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A skeleton of the pike Esox cf. lucius L. from the Pleistocene of the Ishim-Irtysh interfluve. / Sytchevskaya, E.K.; Laukhin, S.A.; Larin, S.I.; Maksimov, F.E.; Sanko, A.F.

In: Paleontological Journal, Vol. 49, No. 5, 2015, p. 501-506.

Research output: Contribution to journalArticlepeer-review

Harvard

Sytchevskaya, EK, Laukhin, SA, Larin, SI, Maksimov, FE & Sanko, AF 2015, 'A skeleton of the pike Esox cf. lucius L. from the Pleistocene of the Ishim-Irtysh interfluve', Paleontological Journal, vol. 49, no. 5, pp. 501-506. https://doi.org/10.1134/S0031030115050135

APA

Sytchevskaya, E. K., Laukhin, S. A., Larin, S. I., Maksimov, F. E., & Sanko, A. F. (2015). A skeleton of the pike Esox cf. lucius L. from the Pleistocene of the Ishim-Irtysh interfluve. Paleontological Journal, 49(5), 501-506. https://doi.org/10.1134/S0031030115050135

Vancouver

Author

Sytchevskaya, E.K. ; Laukhin, S.A. ; Larin, S.I. ; Maksimov, F.E. ; Sanko, A.F. / A skeleton of the pike Esox cf. lucius L. from the Pleistocene of the Ishim-Irtysh interfluve. In: Paleontological Journal. 2015 ; Vol. 49, No. 5. pp. 501-506.

BibTeX

@article{50e1c7fcb5244875aa87fb458556c0a8,
title = "A skeleton of the pike Esox cf. lucius L. from the Pleistocene of the Ishim-Irtysh interfluve",
abstract = "{\textcopyright} 2015, Pleiades Publishing, Ltd. A complete skeleton of the pike Esox cf. lucius L. from the Late Pleistocene deposits of the IshimIrtysh interfluve (village of Kotochiga, Western Siberia) is described. The specimen is morphologically close to the northern pike, which presently has a circumboreal range. A number of primitive characters in the structure and dentition of the dentary and palatine resemble some Pliocene specimens, although they are rather incomplete, precluding the estimation of the taxonomic value of such characters. The preservation of scales and bones in the pike from Western Siberian suggests immediate burial in the place of its death in a lacustrine basin. The material comes from loam, with traces of a paleocryogenic texture. The underlying sand bed contains abundant shells of freshwater mollusks, suggesting that the climate was comparable to that in the Recent or even softer. The 14C dating giving the age about 25 ka (MIS3) was obtained for the first time in the horizon of buried soil at t",
author = "E.K. Sytchevskaya and S.A. Laukhin and S.I. Larin and F.E. Maksimov and A.F. Sanko",
year = "2015",
doi = "10.1134/S0031030115050135",
language = "English",
volume = "49",
pages = "501--506",
journal = "Paleontological Journal",
issn = "0031-0301",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "5",

}

RIS

TY - JOUR

T1 - A skeleton of the pike Esox cf. lucius L. from the Pleistocene of the Ishim-Irtysh interfluve

AU - Sytchevskaya, E.K.

AU - Laukhin, S.A.

AU - Larin, S.I.

AU - Maksimov, F.E.

AU - Sanko, A.F.

PY - 2015

Y1 - 2015

N2 - © 2015, Pleiades Publishing, Ltd. A complete skeleton of the pike Esox cf. lucius L. from the Late Pleistocene deposits of the IshimIrtysh interfluve (village of Kotochiga, Western Siberia) is described. The specimen is morphologically close to the northern pike, which presently has a circumboreal range. A number of primitive characters in the structure and dentition of the dentary and palatine resemble some Pliocene specimens, although they are rather incomplete, precluding the estimation of the taxonomic value of such characters. The preservation of scales and bones in the pike from Western Siberian suggests immediate burial in the place of its death in a lacustrine basin. The material comes from loam, with traces of a paleocryogenic texture. The underlying sand bed contains abundant shells of freshwater mollusks, suggesting that the climate was comparable to that in the Recent or even softer. The 14C dating giving the age about 25 ka (MIS3) was obtained for the first time in the horizon of buried soil at t

AB - © 2015, Pleiades Publishing, Ltd. A complete skeleton of the pike Esox cf. lucius L. from the Late Pleistocene deposits of the IshimIrtysh interfluve (village of Kotochiga, Western Siberia) is described. The specimen is morphologically close to the northern pike, which presently has a circumboreal range. A number of primitive characters in the structure and dentition of the dentary and palatine resemble some Pliocene specimens, although they are rather incomplete, precluding the estimation of the taxonomic value of such characters. The preservation of scales and bones in the pike from Western Siberian suggests immediate burial in the place of its death in a lacustrine basin. The material comes from loam, with traces of a paleocryogenic texture. The underlying sand bed contains abundant shells of freshwater mollusks, suggesting that the climate was comparable to that in the Recent or even softer. The 14C dating giving the age about 25 ka (MIS3) was obtained for the first time in the horizon of buried soil at t

U2 - 10.1134/S0031030115050135

DO - 10.1134/S0031030115050135

M3 - Article

VL - 49

SP - 501

EP - 506

JO - Paleontological Journal

JF - Paleontological Journal

SN - 0031-0301

IS - 5

ER -

ID: 3989538