A A Abzaeva
Biographic Data
| ID | 4062257 |
|---|---|
| NAME | A A Abzaeva |
| GIVEN NAMES | A A |
| FAMILY NAME | Abzaeva |
| SIGNATURE | ABZAEVA A A |
| VERIFIED | No |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 11 |
| AUTHOR COUNT | 3 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2005 |
| LATEST PUBLICATION YEAR | 2009 |
| H-INDEX | 2 |
Environment and Human Behavior in Northern Mongolia During the Upper Pleistocene
This paper discusses the results of multidisciplinary studies of culture-bearing horizons uncovered at the Tolbor-4 site in Mongolia. Lithological analysis suggests that the entire sedimentary sequence belongs to the terminal Upper Pleistocene. The lowermost portion of the profi le is attributed to the late Zyryanka period, the middle portion to the Karga period, and the upper portion, Layers 2 and 3, to the Sartan period. Layers 4 and 5 seem to …
Evidence of Environmental Instability of the Lake Baikal Area After the Last Glaciation (Based on Pollen Records From Peatlands)
Pollen analysis of two dated sedimentary cores from lacustrine-boggy sediments in various parts of the Lake Baikal area yielded the first complete record of deep changes in the lake catchment area during the Late Glacial and Early Holocene. The Early Middle Holocene record shows an optimum – a humid and mild climate with warm winters between ca 10,000 and 7000 BP. During the Late Holocene, the climate grew more and more continental, and dark coni…
Post-glacial history of Siberian spruce (Picea obovata) in the Lake Baikal area and the significance of this species as a paleo-environmental indicator
Environment and Human Behavior in Northern Mongolia During the Upper Pleistocene
This paper discusses the results of multidisciplinary studies of culture-bearing horizons uncovered at the Tolbor-4 site in Mongolia. Lithological analysis suggests that the entire sedimentary sequence belongs to the terminal Upper Pleistocene. The lowermost portion of the profi le is attributed to the late Zyryanka period, the middle portion to the Karga period, and the upper portion, Layers 2 and 3, to the Sartan period. Layers 4 and 5 seem to …
Evidence of Environmental Instability of the Lake Baikal Area After the Last Glaciation (Based on Pollen Records From Peatlands)
Pollen analysis of two dated sedimentary cores from lacustrine-boggy sediments in various parts of the Lake Baikal area yielded the first complete record of deep changes in the lake catchment area during the Late Glacial and Early Holocene. The Early Middle Holocene record shows an optimum – a humid and mild climate with warm winters between ca 10,000 and 7000 BP. During the Late Holocene, the climate grew more and more continental, and dark coni…
Post-glacial history of Siberian spruce (Picea obovata) in the Lake Baikal area and the significance of this species as a paleo-environmental indicator
Environment and Human Behavior in Northern Mongolia During the Upper Pleistocene
This paper discusses the results of multidisciplinary studies of culture-bearing horizons uncovered at the Tolbor-4 site in Mongolia. Lithological analysis suggests that the entire sedimentary sequence belongs to the terminal Upper Pleistocene. The lowermost portion of the profi le is attributed to the late Zyryanka period, the middle portion to the Karga period, and the upper portion, Layers 2 and 3, to the Sartan period. Layers 4 and 5 seem to …
Evidence of Environmental Instability of the Lake Baikal Area After the Last Glaciation (Based on Pollen Records From Peatlands)
Pollen analysis of two dated sedimentary cores from lacustrine-boggy sediments in various parts of the Lake Baikal area yielded the first complete record of deep changes in the lake catchment area during the Late Glacial and Early Holocene. The Early Middle Holocene record shows an optimum – a humid and mild climate with warm winters between ca 10,000 and 7000 BP. During the Late Holocene, the climate grew more and more continental, and dark coni…
Ecology (3 works) · Geography (3 works) · Geology (3 works) · Geology and Paleoclimatology Research (3 works) · Physical geography (3 works) · Archaeology (2 works) · Glacial period (2 works) · Holocene (2 works) · Oceanography (2 works) · Paleontology (2 works)