc

Titanethes biseriatus:

Tabacaru 1996

1996
Loc

Microtitanethes licodrensis:

Tabacaru 1996

1996
Loc

Microtitanethes licodrensis: Pljakić, 1977

: Pljakic 1977

1977