Paracaudina reductia, Davey, Nicola & O’Loughlin, Mark, 2013

Davey, Nicola & O’Loughlin, Mark, 2013, The caudinid sea cucumbers of New Zealand (Echinodermata: Holothuroidea: Molpadida: Caudinidae), Zootaxa 3613 (4), pp. 357-368 : 366

publication ID

https://doi.org/ 10.11646/zootaxa.3613.4.3

publication LSID

lsid:zoobank.org:pub:8CB909FF-24BF-4083-A113-A32C872DCF67

DOI

https://doi.org/10.5281/zenodo.6153066

persistent identifier

https://treatment.plazi.org/id/DAF1E47A-2429-4C6C-AFAC-03C076DF7D71

taxon LSID

lsid:zoobank.org:act:DAF1E47A-2429-4C6C-AFAC-03C076DF7D71

treatment provided by

Plazi

scientific name

Paracaudina reductia
status

sp. nov.

Paracaudina reductia View in CoL sp. nov.

Figures 1 View FIGURE 1 f, 7

Paracaudina species O’Loughlin et al. (2011)

Material examined. Holotype. New Zealand, Chatham Rise, NIWA 70957, Cruise 2029/Stn V371, 43.00 S, 179.00 E, 546 m, 12/09/1989.

Description. Paracaudina species up to 37 mm total length, diameter up to 6 mm, caudal taper and long discrete tail 15 mm long; body wall parchment like and flexible, prickly, finely wrinkled anteriorly and posteriorly, tail brittle.

Ossicles in mid-body wall and tail are marginally knobbed octagonal closed cups with a basal cross central superstructure reduced to a small X or H-shape, up to 70 µ m long, and with approximately 8 marginal perforations and a large central one beneath the cross.

Colour (preserved). White

Distribution. New Zealand: Chatham Rise, 546 m.

Etymology. From the Latin reductio (reduced), referring to the reduced cross superstructure that characterise the knobbed closed cup ossicles in this species.

Remarks. O’Loughlin et al. (2011) illustrated the body wall ossicles of a single specimen of a Paracaudina species from Chatham Rise and suspected it to be new. This same specimen is here described as P. re d u c t i a sp. nov. We have added some ossicle and specimen photos to further illustrate the single specimen. P. re d u c t i a is distinguished from other New Zealand species of Paracaudina by the distinctly reduced nature of the nonperforated central cross superstructure on the ossicle. This reduced cross sometimes appears as a low H-shape and the specimen does not exhibit any of the ossicle types of P. chilensis or P. coriacea , as stated by O’Loughlin et al. (2011).

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