Dacromya chetaensis Sanin 1976

• Main Authors: Hryniewicz, Krzysztof, Little, Crispin T. S., Nakrem, Hans Arne
• Format: Text
• Language: unknown
• Published: Zenodo 2014
• Subjects: Biodiversity; Taxonomy; Animalia; Mollusca; Bivalvia; Nuculanida; Nuculanidae; Dacromya; Dacromya chetaensis; Arctic; Svalbard; Slottsmøya; Zakharov; khatanga; Taimyr; Siberia; Spitsbergen
• Online Access: https://dx.doi.org/10.5281/zenodo.4929766; https://zenodo.org/record/4929766

Dacromya chetaensis Sanin, 1976 (Figure 5 O–Q) 1976 Dacromya chetaensis nov. sp. —Sanin, p. 26, pl. 6, figs. 10–11; pl. 7, figs. 1–6. Material examined. Three specimens; articulated internal moulds with some preserved shell material. See Appendix 1 for the list of specimens. Dimensions. 7–11.5 mm in length, 5.1–7.25 mm in height, 3.1–5.25 mm in width. See Appendix 2C for details. Description. Shell small, with tear-drop shaped outline. Preserved shell fragments thin, with fine, densely spaced commarginal growth lines. Moderately to strongly inflated, with greatest width medially. Shell height around two-thirds of length, reaching a maximum medially and gradually diminishing towards anterior and posterior extremities. Anterior part of shell longer than posterior, arcuate, gently tapering. Anterodorsal margin weakly convex, more inclined than anteroventral margin. Ventral margin very gently rounded. Posterior shell part shorter than anterior, rostrate, rounded, and curved dorsally. Posterodorsal margin concave, hosting deep escutcheon. Beaks opisthogyrate, lunule elongated, sunken close to beaks, emerging towards anterior. Dentition taxodont with more than 10 teeth in anterior row and 7 to 10 teeth in posterior row. Cardinal area and ligament not preserved. Anterior and posterior adductor muscle scars circular, small, adhering to pallial line and positioned close to shell extremities on inside of pallial line. Posterior adductor muscle scar connected to beak with grooves, most likely formed during descending muscle growth. Pallial line entire. Remarks. We include this species into Dacromya chetaensis Sanin, 1976, based on its shell proportions, gently arched anterior margin and external ornament. It differs from Dacromya venusta (Sauvage, 1871) from the Kimmeridgian of England (Clausen & Wignall 1990) in having a more rounded anterior margin, less sloping anterodorsal margin and an external ornament of commarginal growth lines. Dacromya chetaensis is less elongated, has more pointed umbones and shorter rostrum than D. gigantea Zakharov & Shurigin, 1974, from the Aalenian of the Taimyr Peninsula (Zakharov & Shurigin 1974; 1978). Occurrence. Seep 12 (Upper Ryazanian), Slottsmøya Member, Svalbard (Tab. 1). Known also from the Volgian–Valanginian of the Khatanga Depression, Northern Siberia (Sanin 1976). Palaeoecology. Dacromya chetaensis was probably a mobile shallow burrowing deposit feeder without a siphon, as indicated by the lack of a pallial sinus. The streamlined shell with a blunt, weakly pointed anterior and short, rostrate posterior shows that it was probably an efficient burrower. In Siberia it is associated with sandy mudstones that were deposited in a low energy, shallow water setting (Sanin 1976). This mode of life is typical for Recent nuculids, which are shallow burrowers using palps to collect sediment, which they process for organic material (Stanley 1970). : Published as part of Hryniewicz, Krzysztof, Little, Crispin T. S. & Nakrem, Hans Arne, 2014, Bivalves from the latest Jurassic-earliest Cretaceous hydrocarbon seep carbonates from central Spitsbergen, Svalbard, pp. 1-66 in Zootaxa 3859 (1) on pages 15-16, DOI: 10.11646/zootaxa.3859.1.1, http://zenodo.org/record/4930112 : {"references": ["Sanin, V. Ya. (1976) Early Cretaceous Ctenodontida of the North of Siberia. Transactions of the Institute of Geology and Geophysics, Siberian Branch of the Academy of Science of USSR, 310, 1 - 70. [in Russian]", "Sauvage, H. E. & Rigaux, E. (1871) Diagnoses d'especes nouvelles des Terrains jurassiques superieurs de Boulogne-sur-Mer (Pas de Calais). Journal de Conchology, 20, 165 - 187, pls. 8 - 12.", "Clausen, C. K. & Wignall, P. B. (1990) Early Kimmeridgian bivalves of southern England. Mesozoic Research, 2, 97 - 149.", "Zakharov, V. A. & Shurigin, B. N. (1974) Biostratigraphic and palaeobiogeographic significance of rare Middle Jurassic bivalve mollusks of the Northern Siberia. Biostratigraphy of the Boreal Mesozoic. Transactions of the Institute of Geology and Geophisics, Siberian Branch of the Academy of Science of USSR, 136, 109 - 120, pls. 9 - 10. [in Russian]", "Zakharov, V. A. & Shurigin, B. N. (1978) Biogeography, facies and stratigraphy of the Middle Jurassic of Soviet Arctic (by bivalve molluscs). Transactions of the Institute of Geology and Geophysics, Siberian Branch of the Academy of Science of USSR, 352, 1 - 206. [in Russian]", "Stanley, S. M. (1970) Relation of shell form to life habits of the Bivalvia (Mollusca). The Geological Society of America Memoir, 125, 1 - 296. http: // dx. doi. org / 10.1130 / mem 125 - p 1"]}