A V Panin
Datos Biográficos
| ID | 52067 |
|---|---|
| NOMBRE | A V Panin |
| NOMBRES | A V |
| APELLIDO | Panin |
| FIRMA | PANIN A V |
| AFILIACIONES | Institute of Geography |
| ORCID | 0000-0001-9587-1260 |
| VERIFICADO | Sí |
| TOTAL DE OBRAS | 24 |
| TOTAL DE CITAS | 10 |
| TOTAL COMO AUTOR | 24 |
| TOTAL COMO EDITOR | 0 |
| PRIMER AÑO DE PUBLICACIÓN | 2012 |
| AÑO MÁS RECIENTE DE PUBLICACIÓN | 2026 |
| ÍNDICE H | 2 |
From dead ice to a small lake
New Data on the Stone Age of the Southeastern Caspian Region
Field study in Turkmenistan was organized in March 2025 as part of several research programs. During the study, known Stone Age sites were visited and several areas within the Krasnovodsk Peninsula, the Great Balkhan Range, the Kemal-Uzboy Depression, and the Kyzylburun Range were surveyed. As part of the study, we characterized geomorphological situation at several Stone Age sites explored in the second half of the 20th century, surveyed for new…
Radiocarbon dating of the end of the latest Caspian Sea overflow through the Manych Depression (southeastern European Plain)
The Manych Depression is a relatively narrow elongated depression of tectonic origin, connecting the Caspian and Azov-Black Sea basins. The Caspian Sea repeatedly discharged its waters through this depression into the Black Sea and further into the Mediterranean Sea during the Quaternary period. The last discharge occurred in MIS 2 when the Khvalynian transgression waters exceeded the drainage divide between those two basins. The geochronology of…
The World of Middle Palaeolithic Humans of the Donbass and Azov Regions
The Middle Paleolithic, as an epoch in the development of human society, was characterized by the homeostasis between the socio-cultural systems and their natural environments. Middle Paleolithic сommunities settled in the areas with the most favorable combinations of basic resources. At that time, almost the entire territory of the southern part of the Russian Plain, including the Donbass and Azov regions, was dominated by steppe landscapes. In …
Hydrological Regime of Rivers in the Periglacial Zone of the East European Plain in the Late MIS 2
At the end of the Pleniglacial and the first half of the Late Glacial period, approximately between 18 and 14 ka BP, rivers of the central and southern parts of the East European Plain had channels up to 10 times as large as the present day channels of the same rivers. These ancient channels, called large meandering palaeochannels, are widespread in river floodplains and low terraces. The hydrological regime of these large rivers is of great inte…
Short-Term Climatic Oscillations in the Central Region of the East-European Plain at the Beginning of the Holocene Based on Palynological Studies of Lacustrine Deposits
The Preboreal (11.75–10.70 ka BP) is still the least paleogeographically studied time interval in the central part of the East European Plain. High-resolution multi-proxy studies of lacustrine sediments at the Seltso site located in the Desna River floodplain (Dnieper River basin) were conducted. Radiocarbon dating, loss-on-ignition determination, sedimentological and palynological studies and identification of Non-Pollen Palynomorphs in lacustri…
Palaeoenvironmental Conditions of the Upper Middle Pleistocene Warm Intervals in the Upper Volga Region, Northwestern Russia, Based on Palynological, Paleocarpological and Quantitative Geochronologica…
The climatostratigraphic scale of the Upper Middle Pleistocene in the northwest of the East European Plain contains a number of controversial issues, one of which is the position of the Likhvin (Holstein) Interglacial and lesser warm (interstadial) climatic events. To approach this problem, we have studied two sections of Quaternary deposits, Bolshaya Kosha (a well-known and long-studied natural exposure) and Nazarovo (a new, previously unknown s…
Aeolian sedimentation in the Vychegda river valley, north-eastern Europe, during MIS 2–1
Chronology of the Upper Palaeolithic Sites of Byki (Centre of the East European Plain) According to 14C and OSL Dating
Series of 14C dates from cultural layers (CL) of Byki sites are in the range 1—5 thousand years. Simple statistical processing does not allow to narrow down the age estimates. To assess the reliability of 14C dates, we developed an approach based on the assessment of sedimentation dynamics using luminescence (OSL) dating and age determination of the main lithostratigraphic units. The OSL method was used to date the section of the multilayer site …
