The end‐Neoproterozoic transition marked a gradual but permanent shift between distinct
configurations of Earth's biosphere. This interval witnessed the demise of the enigmatic …

Re-evaluation of eumetazoan modular coloniality gives a new perspective to Ediacaran–
Ordovician animal diversification. Highly integrated eumetazoan colonies (porpitids …

Paraconularia ediacara n. sp., the oldest documented conulariid cnidarian, is described
based on a compressed thin specimen from the terminal Ediacaran Tamengo Formation …

Abstract The Ediacaran-Cambrian Bambuí Group in Brazil records an anomalously positive
excursion in carbonate carbon isotopes (δ 13 C carb) with a sustained plateau of ca.+ …

Owing to their temporal position during the decline of the classic Ediacara biota and the
appearance of the more recognizable metazoans of the Cambrian Period, the terminal …

The index ichnofossil Treptichnus pedum Seilacher 1955 and four types of Microbially
Induced Sedimentary Structures (MISS)-variants of wrinkle and elephant skin structures–are …

The Ediacaran tubular fossils Cloudina, Sinotubulites, and Conotubus are taxonomically
revised with type materials. It is proposed that Aulophycus lucianoi Beurlen and Sommer …

Mixed carbonate–siliciclastic deposits of the Tamengo Formation (terminal Ediacaran),
record the rise of calcifying metazoans and the origin of exoskeletons in animals. To explore …

The Ediacaran period is marked by global icehouse episode, greenhouse period, increasing
levels of oxygen-carbon dioxide, syn-glaciogenic structures-BIFs, typical Ediacaran biota …

A well preserved assemblage of organic-walled microfossils is described from the Alicia and
Cerro Negro formations of the La Providencia Group. The microbiota is dominated by …