Unambiguous magnetic mineral identification in sediments is a prerequisite for
reconstructing paleomagnetic and paleoenvironmental information from environmental …

Red clay widely occupies the seafloor of pelagic environments in middle latitudes, and
potentially preserves long paleoceanographic records. We conducted a rock-magnetic study …

Magnetotactic bacteria (MTB) have long fascinated geologists and biologists because they
biomineralize intracellular single domain (SD) magnetite crystals within magnetosomes that …

Magnetotactic bacteria (MTB) preserved in sediments (magnetofossils) are highly sensitive
to environmental and climatic forcing and can therefore be used as an easy-to-measure …

First-order reversal curve diagrams, or FORC diagrams, have been studied to determine if
the widths of their distributions along the interaction and coercivity axes can be related to the …

Records of natural remanent magnetization (NRM) and geomagnetic polarity reversals
preserved within ferromanganese (Fe-Mn) crusts, together with the application of fine …

First‐order reversal curve (FORC) distributions are a powerful diagnostic tool for
characterizing and quantifying magnetization processes in fine magnetic particle systems …

Bedded chert is a distinctive rock type characterized by a rhythmic alternation of quartz-rich
chert beds and clay-rich interbeds. The origin of the lithologic variations is not well …

The strong glacial–interglacial similarity between the magnetic susceptibility (MS) of
Southern Ocean sediments and Antarctic ice core dust records has often been used to …

Reductive dissolution of magnetite is known to occur below the Fe-redox boundary in
sediments. In this study, detailed processes associated with biogenic magnetite dissolution …