Department of Biological Sciences, Florida Institute of Technology, Melbourne, Florida 32901, USA.
Ecology. 2012 Aug;93(8):1853-66. doi: 10.1890/11-1545.1.
A high-resolution (2-9 year sampling interval) fossil pollen record from the Galápagos Islands, which spans the last 2690 years, reveals considerable ecosystem stability. Vegetation changes associated with independently derived histories of El Niño Southern Oscillation variability provided evidence of shifts in the relative abundance of individual species rather than immigration or extinction. Droughts associated with the Medieval Climate Anomaly induced rapid ecological change that was followed by a reversion to the previous state. The paleoecological data suggested nonneutral responses to climatic forcing in this ecosystem prior to the period of human influence. Human impacts on the islands are evident in the record. A marked decline in long-term codominants of the pollen record, Alternanthera and Acalypha, produced a flora without modern analogue before 1930. Intensified animal husbandry after ca. 1930 may have induced the local extinction of Acalypha and Alternanthera. Reductions in populations of grazing animals in the 1970s and 1980s did not result in the return of the native flora, but in invasions by exotic species. After ca. 1970 the trajectory of habitat change accelerated, continuously moving the ecosystem away from the observed range of variability in the previous 2690 years toward a novel ecosystem. The last 40 years of the record also suggest unprecedented transport of lowland pollen to the uplands, consistent with intensified convection and warmer wet seasons.
来自加拉帕戈斯群岛的高分辨率(2-9 年采样间隔)化石花粉记录,跨越了过去的 2690 年,揭示了相当大的生态系统稳定性。与厄尔尼诺南方涛动变化的独立衍生历史相关的植被变化提供了证据,表明个别物种的相对丰度发生了变化,而不是移民或灭绝。与中世纪气候异常相关的干旱导致了快速的生态变化,随后又恢复到以前的状态。古生态学数据表明,在人类影响时期之前,该生态系统对气候强迫的反应是非中性的。人类对岛屿的影响在记录中很明显。长期花粉记录中的共同优势种Alternanthera 和 Acalypha 的显著减少,导致在 1930 年之前形成了没有现代类似物的植物群。大约 1930 年后,畜牧业的加强可能导致了 Acalypha 和 Alternanthera 的局部灭绝。20 世纪 70 年代和 80 年代食草动物数量的减少并没有导致本地植物群的回归,而是导致了外来物种的入侵。大约 1970 年后,栖息地变化的轨迹加速,生态系统不断远离过去 2690 年观察到的可变性范围,向新的生态系统发展。记录的最后 40 年也表明,低地花粉以前所未有的方式被输送到高地,这与对流的加强和更温暖的湿润季节一致。