A A Golyeva
Biographic Data
| ID | 47659 |
|---|---|
| NAME | A A Golyeva |
| GIVEN NAMES | A A |
| FAMILY NAME | Golyeva |
| SIGNATURE | GOLYEVA A A |
| AFFILIATIONS | Institute of Geography |
| ORCID | 0000-0002-1162-3321 |
| VERIFIED | Yes |
| TOTAL WORKS | 9 |
| TOTAL CITATIONS | 10 |
| AUTHOR COUNT | 9 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2001 |
| LATEST PUBLICATION YEAR | 2025 |
| H-INDEX | 1 |
The Late Weichselian/Holocene transition on the East European Plain
Few sites in the East European Plain have yielded detailed multi-proxy data for the late Weichselian to Holocene transition. This paper provides a comprehensive palaeobotanical analysis of the lower part of a core of biogenic deposits from the Serteya Mire in the western part of the East European Plain (Western Russia). The studied reservoir, is located in a kettle hole and is dated to the Allerød, as confirmed by radiocarbon dating of the basal …
Application of Microbiomorphic and Total Phosphorus Analyses to the Archaeological Study of the Sredny Zelenchuk Temple, Nizhny Arkhyz Hillfort
The article presents the results of the first geoarchaeological study of the materials of Christian burials identified in the interior of the Middle Zelenchuk temple of the 10th century in the Nizhne-Arkhyz ancient settlement (Republic of Karachay-Cherkessia). The results of microbiomorphic (phytolith) and total phosphorus content analyses allowed us to reveal previously unknown features of the funeral rites of the multicultural and multi-ethnic …
Microbiomarkers of the local environment and interior of Neolithic and Eneolithic dwellings (settlements of Mergen 6 and 7)
The paper concerns the analysis of the local environment around the multi-layer settlements of Mergen 6 and 7 situated in the immediate vicinity of each other. The settlements existed successively (partly contempora-neously in the early and high Neolithic) in the forest-steppe belt of Western Siberia. Two methods were chosen to obtain the results: spore-and-pollen (palynological) and microbiomorphic analyses of the cultural layers of the settleme…
Dynamics of paleoenvironments in the Cis-Ural steppes during the mid- to late Holocene
The multi-layered settlement of Turganik in the Tok River valley (steppe region west of the Urals) has been studied using paleopedological and microbiomorphical methods. Early humans lived in the settlement during the Eneolithic epoch (the fifth millennium BC) and in the Early Bronze Age (the fourth millennium BC). The cultural layers attributable to the Atlantic period of the Holocene developed under conditions of a rather dry climate, with the …
A palaeoenvironmental reconstruction of the rampart construction of the medieval ring-fort in Rozprza, Central Poland
During archaeological excavations of a medieval stronghold in Rozprza, a buried thick deposit of deep black (Dark Earth type) soil was discovered. A multianalytical (sedimentological, geochemical and archaeobotanical) study was carried out in order to identify traits the Rozprza Dark Earth. The analyses demonstrated that the soil was formed as an effect of surface accumulation of organic deposits from swampy areas and waste materials with rich ad…
Paleolandscape Reconstruction of the Abrau Peninsula Littoral (Krasnodar Territory)
Burial ground horizons dating as far back as the 6th–2nd centuries BC and the cultural layers associated with settlements dated to the Late Bronze (?) Age, the Classical Antiquity, and the Middle Ages, have been identified during a multidisciplinary study of sediments exposed by trenching at the entrance of Lobanova Shchel (Lobanova Gorge), near a burial ground of the 6th–2nd centuries BC. The study has provided insights into general regularities…
The Black San Pablo Paleosol of the Teotihuacan Valley, Mexico
Although archaeologists have generally assumed that the ancient landscape in the Teotihuacan Valley was somewhat similar to the present day, recent research has documented large‐scale modification of the soil by accelerated human‐induced erosion–sedimentation processes from the pre‐Hispanic and Colonial periods up until the present. Consequently, the Formative and Classic period soil (approximately 400 B.C.–A.D. 650) is buried in most of the Teot…
Palaeoenvironmental reconstruction of Hungarian kurgans on the basis of the examination of palaeosoils and phytolith analysis
Soil evolution and accumulation of loess-like material in the Chechen depression, Northern Caucasus, Russia
The Black San Pablo Paleosol of the Teotihuacan Valley, Mexico
Although archaeologists have generally assumed that the ancient landscape in the Teotihuacan Valley was somewhat similar to the present day, recent research has documented large‐scale modification of the soil by accelerated human‐induced erosion–sedimentation processes from the pre‐Hispanic and Colonial periods up until the present. Consequently, the Formative and Classic period soil (approximately 400 B.C.–A.D. 650) is buried in most of the Teot…
Microbiomarkers of the local environment and interior of Neolithic and Eneolithic dwellings (settlements of Mergen 6 and 7)
