Higashi-Tanakura Group Kubota Fm Molluscan Fauna Locality 7: Late/Upper Miocene, Japan

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Gastropoda - Neotaenioglossa - Calyptraeidae
Crepidula sp. Lamarck 1799
Gastropoda - Cerithiidae
Cerithium kobelti
Gastropoda - Turritellidae
Turritella tanaguraensis
Gastropoda - Naticidae
Sinum yabei Otuka 1934
synonym of Sinum ineptum
Neverita kiritaniana (Yokoyama 1931)
synonym of Glossaulax didyma
Gastropoda - Neogastropoda - Cancellariidae
Cancellaria hukusimana
Gastropoda - Neogastropoda - Buccinidae
Siphonalia cf. spadicea
Phos iwakianus
Gastropoda - Neogastropoda - Nassariidae
Nassarius acutidentatus
Bivalvia - Cardiida - Ungulinidae
Felaniella usta
synonym of Diplodonta
Bivalvia - Cardiida - Veneridae
Mercenaria chitaniana
Protothaca tateiwai
synonym of Leukoma
Dosinia kaneharai
Dosinia japonica
Bivalvia - Cardiida - Tellinidae
Macoma incongrua (Martens 1865)
recombined as Macoma (Macoma) incongrua
Bivalvia - Cardiida - Cardiidae
Laevicardium shiobarense
Bivalvia - Lucinida - Lucinidae
Lucinoma annulata (Reeve 1850)
recombined as Lucinoma annulatum
Bivalvia - Pectinida - Anomiidae
Anomia cytaeum
Bivalvia - Ostreida - Ostreidae
Ostrea gravitesta
Bivalvia - Arcida - Arcidae
Anadara ninohensis
Dominant species at locality
see common names

Geography
Country:Japan
Coordinates: 37.5° North, 140.0° East (view map)
Paleocoordinates:38.9° North, 138.4° East
Basis of coordinate:based on political unit
Geographic resolution:local area
Time
Period:Neogene Epoch:Miocene
10 m.y. bin:Cenozoic 6
Key time interval:Late/Upper Miocene
Age range of interval:11.63000 - 5.33300 m.y. ago
Stratigraphy
Geological group:Higashi-Tanakura Formation:Kubota
Stratigraphic resolution:formation
Stratigraphy comments: Higbashi-Tanajura group is a marine representative of the regressive Genjigawa stage
Lithology and environment
Primary lithology:medium,micaceous,gray,blue lithified argillaceous sandstone
Secondary lithology:fine,micaceous,black,blue lithified argillaceous sandstone
Includes fossils?Y
Includes fossils?Y
Lithology description: massive medium sandstone in the lower part and massive fine sandstone with intercalations of several ash tuff layers in the central and upper part of the basin...characterized by abundant occurrence of molluscan fossils. Bluish-gray medium to fine sandstone covers (beds below) and consists mainly of quartz and mica grains with argillaceous materials. It is fine in the west, and becomes coarser eastward...The medium sandstone is covered by massive fine sandstone in the southern area. This fine sandstone is bluish-black colored, massive, homogeneous, argillaceous and rich in mica flakes. Several white fine ash tuff layers are intercalated in the middle part of the fine sandstone. They are concentrated in three restricted horizons. Coarse sandstone lenses, rich in shell fragments and quartz grains are found at Okada. They are more than 10m in thickness and are contemporaneous with the fine sandstone and diminish laterally into the fine sandstone.
Environment:marginal marine indet.
Geology comments: Lateral and vertical changes of lithofacies indicate that the group had been accumulated in the course of a local transgression and regression. Sediment is supplied from Abukuma mountain block. Paleogeographically, Higashi-Tanakura group is the deposits filling up a small shallow embayment open to the north.
Taphonomy
Modes of preservation:body
Collection methods and comments
Reason for describing collection:paleoecologic analysis
Metadata
Also known as:Locality 7
Database number:52112
Authorizer:A. Miller Enterer:K. Bulinski
Modifier:K. Bulinski Research group:marine invertebrate
Created:2005-07-25 13:20:30 Last modified:2005-08-01 11:58:34
Access level:the public Released:2005-07-25 13:20:30
Creative Commons license:CC BY
Reference information

Primary reference:

13978. Y. Iwasaki. 1970. The Shiobara-type Molluscan Fauna: An ecological analysis of fossil molluscs. Journal of the faculty of science, University of Tokyo, Section 2 17(3):351-444 [A. Miller/K. Bulinski/K. Bulinski]