Orostylis timucuorum, GOBERT, STEFAN, ARMONIES, WERNER, DIEZ, YANDER L., JOUK, PHILIPPE, MONNENS, MARLIES, REVIS, NATHALIE, REYGEL, PATRICK, SMITH, JULIAN III, STEENKISTE, NIELS VAN & ARTOIS, TOM, 2022

GOBERT, STEFAN, ARMONIES, WERNER, DIEZ, YANDER L., JOUK, PHILIPPE, MONNENS, MARLIES, REVIS, NATHALIE, REYGEL, PATRICK, SMITH, JULIAN III, STEENKISTE, NIELS VAN & ARTOIS, TOM, 2022, Orostylis gen. nov., a new genus of Dalytyphloplanida with seven new species (Platyhelminthes: Rhabdocoela), Zootaxa 5115 (1), pp. 29-46 : 37

publication ID

https://doi.org/ 10.11646/zootaxa.5115.1.2

publication LSID

lsid:zoobank.org:pub:E78C0947-2E8A-4663-A428-9303E84D6924

DOI

https://doi.org/10.5281/zenodo.6346937

persistent identifier

https://treatment.plazi.org/id/5A2B6C82-8F59-42B1-8B21-67A5B366D0B4

taxon LSID

lsid:zoobank.org:act:5A2B6C82-8F59-42B1-8B21-67A5B366D0B4

treatment provided by

Plazi

scientific name

Orostylis timucuorum
status

sp. nov.

Orostylis timucuorum sp. nov. Smith III

( Figs 3H View FIGURE 3 , 5 View FIGURE 5 , S 1–S View FIGURE 1 3 View FIGURE 3 )

Localities. Small beach facing the intracoastal waterway near the boat launch and pier, Whitney Marine Laboratory, FL (29°40’14”N; 81°12’57”W) Muddy sand with oyster shells and shell fragments (May 21, 2019): Type locality. Bear Island   GoogleMaps , NC (approximately 34°38’51”N; 77°07’02”W) Muddy   GoogleMaps sand-flat near tidal drainage stream (Jun., 2018). Outer   GoogleMaps sandy beach on Bogue Banks, Emerald Isle Site, NC (34°38’42”N; 77°05’23”W) Surface sediment halfway between MTL and LTL (Mar. 15, 2013). “Anne McCrary’s Mudflat” (muddy sand-flat facing the intracoastal waterway near Wilmington, NC —approximately 34°13’11”N; 77°48’49”W) (Jan. and Feb., 1970) by R. M. Rieger. Bogue Inlet, NC. Shallow subtidal in “ Amphioxus sand” (date unknown) by R. M. Rieger.

Material. Five specimens studied alive; two turned into whole mounts; one designated holotype ( FMNH KV.696); the other reference material (HU XIV.3.19); three specimens examined by confocal microscopy; three live-drawings made by R. M. Rieger .

Etymology. The specific epithet is in honour of the people (called “Timucua” by the Spanish) who first inhabited the region near the type locality.

Description. Living, sexually mature specimens from the type locality measure 705–895 µm long; all specimens possess a pair of pigmented eyes, as well as the general characters of the genus ( Fig. 5A View FIGURE 5 ). The pharynx averages 16% of the body length ( Fig. 5A View FIGURE 5 : ph; n = 3). The pharynx bears 6 club-tipped, distal tentacles ( Figs. 5A View FIGURE 5 inset, S1). Radial pharyngeal musculature is thickly arranged and pseudostriated ( Fig. 5B View FIGURE 5 : rm). The male organ is directed forward and lies just behind or beside the pharynx; testes are paired ( Figs. 5A View FIGURE 5 : t, S2). The ovary is V-shaped, with paired germinal zones, sometimes giving the impression of two ovaries ( Figs. 5A,C View FIGURE 5 : ov). The vitellarium is either very large, or paired, situated immediately behind the ovary and extending posteriorly ( Fig. 5C View FIGURE 5 : vit). A bursal tissue lies in the ventral midline at approximately the level of the ovaries ( Fig. 5A,D View FIGURE 5 : bu). Confocal microscopy reveals a musculature associated with this that appears to lead to a mid-ventral pore ( Figs. 5D,E View FIGURE 5 : red arrow). The 58-µmlong stylet ranges in length from 47 to 69 µm (n = 5), possessing a flared base with two distinct areas ( Figs. 3H View FIGURE 3 , 5F–G; 5H View FIGURE 5 : sb, st). The stylet appears to have separate pathways for sperm and prostatic secretions. The stylet has a lateral slit that extends at least partway along it ( Fig. 5F View FIGURE 5 , arrows). Squeezing apparently flattens a stylet that, at rest, comprises a base with an elongate, semi-circular tip whose point rests in a small “cup” ( Fig. 5H View FIGURE 5 : green arrow); the base and tip are in nearly orthogonal planes ( Fig. 5H View FIGURE 5 : red arrows). Connection of the male canal with the pharynx tube could not be confirmed with the material at hand.

FMNH

Field Museum of Natural History

R

Departamento de Geologia, Universidad de Chile

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