Paläontologisches Institut und Museum, Universität Zürich, Zürich, Switzerland.
West Jordan, Utah, United States of America; New Mexico Museum of Natural History and Science, Albuquerque, New Mexico, United States of America.
PLoS One. 2014 Mar 19;9(3):e88987. doi: 10.1371/journal.pone.0088987. eCollection 2014.
Examining the geological past of our planet allows us to study periods of severe climatic and biological crises and recoveries, biotic and abiotic ecosystem fluctuations, and faunal and floral turnovers through time. Furthermore, the recovery dynamics of large predators provide a key for evaluation of the pattern and tempo of ecosystem recovery because predators are interpreted to react most sensitively to environmental turbulences. The end-Permian mass extinction was the most severe crisis experienced by life on Earth, and the common paradigm persists that the biotic recovery from the extinction event was unusually slow and occurred in a step-wise manner, lasting up to eight to nine million years well into the early Middle Triassic (Anisian) in the oceans, and even longer in the terrestrial realm. Here we survey the global distribution and size spectra of Early Triassic and Anisian marine predatory vertebrates (fishes, amphibians and reptiles) to elucidate the height of trophic pyramids in the aftermath of the end-Permian event. The survey of body size was done by compiling maximum standard lengths for the bony fishes and some cartilaginous fishes, and total size (estimates) for the tetrapods. The distribution and size spectra of the latter are difficult to assess because of preservation artifacts and are thus mostly discussed qualitatively. The data nevertheless demonstrate that no significant size increase of predators is observable from the Early Triassic to the Anisian, as would be expected from the prolonged and stepwise trophic recovery model. The data further indicate that marine ecosystems characterized by multiple trophic levels existed from the earliest Early Triassic onwards. However, a major change in the taxonomic composition of predatory guilds occurred less than two million years after the end-Permian extinction event, in which a transition from fish/amphibian to fish/reptile-dominated higher trophic levels within ecosystems became apparent.
研究我们星球的地质过去,可以让我们研究严重的气候和生物危机时期以及复苏、生物和非生物生态系统波动,以及随时间推移的动物群和植物群更替。此外,大型捕食者的恢复动态为评估生态系统恢复的模式和速度提供了关键,因为捕食者被认为对环境动荡最敏感。二叠纪末期大灭绝是地球上生命经历的最严重危机,普遍存在的观点认为,生物从灭绝事件中的恢复异常缓慢,并以逐步的方式发生,在海洋中持续了长达 800 到 900 万年,进入早三叠世(安尼期)后甚至更长时间。在这里,我们调查了早三叠世和安尼期海洋掠食性脊椎动物(鱼类、两栖动物和爬行动物)的全球分布和体型谱,以阐明在二叠纪末期事件之后的营养金字塔的高度。通过编译硬骨鱼和一些软骨鱼的最大标准长度,以及四足动物的总尺寸(估计值),对体型进行了调查。由于保存假象,后者的分布和体型谱难以评估,因此主要以定性方式讨论。然而,这些数据表明,从早三叠世到安尼期,捕食者的体型没有明显增加,这与长期且逐步的营养恢复模型预期的情况不符。这些数据进一步表明,从最早的早三叠世开始,就存在具有多个营养层次的海洋生态系统。然而,在二叠纪末期灭绝事件后不到 200 万年,捕食者的分类组成发生了重大变化,生态系统内从鱼类/两栖动物到鱼类/爬行动物为主的较高营养层次的转变变得明显。