Neopetrosia subtriangularis ( Duchassaing, 1850 )
publication ID |
https://doi.org/ 10.11646/zootaxa.5004.2.2 |
publication LSID |
lsid:zoobank.org:pub:B1B2F144-2B51-4079-ACB5-6D78B38B32E7 |
persistent identifier |
https://treatment.plazi.org/id/385D87B7-FFA4-F860-2D94-FA14FD2DF849 |
treatment provided by |
Plazi |
scientific name |
Neopetrosia subtriangularis ( Duchassaing, 1850 ) |
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Neopetrosia subtriangularis ( Duchassaing, 1850) View in CoL
Brazilian records (not examined): Brazil, Maranhão State, MCNPOR 5340, 0.36667º S, 44.86667º W, 72 m depth, Coll. R. V. ‘Antares’, 2001.7.18 GoogleMaps ; MCNPOR 5003, 0.58667º S, 43.34861º W, 94 m depth, Coll. R. V. ‘Antares’, 1999.6.14 GoogleMaps .
Diagnosis. Thick ramose fragments. Smooth surface, with conspicuous oscules, 1.5–6 mm diam. Ectosome uni- to multispicular network, with triangular to polygonal meshes (80–280 μm in diam., tracts 10–90 μm thick). Choanosome with rectangular and triangular meshes (80–250 μm diam.), channels 200–440 μm diam., primary multispicular ascending tracts (up to 15 spicules across, 40–60 μm diam.), uni to plurispicular interconnecting sec- ondary tracts (20–70 μm thick). Oxeas, slightly curved, acerate, blunt to conical ends, simple or stepped, 60–230 x 2.5–6.9 μm [adapted from Campos et al. 2005].
Description. Refer to Campos et al. (2005).
Distribution. Tropical Atlantic. Brazil: Maranhão State ( Campos et al. 2005); Caribbean ( Van Soest 1980; Zea 1987; Lehnert 1993); Suriname ( Van Soest 2017).
R |
Departamento de Geologia, Universidad de Chile |
V |
Royal British Columbia Museum - Herbarium |
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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