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Parallelodus obliquus

Bivalvia - Modiomorphida - Modiomorphidae

Taxonomy
Parallelodus obliquus was named by Branson (1909) [DISTRIBUTION: Middle Ordovician; Missouri.]. Its type specimen is Walker Museum 11534, a shell, and it is a 3D body fossil. Its type locality is Residuary Auburn Chert Beds, east of Auburn , which is in a Turinian carbonate claystone in the Decorah Formation of Missouri.

It was corrected as Parallelodus obliqua by Foerste (1920).

Sister species lacking formal opinion data

Synonymy list
YearName and author
1909Parallelodus obliquus Branson p. 43 figs. Pl. vii. f. .9-10.
1920Parallelodus obliqua Foerste p. 206
1969Parallelodus obliquus Cox et al. p. N398

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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
orderModiomorphida(Newell 1969)
superfamilyModiomorphoidea(Miller 1877)
familyModiomorphidae
genusParallelodusBranson 1909
speciesobliquus

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.

Parallelodus obliquus Branson 1909
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Diagnosis
ReferenceDiagnosis
E.B. Branson 1909Shell obliquely subovate, strongly convex, maximum length observed forty millimeters, width half the length, widest at posterior end of hinge. Hinge plate nearly straight, about half the length of the shell. Beaks situ ated slightly in front of the middle of the hinge line. One tooth anterior and one posterior to beaks in right valve; two teeth anterior and two posterior to beaks in left valve. Teeth long, almost parallel to hinge line. The anterior margin of the shell curves abruptly downward from the hinge to the ventral margin, ventral margin moderately and evenly convex, posterior margin passing downward and backward in a nearly straight line to the ventral margin. Umbones prominent, curving inward over the hinge line. An umbonal ridge, prominent for half the length of the shell, extends backward to the pos tero-ventral margin. Surface of shell marked with rather coarse concentric striae, faintly impressed on casts. Mus cular scars not traceable on casts.
Measurements
No measurements are available
Composition: aragonitec
Entire body: yesf
Adult length: 10 to < 100f
Adult width: 10 to < 100f
Locomotion: stationaryf
Attached: yesf
Life habit: epifaunalf
Diet: suspension feederf
Vision: blindc
Created: 2009-06-11 18:04:52
Modified: 2009-10-10 17:34:00
Source: f = family, c = class
References: Hendy 2009, Aberhan et al. 2004

Age range: Turinian or 457.30000 to 453.80000 Ma

Collections (2 total)


Time interval Ma Country or state Original ID and collection number
Turinian457.3 - 453.8USA (Missouri) Parallelodus obliqua (181091) Parallelodus obliquus (type locality: 175724)