The Paleocene‐Eocene Thermal Maximum, which occurred∼ 55.5 Ma, was caused by a
massive release of carbon, as indicated by an∼ 3‰ negative carbon isotope excursion …

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

Many sources of magnetic minerals have been implicated as potential influences on the
magnetic record of lake and ocean sediments. The “state-of-the-art” of our knowledge of …

New rock magnetic results (thermal fluctuation tomography, high-resolution first-order
reversal curves and low temperature measurements) for samples from the Paleocene …

We report a novel authigenic nanoscale magnetite source in marine methane seep
sediments. The magnetite occurs in large concentrations in multiple horizons in a 230 m …

Abstract Sediments from the Tasman Basin in the southwest Pacific Ocean show a cyclic
pattern of variation in mineral magnetic properties, including susceptibility and remanence …

Environmental magnetic studies of annually laminated sediments from Lake Ely,
northeastern Pennsylvania, USA indicate that bacterial magnetite is the dominant magnetic …

Magnetite is the magnetic mineral most prominent as a remanence carrier in sediments. Not
surprisingly, the discovery of a magnetic bacterium (Blakemore, 1975) caught the attention …

We have investigated the variability of the magnetic properties of surface sediments across
eight Minnesota lake basins. The measured magnetic properties are controlled by the …

The Paleocene–Eocene boundary (∼ 55.8 million years ago) is marked by an abrupt
negative carbon isotope excursion (CIE) that coincides with an oxygen isotope decrease …