Two pulses of faunal mortality occurred during the Late Ordovician mass extinction (ca. 445 Ma). This biocrisis is recorded in Hirnantian strata of South China as a stepwise extinction of …
The rise of atmospheric oxygen fundamentally changed the chemistry of surficial environments and the nature of Earth's habitability. Early atmospheric oxygenation occurred …
Rare earth elements and yttrium (REY) have a distinct distribution pattern in seawater, and this pattern may be faithfully preserved in carbonate sediments and rocks. Anomalous …
Oceanic anoxia—including euxinic settings defined by the presence of water column hydrogen sulfide (H2S)—is minor in the ocean today. Such conditions, however, were …
C Zou, Z Qiu, SW Poulton, D Dong, H Wang… - …, 2018 - pubs.geoscienceworld.org
Abstract The Late Ordovician mass extinction (LOME, ca. 445 Ma) was the first of the “Big Five” Phanerozoic extinction events and comprised two extinction pulses. Proposed kill …
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 …
The rise of atmospheric oxygen during the Great Oxidation Event some 2.4 billion years ago was a defining transition in the evolution of global biogeochemical cycles and life on Earth …
K Zhang, X Zhu, RA Wood, Y Shi, Z Gao… - Nature Geoscience, 2018 - nature.com
Abstract The Mesoproterozoic era (1,600–1,000 million years ago (Ma)) has long been considered a period of relative environmental stasis, with persistently low levels of …
The speciation of iron in sediments and sedimentary rocks is a widely used proxy for the chemistry and oxidation state of ancient water bodies. Specifically, the fraction of reactive …