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Yancheva et al. reply

Author

Listed:
  • Gergana Yancheva

    (GeoForschungsZentrum Potsdam)

  • Norbert R. Nowaczyk

    (GeoForschungsZentrum Potsdam)

  • Jens Mingram

    (GeoForschungsZentrum Potsdam)

  • Peter Dulski

    (GeoForschungsZentrum Potsdam)

  • Georg Schettler

    (GeoForschungsZentrum Potsdam)

  • Jörg F. W. Negendank

    (GeoForschungsZentrum Potsdam)

  • Jiaqi Liu

    († Institute of Geology and Geophysics, Chinese Academy of Sciences, PO Box 9825, Beijing 100029, China)

  • Daniel M. Sigman

    (Princeton University)

  • Larry C. Peterson

    (Rosenstiel School of Marine and Atmospheric Science, University of Miami)

  • Gerald H. Haug

    (Geological Institute)

Abstract

Replying to: H. Zhou et al. Nature 450, doi: 10.1038/nature06408 (2007). Zhou et al. 1 raise the possibility that the titanium (Ti) record at Lake Huguang Maar is controlled by local erosion and runoff to the lake, or through hydrological changes in the lake such as level fluctuations, rather than by changes in the inputs of airborne material2. The authors come to this conclusion by considering the Ti record in isolation. They ignore the redox-sensitive parameters of the S-ratio, total organic-matter content, the Mn/Fe ratio, and magnetic susceptibility records. We believe that their case against our interpretation of the Ti record is weak, and that their interpretation can be ruled out if the other measurements are taken into account2.

Suggested Citation

  • Gergana Yancheva & Norbert R. Nowaczyk & Jens Mingram & Peter Dulski & Georg Schettler & Jörg F. W. Negendank & Jiaqi Liu & Daniel M. Sigman & Larry C. Peterson & Gerald H. Haug, 2007. "Yancheva et al. reply," Nature, Nature, vol. 450(7168), pages 11-11, November.
    • Handle: RePEc:nat:nature:v:450:y:2007:i:7168:d:10.1038_nature06409
    DOI: 10.1038/nature06409
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