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 …

Phosphorus is a limiting nutrient that is thought to control oceanic oxygen levels to a large
extent,–. A possible increase in marine phosphorus concentrations during the Ediacaran …

The largest negative inorganic carbon isotope excursion in Earth's history, namely the
Ediacaran Shuram Excursion (SE), closely followed by early animal radiation, has been …

Glacial erosion has long been recognized as a significant factor contributing to continental
denudation during the Ediacaran Period, consequently leading to geochemical …

The realization of practical lithium–sulfur (Li–S) batteries is contingent on the development
of innovative electrode designs having high energy, high power and a long lifespan. Herein …

Earth is the only planet known to be habitable, and is also unique with its liquid water, and
the operation of plate tectonics. The geological record shows that the habitability of our …

Abstracts Cap carbonate is the most unique component of a Snowball Earth glaciation, ie,
two Cryogenian global glaciations. In the canonical model, cap carbonate precipitation …

Abstract The Ediacaran-Cambrian transition is recognized as a warm period. However,
glaciations have been reported in many paleocontinents worldwide during this transition …

Abstract The Ediacaran Period (635–539 Ma) witnessed the largest negative excursion in
inorganic carbon isotope (δ13Ccarb) over the Earth's geological history, also known as the …

Abstract The late Neoproterozoic Takab banded iron formation (BIF) occurs in one of the
most important part of the Iranian plateau containing Precambrian crustal segments, now …