Yancheva et al. reply

Gergana Yancheva, Norbert R. Nowaczyk, Jens Mingram, Peter Dulski, Georg Schettler, Jörg F. W. Negendank, Jiaqi Liu, Daniel M. Sigman, Larry C. Peterson and Gerald H. Haug ()
Additional contact information
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

Nature, 2007, vol. 450, issue 7168, E11-E11

Abstract: 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.

Date: 2007
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DOI: 10.1038/nature06409

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