MolluscaBase name details
Arkansia macneili Modell, 1957 †
1536128 (urn:lsid:marinespecies.org:taxname:1536128)
unaccepted > superseded combination
Species
fossil only
Modell, H. (1957). Die fossilen Najaden Nordamerikas. Ein Klassifizierungsversuch. <em>Archiv für Molluskenkunde.</em> 86(4/6): 183-200.
page(s): 191 [details] Available for editors
[request]
page(s): 191 [details] Available for editors
[request]
Note "Catahoula beds, Texas". MacNeil (1935)...
Type locality "Catahoula beds, Texas". MacNeil (1935) specified the locality more clearly: "5 miles north of the town of La Grange [Fayette Co., Texas], about one-half mile northwest of the south corner of the James Green League. The fossils were found in the upper part of a quartzitic sandstone which is developed only locally about 30 to 40 feet above the base of the Catahoula formation as described after Alexander Deussen, [U. S. Geol. Survey] Professional Paper 126." [details]
MolluscaBase eds. (2024). MolluscaBase. Arkansia macneili Modell, 1957 †. Accessed at: https://www.molluscabase.org/aphia.php?p=taxdetails&id=1536128 on 2025-04-02
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original description
Modell, H. (1957). Die fossilen Najaden Nordamerikas. Ein Klassifizierungsversuch. <em>Archiv für Molluskenkunde.</em> 86(4/6): 183-200.
page(s): 191 [details] Available for editors [request]
additional source MacNeil, F.S. (1935). Fresh-water Mollusks from the Catahoula Sandstone (Miocene) of Texas. <em>Journal of Paleontology.</em> 9(1): 10-17. [details] Available for editors [request]
page(s): 191 [details] Available for editors
[request]additional source MacNeil, F.S. (1935). Fresh-water Mollusks from the Catahoula Sandstone (Miocene) of Texas. <em>Journal of Paleontology.</em> 9(1): 10-17. [details] Available for editors
[request]
Present Inaccurate Introduced: alien Containing type locality
From editor or global species database
Type locality "Catahoula beds, Texas". MacNeil (1935) specified the locality more clearly: "5 miles north of the town of La Grange [Fayette Co., Texas], about one-half mile northwest of the south corner of the James Green League. The fossils were found in the upper part of a quartzitic sandstone which is developed only locally about 30 to 40 feet above the base of the Catahoula formation as described after Alexander Deussen, [U. S. Geol. Survey] Professional Paper 126." [details]
