N I Dorofeyuk
Biographic Data
| ID | 4063190 |
|---|---|
| NAME | N I Dorofeyuk |
| GIVEN NAMES | N I |
| FAMILY NAME | Dorofeyuk |
| SIGNATURE | DOROFEYUK N I |
| AFFILIATIONS | Severtsov Institute of Ecology and Evolution |
| ORCID | 0000-0001-6953-8384 |
| VERIFIED | Yes |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 7 |
| AUTHOR COUNT | 4 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 1998 |
| LATEST PUBLICATION YEAR | 2021 |
| H-INDEX | 1 |
Palaeoenvironmental and climatic changes during the Late Glacial and Holocene in the Mongolia and Baikal region
Holocene environments and climate in the Mongolian Altai reconstructed from the Hoton-Nur pollen and diatom records
Environmental Changes in the Mongolian Altai During the Holocene
Based on palynological and diatom analyses of the sediment core from Lake Hoton Nuur situated at 2083 m asl, environmental changes in the Mongolian Altai during the Holocene are described. The results suggest that the Late Pleistocene and Early Holocene (11.5–10.7 ka) climate of that area was cold and arid, and plant associations were of a steppe type. The Middle Holocene (9.3–6.5 ka) climate was warm and humid, resulting in the expansion of fore…
Present‐day and mid‐Holocene biomes reconstructed from pollen and plant macrofossil data from the former Soviet Union and Mongolia
Fossil pollen data supplemented by tree macrofossil records were used to reconstruct the vegetation of the Former Soviet Union and Mongolia at 6000 years. Pollen spectra were assigned to biomes using the plant‐functional‐type method developed by Prentice et al . (1996). Surface pollen data and a modern vegetation map provided a test of the method. This is the first time such a broad‐scale vegetation reconstruction for the greater part of northern…
Environmental Changes in the Mongolian Altai During the Holocene
Based on palynological and diatom analyses of the sediment core from Lake Hoton Nuur situated at 2083 m asl, environmental changes in the Mongolian Altai during the Holocene are described. The results suggest that the Late Pleistocene and Early Holocene (11.5–10.7 ka) climate of that area was cold and arid, and plant associations were of a steppe type. The Middle Holocene (9.3–6.5 ka) climate was warm and humid, resulting in the expansion of fore…
Present‐day and mid‐Holocene biomes reconstructed from pollen and plant macrofossil data from the former Soviet Union and Mongolia
Fossil pollen data supplemented by tree macrofossil records were used to reconstruct the vegetation of the Former Soviet Union and Mongolia at 6000 years. Pollen spectra were assigned to biomes using the plant‐functional‐type method developed by Prentice et al . (1996). Surface pollen data and a modern vegetation map provided a test of the method. This is the first time such a broad‐scale vegetation reconstruction for the greater part of northern…
Environmental Changes in the Mongolian Altai During the Holocene
Based on palynological and diatom analyses of the sediment core from Lake Hoton Nuur situated at 2083 m asl, environmental changes in the Mongolian Altai during the Holocene are described. The results suggest that the Late Pleistocene and Early Holocene (11.5–10.7 ka) climate of that area was cold and arid, and plant associations were of a steppe type. The Middle Holocene (9.3–6.5 ka) climate was warm and humid, resulting in the expansion of fore…
Holocene environments and climate in the Mongolian Altai reconstructed from the Hoton-Nur pollen and diatom records
Palaeoenvironmental and climatic changes during the Late Glacial and Holocene in the Mongolia and Baikal region
Climate change (4 works) · Geography (4 works) · Geology and Paleoclimatology Research (4 works) · Holocene (4 works) · Physical geography (4 works) · Pleistocene-Era Hominins and Archaeology (4 works) · Steppe (4 works) · Archaeology (3 works) · Arctic (3 works) · Geological formations and processes (3 works)