OMPARISON OF FORAMINIFERAL TAPHOCOENOSE ASSEMBLAGES SEDIMENTS FROM SOUTHERN BOHAI SEA

LI Rihui; SUN Rongtao; CHEN Xiaohui

doi:10.16562/j.cnki.0256-1492.2017.03.002

Marine Geology & Quaternary Geology > 2017 > 37(3): 17-27. > DOI: 10.16562/j.cnki.0256-1492.2017.03.002

LI Rihui, SUN Rongtao, CHEN Xiaohui. OMPARISON OF FORAMINIFERAL TAPHOCOENOSE ASSEMBLAGES SEDIMENTS FROM SOUTHERN BOHAI SEA[J]. Marine Geology & Quaternary Geology, 2017, 37(3): 17-27. DOI: 10.16562/j.cnki.0256-1492.2017.03.002

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OMPARISON OF FORAMINIFERAL TAPHOCOENOSE ASSEMBLAGES SEDIMENTS FROM SOUTHERN BOHAI SEA

1.
Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071
2.
Key Laboratory of Marine Hydrocarbon Resource and Environmental Geology, Ministry of Land and Resources, China Geological Survey, Qingdao Institute of Marine Geology, Qingdao 266071
3.
School of Resources and Environment Engineering, Shandong University of Technology, Zibo 255049

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Received Date: February 27, 2017
Revised Date: May 06, 2017

Graphical Abstract

Abstract

Abstract

84 surficial sediment samples obtained from the southern Bohai Sea were selected for revealing the distribution pattern of the benthic foraminifera and their relationships with the marine environmental parameters of the sediments. The data suggests that the study area was dominated by the foraminiferal species with high tolerances to low temperature and low salinity. Moreover, 38 species/genera with relatively higher abundances were chosen for Q-mode factor analysis, and then 4 varimax factors corresponding respectively to 4 foraminiferal assemblages were obtained. Comparison between the assemblages and environmental parameters leads to the following conclusions: first, the Protelphidium turberculatum-Buccella frigida assemblage dominates the cold bottom water mass in the central Bohai Sea; second, the Cribrononion subincertum - Buccella frigida assemblage is mainly controlled by both the remanent Yellow Sea warm current and the grain size of bottom sediment; third, the Ammonia becarii var.- Ammonia aomoriensis assemblage was dominated in the coastal water masses with low salinity; and forth, the Elphidium advenum - Textularia foliacea assemblage was mainly constrained by the grain size of sediment. In general, water depth and sea floor topographic fluctuation show little influence on the distribution pattern of foraminifera. Instead, temperature, salinity, and sediment grain size are the main factors which decide the distribution pattern of benthic foraminifera in the study area.
- the Bohai Sea,
- benthic foraminifera,
- marine environment

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References (18)

References

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