P M Dolukhanov
Biographic Data
| ID | 3644792 |
|---|---|
| NAME | P M Dolukhanov |
| GIVEN NAMES | P M |
| FAMILY NAME | Dolukhanov |
| SIGNATURE | DOLUKHANOV P M |
| VERIFIED | No |
| TOTAL WORKS | 15 |
| TOTAL CITATIONS | 75 |
| AUTHOR COUNT | 15 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 1970 |
| LATEST PUBLICATION YEAR | 2009 |
| H-INDEX | 4 |
Multiple sources of the European Neolithic
Climate, subsistence and human movements in the Western Dvina – Lovat River Basins
The Baltic Sea and Ladoga Lake transgressions and early human migrations in North-western Russia
Holocene oscillations of the Baltic Sea and Lake Ladoga levels and early human movements
Human socio-economic adaptation to environment in Late Palaeolithic, Mesolithic and Neolithic Eastern Europe
Climate, Black Sea levels and human settlements in Caucasus Littoral 50,000–9000 BP
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
The Pleistocene-Holocene transition in northern Eurasia
Archaeology in the ex-USSR
An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content
The Ecological Prerequisites for Early Farming in Southern Turkmenia
The evolution of early farming in southern Turkmenistan was a turning point in the development of the productive forces of the prehistoric population of the USSR. The mechanism of this process is of great importance from both theoretical and practical points of view. There is no doubt whatsoever that the evolution of agriculture was a complicated process shaped by both social and natural factors. On the one hand, this process largely depended on …
Radiocarbon Dates of the Institute of Archaeology III
This list contains radiocarbon dates of archaeologic samples of wood, charcoal, and peat measured between 1967 and 1973, analyzed by the Laboratory of the Institute of Archaeology, Leningrad Branch, USSR Academy of Sciences. The samples measured include charcoal from cultural strata and hearths, wood from kurgans and cultural strata, peat, etc, coll from various archaeologic sites by Soviet scientists, as well as a series from Dashly site, Afghan…
Radiocarbon Dates of the Institute of Archaeology III
The current list presents samples measured in the radiocarbon laboratory, Leningrad Branch Inst. of Archaeol., Acad. of Sci., USSR, from July 1967 through June 1969. Ages of 85 archaeologic samples of wood, charcoal, and peat have been determined
Radiocarbon Dates of the Institute of Archaeology II
The present list covers samples measured between 1963 and July, 1967. Three previous lists have been published in Leningrad I (Sovetskaya arkheologiya, 1961, p. 3); Leningrad II (The Absolute Geochronology of the Quaternary Period, 1963); and Leningrad III (New Methods in Archaeological Investigations, 1963, p. 9–56). The samples measured include charcoal from cultural layers and hearths, wood from barrows [kurgans] and cemeteries, wooden tools f…
Colonization of Northern Eurasia by Modern Humans
Radiocarbon Dates of the Institute of Archaeology II
The present list covers samples measured between 1963 and July, 1967. Three previous lists have been published in Leningrad I (Sovetskaya arkheologiya, 1961, p. 3); Leningrad II (The Absolute Geochronology of the Quaternary Period, 1963); and Leningrad III (New Methods in Archaeological Investigations, 1963, p. 9–56). The samples measured include charcoal from cultural layers and hearths, wood from barrows [kurgans] and cemeteries, wooden tools f…
Radiocarbon Dates of the Institute of Archaeology III
The current list presents samples measured in the radiocarbon laboratory, Leningrad Branch Inst. of Archaeol., Acad. of Sci., USSR, from July 1967 through June 1969. Ages of 85 archaeologic samples of wood, charcoal, and peat have been determined
Holocene oscillations of the Baltic Sea and Lake Ladoga levels and early human movements
Human socio-economic adaptation to environment in Late Palaeolithic, Mesolithic and Neolithic Eastern Europe
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 …
Archaeology in the ex-USSR
An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content
Radiocarbon Dates of the Institute of Archaeology III
This list contains radiocarbon dates of archaeologic samples of wood, charcoal, and peat measured between 1967 and 1973, analyzed by the Laboratory of the Institute of Archaeology, Leningrad Branch, USSR Academy of Sciences. The samples measured include charcoal from cultural strata and hearths, wood from kurgans and cultural strata, peat, etc, coll from various archaeologic sites by Soviet scientists, as well as a series from Dashly site, Afghan…
Radiocarbon Dates of the Institute of Archaeology II
The present list covers samples measured between 1963 and July, 1967. Three previous lists have been published in Leningrad I (Sovetskaya arkheologiya, 1961, p. 3); Leningrad II (The Absolute Geochronology of the Quaternary Period, 1963); and Leningrad III (New Methods in Archaeological Investigations, 1963, p. 9–56). The samples measured include charcoal from cultural layers and hearths, wood from barrows [kurgans] and cemeteries, wooden tools f…
Radiocarbon Dates of the Institute of Archaeology III
The current list presents samples measured in the radiocarbon laboratory, Leningrad Branch Inst. of Archaeol., Acad. of Sci., USSR, from July 1967 through June 1969. Ages of 85 archaeologic samples of wood, charcoal, and peat have been determined
Radiocarbon Dates of the Institute of Archaeology III
This list contains radiocarbon dates of archaeologic samples of wood, charcoal, and peat measured between 1967 and 1973, analyzed by the Laboratory of the Institute of Archaeology, Leningrad Branch, USSR Academy of Sciences. The samples measured include charcoal from cultural strata and hearths, wood from kurgans and cultural strata, peat, etc, coll from various archaeologic sites by Soviet scientists, as well as a series from Dashly site, Afghan…
The Ecological Prerequisites for Early Farming in Southern Turkmenia
The evolution of early farming in southern Turkmenistan was a turning point in the development of the productive forces of the prehistoric population of the USSR. The mechanism of this process is of great importance from both theoretical and practical points of view. There is no doubt whatsoever that the evolution of agriculture was a complicated process shaped by both social and natural factors. On the one hand, this process largely depended on …
Archaeology in the ex-USSR
An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content
The Pleistocene-Holocene transition in northern Eurasia
Colonization of Northern Eurasia by Modern Humans
Reply to Y. V. Kuzmin, S. G. Keates (Journal of Archaeological Science 31 (2004) 141–143)
Climate, Black Sea levels and human settlements in Caucasus Littoral 50,000–9000 BP
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 …
Human socio-economic adaptation to environment in Late Palaeolithic, Mesolithic and Neolithic Eastern Europe
Multiple sources of the European Neolithic
Climate, subsistence and human movements in the Western Dvina – Lovat River Basins
The Baltic Sea and Ladoga Lake transgressions and early human migrations in North-western Russia
Holocene oscillations of the Baltic Sea and Lake Ladoga levels and early human movements
Archaeology (15 works) · Geography (14 works) · Geology (11 works) · Archaeology and ancient environmental studies (10 works) · Paleontology (7 works) · Radiocarbon dating (7 works) · Ancient and Medieval Archaeology Studies (6 works) · Geology and Paleoclimatology Research (6 works) · Physical geography (6 works) · Holocene (5 works)