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. 2017 May 10;68(11):2871–2883. doi: 10.1093/jxb/erx148

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© The Author 2017. Published by Oxford University Press on behalf of the Society for Experimental Biology.

This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted reuse, distribution, and reproduction in any medium, provided the original work is properly cited.

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Fig. 5. — The relationship of (A) the total leaf conductance (g_tot), (B) the leaf mesophyll conductance (g_m), and (C) the chloroplast CO₂ concentration (C_c) to the net photosynthetic CO₂ assimilation rate (A_N) of D. antarctica (open circles) and C. quitensis (filled circles) in King George (KGI) and Lagotellerie Island (LAG). Goodness of fit with a saturation model is shown for both species and considering all populations and measurement temperatures together. Values are means ± SE (n=5–7).