School of Geosciences, University of the Witwatersrand, Johannesburg 2017, South Africa.
Department of Geosciences, Princeton University, Princeton, NJ 08544.
Proc Natl Acad Sci U S A. 2024 Nov 19;121(47):e2322875121. doi: 10.1073/pnas.2322875121. Epub 2024 Nov 4.
Northeast China's Early Cretaceous Yixian Formation preserves spectacular fossils that have proved extraordinarily important in testing evolutionary hypotheses involving the origin of birds and the distribution of feathers among nonavian dinosaurs. These fossils occur either flattened with soft tissue preservation (including feathers and color) in laminated lacustrine strata or as three-dimensional (3D) skeletons in "life-like" postures in more massive deposits. The relationships of these deposits to each other, their absolute ages, and the origin of the extraordinary fossil preservation have been vigorously debated for nearly a half century, with the prevailing view being that preservation was linked to violent volcanic eruptions or lahars, similar to processes that preserved human remains at Pompeii. We present high-precision zircon U-Pb geochronology from cores and outcrops, demonstrating that Yixian Formation accumulation rates are more than an order of magnitude higher than usually estimated. Additionally, we provide zircon provenance and sedimentological data from 3D dinosaur fossils, which imply that their death and burial occurred in collapsed burrows, rather than via a catastrophic volcanogenic mechanism. In the studied area, the three principal fossil-rich intervals of the Yixian occur as a cyclic sequence that correspond to periods of high precipitation. Using Bayesian-Markov Chain Monte Carlo approaches, we constrain the total duration of the sequence to less than ~93,000 y and suggest that climatic precession paced the expression of these cyclic sediments. Rather than representing multiple, Pompeii-like catastrophes, the Yixian Formation is instead a brief snapshot of normal life and death in an Early Cretaceous continental community.
中国东北早白垩世义县组保存了大量壮观的化石,这些化石对于检验鸟类起源和非鸟类恐龙羽毛分布的进化假说非常重要。这些化石要么以压扁的形式保存下来,软组织完整(包括羽毛和颜色),保存在层状湖相地层中,要么以“栩栩如生”的三维(3D)骨架形式保存在更致密的沉积物中。这些沉积物之间的关系、它们的绝对年龄以及非凡化石保存的起源近半个世纪以来一直备受争议,主流观点认为保存与剧烈的火山爆发或火山泥流有关,类似于保存在庞贝古城的人类遗骸的过程。我们提供了来自岩芯和露头的高精度锆石 U-Pb 年代学数据,表明义县组的堆积速率比通常估计的要高出一个数量级以上。此外,我们还提供了来自 3D 恐龙化石的锆石物源和沉积学数据,这表明它们的死亡和埋葬发生在坍塌的洞穴中,而不是通过灾难性的火山成因机制。在所研究的地区,义县组的三个主要富化石层段呈循环序列,与高降水期相对应。使用贝叶斯-马尔可夫链蒙特卡罗方法,我们将序列的总持续时间约束在不到 93000 年以内,并表明气候进动控制了这些循环沉积物的表达。义县组不是多次类似于庞贝城的灾难,而是早白垩世大陆群落中正常生活和死亡的短暂瞬间。