16 research outputs found

    Predicted Pleistocene-Holocene range shifts of the tiger (Panthera tigris)

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    Aim In this article, we modelled the potential range shifts of tiger (Panthera tigris) populations over the Late Pleistocene and Holocene, to provide new insights into the evolutionary history and interconnectivity between populations of this endangered species. Location Asia. Methods We used an ecological niche approach and applied a maximum entropy (Maxent) framework to model potential distributions of tigers. Bioclimatic conditions for the present day and mid-Holocene, and for the Last Glacial Maximum (LGM), were used to represent interglacial and glacial conditions of the Late Pleistocene, respectively. Results Our results show that the maximum potential tiger range during modern climates (without human impacts) would be continuous from the Indian subcontinent to north-east Siberia. During the LGM, distributions are predicted to have contracted to southern China, India and Southeast Asia and remained largely contiguous. A potential distribution gap between Peninsular Malaya and Sumatra could have effectively separated tigers on the Sunda Islands from those in continental Asia during interglacials. Main conclusions The continuous modelled distribution of tigers in mainland Asia supports the idea of mainly unimpeded gene flow between all populations throughout the Late Pleistocene and Holocene. Thus, our data support a pragmatic approach to tiger conservation management, especially of mainland populations, as it is likely that only recent anthropogenic changes caused separation of these populations. In contrast, Sunda tigers are likely to have separated and differentiated following the Last Glacial Maximum and thus warrant separate management

    A second extinct big cat from the late quaternary of Sri Lanka

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    A second extinct big cat, tentatively considered to be a tiger (Panthera tigris), is recorded from Sri Lanka for the first time from a fossil left lower carnassial found in alluvium near Ratnapura in 1962 and a sub-fossil right middle phalanx 14C dated to ~ 16,500 ybp, discovered in 1982 in a prehistoric midden at Batadomba Cave, near Kuruwita. The species is diagnosed from the only other big cats known from Sri Lanka, Panthera pardus and the extinct P. leo sinhaleyus Deraniyagala, 1938. This record significantly advances the timing of dispersal of tigers into the Indian peninsula. Tigers appear to have arrived in Sri Lanka during a pluvial period during which sea levels were depressed, evidently prior to the last glacial maximum ca. 20,000 years ago. The lion appears to have become extinct in Sri Lanka prior to the arrival of culturally modern humans, ca. 37,000 ybp
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