The impact of early smelting on the environment of Huoshiliang in Hexi Corridor, NW China, as recorded by fossil charcoal and chemical elements

dc.contributor.authorLi, XQen_AU
dc.contributor.authorSun, Nen_AU
dc.contributor.authorDodson, JRen_AU
dc.contributor.authorJi, Men_AU
dc.contributor.authorZhao, KLen_AU
dc.contributor.authorZhou, XYen_AU
dc.date.accessioned2011-10-06T05:23:31Zen_AU
dc.date.available2011-10-06T05:23:31Zen_AU
dc.date.issued2011-05-15en_AU
dc.date.statistics2011-10-06en_AU
dc.description.abstractRecent research has greatly increased our knowledge of early human impacts on the environment. Records of fossil charcoal and chemical elements from a bronze smelting site at Huoshiliang, in the Hexi corridor of northwest China, provide material with which to estimate the extent of smelting activity and its impact on the environment. Analysis of the microstructure of wood fossil charcoal is used to identify the types of charred wood and to reconstruct the local vegetation present during the period of smelting. Four wood types were used as firewood for smelting: Tamarix, Populus, Salix, and Polygonaceae. The assemblages of fossil charcoal showed that Tamarix was the most dominant shrub and was widely used as firewood, as a percentage of charcoal it increased from 89% to 97% over the smelting period. Populus. Polygonaceae and Salix were much less common and finally disappeared completely. When the trees and shrubs were used as fuel, the vegetation cover was reduced and erosion rates increased. This erosion increase was recorded in the higher values of the Rb/Sr ratio in the lacustrine sediment of Tiaohu lake, located near the Huoshiliang site. The deforestation caused by smelting activity sharply reduced the vegetation coverage and had serious impacts on the environment. When the available fuel wood ceased to meet the needs of smelting and human settlement, the Huoshiliang site was eventually abandoned in about 1860 BC. (C) 2011 Elsevier B.V.en_AU
dc.identifier.citationLi, X.Q., Sun, N., Dodson, J., Ji, M., Zhao, K.L., Zhou, X.Y. (2011). The impact of early smelting on the environment of Huoshiliang in Hexi Corridor, NW China, as recorded by fossil charcoal and chemical elements. Palaeogeography, Palaeoclimatology, Palaeoecology, 305 (1-4); 329-336. doi:10.1016/j.palaeo.2011.03.015en_AU
dc.identifier.govdoc3401en_AU
dc.identifier.issn0031-0182en_AU
dc.identifier.issue1-4en_AU
dc.identifier.journaltitlePalaeogeography, Palaeoclimatology, Palaeoecologyen_AU
dc.identifier.pagination329-336en_AU
dc.identifier.urihttp://dx.doi.org/10.1016/j.palaeo.2011.03.015en_AU
dc.identifier.urihttp://apo.ansto.gov.au/dspace/handle/10238/3796en_AU
dc.identifier.volume305en_AU
dc.language.isoenen_AU
dc.publisherElsevieren_AU
dc.subjectFossilsen_AU
dc.subjectSmeltingen_AU
dc.subjectCharcoalen_AU
dc.subjectEnvironmenten_AU
dc.subjectWooden_AU
dc.subjectPlantsen_AU
dc.titleThe impact of early smelting on the environment of Huoshiliang in Hexi Corridor, NW China, as recorded by fossil charcoal and chemical elementsen_AU
dc.typeJournal Articleen_AU
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