Abstract The Ediacaran-Cambrian transition, which incorporates the radiation of animals,
lacks a robust global temporal and spatial framework, resulting in major uncertainty in the …

Water plays a critical role in erosion and sediment transport and this relationship is most
evident in the hyperarid Atacama Desert of Northern Chile, a region characterized by …

The emergence of the Ediacara biota soon after the Gaskiers glaciation ca. 580 million years
ago (Ma) implies a possible glacial fuse for the evolution of animals. However, the timing of …

The Ediacara Biota—the oldest communities of complex, macroscopic fossils—consists of
three temporally distinct assemblages: the Avalon (ca. 575–560 Ma), White Sea (ca. 560 …

Abstract The Ediacaran Shuram carbon isotope excursion (CIE) follows the regional
Gaskiers glaciation and occurs before the appearance of macroscopic animal fossils …

The morphologically differentiated benthic macrofossils of algae and putative animal
affinities of the Lantian biota in China represents the oldest known Ediacaran macroscopic …

Glacial depositions are widely discovered in the late Ediacaran strata all over the world, but
the temporal and spatial distributions of the Ediacaran glaciations remain poorly …

The transition from the terminal Ediacaran to early Cambrian (ca. 550–530 Ma) witnessed
both the decline of Ediacaran-type soft-bodied and skeletal biota and the rapid …

Abstract The Nama Group exposed on the Neint Nababeep Plateau along the Orange River
in northwestern Republic of South Africa is now recognized as an expanded record of the …

The advent of animal (metazoan) biomineralization marks a fundamental transition in Earth's
history, facilitating the diversification of novel body plans as well as the biological control of …