MolluscaBase taxon details

Lioplacodes shouchangensis H.-Z. Pan, 1980 †

1328477  (urn:lsid:marinespecies.org:taxname:1328477)

accepted
Species
marine, brackish, fresh, terrestrial
fossil only
Yü, W.; Pan, H.-Z. (1980). Mesozoic Non-marine Gastropods from Zhejiang and South Anhui. In: Anonymous Divisions and correlation of the Mesozoic volcano-sedimentary rocks in Zhejiang and Anhui provinces, China. Academia Sinica, Nanking Institute of Geology and Paleontology, Nanking, pp. 135-172.
page(s): 147, pl. 1, figs 6, 7 [details]  Available for editors  PDF available [request] 
Type locality contained in Zhejiang  
type locality contained in Zhejiang [details]
Stratigraphy The species was described from the Laocun Formation. Zhang (2009) lists two different entries for homonymous formations,...  
Stratigraphy The species was described from the Laocun Formation. Zhang (2009) lists two different entries for homonymous formations, one being of Late Jurassic, the other of Early Cretaceous age. [details]
MolluscaBase eds. (2024). MolluscaBase. Lioplacodes shouchangensis H.-Z. Pan, 1980 †. Accessed at: https://www.molluscabase.org/aphia.php?p=taxdetails&id=1328477 on 2024-04-18
Date
action
by
2019-02-26 07:58:26Z
created
2019-03-04 13:35:36Z
changed
2020-03-25 10:18:25Z
changed
2021-10-08 13:28:26Z
changed

Creative Commons License The webpage text is licensed under a Creative Commons Attribution 4.0 License


original description Yü, W.; Pan, H.-Z. (1980). Mesozoic Non-marine Gastropods from Zhejiang and South Anhui. In: Anonymous Divisions and correlation of the Mesozoic volcano-sedimentary rocks in Zhejiang and Anhui provinces, China. Academia Sinica, Nanking Institute of Geology and Paleontology, Nanking, pp. 135-172.
page(s): 147, pl. 1, figs 6, 7 [details]  Available for editors  PDF available [request] 
 
 Present  Inaccurate  Introduced: alien  Containing type locality 
   

From editor or global species database
Stratigraphy The species was described from the Laocun Formation. Zhang (2009) lists two different entries for homonymous formations, one being of Late Jurassic, the other of Early Cretaceous age. [details]

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