Mississippian foraminifers from the Onimaru Formation in the Hikoroichi area, South Kitakami Belt, Northeast Japan
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引用本文:Katsumi UENO,Tomohide MIYAZAKI.2009.Mississippian foraminifers from the Onimaru Formation in the Hikoroichi area, South Kitakami Belt, Northeast Japan[J].地球学报,30(S1):82-86.
DOI:10.3975/cagsb.2009.s1.32
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作者单位E-mail
Katsumi UENO Department of Earth System Science, Faculty of Science, Fukuoka University, Fukuoka 814-0180 Japan katsumi@fukuoka-u.ac.jp. 
Tomohide MIYAZAKI Hikawanishi Junior High School, Hikawa, Shimane 699-0631 Japan  
中文摘要:Abundant foraminifers were found from the Mississippian Onimaru Formation distributed in the Hikoroichi area of the central part of the South Kitakami Belt, Northeast Japan. They include Brunsia pulchra, Archaediscus sp., Paraarchaediscus? sp., Neoarchaediscus? sp., Palaeotextularia spp., Climacammina, spp., Tetrataxis spp., Haplophragmella sp., Lituotubella? sp., Forschiella sp., Cribrospira sp., Bradyina spp., Janischewskina sp., Endothyra spp., Planoendothyra aljutovica., Endothyranopsis compressa, E. crassa, Omphalotis samarica, Eo-staffella spp., Mediocris breviscula, and several others. The Onimaru foraminiferal fauna is similar to those re-ported from MFZ (Mamet Foraminiferal Zone) 15-16. This supports a late Visean (V3b-V3c) age of the formation, which has been proposed previously by rugose corals.
中文关键词:Mississippian foraminifers  Northeast Japan  Onimaru Formation  South Kitakami Belt  Visean
 
Mississippian foraminifers from the Onimaru Formation in theHikoroichi area, South Kitakami Belt, Northeast Japan
Abstract:Abundant foraminifers were found from the Mississippian Onimaru Formation distributed in the Hikoroichi area of the central part of the South Kitakami Belt, Northeast Japan. They include Brunsia pulchra, Archaediscus sp., Paraarchaediscus? sp., Neoarchaediscus? sp., Palaeotextularia spp., Climacammina, spp., Tetrataxis spp., Haplophragmella sp., Lituotubella? sp., Forschiella sp., Cribrospira sp., Bradyina spp., Janischewskina sp., Endothyra spp., Planoendothyra aljutovica., Endothyranopsis compressa, E. crassa, Omphalotis samarica, Eo-staffella spp., Mediocris breviscula, and several others. The Onimaru foraminiferal fauna is similar to those re-ported from MFZ (Mamet Foraminiferal Zone) 15-16. This supports a late Visean (V3b-V3c) age of the formation, which has been proposed previously by rugose corals.
keywords:Mississippian foraminifers  Northeast Japan  Onimaru Formation  South Kitakami Belt  Visean
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