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Results: 2
The high oxygen atmosphere toward the end-Cretaceous; a possible contributing factor to the K/T boundary extinctions and to the emergence of C-4 species
Authors: Gale, J Rachmilevitch, S Reuveni, J Volokita, M
Citation: J. Gale et al., The high oxygen atmosphere toward the end-Cretaceous; a possible contributing factor to the K/T boundary extinctions and to the emergence of C-4 species, J EXP BOT, 52(357), 2001, pp. 801-809
A high level of atmospheric oxygen, as occurred toward the end of the Cretaceous period, increases leaf diffusion conductance
Authors: Rachmilevitch, S Reuveni, J Pearcy, RW Gale, J
Citation: S. Rachmilevitch et al., A high level of atmospheric oxygen, as occurred toward the end of the Cretaceous period, increases leaf diffusion conductance, J EXP BOT, 50(335), 1999, pp. 869-872
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