Archaeological sites as markers of Neopleistocene-Holocene hydrological system transformation in the Kurai and Chuya basins, Southeastern Altai
Results of geomorphological and geoarchaeological studies
Bibliographic Data
| ID | 6036765 |
|---|---|
| Authors | A R Agatova (0000-0002-1823-218X), R K Nepop (0000-0002-2046-6030), Р К Непоп, I Y Slyusarenko (0000-0002-1243-0900), Myglan (0000-0002-5268-653X), V S Myglan, Valentin V Barinov (0000-0002-3582-3440), V Barinov |
| Year | 2016 |
| Volume | 44 |
| Issue | 4 |
| Pages | 26-34 |
| Publication date | 2016-01-01 |
| Peer Reviewed | Yes |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | Archaeology Ethnology and Anthropology of Eurasia (JOURNAL) |
| Journal identifiers | ISSN: 1563-0110 • E-ISSN: 1531-832X |
| Publisher | Institute of Archaeology and Ethnography SB RAS (PUBLISHER) |
| DOI | 10.17746/1563-0110.2016.44.4.026-034 |
| OpenAlex | W2562481412 |
| Language | EN |
| Citations received | 2 |
| References cited | 1 |
Multidisciplinary studies using geomorphological, geoarchaeological, and geochronological approaches indicate contrasting environmental changes in southeastern Altai beginning from the Late Pleistocene. Twenty-eight new radiocarbon dates from the subaerial complex overlying Late Neopleistocene sediments in the high-altitude Kurai and Chuya basins confi rm the degradation of a single ice-dammed reservoir in that area during the Early Holocene. In the first half of the Holocene, those basins were filled with isolated lakes. At the Baratal River mouth in the western Kurai basin, a reservoir with a water level of at least 1480 m a.s.l. emerged ca 10-6.5 ka BP, whereas in the Chuya depression, numerous residual lakes had existed at least 8 ka BP. Landslide- and morainedammed lakes between the depressions in the Chuya valley had existed until 7-3 ka BP, when they drained away. The preservation state of in situ archaeological sites, their cultural affiliation, and their location within the depressions and along the main Chuya valley attest to spatial and temporal changes of the hydrological system. This evolution occurred in the second half of the Holocene and did not entail major consequences for humans. © 2016 Siberian Branch of the Russian Academy of Sciences
Archaeology · Carbonate · Cave · Geography · Holocene · Period (music · Physical geography · Pleistocene · Radiocarbon dating · Structural basin · Tufa · Geology and Paleoclimatology Research · Marine and environmental studies · Pleistocene-Era Hominins and Archaeology · Geology · Paleontology
| Unique citing works | 2 |
|---|---|
| Citations per year | 0,25 |
| Citation span | 2018 - 2018 (1) |
| Citation velocity | historical |
| Highly cited | No |
| Citation types | Neutral: 1 |