A new anobasicrinid (Crinoidea, Cladida) from the Upper Carboniferous of the Moscow Region
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Jimushaer sag is the main Oil and Gas unit in the eastern part of Junggar Basin,it shows good exploration prospect in Carboniferous formation by accessing to industrial oil flow of well Ji15,We can find a clear overlap and trunction featrues by the detailed study of the seismic reflection characteristics of the Carboniferous in the area,and those characteristic can be carried out a very good comparison that used for strata correlation of the Carboniferous in the area.Based on the above,we classify the Bashan Formation in Upper Carboniferous and Low Carboniferous,then we divide the tectonic units of Carboniferous in the area.These results will play an important role in the exploration of Carboniferous
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This occurrence of Septosyringothyris in Upper Carboniferous rocks increases the stratigrapnic range of the genus considerably. It was previously known from the Tournaisian only. The new species Septosyringothyris pamirensis Volgin is described. -- E. W. Bamber.
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Pleionastraea gen. nov. of the family Lithostrotionidae is described from the Lower Carboniferous Brigantian Stage of northern England. Two species, P. magna P. matura , are referred to it. This astraeoid/thamnasterioid genus is distinguished from Orionastraea by its larger dimensions, but is considered to have followed the same evolutionary trend of a gradual breakdown of the corallite wall.
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Abstract The Carboniferous ostracod Rhombina Jones and Kirkby is shown to have been misinterpreted. The genus is redescribed, a new family is erected for its reception, and a new genus, Palaeophilomedes , proposed as a second member of this family.
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The new genus Repandocosta is described for twelve North American and at least three European ostracode species that have been placed mainly in Trachyleberidea or Cythereis. Cythereis pauca Schmidt, 1948, is designated as the type species. The new genus has a stratigraphic range in North America of Coniacian [Cretaceous] to upper Eocene; in Europe it is known from middle Paleocene to upper Oligocene.
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