Standard

Stem therian mammal Amphibetulimus from the Middle Jurassic of Siberia. / Averianov, A.; Martin, T.; Lopatin, A.; Krasnolutskii, S.

In: Palaontologische Zeitschrift, Vol. 89, No. 2, 2015, p. 197-206.

Research output: Contribution to journal › Article

Harvard

Averianov, A, Martin, T, Lopatin, A & Krasnolutskii, S 2015, 'Stem therian mammal Amphibetulimus from the Middle Jurassic of Siberia', Palaontologische Zeitschrift, vol. 89, no. 2, pp. 197-206. https://doi.org/10.1007/s12542-013-0217-x

APA

Averianov, A., Martin, T., Lopatin, A., & Krasnolutskii, S. (2015). Stem therian mammal Amphibetulimus from the Middle Jurassic of Siberia. Palaontologische Zeitschrift, 89(2), 197-206. https://doi.org/10.1007/s12542-013-0217-x

Vancouver

Averianov A, Martin T, Lopatin A, Krasnolutskii S. Stem therian mammal Amphibetulimus from the Middle Jurassic of Siberia. Palaontologische Zeitschrift. 2015;89(2):197-206. https://doi.org/10.1007/s12542-013-0217-x

Author

Averianov, A. ; Martin, T. ; Lopatin, A. ; Krasnolutskii, S. / Stem therian mammal Amphibetulimus from the Middle Jurassic of Siberia. In: Palaontologische Zeitschrift. 2015 ; Vol. 89, No. 2. pp. 197-206.

BibTeX

@article{3796e467ffe647b9a50b452551ea58a9,
title = "Stem therian mammal Amphibetulimus from the Middle Jurassic of Siberia",
abstract = "Amphibetulimus krasnolutskii is known from the Middle Jurassic (Bathonian) Itat Formation of Krasnoyarsk Territory, West Siberia, Russia, by several edentulous and three dentigerous dental fragments, preserving p1, antepenultimate, and ultimate lower molars, and by an upper molar. It is unique among stem therians by widely open trigonids on the posterior lower molars, paraconids that are higher than the metaconids and have keeled mesiolingual vertical crests, pronounced unilateral hypsodonty of the lower molars and correlated unequal alveolar borders of the dentary ramus, and a linear Meckelian groove that is not connected to the mandibular foramen and extends along the pterygoid ridge. Amphibetulimus differs from more derived stem therians by a simple unicuspid talonid without an incipient talonid basin and a distinct labial cingulum on the upper molars. The lack of an ectotympanic facet and the long linear Meckelian groove extending onto the pterygoid ridge suggest that Amphibetulimus had a derived state of",
keywords = "Mammalia Stem Theria Middle Jurassic Asia",
author = "A. Averianov and T. Martin and A. Lopatin and S. Krasnolutskii",
year = "2015",
doi = "10.1007/s12542-013-0217-x",
language = "English",
volume = "89",
pages = "197--206",
journal = "Palaontologische Zeitschrift",
issn = "0031-0220",
publisher = "Springer Nature",
number = "2",

}

RIS

TY - JOUR

T1 - Stem therian mammal Amphibetulimus from the Middle Jurassic of Siberia

AU - Averianov, A.

AU - Martin, T.

AU - Lopatin, A.

AU - Krasnolutskii, S.

PY - 2015

Y1 - 2015

N2 - Amphibetulimus krasnolutskii is known from the Middle Jurassic (Bathonian) Itat Formation of Krasnoyarsk Territory, West Siberia, Russia, by several edentulous and three dentigerous dental fragments, preserving p1, antepenultimate, and ultimate lower molars, and by an upper molar. It is unique among stem therians by widely open trigonids on the posterior lower molars, paraconids that are higher than the metaconids and have keeled mesiolingual vertical crests, pronounced unilateral hypsodonty of the lower molars and correlated unequal alveolar borders of the dentary ramus, and a linear Meckelian groove that is not connected to the mandibular foramen and extends along the pterygoid ridge. Amphibetulimus differs from more derived stem therians by a simple unicuspid talonid without an incipient talonid basin and a distinct labial cingulum on the upper molars. The lack of an ectotympanic facet and the long linear Meckelian groove extending onto the pterygoid ridge suggest that Amphibetulimus had a derived state of

AB - Amphibetulimus krasnolutskii is known from the Middle Jurassic (Bathonian) Itat Formation of Krasnoyarsk Territory, West Siberia, Russia, by several edentulous and three dentigerous dental fragments, preserving p1, antepenultimate, and ultimate lower molars, and by an upper molar. It is unique among stem therians by widely open trigonids on the posterior lower molars, paraconids that are higher than the metaconids and have keeled mesiolingual vertical crests, pronounced unilateral hypsodonty of the lower molars and correlated unequal alveolar borders of the dentary ramus, and a linear Meckelian groove that is not connected to the mandibular foramen and extends along the pterygoid ridge. Amphibetulimus differs from more derived stem therians by a simple unicuspid talonid without an incipient talonid basin and a distinct labial cingulum on the upper molars. The lack of an ectotympanic facet and the long linear Meckelian groove extending onto the pterygoid ridge suggest that Amphibetulimus had a derived state of

KW - Mammalia Stem Theria Middle Jurassic Asia

U2 - 10.1007/s12542-013-0217-x

DO - 10.1007/s12542-013-0217-x

M3 - Article

VL - 89

SP - 197

EP - 206

JO - Palaontologische Zeitschrift

JF - Palaontologische Zeitschrift

SN - 0031-0220

IS - 2

ER -

ID: 3924349