Reduction–oxidation (redox) reactions occur during burial because sediments contain
reactive mixtures of oxidised and reduced components. Diagenetic chemical reactions …

Greigite (Fe3S4) is an authigenic ferrimagnetic mineral that grows as a precursor to pyrite
during early diagenetic sedimentary sulfate reduction. It can also grow at any time when …

Abstract The Quaternary System/Period represents the past 2.58 million years and is
officially subdivided into the Pleistocene and Holocene series/epochs, with the base of the …

Abstract The Executive Committee of the International Union of Geological Sciences on
January 17, 2020 ratified the Global Boundary Stratotype Section and Point (GSSP) defining …

The Quaternary Period, comprising the Holocene and Pleistocene Epochs, encompasses
the last~ 2.6 Ma during which time Earth's climate was strongly influenced by bipolar …

Authigenic greigite may form at any time within a sediment during diagenesis. Its formation
pathway, timing of formation, and geological preservation potential are key to resolving the …

Abstract The Global Boundary Stratotype Section and Point (GSSP) defining the base of the
Chibanian Stage and Middle Pleistocene Subseries at the Chiba section, Japan, was ratified …

Continental shelves serve as a bridge between the continent and ocean and sediments in
this region are sensitive to land-sea interaction, sea-level variation and local subsidence. In …

Sediments from the continental shelf are sensitive to sea level, climatic changes, and local
tectonic history. In this study, we carried out a high‐resolution magnetostratigraphic …

Abstract Greigite (Fe3S4) is a widespread authigenic magnetic mineral in anoxic sediments
and is also commonly biosynthesized by magnetotactic bacteria in aqueous environments …