Looy C V, Twitchett R J, Dilcher D L, Van Konijnenburg-Van Cittert J H, Visscher H
Laboratory of Palaeobotany and Palynology, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, The Netherlands.
Proc Natl Acad Sci U S A. 2001 Jul 3;98(14):7879-83. doi: 10.1073/pnas.131218098. Epub 2001 Jun 26.
The fossil record of land plants is an obvious source of information on the dynamics of mass extinctions in the geological past. In conjunction with the end-Permian ecological crisis, approximately 250 million years ago, palynological data from East Greenland reveal some unanticipated patterns. We document the significant time lag between terrestrial ecosystem collapse and selective extinction among characteristic Late Permian plants. Furthermore, ecological crisis resulted in an initial increase in plant diversity, instead of a decrease. Paradoxically, these floral patterns correspond to a "dead zone" in the end-Permian faunal record, characterized by a paucity of marine invertebrate megafossils. The time-delayed, end-Permian plant extinctions resemble modeled "extinction debt" responses of multispecies metapopulations to progressive habitat destruction.
陆地植物的化石记录是了解地质历史时期大规模灭绝动态的一个明显信息来源。大约2.5亿年前,伴随着二叠纪末期的生态危机,来自东格陵兰的孢粉学数据揭示了一些意想不到的模式。我们记录了陆地生态系统崩溃与二叠纪晚期典型植物选择性灭绝之间的显著时间滞后。此外,生态危机导致植物多样性最初增加,而非减少。矛盾的是,这些植物模式对应于二叠纪末期动物化石记录中的一个“死亡带”,其特征是海洋无脊椎动物大型化石稀少。二叠纪末期延迟的植物灭绝类似于多物种集合种群对渐进性栖息地破坏的模拟“灭绝债务”反应。