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

Luminescence holds unique potential as a sediment tracer and provenance method. The
tracer application of luminescence has key advantages including ease of measurement …

Magnetotactic bacteria (MTB) produce single‐stranded or multi‐stranded chains of magnetic
nanoparticles that contribute to the magnetization of sediments and rocks. Their magnetic …

Iron-bearing minerals are sensitive to a wide spectrum of natural processes and thus carry
important environmental information. In environmental magnetism, various techniques are …

Tropical hydroclimatic events, characterized by extreme regional rainfall anomalies, were a
recurrent feature of marine isotope stages 2–4 and involved some of the most abrupt and …

The anhysteretic remanent magnetization (ARM) is an important magnetic parameter for
quantifying the concentration of “fine”, mostly sub‐micron ferrimagnetic particles in rocks and …

Today's paleomagnetic and magnetic proxy studies involve processing of large sample
collections while simultaneously demanding high quality data and high reproducibility. Here …

The carbonate‐free abyss of the North Pacific defies most paleoceanographic proxy
methods and hence remains a “blank spot” in ocean and climate history. Paleomagnetic and …

As iron‐bearing minerals—ferrimagnetic minerals in particular—are sensitive to stress,
temperature, and presence of fluids in fault zones, their magnetic properties provide …

Continental margin sediments of SE South America originate from various terrestrial
sources, each conveying specific magnetic and element signatures. Here, we aim to identify …