|
ИСТИНА |
Войти в систему Регистрация |
ИПМех РАН |
||
Middle Pleistocene small mammal and mollusk locality Levada (lower Dniester River basin) and its position in the Tiraspolian faunas of the Russian Plainстатья
- Авторы: Markova Anastasia K., Chepalyga Andrey L., Puzachenko Andrey Yu
- Журнал: Elsevier. Quaternary-International
- Том: 605
- Год издания: 2021
- Первая страница: 81
- Последняя страница: 92
- DOI: 10.1016/j.quaint.2020.08.006
- Аннотация: The analysis of small mammal and freshwater mollusk remains from the fluvialdeposits of VI terrace of Dniester R. in Levada section (Moldova, Transnistria) revealedthe main characteristic of species composition and evolutionary level of these remainsand permitted their placement in the stratigraphic scale of Middle Pleistocene faunas ofEastern Europe. The Levada fauna corresponds to the same stage as the fauna fromthe fluvial deposits of VI terrace of Dniester in stratotype of Tiraspolian faunisticcomplex in Kolkotova Balka section. These faunas existed between the EarlyTiraspolian faunas which correlate to the second part of MIS 19 and with MIS 18, andthe Late Tiraspolian (MIS 16 and MIS 15). Mimomys savini, Lagurus transiens,Microtus (Terricola) arvalidens, Lasiopodomys (Stenocranius) gregaloides are thespecies most characteristic of these faunas. The Levada fauna reflects interglacialclimate conditions. The faunas of this evolutionary level existed during the second partof the Ilyinskian Interglacial of the Russian Plain and during the Cromer Interglacial 2 ofWest Europe. The freshwater mollusks from Levada section (Viviparus tiraspolitanusPavl., V. subcrasus Lung., Lithoglithus naticoides С. Pf. and others) reflects a warmclimate close to that of the Mediterranean.
- Добавил в систему: Маркова Анастасия Константиновна
Прикрепленные файлы
| № | Имя | Описание | Имя файла | Размер | Добавлен |
|---|---|---|---|---|---|
| 1. | Полный текст | 2020_Markova_QI_Levada.pdf | 3,4 МБ | 28 октября 2020 [Markova_AK] |