Proterozoic:
NeoProterozoic:
The Royal Tyrrell Museum has a lecture on the Ediacaran.
There is stronger evidence for the biomarkers for sponges being present starting in the Cryogenian.
MesoProterozoic:
The shallow seawaters of the Calymmian MesoProterozoic were very hypoxic, showing evidence of having .1% of the current oxygen in seawater.
PaleoProterozoic:
There is evidence of intracontinental rifting from China during the Rhyacian Paleoproterozoic.
Was there a 'Mawson continent' during the Paleoproterozoic?
Archean:
The SETI Institute has a lecture on volcanism during the Archean.
PaleoArchean:
NeoProterozoic:
The Royal Tyrrell Museum has a lecture on the Ediacaran.
There is stronger evidence for the biomarkers for sponges being present starting in the Cryogenian.
MesoProterozoic:
The shallow seawaters of the Calymmian MesoProterozoic were very hypoxic, showing evidence of having .1% of the current oxygen in seawater.
PaleoProterozoic:
There is evidence of intracontinental rifting from China during the Rhyacian Paleoproterozoic.
Was there a 'Mawson continent' during the Paleoproterozoic?
Archean:
The SETI Institute has a lecture on volcanism during the Archean.
PaleoArchean:
At least part of the trace fossils from Australia are pseudofossils (not real fossils).
EoArchean:
There is evidence of atmospheric oxygen from the EoArchean, 800 million years earlier than ever detected (or suspected) before.
Hadean:
In an almost extraordinary claim, the Siberian Craton may have bits of the crust from the Hadean!
Hadean:
In an almost extraordinary claim, the Siberian Craton may have bits of the crust from the Hadean!
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