Evolution of waterways and early human settlements in the Eastern Baltic area: Radiocarbon-based chronology

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Abstract

Newly obtained radiocarbon measurements are used to suggest that the initial settlement of the northeastern Baltic area was largely controlled by the Ladoga-Baltic waterway in the north of the Karelian Isthmus, which emerged ~11,500 cal BP and remained in action for ~7000 yr. The transgression of Ladoga Lake started ~5000 cal BP and reached its maximum at ~3000 cal BP (~1100-1000 cal BC). The formation of a new outlet via the Neva River led to a rapid regression of the lake that stimulated the spread of farming populations. © 2007 by the Arizona Board of Regents on behalf of the University of Arizona.

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Dolukhanov, P. M., Shukurov, A. M., Arslanov, K. A., Subetto, D. A., Zaitseva, G. I., Djinoridze, E. N., … Savelieva, L. A. (2007). Evolution of waterways and early human settlements in the Eastern Baltic area: Radiocarbon-based chronology. Radiocarbon, 49(2), 527–542. https://doi.org/10.1017/S0033822200042442

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