A M Shukurov
Biographic Data
| ID | 5601530 |
|---|---|
| NAME | A M Shukurov |
| GIVEN NAMES | A M |
| FAMILY NAME | Shukurov |
| SIGNATURE | SHUKUROV A M |
| VERIFIED | No |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 40 |
| AUTHOR COUNT | 4 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2002 |
| LATEST PUBLICATION YEAR | 2009 |
| H-INDEX | 2 |
Climate, subsistence and human movements in the Western Dvina – Lovat River Basins
Evolution of Waterways and Early Human Settlements in the Eastern Baltic Area
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 …
Reply to Y. V. Kuzmin, S. G. Keates (Journal of Archaeological Science 31 (2004) 141–143)
Colonization of Northern Eurasia by Modern Humans
Colonization of Northern Eurasia by Modern Humans
Evolution of Waterways and Early Human Settlements in the Eastern Baltic Area
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 …
Colonization of Northern Eurasia by Modern Humans
Reply to Y. V. Kuzmin, S. G. Keates (Journal of Archaeological Science 31 (2004) 141–143)
Evolution of Waterways and Early Human Settlements in the Eastern Baltic Area
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 …
Climate, subsistence and human movements in the Western Dvina – Lovat River Basins
Archaeology (4 works) · Archaeology and ancient environmental studies (4 works) · Geography (4 works) · Geology (4 works) · Paleontology (3 works) · Chronology (2 works) · Geology and Paleoclimatology Research (2 works) · Holocene (2 works) · Human settlement (2 works) · Physical geography (2 works)