Strigamia Gray, 1843

Bonato, Lucio, Dányi, László, Socci, Antonio Augusto & Minelli, Alessandro, 2012, Species diversity of Strigamia Gray, 1843 (Chilopoda: Linotaeniidae): a preliminary synthesis, Zootaxa 3593, pp. 1-39 : 3-7

publication ID

https://doi.org/ 10.5281/zenodo.214898

publication LSID

lsid:zoobank.org:pub:56D84A4E-E8A7-4C78-8C58-F85BAA13B9DF

DOI

https://doi.org/10.5281/zenodo.5613178

persistent identifier

https://treatment.plazi.org/id/03A2607E-876D-FF82-B398-FAD7FA62F80C

treatment provided by

Plazi

scientific name

Strigamia Gray, 1843
status

 

Strigamia Gray, 1843 View in CoL View at ENA

Diagnosis. Geophilomorphs with body distinctly narrowing towards both the anterior and the posterior end ( Fig. 1 View FIGURE 1. A ). Head about as long as wide ( Fig. 2 View FIGURES 2 – 4 ). Antenna about uniform in width or slightly tapering ( Fig. 3 View FIGURES 2 – 4 ); club-like sensilla (sensilla basiconica) only on the terminal article; apical sensilla (sensilla brachyconica) without projections. Clypeus uniformly areolate, without clypeal areas ( Fig. 2 View FIGURES 2 – 4 ). Labrum without anterior alae and without obviously distinct lateral parts; margin concave, lined with short denticles. Epipharynx with bilobate border between clypeal and labral parts. Mandible with a single pectinate lamella. First maxillae with distinct, entire coxosternite and bi-articulate telopodites, without elongate lappets ( Fig. 2 View FIGURES 2 – 4 ). Second maxillary coxosternite uniformly sclerotized, the anterior margin concave, without inner processes; telopodite composed of three articles, bearing a subconic bent claw ( Fig. 2 View FIGURES 2 – 4 ). Forcipular metatergite subtrapezoid, posteriorly as wide as the subsequent tergite, the lateral margins converging anteriorly. Forcipular coxosternite wider than long, without anterior denticles; coxopleural sutures complete, entirely ventral, sinuous and distinctly diverging anteriorly; chitin-lines indistinct ( Fig. 4 View FIGURES 2 – 4 ). Forcipule relatively short, the trochanteroprefemur without denticles, two distinct intermediate articles, the tarsungulum with one large basal denticle ( Fig. 4 View FIGURES 2 – 4 ). Leg-bearing segments without paratergites and without carpophagus pits; metasternites with two paired subovoid posterior pore-fields, usually also two smaller paired anterior pore-fields. Leg claws bearing two slender accessory spines. Ultimate leg-bearing segment with subtrapezoid metasternite; coxal pores present, on the ventral side only ( Figs 5–6 View FIGURES 5 – 6 ). Telopodites of the ultimate pair approximately as long as those of the penultimate pair, composed of six articles, swollen in male in comparison with the female, bearing a claw ( Figs 7–8 View FIGURES 7 – 8 ). Bi-articulated gonopods in the male, short bilobate gonopodal lamina in the female; a pair of anal pores.

Type species: Strigamia fulva Sager, 1856 , by subsequent monotypy (I.C.Z.N. 1999: art. 69.3).

Synonyms: Linotaenia C.L. Koch ; Scolioplanes Bergsøe & Meinert, 1866 ; Tomotaenia Cook, 1895; Diplochora Attems, 1903 ; Paraplanes Verhoeff, 1933 ; Leptodampius Chamberlin, 1938 (new synonymy); Korynia Chamberlin, 1941 (new synonymy).

Notes on synonymies. All nominal genera listed above are either confirmed or recognized for the first time as synonyms of Strigamia because their type species match the diagnosis of Strigamia given above. For the species that are known only from the literature, this evaluation was obviously limited to the characters described or illustrated; however, we found no evidence of major differences that justify recognizing these species in distinct genera. In the following, the history of taxonomic opinions is summarized, and arguments for the new synonymies are discussed.

