At Owens Lake, California, paleomagnetic data document the Matuyama/Brunhes polarity
boundary near the bottom of a 323-m core (OL-92) and display numerous directional …

The recent development of automated pass-through cryogenic magnetometers for
measuring remanence directions, and equipment for the rapid measurement of mineral …

Sediments recovered from the most seaward site of the Baja Transect of the California
Margin (ODP Leg 167) yielded a high-fidelity magnetostratigraphic record spanning the last …

New developments and discoveries in biomineralization have occurred almost continuously
in the intervening decade since the previous IUGG quadrennial report on biomineralization …

The capacity of rocks to magnetically record Earth history has played a crucial part in
transforming the way we look at our planet. It has also provided much stimulus for the study …

We have developed a quantification method that uses mainly room temperature rock
magnetic measurements to calculate concentrations of ferrimagnetic particles in sediments …

Continental shelf sediments along the northeast continental margin of North America contain
a magnetofossil‐rich interval deposited during the Paleocene‐Eocene Thermal Maximum …

On the mid‐Atlantic Coastal Plain of the United States, Paleocene sands and silts are
replaced during the Paleocene‐Eocene Thermal Maximum (PETM) by the kaolinite‐rich …

Magnetofossils are magnetic nanoparticles that represent the fossil remains of
microorganisms that biomineralize magnetic minerals in a genetically controlled manner …

Remanent magnetism in marine sediments has been used extensively over the past twenty
years to calibrate the geological time-scale, study geomagnetic reversals and secular …