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Seaborne movement underpins frontier research in prehistoric archaeology, including water-crossings in the context of human dispersals, and island colonisation. Yet, it also controls the degree of interaction between locations, which in turn is essential for investigating the properties of maritime networks. The onset of the Holocene (circa 12,000 years ago) is a critical period for understanding the origins of early visitors/inhabitants to the island of Cyprus in the Eastern Mediterranean in connection with the spread of Neolithic cultures in the region. The research undertaken in this work exemplifies the synergies between archaeology, physical sciences and geomatics, towards providing novel insights on the feasibility of drift-induced seaborne movement and the corresponding trip duration between Cyprus and coastal regions on the surrounding mainland. The overarching objective is to support archaeological inquiry regarding the possible origins of these visitors/inhabitants—Anatolia and/or the Levant being two suggested origins. [ABSTRACT FROM AUTHOR]

The environmental extremes of the Last Glacial Maximum and the subsequent warming and sea-level rise into the Holocene had profound implications for human behavior across much of the world. In northern New Guinea, the Maluku Islands, and the Philippines, shell adzes appear during this period alongside contact between islands. In this paper we present new data from the site of Asitau Kuru, Timor-Leste, to show that the creation of shell adzes and greater inter-island connectivity also characterizes the early and middle and early Holocene in the Nusa Tenggara archipelago of southern Wallacea. We suggest that one of the functions of these shell adzes was in making dugout canoes enabling regular access to neighboring islands; the import of exotic stone materials; long-term occupation of very small islands; and, with new hook and line technology, the capture of more fish. This evidence predates the Neolithic in the region and corroborates a linguistic hypothesis that there was a pre-Austronesian interaction sphere covering much of Wallacea. [ABSTRACT FROM AUTHOR]

This study analysed over 1000 obsidian stone artefacts excavated from two adjoining shelters at Tron Bon Lei on Alor Island Indonesia using portable XRF. The study showed an unambiguous separation of three different source locations (Groups 1, 2 and 3). Two sources (Group 2 and 3a, b, c) dominate the assemblage numerically. Group 1 and 2 indicate use of a single volcanic formation with a strong match between Group 1 artefacts and artefacts from sites in Timor Leste. Obsidian occurs in the earliest occupation layer in the Alor sites but does not include Group 1 artefacts which occur only after approx. 12,000 cal BP. Currently the geographical location of the Group 1 outcrop is unknown, however, based on the late appearance of the Group 1 artefacts in the Alor sequence it is likely that the location is not on Alor, but rather on another island of the Sunda chain. The dating of Group 1 artefacts in widely spaced sites on the never geographically connected islands of Timor and Alor indicates that maritime interaction between islands began by at least the terminal Pleistocene. The distribution of the obsidian in Tron Bon Lei shelter Pit B shows that there were periods of more intense interaction punctuated by periods when interaction declined or ceased. [ABSTRACT FROM AUTHOR]

The role of AD 1300 climate change in widespread societal change in Palau and the Pacific Basin has recently been debated by Fitzpatrick (2010, 2011) and Nunn and Hunter-Anderson (2011). The central proposition examined here is the link between a sea-level driven food crisis and the outbreak of conflict, which is hypothesized in the AD 1300 event model to have led people to shift from unprotected coastal parts of large islands (e.g. volcanic Babeldaob) to more readily defensible offshore islands (e.g. limestone 'Rock Islands') during the transition between the Medieval Warm Period (MWP) and the Little Ice Age (LIA). Revision of radiocarbon dates from village sites in the Rock Islands suggests instead that permanent settlements were established on small offshore islands during the MWP with village abandonment during the LIA. Palaeoclimate records from equatorial islands show that during the LIA Palau had less rainfall from the southward movement of the Intertropical Convergence Zone (ITCZ). The abandonment of multiple limestone islands by a population estimated at 4000-6000 people may have been influenced by decreased precipitation and more tentatively from a decline in near-shore marine foods as a result of sea-level fall. [ABSTRACT FROM AUTHOR]

Abstract: This paper discusses new evidence of long-distance interaction networks in Island Southeast Asia obtained from geochemical analyses using SEM-EDXA and LA-ICPMS of 101 obsidian samples from 25 locations including seven obsidian sources and 19 archaeological sites. Given that there are obsidian sources distributed throughout much of Island Southeast Asia, the potential for obsidian studies to provide greater understanding of patterns of mobility and exchange in the Pre-Neolithic and Neolithic periods would seem to be considerable. This potential, however, remains largely unrealised as obsidian sourcing has hitherto only been carried out intermittently in Island Southeast Asia using PIXE-PIGME, XRF and other methods. [Copyright &y& Elsevier]

Abstract: This paper summarises research on obsidian findings across the region of Island Southeast Asia (ISEA), from the first reporting of obsidian on Sumatra as a result of cave excavations in the early 1900s through to the latest published discoveries in 2009. These results are the background for the first region-wide research project focussing on obsidian characterisation and its role in prehistoric inter-island exchange. It is commonly held that distribution of obsidian in ISEA was only localised and inter-island transportation limited. The review, however, suggests that this hypothesis derives from an incomplete knowledge of obsidian distribution in the region rather than typifying prehistoric social patterns. Obsidian sourcing has been carried out only intermittently in ISEA since the 1970s and has generally been focussed only at the single site level, thus explaining this very partial understanding. [Copyright &y& Elsevier]

Aboriginal manufacture and use of pottery was unknown in Australia prior to European settlement, despite well-known ceramic-making traditions in southern Papua New Guinea, eastern Indonesia, and the western Pacific. The absence of ancient pottery manufacture in mainland Australia has long puzzled researchers given other documented deep time Aboriginal exchange networks across the continent and the close proximity of pottery-bearing Lapita and post-Lapita maritime communities in the western Pacific with ocean-going watercraft and sophisticated navigation abilities. We report the oldest securely dated ceramics found in Australia from archaeological excavations on Jiigurru (Lizard Island Group) on the Great Barrier Reef, northeast Australia. Comprehensive radiocarbon dating and Bayesian modelling constrains ceramic deposition to between 2950–2545 cal BP and 1970–1815 cal BP. This timing overlaps with late Lapita and post-Lapita ceramic traditions of southern Papua New Guinea. Geological characterisation of the sherds strongly suggests local manufacture as the vessels belong to three temper and clay groups locally sourced to northeast Australia, and most likely to Jiigurru. The oldest occupation layers date to 6510–5790 cal BP, making Jiigurru the earliest offshore island occupied on the northern Great Barrier Reef. The results demonstrate that northeast Australian First Nations communities had sophisticated canoe voyaging technology and open-sea navigational skills and were intimately engaged in ancient maritime networks, connecting them with peoples, knowledges, and technologies across the Coral Sea region. • We report the oldest securely dated ceramics found in Australia. • Earliest known offshore island occupation on the northern Great Barrier Reef. • Ceramic analysis suggests local raw material sources and manufacture. • Results demonstrate that Australia was intimately engaged in ancient maritime networks. [ABSTRACT FROM AUTHOR]