Vanderbilt University, Nashville, TN 37235-1805, USA.
Oxford University Museum of Natural History, Oxford OX1 3PW, UK.
Sci Adv. 2019 Jun 19;5(6):eaaw0260. doi: 10.1126/sciadv.aaw0260. eCollection 2019 Jun.
Reconstructing Precambrian eukaryotic paleoecology is pivotal to understanding the origins of the modern, animal-dominated biosphere. Here, we combine new fossil data from southern Namibia with computational fluid dynamics (CFD) to test between competing feeding models for the Ediacaran taxon . In addition, we perform simulations for multiple individuals, allowing us to analyze hydrodynamics of living communities. We show that lived gregariously, forming shallow marine aggregations in the latest Ediacaran, 548 to 541 million years (Ma) ago. We demonstrate enhanced vertical mixing of the water column above aggregations and preferential redirection of current into body cavities of downstream individuals. These results support the reconstruction of as a macroscopic suspension feeder and also provide a convincing paleoecological advantage to feeding in aggregations analogous to those recognized in many extant marine metazoans. These results provide some of the oldest evidence of commensal facilitation by macroscopic eukaryotes yet recognized in the fossil record.
重建前寒武纪真核生物古生态学对于理解现代以动物为主导的生物圈的起源至关重要。在这里,我们结合纳米比亚南部的新化石数据和计算流体动力学 (CFD),对埃迪卡拉纪分类单元的竞争觅食模型进行了测试。此外,我们还对多个个体进行了模拟,从而能够分析活群落的水动力。我们表明, 群居生活,在 5.48 亿至 5.41 亿年前的最新埃迪卡拉纪时期,形成了浅海聚集。我们证明了聚集上方水柱的垂直混合增强,并且水流更倾向于流入下游个体的体腔。这些结果支持将 重建为宏观悬浮食者,并且还为在类似于许多现存海洋后生动物中所识别的聚集中觅食提供了令人信服的古生态优势。这些结果提供了在化石记录中最早的由宏观真核生物共生促进的证据之一。