Holocene microfaunal records in the central Pearl River Delta and implications for palaeoenvironmental changes

WU Yueqin; LIU Chunlian; YANG Xiaoqiang; HANG Yi; YIN Jian; ZHANG Kai

doi:10.16562/j.cnki.0256-1492.2018042801

Marine Geology & Quaternary Geology > 2019 > 39(2): 31-43. > DOI: 10.16562/j.cnki.0256-1492.2018042801

WU Yueqin, LIU Chunlian, YANG Xiaoqiang, HANG Yi, YIN Jian, ZHANG Kai. Holocene microfaunal records in the central Pearl River Delta and implications for palaeoenvironmental changes[J]. Marine Geology & Quaternary Geology, 2019, 39(2): 31-43. DOI: 10.16562/j.cnki.0256-1492.2018042801

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Holocene microfaunal records in the central Pearl River Delta and implications for palaeoenvironmental changes

1.
School of Earth Sciences and Engineering, Sun Yat-sen University, Guangdong Provincial Key Laboratory of Geological Processes and Mineral Resource Exploration, Guangzhou 510275, China
2.
Guangdong Provincial Key Laboratory of Mineral Resources and Geological Processes, Guangzhou 510275, China
3.
South China Sea Institute of Planning and Environmental Research, SOA, Guangzhou 510300, China
4.
Key Laboratory of Marine Mineral Resources, Ministry of Natural Resources, Guangzhou 510075, China

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Received Date: April 27, 2018
Revised Date: July 09, 2018

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Abstract

Abstract

Holocene palaeoenvironmental reconstruction was carried out with the data of microfauna (foraminifers and ostracods), AMS¹⁴C dating, sediment grain size distribution, and molluscs, from a borehole drilled in the central Pearl River Delta. During the last glacial maximum, the whole Pearl River mouth was exposed and suffered subaerial weathering, suggested by a layer of extensively distributed mottled clay. A rapid relative sea level rising occurred with the warming of climate during Early Holocene. The marine water intruded into the deltaic area, firstly from the eight south entrances. At about 9010 cal.aBP, marine waters arrived at the central part of the deltaic area. Since then, the study area has become an estuarine environment under water until ~4510 cal.aBP. During the transgression, there were two short-terms of environmental fluctuations recorded by microfauna. The peak of transgression occurred in the time interval from ~7000 to 5630 cal.aBP marked by the highest microfaunal abundance. Since 4510 cal.aBP, however, marine influence weakened and an alluvial plain developed in the central Pearl River Delta area.
- foraminifers,
- ostracods,
- Holocene,
- palaeoenvironmentthe,
- Pearl River Delta

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References (68)

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Holocene microfaunal records in the central Pearl River Delta and implications for palaeoenvironmental changes