Redox conditions of shallow seawater across the Ediacaran-Cambrian transition: Insights from trace elements, REE, and eustatic changes-Reference-Cited by-同舟云学术

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Redox conditions of shallow seawater across the Ediacaran-Cambrian transition: Insights from trace elements, REE, and eustatic changes

Published:2020 Issue:6 Volume:54 Page:365-379
ISSN:0016-7002
Container-title:GEOCHEMICAL JOURNAL
language:en
Short-container-title:Geochem. J.

Author:

Yang Yang¹²,Wen Hanjie¹²,Liu Jie³,Jeffrey de Fourestier⁴

Affiliation:

1. State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences

2. University of Chinese Academy of Sciences

3. Shaanxi Earthquake Agency

4. State Key Laboratory of Nuclear Resources and Environment (East China University of Technology)

Publisher

Geochemical Society of Japan

Subject

Geochemistry and Petrology,Geophysics

Link

https://www.jstage.jst.go.jp/article/geochemj/54/6/54_2.0607/_pdf

Reference62 articles.

1. Algeo, T. J. and Tribovillard, N. (2009) Environmental analysis of paleoceanographic systems based on molybdenum-uranium covariation. Chem. Geol. 268, 211−225.

2. Amthor, J. E., Grotzinger, J. P., Schroder, S., Bowring, S. A., Ramezani, J., Martin, M. W. and Matter, A. (2003) Extinction of Cloudina and Namacalathus at the Precambrian-Cambrian boundary in Oman. Geology 31, 431−434.

3. Bau, M. and Dulski, P. (1999) Comparing yttrium and rare earths in hydrothermal fluids from the Mid-Atlantic Ridge: implications for Y and REE behavior during nearvent mixing and for the Y/Ho ratio of Proterozoic seawater. Chem. Geol. 155, 77−90.

4. Bau, M., Koschinsky, A., Dulski, P. and Hein, J. R. (1996) Comparison of the partitioning behaviours of yttrium, rare earth elements, and titanium between hydrogenetic marine ferromanganese crusts and seawater. Geochim. Cosmochim. Acta 60(10), 1709−1725.

5. Bau, M., Möller, P. and Dulski, P. (1997) Yttrium and lanthanides in eastern Mediterranean seawater and their fractionation during redox-cycling. Mar. Chem. 56(1−2), 123−131.

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