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CHEN Huixian, WANG Jianhua, DONG Weichen, HUANG Kangyou, ZHANG Kai, CHEN Zihao. Late Holocene foraminiferal record from mangrove reserve, Qi’ao Island, Pearl River Estuary and its implications for paleoenvironment[J]. Marine Geology & Quaternary Geology, 2020, 40(3): 74-86. doi: 10.16562/j.cnki.0256-1492.2019031502
Citation: CHEN Huixian, WANG Jianhua, DONG Weichen, HUANG Kangyou, ZHANG Kai, CHEN Zihao. Late Holocene foraminiferal record from mangrove reserve, Qi’ao Island, Pearl River Estuary and its implications for paleoenvironment[J]. Marine Geology & Quaternary Geology, 2020, 40(3): 74-86. doi: 10.16562/j.cnki.0256-1492.2019031502
shu

Late Holocene foraminiferal record from mangrove reserve, Qi’ao Island, Pearl River Estuary and its implications for paleoenvironment

  • 1.

    School of Earth Science and Engineering, Sun Yat-sun University, Guangzhou 510275, China

  • 2.

    South Marine Science and Engineering Laboratory, Zhuhai 519000, China

More Information
Received Date:  15 March 2019
Revised Date:  13 March 2020
Publish Date:  25 June 2020
    Abstract

  • Intertidal foraminifera has been widely used in paleoenvironmental reconstruction, and especially, in researches on high-resolution relative sea-level fluctuation. Unfortunately, such researches are lacking in the South China coast. This time, a long core up to 300 cm in length was retrieved from the upper intertidal zone of the mangrove on the Qi’ao Island of the Pearl River estuary. AMS14C dating, foraminifera, grain size distribution and grayscale analysis were employed to ascertain the possibility to apply the mangrove foraminifera as a high-resolution proxy for sea level fluctuation and paleoenvironmental evolution. Two foraminiferal assemblages were acquired from the core QA, a calcareous group dominated by Ammonia becсarii (78.7%), with common species Proelphidium granosum (6.6%) and Elphidiella kiangsuensis (5.6%), from a clayey slit sediment, indicating an estuarine subtidal environment; and an agglutinated assemblage dominated by Arenoparella mexicana (50.6%) with common species Miliammina fusca (17.5%), Trochammia sp. (6.8%), from a layer of sandy silt deposits with abundant plants debris and residues, indicating an upper or middle mangrove intertidal environment. AMS14C dates suggest that, the sediments formed approximately 4 200 cal. aBP, when the study area was a subtidal or mudflats environments. It turned to a middle-high mangrove at ～2 400 cal. aBP, resulted from the falling of relative sea-level caused by deltaic progradation. Two fine grained layers were intercalated in mangrove sediments, which contain calcareous foraminiferal tests corresponding to 1 022 ～ 729 cal. aBP and 508 ～ 358 cal. aBP respectively, probably related to a sub-regional sea-level rise. The grayscale suggests three phases of high humification, corresponding to ～3 000～2 700 cal. aBP, 1 200～1 100 cal. aBP, 600～500 cal. aBP respectively, indicating a warm and humid climate, which are close to the sea-level rise periods.

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