Abstract

AimWe use ecological niche models and environmental stratification of palaeoclimate to reconstruct the changing range of the lion (Panthera leo) during the late Pleistocene and Holocene.LocationThe modern (early 21st century) range of the lion extends from southern Africa to the western Indian Subcontinent, yet through the 20th century this range has been drastically reduced in extent and become increasingly fragmented as a result of human impacts.MethodsWe use Global Environmental Stratification with MaxEnt ecological niche models to map environmental suitability of the lion under current and palaeoclimatic scenarios. By examining modelled lion range in terms of categorical environmental strata, we characterise suitable bioclimatic conditions for the lion in a descriptive manner.ResultsWe find that lion habitat suitability has reduced throughout the Holocene, controlled by pluvial/interpluvial cycles. The aridification of the Sahara 6ka dramatically reduced lion range throughout North Africa. The association of Saharan aridification with the development of pastoralism and the growth of sedentary communities, who practised animal husbandry, would have placed additional and lasting anthropogenic pressures on the lion.Main ConclusionsThis research highlights the need to integrate the full effects of the fluctuating vegetation and desiccation of the Sahara into palaeoclimatic models, and provides a starting point for further continental-scale analyses of shifting faunal ranges through North Africa and the Near East during the Holocene. This scale of ecological niche modelling does not explain the current pattern of genetic variation in the lion, and we conclude that narrow but substantial physical barriers, such as rivers, have likely played a major role in population vicariance throughout the Late Pleistocene.

Highlights

  • The overall aim of this paper is to model the range changes of the lion (Panthera leo) driven by large-scale climate changes since the Last Glacial Maximum, and evaluate their likely consequences on population distribution and connectivity

  • The known historical range of the lion included much of Africa and southeastern Europe; it extended to the Near East, the Arabian Peninsula, and southwest Asia as far as the Indian Subcontinent (Ray, Hunter & Zigouris, 2005; Schnitzler & Hermann, 2019; Yamaguchi et al, 2004), but today this range is considerably reduced

  • Whilst certain environmental zones are more favoured by lions, no zone is modelled as universally suitable for the lion, as both favoured and highly favoured strata are found within environmental zones that include unsuitable and low-use strata

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Summary

Introduction

The overall aim of this paper is to model the range changes of the lion (Panthera leo) driven by large-scale climate changes since the Last Glacial Maximum, and evaluate their likely consequences on population distribution and connectivity. This is essential contextualisation for current and continuing anthropogenic impacts on the species. Key threats to the lion in both modern and historic times are habitat reduction, depletion of the wild prey base and direct persecution, which are frequently associated with livestock husbandry and management (Bauer, De Iongh & Sogbohossou, 2010; Black et al, 2013; Inskip & Zimmermann, 2009). The population and range contraction of the lion is even more pronounced, if the closely related taxa, P. (l.) spelaeus (Eurasian cave lion) and P. (l.) atrox, (American lion) are included and longer periods of time are considered

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