The Roman Ship 'punta Scifo d' and its Marble Cargo (Crotone,Italy)

In the first three centuries AD, large‐scale building projects, both in Rome and in the western colonies, stimulated the demand for marble from the eastern quarries. The Punta Scifo D shipwreck – discovered in 1986 in the Bay of Scifo, south of Crotone, Italy, and investigated in 2011 and 2013 by a team from the Università Ca' Foscari of Venice – is an important source for the reconstruction of this kind of trade in the Roman Empire. Studies of the cargo, dated to the third century AD, were the basis for the virtual reconstruction of a barge about 40 m long carrying a cargo of almost 340 tons. Petrographic and isotopic analyses demonstrated that it carried three different types of marble: mainly Proconnesian, some Pentelic, and one slab of Dokimean marble. The ship probably departed from the island of Marmara, and stopped at Ephesos, and perhaps also at Piraeus.     

Mesolithic shellfish exploitation in SW Italy: seasonal evidence from the oxygen isotopic composition of Osilinus turbinatus shells

Oxygen isotope analyses were carried out on the topshell Osilinus turbinatus from archaeological sites with the aim to investigate the temporal exploitation patterns by Mesolithic groups inhabiting coastal caves in SW Italy. In order to assess the present day O. turbinatus intra-annual δ¹⁸O variability, living specimens were collected monthly at Marina di Camerota (SW Italian peninsula). Their shell-edges were analysed and the seasonal results were compared with archaeozoological material. Our findings show that Mesolithic O. turbinatus exploitation was carried out almost exclusively during the colder and intermediary seasons (e.g. autumn, winter, spring), with very sporadic harvesting during the warmer seasons. Results suggest a possible regional exploitation pattern of O. turbinatus by Mesolithic groups inhabiting this region.     

American Seeds of ABACC? Findley's Proposal to Create a Mutual Nuclear Inspections System Between Brazil and Argentina

ABSTRACT

After the first Indian peaceful nuclear explosion in 1974 international observers perceived Argentina and Brazil, long-time rivals in South America, as countries that could follow suit. Not only had they not signed the Nuclear Non-Proliferation Treaty (NPT), they had also not joined the Tlatelolco Treaty: the Latin American and Caribbean nuclear-weapon-free zone. In this context, the US began to reassess and tighten its nonproliferation policy, particularly throughout the Jimmy Carter presidency (1977–1981). Carter's foreign policy sought to stall Argentine–Brazilian efforts to master the nuclear fuel cycle, as well as push them toward Tlatelolco. These efforts ultimately proved unsuccessful. However, after a visit to Argentina and Brazil, US congressman Paul Findley suggested in 1977 that they consider a bilateral agreement, whereby they would agree to mutual inspections and renounce the right to conduct peaceful nuclear explosions. Even though it was disregarded at the time, these are the core ideas behind the creation of the Brazilian–Argentine Agency for Accounting and Control of Nuclear Materials (ABACC) established in 1991. This article, then, seeks to fill the gaps in what today constitutes an unknown episode in the dense nuclear nonproliferation history of the 1970s.     

Non-destructive characterization of archeological Cu-based artifacts from the early metallurgy of southern Portugal

In this study, Monte Carlo (MC) simulations combined with energy dispersive X-ray fluorescence (EDXRF) spectroscopy have been used to characterize non-destructively a collection of Cu-based artifacts recovered from two archeological sites in southern Portugal: (a) the Chalcolithic E.T.A.R. site of Vila Nova de Mil Fontes and (b) the Middle Bronze Age site of Quinta do Estácio 6. The metal artifacts show a multilayered structure made up of three distinct layers: (a) brownish carbonate soil-derived crust, (b) green oxidized corrosion patina, and (c) bulk metal. In order to assess the reliability of the EDXRF-based Monte Carlo simulations to reproduce the composition of the alloy substrate in archeological bronze artifacts without the need to previously remove the superficial corrosion and soil derived patinas, EDXRF analysis together with scanning electron microscopy with energy dispersive X-ray spectroscopy (SEM-EDS) was also performed on cleaned and patina-/crust-coated areas of the artifacts. Characterization of the mineralogical composition of the corrosion products in the surface patinas was further determined by means of X-ray diffraction (XRD). Results suggest that the adopted EDXRF/Monte Carlo protocol may represent a safe and fast analytical approach in the quantitative characterization of the bulk chemical composition of Cu-based metal artifacts even in the presence of fairly thick corrosion patinas and/or soil-derived encrustations at the surface of the archeological objects.     

