JMB_THG_DV_EV_TD_Supplementary_Material

Supplementary Material for the manuscript:<br><b>Messinian vegetation and climate of the intermontane Florina-Ptolemais-Servia Basin, NW Greece inferred from palaeobotanical data: How well do plant fossils reflect past environments?</b><b> </b><b>Supplementary Material Tables S1 </b>- Climatic parameters of NLR. <b> </b><b>Table S1 (1).</b> Fossil species and climatic parameters of the corresponding NLR (depending on the fossil-species and their botanical affinities, climate parameters of species, sections, subgenera, genera, or subfamilies are used as NLR). <b>Table S1 (2).</b> Climatic parameters of NLR. <b>Supplementary Material Tables S2 </b>- Köppen-Geiger climate type signatures.<b></b> <b>Table S2 (1).</b> Scored Köppen-Geiger signatures of all NLR species of the macrofossil and pollen flora of Vegora. <b>Tables S2 (2).</b> Köppen-Geiger signature values and diagram of the macrofossil and pollen flora of Vegora. <br><b>Supplementary Material S3 - </b>Systematic palaeobotany and descriptions of palynomorphs from the plant fossil bearing strata of Vegora (sample S115992).<b></b><b> </b><b>Supplementary Material Tables S4 </b>- Palynomorph abundance of sample S115992.<b></b><b> </b><b>Supplementary Material S5 </b>- Coding of leaf physiognomic characters for morphotypes from the Vegora lignite mine macroflora. Output PDF files from online CLAMP analysis (http://clamp.ibcas.ac.cn).<b> </b>