The paper concerns the analysis of the local environment around the multi-layer settlements of Mergen 6 and 7 situated in the immediate vicinity of each other. The settlements existed successively (partly contempora-neously in the early and high Neolithic) in the forest-steppe belt of Western Siberia. Two methods were chosen to obtain the results: spore-and-pollen (palynological) and microbiomorphic analyses of the cultural layers of the settleme…
A palaeoenvironmental reconstruction of the rampart construction of the medieval ring-fort in Rozprza, Central Poland
During archaeological excavations of a medieval stronghold in Rozprza, a buried thick deposit of deep black (Dark Earth type) soil was discovered. A multianalytical (sedimentological, geochemical and archaeobotanical) study was carried out in order to identify traits the Rozprza Dark Earth. The analyses demonstrated that the soil was formed as an effect of surface accumulation of organic deposits from swampy areas and waste materials with rich ad…
Soil evolution and accumulation of loess-like material in the Chechen depression, Northern Caucasus, Russia
Palaeoenvironmental reconstruction of Hungarian kurgans on the basis of the examination of palaeosoils and phytolith analysis
The Black San Pablo Paleosol of the Teotihuacan Valley, Mexico
Although archaeologists have generally assumed that the ancient landscape in the Teotihuacan Valley was somewhat similar to the present day, recent research has documented large‐scale modification of the soil by accelerated human‐induced erosion–sedimentation processes from the pre‐Hispanic and Colonial periods up until the present. Consequently, the Formative and Classic period soil (approximately 400 B.C.–A.D. 650) is buried in most of the Teot…
Paleolandscape Reconstruction of the Abrau Peninsula Littoral (Krasnodar Territory)
Burial ground horizons dating as far back as the 6th–2nd centuries BC and the cultural layers associated with settlements dated to the Late Bronze (?) Age, the Classical Antiquity, and the Middle Ages, have been identified during a multidisciplinary study of sediments exposed by trenching at the entrance of Lobanova Shchel (Lobanova Gorge), near a burial ground of the 6th–2nd centuries BC. The study has provided insights into general regularities…
Dynamics of paleoenvironments in the Cis-Ural steppes during the mid- to late Holocene
The multi-layered settlement of Turganik in the Tok River valley (steppe region west of the Urals) has been studied using paleopedological and microbiomorphical methods. Early humans lived in the settlement during the Eneolithic epoch (the fifth millennium BC) and in the Early Bronze Age (the fourth millennium BC). The cultural layers attributable to the Atlantic period of the Holocene developed under conditions of a rather dry climate, with the …
A palaeoenvironmental reconstruction of the rampart construction of the medieval ring-fort in Rozprza, Central Poland
During archaeological excavations of a medieval stronghold in Rozprza, a buried thick deposit of deep black (Dark Earth type) soil was discovered. A multianalytical (sedimentological, geochemical and archaeobotanical) study was carried out in order to identify traits the Rozprza Dark Earth. The analyses demonstrated that the soil was formed as an effect of surface accumulation of organic deposits from swampy areas and waste materials with rich ad…
Microbiomarkers of the local environment and interior of Neolithic and Eneolithic dwellings (settlements of Mergen 6 and 7)
The paper concerns the analysis of the local environment around the multi-layer settlements of Mergen 6 and 7 situated in the immediate vicinity of each other. The settlements existed successively (partly contempora-neously in the early and high Neolithic) in the forest-steppe belt of Western Siberia. Two methods were chosen to obtain the results: spore-and-pollen (palynological) and microbiomorphic analyses of the cultural layers of the settleme…
Application of Microbiomorphic and Total Phosphorus Analyses to the Archaeological Study of the Sredny Zelenchuk Temple, Nizhny Arkhyz Hillfort
The article presents the results of the first geoarchaeological study of the materials of Christian burials identified in the interior of the Middle Zelenchuk temple of the 10th century in the Nizhne-Arkhyz ancient settlement (Republic of Karachay-Cherkessia). The results of microbiomorphic (phytolith) and total phosphorus content analyses allowed us to reveal previously unknown features of the funeral rites of the multicultural and multi-ethnic …
The Late Weichselian/Holocene transition on the East European Plain
Few sites in the East European Plain have yielded detailed multi-proxy data for the late Weichselian to Holocene transition. This paper provides a comprehensive palaeobotanical analysis of the lower part of a core of biogenic deposits from the Serteya Mire in the western part of the East European Plain (Western Russia). The studied reservoir, is located in a kettle hole and is dated to the Allerød, as confirmed by radiocarbon dating of the basal …
Geography (8 works) · Archaeology (7 works) · Geology (6 works) · Geology and Paleoclimatology Research (5 works) · Ancient and Medieval Archaeology Studies (4 works) · Marine and environmental studies (4 works) · Physical geography (4 works) · Soil and Environmental Studies (4 works) · Soil water (4 works) · Archaeology and ancient environmental studies (3 works)