Magnetofossil spike during the Paleocene‐Eocene thermal maximum: Ferromagnetic resonance, rock magnetic, and electron microscopy evidence from Ancora, New …
Previous workers identified a magnetically anomalous clay layer deposited on the northern
United States Atlantic Coastal Plain during the Paleocene‐Eocene thermal maximum …
United States Atlantic Coastal Plain during the Paleocene‐Eocene thermal maximum …
Discovery of giant magnetofossils within and outside of the Palaeocene-Eocene Thermal Maximum in the North Atlantic
P Xue, L Chang, Z Pei, RJ Harrison - Earth and Planetary Science Letters, 2022 - Elsevier
Giant magnetofossils have exceptionally large grain sizes and peculiar morphologies
compared to conventional biogenic magnetite nanoparticles. The origin of these unusual …
compared to conventional biogenic magnetite nanoparticles. The origin of these unusual …
Gigantism in unique biogenic magnetite at the Paleocene–Eocene Thermal Maximum
We report the discovery of exceptionally large biogenic magnetite crystals in clay-rich
sediments spanning the Paleocene–Eocene Thermal Maximum (PETM) in a borehole at …
sediments spanning the Paleocene–Eocene Thermal Maximum (PETM) in a borehole at …
Quantified abundance of magnetofossils at the Paleocene–Eocene boundary from synchrotron-based transmission X-ray microscopy
H Wang, J Wang, YK Chen-Wiegart… - Proceedings of the …, 2015 - National Acad Sciences
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 …
negative carbon isotope excursion (CIE) that coincides with an oxygen isotope decrease …
Giant magnetofossils and hyperthermal events
Magnetotactic bacteria biomineralize magnetic minerals with precisely controlled size,
morphology, and stoichiometry. These cosmopolitan bacteria are widely observed in aquatic …
morphology, and stoichiometry. These cosmopolitan bacteria are widely observed in aquatic …
Diversification of iron‐biomineralizing organisms during the Paleocene‐Eocene Thermal Maximum: Evidence from quantitative unmixing of magnetic signatures of …
Conventional magnetofossils represent magnetic mineral remains of magnetotactic bacteria.
Giant magnetofossils have no known modern analog. Both conventional and giant …
Giant magnetofossils have no known modern analog. Both conventional and giant …
A biogenic origin for anomalous fine‐grained magnetic material at the Paleocene‐Eocene boundary at Wilson Lake, New Jersey
PC Lippert, JC Zachos - Paleoceanography, 2007 - Wiley Online Library
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 …
massive release of carbon, as indicated by an∼ 3‰ negative carbon isotope excursion …
An Appalachian Amazon? Magnetofossil evidence for the development of a tropical river‐like system in the mid‐Atlantic United States during the Paleocene‐Eocene …
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 …
replaced during the Paleocene‐Eocene Thermal Maximum (PETM) by the kaolinite‐rich …
Chains, clumps, and strings: Magnetofossil taphonomy with ferromagnetic resonance spectroscopy
Magnetotactic bacteria produce intracellular crystals of magnetite or greigite, the properties
of which have been shaped by evolution to maximize the magnetic moment per atom of iron …
of which have been shaped by evolution to maximize the magnetic moment per atom of iron …
Key signatures of magnetofossils elucidated by mutant magnetotactic bacteria and micromagnetic calculations
Magnetotactic bacteria (MTB) produce single‐stranded or multi‐stranded chains of magnetic
nanoparticles that contribute to the magnetization of sediments and rocks. Their magnetic …
nanoparticles that contribute to the magnetization of sediments and rocks. Their magnetic …