The North Dvina river delta development over the Holocene: Geochronology and palaeoenvironment
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 other field surveys, and plant macrofossil and palynological data. We have identified three main stages of the d...
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Published in | Geochronometria Vol. 38; no. 2; pp. 116 - 127 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
Published |
Heidelberg
SP Versita
01.06.2011
Versita |
Subjects | |
Online Access | Get full text |
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Summary: | 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 other 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. |
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ISSN: | 1733-8387 1897-1695 |
DOI: | 10.2478/s13386-011-0012-y |