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- W2371566315 abstract "Microfaunas of borehole PRD16 in the Pearl River Delta have been quantitatively analyzed in this paper.A total of 24 benthic foraminifera species referred to 12 genera and 13 ostracod species referred to 9 genera were found in the borehole.They can be divided into 3 ecological groups.The microfaunal analytical results,combined with lithological and sedimentary grain characteristics,suggest that the study area experienced environmental changes since the Late Pleistocene.A riverine environment began to develop before 34 600 cal a BP.Between 34 600 and 23 900 cal a BP,the environment generally changed to an estuarine condition.Between 23 900 and 7 960 cal a BP,the sediments experienced weathering and erosion,characterized by a layer of mottled clay.At around 7 960 cal a BP,sea level rose rapidly and an estuary environment with euryhaline foraminifera and brackish ostracod faunas existed until 2 810 cal a BP.Two second-order sea level fluctuations can be recognized based on the composition and abundance of microfaunas.The maximum water depth occurred at approximately 3 873 cal a BP,demonstrated by the highest abundance of foraminifera and ostracods in the borehole.Since 2 810 cal a BP,the environment gradually changed into a fluvial supratidal zone with increased influence of river processes." @default.
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- W2371566315 date "2013-05-25" @default.
- W2371566315 modified "2023-09-26" @default.
- W2371566315 title "Microfossil Records of Borehole PRD16 and Palaeoenvironment since the Late Pleistocene in the Pearl River Delta" @default.
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