HOLOCENE FORAMINIFERA FROM THE MUD AREA OF THE INNER SHELF,EAST CHINA SEA AND THEIR PALEOENVIRONMENTAL SIGNIFICANCE

LI Xiaoyan; JIAN Zhimin; SHI Xuefa; LIU Shengfa

doi:10.3724/SP.J.1140.2012.04061

Marine Geology & Quaternary Geology > 2012 > 32(4): 61-71. > DOI: 10.3724/SP.J.1140.2012.04061

LI Xiaoyan, JIAN Zhimin, SHI Xuefa, LIU Shengfa. HOLOCENE FORAMINIFERA FROM THE MUD AREA OF THE INNER SHELF,EAST CHINA SEA AND THEIR PALEOENVIRONMENTAL SIGNIFICANCE[J]. Marine Geology & Quaternary Geology, 2012, 32(4): 61-71. DOI: 10.3724/SP.J.1140.2012.04061

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HOLOCENE FORAMINIFERA FROM THE MUD AREA OF THE INNER SHELF,EAST CHINA SEA AND THEIR PALEOENVIRONMENTAL SIGNIFICANCE

1 Key Lab of Marine Sedimentology and Enviromental Geology, SOA, Qingdao 266061, China;
2 First Institute of Oceanography, SOA, Qingdao 266061, China;
3. Tongji University, Key Lab of Marine Geology, Shanghai 200092, China

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Received Date: July 09, 2012
Revised Date: July 19, 2012

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Abstract

Abstract

The mud area on the inner shelf of the East China Sea is one of the depocenters since the high sea-level of the Holocene. Sedimentary records since the post-glacial saved in this area provide excellent materials for studying paleoceanographic and paleoenvironmental changes during the Holocene. The Core of MZ02 was recovered from the middle of the mud area(121.89°E,28.17°N,water depth 32 m,core length 35.3 m), and radiocarbon dating, grain-size and foraminiferal analyses were performed for paleoceanographic and paleoenvironmental reconstruction. Results show that the environmental evolution in the Holocene can be divided into 4 stages:the stage I was the coastal inner shelf during 10.8~10.5 cal. kaBP; the stage Ⅱ was the period of the rapid sea-level rise from coastal shelf to the middle shelf during 10.5~8.3 cal. kaBP; the stage Ⅲ was the inner-middle shelf with the Taiwan Warm Current close to the studied area during 8.3~5.2 cal. kaBP; and the stage IV was the inner shelf under the action of the enhanced coastal current. The abundance of warm-water species increased markedly at 8.4 cal. kaBP, suggesting the invasion of the Taiwan Warm Current since then. The lower δ¹⁸O in benthic foraminifera and higher abundance of epifaunal species are thought to be closely related to the enhancement of the coastal current since~4.0 cal. kaBP.
- East China Sea,
- paleoceanography and paleoenvironment,
- foraminifera,
- Holocene

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HOLOCENE FORAMINIFERA FROM THE MUD AREA OF THE INNER SHELF,EAST CHINA SEA AND THEIR PALEOENVIRONMENTAL SIGNIFICANCE