作者: G.A. Clark , C. Michael Barton
DOI: 10.1016/J.QUAINT.2016.08.002
关键词: Geology 、 Radiocarbon dating 、 Sedimentary depositional environment 、 Lithic analysis 、 Paleontology 、 Cave 、 Climate change 、 Artifact (archaeology) 、 Ice core 、 Rock shelter
摘要: Abstract With the recognition that practically all archaeological sites are depositional composites unrelated to activities of any contemporaneous group individuals (i.e., palimpsests) and forager adaptations not ‘site-specific’ but rather landscape-scaled phenomena, statistical approaches designed take these predicates into account have been developed over past 20 years depart from traditional techno-typological systematics used for decades in much Europe Levant. Based on artifact density frequency retouched pieces scaled volume sediment excavated cave rock shelter sites, – surface ratio artifacts totals unit area, they can potentially determine whether or changes mobility land-use often assumed coincided with major evolutionary events (e.g., Middle-Upper Paleolithic transition) actually occurred. Lithic counts densities La Riera (Posada de Llanes, Asturias, Spain) here illustrate potential approach. Changes volumetric then compared a radiocarbon summed probability curve using calibrated BP dates against oxygen isotope ratios GISP2 ice core. The intent is what extent macroclimatic change 30–10 ka cal interval compares sequence.