Taphonomic Patterns of Elemental Enrichment: Synchrotron X-ray Fluorescence of Diverse Fossils From Multiple Konservat-lagerstätten, Extant Organisms, and Artificial Maturation Experiments
This study utilizes synchrotron X-ray fluorescence to demonstrate that fossil elemental compositions are primarily driven by diagenetic processes and sediment interaction rather than original tissue chemistry, indicating that most detected elemental signatures are exogenous and that attempts to identify tissue-specific markers must strictly control for geologic formation.