Natural and Anthropogenic Changes in the Soils and Environment of the Moskva River Floodplain in the Holocene: Pedogenic, Palynological, and Anthracological Evidences
作者: A. L. AleksandrovskiiE. G. ErshovaE. V. PonomarenkoN. A. KrenkeV. V. Skripkin
作者单位: 1Institute of Geography, Russian Academy of Sciences
2Kazan Federal University
3University of Ottawa, Faculty of Geography
4Institute of Archaeology, Russian Academy of Sciences
5Kyiv Radiocarbon Laboratory, National Academy of Sciences of Ukraine
刊名: Eurasian Soil Science, 2018, Vol.51 (6), pp.613-627
来源数据库: Springer Journal
DOI: 10.1134/S1064229318060029
关键词: PaleosolsPaleobotanical methodsExtreme environmental conditionsForest zoneDark-humus soils
英文摘要: Abstract(#br)Several series of well-developed paleosols of different ages have been examined on the Moskva River floodplain. In the beginning of the Holocene, forest-steppe biomes were widespread in this area, and dark-humus (Black) soils with stable humate humus and without features of textural differentiation predominated on the floodplain. The presence of meadow-steppe vegetation communities during this period is confirmed by the results of palynological and anthracological analyses. The lower paleosol in section RANIS 2 is represented by the deep humus horizon with 14 C dates from 5500 to 8400 BP and the carbonate-accumulative horizon; it also contains large and deep tunnels of burrowing animals typical of chernozems. Wood charcoal is absent, and pollen of Artemisia and Chenopodium...
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影响因子:0.216 (2012)

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