L A Orlova
Dados Biográficos
| ID | 631744 |
|---|---|
| NOME | L A Orlova |
| PRENOMES | L A |
| SOBRENOME | Orlova |
| ASSINATURA | ORLOVA L A |
| AFILIAÇÕES | V.S. Sobolev Institute of Geology and Mineralogy |
| VERIFICADO | Não |
| TOTAL DE OBRAS | 13 |
| TOTAL DE CITAÇÕES | 73 |
| TOTAL COMO AUTOR | 13 |
| TOTAL COMO EDITOR | 0 |
| PRIMEIRO ANO DE PUBLICAÇÃO | 1974 |
| ANO MAIS RECENTE DE PUBLICAÇÃO | 2016 |
| ÍNDICE H | 6 |
Human occupation of South Eastern Altai highlands (Russia) in the context of environmental changes
Paleodiet, Radiocarbon Chronology, and the Possibility of Freshwater Reservoir Effect for Preobrazhenka 6 Burial Ground, Western Siberia
This article presents the results of radiocarbon dating and a chronology of the Preobrazhenka 6 site of the Odino culture (Baraba forest steppe, western Siberia). Currently available 14 C data for the necropolis do not allow accurate determination of the presence or absence of reservoir effects, and as such, further research is needed. Accelerator mass spectrometry (AMS) 14 C dating of paired samples of terrestrial faunal and fish remains from a …
C Chronology of Burial Grounds of the Andronovo Period (Middle Bronze Age) in Baraba Forest Steppe, Western Siberia
This paper focuses on the chronology of Middle Bronze Age complexes in the Baraba forest steppe (western Siberia). Three sites were radiocarbon dated, Stary Tartas 4, Sopka 2, and Tartas 1. The Late Krotovo culture was dated to the 18–19th centuries BC, the Andronovo complex (Fedorovo stage) to the 15–18th centuries BC, and the Mixed Andronovo complex dated to the 15–17th centuries BC. These values are some 300–500 yr older than previously though…
Periods, Boundaries, and Contact Zones in the Far Eastern Insular World of the Neolithic
In the present article, a full summary of radiocarbon dates of Neolithic sites in Sakhalin and the Kuril Islands is used to elaborate a periodization of archaeological cultures in the Russian Far East. Materials assembled over recent years make it possible to reconstruct patterns of human adaptation to the changing Holocene environment, economic activities, and the exploitation of natural resources. Shifts in the boundaries of cultural zones are …
Climatic Signature and Radiocarbon Chronology of Middle and Late Pleniglacial Loess from Eurasia
Recent investigations devoted to the Eurasian loess formations have provided an integrated high-resolution climatic sequence well radiocarbon dated between 13.4 and 42.5 kyr BP on charcoal and wood remains. Here, we show that the reproducible climatic signature of this loess sequence can be compared by proxy-correlation with the Greenland ice climatic signals, taking into account the distribution of the aeolian components in both records. This co…
Evidence of Environmental Instability of the Lake Baikal Area After the Last Glaciation (Based on Pollen Records From Peatlands)
Pollen analysis of two dated sedimentary cores from lacustrine-boggy sediments in various parts of the Lake Baikal area yielded the first complete record of deep changes in the lake catchment area during the Late Glacial and Early Holocene. The Early Middle Holocene record shows an optimum – a humid and mild climate with warm winters between ca 10,000 and 7000 BP. During the Late Holocene, the climate grew more and more continental, and dark coni…
New pollen records of Late Pleistocene and Holocene changes of environment and climate in the Lower Amur River basin, NE Eurasia
Multidisciplinary paleontological and stratigraphic studies at Lugovskoe (2002–2004)
Post-glacial history of Siberian spruce (Picea obovata) in the Lake Baikal area and the significance of this species as a paleo-environmental indicator
C Chronology of Late Pleistocene–Holocene Events in the Nizhnee Priamurie (Southeast Russia)
The Russian Far East is characterized by widespread peat bogs with a sufficiently thick peat accumulation. A series of radiocarbon dates from the studied peat bogs (in Lower Amur) were obtained. Analysis of these dates shows that the total peat formation in this territory began in the Late Pleistocene–Holocene (11830 ± 820, TIG-157; 9975 ± 120, SOAN-4025). The rates of peat accumulation and the humidity index were counted. In addition, the botani…
C Wiggle Matching of the ‘Floating’ Tree-Ring Chronology from the Altai Mountains, Southern Siberia
The Bayesian approach to calibration of radiocarbon dates was used to wiggle-match the “floating” tree-ring chronology from a Pazyryk culture (Scythian-type complex from Sayan-Altai Mountain system, southern Siberia) burial ground in order to estimate the calendar age of its construction. Seventeen bidecadal tree-ring samples were 14 C dated with high precision (±20–30 yr). The results of wiggle-matching show that the Pazyryk-type burial mounds i…
