2016 in paleontology



Cnidarians

Research

Yunnanoascus haikouensis, previously thought to be a member of Ctenophora, is reinterpreted as a crown-group medusozoan by Han et al..

Molluscs

Amphibians

Research

Synapsids

Non-mammalian synapsids

Research

Other animals

Research

Other organisms

Research

  • Probable stromatolites are described from the 3,700-Myr-old rocks from the Isua supracrustal belt by Nutman et al. ; however, Allwood et al. subsequently argue that these putative stromatolites as more likely to be structures of non-biological origin.
  • Exceptionally large, organic, smooth-walled, coccoidal microfossils are described from the 2.52 Ga Gamohaan Formation by Czaja, Beukes & Osterhout, who interpret them as fossils of sulfur-oxidizing bacteria similar to members of the modern genus Thiomargarita.
  • Macroscopic fossils up to 30 cm long and nearly 8 cm wide are described from the 1,56-billion-year-old Gaoyuzhuang Formation by Zhu et al., who interpret them as probable fossils of benthic multicellular eukaryotes of size that is unprecedentedly large for eukaryotes older than the Ediacaran Period.
  • Organic-walled microfossils with holes in the walls similar to those formed by predatory protists in the walls of their prey to consume the contents inside are described from the 780–740 million-year-old Chuar Group by Porter.
  • Tubular microfossils showing similarities to modern coenocytic green and yellow-green algae are described from the ~2.8 to 2.7 Ga lacustrine deposits in South Africa by Kaźmierczak et al..
  • Soft-bodied discoidal specimens resembling Aspidella are described from the Ediacaran Cerro Negro Formation by Arrouy et al..