Roopnarine Peter D, Angielczyk Kenneth D, Wang Steve C, Hertog Rachel
Department of Invertebrate Zoology and Geology, California Academy of Sciences, 875 Howard Street, San Francisco, CA 94103, USA.
Proc Biol Sci. 2007 Sep 7;274(1622):2077-86. doi: 10.1098/rspb.2007.0515.
Studies of the end-Permian mass extinction have emphasized potential abiotic causes and their direct biotic effects. Less attention has been devoted to secondary extinctions resulting from ecological crises and the effect of community structure on such extinctions. Here we use a trophic network model that combines topological and dynamic approaches to simulate disruptions of primary productivity in palaeocommunities. We apply the model to Permian and Triassic communities of the Karoo Basin, South Africa, and show that while Permian communities bear no evidence of being especially susceptible to extinction, Early Triassic communities appear to have been inherently less stable. Much of the instability results from the faster post-extinction diversification of amphibian guilds relative to amniotes. The resulting communities differed fundamentally in structure from their Permian predecessors. Additionally, our results imply that changing community structures over time may explain long-term trends like declining rates of Phanerozoic background extinction.
二叠纪末大灭绝的研究主要聚焦于潜在的非生物成因及其直接的生物效应。对于生态危机导致的次生灭绝以及群落结构对此类灭绝的影响,关注较少。在此,我们使用一个结合了拓扑学和动力学方法的营养网络模型,来模拟古群落初级生产力的中断。我们将该模型应用于南非卡鲁盆地的二叠纪和三叠纪群落,结果表明,虽然没有证据表明二叠纪群落特别容易灭绝,但早三叠世群落似乎本质上就不太稳定。这种不稳定性很大程度上源于两栖类群落相对于羊膜动物在灭绝后更快的多样化。由此产生的群落结构与二叠纪的前身有根本差异。此外,我们的研究结果表明,群落结构随时间的变化可能解释了诸如显生宙背景灭绝速率下降等长期趋势。