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Unionites subrectus

Bivalvia - Cardiida - Anthracosiidae

Taxonomy
Anodontophora subrecta was named by Bittner (1901) [= Triaphorus aff. multiformis Kiparisova sensu Kumagae & Nakazawa 2009: 171, fig. 145, 18–25.]. It is a 3D body fossil. Its type locality is Vámos-Katrabocza, which is in a Ladinian carbonate limestone in Hungary.

It was recombined as Unionites subrectus by Vörös (1987) and Foster et al. (2017).

Sister species lacking formal opinion data

Synonymy list
YearName and author
1901Anodontophora subrecta Bittner p. 100 figs. pl. 7, figs 28–30.
1987Unionites subrectus Vörös
2017Unionites subrectus Foster et al. p. 862 fig. 8

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RankNameAuthor
kingdomAnimalia()
Bilateria
EubilateriaAx 1987
Protostomia
Spiralia
superphylumLophotrochozoa
phylumMollusca
classBivalvia
Eubivalvia
subclassAutobranchia(Groblen 1894)
infraclassHeteroconchia(Gray 1854)
RankNameAuthor
CardiomorphiFerussac 1822
CardioniFerussac 1822
CardiidiaFerussac 1822
CardiataFerussac 1822
superorderCardiiformiiFerussac 1822
orderCardiidaFerussac 1822
suborderAnthracosiidinaSilantiev and Carter 2011
superfamilyAnthracosioidea(Amalizky 1892)
familyAnthracosiidaeAmalizky 1892
genusUnionitesWissman 1841
speciessubrectus()

If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.

Unionites subrectus Bittner 1901
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Diagnosis
ReferenceDiagnosis
W. J. Foster et al. 2017Outline elongate-elliptical. Shell equivalved, inflated below the umbo, and inequilateral with beak positioned approximately 85% along the length of the dorsal margin from the posterior. Lower part of anterior dorsal margin projects slightly beyond plane of commissure. Posterodorsal margin is almost straight to slightly round and gently sloping. Lunule is long and narrow, with deeply impressed escutcheon. Umbo is prosogyrate and rises above the hinge margin. Ornamented withfine concentric growth lines. The entire inner margin is smooth. Prodissoconch is smooth and orbicular.

A small subumbonal groove limits the shell projection posteriorly. Short lateral tooth, left valve possesses a weak secondary ridge creating a shallow socket. Hinge of left valve has an anterior platform that bears a depression for the corresponding anterior hinge margin of the right valve; posterior to this is a small, tuberculiform subumbonal tooth fitting above posterior lateral tooth of right valve. Ligament is fixed to a nymph, which extends about half the length of the posterior dorsal margin. Isomyarian muscle scars with a deeply impressed anterior adductor muscle scar
Measurements
partNmeanminimummaximummedians.d.
valve height287.213.4011.87.852.12

Composition: aragonitec
Locomotion: facultatively mobilec
Life habit: infaunalc
Diet: suspension feederc
Vision: blindc
Created: 2004-02-28 11:33:36
Modified: 2010-02-12 03:59:35
Source: c = class
Reference: Aberhan et al. 2004

Age range: base of the Smithian to the top of the Lacian or 251.30000 to 215.56000 Ma

Collections (16 total)


Time interval Ma Country or state Original ID and collection number
Induan252.17 - 251.2Svalbard and Jan Mayen Anodontophora subrecta (212933 212966)
Griesbachian251.902 - 250.5Svalbard and Jan Mayen Unionites subrectus (182611 182612)
Griesbachian251.902 - 250.5Greenland Anodontophora subrecta (48115)
Griesbachian251.902 - 250.5Russian Federation Triaphorus multiformis (90207)
Smithian251.3 - 247.2Russian Federation Triaphorus multiformis (90220 90221)
Anisian247.2 - 242.0Hungary Anodontophora subrecta (203401)
Anisian247.2 - 242.0Hungary (Veszprem) Unionites subrectus (43725 43730 44292)
Pelsonian247.2 - 242.0Hungary (Mecsek) Unionites subrectus (197096)
Ladinian242.0 - 237.0Hungary (Bakony) Anodontophora subrecta (type locality: 203348)
Norian - Rhaetian228.0 - 201.3Russian Federation Anodontophora subrecta (39315)
Lacian221.5 - 215.56Russian Federation Anodontophora subrecta (39313)