В А Климанов
Biographic Data
| ID | 6372704 |
|---|---|
| NAME | В А Климанов |
| GIVEN NAMES | В А |
| FAMILY NAME | Климанов |
| SIGNATURE | КЛИМАНОВ В А |
| AFFILIATIONS | Institute of Geography |
| VERIFIED | No |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 2 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2001 |
| LATEST PUBLICATION YEAR | 2002 |
| H-INDEX | 0 |
Late Pleistocene and Holocene Vegetation and Climate on the Taymyr Lowland, Northern Siberia
Pollen records from perennially frozen sequences provide vegetation and climate reconstruction for the last 48,000 14 C years in the central part of Taymyr Peninsula. Open larch forest with Alnus fruticosa and Betula nana grew during the Kargin (Middle Weichselian) Interstade, ca. 48,000–25,000 14 C yr B.P. The climate was generally warmer and wetter than today. Open steppe-like communities with Artemisia , Poaceae, Asteraceae, and herb tundralik…
Vegetation and climate in the lower reaches of the Yana River during the Holocene
The Holocene climate history of the region near the mouth of the Yana River in Yakutia (Sakha Republic) is reconstructed from two sections of the Kazach'ye and Khocho peat bogs along the banks of the Yana River. Spore‐pollen analysis and an information‐statistical method are used to reconstruct temperature and precipitation histories that are compared with present‐day conditions
No prominent works on this page.
Vegetation and climate in the lower reaches of the Yana River during the Holocene
The Holocene climate history of the region near the mouth of the Yana River in Yakutia (Sakha Republic) is reconstructed from two sections of the Kazach'ye and Khocho peat bogs along the banks of the Yana River. Spore‐pollen analysis and an information‐statistical method are used to reconstruct temperature and precipitation histories that are compared with present‐day conditions
Late Pleistocene and Holocene Vegetation and Climate on the Taymyr Lowland, Northern Siberia
Pollen records from perennially frozen sequences provide vegetation and climate reconstruction for the last 48,000 14 C years in the central part of Taymyr Peninsula. Open larch forest with Alnus fruticosa and Betula nana grew during the Kargin (Middle Weichselian) Interstade, ca. 48,000–25,000 14 C yr B.P. The climate was generally warmer and wetter than today. Open steppe-like communities with Artemisia , Poaceae, Asteraceae, and herb tundralik…
Archaeology (2 works) · Biology (2 works) · Geography (2 works) · Geology and Paleoclimatology Research (2 works) · Holocene (2 works) · Physical geography (2 works) · Arctic (1 work) · Bog (1 work) · Climate change (1 work) · Climatology (1 work)