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Agriculture and environmental change at Qingpu, Yangtze delta region, China: a biomarker, stable isotope and palynological approach

Pia Atahan

School of Earth and Geographical Sciences, The University of Western Australia, 35 Stirling Highway, Crawley WA 6009, Australia, patahan{at}student.uwa.edu.au

Kliti Grice

Stable Isotope and Molecular Biogeochemistry Group, The Institute for Geoscience Research, Department of Applied Chemistry, Curtin University of Technology, Perth WA 6102, Australia

John Dodson

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 (C27—C31 with odd/even preference, {delta} 13C —29.8{per thousand} to —36.3{per thousand}). Also, high concentrations of a C20 highly branched isoprenoid (HBI) thought to be from epiphytic algae associated with rice agriculture occur after c. 2400 cal. BP. 13C-depleted diploptene (in high concentrations) and 13C-depleted C31 3b-methyl-hopanes of methanotrophic bacterial origin also occur after c. 2400 cal. BP. The strong methane cycle detected in the trench sediment may have provided an alternative CO2 source for plants and algae associated with rice agriculture.

Key Words: Pollen • biomarkers • stable isotopes • Yangtze delta • China • rice • Neolithic • agriculture • late Holocene.

The Holocene, Vol. 17, No. 4, 507-515 (2007)
DOI: 10.1177/0959683607076451


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F. Itzstein-Davey, P. Atahan, J. Dodson, D. Taylor, and Hongbo Zheng
A sediment-based record of Lateglacial and Holocene environmental changes from Guangfulin, Yangtze delta, eastern China
The Holocene, December 1, 2007; 17(8): 1221 - 1231.
[Abstract] [PDF]