

FOLLOWUS
1.College of Chemistry and Molecular Engineering, College of Marine Science and Biological Engineering, Qingdao University of Science and Technology, Qingdao 266042, China
2.Public Technology Service Center, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
3.Key Laboratory of Marine Ecology & Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
4.Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China
5.Qingdao National Laboratory for Marine Science and Technology, Qingdao 266061, China
6.Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
jmsong@qdio.ac.cn
yuanyuan.xiao@qdio.ac.cn
Received:13 January 2022,
Accepted:17 May 2022,
Online First:26 June 2022,
Published:01 September 2023
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SUN Ziwei,LIU Jin,ZHANG Yue,et al.Compositional characteristics of sediment from Jiaozhou Bay in North China and the implication to the provenance[J].Journal of Oceanology and Limnology,2023,41(05):1729-1741.
Rare earth elements (REEs) can be used to trace source materials and identify their provenances
because of significant conservation and immobility during chemical alteration processes after erosion of materials from the provenance. This study focused on the temporal variation of REEs for columnar sediments from the mouth of Jiaozhou Bay in North China to understand the potential controls for the geochemical variations of sediments. Through extraction experiments
we identified that the residual fraction is the main host for REEs compared with other fractions (i.e.
exchangeable and carbonate fraction
easily reducible oxides fraction
reducible oxides fraction
magnetite fraction). REE ratios (e.g.
La
N
/Sm
N
and La
N
/Yb
N
; N: normalized by chondrite) lack correlations with grain size or the chemical index of alteration (CIA)
which is correlated with major elements. All these indicate that these REE variations reflect the varying contribution of source materials from different provenances instead of grain size or chemical weathering effects. REE ratios (e.g.
La
N
/Sm
N
and La
N
/Yb
N
) remain relatively constant until the depth of roughly 40 cm (equivalent to the year 1995)
and show obvious changes beyond this depth. Compared REE characteristics of Jiaozhou Bay with those of neighboring rivers and bedrocks
the relative contributions of Dagu River-Jiaolai River
and Licun River may have been increased during the sedimentary processes
which could be caus
ed by the construction of reservoir and related change of aquaculture (e.g.
rapid accumulation of organic materials).
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