“…Chemical approaches in particular have proven successful when applied to anthropogenic deposits, including applications of bulk sediment geochemistry, such as energy and wave dispersive X‐ray fluorescence (XRF) spectrometry (ED‐XRF and WD‐XRF, respectively), phosphate extraction, inductively coupled plasma atomic emission spectroscopy, inductively coupled plasma mass spectroscopy, atomic absorption spectrometry (AAS), and sometimes Neutron Activation Analysis, which have aided archaeologists interested in identifying site‐specific activity areas such as food processing, floor construction, and fire maintenance (e.g., Barba, ; Beck, ; Entwistle & Abrahams, ; Entwistle, Dodgshon, & Abrahams, ; Fernández, Terry, Inomata, & Eberl, ; Middleton & Price, ; Middleton et al, ; Milek & Roberts, ; Neff et al, ; Parnell, Terry, & Nelson, ; Terry, Fernández, Parnell, & Inomata, ; Wells, ; Wilson, Davidson, & Cresser, ). However, while these methods provide valuable chemical information, they can be more reflective of natural processes because bulk sampling is too coarse to disentangle complex anthropogenic deposits, such as hearths, middens, or roof and floor sequences, and may conflate multiple daily activities that exist at the microscale (Courty et al, ; Karkanas & Goldberg, ).…”