The silicon isotope composition of Ethmodiscus rex laminated diatom mats from the tropical West Pacific: Implications for silicate cycling during the Last Glacial Maximum

Xiong, Z;Li, Tiegang;Algeo, Thomas;Doering, Kristin;Zhai, Bin;et.al.
(2015) Paleooceanography — n° 30, p. 803-823 (2015)

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Authors
  • Xiong, ZKey Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, China
    Author
  • Li, TiegangKey Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, China
    Author
  • Algeo, ThomasUniversity of Cincinnati (USA) - China University of Geosciences, Wuhan, China
    Author
  • Doering, KristinUniversity of Kiel, Germany - Geomar, Germany
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  • Opfergelt, SophieUCLouvain
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  • Zhai, BinInstitute of Marine Geology, Ministry of Land and Resources, Qingdao, China
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Xiong, Z., Li, T., Algeo, T., Doering, K., Frank, M., Brzezinski, M. A., Chang, F., Opfergelt, S., Crosta, X., Jiang, F., Wan, S., & Zhai, B. (2015). The silicon isotope composition of Ethmodiscus rex laminated diatom mats from the tropical West Pacific: Implications for silicate cycling during the Last Glacial Maximum. Paleooceanography, 30, 803-823. https://doi.org/10.1002/2015PA002793 (Original work published 2015)