MolluscaBase name details

Arkansia macneili Modell, 1957 †

1536128  (urn:lsid:marinespecies.org:taxname:1536128)

 unaccepted > superseded combination
Species
marine, brackish, fresh, terrestrial
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  PDF available [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 2024-02-23
Date
action
by
2021-08-29 08:16:36Z
created
2022-09-14 06:44:10Z
changed

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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  PDF available [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  PDF available [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]

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