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. 2016 Mar 22;181:931–945. doi: 10.1007/s00442-016-3608-3

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© The Author(s) 2016

Open AccessThis article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.

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Fig. 4 — Water lines (δ²H vs. δ¹⁸O) for AP source water samples (light grey y = 7.3x − 5.4, r ² = 0.99, n = 57, P < 0.0001) and moss water samples (black y = 6.7x − 23.8, r ² = 0.95, P < 0.0001) in which water was distilled from surface moss samples. Long dashed line represents the global meteoric water line (GMWL; y = 8x − 10), dotted line is Vernadsky LMWL. Dashed lines represent 95 % confidence intervals of linear models