Plestocene small mammal faunas from the fluvial deposits of SW regions of Eastern Europe

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The investigation of the Pleistocene small mammal faunas from the south-western regions of the Russian Plain permits to reconstruct their principal evolutional stages during last ~1 400 000 yr. These materials took the possibilities to date the Pleistocene alluvial, liman and marine deposits and also the horizons of the fossil soils.

The unique small mammal and brackish-water mollusk localities in marine and liman-deltaic deposits of the Black Sea permits to demonstrate a direct correlation between the events in the Black Sea basin and on the continent. The direct correlations of the events (transgressions) in the Black Sea and on the continent were made based on the joint finds of the brackish-water mollusks and the small mammal remains. Thus, the Tiraspolian faunas synchronous to the Chaudian transgression of the Black Sea; the faunas of the Gunkovian small mammal assemblage (MIS 11, Likhvin interglacial) are correlated to the Early Euxinian transgression. The faunas existing in the last warming (Interglacial?) of the Middle Pleistocene (MIS 7) are synchronous to the Uzunlar transgression, and the faunas of the Mikulino (=Eemian) Interglacial are correlated with Karangat transgression (MIS 5e). The species of the open (steppe and forest-steppe) landscapes prevailed in the all of the faunas.

Sobre autores

A. Markova

Institute of Geography RAS

Autor responsável pela correspondência
Email: amarkova@list.ru
Rússia, Moscow

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2. Fig. 1. Pleistocene small mammal localities mentioned in the text. 1 — Nagornoe, 2 — Suvorovo, 3 — Ozernoe (Babel), 4 — Uzmari, 5 — Cheshmikioi, 6 — Plavni, 7 — Novonekrasovka, 8 — Kolkotova Balka, 9 — Levada, 10 — Khadzhimus, 11 — Roksokany, 12 — Cherevichnoe 1 (Morozovka), 13 — Nogaisk (Primorskoe), 14 — Karai-Dubina (Berezhanka), 15 — Zapadnye Kairy, 16 — Ushkalka, 17 — Port-Katon, 18 — Litvin, 19 — Uzunlar, 20 — Pekla.

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3. Fig. 2. The structure of Khadzhimus section (IX Dniester terrace) (after Dr. A. I. Tsatskin, per. comm.). BR — Briansk paleosol (MIS3), MEZ — Mezin soil complex (MIS5e), RM — Romny paleosol (MIS7), KM — Kamenka paleosol (MIS9), INZH — Inzhava paleosol (MIS11), VOR — Vorona paleosol (MIS15), KOL — Kolkotova paleosol (MIS17), Embr. soil — embryonic soil, MIKH (II phase) — Mikhailovka paleosol (II phase) (MIS19), MIKH (I phase) — Mikhailovka paleosol (MIS21), KITSK — Kitskansk paleosol (MIS?), SM LOC (up. layer) — small mammal locality (upper layer), ALL of IX Dniester terrace — alluvium of IX Dniester terrace, SM LOC (low. layer) — small mammal locality (lower layer), JR — Jaramillo palaeomagnetic episode. 1 — soil; 2 — loess; 3 — bones of small mammals; 4 — molehill.

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4. Fig. 3. Levada section (VI Dniester R. terrace). H — Holocene soil; R? — Romny paleosol (?); K — Kamenka paleosol; In — Inzhava paleosol; V — Vorona paleosol. 1 — soil; 2 — loess; 3 — loam; 4 — sandy loam; 5 — obliquely layered sands; 6 — sands; 7 — gravelite; 8 — molehill; 9 — bones of small mammals; 10 — mollusk shells.

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5. Fig. 4. Novonekrasovka section (II Danube R. terrace). BR(?) — Briansk paleosol (?), MEZ — Mezin paleosol; SM LOC — small mammal’ localities in the Karangatian liman deposits of the Black Sea (MIS5e). 1 — soil; 2 — loess; 3 — loam; 4 — clay; 5 — sand; 6 — bones of small mammals; 7 — molehill; 8 — gravelite.

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