Natural and anthropogenic impacts on Lake Ladoga and its catchment area through the late glacial and Holocene according to a new paleolimnological record
A ca. 12,700 year-long pollen and diatom record, as well as data on lithology, geochemistry, and grain size were obtained from two sediment cores retrieved in the southwest part of Lake Ladoga. Changes in phosphorus content during the Holocene were recorded from this sequence dated by the radiocarbo...
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description | A ca. 12,700 year-long pollen and diatom record, as well as data on lithology, geochemistry, and grain size were obtained from two sediment cores retrieved in the southwest part of Lake Ladoga. Changes in phosphorus content during the Holocene were recorded from this sequence dated by the radiocarbon method. An increase in phosphorus, loss-on-ignition and the Fe/Mn ratio was recorded during the climatic optimum of the Holocene ca. 7500–7250 cal yr BP. At the same time, pollen data showed the spread of broad-leaved forests. The peak in phosphorus in the upper part of the core associated with anthropogenic activities is smaller to the peak corresponding to the Holocene climatic optimum. This may indicate that climatic factors affect the ecosystems of large lakes more significantly than anthropogenic ones. According to our new pollen data, first human impact is recorded in Lake Ladoga sediments ca. 2580 cal yr BP. |
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Changes in phosphorus content during the Holocene were recorded from this sequence dated by the radiocarbon method. An increase in phosphorus, loss-on-ignition and the Fe/Mn ratio was recorded during the climatic optimum of the Holocene ca. 7500–7250 cal yr BP. At the same time, pollen data showed the spread of broad-leaved forests. The peak in phosphorus in the upper part of the core associated with anthropogenic activities is smaller to the peak corresponding to the Holocene climatic optimum. This may indicate that climatic factors affect the ecosystems of large lakes more significantly than anthropogenic ones. 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Changes in phosphorus content during the Holocene were recorded from this sequence dated by the radiocarbon method. An increase in phosphorus, loss-on-ignition and the Fe/Mn ratio was recorded during the climatic optimum of the Holocene ca. 7500–7250 cal yr BP. At the same time, pollen data showed the spread of broad-leaved forests. The peak in phosphorus in the upper part of the core associated with anthropogenic activities is smaller to the peak corresponding to the Holocene climatic optimum. This may indicate that climatic factors affect the ecosystems of large lakes more significantly than anthropogenic ones. According to our new pollen data, first human impact is recorded in Lake Ladoga sediments ca. 2580 cal yr BP.</abstract><cop>Dordrecht</cop><pub>Springer Netherlands</pub><doi>10.1007/s10933-024-00329-9</doi><tpages>19</tpages></addata></record> |
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subjects | anthropogenic activities Anthropogenic factors Aquatic ecosystems Bacillariophyceae carbon radioisotopes Catchment area Catchment areas Climate Change Cores Diatoms Earth and Environmental Science Earth Sciences Forests Freshwater & Marine Ecology Geochemistry Geology Grain size Holocene Holocene epoch Human impact Human influences Lakes Lithology Original Paper Paleontology Papal visits Phosphorus phosphorus content Physical Geography Pollen Radiocarbon dating Sediment Sedimentation & deposition Sedimentology Sediments Taiga & tundra Topography watersheds |
title | Natural and anthropogenic impacts on Lake Ladoga and its catchment area through the late glacial and Holocene according to a new paleolimnological record |
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