Archaeological discontinuities in the southern hemisphere: A working agenda
Section snippets
Archaeological discontinuities: An introduction
Change is the norm rather than the exception in archaeological scale, though its rate and mode are not uniform in time or space. Change accelerates its pace at given times and places along the course of human history, producing what we perceive as discontinuities or transitions in archaeological scale. Beyond its empirical or historical basis, recording and –above all – explaining archaeological discontinuities are eminently theoretical endeavors. Two of the most important sources of
Deconstructing discontinuities I: time
As championed from different backgrounds by Braudel’s (1958) Annales school and Bailey’s time perspectivism, ‘differing timescales bring into focus different features of behavior, requiring different sorts of explanatory principles’ (Bailey, 1981, 103; see also Bailey, 2007). This insightful assertion is nowhere more valid and in need of current attention than in the interpretation of archaeological discontinuities. What sort of past phenomena are we dealing with when assessing discontinuities
Deconstructing discontinuities II: space
Archaeological discontinuities recorded at different spatial scales would require different explanatory mechanisms that can be connected hierarchically (Delcourt and Delcourt, 1988). As Barberena, Méndez and de Porras (this volume) argue, we can use the multi-level character of historic processes in our favor by shifting spatial scales in order to visualize archaeological patterns. Complementing the strategy mentioned above for deconstructing discontinuities in time, the most productive
A working agenda
As we have already mentioned, archaeological discontinuities are a multi-dimensional set of phenomena with distinct expressions throughout the southern continents, though as we argue below, there are many shared processual aspects. Neither this introductory essay nor the papers contained in this volume encompass the full range of topics or approaches to this field. In this section we select a few issues that we consider worthy of systematic comparative attention in the years to come. These
Acknowledgments
We deeply thank Gustavo Politis and John M. O’Shea for their help and advice during the production of this volume. We acknowledge the support of Wenner-Gren Foundation in funding the workshop held in the context of the 4th Southern Deserts Conference from which this volume developed. Valeria Cortegoso offered comments that helped to improve the manuscript, while discussions with César Méndez contributed to build some arguments. Alejandra Gasco kindly allowed us to use the photo represented in
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Cited by (14)
Updated Peru archaeological radiocarbon database, 20,000–7000 <sup>14</sup>C BP
2024, Quaternary InternationalArchaeological discontinuity in Ultima Esperanza: A supra-regional overview
2018, Quaternary InternationalCitation Excerpt :O'Connor et al. (1999) defined several classes of discontinuity, including stratigraphic –sterile sediments between occupations-, chronological –important temporal differences between contiguous occupations- and cultural –typological, technological or behavioral differences between contiguous occupations-. These are not discontinuities derived from the artificial units used to organize the archaeological record (Barberena et al., 2016b; Veth et al., 2016), but the result of true gaps recorded in the sequences of the relevant sites. The archaeological Late Pleistocene record is limited to short occupations at two sites, Cueva del Medio and Cueva Lago Sofía 1, plus the suggested human presence at Cueva del Milodón based on cut marks on extinct horse bones (Hippidion saldiasi) (Martin, 2013, p. 263).
Early human occupation of a maritime desert, Barrow Island, North-West Australia
2017, Quaternary Science ReviewsCitation Excerpt :SU6 has mixed terrestrial and marine dietary assemblages containing four taxa of molluscs; Nerita, Tellina, Terebralia and Melo. A chronological discontinuity following this period coincides with the LGM, and is a common phenomenon in desert lowlands of the Southern Hemisphere (Barberena et al., 2017; Veth et al., 2017). Following the discontinuity, marine fauna increase markedly during SU5, dated to 22.4–7.2 ka, and coincident with the onset of the Indonesian-Australian Summer Monsoon and rapid sea level rises associated with Meltwater Phase 1A (Denniston et al., 2013).
Reconceptualising Last Glacial Maximum discontinuities: A case study from the maritime deserts of north-western Australia
2017, Journal of Anthropological ArchaeologyCitation Excerpt :They found that the grass steppe preserved a relatively continuous temporal record in contrast to the shrub steppe and Andean forest, where the record was discontinuous. Barberena et al. (2015) concluded that the observed differences represent ‘refugia - temporary barrier’ demographic dynamics (sensu Veth, 1993a, 1993b), with occupation favouring better hunting grounds on the grass steppe (and see Barberena et al. 2017). Australia, Veth et al. (2009) have argued that the concept of the ‘barrier desert’ should now be revised as new terminal Pleistocene sequences are being recovered within these lowlands.
An archaeological radiocarbon database for southern Africa
2019, Antiquity