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231.
M. Llobera P. Fábrega-Álvarez C. Parcero-Oubiña 《Journal of archaeological science》2011,38(4):843-851
The aim of this paper is to extend the range of current analytical procedures that archaeologists use to understand movement. In particular, how a landscape becomes ordered by simply defining a destination. More specifically, this study proposes the derivation of a focal mobility network, i.e. the network of most likely paths towards a given destination, and explores several of its applications within a landscape archaeology framework. The suggested extensions are based on existing standard procedures within most GIS. A series of synthetic control surfaces and an archaeological study focused around Iron Age hillforts in Galicia (NW Spain) are used as case studies to illustrate different analytical possibilities. 相似文献
232.
DENISSE SEPULVEDA SANCHEZ ANNE LAVANCHY CÉLINE HEINI ALINE ACEVEDO 《Anthropology today》2021,37(2):23-25
One of the most important social upheavals in Chile since the end of the dictatorship started in October 2019, and continued until the coronavirus outbreak in March 2020. The event affected the ethnographic fieldwork that we, four anthropologists, were conducting at that time. This article draws on the recognition that, while being in different geographical locations, our respective experiences involve similar affects. Drawing on feminist epistemology, we have utilized these emotional experiences as a methodological tool to spark curiosity and open up a space for reconsidering fieldwork as ‘feel-work’. Our respective positioning, in terms of national and emotional feelings of belonging as well as physical location, created affective dissonances that raised uneasiness while at the same time opening up a productive space to think about fieldwork as an experience of ‘out-of-place’ bodies and ‘out-of-place’ feelings. 相似文献
233.
Cristian Kaufmann María A. Gutiérrez María C. Álvarez Mariela E. González Agustina Massigoge 《Journal of archaeological science》2011,38(2):334-344
Hydrodynamic sorting is a taphonomic process able to transport and scatter bones deposited in archaeological and paleontological sites. This study presents the results of experimentation performed in an artificial flume with guanaco (Lama guanicoe) bones of different ontogenetic development, dry and saturated in water, in hydric flows velocities of 15 and 30 cm/s. The obtained results show that bone global density, the age of the individual, the dry or wet bone state, and the hydric flow velocity influence significantly bone dispersion. In this way, bones from immature individuals with unfused secondary growth centers and relatively low bulk density have better possibility of being transported than fused bones from adult individuals. Taking into account the results obtained in this experimentation and the feasibility of discriminating age categories in fossil assemblages, two bone groups with differential potential transport are presented in this paper. These transport groups constitute a methodological tool to evaluate the role hydric current may had played in the formation of a fossil assemblage. 相似文献
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