A Holocene record of savanna vegetation dynamics in southern lowland Papua New Guinea

The southern lowlands of Papua New Guinea (PNG) are biogeographically distinct. Vast tracts of savanna vegetation occur there and yet most palaeoecological studies have focused on highlands and/or forest environments. Greater focus on long-term lowland environments provides a rare opportunity to understand and promote the significance of local and regional savannas, ultimately allowing non-forested and forested ecosystem dynamics to be compared. This paper examines palaeoecological and archaeological data from a lowland open savanna site situated on the south-central PNG coastline. The methods used incorporate pollen and micro-charcoal analyses, artefact recovery and sediment descriptions. We conclude with an environmental model of sedimentation and vegetation change for the past c. 5,800 years, revealing a mid to late Holocene savanna interchange between herbaceous and woody plant growth, with fluctuating fire occurrence increasing toward the present day. Increased silt deposition and modified regional hydrology are also recorded. Environmental changes correspond in timing with the start of permanent settlements and human use of fire. In particular, landscape burning for hunting and gardens for agriculture have helped create the open ecosystem still evident today

Geomorphological context and formation history of Cloggs Cave: What was the cave like when people inhabited it?

New research undertaken at Cloggs Cave, in the foothills of the Australian Alps, employed an integrated geological-geomorphological-archaeological approach with manifold dating methods and fine resolution LiDAR 3D mapping. Long-standing questions about the site's chronostratigraphy (e.g. the exact relationship between basal megafaunal deposits and archaeological layers), sedimentation processes and geomorphic changes were resolved. The cave's formation history was reconstructed to understand its changing morphology and morphogenic processes, and to clarify how these processes shaped the cave's deposits. Key findings include the identification of: 1) the geomorphological processes that caused the lateral juxtaposition of 52,000 year-old megafaunal and later occupational layers; 2) the existence of one and possibly two (now-buried) palaeo-entrance(s) that enabled now-extinct megafauna and extant large fauna to enter the cave, most likely via a free-roaming passage rather than a pit drop; 3) morphological changes to the cave during the time of the Old People, including the timing of changes to the inclination of palaeo-surfaces; and 4) modifications to stalactites, crushing of calcite formations for the manufacture of powder, construction of a stone arrangement, and movement of large limestone blocks by the Old People. Ultimately, these findings demonstrate that to properly understand what Cloggs Cave was like when the Old People visited the site requires the construction of a narrative that spans some 400 million years and the development of an approach capable of integrating the many scales and processes (e.g. geological, geomorphological, archaeological) that configured to shape the site

Interpreting the mammal deposits of Cloggs Cave (SE Australia), GunaiKurnai Aboriginal Country, through community-led partnership research

Palaeontological animal bone deposits are rarely investigated through research partnerships where the local First Nations communities have a defining hand in both the research questions asked and the research processes. Here we report research undertaken through such a partnership approach at the iconic archaeological site of Cloggs Cave (GunaiKurnai Country, East Gippsland), in the southern foothills of SE Australia's Great Dividing Range. A new excavation was combined with detailed chronometric dating, high-resolution 3D mapping and geomorphological studies. This allowed interpretation of a sequence of stratigraphic layers spanning from a lowermost excavated mixed layer dated to between 25,640 and 48,470 cal BP, to a dense set of uppermost, ash layers dated to between 1460 and 3360 cal BP. This long and well-dated chronostratigraphic sequence enabled temporal trends in the abundant small mammal remains to be examined. The fossil assemblage consists of at least 31 taxa of mammals which change in proportions through time. Despite clear evidence that the Old Ancestors repeatedly carried vegetation into the cave to fuel cool fires (no visible vegetation grows in Cloggs Cave), we observed little to no evidence of cooking fires or calcined bone, suggesting that people had little involvement with the accumulation of the faunal remains. Small mammal bones were most likely deposited in the cave by large disc-faced owls, Tyto novaehollandae (Masked Owl) or Tyto tenebricosa (Sooty Owl). Despite being well dated and largely undisturbed, the Cloggs Cave assemblage does not appear to track known Late Quaternary environmental change. Instead, the complex geomorphology of the area fostered a vegetation mosaic that supported mammals with divergent habitat preferences. The faunal deposit suggests a local ancestral landscape characterised by a resilient mosaic of habitats that persisted over thousands of years, signalling that the Old Ancestors burned landscape fires to encourage and manage patches of different vegetation types and ages within and through periods of climate change

