Academic Journal

Oligocene stratigraphy across the Eocene and Miocene boundaries in the Valley of Lakes (Mongolia)

التفاصيل البيبلوغرافية
العنوان: Oligocene stratigraphy across the Eocene and Miocene boundaries in the Valley of Lakes (Mongolia)
المؤلفون: Daxner-Höck, Gudrun, Badamgarav, Demchig, Barsbold, Rinchen, Erbajeva, Margarita, Bettina Göhlich, Ursula, Harzhauser, M., Höck, E., Höck, Volger, Ichinnorov, Niiden, Khand, Yondon, López-Guerrero, Paloma, Maridet, O., Neubauer, Thomas.A., Oliver Pérez, Adriana, Piller, W. E., Tsogtbaatar, Khishigjav, Ziegler, R.
المساهمون: Austrian Science Fund, Austrian Academy of Sciences
بيانات النشر: Springer
سنة النشر: 2017
المجموعة: Digital.CSIC (Consejo Superior de Investigaciones Científicas / Spanish National Research Council)
مصطلحات موضوعية: Oligocene, Mammals, Stratigraphy, Correlation, Mongolia, Miocene
الوصف: Cenozoic sediments of the Taatsiin Gol and TaatsiinTsagaan Nuur area are rich in fossils that provide unique evidence of mammal evolution in Mongolia. The strata are intercalated with basalt flows. 40Ar/39Ar data of the basalts frame the time of sediment deposition and mammal evolution and enable a composite age chronology for the studied area. We investigated 20 geological sections and 6 fossil localities of Oligocene and early Miocene deposits from this region. Seventy fossil beds yielded more than 19,000 mammal fossils. This huge collection encompasses 175 mammal species: 50% Rodentia, 13% Eulipotyphla and Didelphomorphia, and 12% Lagomorpha. The remaining 25% of species are distributed among herbivorous and carnivorous large mammals. The representation of lower vertebrates and gastropods is comparatively poor. Several hundred SEM images illustrate the diversity of Marsupialia, Eulipotyphla, and Rodentia dentition and give insight into small mammal evolution in Mongolia during the Oligocene and early Miocene. This dataset, the radiometric ages of basalt I (∼31.5 Ma) and basalt II (∼27 Ma), and the magnetostratigraphic data provide ages of mammal assemblages and time ranges of the Mongolian biozones: letter zone A ranges from ∼33 to ∼31.5 Ma, letter zone B from ∼31.5 to ∼28 Ma, letter zone C from ∼28 to 25.6 Ma, letter zone C1 from 25.6 to 24 Ma, letter zone C1-D from 24 to ∼23 Ma, and letter zone D from ∼23 to ∼21 Ma. ; Open access funding provided by Austrian Science Fund (FWF). This research was supported by four projects of the Austrian Science Fund (FWF): P-10505-GEO, P-15724-N06, P-23061-N19 to G.D.-H. and a Lise Meitner grant M-1357-B17 to O.M. Travel expenses of G.D.-H. to China and Mogolia were partly covered by the Austrian Academy of Sciences. ; Peer Reviewed
نوع الوثيقة: article in journal/newspaper
اللغة: unknown
تدمد: 1867-1594
1867-1608
28450965
Relation: https://doi.org/10.1007/s12549-016-0257-9; Sí; Palaeobiodiversity and Palaeoenvironments 97(1): 111-218 (2017); http://hdl.handle.net/10261/195982; http://dx.doi.org/10.13039/501100002428; http://dx.doi.org/10.13039/501100001822
DOI: 10.1007/s12549-016-0257-9
DOI: 10.13039/501100002428
DOI: 10.13039/501100001822
الاتاحة: http://hdl.handle.net/10261/195982
https://doi.org/10.1007/s12549-016-0257-9
https://doi.org/10.13039/501100002428
https://doi.org/10.13039/501100001822
Rights: none
رقم الانضمام: edsbas.BEC2D93
قاعدة البيانات: BASE
الوصف
تدمد:18671594
18671608
28450965
DOI:10.1007/s12549-016-0257-9