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Formation Process Analysis×Soil Micromorphology×
AlanArkeolojiArkeoloji
AileProcess / pipelineProcess / pipeline
Köken yılı19871938
KökenMichael B. Schiffer (behavioral archaeology)Walter L. Kubiëna (soil micromorphology); applied to archaeology by Goldberg, Macphail, Courty and others
TürInferential framework and analysis pipeline for record formationMicroscopic thin-section analysis pipeline for site formation
Seminal kaynakSchiffer, M. B. (1987). Formation Processes of the Archaeological Record. University of New Mexico Press. ISBN: 9780826309631Goldberg, P., & Macphail, R. I. (2006). Practical and Theoretical Geoarchaeology. Blackwell Publishing. ISBN: 9780632060443
Diğer adlarSite Formation Analysis, C-transforms and N-transforms, Behavioral Archaeology Formation Theory, Archaeological Record FormationArchaeological Micromorphology, Thin-Section Micromorphology, Sediment Thin-Section Analysis, Micromorphological Analysis
İlişkili22
ÖzetFormation process analysis is the framework for identifying the cultural and natural processes that transform materials from their living, systemic context into the archaeological record we excavate. Developed by Michael Schiffer within behavioral archaeology and codified in his 1987 Formation Processes of the Archaeological Record, it insists that the archaeological record is not a fossilized snapshot of past life but the cumulative product of how things were discarded, lost, reused, and disturbed (cultural or C-transforms) and how they then decayed, moved, and mixed in the ground (natural or N-transforms). Because every deposit has been filtered and rearranged by these processes, sound inference about past behavior requires first reconstructing the formation history of the record and correcting for it. Formation process analysis is therefore foundational to interpretation, linking excavation, geoarchaeology, and taphonomy.Soil micromorphology is the microscopic study of undisturbed soils and sediments in thin section to reconstruct how archaeological deposits formed and were altered. An oriented block is cut from a deposit without disturbing its internal structure, hardened with resin, and ground into a slice about thirty micrometers thick that can be examined under a petrographic microscope. At that scale the analyst can read features invisible in the field — the arrangement of mineral grains, microscopic charcoal and bone, plastered surfaces, dung, trampling fabrics, and the pedofeatures left by water, roots, and burrowing organisms. Developed for soil science by Walter Kubiëna and adapted for archaeology by geoarchaeologists such as Goldberg, Macphail, and Courty, micromorphology is the highest-resolution tool for interpreting site formation, occupation surfaces, and anthropogenic deposits in their original spatial context.
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