Geochemical characteristics of hadal sediment in the northern Yap Trench

Yuhuan HUANG; Chengjun SUN; Guipeng YANG; Xin'an YUE; Fenghua JIANG; Wei CAO; Xiaofei YIN; Chaonan GUO; Jiaohong NIU; Haibing DING

doi:10.1007/s00343-019-9010-3

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Geochemical characteristics of hadal sediment in the northern Yap Trench

Special Section on Yap Trench | Updated：2023-05-19

- Geochemical characteristics of hadal sediment in the northern Yap Trench
- Journal of Oceanology and Limnology Vol. 38, Issue 3, Pages: 650-664(2020)
- Affiliations：
  
  1.Key Laboratory of Marine Chemistry Theory and Technology/Ministry of Education, Ocean University of China, Qingdao 266100, China
  2.Key Laboratory of Marine Eco-environmental Science and Technology, Marine Bioresource and Environment Research Center, First Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, China
  3.College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China
  4.Marine Ecology and Environmental Science Laboratory, Pilot National Laboratory for Marine Science and Technology, Qingdao 266237, China
  5.Qingdao Collaborative Innovation Center of Marine Science and Technology, Qingdao 266100, China
  6.South China Sea Environment Monitoring Center, State Oceanic Administration, Guangzhou 510300, China
- Author bio：
  
  DING Haibing, dinghb@ouc.edu.cn
- Funds：
- DOI：10.1007/s00343-019-9010-3
  CLC：
- Received：17 January 2019，
  
  Accepted：25 March 2019，
  
  Online First：03 July 2019，
  
  Published：2020-03
- Accepted：
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Yuhuan HUANG, Chengjun SUN, Guipeng YANG, et al. Geochemical characteristics of hadal sediment in the northern Yap Trench[J]. Journal of Oceanology and Limnology, 2020, 38(3): 650-664.
DOI：

Yuhuan HUANG, Chengjun SUN, Guipeng YANG, et al. Geochemical characteristics of hadal sediment in the northern Yap Trench[J]. Journal of Oceanology and Limnology, 2020, 38(3): 650-664. DOI： 10.1007/s00343-019-9010-3.

摘要

Abstract

Two sediment cores were retrieved in the hadal zone of the Yap Trench

and their concentrations of six major elements Mg

Mn and Fe and nine trace elements Sr

Cu and Zn were determined in inductively coupled plasma atomic emission spectrometry (ICP-AES). According to the vertical distribution profiles of the 15 elements

the correlation of their concentrations

the ratios of Ni/Co

V/Cr

Fe/Al

and Ti/Al

and morphological characteristics of the sediment samples

the implications of the depositional environment and the sediment provenance were analyzed. The results show that the ratio of Ni/Co in all depths of the two sediment cores were below 5

and the ratio of V/Cr were lower than 2

indicating that the depositional environment of the hadal zone in the trench was oxidative and might have inflow of the Antarctic bottom oxygen-rich water. The sediment samples on the eastern side of the trench were siliceous mud mainly composed of diatoms

radiolarian

and sponge needles from surface to deep layer. The vertical profile of the elements

the concentration of TOC and the fossil record indicated that the sediment sample from station Dive113 was well mixed from surface to bottom layer. Based on the correlation of concentrations of the elements

the morphological characteristics of the sediment

and the ratios of Fe/Al and Ti/Al

we inferred that the sediment in the hadal zone of the trench had terrestrial

volcanic

biological

and authigenic sources. Major source of the sediment in the eastern side of the trench were terrestrial; whereas the sediment in the western side of the trench received more volcaniclastic input.

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Keywords

references

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