The name Strigamia was first introduced by Jones (1843), who acknowledged J.E. Gray as its author. The name was explicitly adopted for the genus that had been previously called Geophilus Leach , but without providing reasons for the substitution. When introduced, Strigamia was accompanied by a very vague diagnosis that fits the concept of the entire Geophilomorpha , and no species were included in it. The concept of Strigamia and the identity of its type species remained unclear for about a century, with different students elaborating different opinions. Some authors considered Strigamia merely a junior synonym of Geophilus ( Gervais 1847; Newport 1856; Latzel 1880; Cook 1895). Instead, Wood (1862, 1865, 1867) adopted Strigamia as a valid genus name, with a concept much broader than the current one. Conversely, other influential authors introduced and adopted different generic names for species that are now in Strigamia ( C.L. Koch 1847; Bergsøe & Meinert 1866; Cook 1895; Attems 1903, 1929). Such nomenclatural and taxonomic uncertainties were debated between Crabill (1953, 1954a, 1954b, 1962a) and Chamberlin (1954, 1963). The confusion surrounding the type species of Strigamia was eventually clarified by Crabill (1953), who pointed to the fact that S. fulva was the first species included in the genus. Only after that, Strigamia began to be adopted broadly, in a concept broadly corresponding to the one here defined.

Linotaenia was introduced by C.L. Koch (1847) to include four species, namely Geophilus crassipes C.L. Koch (currently Strigamia crassipes View in CoL ), Geophilus subtilis C.L. Koch and Linotaenia rosulans C.L. Koch (both currently regarded as junior synonyms of Geophilus acuminatus Leach , currently Strigamia acuminata View in CoL ), and Geophilus nemorensis C.L. Koch (currently Schendyla nemorensis View in CoL , in the Schendylidae View in CoL ), but without selecting a type species. Because of the heterogeneous original circumscription of Linotaenia, Meinert (1870) and other authors considered it as corresponding partly to Scolioplanes View in CoL (currently regarded as a synonym of Strigamia View in CoL ) and partly to Schendyla Bergsøe & Meinert. View in CoL L. rosulans was selected validly as the type species by Pocock (1890), whereas other designations are invalid either because they are subsequent or because the selected species was not originally included in the genus. Linotaenia was adopted with a concept approximately corresponding to our concept of Strigamia View in CoL , by some of the most active American authors (including C.H. Bollman and R.V. Chamberlin), whereas most European authors rejected it for Scolioplanes View in CoL . Linotaenia was also adopted by Crabill (1953) as a subgenus of Strigamia View in CoL but later synonymized under Strigamia View in CoL by Crabill himself (1960a). The latter opinion was followed by most subsequent authors.

Scolioplanes View in CoL was introduced by Bergsøe & Meinert (1866) to include three species, namely Geophilus acuminatus Leach , Geophilus crassipes C.L. Koch and Geophilus maritimus Leach (all currently under Strigamia View in CoL ), without selecting a type species. G. maritimus was selected validly as the type species by Cook (1895). Scolioplanes View in CoL was used as a valid genus, with a concept approximately corresponding to our concept of Strigamia View in CoL , by most European and Japanese authors (including C. Attems, H.W. Brölemann, F. Meinert, A. Seliwanoff, Y. Takakuwa, and K.W. Verhoeff), while other students regarded Scolioplanes View in CoL as a junior synonym of Linotaenia ( Pocock 1890; Bollman 1893a, 1893b; Cook 1895; Silvestri 1905; Crabill 1953; Chamberlin 1954). Scolioplanes View in CoL was first synonymized under Strigamia View in CoL by Crabill (1960a), followed by most subsequent authors.

Tomotaenia was introduced by Cook (1895) by designating Strigamia parviceps Wood View in CoL as type species and including tentatively another twelve species, namely S. bidens Wood View in CoL , S. bothriopus Wood View in CoL , S. chionophila Wood View in CoL , S. fulva Sager View in CoL , S. laevipes Wood View in CoL , S. maculaticeps Wood View in CoL , S. walkeri Wood View in CoL , Linotaenia branneri Bollman and Scolioplanes exul Meinert (both currently included in Strigamia View in CoL ), Scolioplanes robustus Meinert View in CoL and Scolioplanes ruber Bollman View in CoL (both synonymized under Strigamia View in CoL species), and Scolioplanes longicornis Meinert (of uncertain identity). Tomotaenia was used as valid only by a few other authors ( Crabill 1954a; Kevan & Scudder 1989; Bonato et al. 2011), but it was rejected or at least ignored by most other authors. It was listed explicitly among the synonyms of Scolioplanes View in CoL by Attems (1929) and among those of Strigamia View in CoL by Matic (1972). As it is dubious if the type species S. parviceps View in CoL actually belongs to the genus Strigamia View in CoL as diagnosed here (see below under “Uncertain species”), the synonymy of Tomotaenia under Strigamia View in CoL is followed here only provisionally.

