Tiina Manne

Human occupation of northern Australia by 65,000 years ago

The time of arrival of people in Australia is an unresolved question. It is relevant to debates about when modern humans first dispersed out of Africa and when their descendants incorporated genetic material from Neanderthals, Denisovans and possibly other hominins. Humans have also been implicated in the extinction of Australia’s megafauna. Here we report the results of new excavations conducted at Madjedbebe, a rock shelter in northern Australia. Artefacts in primary depositional context are concentrated in three dense bands, with the stratigraphic integrity of the deposit demonstrated by artefact refits and by optical dating and other analyses of the sediments. Human occupation began around 65,000 years ago, with a distinctive stone tool assemblage including grinding stones, ground ochres, reflective additives and ground-edge hatchet heads. This evidence sets a new minimum age for the arrival of humans in Australia, the dispersal of modern humans out of Africa, and the subsequent interactions of modern humans with Neanderthals and Denisovans.

The archaeology, chronology and stratigraphy of Madjedbebe (Malakunanja II): A site in northern Australia with early occupation.

Published ages of >50 ka for occupation at Madjedbebe (Malakunanja II) in Australias north have kept the site prominent in discussions about the colonisation of Sahul. The site also contains one of the largest stone artefact assemblages in Sahul for this early period. However, the stone artefacts and other important archaeological components of the site have never been described in detail, leading to persistent doubts about its stratigraphic integrity. We report on our analysis of the stone artefacts and faunal and other materials recovered during the 1989 excavations, as well as the stratigraphy and depositional history recorded by the original excavators. We demonstrate that the technology and raw materials of the early assemblage are distinctive from those in the overlying layers. Silcrete and quartzite artefacts are common in the early assemblage, which also includes edge-ground axe fragments and ground haematite. The lower flaked stone assemblage is distinctive, comprising a mix of long convergent flakes, some radial flakes with faceted platforms, and many small thin silcrete flakes that we interpret as thinning flakes. Residue and use-wear analysis indicate occasional grinding of haematite and woodworking, as well as frequent abrading of platform edges on thinning flakes. We conclude that previous claims of extensive displacement of artefacts and post-depositional disturbance may have been overstated. The stone artefacts and stratigraphic details support previous claims for human occupation 50-60 ka and show that human occupation during this time differed from later periods. We discuss the implications of these new data for understanding the first human colonisation of Sahul.

Prying New Meaning from Limpet Harvesting at Vale Boi During the Upper Paleolithic

The late Pleistocene record for human exploitation of marine resources is generally accepted as being underrepresented world-wide. The global lowering of sea levels during the last glacial maximum (LGM) extended coastlines, presumably causing much of the evidence for coastal living from that period to be inundated today. The southern coast of Iberia is no exception, having a gently sloping, submerged continental shelf along much of its coastline. During the LGM, this continental shelf would have been partially exposed, with the coastal shore lying a considerable distance south of where it is today. This set of circumstances has no doubt contributed to the lack of known Upper Paleolithic coastal sites in southern Iberia containing records of marine exploitation. However, two key southern Iberian sites provide evidence of long-term marine resource use in this region: Cueva de Nerja and Vale Boi. The southeastern Spanish site of Cueva de Nerja is known for its record of marine fish and shellfish exploitation beginning in the Solutrean (Cortes-Sanchez et al. 2008; Jorda 1986; Morales and Rosello 2008; Serrano et al. 1995). Now the Portuguese site of Vale Boi significantly adds to the evidence of long-term utilization of coastal resources, with its record of marine resource exploitation beginning in the Gravettian.

Coastal feasts: a Pleistocene antiquity for resource abundance in the maritime deserts of north west Australia?

ABSTRACT Located on the edge of Australias North West continental shelf, Barrow Island is uniquely located to address a number of research questions, such as the antiquity and changing nature of Indigenous occupation, including shifting uses of regional economic resources in response to post-glacial sea-level rise. These questions are addressed from a range of archaeological, zooarchaeological, and geoarchaeological disciplines. Although only preliminary, results to date indicate the presence of marine resources dating to before sea-level stabilization (∼ 7.5 ka) that contain both dietary and utilitarian species, including high-ranked species such as sea turtle. The marine assemblages reflect a variety of habitats and substrates with a 17,000-year record for the presence of a former tidal marsh or estuary. We also note recently obtained 14C and OSL dates that extend the dietary marine faunas and initial occupation to well before 41 ka. This demonstrates that consumption of coastal resources began prior to the Holocene, when we begin to observe more widespread evidence of marine resource exploitation in the broader Canarvon Bioregion of northwest Australia. This evidence supports arguments for further research to directly test both the productivity of, and human reliance on, marine habitats from initial occupation.

To the islands born: The research potential of submerged landscapes and human habitation sites from the islands of NW Australia

Abstract This paper focuses on the continental shelf of NW Australia, and on models for change in littoral and offshore environments of relevance to human occupation over the last 50 kyr. Major island groups occur on the shelf including the Montebello and Barrow islands, and those of the Dampier Archipelago. At lowest sea level around 22 ka, these would have been uplands that then became progressively isolated by subsequent sea-level rise. By integrating archaeological and zooarchaeological records from excavations on these islands with the geology and geomorphology, we interpret palaeoeconomic resource potential in relation to changing sea level and coastline morphology. The preservation potential for submerged archaeological sites and features is also assessed. Current archaeological evidence from these offshore islands indicates that the submerged coastal landscape is likely to have been a potentially rich environment for resources and human occupation, even at times of lowest sea level and regional aridity. Should any exploration of submerged archaeology be carried out in this region, it is likely to be rewarding, offering unique insights into Late Pleistocene coastal occupation.