| Citation: |
Zhi-wen Shang, Jian-fen Li, Holger Freund, Pei-xin Shi, Hong Wang, 2023. Quantitative relationship between surface sedimentary diatoms and water depth in North-Central Bohai Bay, China, China Geology, 6, 61-69. doi: 10.31035/cg2022040
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Quantitative relationship between surface sedimentary diatoms and water depth in North-Central Bohai Bay, China
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Abstract
To study the quantitative relationship between surface sedimentary diatoms and water depth, 67 surface samples were collected for diatom analysis on eight profiles with water depth variation from the muddy intertidal zone to the shallow sea area in North-Central Bohai Bay, China. The results showed that the distribution of diatoms changed significantly in response to the change in water depth. Furthermore, the quantitative relationship between the distribution of dominant diatom species, their assemblages, and the water depth was established. The water depth optima for seven dominant species such as Cyclotella striata/stylorum, Paralia sulcata, and Coscinodiscus perforatus and the water depth indication range of seven diatom assemblages were obtained in the study area above the water depth (elevation) of −10 m. The quantitative relationship between surface sedimentary diatoms and water depth provides a proxy index for diatom-paleo-water depth reconstruction in the strata in Bohai Bay, China.
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References
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Zhi-wen Shang, Jian-fen Li, Holger Freund, Pei-xin Shi, Hong Wang, 2023. Quantitative relationship between surface sedimentary diatoms and water depth in North-Central Bohai Bay, China, China Geology, 6, 61-69. doi: 10.31035/cg2022040
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Figure 1.
Map showing the Bohai Sea, China. a-Regional background and the location of the study area (marked with a red square); b-map showing the study area, Bohai Bay. R.−River.
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Figure 2.
Location map of the surficial sampling stations for diatom analysis in the North-Central Bohai Bay. The bottom water depth contours were drawn based on the measured data from 2006 to 2008. R.−River.
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Figure 3.
Vertical distribution characteristics of the dominant non-planktonic diatom species response to the change of water depth of the surficial sediments in the muddy intertidal zone and the contiguous shallow sea area in the North-Central Bohai Bay, China.
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Figure 4.
Vertical cluster characteristics of the surface sedimentary diatom assemblages’ response to the water depth change in the muddy intertidal zone and the contiguous shallow sea in North-Central Bohai Bay, China.
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Figure 5.
Vertical zonations of the surface sedimentary diatom species, assemblages, and their relationships with water depth in the muddy intertidal zone and the contiguous shallow sea in the North-Central Bohai Bay, China.