N Jiao, T Luo, Q Chen, Z Zhao, X Xiao, J Liu… - Nature reviews …, 2024 - nature.com
The ocean has been a regulator of climate change throughout the history of Earth. One key mechanism is the mediation of the carbon reservoir by refractory dissolved organic carbon …
PR Johnson, A Andresen, AS Collins, AR Fowler… - Journal of African Earth …, 2011 - Elsevier
During the late Cryogenian–Ediacaran (650–542Ma), the Arabian–Nubian Shield (ANS) underwent final assembly and accretion to the Saharan Metacraton concurrent with the …
The oxygen content of the Earth's surface environment is thought to have increased in two broad steps: the Great Oxygenation Event (GOE) around the Archean–Proterozoic boundary …
GM Cox, GP Halverson, RK Stevenson… - Earth and Planetary …, 2016 - Elsevier
Atmospheric CO 2 levels and global climate are regulated on geological timescales by the silicate weathering feedback. However, this thermostat has failed multiple times in Earth's …
The Ediacaran Doushantuo Formation (ca. 635–551Ma) in South China contains exceptionally well-preserved fossils of multicellular eukaryotes including early animals, and …
The secular trend of seawater strontium isotope ratio (87 Sr/86 Sr) reflects changes in the relative contributions of continental versus mantle reservoirs to ocean composition, and …
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 …
Abstract The Ediacaran Shuram carbon isotope excursion (CIE) follows the regional Gaskiers glaciation and occurs before the appearance of macroscopic animal fossils …
Abstract The Ediacaran Period follows the Cryogenian Period in the wake of a snowball Earth glaciation and precedes the Cambrian Period with its rising tide of animal radiation. It …