Centre for Biodiversity and Conservation Science, School of Biological Sciences, The University of Queensland, Brisbane, Queensland 4072, Australia.
CSIRO, Dutton Park, Queensland 4102, Australia.
Nature. 2017 Jul 6;547(7661):49-54. doi: 10.1038/nature22996. Epub 2017 Jun 28.
Antarctic terrestrial biodiversity occurs almost exclusively in ice-free areas that cover less than 1% of the continent. Climate change will alter the extent and configuration of ice-free areas, yet the distribution and severity of these effects remain unclear. Here we quantify the impact of twenty-first century climate change on ice-free areas under two Intergovernmental Panel on Climate Change (IPCC) climate forcing scenarios using temperature-index melt modelling. Under the strongest forcing scenario, ice-free areas could expand by over 17,000 km by the end of the century, close to a 25% increase. Most of this expansion will occur in the Antarctic Peninsula, where a threefold increase in ice-free area could drastically change the availability and connectivity of biodiversity habitat. Isolated ice-free areas will coalesce, and while the effects on biodiversity are uncertain, we hypothesize that they could eventually lead to increasing regional-scale biotic homogenization, the extinction of less-competitive species and the spread of invasive species.
南极陆地生物多样性几乎仅存在于无冰区,而这些无冰区的面积不到南极大陆的 1%。气候变化将改变无冰区的范围和格局,但这些影响的分布和严重程度仍不清楚。在这里,我们使用基于温度指数的融冰模型,根据政府间气候变化专门委员会(IPCC)的两种气候强迫情景,量化了 21 世纪气候变化对无冰区的影响。在最强的强迫情景下,到本世纪末,无冰区的面积可能会增加 17000 多公里,接近 25%的增幅。这种扩张主要发生在南极半岛,那里无冰区的面积可能会增加两倍,从而极大地改变生物多样性栖息地的可利用性和连通性。孤立的无冰区将融合在一起,尽管对生物多样性的影响尚不确定,但我们假设,这最终可能导致区域尺度生物同质化的增加、竞争力较弱的物种灭绝和入侵物种的传播。