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Mammals from the Middle Jurassic Balabansai Formation of the Fergana Depression, Kyrgyzstan. / Martin, T.; Averianov, A.O.

In: Journal of Vertebrate Paleontology, Vol. 30, No. 3, 2010, p. 855-871.

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Martin, T. ; Averianov, A.O. / Mammals from the Middle Jurassic Balabansai Formation of the Fergana Depression, Kyrgyzstan. In: Journal of Vertebrate Paleontology. 2010 ; Vol. 30, No. 3. pp. 855-871.

BibTeX

@article{c98ab115f90c434fb241965314c766dc,
title = "Mammals from the Middle Jurassic Balabansai Formation of the Fergana Depression, Kyrgyzstan",
abstract = "At least 10 (or more) mammal taxa have been identified from the Middle Jurassic (Callovian) Balabansai Formation in northern Fergana Depression, Kyrgyzstan, on the basis of mostly isolated and fragmentary teeth: docodontans cf. Simpsonodon spp., Paritatodon sp. [Paritatodon, gen. nov., is established for {\textquoteleft}Shuotherium kermacki{\textquoteright} Sigogneau-Russell, 1998, from the Bathonian of England], Tashkumyrodon desideratus, Tegotheriidae indet.; and Docodonta indet.; eutriconodontans Amphilestidae indet.; Ferganodon narynensis, cf. Ferganodon sp., and Triconodontidae indet.; {\textquoteleft}symmetrodontan{\textquoteright} Tinodontidae indet.; and cladotherians Paurodontidae indet. and Amphitheriidae indet. The occurrences of Triconodontidae, Tinodontidae, and Paurodontidae in the Balabansai Formation represent the oldest-known records of these groups. The Balabansai mammal assemblage is basically similar to the Bathonian mammals of the Forest Marble in England and the Itat mammal assemblage in Siberia respectively, revealing at present knowledge a marked",
author = "T. Martin and A.O. Averianov",
year = "2010",
doi = "10.1080/02724631003758045",
language = "English",
volume = "30",
pages = "855--871",
journal = "Journal of Vertebrate Paleontology",
issn = "0272-4634",
publisher = "Taylor & Francis",
number = "3",

}

RIS

TY - JOUR

T1 - Mammals from the Middle Jurassic Balabansai Formation of the Fergana Depression, Kyrgyzstan

AU - Martin, T.

AU - Averianov, A.O.

PY - 2010

Y1 - 2010

N2 - At least 10 (or more) mammal taxa have been identified from the Middle Jurassic (Callovian) Balabansai Formation in northern Fergana Depression, Kyrgyzstan, on the basis of mostly isolated and fragmentary teeth: docodontans cf. Simpsonodon spp., Paritatodon sp. [Paritatodon, gen. nov., is established for ‘Shuotherium kermacki’ Sigogneau-Russell, 1998, from the Bathonian of England], Tashkumyrodon desideratus, Tegotheriidae indet.; and Docodonta indet.; eutriconodontans Amphilestidae indet.; Ferganodon narynensis, cf. Ferganodon sp., and Triconodontidae indet.; ‘symmetrodontan’ Tinodontidae indet.; and cladotherians Paurodontidae indet. and Amphitheriidae indet. The occurrences of Triconodontidae, Tinodontidae, and Paurodontidae in the Balabansai Formation represent the oldest-known records of these groups. The Balabansai mammal assemblage is basically similar to the Bathonian mammals of the Forest Marble in England and the Itat mammal assemblage in Siberia respectively, revealing at present knowledge a marked

AB - At least 10 (or more) mammal taxa have been identified from the Middle Jurassic (Callovian) Balabansai Formation in northern Fergana Depression, Kyrgyzstan, on the basis of mostly isolated and fragmentary teeth: docodontans cf. Simpsonodon spp., Paritatodon sp. [Paritatodon, gen. nov., is established for ‘Shuotherium kermacki’ Sigogneau-Russell, 1998, from the Bathonian of England], Tashkumyrodon desideratus, Tegotheriidae indet.; and Docodonta indet.; eutriconodontans Amphilestidae indet.; Ferganodon narynensis, cf. Ferganodon sp., and Triconodontidae indet.; ‘symmetrodontan’ Tinodontidae indet.; and cladotherians Paurodontidae indet. and Amphitheriidae indet. The occurrences of Triconodontidae, Tinodontidae, and Paurodontidae in the Balabansai Formation represent the oldest-known records of these groups. The Balabansai mammal assemblage is basically similar to the Bathonian mammals of the Forest Marble in England and the Itat mammal assemblage in Siberia respectively, revealing at present knowledge a marked

U2 - 10.1080/02724631003758045

DO - 10.1080/02724631003758045

M3 - Article

VL - 30

SP - 855

EP - 871

JO - Journal of Vertebrate Paleontology

JF - Journal of Vertebrate Paleontology

SN - 0272-4634

IS - 3

ER -

ID: 5240860