Cambro-Ordovician microorganisms: acritarchs and endoliths
Organic-walled microfossils are abundant and taxonomically diverse in Cambrian-Ordovician strata; some are important for biostratigraphy and for the correlation of geological successions. New assemblages of Cambrian-Ordovician acritarchs from Kolguev Island, Arctic Russia and Middle Cambrian ichnofossils of endoliths from Peary Land, North Greenland ...
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Evolutionary escalation in an exceptionally preserved Cambrian biota from the Grand Canyon (Arizona, USA). [PDF]
Mussini G +7 more
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Marine and non-marine strata preserving Ediacaran microfossils. [PDF]
Lehn I, Horodyski RS, Paim PSG.
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Proterozoic acritarchs and divergences of green microalgae
The morphology of microfossils with resistant cell walls, their ornamentation and functionally identifiable structures are the first source of information used to assess their biological affinities. Difficulties in relying on morphology alone due to the problem of convergent morphology may be resolved by the ultrastructure of the cell wall and its ...
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Environmental phylogenetics supports a steady diversification of crown eukaryotes starting from the mid-Proterozoic. [PDF]
Sandin MM, Cohen PA, Morlon H, Burki F.
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Lethal microbial blooms delayed freshwater ecosystem recovery following the end-Permian extinction. [PDF]
Mays C +5 more
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Causes and consequences of end-Ediacaran extinction: An update. [PDF]
Darroch SAF +5 more
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The hard steps model and whole Earth-system transitions. [PDF]
Watson A.
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Age and paleo-environmental evolution of the Douala Basin (Cameroon) during the Cenozoic: insights from palynology and sequence analysis. [PDF]
Mfayakouo BC, Ngaha PRN, Bitom DL.
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