A V Daryin
Biographic Data
| ID | 4063194 |
|---|---|
| NAME | A V Daryin |
| GIVEN NAMES | A V |
| FAMILY NAME | Daryin |
| SIGNATURE | DARYIN A V |
| AFFILIATIONS | Institute of the Earth’s Crust |
| VERIFIED | No |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 7 |
| WORKS AS AUTHOR | 3 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2007 |
| LATEST PUBLICATION YEAR | 2009 |
| H-INDEX | 1 |
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…
Yr-long records of annual air temperature and precipitation over southern Siberia inferred from Teletskoye Lake sediments
A unique 800-yr-long record of annual temperatures and precipitation over the south of western Siberia has been reconstructed from the bottom sediments of Teletskoye Lake, Altai Mountains using an X-ray fluorescence scanner (XRF) providing 0.1-mm resolution timeseries of elemental composition and X-ray density (XRD). Br content appears to be broadly correlative with mean annual temperature variations because of changes in catchment vegetation pro…
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…
Yr-long records of annual air temperature and precipitation over southern Siberia inferred from Teletskoye Lake sediments
A unique 800-yr-long record of annual temperatures and precipitation over the south of western Siberia has been reconstructed from the bottom sediments of Teletskoye Lake, Altai Mountains using an X-ray fluorescence scanner (XRF) providing 0.1-mm resolution timeseries of elemental composition and X-ray density (XRD). Br content appears to be broadly correlative with mean annual temperature variations because of changes in catchment vegetation pro…
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
Climate change (3 works) · Geology and Paleoclimatology Research (3 works) · Physical geography (3 works) · Diatom (2 works) · Geography (2 works) · Geological formations and processes (2 works) · Geology (2 works) · Holocene (2 works) · Oceanography (2 works) · Paleontology (2 works)