A 5th‐Century‐AD Sewn‐Plank River Barge at St Maria in Padovetere (Comacchio‐FE), Italy: an interim report

This article reports on the remains of a 5th‐century‐AD river barge excavated in 2014 and 2015. Most of the flat bottom and one side are preserved. The barge is at least 20 m in length and 2.9 m across the floor, and is constructed using sewn planks, iron nails and mortise‐and‐tenon fasteners. Both flush‐laid and lapstrake planks are recorded. Archaeological, historical, iconographic and ethnographic evidence is used to propose explanations for features, such as the use of lapstrakes, a possible steering system and platform, and the likely position of a pump, while setting the barge in the context of the North Adriatic shipbuilding tradition.     

Immunological evidence of Plasmodium falciparum infection in an Egyptian child mummy from the Early Dynastic Period

A 15–18 months old child mummy, presently housed in Turin's Museum of Anthropology, was discovered in Gebelein (Upper Egypt) during excavations carried out by the Missione Archeologica Italiana, most likely in 1914.     

Mesowear as a means of determining diets in African antelopes

Analysis of dental mesowear is a useful tool to examine dietary strategies in ungulates, and provides a palaeoenvironmental proxy at archaeological and palaeontological sites. We examine the distribution of traditional qualitative mesowear variables amongst 33 species of extant African antelope. We also examine the relationship of our dataset with the original dataset of Fortelius and Solounias (2000). We find that confining mesowear analyses to antelope species alone reduces their discriminating power relative to that found in analyses using a broader range of taxa. Variability in mesowear scores along the toothrow suggest that different teeth do not wear equivalently over an individual’s life-time, so it is important to confine comparisons to individual tooth positions for palaeodietary classifications. Mesowear scores from the third upper molar were found to have the greatest discriminating power. Frugivores displayed unique mesowear signatures, suggesting that this trophic guild should be taken into consideration separately in future mesowear analyses. These results have implications which can improve the application and the discriminatory power of mesowear analyses for the determination of the palaeodiets of extinct taxa, and, by extension, their palaeoenvironments.     

Oxygen isotopic composition of limpet shells from the Beagle Channel: implications for seasonal studies in shell middens of Tierra del Fuego

Shell middens distributed along the coastal areas of the Beagle Channel (Tierra del Fuego) testify the primary role of marine resources in the successful social dynamic of hunter–gatherer–fisher societies (HGF) in extreme high latitude environmental conditions. Intertidal and subtidal limpet species are frequently identified taxa of these archaeological deposits. We investigated whether shell δ¹⁸O of the limpet species Nacella deaurata is a valuable record of local sea surface temperature (SST) and ambient water δ¹⁸O (δ¹⁸Ow) fluctuations, and in turn can be used to estimate the season of its exploitation by Holocene HGF. Sequential shell δ¹⁸O of modern species track seasonal changes of SST and δ¹⁸Ow. The comparison of shell δ¹⁸O profiles of N. deaurata and Nacella magellanica (a coexisting species) suggests the occurrence of distinct growth rate and physiological adaptations between species. Shell δ¹⁸O of zooarchaeological specimens of N. deaurata from Lanashuaia II suggests that animals were exploited predominantly in winter and that experienced similar environmental conditions of present day at ∼1320 years BP. Results also indicate that N. deaurata is a valuable candidate for studying past seasonal changes in SST and δ¹⁸Ow in this southernmost part of South America.