Diplochora View in CoL was introduced by Attems (1903) for the single species D. fusata Attems , which is the type species by monotypy. No other species were assigned to Diplochora View in CoL , which was merely cited by other authors. Diplochora View in CoL was synonymized under Tomotaenia by Crabill (1962a, 1962b), followed by Chamberlin (1963), who also synonymized the type species of the two genera. Diplochora View in CoL was first regarded as a synonym of Strigamia View in CoL by Mercurio (2010).

Paraplanes View in CoL was introduced by Verhoeff (1933) for the single species P. svenhedini Verhoeff , which is thus the type species by monotypy. Verhoeff (1938a) subsequently included another species, P. californicus Ve View in CoL rh o eff (currently a synonym of Strigamia fusata ). Paraplanes View in CoL was synonymized under Tomotaenia by Chamberlin (1941), but it has been cited as valid also later ( Shinohara 1981a; Wang & Mauriès 1996). It was first listed among the synonyms of Strigamia View in CoL by Mercurio (2010).

Leptodampius was introduced by Chamberlin (1938) for the single species L. lamprus Chamberlin , which is the type species by original designation. The validity of the genus was never questioned. As to its taxonomic position, Chamberlin (1938) did not assign it explicitly to any family but described it as a “geophiloid”, Crabill (1962b) recognized it as belonging to Dignathodontidae View in CoL under a concept including also Linotaeniidae View in CoL , but recent catalogues listed it as a member of the family Geophilidae View in CoL ( Kevan 1983; Mercurio 2010). Leptodampius is recognized here as a synonym of Strigamia View in CoL because the original description of L. lamprus matches Strigamia View in CoL in major diagnostic features such as the elongation of the head and the forcipules, the shape of the forcipular tarsungula, the absence of chitin-lines, and the size of the ultimate legs; additionally, Chamberlin (1938) acknowledged that Leptodampius is similar to Agathothus Bollman View in CoL (which is close to Strigamia View in CoL ; see below under “Similar genera”) and differs from it mainly for a large basal denticle on the forcipular tarsungulum and the narrower metasternite of the ultimate leg-bearing segment, two characters that are found in Strigamia View in CoL but not in Agathothus View in CoL .

Korynia View in CoL was introduced by Chamberlin (1941) to include three species, namely K. carmela Chamberlin , K. texensis Chamberlin and K. tripora Chamberlin , among which K. carmela was designated originally as the type species. Another species, K. auxa Chamberlin , was later described under the genus ( Chamberlin 1954). Crabill (1954a) treated Korynia View in CoL as a subgenus of Tomotaenia, and assigned to it also D. fusata and his new species T. (K.)

urania Crabill. However , Crabill’s classification was not followed by other authors, and Korynia View in CoL was often ignored although not rejected formally ( Mercurio 2010). Korynia View in CoL is recognized here as a synonym of Strigamia View in CoL because, based on the accounts by Chamberlin (1941, 1954), it matches Strigamia View in CoL in major diagnostic features such as the shape of the head, the forcipules and the ultimate legs in the male. However, the ventral pore-fields were not mentioned by Chamberlin (1941), while they were described as “not detected” by Chamberlin (1954) in K. texensis , but we agree with Crabill (1954a) that this should not be construed as a reliable indication by Chamberlin that the pores are actually absent in the Korynia View in CoL species. Actually, Crabill (1954a) found that, in another species recognized by him as representative of Korynia View in CoL , the pores are present, at least in the anterior part of trunk, although detectable with difficulty. Supporting our opinion is also the fact that Chamberlin acknowledged explicitly that Korynia View in CoL resembles Linotaenia specifically in the head shape, the labrum, the mouth parts, and the basal denticle of the forcipular tarsungulum ( Chamberlin 1941), and that it resembles Tomotaenia specifically in the pattern of coxal pores ( Chamberlin 1954).

