Austronesian speaking peoples left Southeast Asia and entered the Western Pacific c.4000-3000 years ago, continuing on to colonise Remote Oceania for the first time, where they became the ancestral populations of Polynesians....
moreAustronesian speaking peoples left Southeast Asia and entered the Western Pacific c.4000-3000 years ago, continuing on to colonise Remote Oceania for the first time, where they became the ancestral populations of Polynesians. Understanding the impact of these peoples on the mainland of New Guinea before they entered Remote Oceania has eluded archaeologists. New research from the archaeological site of Wañelek in the New Guinea Highlands has broken this silence. Petrographic and geochemical data from pottery and new radiocarbon dating demonstrates that Austronesian influences penetrated into the highland interior by 3000 years ago. One potsherd was manufactured along the northeast coast of New Guinea, whereas others were manufactured from inland materials. These findings represent the oldest securely dated pottery from an archaeological context on the island of New Guinea. Additionally, the pottery comes from the interior, suggesting the movements of people and technological practices, as well as objects at this time. The antiquity of the Wañelek pottery is coincident with the expansion of Lapita pottery in the Western Pacific. Such occupation also occurs at the same time that changes have been identified in subsistence strategies in the archaeological record at Kuk Swamp suggesting a possible link between the two.
The south Papuan coast has seen a rapid transition in cultural changes during the late Holocene. Colonisation by the sea-faring Lapita people almost 3000 years ago is the earliest evidence of ceramic producing people in the region....
moreThe south Papuan coast has seen a rapid transition in cultural changes during the late Holocene. Colonisation by the sea-faring Lapita people almost 3000 years ago is the earliest evidence of ceramic producing people in the region. Subsequent cultural development in the region led to the highly specialised exchange systems of the ethnographic period, such as the Motu Hiri. A poorly understood period during this sequence is the so-called "Papuan Hiccup" (c. 750-1150AD), during which a series of abrupt, localised socio-economic changes occurred along the entire coast. The Papuan Hiccup separates an early ceramic period, in which Lapita-derived Early Papuan Pottery (EPP) traditions are found at sites right across the region, and a more recent phase of localised ceramic sequences. A correspondence between the timing of the Papuan Hiccup and a peak in El-Niño Southern Oscillation (ENSO) activity suggests a mechanism for this cultural transformation. This paper contributes new d...
... 2009 doi: 10.2984/049.063.0402. On the Rat Trail in Near Oceania: Applying the Commensal Model to the Question of the Lapita Colonization 1. E. Matisoo-Smith, 2, 4, 7 M. Hingston, 3, 4 G. Summerhayes, 5 J. Robins, 2, 4 HA Ross, 3 and...
more... 2009 doi: 10.2984/049.063.0402. On the Rat Trail in Near Oceania: Applying the Commensal Model to the Question of the Lapita Colonization 1. E. Matisoo-Smith, 2, 4, 7 M. Hingston, 3, 4 G. Summerhayes, 5 J. Robins, 2, 4 HA Ross, 3 and M. Hendy 6. ... Bull. Am. Mus. Nat. Hist. ...
This paper uses strontium isotope (87Sr/86Sr), oxygen isotope (δ18O) and Ba/Sr trace element data in archaeological tooth enamel samples to investigate migration and mobility at the Late Lapita site of SAC, Watom Island in the Bismarck...
moreThis paper uses strontium isotope (87Sr/86Sr), oxygen isotope (δ18O) and Ba/Sr trace element data in archaeological tooth enamel samples to investigate migration and mobility at the Late Lapita site of SAC, Watom Island in the Bismarck Archipelago. Previous archaeological models have identified Lapita mobility at a community level using obsidian distribution patterns and changes in ceramic design, whereas isotope and trace element data can potentially reconstruct prehistoric mobility on an individual level. Human and pig teeth were sampled from SAC and a selection of human teeth were included from the Late–Post Lapita site of Lifafaesing, Tanga Islands as a geographic/geological comparison.The results indicate that there is a large amount of isotopic variation in the Bismarck Archipelago which is useful for identifying non-local individuals and possibly determining their origins. One human individual and several pigs were suggested as coming from elsewhere in the region. Three potentially separate locations were identified for the non-local pigs. It is argued, using the data from SAC, that Late Lapita communities in the Bismarck Archipelago were more mobile than previously assumed. The potential for identifying individual migrants in a Lapita context are discussed in terms of assessing the more subtle aspects of Lapita society in the Southwest Pacific Islands.
