E Zazovskaya
Biographic Data
| ID | 5597090 |
|---|---|
| NAME | E Zazovskaya |
| GIVEN NAMES | E |
| FAMILY NAME | Zazovskaya |
| SIGNATURE | ZAZOVSKAYA E |
| VERIFIED | No |
| TOTAL WORKS | 5 |
| TOTAL CITATIONS | 22 |
| WORKS AS AUTHOR | 5 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2012 |
| LATEST PUBLICATION YEAR | 2018 |
| H-INDEX | 2 |
Development of Surficial Deposits on Belyi Island (Kara Sea) during the Last 40,000 Years
A series of radiocarbon ( 14 C) dates of peat and other materials, containing organic matter, were obtained from Belyi Island. We have identified a large group of dates associates with MIS 1, as well as a significant group of dates associated with the Kargin (MIS 3) period (40–31 ka cal BP). A large number of dates from the Late Glacial period and from the Early Holocene (MIS 1—ca. 14–9 ka cal BP) point to this time interval being associated with…
Radiocarbon Age of Soils in Oases of East Antarctica
This article discusses radiocarbon dating results for soils and soil-like systems in the East Antarctic oases, including Schirmacher, Thala Hills, and Larsemann Hills. The organic matter of endolithic and hypolithic systems, soils of wind shelters, and soils under moss-algae vegetation were dated along with micro- and macroprofiles. Organic matter pools formed under extreme climatic conditions and originated not from vascular plants but from cryp…
Organic Matter of Cultural Layers as a Material for Radiocarbon Dating
This article focuses on radiocarbon ( 14 C) dating of the organic matter (OM) of natural-anthropogenic objects—the cultural layers (CLs) of archaeological sites. Using examples from three ancient sites located within the European part of Russia, in southern taiga and forest-steppe natural zones, we demonstrate approaches to the interpretation of 14 C dating of OM derived from the organomineral material of the CLs studied. We use the term “archaeo…
Reservoir Effect of Archaeological Samples from Steppe Bronze Age Cultures in Southern Russia
Human and animal bone collagen from different Steppe Bronze Age cultures, including the Yamnaya, East Manych Catacomb, and Lola cultures, show large variations in δ 13 C and δ 15 N values. More positive values of δ 13 C and δ 15 N are caused by change in diet and/or a more arid climate. Human bones show reservoir effects caused by aquatic diet components. These effects can be quantified by paired dating of human bone and associated terrestrial sa…
Isotopes, Plants, and Reservoir Effects
Bronze Age human and animal bone collagen from several steppe Bronze Age cultures (i.e. Early Catacomb, East and West Manych Catacomb, and Lola cultures) shows large variations in δ 13 C and δ 15 N values. In general, we observed that the older the sample, the lower the δ 13 C and δ 15 N values. We hypothesize that more positive values of δ 13 C and δ 15 N are caused by change in diet and a more arid climate. For ancient sheep during drier period…
Isotopes, Plants, and Reservoir Effects
Bronze Age human and animal bone collagen from several steppe Bronze Age cultures (i.e. Early Catacomb, East and West Manych Catacomb, and Lola cultures) shows large variations in δ 13 C and δ 15 N values. In general, we observed that the older the sample, the lower the δ 13 C and δ 15 N values. We hypothesize that more positive values of δ 13 C and δ 15 N are caused by change in diet and a more arid climate. For ancient sheep during drier period…
Reservoir Effect of Archaeological Samples from Steppe Bronze Age Cultures in Southern Russia
Human and animal bone collagen from different Steppe Bronze Age cultures, including the Yamnaya, East Manych Catacomb, and Lola cultures, show large variations in δ 13 C and δ 15 N values. More positive values of δ 13 C and δ 15 N are caused by change in diet and/or a more arid climate. Human bones show reservoir effects caused by aquatic diet components. These effects can be quantified by paired dating of human bone and associated terrestrial sa…
Radiocarbon Age of Soils in Oases of East Antarctica
This article discusses radiocarbon dating results for soils and soil-like systems in the East Antarctic oases, including Schirmacher, Thala Hills, and Larsemann Hills. The organic matter of endolithic and hypolithic systems, soils of wind shelters, and soils under moss-algae vegetation were dated along with micro- and macroprofiles. Organic matter pools formed under extreme climatic conditions and originated not from vascular plants but from cryp…
Isotopes, Plants, and Reservoir Effects
Bronze Age human and animal bone collagen from several steppe Bronze Age cultures (i.e. Early Catacomb, East and West Manych Catacomb, and Lola cultures) shows large variations in δ 13 C and δ 15 N values. In general, we observed that the older the sample, the lower the δ 13 C and δ 15 N values. We hypothesize that more positive values of δ 13 C and δ 15 N are caused by change in diet and a more arid climate. For ancient sheep during drier period…
Reservoir Effect of Archaeological Samples from Steppe Bronze Age Cultures in Southern Russia
Human and animal bone collagen from different Steppe Bronze Age cultures, including the Yamnaya, East Manych Catacomb, and Lola cultures, show large variations in δ 13 C and δ 15 N values. More positive values of δ 13 C and δ 15 N are caused by change in diet and/or a more arid climate. Human bones show reservoir effects caused by aquatic diet components. These effects can be quantified by paired dating of human bone and associated terrestrial sa…
Radiocarbon Age of Soils in Oases of East Antarctica
This article discusses radiocarbon dating results for soils and soil-like systems in the East Antarctic oases, including Schirmacher, Thala Hills, and Larsemann Hills. The organic matter of endolithic and hypolithic systems, soils of wind shelters, and soils under moss-algae vegetation were dated along with micro- and macroprofiles. Organic matter pools formed under extreme climatic conditions and originated not from vascular plants but from cryp…
Organic Matter of Cultural Layers as a Material for Radiocarbon Dating
This article focuses on radiocarbon ( 14 C) dating of the organic matter (OM) of natural-anthropogenic objects—the cultural layers (CLs) of archaeological sites. Using examples from three ancient sites located within the European part of Russia, in southern taiga and forest-steppe natural zones, we demonstrate approaches to the interpretation of 14 C dating of OM derived from the organomineral material of the CLs studied. We use the term “archaeo…
Development of Surficial Deposits on Belyi Island (Kara Sea) during the Last 40,000 Years
A series of radiocarbon ( 14 C) dates of peat and other materials, containing organic matter, were obtained from Belyi Island. We have identified a large group of dates associates with MIS 1, as well as a significant group of dates associated with the Kargin (MIS 3) period (40–31 ka cal BP). A large number of dates from the Late Glacial period and from the Early Holocene (MIS 1—ca. 14–9 ka cal BP) point to this time interval being associated with…
Geography (5 works) · Geology (5 works) · Physical geography (5 works) · Archaeology (4 works) · Paleontology (4 works) · Pleistocene-Era Hominins and Archaeology (4 works) · Radiocarbon dating (4 works) · Archaeology and ancient environmental studies (3 works) · Biology (3 works) · Geology and Paleoclimatology Research (3 works)