The article represents an overview and
generalization of the microprobe and thermomagnetic data on the distribution,
content and composition of metallic iron in Pleistocene
lacustrine sediments of the Darhad Basin, northern Mongolia, in the Upper
Miocene sediments of Lake Baikal.
Epicontinental sediments of Miocene-Late
Jurassic, and Early Cambrian ages in different regions of North Eurasia and in
Miocene-Late Jurassic oceanic sediments of North- Western Atlantic.
Iron particles percentage varies from ~10-5 to
0.05%, their distribution is bimodal with the distinct zero mode, and the
accumulation of iron particles is inversely linked with the rate of
sedimentation. Pyrite and pyrrhotite are widespread in the studied sediments,
and the distribution of metallic iron does not depend on the presence of pyrite.