Multi-scale palaeolandscape reconstruction at the Upper Paleolithic Byki sites, central East European Plain
Initial settlement of the Upper Volga region, Centre of the East European Plain, in the Late Glacial and Early Holocene (based on geoarchaeological research in the Zabolotsky peat bog area)
Evolution of the Upper Reaches of Fluvial Systems within the Area of the East European Plain Glaciated during MIS 6
The headwaters of fluvial systems on the East European Plain between the boundaries of the Marine Isotope Stage 2 (MIS 2) and MIS 6 glaciations evolved during the last 150,000 years. At least three main events of high surface runoff caused intensive erosion: at the end of MIS 6, at the end of MIS 2 and in the Middle Holocene. Erosion developed in the territory with variable resistance of geological substrate, from hard-to-erode tills to weak sand…
Landscape development history of the Zabolotsky peat bog in the context of initial settlement of the Dubna River lowland (Upper Volga basin)
Zabolotsky peat bog is a unique biospheric and cultural-historical archive located in the north of the Moscow Region on the territory of the Dubna River lowland. Despite the advances in studying the Zabolotsky region, the question of reconstruction of the primitive population habitat remains unresolved. Until recently, it has been be-lieved that in the Late Valdai period, the Dubna River lowland was covered by the waters of an extensive glacier-d…
Initial Development of the Zabolotye Region Based on the Recent Geoarchaeological Studies
В 2018 г. были возобновлены геоархеологические исследования в котловине Заболотского палеоозера (Московская область) - одного из реликтов территории Дубнинской низменности. В процессе трехлетних работ был выполнен значительный объем изысканий, приведших к радикальному пересмотру представлений о развитии геоморфологической обстановки изучаемого региона. Было установлено, что в течение последней (валдайской) ледниковой эпохи на этой территории госп…
The studies on the Sungir Upper Paleolithic site in 2014–2015
The article is devoted to the results of archaeological excavations carried out on the Sungir in 2014-2015. The main purpose of these works was to obtain new data on the spatial structure of the cultural layer of the Sungir site. The relevance of these studies is caused by still unsolved question of whether Sungir can be considered as a site with a complex archaeological stratigraphy or the features of its spatial structure are only the result of…
The time of emergence of the Gnezdovo settlement based on radiocarbon dating
The Late Quaternary Evolution of the Upper Reaches of Fluvial Systems in the Southern East European Plain
Networks of dry valleys (or balkas) and hollows in the upper reaches of fluvial basins in extraglacial areas in the Penultimate Glaciation (Marine Isotope Stage 6—MIS 6) regions of the East European Plain demonstrate clear incision/aggradation rhythms corresponding to global glacial/interglacial climate cycles. The first phase of each incision/aggradation rhythm began after the global glacial maximum and was characterized by a cool and humid clim…
Pleistocene stratigraphy of the Vychegda River basin, European North-East
Magnitude and chronology of extreme floods in the last 2 ka based on the stratigraphy of a riverine archeological site (Schurovo settlement, middle Oka River, Central European Russia)
Climatic fluctuations reflected in the evolution of fluvial systems of Central-Eastern Europe (60–8 ka cal BP)
Multidisciplinary field training in undergraduate Physical Geography
Field training is seen as a central component of the discipline of Physical Geography and an essential part of the undergraduate curriculum. This paper explores the structure and relationships between fieldwork and theoretical courses and the abundant experiences of field training in the undergraduate curriculum of 37 Russian universities. It details a case study of the Faculty of Geography, Lomonosov Moscow State University, Russia's largest cen…
The Application of Cliff Degradation Models for Estimation of the Initial Height of Rammed‐earth Walls (Por‐bajin Fortress, Southern Siberia, Russia)
The main objective of this study is to recover the initial geometry of earthen walls from the shape of wall remains. The original parameters of the walls have been estimated by fitting the field‐measured profiles with the theoretical shape predicted by the model. We estimate: (i) the initial wall height (between 2 and 3 m); (ii) their shape (vertical or nearly vertical); and (iii) the time for complete degradation (between 250 and 400 years, depe…
