Okudrilus monticolus Csuzdi & Sherlock, 2015
publication ID |
https://doi.org/ 10.5733/afin.056.0103 |
publication LSID |
lsid:zoobank.org:pub:1E8310B9-5759-4C6B-BA3D-C33659D21DE3 |
DOI |
https://doi.org/10.5281/zenodo.7670468 |
persistent identifier |
https://treatment.plazi.org/id/31FE29C4-AE9D-48F7-8845-D158D3AFA6D4 |
taxon LSID |
lsid:zoobank.org:act:31FE29C4-AE9D-48F7-8845-D158D3AFA6D4 |
treatment provided by |
Felipe |
scientific name |
Okudrilus monticolus Csuzdi & Sherlock |
status |
sp. nov. |
Okudrilus monticolus Csuzdi & Sherlock sp. n.
Figs 5, 6 View Figs5, 6
Etymology: From Latin monticolus (adj.) (mountain dweller) in reference to the type locality, the summit of Mount Oku.
Diagnosis: L: 150–190 mm, D: 5–7 mm. Colour reddish-brown, paler on ventrum. Head epilobous, setae closely paired. Clitellum annular on ½13–18. Prostatic pores in 17/18 a–a, spermathecal pores 12/13 between a–a, female pores on 14 close to 14/ 15 in d. Gizzard in 6, calciferous glands in 12, chylus-sacs in 10, 11. Testes in 11, vesicles in 12 long, running back to 45. Ovo-spermathecal apparatus paired, spermathecal ampulla elongated, apically continues in an ovo-spermathecal duct communicating with the ovarian capsule. The right and left ovarian duct interconnected by a small channel. Prostates without copulatory sacs. Simple penial setae 4 mm in length and 0.03 mm in diameter.
Description:
External characters:
Holotype: Preserved length 190 mm, diameter after clitellum 7 mm. Segment number: 274. Paratype: (aclitellate) 155 mm in length, 5 mm in diameter. Segment number: 268. Colour: Preserved dark reddish-brown between setae d–d, paler on ventrum. Head: Epilobous, ½ closed. Dorsal pores: Lacking. Setae: Closely paired, setal ratio aa:ab:bc:cd:dd = 11.2:2:8:1:36. Nephridial pores: Begin on segment 2, somewhat dorsal to setal line d.
Clitellum: Highly glandular, annular on segments ½13–18. Prostatic pores: Ventral on a spectacles-shaped papilla in 17/18, aligned with setal line a–a. Female pores: Small dots on 14, close to the intersegmental furrow 14/15 just below setal line d. Spermathecal pores: Paired on a spectacles-shaped papilla in intersegmental furrow 12/13 between setae a–a ( Fig. 5 View Figs5, 6 ).
Internal characters:
Muscular gizzard: In 6, well-developed, cylindrical. Septa : 6/7, 11/12 thickened, 7/8–10/11 highly strengthened. Calciferous glands: Paired in 12, large curved like a goat-horn, chylus-sacs in 10, 11. Dorsal blood vessel: Simple throughout. Hearts: In 9–11, large moniliform. Testes and sperm funnels: In 11 enclosed in an oval spermreservoir. Seminal vesicles: Long, running alongside the intestine from 12 to 45. Ovospermathecal apparatus: Ovaries in 13 enclosed in an ovarian capsule pendant from septum 12/13. This ovarian capsule medially continuing in an ovarian duct becoming undulating before joining the fertilisation chamber bearing a pendant ovisac. From the fertilisation chamber a straight oviduct leads to the female pore. The ovarian capsule laterally communicates with an ovo-spermathecal duct joining apically to the elongated and muscular spermathecal ampulla. The spermathecal ampulla joins a one-third as long spermathecal duct opening into the spermathecal pore in 12/13. The left and right ovarian ducts communicate by a small interconnecting channel ( Fig. 6 View Figs5, 6 ). Prostates: Long simple tubes without bursa copulatrix or bursa propulsoria. Penial setae: Simple with blunt tip, c. 4 mm long and 0.03 mm in diameter, almost smooth except for the apex which bears fine granulatiOn.
Holotype: CAMEROON: North-West Region, summit of the Oku Mt , 2867-2922 m, 15.vi.2012, T. DohertyBone ( NHM 2013.441 ).
Paratype: Same data as Holotype ( NHM 2013.442 1 preadult ex.) .
Remarks: The new species differs from the other two Okudrilus species in the position of the spermathecal pores located in intersegmental furrow 12/13 (11 in O. sulcatus , 12 in O. nyosensis ) and furthermore in the structure of the ovo-spermathecal apparatus. Habitat consists of loamy soil in high elevation (> 2000 m) sub-alpine grassland.
T |
Tavera, Department of Geology and Geophysics |
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