Moiapu 3: Settlement on Moiapu Hill at the very end of Lapita, Caution Bay hinterland

The Caution Bay archaeological project on the south coast of mainland Papua New Guinea has excavated 122 sites over a 9 km² area. Lapita ceramics appear at a number of sites at c. 2900 cal. BP. Here we present the results of excavations at Moiapu 3, a site that helps define the end of the dentate-stamped Lapita phase of this region. It is suggested that the decline and ultimate cessation of dentate stamping related to a loss of symbolism during a period of major socioeconomic readjustment and innovation

Ruisasi 1 and the earliest evidence of mass-produced ceramics in Caution Bay (Port Moresby region), Papua New Guinea

The history of pottery use along the south coast of Papua New Guinea spans from Lapita times, here dated to 2900–2600 cal BP, through to mass production of pottery associated with a number of ethnographically-known interaction (and exchange) networks. Understanding the antecedents and developmental histories of these interaction networks is of considerable importance to archaeological research from local to western Pacific geographical scales. The archaeological site of Ruisasi 1 located at Caution Bay near Port Moresby provides new insights into scales of pottery production before the development of the regional Motu hiri exchange system within the past 500 years. Here faunal remains indicate occupation by marine specialists who exploited a diverse range of local marine environments. Nearly 20,000 ceramic sherds are present in Square A, mostly from a 26 cm thick ‘pottery midden’. A minimum of 45 red slip/plainware vessels based on conjoined sets of sherds plus two vessels with incised decoration are present; the maximum number of clay vessels based on Fabric Types is 155. The globular red slip/plainware pots have highly standardized shapes and sizes, consistent with mass pottery production. The concentration of sherds from these pots within the pottery midden reflects short-duration depositional events within the period of village life c. 1630–1220 cal BP. Whether or not the pots were made locally or imported is the subject of ongoing research. Whatever the case, Ruisasi 1 raises the possibility of mass pottery production possibly linked to a regional interaction network pre-dating the hiri

Geomorphological context and formation history of Cloggs Cave: What was the cave like when people inhabited it?

New research undertaken at Cloggs Cave, in the foothills of the Australian Alps, employed an integrated geological-geomorphological-archaeological approach with manifold dating methods and fine resolution LiDAR 3D mapping. Long-standing questions about the site’s chronostratigraphy (e.g. the exact relationship between basal megafaunal deposits and archaeological layers), sedimentation processes and geomorphic changes were resolved. The cave’s formation history was reconstructed to understand its changing morphology and morphogenic processes, and to clarify how these processes shaped the cave’s deposits. Key findings include the identification of: 1) the geomorphological processes that caused the lateral juxtaposition of 52,000 year-old megafaunal and later occupational layers; 2) the existence of one and possibly two (now-buried) palaeo-entrance(s) that enabled now-extinct megafauna and extant large fauna to enter the cave, most likely via a free-roaming passage rather than a pit drop; 3) morphological changes to the cave during the time of the Old People, including the timing of changes to the inclination of palaeo-surfaces; and 4) modifications to stalactites, crushing of calcite formations for the manufacture of powder, construction of a stone arrangement, and movement of large limestone blocks by the Old People. Ultimately, these findings demonstrate that to properly understand what Cloggs Cave was like when the Old People visited the site requires the construction of a narrative that spans some 400 million years and the development of an approach capable of integrating the many scales and processes (e.g. geological, geomorphological, archaeological) that configured to shape the site

Sediment mixing at Nonda Rock: investigations of stratigraphic integrity at an early archaeological site in northern Australia and implications for the human colonisation of the continent

