| Sign In to gain access to subscriptions and/or personal tools. |
Agriculture and environmental change at Qingpu, Yangtze delta region, China: a biomarker, stable isotope and palynological approachSchool of Earth and Geographical Sciences, The University of Western Australia, 35 Stirling Highway, Crawley WA 6009, Australia, patahan{at}student.uwa.edu.au
Stable Isotope and Molecular Biogeochemistry Group, The Institute for Geoscience Research, Department of Applied Chemistry, Curtin University of Technology, Perth WA 6102, Australia
Institute for Environmental Research, Australian Nuclear Science and Technology Organisation, New Illawarra Road, Lucas Heights NSW 2234, Australia
Rice (Oryza sp.) agriculture sustains vast numbers of people and, despite great advancements made in recent years, questions about its origins and spread throughout Asia remain unanswered. This study uses sedimentary biomarker, stable carbon isotope and palynological analyses to investigate early rice agriculture in the Yangtze delta, a region where rice agriculture emerged at least 7000 years ago. Accelerator mass spectrometer (AMS) 14C dating reveals the age of sedimentary section to be between c. 6000 and 1800 cal. BP. Widespread clearing of forest vegetation c. 2400 cal. BP, is the earliest major human influence detected in the Qingpu record. Following this, rice agriculture probably dominated the Qingpu area. Evidence supporting rice agriculture after c. 2400 cal. BP is provided by increased Poaceae and Cereal-type taxa, which occur with high concentrations of plant wax n-alkanes with a dominant C3 plant origin (C27C31 with odd/even preference,
Key Words: Pollen biomarkers stable isotopes Yangtze delta China rice Neolithic agriculture late Holocene.
The Holocene, Vol. 17, No. 4,
507-515 (2007) This article has been cited by other articles:
|
|||||||||||||||
13C 29.8
to 36.3