Pollen and phytolith evidence for rice cultivation and vegetation change during the mid-late holocene at the Jiangli site, Suzhou, East China

Pollen and phytolith analyses were undertaken at the Jiangli site in Suzhou, Jiangsu Province, combined with studies on macrofossils by flotation. The concentration of pollen decreased while the percentage of Poaceae pollen in the profile increased from the late phase of the Majiabang Culture to the...

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Veröffentlicht in:PloS one 2014-01, Vol.9 (1), p.e86816
Hauptverfasser: Qiu, Zhenwei, Jiang, Hongen, Ding, Jinlong, Hu, Yaowu, Shang, Xue
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description Pollen and phytolith analyses were undertaken at the Jiangli site in Suzhou, Jiangsu Province, combined with studies on macrofossils by flotation. The concentration of pollen decreased while the percentage of Poaceae pollen in the profile increased from the late phase of the Majiabang Culture to the Songze Culture suggesting that human impact on the local environment intensified gradually. The discovery of rice paddy implies a relatively advanced rice cultivation in this area during the middle-late Holocene. Other than phytoliths, the high percentage of Oryza-type Poaceae pollen (larger than 40 µm) supplied robust evidence for the existence of rice paddy. Moreover, the fact that the farther from the rice paddy, the lower the concentration and percentage of Poaceae pollen also proves that the dispersal and deposition of pollen is inversely proportional to the distance.
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subjects Agriculture
Archaeology
Biology
China
Climate Change
Corn
Crops, Agricultural
Cultivation
Dispersal
Earth Sciences
Environment
Environmental impact
Evolution
Farming
Flotation
Fossils
Grain cultivation
Historic buildings & sites
Holocene
Human factors
Human impact
Human influences
Human-environment relationship
Humans
Laboratories
Neolithic
Oryza
Oryza - growth & development
Paleontology
Poaceae - growth & development
Pollen
Rice
Rice fields
Seeds
Social and Behavioral Sciences
Studies
Vegetation
title Pollen and phytolith evidence for rice cultivation and vegetation change during the mid-late holocene at the Jiangli site, Suzhou, East China
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