2016년 12월 7일 수요일

Inoceramus

Inoceramus

Inoceramus
The habitation generation: 189–66 Ma
InoceramusCretaceousSouthDakota.jpg
An inoceramus of the Cretaceous system which I produced from South Dakota.
Maintenance situation evaluation
The extinction (fossil)
The geological age
The end of the – Cretaceous in the first half of the Jurassic for the Mesozoic
Classification
: Animal kingdom Animalia
Subkingdom : Genuine Metazoa subkingdom Eumetazoa
There is no rank : (unfiled [1])
Bilateria Bilateria
(unfiled)
Old mouth animal super gate Protostomia


The upper gate : It is gate Lophotrochozoa in a crown ring animal
The gate : Mollusca Mollusca
Rope : Ax foot rope Bivalvia
There is no rank : Inherent valve gills subclass
Autolamellibranchia
Subclass : Alary subclass Pteriomorphia
Gradation scale : Eupteriomorphia
Eyes : Persimmon eyes Ostreoida
Course : Inoceramus department Inoceramidae
The genus : Inoceramus Inoceramus
(Sowerby, 1814)

The inoceramus (a scientific name: Inoceramus) is one genus of the bivalve belonging to alary subclass, persimmon eyes, inoceramus department. The scientific name means "a firm pot" in Greek.

Table of contents

Biologic characteristic

The inoceramus has a thick husk with the pearlescence by "prism" of the calcite [2]. The inoceramus is known how many a kind becoming considerably large is, but thinks that the paleontologist let you make gills big to be able to live in the water of the lack of oxygen state that I eutrophicated [2].

Distribution

The inoceramus was distributed over the whole world over (approximately 189,600,000 years - approximately 66,040,000 years) in the Cretaceous from the Jurassic [3]. Many kinds are reported from the Pierre shale which is the sediment of the western part inland sea route which there was in the North America. Canada Vancouver Island [2], Greenland, Spain, France, Germany, Japan, the production in Alaska are known in other areas. A large-scale kind (I.(Sphenoceramus) steenstrupi) to become 187cm is reported in Greenland in particular (cf. gallery).

Gallery

Documents

  • W. J. Kennedy, E. G. Kauffman, and H. C. Klinger. 1973. Upper Cretaceous Invertebrate Faunas from Durban, South Africa. Geological Society of South Africa Transactions 76(2): 95-111
  • H. C. Kinger and W., J. Kennedy. 1980. Upper Cretaceous ammonites and inoceramids from the off-shore Alphard Group of South Africa. Annals of the South African Museum 82(7): 293-320
  • Ludvigsen, Rolf & Beard, Graham. 1997. West Coast Fossils: A Guide to the Ancient Life of Vancouver Island. pg. 102-103
  • H. Gebhardt. 2001. Inoceramids, Didymotis and ammonites from the Nkalagu Formation type locakity (late Turonian to Coniacian, southern Nigeria): biostratigraphy and palaeoecologic implications). Neues Jahrbuch für Geologie und Palaeontologie, Monatshefte 2001 (4): 193-212
  • G. M. El Qot. 2006. Late Cretaceous macrofossils from Sinai, Egypt. Beringeria 36:3-163

Footnote

  1. The rank that is unfiled in ^ taxonomy now. As well as the following.
  2. ^ a b c Ludvigsen, Rolf & Beard, Graham. 1997. West Coast Fossils: A Guide to the Ancient Life of Vancouver Island. pg. 102-103
  3. ^ Inoceramus at Fossilworks

This article is taken from the Japanese Wikipedia Inoceramus

This article is distributed by cc-by-sa or GFDL license in accordance with the provisions of Wikipedia.

Wikipedia and Tranpedia does not guarantee the accuracy of this document. See our disclaimer for more information.

In addition, Tranpedia is simply not responsible for any show is only by translating the writings of foreign licenses that are compatible with CC-BY-SA license information.

0 개의 댓글:

댓글 쓰기