Paleochannel Studies in Archaeology
Geological and geomorphological settings are often taken into account when choosing strategy in archaeological studies. In the Vychegda River valley (Archangelsk Province, Komi Republic), at the end of the Late Pleistocene and in the Holocene, lateral channel migrations were the dominant process of riverine landscape changes and hence directly influenced human occupation of the valley. Therefore, to assess the physical settings of archaeological …
Radiocarbon Chronology of the Schurovo Burial Mound Cremation Complex (Viking Times, Middle Oka River, Russia)
Excavation of the Schurovo archaeological site, located on a ∼12-m river terrace, has revealed 3 occupation periods: 1) as a dwelling site of the Migration period (4th–5th centuries AD); 2) as local burial mounds (termed “houses of the dead” in Russian); 3) and as a ground burial period, which left a cremation layer directly on the ground and is now covered by the Little Ice Age overbank alluvium. The latter 2 periods contain few artifacts, which…
Multidisciplinary field training in undergraduate Physical Geography
Field training is seen as a central component of the discipline of Physical Geography and an essential part of the undergraduate curriculum. This paper explores the structure and relationships between fieldwork and theoretical courses and the abundant experiences of field training in the undergraduate curriculum of 37 Russian universities. It details a case study of the Faculty of Geography, Lomonosov Moscow State University, Russia's largest cen…
Paleochannel Studies in Archaeology
Geological and geomorphological settings are often taken into account when choosing strategy in archaeological studies. In the Vychegda River valley (Archangelsk Province, Komi Republic), at the end of the Late Pleistocene and in the Holocene, lateral channel migrations were the dominant process of riverine landscape changes and hence directly influenced human occupation of the valley. Therefore, to assess the physical settings of archaeological …
Landscape development history of the Zabolotsky peat bog in the context of initial settlement of the Dubna River lowland (Upper Volga basin)
Zabolotsky peat bog is a unique biospheric and cultural-historical archive located in the north of the Moscow Region on the territory of the Dubna River lowland. Despite the advances in studying the Zabolotsky region, the question of reconstruction of the primitive population habitat remains unresolved. Until recently, it has been be-lieved that in the Late Valdai period, the Dubna River lowland was covered by the waters of an extensive glacier-d…
Radiocarbon dating of the end of the latest Caspian Sea overflow through the Manych Depression (southeastern European Plain)
The Manych Depression is a relatively narrow elongated depression of tectonic origin, connecting the Caspian and Azov-Black Sea basins. The Caspian Sea repeatedly discharged its waters through this depression into the Black Sea and further into the Mediterranean Sea during the Quaternary period. The last discharge occurred in MIS 2 when the Khvalynian transgression waters exceeded the drainage divide between those two basins. The geochronology of…
Radiocarbon Chronology of the Schurovo Burial Mound Cremation Complex (Viking Times, Middle Oka River, Russia)
Excavation of the Schurovo archaeological site, located on a ∼12-m river terrace, has revealed 3 occupation periods: 1) as a dwelling site of the Migration period (4th–5th centuries AD); 2) as local burial mounds (termed “houses of the dead” in Russian); 3) and as a ground burial period, which left a cremation layer directly on the ground and is now covered by the Little Ice Age overbank alluvium. The latter 2 periods contain few artifacts, which…
Multidisciplinary field training in undergraduate Physical Geography
Field training is seen as a central component of the discipline of Physical Geography and an essential part of the undergraduate curriculum. This paper explores the structure and relationships between fieldwork and theoretical courses and the abundant experiences of field training in the undergraduate curriculum of 37 Russian universities. It details a case study of the Faculty of Geography, Lomonosov Moscow State University, Russia's largest cen…
