Kolaptokonus - Colaptoconus

Kolaptokonus
Vaqtinchalik diapazon: 478.6–468.1 Ma
Conodonts00.jpg
D_E, F Colaptoconus quadraplicatus (Branson va Mehl)
tafsilot
Missurining janubi-sharqidagi Gasconade, Roubidoux va Jefferson Siti shakllanishidagi ba'zi vakili kondont elementlarning elektron mikroskopini (SEM) skanerlash. Tasvirlangan namunalar Paleobiologiya bo'limi, AQSh Milliy muzeyi (USNM), Vashington, Kolumbiya, 20560 y.
D_E, Colaptoconus quadraplicatus (Branson va Mehl); mos ravishda triplicatiform va quadraplicatiform elementlarning posterolateral (D) va lateral (E) ko'rinishlari; D, JF-H namunasidan, Jaklar vilkasi bo'limi, X 110, USNM 498499; J, JC-J namunasidan, Jim's Creek qismidagi Jefferson Siti Dolomitning pastki qismi, X 64, USNM 498500. F, qarang. Colaptoconus quadraplicatus (Branson va Mehl); sayoz yivli namuna, JF-J namunasidan Jacks Fork qismida, X 90, USNM 498501.
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Kolaptokonus

Turlar
  • Colaptoconus emarginatus
  • Colaptoconus quadraplicatus
Sinonimlar

Glyptoconus Kennedi, 1981 (sin. Glyptoconus fon Moellendorff, 1894)[1]

Kolaptokonus qirilib ketgan jins kondontslar.

Adabiyotlar

  1. ^ Colaptoconus (Conodonta), Glyptoconus Kennedy uchun almashtirilgan ism, 1981, Glyptoconus von Moellendorff, 1894. Devid J. Kennedi, Paleontologiya jurnali, 1994 yil noyabr, 68-jild, 6-son (havola )
  • S. Desbiens, T. E. Bolton va A.D. Makkracken. 1996. Quyi Boharnois formasiyasining hayvonot dunyosi (Beekmantown Group, Quyi Ordovik (, ​​Grand íle, Quebec. Kanadaning Journal of Earth Science) 33 (8): 1132-1153

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