Abstract

Pterocarya fraxinifolia, native to the southern Caucasus and adjacent areas, has been widely introduced in Europe. In this study, we investigate the following: (1) How did its current distribution form? (2) What are the past, current, and future suitable habitats of P. fraxinifolia? (3) What is the best conservation approach? Ecological niche modeling was applied to determine its climatic demands and project the distribution of climatically suitable areas during three periods of past, current, and future (2070) time. Then, an integrated analysis of fossil data was performed. Massive expansion of Pterocarya species between the Miocene and Pliocene facilitated the arrival of P. fraxinifolia to the southern Caucasus. The Last Glacial Maximum played a vital role in its current fragmented spatial distribution in the Euxinian and Hyrcanian regions with lower elevations, and Caucasian and Irano-Turanian regions with higher elevations. Climatic limiting factors were very different across these four regions. Future climate change will create conditions for the expansion of this species in Europe. Human activities significantly decreased the suitable area for P. fraxinifolia, especially in the Euxinian, Hyrcanian, and Irano-Turanian regions. Considering genetic diversity, climate vulnerability, and land utilization, the Euxinian, Hyrcanian, and Irano-Turanian regions have been recognized as conservation priority areas for P. fraxinifolia.

Highlights

  • The geographical ranges of species are not static in time, showing expansions and contractions that depend on changes in climate variability and human influence (RocesDiaz et al 2018; Scheffers et al 2016)

  • Our models showed excellent performance with area under the curve (AUC) scores above 0.98, which indicates high reliability of the results

  • Pterocarya fraxinifolia is characteristic of lowlands, riparian, and floodplain forests, mainly occurring between 0 and 400 m in the Euxinian (100%) and Hyrcanian (77.2%) regions, along the shores of the Black Sea and Caspian Sea

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Summary

Introduction

The geographical ranges of species are not static in time, showing expansions and contractions that depend on changes in climate variability and human influence (RocesDiaz et al 2018; Scheffers et al 2016). Relict trees refer to trees that at an earlier time were abundant in a large area but occur only in one or a few small areas (Milne and Abbott 2002). Tree flora experienced a severe Plio-Pleistocene extinction in the European continent at the end of the Neogene due to: (1) the Mediterranean Sea and east–west-oriented mountains preventing southward migration of trees during cold stages (Svenning 2003; Tallis 1991), and (2) a climate shift from warm-temperate to summer-dry in the Mediterranean region from the middle Pliocene (Suc 1984; Svenning 2003)

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