D A Subetto
Biographic Data
| ID | 5600426 |
|---|---|
| NAME | D A Subetto |
| GIVEN NAMES | D A |
| FAMILY NAME | Subetto |
| SIGNATURE | SUBETTO D A |
| VERIFIED | No |
| TOTAL WORKS | 7 |
| TOTAL CITATIONS | 13 |
| WORKS AS AUTHOR | 7 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1999 |
| LATEST PUBLICATION YEAR | 2023 |
| H-INDEX | 2 |
From a large basin to a small lake
Fingerprint of the geographic and climate evolution of the Baltic–White Sea region in the Late Pleistocene-Holocene in groundwater stable isotopes (2H, 18O)
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
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 …
New Data on Chronology of Landscape-Paleoclimatic Stages in Northwestern Russia During the Late Glacial and Holocene
Two lake and bog sediments have been thoroughly studied using palynological and radiocarbon dating methods. These are the Lembolovskoye Lake section located in the southern part of the Karelian Ithmus and the Mshinskoye bog section located in the southwestern part of the Leningrad province. The data obtained allow us to reconstruct the main features of the vegetation cover evolution, the chronology for the appearance and a real distribution of th…
Chronology of Vegetation and Paleoclimatic Stages of Northwestern Russia During the Late Glacial and Holocene
We have studied 6 reference sections of bog and lake sediments in the Leningrad and Novgorod provinces to develop a geochronological scale for vegetational and paleoclimatic changes in northwestern Russia during the Late Glacial and Holocene. Every 10-cm layer along the peat and gyttja sections (4–8.5 m thick) was investigated palynologically and the great majority of them were radiocarbon dated. Using the data obtained, standard palynological di…
Holocene oscillations of the Baltic Sea and Lake Ladoga levels and early human movements
Chronology of Vegetation and Paleoclimatic Stages of Northwestern Russia During the Late Glacial and Holocene
We have studied 6 reference sections of bog and lake sediments in the Leningrad and Novgorod provinces to develop a geochronological scale for vegetational and paleoclimatic changes in northwestern Russia during the Late Glacial and Holocene. Every 10-cm layer along the peat and gyttja sections (4–8.5 m thick) was investigated palynologically and the great majority of them were radiocarbon dated. Using the data obtained, standard palynological di…
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 …
Chronology of Vegetation and Paleoclimatic Stages of Northwestern Russia During the Late Glacial and Holocene
We have studied 6 reference sections of bog and lake sediments in the Leningrad and Novgorod provinces to develop a geochronological scale for vegetational and paleoclimatic changes in northwestern Russia during the Late Glacial and Holocene. Every 10-cm layer along the peat and gyttja sections (4–8.5 m thick) was investigated palynologically and the great majority of them were radiocarbon dated. Using the data obtained, standard palynological di…
New Data on Chronology of Landscape-Paleoclimatic Stages in Northwestern Russia During the Late Glacial and Holocene
Two lake and bog sediments have been thoroughly studied using palynological and radiocarbon dating methods. These are the Lembolovskoye Lake section located in the southern part of the Karelian Ithmus and the Mshinskoye bog section located in the southwestern part of the Leningrad province. The data obtained allow us to reconstruct the main features of the vegetation cover evolution, the chronology for the appearance and a real distribution of th…
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 …
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
Fingerprint of the geographic and climate evolution of the Baltic–White Sea region in the Late Pleistocene-Holocene in groundwater stable isotopes (2H, 18O)
From a large basin to a small lake
Geology (7 works) · Geology and Paleoclimatology Research (7 works) · Geography (6 works) · Holocene (6 works) · Oceanography (6 works) · Paleontology (6 works) · Physical geography (6 works) · Archaeology (5 works) · Ecology (4 works) · Radiocarbon dating (4 works)