Elena D Lapshina
Biographic Data
| ID | 4640264 |
|---|---|
| NAME | Elena D Lapshina |
| GIVEN NAMES | Elena D |
| FAMILY NAME | Lapshina |
| SIGNATURE | LAPSHINA E D |
| AFFILIATIONS | Yugra State University |
| ORCID | 0000-0001-5571-7787 |
| VERIFIED | Yes |
| TOTAL WORKS | 8 |
| TOTAL CITATIONS | 9 |
| AUTHOR COUNT | 8 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2004 |
| LATEST PUBLICATION YEAR | 2026 |
| H-INDEX | 2 |
Regional and local drivers of vegetation and humidity dynamics in Western Siberia during the Holocene
The Western Siberian peatlands rank among the largest in the Northern Hemisphere. This study investigates peatland development and palaeohydrological changes of the Mukhrino mire during the Holocene focussing on climatic, regional and local factors. The multiproxy and multi-core approach reveals spatial variability driven by topography and sedimentary conditions. Our study integrates testate amoebae, plant macrofossils, peat geochemical and bioma…
Great Vasyugan Mire
Connecting biodiversity and human dimensions through ecosystem services
Key periods of peatland development and environmental changes in the middle taiga zone of Western Siberia during the Holocene
Defending dissertations in the Ifes in 2019
The biophysical climate mitigation potential of boreal peatlands during the growing season
Peatlands and forests cover large areas of the boreal biome and are critical for global climate regulation. They also regulate regional climate through heat and water vapour exchange with the atmosphere. Understanding how land-atmosphere interactions in peatlands differ from forests may therefore be crucial for modelling boreal climate system dynamics and for assessing climate benefits of peatland conservation and restoration. To assess the bioph…
Postglacial flooding and vegetation history on the Ob River terrace, central Western Siberia based on the palaeoecological record from Lake Svetlenkoye
The hemispheric-scale climatic fluctuations during the Holocene have probably influenced the large Siberian rivers. However, detailed studies of the West Siberian Plain postglacial environmental change are scarce and the records of millennial-scale palaeohydrology are nearly absent. This paper presents the Holocene palaeoecological reconstruction based on the sedimentary record of Lake Svetlenkoye, located near the confluence of major Siberian ri…
Holocene peat and carbon accumulation rates in the southern taiga of western Siberia
Although recent studies have recognized peatlands as a sink for atmospheric CO 2 , little is known about the role of Siberian peatlands in the global carbon cycle. We have estimated the Holocene peat and carbon accumulation rate in the peatlands of the southern taiga and subtaiga zones of western Siberia. We explain the accumulation rates by calculating the average peat accumulation rate and the long-term apparent rate of carbon accumulation (LOR…
Great Vasyugan Mire
Key periods of peatland development and environmental changes in the middle taiga zone of Western Siberia during the Holocene
Postglacial flooding and vegetation history on the Ob River terrace, central Western Siberia based on the palaeoecological record from Lake Svetlenkoye
The hemispheric-scale climatic fluctuations during the Holocene have probably influenced the large Siberian rivers. However, detailed studies of the West Siberian Plain postglacial environmental change are scarce and the records of millennial-scale palaeohydrology are nearly absent. This paper presents the Holocene palaeoecological reconstruction based on the sedimentary record of Lake Svetlenkoye, located near the confluence of major Siberian ri…
Connecting biodiversity and human dimensions through ecosystem services
Holocene peat and carbon accumulation rates in the southern taiga of western Siberia
Although recent studies have recognized peatlands as a sink for atmospheric CO 2 , little is known about the role of Siberian peatlands in the global carbon cycle. We have estimated the Holocene peat and carbon accumulation rate in the peatlands of the southern taiga and subtaiga zones of western Siberia. We explain the accumulation rates by calculating the average peat accumulation rate and the long-term apparent rate of carbon accumulation (LOR…
Defending dissertations in the Ifes in 2019
The biophysical climate mitigation potential of boreal peatlands during the growing season
Peatlands and forests cover large areas of the boreal biome and are critical for global climate regulation. They also regulate regional climate through heat and water vapour exchange with the atmosphere. Understanding how land-atmosphere interactions in peatlands differ from forests may therefore be crucial for modelling boreal climate system dynamics and for assessing climate benefits of peatland conservation and restoration. To assess the bioph…
Postglacial flooding and vegetation history on the Ob River terrace, central Western Siberia based on the palaeoecological record from Lake Svetlenkoye
The hemispheric-scale climatic fluctuations during the Holocene have probably influenced the large Siberian rivers. However, detailed studies of the West Siberian Plain postglacial environmental change are scarce and the records of millennial-scale palaeohydrology are nearly absent. This paper presents the Holocene palaeoecological reconstruction based on the sedimentary record of Lake Svetlenkoye, located near the confluence of major Siberian ri…
Great Vasyugan Mire
Connecting biodiversity and human dimensions through ecosystem services
Key periods of peatland development and environmental changes in the middle taiga zone of Western Siberia during the Holocene
Regional and local drivers of vegetation and humidity dynamics in Western Siberia during the Holocene
The Western Siberian peatlands rank among the largest in the Northern Hemisphere. This study investigates peatland development and palaeohydrological changes of the Mukhrino mire during the Holocene focussing on climatic, regional and local factors. The multiproxy and multi-core approach reveals spatial variability driven by topography and sedimentary conditions. Our study integrates testate amoebae, plant macrofossils, peat geochemical and bioma…
Environmental Science (6 works) · Geography (6 works) · Peat (6 works) · Peatlands and Wetlands Ecology (5 works) · Climate change (4 works) · Ecology (4 works) · Geology and Paleoclimatology Research (4 works) · Holocene (4 works) · Physical geography (4 works) · Boreal (3 works)