Max Planck Institute for Biogeochemistry, Jena, Germany.
MARUM-Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany.
Nat Ecol Evol. 2019 Apr;3(4):577-581. doi: 10.1038/s41559-019-0806-5. Epub 2019 Mar 4.
The dawn of animals remains one of the most mysterious milestones in the evolution of life. The fossil lipids 24-isopropylcholestane and 26-methylstigmastane are considered diagnostic for demosponges-arguably the oldest group of living animals. The widespread occurrence and high relative abundance of these biomarkers in Ediacaran sediments from 635-541 million years (Myr) ago have been viewed as evidence for the rise of animals to ecological importance approximately 100 Myr before their rapid Cambrian radiation. Here we show that the biosynthesis of 24-isopropylcholestane and 26-methylstigmastane precursors is common among early-branching unicellular Rhizaria-heterotrophic protists that play an important role in trophic cycling and carbon export in the modern ocean. Negating these hydrocarbons as sponge biomarkers, our study places the oldest evidence for animals closer to the Cambrian Explosion. Cambrian silica hexactine spicules that are approximately 535 Myr old now represent the oldest diagnostic sponge remains, whereas approximately 558-Myr-old Dickinsonia and Kimberella (Ediacara biota) provide the most reliable evidence for the emergence of animals. The proliferation of predatory protists may have been responsible for much of the ecological changes during the late Neoproterozoic, including the rise of algae, the establishment of complex trophic relationships and the oxygenation of shallow-water habitats required for the subsequent ascent of macroscopic animals.
动物的出现仍然是生命进化中最神秘的里程碑之一。化石脂质 24-异丙基胆甾烷和 26-甲基甾烷被认为是海绵动物的特征标志物——它们可能是现存动物中最古老的群体。这些生物标志物在 6.35 亿至 5.41 亿年前的埃迪卡拉纪沉积物中广泛存在且相对丰度较高,这被认为是动物在寒武纪辐射之前约 1 亿年左右上升到生态重要性的证据。在这里,我们表明,24-异丙基胆甾烷和 26-甲基甾烷前体的生物合成在早期分支的单细胞根足虫中很常见——异养原生动物在现代海洋的营养循环和碳输出中起着重要作用。我们的研究否定了这些碳氢化合物作为海绵生物标志物的地位,将动物最早的证据推得更接近寒武纪大爆发。大约 5.35 亿年前的寒武纪硅质六方角刺现在代表了最古老的海绵诊断遗骸,而大约 5.58 亿年前的狄更逊虫和金伯利虫(埃迪卡拉生物群)为动物的出现提供了最可靠的证据。捕食性原生动物的大量繁殖可能是晚新元古代生态变化的主要原因之一,包括藻类的兴起、复杂营养关系的建立以及浅海栖息地的氧化,这些都是随后宏观动物上升的必要条件。