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Cummingella : ウィキペディア英語版
Cummingella

''Cummingella'' is a genus trilobite that lived during from the earliest Carboniferous until the Middle Permian. Its remains have been found in Belgium, the Czech Republic, France, Germany, the Netherlands, Slovenia, Spain, the United Kingdom and the United States.
== Distribution ==

* ''C. arbizui'' was found in the Lower Carboniferous of Spain (Tournaisian, Perna Formation, 1.450 m SSE of Cerro de Perna, 5 km SE of Aliseda, Cáceres).〔 ''cited in'' 〕
* ''C. auge'', ''C. carringtonensis'', ''C. insulae'', and ''C. tuberculigenata'' occur at the Lower Carboniferous of the United Kingdom (Asbian, Bee Low Limestones Formation, Treak Cliff, England).〔 ''cited in'' 〕
* ''C. auge'' was excavated from the earliest Carboniferous of the Czech Republic (Tournaisian, ''Scaliognathus anchoralis''-conodont zone, Brezina Formation, near Mokra village)〔 ''cited in'' 〕 and Germany (Tournaisian, Erdbach Limestone Formation, quarry at north-western margin of Steeden, Hessen;〔 ''cited in'' 〕 and quarry and slope at the Iberg-Winterberg, Bad Grund, Harz, Lower Saxony).〔 ''cited in'' 〕
* ''C. belisama'' is present in the Lower Carboniferous of Belgium (Tournaisian; Carrières Gauthier-Wincqz Soignies, Carrières Cimescaut, Antoing, Modave Shale, Huy, Carrière do Clypot, Neufville-lez-Soignies; Hainaut)〔(【引用サイトリンク】title= Primary (Paleozoic) - Lower Carboniferous - Tournaisian (345-335 MA) )〕〔 ''cited in'' 〕〔 ''cited in'' 〕 and the Netherlands (IJburg, Amsterdam).
* ''C. boikoi'' is known from the Lower Permian of the Russian Federation (Sakmarian, Tastuba quarry, Voznesenka, Bashkortostan).
* ''C. carringtonensis'' has been found in the Lower Carboniferous of Belgium (Viséan; Tournaisian, Heibaart, Louenhout),〔 ''cited in'' 〕 Germany (Velbert "Am Wasserfall").〔 ''cited in'' 〕 and the United Kingdom (Asbian, Hopedale Limestones Formation, Gateham Hill, England;〔 ''cited in'' 〕 and Benburb type section (Viséan, Gorestown Mudstone Member, Blackstokes Limestone Formation, Northern Ireland).〔 ''cited in'' 〕
* ''C. jonesii'' comes from earliest Carboniferous of France (Tournaisian, Mitzach, Southern Vosges, Alsace)〔 ''cited in'' 〕 and Germany (Ratingen; Sondern, quarry east of Sondern).〔 ''cited in'' 〕
* ''C. laticaudata'' occurs in the Lower Carboniferous of the United Kingdom (Viséan, Monsal Dale Limestones Formation, Mich Low, England).〔 ''cited in'' 〕
* ''C. raniceps'' is present in the Carboniferous of the United Kingdom (Visean, Milldale Limestone Formation, Thorpe Cloud, England).〔 ''cited in'' 〕
* ''C. slovenica'' occurs in the Lower Permian of Slovenia (Asselian, Dolzanova Soteska Formation, Na Peceh, North of Jesenice, Karavanke Mountains).〔 ''cited in'' 〕

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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