Antropora gemarita Ramalho, 2020

Ramalho, Laís V., López-Fé, Carlos M., Mateo-Ramírez, Angel & Rueda, José Luis, 2020, Bryozoa from deep-sea habitats of the northern Gulf of Cádiz (Northeastern Atlantic), Zootaxa 4768 (4), pp. 451-478 : 462-463

publication ID

https://doi.org/ 10.11646/zootaxa.4768.4.1

publication LSID

lsid:zoobank.org:pub:341C80B1-AE7A-46A9-AEC6-EE11CD1E3106

DOI

https://doi.org/10.5281/zenodo.3794581

persistent identifier

https://treatment.plazi.org/id/03C8879D-FFDD-FFA4-5887-FCCCFE5F5D9B

treatment provided by

Plazi

scientific name

Antropora gemarita Ramalho
status

 

Antropora gemarita Ramalho & López-Fé n. sp.

( Fig. 3 View FIGURE 3 B–D; Table 4)

Material examined. Holotype: MNCN 25.03 View Materials /4197: DA10, Gazul MV, 390–410 m depth, 26 June 2010, INDE- MARES CHICA project, IEO coll., on MDACs . Paratypes: MNCN 25.03 View Materials /4196: DA02, Gazul MV, 402–451 m depth, 21 June 2010 , INDEMARES CHICA project, IEO coll., on MDACs; MNCN 25.03 View Materials /4198: BT17, Pipoca MV, 564–695 m depth, 23 February 2011 , INDEMARES CHICA project, IEO coll., on shells.

Etymology. The specific name ‘ gemarita ’ is a combination of the name ‘ gemar ’ (short name of the GEociencias MARinas (Marine Geoscience) research group of the Instituto Español de Oceanografía, and ‘- ita ’ (in Latin suffix that means ‘belonging to’), in honour of the scientists and students of the GEMAR research group who helped in the INDEMARES CHICA project.

Description. Colony encrusting, uni- to multilaminar. Autozooids large, oval, distinct by shallow grooves between thin, raised rims, not disjunct ( Fig. 3B, C View FIGURE 3 ). Gymnocyst absent; cryptocyst narrower distally and laterally, more developed and asymmetrical proximally, very finely crenulated. Opesia occupying three quarters of the frontal area ( Fig. 3B, C View FIGURE 3 ). One small, interzooidal avicularium usually located at the proximal corner of each zooid, in the angular interzooidal spaces, with each autozooid surrounded by six avicularia ( Fig. 3B, C View FIGURE 3 ). Rostrum elongate-oval, rounded and slightly broader at the tip, sometimes serrated, variably directed, without crossbar ( Fig. 3C View FIGURE 3 ). Large interzooidal avicularia not observed. Ovicell endozooecial, cap-shaped, extending beneath the cryptocyst of the distal zooid ( Fig. 3D View FIGURE 3 ).

Remarks. Thirty-four species of Antropora have been described around the world, and most of them are fossil ( Bock 2019; accessed 02.12.2019). Among the Recent species, two of them— A. compressa ( Osburn, 1927) and A. minor ( Hincks, 1880b) —resemble Antropora gemarita Ramalho & López-Fé n. sp. The former species was de- scribed from the Caribbean Sea and has zooids disposed very close to each other without indication of an interopesial area. It also has interzooidal avicularia similar in shape but distally directed (in A. gemarita Ramalho & López- Fé n. sp. avicularia are variably directed), and smaller autozooids (300–400 µm long x 200–300 µm wide) ( Osburn 1927). The latter species has similar cryptocyst appearance, but smaller zooids (320–500 µm long x 150–350 µm wide) ( Tilbrook 1998), and a single avicularium (40–90 µm long).

Habitat and associated species. This species was found on MDACs intermixed with coarse sediment dominated by sponges and coral rubble (mainly of M. oculata ). It was also found in sandy mud with MDACs, sponges ( Asconema setubalense Kent), small gorgonians ( Acanthogorgia hirsuta Gray or Swiftia sp.), and echinoderms ( C. cidaris and L. phalangium ).

MV

University of Montana Museum

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