Trace metal elements as paleoenvironmental proxies: Why should we account for sedimentation rate variations?

Vincent Crombez, Sébastien Rohais, Tristan Euzen, Laurent Riquier, François Baudin, Eider Hernandez-Bilbao

DOI: 10.1130/g47150.1
Published: 2020-05-29
Container: Geology
Publisher: Not recorded
Open access: yes

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Cite this work

BibTeX

@article{allodium:10.1130/g47150.1,
  title = {Trace metal elements as paleoenvironmental proxies: Why should we account for sedimentation rate variations?},
  author = {Vincent Crombez and Sébastien Rohais and Tristan Euzen and Laurent Riquier and François Baudin and Eider Hernandez-Bilbao},
  year = {2020},
  journal = {Geology},
  doi = {10.1130/g47150.1},
  url = {https://doi.org/10.1130/g47150.1}
}

RIS

TY  - JOUR
TI  - Trace metal elements as paleoenvironmental proxies: Why should we account for sedimentation rate variations?
AU  - Vincent Crombez
AU  - Sébastien Rohais
AU  - Tristan Euzen
AU  - Laurent Riquier
AU  - François Baudin
AU  - Eider Hernandez-Bilbao
PY  - 2020
JO  - Geology
DO  - 10.1130/g47150.1
UR  - https://doi.org/10.1130/g47150.1
ER  -

APA

Crombez, V., Rohais, S., Euzen, T., Riquier, L., Baudin, F., & Hernandez-Bilbao, E. (2020). Trace metal elements as paleoenvironmental proxies: Why should we account for sedimentation rate variations?. Geology. https://doi.org/10.1130/g47150.1

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hal · retrieved 2026-09-25T09:19:53.711Z