The Application of Cliff Degradation Models for Estimation of the Initial Height of Rammed‐earth Walls (Por‐bajin Fortress, Southern Siberia, Russia)
The main objective of this study is to recover the initial geometry of earthen walls from the shape of wall remains. The original parameters of the walls have been estimated by fitting the field‐measured profiles with the theoretical shape predicted by the model. We estimate: (i) the initial wall height (between 2 and 3 m); (ii) their shape (vertical or nearly vertical); and (iii) the time for complete degradation (between 250 and 400 years, depe…
Paleochannel Studies in Archaeology
Geological and geomorphological settings are often taken into account when choosing strategy in archaeological studies. In the Vychegda River valley (Archangelsk Province, Komi Republic), at the end of the Late Pleistocene and in the Holocene, lateral channel migrations were the dominant process of riverine landscape changes and hence directly influenced human occupation of the valley. Therefore, to assess the physical settings of archaeological …
Climatic fluctuations reflected in the evolution of fluvial systems of Central-Eastern Europe (60–8 ka cal BP)
Magnitude and chronology of extreme floods in the last 2 ka based on the stratigraphy of a riverine archeological site (Schurovo settlement, middle Oka River, Central European Russia)
The time of emergence of the Gnezdovo settlement based on radiocarbon dating
The Late Quaternary Evolution of the Upper Reaches of Fluvial Systems in the Southern East European Plain
Networks of dry valleys (or balkas) and hollows in the upper reaches of fluvial basins in extraglacial areas in the Penultimate Glaciation (Marine Isotope Stage 6—MIS 6) regions of the East European Plain demonstrate clear incision/aggradation rhythms corresponding to global glacial/interglacial climate cycles. The first phase of each incision/aggradation rhythm began after the global glacial maximum and was characterized by a cool and humid clim…
Pleistocene stratigraphy of the Vychegda River basin, European North-East
Initial Development of the Zabolotye Region Based on the Recent Geoarchaeological Studies
В 2018 г. были возобновлены геоархеологические исследования в котловине Заболотского палеоозера (Московская область) - одного из реликтов территории Дубнинской низменности. В процессе трехлетних работ был выполнен значительный объем изысканий, приведших к радикальному пересмотру представлений о развитии геоморфологической обстановки изучаемого региона. Было установлено, что в течение последней (валдайской) ледниковой эпохи на этой территории госп…
The studies on the Sungir Upper Paleolithic site in 2014–2015
The article is devoted to the results of archaeological excavations carried out on the Sungir in 2014-2015. The main purpose of these works was to obtain new data on the spatial structure of the cultural layer of the Sungir site. The relevance of these studies is caused by still unsolved question of whether Sungir can be considered as a site with a complex archaeological stratigraphy or the features of its spatial structure are only the result of…
Evolution of the Upper Reaches of Fluvial Systems within the Area of the East European Plain Glaciated during MIS 6
The headwaters of fluvial systems on the East European Plain between the boundaries of the Marine Isotope Stage 2 (MIS 2) and MIS 6 glaciations evolved during the last 150,000 years. At least three main events of high surface runoff caused intensive erosion: at the end of MIS 6, at the end of MIS 2 and in the Middle Holocene. Erosion developed in the territory with variable resistance of geological substrate, from hard-to-erode tills to weak sand…
Landscape development history of the Zabolotsky peat bog in the context of initial settlement of the Dubna River lowland (Upper Volga basin)
Zabolotsky peat bog is a unique biospheric and cultural-historical archive located in the north of the Moscow Region on the territory of the Dubna River lowland. Despite the advances in studying the Zabolotsky region, the question of reconstruction of the primitive population habitat remains unresolved. Until recently, it has been be-lieved that in the Late Valdai period, the Dubna River lowland was covered by the waters of an extensive glacier-d…
Hydrological Regime of Rivers in the Periglacial Zone of the East European Plain in the Late MIS 2