Similar genera. Strigamia View in CoL is most similar to the genera Agathothus Bollman, 1893 View in CoL , Araucania Chamberlin, 1955 View in CoL , Damothus Chamberlin, 1960 View in CoL , and Zantaenia Chamberlin, 1960 View in CoL . These are all small genera, including one or two species each. To the exclusion of Araucania View in CoL , which is endemic to a small region in the central-southern Andes, all others inhabit North America within the range of Strigamia View in CoL . With the exception of Damothus View in CoL , the morphology of these genera is not known at a satisfactory level, and they have been recorded very rarely. As far as known, most of them differ from Strigamia View in CoL in the basal denticle of the forcipular tarsungulum, which is completely wanting in Agathothus View in CoL and Zantaenia View in CoL , and double in Damothus View in CoL . Additionally, the labrum is lined with many projections besides the medial tubercles in Araucania View in CoL , the legs of the ultimate pair are distinctly longer than the penultimate pair at least in Agathothus View in CoL and Damothus View in CoL , the ventral glandular pores are putatively lacking in Damothus View in CoL , and the ultimate legs of the male lack claws in Zantaenia View in CoL .

Other genera have been considered in the past as closely related to Strigamia View in CoL or even as its synonyms, and thus often classified in the same family Linotaeniidae View in CoL . This is the case of Horonia Chamberlin, 1966 View in CoL , Javaenia Chamberlin, 1944 View in CoL , Malochora Chamberlin, 1941 View in CoL and Pagotaenia Chamberlin, 1915 View in CoL . However, based on their original descriptions, they are most probably much more distant from Strigamia View in CoL , if not misplaced at all.

Included species. The species we recognize in Strigamia View in CoL are listed below in alphabetic order. Main morphological features are given in Table 1 View TABLE 1 . An asterisk (*) indicates the species whose taxonomic validity is tentative only. Original combinations, type localities and information about type specimens are given in Appendix 2.

...... continued on the next page

TABLE 1. Main characters of the species of Strigamia recognized here as valid. An asterisk (*) indicates species whose taxonomic distinction is tentative only. The number of specimens upon which body length and number of legs have been evaluated (n) is given in three classes (1 – 2 specimens, 3 – 10 specimens, more than 10 specimens), because sometimes the number is known only approximately.

species n direct obs. max. length [mm] Ƥ leg pairs 3 leg pairs ultimate pleuropretergite entire ultimate metaster nite coxal pores distribution
S. acuminata View in CoL >10 x 40 39–43 37–41 yes narrow scattered W Palaearctic
S. alokosternum View in CoL 3–10 x 40 59–67 51–61 no broad scattered E Palaearctic
S. auxa * 1–2 38 ? 73 no broad all close to metasternite Nearctic
S. bicolor View in CoL 3–10 x 35 45–53 41–49 no narrow scattered E Palaearctic
S. bidens View in CoL >10 x 64 67–81 65–77 yes narrow scattered Nearctic
S. bothriopus View in CoL >10 x 60 47–53 43–51 yes narrow scattered Nearctic
S. branneri * >10 x 37 41–43 39–41 no narrow scattered Nearctic
S. carmela 1–2 16 ? 53 no broad all close to metasternite Nearctic
S. caucasia View in CoL 1–2 28 ? 47 no narrow scattered W Palaearctic
S. chionophila View in CoL >10 x 25 37–47 35–45 no narrow scattered Nearctic
S. cottiana View in CoL 3–10 x 42 59–65 61–65 yes narrow scattered W Palaearctic

Kingdom

Animalia

Phylum

Arthropoda

Class

Chilopoda

Order

Geophilomorpha

Family

Linotaeniidae

Loc

Strigamia Gray, 1843

Bonato, Lucio, Dányi, László, Socci, Antonio Augusto & Minelli, Alessandro 2012
2012
Loc

Horonia

Chamberlin 1966
1966
Loc

Damothus

Chamberlin 1960
1960
Loc

Zantaenia

Chamberlin 1960
1960
Loc

Araucania

Chamberlin 1955
1955
Loc

Javaenia

Chamberlin 1944
1944
Loc

Malochora

Chamberlin 1941
1941
Loc

Pagotaenia

Chamberlin 1915
1915
Loc

Agathothus

Bollman 1893
1893
Loc

Linotaenia

Meinert 1870
1870
GBIF Dataset (for parent article) Darwin Core Archive (for parent article) View in SIBiLS Plain XML RDF