Interest in mineral–microbe interaction has grown enormously over recent decades,
providing information in a puzzle-like manner which points towards an ever increasingly …

Much work has been undertaken quantifying the abundance of phyllosilicate clay minerals
in soils, sediments and rocks of Earth's crust. However, no detailed global compilation of …

For the first four billion years of Earth's history, climate was marked by apparent stability and
warmth despite the Sun having lower luminosity. Proposed mechanisms for maintaining an …

This study aims to determine the interdependence of deposition, tectonics and diagenesis in
a prolific hydrocarbon reservoir. This has been achieved through an integrated field study …

The existence of stabilizing feedbacks within Earth's climate system is generally thought to
be necessary for the persistence of liquid water and life. Over the course of Earth's history …

This study presents a review on palaeogeographic implications and temporal variations of
glaucony covering both modern and ancient records. Phanerozoic glaucony preferably …

Retrograde clay mineral reactions (reverse weathering), including glauconite formation, are
first-order controls on element sequestration in marine sediments. Here, we report …

Although Paleogene warm climatic intervals have received considerable attention for
atmospheric and oceanographic changes, the authigenic mineralization associated with …

The rare earth elements (REEs) are an important tool for understanding biogeochemical
cycling and sedimentary processes in the global ocean. However, ambiguities in the marine …

Three types of glaucony grains were identified in the late Eocene (~ 35.5–34.1 Ma)
sediments from Ocean Drilling Program (ODP) Hole 696B in the northwestern Weddell Sea …