Lituites tenuicaulis Remelé, 1890
publication ID |
https://doi.org/ 10.5852/ejt.2022.799.1681 |
publication LSID |
lsid:zoobank.org:pub:F52DBAB0-38C7-400F-9BA1-E2D8E6B19E7E |
DOI |
https://doi.org/10.5281/zenodo.6343266 |
persistent identifier |
https://treatment.plazi.org/id/03FE5868-FFB2-3D11-DD2E-FB3CFDDEFCD6 |
treatment provided by |
Felipe |
scientific name |
Lituites tenuicaulis Remelé, 1890 |
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Lituites tenuicaulis Remelé, 1890
Figs 50–53 View Fig View Fig View Fig View Fig , Tables 9–11
Lituites tenuicaulis Remelé, 1890 : pl. 3 fig. 2.
Lituites procerus – Foerste 1932: 166, text-fig. 7.
Lituites tenuicaulis – Balashov 1953: 231, pl. 14 fig. 1. — Aubrechtová & Meidla 2020: 278.
Diagnosis
Species of the genus Lituites with the coiled conch 30 mm in diameter; 2–3 tightly coiled whorls, only the mid-part of the last whorl sometimes detached; whorl expansion rate 1.90–2.30. Uncoiled part straight in shape or slightly curved, expansion angle 2–3°. Shell surface in coiled part with fine growth lines and sharp lirae, sometimes with narrow annuli; in the backcoiled part with lirae and low annuli (after Balashov 1953; emended).
Type material
Lectotype GERMANY • Brandenburg, Oderberg; Ordovician (late Lasnamägi Regional Stage, late Darriwilian), Upper Grey Orthoceratite Limestone; Kgl. Forstakademie Eberswalde Coll.; designated by Balashov (1953); illustrated by Remelé (1890: pl. 3 fig. 2), re-illustrated here in Fig. 50A View Fig ; MB.C.5389 .
Additional material
GERMANY • 1 spec.; Brandenburg, Eberswalde; Ordovician, Upper Grey Orthoceratite Limestone; Remelé 1884 Coll.; MB.C.11651 • 2 specs; Brandenburg, Niederfinow; Ordovician, Upper Grey Orthoceratite Limestone; Neben and Krueger Coll.; MB.C.30548 , MB.C.30549 • 1 spec.; Brandenburg, Ringenwalde; Ordovician, Upper Grey Orthoceratite Limestone; Neben and Krueger Coll.; MB.C.30550 .
POLAND • 1 spec.; West Pomerania, Island of Chrząszczewska (former Gristow); Ordovician, Upper Grey Orthoceratite Limestone; Müchner Coll.; MB.C.30551 .
Description
Lectotype MB.C.5389 ( Fig. 50A View Fig ) consists of the coiled part (dm = 28 mm; 1.5 tightly coiled volutions slightly detached in the last half volution) and a part of the backcoiled part (length = 50 mm; wh = 12.4 mm; EA = 2.7°). The whorl profile is compressed (WWI = 0.88). The shell wall is preserved only in the last portion of the coiled part; there the ornament consists of sharp lirae (less than 1 mm apart) and fine growth lines between them. The backcoiled part of the specimen additionally shows imprints of annuli of about 1 mm apart. The chamber length increases during ontogeny from CLR ~ 0.36 to ~ 0.52 ( Fig. 52A–B View Fig ). The siphuncle is visible at the last preserved septum, where it has a relative diameter of 0.18 and a position of 0.32.
A more completely preserved ornament is seen in the specimen MB.C.30551 ( Fig. 50B View Fig ). In this specimen, the coiled part has lirae and narrow annuli, which grade into flat annuli after uncoiling (3–4 mm apart). The annuli of the backcoiled part have coarse lirae in between them (0.3–0.5 mm apart). The ventral sinus of ornament elements is deep and rounded ( Fig. 53 View Fig ). In the coiled part, the ornament elements are laterally straight, while in the backcoiled part, they have a shallow lateral sinus.
Specimen MB.C.30548 has a well-preserved coiled part ( Fig. 51 View Fig ), which consists of nearly two tightly coiled volutions that are slightly detached in the last half volution. By contrast to the lectotype, the chamber length in MB.C.30548 decreases during ontogeny from CLR ~ 0.40 to ~ 0.25 ( Fig. 52C–D View Fig ).
Remarks
Lituites tenuicaulis is distinguished from other species of Lituites by a comparatively large, tightly or nearly tightly coiled conch, an almost straight, slowly expanding backcoiled part and an ornament with lirae in the coiled part, low and wide annuli in the backcoiled part. In these characters, the species is similar to Trilacinoceras discors but that species has smaller, more slender and openly coiled conch.
Geographic and stratigraphic occurrence
Estonia (in situ), northern Germany and northern Poland (in erratics within Pleistocene gravels); late Darriwilian, Middle Ordovician.
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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Lituites tenuicaulis Remelé, 1890
Aubrechtová, Martina & Korn, Dieter 2022 |
Lituites tenuicaulis
Aubrechtova M. & Meidla T. 2020: 278 |
Balashov Z. G. 1953: 231 |
Lituites procerus
Foerste A. F. 1932: 166 |
Lituites tenuicaulis Remelé, 1890
Remelé 1890: 72 |