A high level of atmospheric oxygen, as occurred toward the end of the Cretaceous period, increases leaf diffusion conductance

Autor:	Rachmilevitch, Shimon, Reuveni, Joseph, Pearcy, Robert W., Gale, Joseph
Zdroj:	Journal of Experimental Botany, 1999 Jun 01. 50(335), 869-872.
Databáze:	JSTOR Journals
Externí odkaz:	https://www.jstor.org/stable/23696243 Zobrazit plný text záznamu