Abstract
Pittsburg Basin, a small kettle lake in south-central Illinois, was formed after the retreat of the Illinoian ice sheet (∼130 ka B.P.), and the sedimentary record includes the last interglacial–glacial cycle. Curie temperature measurements, XRD analyses and thermal demagnetization of a low-temperature J rs indicate that the magnetic fraction is characterized by oxidized magnetite and magnetic iron sulfides. The grain size of the magnetic fraction was estimated from ARM/J rs ratios, frequency-dependent susceptibility, and hysteresis parameters. These measurements show that glacial sediments contain coarse-grained, presumably detrital, material while interglacial samples have an additional fine-grained magnetic component, which cannot be explained by a single catchment or climatic process. Early interglacial samples show magnetic properties characteristic of authigenic biogenically produced magnetite, while late interglacial samples are probably influenced by pedogenesis around the basin.
Published Version
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call