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Late Quaternary palaeoenvironmental changes documented by microfaunas and shell stable isotopes in the southern Pearl River Delta plain,South China

引用

Journal of Palaeogeography 2013年第4期2卷 344-361页

作者： Liu Chunlian Franz T. Fürsich Wu Jie Dong Yixin Yang Tingting Yin Jian Department of Earth Sciences Sun Yat-Sen University Geozentrum Nordbayern FG Pal oumwelt der Friedrich-Alexander-Universitt Erlangen Guangdong Provincial Key Laboratory of Mineral Resources and Geological Processes

Ahigh resolution study of sediments,microfaunas(ostracods and foraminifers),and stable isotopes of ostracod shells from core PRD05,sampled from the Da’ao plain of the Pearl River Delta,provides new data about palaeoenvironmental changes during the Late *** basal fluvial gravelly sediments of the core,representing the lowest deposits of the Quaternary at the core site,were possibly formed prior to the transgression associated with the last interglacial *** fluvial setting changed into a marginal marine setting during the last interglacial stage,any record of calcareous fossils were destroyed by subsequent dissolution during the last glacial phase,when the upper part of the deltaic sediments experienced subaerial oxidation,indicated by a mottled clay layer in the *** postglacial sealevel rise in the South China Sea began at16,700 cal yr *** the first phase of sea-level rise(from ~16,700 to 10,100 cal yr B.P.),a swamp environment developed at the core *** ~10,100 cal yr B.P.,marine waters intruded onto the Da’ao plain and reached the core site through the Modaomen *** timing was earlier than in other parts of the Pearl River *** then,a semi-enclosed estuarine environment developed and was maintained until ~5560 cal yr *** this transgressive interval,short-term environmental fluctuations can be recognized based on microfauna and shell geochemical *** ~10,100 to 8630 cal yr B.P.,the sea-level rose,which was followed by a fall from ~8630 to 8520 cal yr *** expanded transgression occurred between ~8520 and 7900 cal yr *** time intervals from ~8520 to 8200 cal yr *** from ~8080 to 7900 cal yr *** marked by peak *** ~7900 to 5560 cal yr B.P.,the core site generally showed a reduced marine influence and enhanced freshwater input.A fluvial environment developed from ~5560 to 3100 cal yr B.P.,and was succeeded by an alluvial plain setting.

关键词： Late Quaternary microfauna shell stable isotopes palaeoenvironment Pearl River Delta

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