During reduction diagenesis, production of dissolved Fe2+ by reduction of ferric oxide starts
at the Fe-redox boundary. The associated magnetic property changes may influence …

We present the magnetostratigraphy and calcareous nannofossil biostratigraphy of the~ 81
m thick upper Paleocene–lower Eocene Cicogna section from the Belluno Basin of NE Italy …

Previous workers identified a magnetically anomalous clay layer deposited on the northern
United States Atlantic Coastal Plain during the Paleocene‐Eocene thermal maximum …

We report the use of S-band ferromagnetic resonance (FMR) spectroscopy to compare the
anisotropic properties of magnetite particles in chains of cultured intact magnetotactic …

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

An archaeomagnetic, rock magnetic and magnetic fabric study has been carried out on
seven anthropogenic ash horizons in the Middle Palaeolithic sedimentary level XXIV at the …

Magnetite (Fe, O) is one of the most stable carriers of natural remanent magnetization (NRM)
in sedimentary rocks, and paleomagnetic studies of magnetite-bearing sediments, such as …

Conventional magnetofossils are the remains of magnetotactic bacteria and giant
magnetofossils are the remains of iron biomineralizing organisms that have not yet been …

Single‐domain magnetite particles produced by magnetotactic bacteria (magnetosomes)
and aligned in chains are of great interest in the biosciences and geosciences. Here, we …

Magnetotactic bacteria (MTB) are known to biosynthesise single-domain magnetite (Fe3O4)
for geomagnetic navigation and their relict magnetosomes (called magnetofossils) can …