Reply to the Comments of Kato and Isozaki on “Evaluation of palaeo-oxygenation of the ocean bottom across the Permian–Triassic boundary” by Y. Kakuwa [Global Planet. Change 63 (2008) 40–56]: Was the Late Permian deep-superocean really oxic?

Kakuwa, Yoshitaka

doi:10.1016/j.gloplacha.2009.08.003

Global and Planetary Change

2009

DOI: 10.1016/j.gloplacha.2009.08.003

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Reply to the Comments of Kato and Isozaki on “Evaluation of palaeo-oxygenation of the ocean bottom across the Permian–Triassic boundary” by Y. Kakuwa [Global Planet. Change 63 (2008) 40–56]: Was the Late Permian deep-superocean really oxic?

Yoshitaka Kakuwa¹

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Reply to the Comments of Kato and Isozaki on “Evaluation of palaeo-oxygenation of the ocean bottom across the Permian–Triassic boundary” by Y. Kakuwa [Global Planet. Change 63 (2008) 40–56]: Was the Late Permian deep-superocean really oxic?

Cited by 1 publication

References 28 publications

An 80 million year oceanic redox history from Permian to Jurassic pelagic sediments of the Mino-Tamba terrane, SW Japan, and the origin of four mass extinctions

An 80 million year oceanic redox history from Permian to Jurassic pelagic sediments of the Mino-Tamba terrane, SW Japan, and the origin of four mass extinctions

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