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

In environmental magnetism, rock and mineral magnetic techniques are used to investigate
the formation, transportation, deposition, and postdepositional alterations of magnetic …

Magnetotactic bacteria (MTB) are a diverse group of microorganisms with the ability to orient
and migrate along geomagnetic field lines. This unique feat is based on specific intracellular …

Magnetotactic bacteria, which most commonly live within the oxic-anoxic transition zone
(OATZ) of aquatic environments, produce intracellular crystals of magnetic minerals …

Magnetotactic bacteria (MTB) are ubiquitous aquatic microorganisms that incorporate iron
from their environment to synthesize intracellular nanoparticles of magnetite (Fe3O4) or …

Magnetic hysteresis measurements of sediments have resulted in widespread reporting of
“pseudo‐single‐domain”‐like magnetic properties. In contrast, the ideal single domain (SD) …

The impacts of the Paleocene‐Eocene thermal maximum (PETM)(∼ 55 Ma), one of the most
rapid and extreme warming events in Earth history, are well characterized in open marine …

We reconstruct eustatic variations during the latest Paleocene and earliest Eocene (∼ 58–
52 Ma). Dinoflagellate cysts, grain size fractions, and organic biomarkers in marine sections …

This book describes the paleomagnetism of sediments and sedimentary rocks, how
sediments and sedimentary rocks become magnetized, and how the physical and chemical …

Magnetotactic bacteria (MTB) belong to several phyla. This class of microorganisms exhibits
the ability of magneto-aerotaxis. MTB synthesize biominerals in organelle-like structures …