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This page is a summary of: Comment on “Early Aptian paleoenvironmental evolution of the Bab Basin at the southern Neo-Tethys margin: Response to global carbon-cycle perturbations across Ocean Anoxic Event 1a” by K. Yamamoto et al., Geochemistry Geophysics Geosystems, May 2014, American Geophysical Union (AGU),
DOI: 10.1002/2014gc005350.
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