4.5 Article

Putative sponge biomarkers in unicellular Rhizaria question an early rise of animals

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NATURE ECOLOGY & EVOLUTION
卷 3, 期 4, 页码 577-581

出版社

NATURE PUBLISHING GROUP
DOI: 10.1038/s41559-019-0806-5

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资金

  1. Max Planck Society
  2. Agouron Institute (Geobiology fellowship)
  3. US National Science Foundation [PLR134161, DBI-1349350]
  4. Swiss National Science Foundation [31003A_179125]
  5. German Research Foundation [NO1090/1-1]
  6. Leibniz Association [SAW-2014-ISAS-2]
  7. Formas, the Swedish Research Council
  8. French National Research Agency [IMPEKAB ANR-15-CE02-001]
  9. Australian Research Council [DP1095247, DP160100607]

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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.

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