Marshall University, Department of Biological Sciences, Huntington, WV 25755, USA; Cincinnati Museum Center, Cincinnati, OH 45203, USA.
Academia Sinica, Biodiversity Research Center, Taipei 11529, Taiwan.
Curr Biol. 2018 Jan 8;28(1):70-76.e4. doi: 10.1016/j.cub.2017.11.021. Epub 2017 Dec 14.
The vertebrate extinction rate over the past century is approximately 22-100 times greater than background extinction rates [1], and large mammals are particularly at risk [2, 3]. Quaternary megafaunal extinctions have been attributed to climate change [4], overexploitation [5], or a combination of the two [6]. Rhinoceroses (Family: Rhinocerotidae) have a rich fossil history replete with iconic examples of climate-induced extinctions [7], but current pressures threaten to eliminate this group entirely. The Sumatran rhinoceros (Dicerorhinus sumatrensis) is among the most imperiled mammals on earth. The 2011 population was estimated at ≤216 wild individuals [8], and currently the species is extirpated, or nearly so, throughout the majority of its former range [8-12]. Understanding demographic history is important in placing current population status into a broader ecological and evolutionary context. Analysis of the Sumatran rhinoceros genome reveals extreme changes in effective population size throughout the Pleistocene. Population expansion during the early to middle Pleistocene was followed by decline. Ecological niche modeling indicated that changing climate most likely played a role in the decline of the Sumatran rhinoceros, as less suitable habitat on an emergent Sundaland corridor isolated Sumatran rhinoceros populations. By the end of the Pleistocene, the Sundaland corridor was submerged, and populations were fragmented and consequently reduced to low Holocene levels from which they would never recover. Past events denuded the Sumatran rhinoceros of genetic diversity through population decline, fragmentation, or some combination of the two and most likely made the species even more susceptible to later exploitation and habitat loss. VIDEO ABSTRACT.
在过去的一个世纪里,脊椎动物的灭绝速度大约是背景灭绝速度的 22-100 倍[1],大型哺乳动物尤其面临风险[2,3]。第四纪巨型动物灭绝归因于气候变化[4]、过度开发[5],或两者的结合[6]。犀牛(Rhinocerotidae 科)有着丰富的化石历史,其中充满了气候引起灭绝的标志性例子[7],但当前的压力有可能使其完全灭绝。苏门答腊犀牛(Dicerorhinus sumatrensis)是地球上最濒危的哺乳动物之一。2011 年的种群估计数为≤216 头野生个体[8],目前该物种在其大部分曾经的分布范围内已经灭绝或几乎灭绝[8-12]。了解种群历史对于将当前的种群状况置于更广泛的生态和进化背景中非常重要。对苏门答腊犀牛基因组的分析揭示了整个更新世有效种群数量的剧烈变化。更新世早期到中期的种群扩张之后是衰退。生态位模型表明,气候变化很可能在苏门答腊犀牛的衰退中发挥了作用,因为新兴的巽他大陆走廊上的适宜栖息地减少,使苏门答腊犀牛的种群隔离。到更新世末期,巽他大陆走廊被淹没,种群被分割,最终减少到低全新世水平,再也无法恢复。过去的事件通过种群衰退、破碎化或两者的结合使苏门答腊犀牛丧失了遗传多样性,这很可能使该物种更容易受到后来的开发和栖息地丧失的影响。视频摘要。