Using chaîne opératoire and communities of practice to identify interaction in the Contact and Mission periods in southern Georgia,AD 1540–1715

ABSTRACT

In this article, the pottery production of indigenous groups living inside and outside of colonial spaces in southern Georgia is compared by identifying portions of the chaîne opératoire of pottery production. Diachronic and geographic changes to production demonstrate that groups living in the interior of Georgia were in continual interaction with coastal groups in the mission system. This interaction likely contributed to the emergence of the Altamaha pottery tradition, which spread from southern South Carolina to northern Florida during Spanish colonization of the region. This research shows that Native American groups navigating colonialism drew on a wide network of communities to alter traditions in the face of unprecedented social change.     

Mesolithic in South‐Eastern Norway

This article discusses the reliability of shore‐line displacement curves based on pollen analysis in the Oslo Fjord area. The conclusion is that only small parts of the curves ‐ in the late Atlantic period ‐ are fairly reliable for the purpose of dating Mesolithic coastal sites.

Twelve Mesolithic settlement sites from Østfold, south‐eastern Norway are classified morphologically. The author suggests a chronological lineal model with four succeeding phases: 1. The Fosna culture, 2. Late Boreal/early Atlantic group, 3. The N?stvet culture, 4. Late flint‐point using group. A connection between the Fosna culture and early Maglemose culture is claimed.

A study of the ecological adaptation in the four phases is based on topographical conditions, on the distribution and situation of settlement sites, and on animal bones from three Mesolithic sites in south‐eastern Norway. Hypotheses on seasonal migrations are suggested.     

In situ oxygen isotope micro-analysis of faunal material and human teeth using a SHRIMP II: a new tool for palaeo-ecology and archaeology

A Sensitive High Resolution Ion MicroProbe (SHRIMP II) has been used to make high spatial resolution in situ micro-analyses of oxygen isotopes in fish otoliths, and teeth from fossil herbivores and a Neanderthal. Large intra-tooth variations in the oxygen isotopic composition (up to 9‰) were observed in the enamel of herbivores from the Neanderthal fossil site of Payre, consistent with preservation of seasonal cyclicity. The range of isotopic compositions observed in Neanderthal tooth enamel was much smaller (∼3‰), possibly the result of a longer enamel maturation time averaging out variability. An archaeological otolith from a Preceramic site in Northern Peru exhibited marked changes in δ¹⁸O over life, due either to the fish occasionally migrating from the sea to a lower salinity habitat, or to short-lived rises in sea water temperature. A fish otolith from Australia's Willandra Lakes World Heritage Area showed clear seasonal variations, but also a general trend towards isotopically heavier and more saline water, as indicated by higher δ¹⁸O and Sr/Ca values resulting from increased evaporation. The results of these case studies are compared to results of oxygen isotope analysis using more conventional methods and demonstrate the ability of the SHRIMP II to provide precise high spatial resolution in-situ oxygen isotope analyses of a variety of biogenic materials. This approach has major advantages over conventional methods. It can provide rapid, micro-scale isotopic analyses of sub-permil precision without the need for chemical preparation of the sample.     

The mineral wealth of ancient Arabia and its use I: Copper mining and smelting at Feinan and Timna – comparison and evaluation of techniques, production, and strategies

Near Eastern fieldwork in mining archaeology and archaeometallurgy began at Timna (Israel) in the 1960s and 1970s and continued in Feinan (Jordan) in the 1980s and 1990s. For the first time, Bronze Age copper mines were excavated and cleared and importance was given to the slag recovered. At both sites copper was produced for over 5000 years, from the Chalcolithic to the Mamluk periods. Although the broad outlines of technical development can be traced, much remains to be learned in future studies.