At the end of the Pleniglacial and the first half of the Late Glacial period, approximately between 18 and 14 ka BP, rivers of the central and southern parts of the East European Plain had channels up to 10 times as large as the present day channels of the same rivers. These ancient channels, called large meandering palaeochannels, are widespread in river floodplains and low terraces. The hydrological regime of these large rivers is of great inte…
Short-Term Climatic Oscillations in the Central Region of the East-European Plain at the Beginning of the Holocene Based on Palynological Studies of Lacustrine Deposits
The Preboreal (11.75–10.70 ka BP) is still the least paleogeographically studied time interval in the central part of the East European Plain. High-resolution multi-proxy studies of lacustrine sediments at the Seltso site located in the Desna River floodplain (Dnieper River basin) were conducted. Radiocarbon dating, loss-on-ignition determination, sedimentological and palynological studies and identification of Non-Pollen Palynomorphs in lacustri…
Palaeoenvironmental Conditions of the Upper Middle Pleistocene Warm Intervals in the Upper Volga Region, Northwestern Russia, Based on Palynological, Paleocarpological and Quantitative Geochronologica…
The climatostratigraphic scale of the Upper Middle Pleistocene in the northwest of the East European Plain contains a number of controversial issues, one of which is the position of the Likhvin (Holstein) Interglacial and lesser warm (interstadial) climatic events. To approach this problem, we have studied two sections of Quaternary deposits, Bolshaya Kosha (a well-known and long-studied natural exposure) and Nazarovo (a new, previously unknown s…
Aeolian sedimentation in the Vychegda river valley, north-eastern Europe, during MIS 2–1
Chronology of the Upper Palaeolithic Sites of Byki (Centre of the East European Plain) According to 14C and OSL Dating
Series of 14C dates from cultural layers (CL) of Byki sites are in the range 1—5 thousand years. Simple statistical processing does not allow to narrow down the age estimates. To assess the reliability of 14C dates, we developed an approach based on the assessment of sedimentation dynamics using luminescence (OSL) dating and age determination of the main lithostratigraphic units. The OSL method was used to date the section of the multilayer site …
Multi-scale palaeolandscape reconstruction at the Upper Paleolithic Byki sites, central East European Plain
Initial settlement of the Upper Volga region, Centre of the East European Plain, in the Late Glacial and Early Holocene (based on geoarchaeological research in the Zabolotsky peat bog area)
New Data on the Stone Age of the Southeastern Caspian Region
Field study in Turkmenistan was organized in March 2025 as part of several research programs. During the study, known Stone Age sites were visited and several areas within the Krasnovodsk Peninsula, the Great Balkhan Range, the Kemal-Uzboy Depression, and the Kyzylburun Range were surveyed. As part of the study, we characterized geomorphological situation at several Stone Age sites explored in the second half of the 20th century, surveyed for new…
Radiocarbon dating of the end of the latest Caspian Sea overflow through the Manych Depression (southeastern European Plain)
The Manych Depression is a relatively narrow elongated depression of tectonic origin, connecting the Caspian and Azov-Black Sea basins. The Caspian Sea repeatedly discharged its waters through this depression into the Black Sea and further into the Mediterranean Sea during the Quaternary period. The last discharge occurred in MIS 2 when the Khvalynian transgression waters exceeded the drainage divide between those two basins. The geochronology of…
The World of Middle Palaeolithic Humans of the Donbass and Azov Regions
The Middle Paleolithic, as an epoch in the development of human society, was characterized by the homeostasis between the socio-cultural systems and their natural environments. Middle Paleolithic сommunities settled in the areas with the most favorable combinations of basic resources. At that time, almost the entire territory of the southern part of the Russian Plain, including the Donbass and Azov regions, was dominated by steppe landscapes. In …
From dead ice to a small lake
Geology (20 obras) · Geography (19 obras) · Paleontology (15 obras) · Archaeology (13 obras) · Geology and Paleoclimatology Research (13 obras) · Marine and environmental studies (13 obras) · Physical geography (13 obras) · Archaeology and ancient environmental studies (9 obras) · Fluvial (9 obras) · Structural basin (9 obras)