Surface deformation in continental interiors is typically coupled to processes at depth.
However, in the Sichuan basin, east of the Tibetan Plateau, recent seismic data detect …

Abstract The Cambrian Period is the first period of the Phanerozoic Eon and witnessed the
explosive appearance of the metazoans, representing the beginning of the modern earth-life …

Abstract The “Cambrian Explosion” is known for rapid increases in the morphological
disparity and taxonomic diversity of metazoans. It has been widely proposed that this …

Abstract The Ediacaran–Cambrian transition is a critical interval marking drastic biological,
oceanic and geochemical co‐evolutions in geological history, but it is poorly constrained …

Given the high oxygen demands of complex metazoans, a sound understanding of marine
redox conditions is essential to reconstruct the factors that lead to the dramatic increases in …

The Neoproterozoic provides an important record of glacial–postglacial paleoenvironments,
organic carbon cycling, and hydrocarbon accumulation. Here, to better understand the …

The Ediacaran–Cambrian transition, one of the most critical intervals in Earth's history, is
marked by dramatic biological, oceanic and geochemical turnovers. Here high-resolution …

The organic-rich sediments were widely deposited over the entire Yangtze Block during the
Early Cambrian (late Nemakit-Daldynian to Botomian). In the mid-upper Yangtze region …

Early Cambrian organic-rich black rocks are extensively distributed in the southern China. In
this study, we have discussed the relation of paleo-sedimentary environments with …

The biosphere experienced episodic perturbations during the Neoproterozoic–early
Cambrian, accompanied by major fluctuations of the carbon cycle. However, compared to …