The Reliability of Radiocarbon Dating Buried Soils
Variable 14 C ages of paleosol organic matter (OM) cause difficulties in interpreting 14 C data. We attempt to determine the reliability of OM 14 C dates by examining different carbon-containing materials from soil horizons and paleosol fractions
Some peculiarities of holocene processes in Western Siberia
Periods, Boundaries, and Contact Zones in the Far Eastern Insular World of the Neolithic
In the present article, a full summary of radiocarbon dates of Neolithic sites in Sakhalin and the Kuril Islands is used to elaborate a periodization of archaeological cultures in the Russian Far East. Materials assembled over recent years make it possible to reconstruct patterns of human adaptation to the changing Holocene environment, economic activities, and the exploitation of natural resources. Shifts in the boundaries of cultural zones are …
Multidisciplinary paleontological and stratigraphic studies at Lugovskoe (2002–2004)
The Reliability of Radiocarbon Dating Buried Soils
Variable 14 C ages of paleosol organic matter (OM) cause difficulties in interpreting 14 C data. We attempt to determine the reliability of OM 14 C dates by examining different carbon-containing materials from soil horizons and paleosol fractions
Human occupation of South Eastern Altai highlands (Russia) in the context of environmental changes
C Chronology of Burial Grounds of the Andronovo Period (Middle Bronze Age) in Baraba Forest Steppe, Western Siberia
This paper focuses on the chronology of Middle Bronze Age complexes in the Baraba forest steppe (western Siberia). Three sites were radiocarbon dated, Stary Tartas 4, Sopka 2, and Tartas 1. The Late Krotovo culture was dated to the 18–19th centuries BC, the Andronovo complex (Fedorovo stage) to the 15–18th centuries BC, and the Mixed Andronovo complex dated to the 15–17th centuries BC. These values are some 300–500 yr older than previously though…
Paleodiet, Radiocarbon Chronology, and the Possibility of Freshwater Reservoir Effect for Preobrazhenka 6 Burial Ground, Western Siberia
This article presents the results of radiocarbon dating and a chronology of the Preobrazhenka 6 site of the Odino culture (Baraba forest steppe, western Siberia). Currently available 14 C data for the necropolis do not allow accurate determination of the presence or absence of reservoir effects, and as such, further research is needed. Accelerator mass spectrometry (AMS) 14 C dating of paired samples of terrestrial faunal and fish remains from a …
C Wiggle Matching of the ‘Floating’ Tree-Ring Chronology from the Altai Mountains, Southern Siberia
The Bayesian approach to calibration of radiocarbon dates was used to wiggle-match the “floating” tree-ring chronology from a Pazyryk culture (Scythian-type complex from Sayan-Altai Mountain system, southern Siberia) burial ground in order to estimate the calendar age of its construction. Seventeen bidecadal tree-ring samples were 14 C dated with high precision (±20–30 yr). The results of wiggle-matching show that the Pazyryk-type burial mounds i…
Climatic Signature and Radiocarbon Chronology of Middle and Late Pleniglacial Loess from Eurasia
Recent investigations devoted to the Eurasian loess formations have provided an integrated high-resolution climatic sequence well radiocarbon dated between 13.4 and 42.5 kyr BP on charcoal and wood remains. Here, we show that the reproducible climatic signature of this loess sequence can be compared by proxy-correlation with the Greenland ice climatic signals, taking into account the distribution of the aeolian components in both records. This co…
Evidence of Environmental Instability of the Lake Baikal Area After the Last Glaciation (Based on Pollen Records From Peatlands)
Pollen analysis of two dated sedimentary cores from lacustrine-boggy sediments in various parts of the Lake Baikal area yielded the first complete record of deep changes in the lake catchment area during the Late Glacial and Early Holocene. The Early Middle Holocene record shows an optimum – a humid and mild climate with warm winters between ca 10,000 and 7000 BP. During the Late Holocene, the climate grew more and more continental, and dark coni…
Some peculiarities of holocene processes in Western Siberia
Some peculiarities of holocene processes in Western Siberia
The Reliability of Radiocarbon Dating Buried Soils
Variable 14 C ages of paleosol organic matter (OM) cause difficulties in interpreting 14 C data. We attempt to determine the reliability of OM 14 C dates by examining different carbon-containing materials from soil horizons and paleosol fractions
