Tonian Period
Diversification of acritarchs
The Tonian is the first period of the Neoproterozoic, occuring after the Stenian (Mesoproterozoic Era) and before the Cryogenian Period
Geologic Age
1,000–720 Ma
Subdivisions
No subdivisions
"Tonian" is Greek for stretch, referring to the continents during the Rodinian break-up
Eon / Era
What happens during this time?
Geophysical
The supercontinent Rodinia begins to break up
Biological
Cyanobacteria present in the fossil record
Stromatolites begin to precipitously decline at about 1.0 Ga (Bernard et al. 2013)
Bitter Springs Formation (Australia) shows a diverse array of cells, called acritarchs
Acritarchs are small organic microfossils in marine sediments
Probably the remains of different organisms (early metazoans, ancestral fungi, and algae), some in their cyst stage
Evidence of Green algae
Filamentous algae fossils from this time show clean-cut circular holes in their cell walls similar to the feeding damage by Vampyrella-like amoebae
Seaweed-like green alga, Proterocladus antiquus, from China found at roughly 1.0 Ga (Tang et al. 2020)
Evidence of macroalgae from around 950 Ma from the Yukon of Canada (Phys.org; Maloney et al. 2021)
Multiple species of algae thrived together on the seafloor nestled between bacterial mounds in a shallow ocean
Researchers have identified a multicellular algae called Arctacellularia tetragonala that has chlorophyll derivatives (nickel-geoporphyrins), preserved in situ in the cells (Sforna et al. 2022)
Evidence of fungi in the fossil record
Multicellular organic-walled microfossils with fungal affinities are found in the shale of the Grassy Bay Formation (Shaler Supergroup, Arctic Canada), approximately 1,010–890 million years ago (Loron et al. 2019)
Fossil filaments and mycelium-like structures with vestigial chitin, remnants of fungal networks, found in dolomitic shale from the Mbuji-Mayi Supergroup, Democratic Republic of Congo from 810 to 715 million year old (Bonneville et al. 2020)
Carbonaceous filaments of ~5 μm in width exhibit low-frequency septation (pseudosepta) and high-angle branching that can form dense interconnected mycelium-like structures
Branching, tubular, meshlike structures found from Northwest Territories (Canada) might be evidence of horny sponges, and the oldest evidence of animals (Turner 2021)
Although, this is disputed as possible microbial or mineral traces
Above: Palaeolyngbya, a cyanobacterium, from Bitter Springs (Schopf).
Above: Acritarch algae
Above: Macroalgae from the Early Tonian of Yukon Territory
Above: Seaweed-like green alga, Proterocladus antiquus
Above: Vampyrella feeding on a filamentous green alga
Above: thin section from the Congolese dolomitic shale rock showing fungal hyphae (Bonneville et al. 2020)