MolluscaBase name details
Leptesthes chingshanense Grabau, 1923 †
1510884 (urn:lsid:marinespecies.org:taxname:1510884)
unaccepted > superseded combination
Species
fossil only
Grabau, A. W. (1923). Cretaceous fossils from Shantung. <em>Bulletin of the Geological Survey of China.</em> 5(2): 143-181.
page(s): 147-149, textfig. 1 [details]
page(s): 147-149, textfig. 1 [details]
Note "in the gray shales which form the basal part...
Type locality "in the gray shales which form the basal part of the Chingshan Formation which disconformably overlies the Laiyang Formation in the Laiyang Valley" [Shandong Province, China] [details]
MolluscaBase eds. (2021). MolluscaBase. Leptesthes chingshanense Grabau, 1923 †. Accessed at: https://molluscabase.org/aphia.php?p=taxdetails&id=1510884 on 2025-09-10
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original description
Grabau, A. W. (1923). Cretaceous fossils from Shantung. <em>Bulletin of the Geological Survey of China.</em> 5(2): 143-181.
page(s): 147-149, textfig. 1 [details]
basis of record Martinson, G. G. (1961). Mezozoiskie i Kaynozoyskie Molluski Kontinentalnykh Otlozheniy Sibirskoy Platformy, Zabaykalya i Mongolii [Mesozoic and Cenozoic Mollusca of the continental deposits of the Sibirican platform, Transbaikalia and Mongolia]. <em>Trudy Baikal'skoi Limnologicheskoi Stantsii [Transactions of Baikalian Limnologic Station].</em> 19:1–332 p., 26 pl. In Russian.
page(s): 230, 231 [details] Available for editors
[request]
page(s): 147-149, textfig. 1 [details]
basis of record Martinson, G. G. (1961). Mezozoiskie i Kaynozoyskie Molluski Kontinentalnykh Otlozheniy Sibirskoy Platformy, Zabaykalya i Mongolii [Mesozoic and Cenozoic Mollusca of the continental deposits of the Sibirican platform, Transbaikalia and Mongolia]. <em>Trudy Baikal'skoi Limnologicheskoi Stantsii [Transactions of Baikalian Limnologic Station].</em> 19:1–332 p., 26 pl. In Russian.
page(s): 230, 231 [details] Available for editors
[request]
Present Inaccurate Introduced: alien Containing type locality
From editor or global species database
Type locality "in the gray shales which form the basal part of the Chingshan Formation which disconformably overlies the Laiyang Formation in the Laiyang Valley" [Shandong Province, China] [details]