C Wiggle Matching of the ‘Floating’ Tree-Ring Chronology from the Altai Mountains, Southern Siberia
The Bayesian approach to calibration of radiocarbon dates was used to wiggle-match the “floating” tree-ring chronology from a Pazyryk culture (Scythian-type complex from Sayan-Altai Mountain system, southern Siberia) burial ground in order to estimate the calendar age of its construction. Seventeen bidecadal tree-ring samples were 14 C dated with high precision (±20–30 yr). The results of wiggle-matching show that the Pazyryk-type burial mounds i…
C Chronology of Late Pleistocene–Holocene Events in the Nizhnee Priamurie (Southeast Russia)
The Russian Far East is characterized by widespread peat bogs with a sufficiently thick peat accumulation. A series of radiocarbon dates from the studied peat bogs (in Lower Amur) were obtained. Analysis of these dates shows that the total peat formation in this territory began in the Late Pleistocene–Holocene (11830 ± 820, TIG-157; 9975 ± 120, SOAN-4025). The rates of peat accumulation and the humidity index were counted. In addition, the botani…
Post-glacial history of Siberian spruce (Picea obovata) in the Lake Baikal area and the significance of this species as a paleo-environmental indicator
Multidisciplinary paleontological and stratigraphic studies at Lugovskoe (2002–2004)
New pollen records of Late Pleistocene and Holocene changes of environment and climate in the Lower Amur River basin, NE Eurasia
Climatic Signature and Radiocarbon Chronology of Middle and Late Pleniglacial Loess from Eurasia
Recent investigations devoted to the Eurasian loess formations have provided an integrated high-resolution climatic sequence well radiocarbon dated between 13.4 and 42.5 kyr BP on charcoal and wood remains. Here, we show that the reproducible climatic signature of this loess sequence can be compared by proxy-correlation with the Greenland ice climatic signals, taking into account the distribution of the aeolian components in both records. This co…
Evidence of Environmental Instability of the Lake Baikal Area After the Last Glaciation (Based on Pollen Records From Peatlands)
Pollen analysis of two dated sedimentary cores from lacustrine-boggy sediments in various parts of the Lake Baikal area yielded the first complete record of deep changes in the lake catchment area during the Late Glacial and Early Holocene. The Early Middle Holocene record shows an optimum – a humid and mild climate with warm winters between ca 10,000 and 7000 BP. During the Late Holocene, the climate grew more and more continental, and dark coni…
Periods, Boundaries, and Contact Zones in the Far Eastern Insular World of the Neolithic
In the present article, a full summary of radiocarbon dates of Neolithic sites in Sakhalin and the Kuril Islands is used to elaborate a periodization of archaeological cultures in the Russian Far East. Materials assembled over recent years make it possible to reconstruct patterns of human adaptation to the changing Holocene environment, economic activities, and the exploitation of natural resources. Shifts in the boundaries of cultural zones are …
C Chronology of Burial Grounds of the Andronovo Period (Middle Bronze Age) in Baraba Forest Steppe, Western Siberia
This paper focuses on the chronology of Middle Bronze Age complexes in the Baraba forest steppe (western Siberia). Three sites were radiocarbon dated, Stary Tartas 4, Sopka 2, and Tartas 1. The Late Krotovo culture was dated to the 18–19th centuries BC, the Andronovo complex (Fedorovo stage) to the 15–18th centuries BC, and the Mixed Andronovo complex dated to the 15–17th centuries BC. These values are some 300–500 yr older than previously though…
Paleodiet, Radiocarbon Chronology, and the Possibility of Freshwater Reservoir Effect for Preobrazhenka 6 Burial Ground, Western Siberia
This article presents the results of radiocarbon dating and a chronology of the Preobrazhenka 6 site of the Odino culture (Baraba forest steppe, western Siberia). Currently available 14 C data for the necropolis do not allow accurate determination of the presence or absence of reservoir effects, and as such, further research is needed. Accelerator mass spectrometry (AMS) 14 C dating of paired samples of terrestrial faunal and fish remains from a …
Human occupation of South Eastern Altai highlands (Russia) in the context of environmental changes
Geology (13 obras) · Geography (12 obras) · Paleontology (10 obras) · Archaeology (9 obras) · Geology and Paleoclimatology Research (9 obras) · Radiocarbon dating (9 obras) · Archaeology and ancient environmental studies (8 obras) · Physical geography (8 obras) · Holocene (7 obras) · Pleistocene-Era Hominins and Archaeology (6 obras)