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Barbatia suzzalloi

Bivalvia - Arcida - Arcidae

Taxonomy
Arca (Barbatia) suzzalloi was named by Weaver and Van Winkle Palmer (1922). Its type specimen is UW (unknown number), a shell, and it is a 3D body fossil. Its type locality is UW 324, which is in a Bartonian marine horizon in the Cowlitz Formation of Washington.

It was recombined as Barbatia (Barbatia) suzzalloi by Reinhart (1943); it was recombined as Barbatia suzzalloi by Hendy (2020).

Synonymy list
YearName and author
1922Arca (Barbatia) suzzalloi Weaver and Van Winkle Palmer p. 8 figs. pl. 8, fig. 6
1943Barbatia (Barbatia) suzzalloi Reinhart p. 29 figs. PI. 1, figs. 14-16
2020Barbatia suzzalloi Hendy

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RankNameAuthor
kingdomAnimalia()
Bilateria
EubilateriaAx 1987
Protostomia
Spiralia
superphylumLophotrochozoa
phylumMollusca
classBivalvia
Eubivalvia
RankNameAuthor
subclassAutobranchia(Groblen 1894)
infraclassPteriomorphia(Beurlen 1944)
OstreomorphiFerussac 1822
ArcioniGray 1854
orderArcida(Stoliczka 1871)
superfamilyArcoidea(Lamarck 1809)
familyArcidaeLamarck 1809
genusBarbatiaGray 1842
speciessuzzalloi()

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.

Barbatia suzzalloi Weaver and Van Winkle Palmer 1922
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Diagnosis
ReferenceDiagnosis
C. E. Weaver and K. Van Winkle Palmer 1922Shell small, elongate in outline; inequilateral, beaks situated
one-third the distance from the anterior end ; dorsal margin straight ; anterior
end nearly straight, sloping at about an angle of 15 with the dorsal margin,
passing into the ventral margin with a broad bow ; ventral margin straight,
produced obliquely ; posterior margin broadly pointed at the ventral end, sloping
to the dorsal margin at about an angle of 40 ; a mid-umbonal sulcus extends to
the ventral margin, sloping obliquely from the beaks ; surface sculptured by concentric
lines of growth crossed by numerous fine, delicate, radiating ribs which
bifurcate, forming two ribs of equal width on the lower region. The bifurcation
of the ribs occurs over the whole of the shell including the posterior as well
as the anterior region of concaveness. Under the microscope these ribs show
a beaded character, which are most numerous on the anterior, umbonal slope;
cardinal area very narrow.
Measurements
No measurements are available
Composition: aragonitef
Entire body: yesf
Adult length: 10 to < 100f
Adult width: 10 to < 100f
Adult height: 10 to < 100f
Thickness: intermediatef
Folds: minorf
Ribbing: majorf
Spines: nonef
Internal reinforcement: nonef
Ontogeny: accretionf
Environment: lagoonal, coastal, inner shelf, outer shelf, oceanic, brackish, freshwaterf
Locomotion: stationaryg
Attached: yesg
Life habit: epifaunalg
Diet: suspension feederg
Vision: limitedf
Created: 2004-02-29 17:10:35
Modified: 2009-09-09 11:04:23
Source: g = genus, f = family
References: Mikkelsen and Bieler 2008, Aberhan et al. 2004

Age range: Bartonian or 41.30000 to 38.00000 Ma

Collections (2 total)


Time interval Ma Country or state Original ID and collection number
Bartonian41.3 - 38.0USA (California) Barbatia suzzalloi (52827)
Bartonian41.3 - 38.0USA (Washington) Arca suzzalloi (type locality: 201121)