Basic info | Taxonomic history | Classification | Included Taxa |
Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Idiospira longa
Taxonomy
Cyclospira longa was named by Cooper (1956) [Cyclospira? longa]. Its type specimen is USNM 111390, a shell, and it is a 3D body fossil. Its type locality is Near Albany, which is in a Trentonian carbonate conglomerate/limestone in the Rysedorf Formation of New York.
It was recombined as Idiospira longa by Candela and Harper (2014).
It was recombined as Idiospira longa by Candela and Harper (2014).
Synonymy list
Year | Name and author |
---|---|
1956 | Cyclospira longa Cooper pp. 693 - 694 figs. Plate 142, 1, figures 39-43 |
1962 | Cyclospira longa Williams pp. 251 - 252 figs. P1. XXIII, figs. 24, 27, 32 |
2014 | Idiospira longa Candela and Harper p. SI |
Is something missing? Join the Paleobiology Database and enter the data
|
|
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.
†Idiospira longa Cooper 1956
show all | hide all
Diagnosis
Reference | Diagnosis | |
---|---|---|
G. A. Cooper 1956 | Shell small, pentagonal in outline, longer than wide with the greatest width at about the middle. Beak acute ; shell posterior to middle narrowing rapidly to the beak ; sides somewhat narrowly rounded ; anterior margin narrow and gently rounded. Anterior part of anterolateral extremities marked by 2 costae ; surface without other ornament than the costae and folds.
Pedicle valve about twice as deep as the brachial valve, moderately convex and with the greatest convexity slightly posterior to the middle. Beak moderately incurved. Umbo narrowly swollen. Fold low, extending to a point slightly anterior to the middle where it passes into 2 narrowly rounded costae bounding a narrow sulcus. Flanks gently concave and with steep slopes to the margins. Brachial valve evenly and gently convex in lateral profile, with greatest convexity at about the middle. Posterior half slightly swollen and marked by a shallow and narrow depression that marks the position of the median septum. Sulcus originating slightly anterior to the middle, widening rapidly to the margin where it occupies about half the valve width. Sulcus for its entire length occupied by a narrowly rounded fold bearing a slight median longitudinal groove. Furrows defining median fold deep; folds bounding sulcus low but narrowly rounded. Median septum extending to point of origin of median fold. | |
A. Williams 1962 | Small, subpentagonal Cyclospira almost nine-tenths as wide as long with a deep, convex pedicle valve inflated to a low fold medianly but flattening laterally and a brachial valve which is gently convex posteriorly and broadly sulcate anterior/y; ventral fold dividing into a pair of costae anteriorly with 3 additional faint costae ornamenting the flanks; teeth small, probably without dental lamellae, ventral muscle area not impressed; hinge-plate divided, supported by a conspicuous median septum extending anteriorly for over one-half the length of the brachial valve. |
Measurements
No measurements are available
|
|
||||
|
|
||||
|
|||||
|
|
||||
|
|
||||
Source: o = order, c = class, p = phylum, uc = unranked clade | |||||
References: Nesnidal et al. 2013, Aberhan et al. 2004 |
Age range: Burrellian or 456.60000 to 452.50000 Ma
Collections (5 total)
Time interval | Ma | Country or state | Original ID and collection number |
---|---|---|---|
Trentonian | USA (New York) | Cyclospira longa (164925) | |
Burrellian | United Kingdom (Scotland) | Cyclospira longa (165038 165046 165048 165050) |