Magnetic mineral diagenesis in the river-dominated inner shelf of the East China Sea, China

Can Ge, Weiguo Zhang, Chenyin Dong, Yan Dong, Xuexin Bai, Jinyan Liu, Nguyen Thi Thu Hien, Huan Feng, Lizhong Yu

Research output: Contribution to journalArticle

13 Citations (Scopus)

Abstract

The inner shelf of the East China Sea is a river-dominated margin characterized by fine-grained mud deposits and a rapid sedimentation rate. Three short sediment cores (∼2.7 m in length) were examined to characterize spatial variations in magnetic mineral diagenesis. The sediment cores were analyzed for sedimentation rates, magnetic properties, particle size distribution, organic carbon, and total sulfur content. The two more proximal cores with higher sedimentation rates (∼2.2 cm/yr and ∼0.96 cm/yr) do not exhibit obvious effects of reductive dissolution of magnetite with increasing depth, which is consistent with their lower total sulfur content. The offshore core, A12-4, which has a lower sedimentation rate, contains clear evidence of magnetite dissolution and increasing total sulfur content with depth. The three cores have a similar sediment source and organic matter input; therefore, we suggest that a higher sedimentation rate will lead to less reductive diagenesis of magnetite, assuming that other factors are constant. The iron-to sulfate-reduction boundary, i.e., revealed by the onset of a rapid decline of magnetic susceptibility, is located 1.0 m below seafloor in core A12-4. This is much deeper than is reported in many other coastal marine environments and can be explained by the higher sedimentation rate, the presence of refractory terrestrial organic matter, and an abundant input of detrital iron oxides. This study demonstrates that analyses of the magnetic mineral zonation provide a straightforward approach to assess diagenetic organic carbon decomposition pathways in marine environments.

Original languageEnglish
Pages (from-to)4720-4733
Number of pages14
JournalJournal of Geophysical Research: Solid Earth
Volume120
Issue number7
DOIs
StatePublished - 1 Jul 2015

Fingerprint

magnetic mineral
shelves
Sedimentation
sedimentation rate
rivers
diagenesis
Minerals
China
Rivers
minerals
Ferrosoferric Oxide
Sulfur
river
magnetite
marine environments
Sediments
sediments
sulfur
Organic carbon
Biological materials

Keywords

  • East China Sea
  • diagenesis
  • magnetic properties
  • organic matter reactivity
  • river-dominated margin
  • sedimentation rate

Cite this

Ge, Can ; Zhang, Weiguo ; Dong, Chenyin ; Dong, Yan ; Bai, Xuexin ; Liu, Jinyan ; Hien, Nguyen Thi Thu ; Feng, Huan ; Yu, Lizhong. / Magnetic mineral diagenesis in the river-dominated inner shelf of the East China Sea, China. In: Journal of Geophysical Research: Solid Earth. 2015 ; Vol. 120, No. 7. pp. 4720-4733.
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Magnetic mineral diagenesis in the river-dominated inner shelf of the East China Sea, China. / Ge, Can; Zhang, Weiguo; Dong, Chenyin; Dong, Yan; Bai, Xuexin; Liu, Jinyan; Hien, Nguyen Thi Thu; Feng, Huan; Yu, Lizhong.

In: Journal of Geophysical Research: Solid Earth, Vol. 120, No. 7, 01.07.2015, p. 4720-4733.

Research output: Contribution to journalArticle

TY - JOUR

T1 - Magnetic mineral diagenesis in the river-dominated inner shelf of the East China Sea, China

AU - Ge, Can

AU - Zhang, Weiguo

AU - Dong, Chenyin

AU - Dong, Yan

AU - Bai, Xuexin

AU - Liu, Jinyan

AU - Hien, Nguyen Thi Thu

AU - Feng, Huan

AU - Yu, Lizhong

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N2 - The inner shelf of the East China Sea is a river-dominated margin characterized by fine-grained mud deposits and a rapid sedimentation rate. Three short sediment cores (∼2.7 m in length) were examined to characterize spatial variations in magnetic mineral diagenesis. The sediment cores were analyzed for sedimentation rates, magnetic properties, particle size distribution, organic carbon, and total sulfur content. The two more proximal cores with higher sedimentation rates (∼2.2 cm/yr and ∼0.96 cm/yr) do not exhibit obvious effects of reductive dissolution of magnetite with increasing depth, which is consistent with their lower total sulfur content. The offshore core, A12-4, which has a lower sedimentation rate, contains clear evidence of magnetite dissolution and increasing total sulfur content with depth. The three cores have a similar sediment source and organic matter input; therefore, we suggest that a higher sedimentation rate will lead to less reductive diagenesis of magnetite, assuming that other factors are constant. The iron-to sulfate-reduction boundary, i.e., revealed by the onset of a rapid decline of magnetic susceptibility, is located 1.0 m below seafloor in core A12-4. This is much deeper than is reported in many other coastal marine environments and can be explained by the higher sedimentation rate, the presence of refractory terrestrial organic matter, and an abundant input of detrital iron oxides. This study demonstrates that analyses of the magnetic mineral zonation provide a straightforward approach to assess diagenetic organic carbon decomposition pathways in marine environments.

AB - The inner shelf of the East China Sea is a river-dominated margin characterized by fine-grained mud deposits and a rapid sedimentation rate. Three short sediment cores (∼2.7 m in length) were examined to characterize spatial variations in magnetic mineral diagenesis. The sediment cores were analyzed for sedimentation rates, magnetic properties, particle size distribution, organic carbon, and total sulfur content. The two more proximal cores with higher sedimentation rates (∼2.2 cm/yr and ∼0.96 cm/yr) do not exhibit obvious effects of reductive dissolution of magnetite with increasing depth, which is consistent with their lower total sulfur content. The offshore core, A12-4, which has a lower sedimentation rate, contains clear evidence of magnetite dissolution and increasing total sulfur content with depth. The three cores have a similar sediment source and organic matter input; therefore, we suggest that a higher sedimentation rate will lead to less reductive diagenesis of magnetite, assuming that other factors are constant. The iron-to sulfate-reduction boundary, i.e., revealed by the onset of a rapid decline of magnetic susceptibility, is located 1.0 m below seafloor in core A12-4. This is much deeper than is reported in many other coastal marine environments and can be explained by the higher sedimentation rate, the presence of refractory terrestrial organic matter, and an abundant input of detrital iron oxides. This study demonstrates that analyses of the magnetic mineral zonation provide a straightforward approach to assess diagenetic organic carbon decomposition pathways in marine environments.

KW - East China Sea

KW - diagenesis

KW - magnetic properties

KW - organic matter reactivity

KW - river-dominated margin

KW - sedimentation rate

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