Archaeological excavations in sediments dating to between 60 000 and 40 000 years ago are rare in Australia. Yet this is precisely the period in which most archaeologists consider that Aboriginal people arrived on the continent. In the few cases where such early sites have been investigated, questions have invariably been raised as to the reliability of stratigraphic associations between cultural items and the surrounding sediments. This paper describes a method for examining sediment mixing in a stratigraphic sequence using the optically stimulated luminescence (OSL) signals from individual sand-sized grains of quartz. We apply this method to the archaeological site of Nonda Rock (north Queensland), in combination with radiocarbon dating of charcoal fragments, to construct chronologies for human occupation and for the preceding, culturally sterile, deposits. Our age estimates have implications for the timing of first human arrival in Australia. Copyright © 2007 John Wiley & Sons, Ltd.Bruno David, Richard G. Roberts, John Magee, Jerome Mialanes, Chris Turney, Michael Bird, Chris White, L. Keith Fifield, John Tibb

Imported obsidian at Caution Bay, south coast of Papua New Guinea: cessation of long distance procurement c. 1,900 cal BP

Until now, the evidence for imported obsidian along the south coast of Papua New Guinea has been limited to eleven excavated sites all dating after c. 2,000 cal. BP. Here we present new archaeological evidence for the sourcing and importation of 4,689 obsidian artefacts from 30 excavated sites at Caution Bay. pXRF analysis of a sample of the artefacts revealed that all but one came from a source on West Fergusson Island some 670 km away. During Lapita (here beginning c. 2,950 cal. BP) and post-Lapita times, the proportion of sites with obsidian artefacts was high, and remained so for a thousand years before suddenly ceasing c. 1,900 cal. BP. Technological analyses of obsidian artefacts from Bogi 1 and ABKL—the richest obsidian sites at Caution Bay—indicate intense unipolar and bipolar reduction and the occasional recycling of unipolar flakes into bipolar cores during both Lapita and post-Lapita times. We suggest that this is a result of the importation of obsidian to Caution Bay through down-the-line exchange

Agila and the reanimation of seafaring on the south coast of Papua New Guinea after 770 cal BP

Seafaring ceramicists connected widely spaced communities along the expanse of PNG’s south coast for more than 1,500 years following the arrival of people using pots with Lapita decoration c.2,900 cal BP. Archaeological investigations at locations from the Gulf of Papua in the west to Mailu Island in the east suggest a major change occurred to seafaring and social relations after 1,200 cal BP. The following five centuries often referred to as the ‘Ceramic Hiccup’ were characterised by a contraction in the scale of formerly long-distance voyaging. Here we present results of recent archaeological excavations at the ancestral village site of Agila in Hood Bay east of Port Moresby. The decorations on older pot sherds at Agila are akin to those on ancestral Motu pottery known from Motupore Island to the west. The decoration changes on more recent sherds which have more in common with ancestral Mailu pottery from Mailu Island to the east. Details of changing seafaring relations–from west to east–at Agila were published in 2018 after our first field season. However, results from the first field season left questions about site antiquity unresolved. We returned to Agila in 2022 and continued excavations to address those questions. Our excavations revealed that initial settlement at Agila coincided with a reanimation of coastal seafaring after 770 cal BP. Results also show that the major pottery manufacturing and seafaring community of Motupore maintained relations with communities to both the east and west. An analysis of the ceramic assemblage allows us to historicise the emergence of social strategies which entrenched Hood Bay at a nexus between Motu and Mailu specialised trading and seafaring communities.</p

New direction in human colonisation of the Pacific: Lapita Settlement of South Coast New Guinea

Expansion of Austronesianspeaking peoples from the Bismarck Archipelago out into the Pacific commencing c.3300 cal BP epresents the last great chapter of human globalcolonisation. The earliest migrants were bearers of inelymade dentate-stamped Lapita pottery, hitherto found only across Island Melanesia and western Polynesia. We document the first known occurrence of Lapita n the New Guinea mainland. The new Lapita sites date from 2900 to 2500 cal BP and represent a newly-discovered migratory arm of Lapita expansions that moved westwards along the southern New Guinea coast towards Australia. These marine specialists ate shellfish, fish and marine turtles along the Papua New Guinea mainland coast, flecting subsistence continuities with local pre-Lapita peoples dating back to 4200 cal BP. Lapita artefacts include characteristic ceramics, shell armbands, stone adzes and obsidian tools. Our Lapita discoveries support hypotheses for the migration of pottery-bearing Melanesian marine specialists into Torres Strait of northeast Australia c.2500 cal B