In 2007 a new Early Lapita site called Tamuarawai (EQS) was located on Emirau Island, Papua New Guinea. Two seasons of excavation (2007, 2008) have been undertaken. This paper describes the site and some of the preliminary analyses...
moreIn 2007 a new Early Lapita site called Tamuarawai (EQS) was located on Emirau Island, Papua New Guinea. Two seasons of excavation (2007, 2008) have been undertaken. This paper describes the site and some of the preliminary analyses undertaken. Some unusual results suggest ...
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...
moreThis 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.
After their emergence by 200,000 years before the present in Africa, modern humans colonized the globe, reaching Australia and New Guinea by 40,000 to 50,000 years ago. Understanding how humans lived and adapted to the range of...
moreAfter their emergence by 200,000 years before the present in Africa, modern humans colonized the globe, reaching Australia and New Guinea by 40,000 to 50,000 years ago. Understanding how humans lived and adapted to the range of environments in these areas has been difficult because well-preserved settlements are scarce. Data from the New Guinea Highlands (at an elevation of ~2000 meters) demonstrate the exploitation of the endemic nut Pandanus and yams in archaeological sites dated to 49,000 to 36,000 years ago, which are among the oldest human sites in this region. The sites also contain stone tools thought to be used to remove trees, which suggests that the early inhabitants cleared forest patches to promote the growth of useful plants.
... Obsidian sources at Mopir, West New Britain Province, Papua New Guinea Richard Fullagar, Glenn Summerhayes, Baiva Ivuyoand Jim Specht Abstract ... Changes through time in relative proportions of obsidian from Lou Island, Talasea and...
more... Obsidian sources at Mopir, West New Britain Province, Papua New Guinea Richard Fullagar, Glenn Summerhayes, Baiva Ivuyoand Jim Specht Abstract ... Changes through time in relative proportions of obsidian from Lou Island, Talasea and Mopir suggest fluctuations in ...
This paper emphasises sub-regional variation in the timing and nature of subsistence changes in the New Guinea Highlands at the Pleistocene–Holocene transition. An analysis of the Kiowa lithic assemblage was used to examine the interplay...
moreThis paper emphasises sub-regional variation in the timing and nature of subsistence changes in the New Guinea Highlands at the Pleistocene–Holocene transition. An analysis of the Kiowa lithic assemblage was used to examine the interplay between tool technology, mobility levels, and subsistence strategies by investigating changes in the procurement, manufacture, and use of different raw stone materials in an overall lithic technology. Throughout Kiowa’s occupation local stone was used extensively, and over time people increased their knowledge of the local lithic landscape, using more diverse local raw materials. Since the terminal Pleistocene, people carried reliable polished axes for a variety of activities and made expedient use of locally abundant river pebbles, while smaller nodules were located and carried as mobile toolkits to facilitate longer distance hunting and collecting excursions. In the mid Holocene exotic raw materials were also traded from more distant zones. The abandonment of Kiowa in the late Holocene shows that hunting became less economically important as cultivation developed in the area. Technological changes, in combination with changes in faunal remains are suggestive of increasing activ- ity at Kiowa through the Holocene as the site became specialised for bat hunting, perhaps driven by restricted land use and reduced mobility, reciprocally affected by increasing populations and the inten- sification of plant food production in the Highlands generally. Despite this, evidence for changes to hor- ticulture around Kiowa itself, in the Chimbu area, is limited to the mid-late Holocene, indicating that the early development of agriculture in the Wahgi may have been relatively localised, and did not necessarily displace existing subsistence strategies elsewhere in the Highlands.
The natural occurrence of obsidian in volcanic flows in West New Britain has been thoroughly investigated and new measurements of the composition of field samples have been made with a proton dose of 150 µC, increased by a factor of three...
moreThe natural occurrence of obsidian in volcanic flows in West New Britain has been thoroughly investigated and new measurements of the composition of field samples have been made with a proton dose of 150 µC, increased by a factor of three compared to ...
... Obsidian sources at Mopir, West New Britain Province, Papua New Guinea Richard Fullagar, Glenn Summerhayes, Baiva Ivuyoand Jim Specht Abstract ... Changes through time in relative proportions of obsidian from Lou Island, Talasea and...
more... Obsidian sources at Mopir, West New Britain Province, Papua New Guinea Richard Fullagar, Glenn Summerhayes, Baiva Ivuyoand Jim Specht Abstract ... Changes through time in relative proportions of obsidian from Lou Island, Talasea and Mopir suggest fluctuations in ...