Climatic changes, successions of peatlands and zonal vegetation, and peat accumulation dynamics in the holocene (the West-Siberia peat profile 'Vodorasdel')
The developmental history of peatland and dry land vegetation within the Ob-Vasugan watershed of Western Siberia was characterized according to features of the plant communities and climatic changes which were revealed by stratigraphic, spore-pollen and C14 (carbon) data obtained from a vertical pea...
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Published in | Climatic change Vol. 55; no. 1-2; pp. 175 - 181 |
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Main Authors | , , |
Format | Conference Proceeding Journal Article |
Language | English |
Published |
Dordrecht
Springer
01.10.2002
Springer Nature B.V |
Subjects | |
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Abstract | The developmental history of peatland and dry land vegetation within the Ob-Vasugan watershed of Western Siberia was characterized according to features of the plant communities and climatic changes which were revealed by stratigraphic, spore-pollen and C14 (carbon) data obtained from a vertical peat profile 'Vodorasdel'. Changes in the paleoecological environment over the last 10000 years were divided into five periods. The climate was characterized in the Holocene according to these periods. At the watershed studied, peatland-forming processes started about 9510 years ago resulting in 550 cm of peat accumulation. The rate of peat accumulation within the watershed decreased over time from 1.9-0.3 mm year-1. |
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AbstractList | The developmental history of peatland and dry land vegetation within the Ob-Vasugan watershed of Western Siberia was characterized according to features of the plant communities and climatic changes which were revealed by stratigraphic, spore-pollen and C14 (carbon) data obtained from a vertical peat profile 'Vodorasdel'. Changes in the paleoecological environment over the last 10000 years were divided into five periods. The climate was characterized in the Holocene according to these periods. At the watershed studied, peatland-forming processes started about 9510 years ago resulting in 550 cm of peat accumulation. The rate of peat accumulation within the watershed decreased over time from 1.9-0.3 mm year-1. The developmental history of peatland and dry land vegetation within the Ob-Vasugan watershed of Western Siberia was characterized according to features of the plant communities and climatic changes which were revealed by stratigraphic, spore-pollen and C super(14) (carbon) data obtained from a vertical peat profile `Vodorasdel'. Changes in the paleoecological environment over the last 10000 years were divided into five periods. The climate was characterized in the Holocene according to these periods. At the watershed studied, peatland-forming processes started about 9510 years ago resulting in 550 cm of peat accumulation. The rate of peat accumulation within the watershed decreased over time from 1.9-0.3 mm year super(- 1). Scientists characterized the developmental history of peatland and dry land vegetation within the Ob-Vasugan watershed of western Siberia based on analyses of the characteristics of plant communities in the region and evidence of historical climatic changes revealed by stratigraphic, spore-pollen and super(14)C data derived from a vertical peat profile <">Vodorasdel." Researchers divided observed changes in the palaeoecological environment over the past 10,000 years into five different periods. Climate during the Holocene was characterized according to these five periods. Evidence showed that peatland forming processes in the watershed under analysis were initiated some 9510 years in the past, producing a 550 cm accumulation of peat. Reductions in peat accumulation with time are detailed. |
Author | KARPENKO, Lyudmila V GLEBOV, Felix Z DASHKOVSKAYA, Irina S |
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Snippet | The developmental history of peatland and dry land vegetation within the Ob-Vasugan watershed of Western Siberia was characterized according to features of the... Scientists characterized the developmental history of peatland and dry land vegetation within the Ob-Vasugan watershed of western Siberia based on analyses of... |
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SubjectTerms | Accumulation Climate change Cotton Flowers & plants Forests Freshwater Holocene Mosses Norms Paleoecology Peat Peatlands Plant communities Pollen Precipitation Stratigraphy Taiga & tundra Temperature Vegetation Watersheds |
Title | Climatic changes, successions of peatlands and zonal vegetation, and peat accumulation dynamics in the holocene (the West-Siberia peat profile 'Vodorasdel') |
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