Proboscisambon, Havlicek and Mergl, 1982
publication ID |
https://doi.org/ 10.4202/app.2013.0010 |
persistent identifier |
https://treatment.plazi.org/id/81298792-FFE5-A24D-FFDC-FA63FB98D242 |
treatment provided by |
Felipe |
scientific name |
Proboscisambon |
status |
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Proboscisambon ? sp.
Fig. 4D, E View Fig .
Material.— Seven specimens embedded in rock. Porkuni Regional Stage , Kuldiga Formation , Hirnantian ( Upper Ordovician ); southwestern Estonia and western Latvia. Drill core and depth (in meters) of sample intervals with brachiopods. Depth interval of fragmentary specimens is marked by “?”. Collection GIT 542 View Materials : Aizpute-41, 997.7–1000.35; Stirnas-18, 908.2; Riekstini-15, 858.6; Ruhnu-500, 613.5; Vilcini-15, 909.5;? Prabut Formation ( Podhalańska 2009): Petrobaltic S-8, 2618.2–2618.28 (sample 47 from the interval 2614.4– 2633 m) .
Remarks.—Small, laterally elongated shells, up to 6.5 mm wide and 4.2 mm long with weakly developed ornament of concentric filae and few costae (nine on the largest valve) appearing at about 2.5 mm from the umbo reminiscent of the genus Proboscisambon first described from Bohemia ( Havlíček and Mergl 1982). The Baltic specimens have obtuse cardinal angles and almost flat valves. The studied specimens are similar to those Paramalomena in having a fine radial ornament differing in lacking the growth lines characteristic of that genus. Depending on preservation, the small Glyptomeninae may be erroneously assigned to the genus Foliomena ; see for example, one specimen (GIT 542-53) from the lowermost Porkuni Regional Stage in the Stirnas-18 core ( Hints et al. 2010). This specimen, in fact, belongs to the genus Proboscisambon .
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