Climate sensitivity of Cryptomeria japonica in two contrasting environments: Perspectives from QTL mapping

S4 Fig. Frequency of dry days in March of the year of tree-ring formation at (A) the Chiba site and (B) the Kumamoto site. (PDF) S5 Fig. Growth response to temperature (right panels) and precipitation (left panels) at the Kumamoto site (upper panels) and the Chiba site (lower panels). Positive and negative correlations are shown with open and closed bars, respectively. Month notation is the same as in Fig 1. (PDF) S6 Fig. Prediction accuracy of the 13 identified QTLs. (PDF) S7 Fig. Results of the QTL analysis using composite interval mapping. The horizontal dashed lines represent the logarithm of odds (LOD) scores of two and three. (PDF) S1 Table. Tree ring width of the mapping populations at the two sites. (CSV) S2 Table. Marker genotypes and positions. (CSV) Acknowledgments We thank Drs. H. Iwata and S. Goto for their helpful advice during this study. Author Contributions Conceptualization: Hideki Mori. Data curation: Hideki Mori. Formal analysis: Hideki Mori. Funding acquisition: Asako Matsumoto. Investigation: Hideki Mori. Methodology: Hideki Mori, Kana Yamashita. Project administration: Hideki Mori. Resources: Kana Yamashita, Asako Matsumoto. Supervision: Tokuko Ujino-Ihara. Visualization: Hideki Mori. Writing – original draft: Hideki Mori, Shin-Taro Saiki. Writing – review & editing: Hideki Mori, Kana Yamashita, Shin-Taro Saiki, Asako Matsu- moto, Tokuko Ujino-Ihara. References 1. IPCC. Climate change 2013: The physical science basis. Contribution of working group i to the fifth

assessment report of the intergovernmental panel on climate change. Cambridge, United Kingdom; New York, NY, USA: Cambridge University Press; 2013. Climate sensitivity of Cryptomeria japonica PLOS ONE | https://doi.org/10.1371/journal.pone.0228278 January 28, 2020 11 / 14