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You are here: Home Archive 2008 Geo-ecological transect studies in northeast Tibet (Qinghai, China) reveal human-made mid- Holocene environmental changes in the upper Yellow River catchment changing forest to grassland

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Geo-ecological transect studies in northeast Tibet (Qinghai, China) reveal human-made mid- Holocene environmental changes in the upper Yellow River catchment changing forest to grassland

DOI: 10.3112/erdkunde.2008.03.01
Year: 2008
Vol: 62
Issue: 3
Pages: 187-199
Summary:

Geo-ecological transect studies in the pastures of the upper catchment of the Huang He (99°30’–100°00’E/35°30’– 35°40’N; 3,000–4,000 m a.s.l., Qinghai province, China) revealed evidence that pastures replace forests. Plot-based vegetation records and fenced grazing exclosure experiments enabled the identification of grazing indicator plants for the first time. The mapping of vegetation patterns of pastures with isolated juniper and spruce forests raise questions as to the origin of the grasslands, which are widely classified as “natural” at present. Soil investigations and charcoal fragments of Juniperus (8,155 ± 63 uncal BP) and Picea (6,665 ± 59 uncal BP) provide evidence of the wider presence of forests. As temperatures and rainfall records undoubtedly represent a forest climate, it is assumed that the present pastures have replaced forests. Circumstantial evidence arising from investigations into the environmental history of the Holocene effectively substantiates this theory.

Zusammenfassung:

Geoökologische Transektuntersuchungen in Hochweiden des oberen Einzugsgebietes des Gelben Flusses (99°30‘–100°00‘E/35°30‘–35°40‘N; 3.000–4.000 m NN, Provinz Qinghai, China) geben Hinweise auf ältere, mutmaßlich menschverursachte Umweltveränderungen. Fünfjährige Weideanschlussexperimente und floristisch vollständige Vegetationsaufnahmen erlauben erstmals die Identifizierung von Weidezeigerpflanzen. Vegetationsmosaike von Triftweiden mit isolierten Baumvorkommen in Normalstandorten sind Grundlage der Hypothese, dass Viehhalter die Wälder durch Weiden mittels Feuer ersetzt haben. Temperatur und Niederschlag weisen das Untersuchungsgebiet als Waldklima aus. Bodenuntersuchungen und determinierte Holzkohlen (Juniperus 8.155 ± 63 uncal BP, Picea 6.665 ± 59 uncal BP) stützen die Hypothese. Der Indizienbeweis wird für den umweltgeschichtlichen Nachweis als hinreichend angesehen.

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