The North Dvina river delta development over the Holocene: geochronology and palaeoenvironment

• Autorzy: Zaretskaya N. E. , Shevchenko N. V. , Simakova A. N. , Sulerzhitsky L. D.
• Języki publikacji: EN

Abstrakty

EN

In this paper, a detailed overview of the Holocene evolution of the North Dvina river (ND) delta (southern White Sea) is presented; it is based on radiocarbon dating, geomorphological and oth-er field surveys, and plant macrofossil and palynological data. We have identified three main stages of the delta evolution: estuary erosional (Allerød – 5700 cal BC), lagoon or tidal-marsh (5700 cal BC – 3700 cal BC) and fan-delta accumulative (3700 cal BC – present). These stages are correlated with local climatic curves, sea level changes, glacioisostatic raise curve and Baltic Sea stages. A variety of landforms has been identified and dated within the delta. These results help to explain the spatial and temporal patterns in the prehistoric human occupation of this area.

Słowa kluczowe

EN

North Dvina River delta; White Sea; Holocene; geochronology; radiocarbon dating; landforms; palaeoenvironmental reconstructions; land evolution

• Wydawca: De Gruyter
• Czasopismo: Geochronometria
• Rocznik: 2011
• Tom: Vol. 38, no. 2
• Strony: 116--127
• Opis fizyczny: Bibliogr. 28 poz., rys., tab.

Twórcy

autor

Zaretskaya N. E.

autor

Shevchenko N. V.

autor

Simakova A. N.

autor

Sulerzhitsky L. D.

• Geological Institute of Russian Academy of Sciences, Pyzhevsky per., 7, Moscow, 119017, Russia,

Bibliografia

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