Eocaudina? subhexagona


Sugerowana cytacja: Piotr Gryz 2020. Eocaudina? subhexagona Gutschick, Canis et Brill 1967. Ikonoteka (http://ikonoteka.paleo.pan.pl/xwiki/bin/viewrev/Species/Eocaudina+subhexagona)

Diagnoza

 See Gutschick et al. 1967


Porównanie

These sclerites are possibly partially non−holothurian in origin. Possibly these are the elements of the central disc of ophiuroids or of the thecal plates of echinoids.

Autekologia


Występowanie geograficzne

Falcovec, Bulgaria; set G1 of Psie Górki, Holy Cross Mountains, Poland;  borehole  Chojnice  2  (3123,7–3129,9  m),  Pomerania,  Poland;  Lodgepole  Limestone, Allan Mountain Limestone, Madison County, Montana; Chouteau, Missouri; Compton Limestone, Cedar County, Missouri and Chappel Limestone, Central Texas, USA.

Zasięg czasowy

Late Frasnian to Tournaisian.?pieces of Devonian limestone in Carboniferous molasse (Westphalian D).

Materiały muzealne

GIUS 56 sieve plates.

Literatura

Boczarowski, A. 2001. Isolated sclerites of Devonian non-pelmatozoan echinoderms. Palaeontologia Polonica 59, 3–220.

Gutschick, R.C., Canis W.F., & Brill, K.G.Jr. 1967. Kinderhook (Mississippian) holothurian sclerites from Montana and Missouri. Journal of Paleontology 41, 1461–1480.


Specyfikacja

Królestwo
ANIMALIA 

Typ
ECHINODERMATA

Podtyp
ELEUTHEROZOA

Gromada
HOLOTHURIOIDEA

Rząd
Dendrochirota

Rodzina
Calclamnidae

Podrodzina
Eocaudiniinae

Gatunek
Eocaudina? subhexagona

Synonimy

Populacja typowa gatunku

Holotyp

Holotype: UND 102, Gutschick et al. 1967: text−fig. 16 

Locus typicus

Not specified, Montana, USA.

Stratum typicum

Tournaisian, Lodgepole Limestone


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Created by Administrator on 2020/04/23 17:22

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