Mass Migration and the Polynesian Settlement of New Zealand

This paper reintroduces the concept of mass migration into debates concerning the timing and nature of New Zealand’s settlement by Polynesians. Upward revisions of New Zealand’s chronology show that the appearance of humans on the landscape occurred extremely rapidly, and that within decades settlements had been established across the full range of climatic zones. We show that the rapid appearance of a strong archaeological signature in the early 14th century AD is the result of a mass migration event, not the consequence of gradual demographic growth out of a currently unidentified earlier phase of settlement. Mass migration is not only consistent with the archaeological record but is supported by recent findings in molecular biology and genetics. It also opens the door to a new phase of engagement between archaeological method and indigenous Maori and Polynesian oral history and tradition.     

Tephrochronology,Environmental Change and the Norse Settlement of Iceland

Abstract

The first human impacts on the Icelandic environment came with the Norse colonisation or Landnám of the ninth century AD. The colonisation represents a fundamental environmental change that is both rapid and profound. In this paper we assess geomorphological dimensions of the initial settlement period using a tephrochronology that includes the Landnám Tephra, erupted ca. 870 AD, two tenth century AD tephras KR 920 and E 935, and 11 other well dated tephra layers. We report a new ¹⁴C age of 1676 ±12 ¹⁴C yr BP (cal AD 345 (400) 419) for the tephra SILK-YN which forms a key prehistoric marker horizon that constrains rates of environmental change in the centuries before Norse Settlement. Aeolian sediment accumulation rates show five geomorphological responses to settlement that differ in the rate and trajectory of change. These distinct anthropogenic signals are the result of spatially variable sensitivity to grazing and deforestation, and reflect the extent of local soil erosion. This critical erosion threshold is variable in space and time.     

Characterization of New Zealand obsidian using PXRF

New Zealand has some of the most active areas of rhyolitic volcanism in the world and this has produced numerous obsidian sources in the northern half of the North Island. In total archaeologists have recognized 27 named locations from which obsidian can be obtained scattered across 4 geological source regions. Shortly after colonization in the late 13th century AD Polynesian settlers began transporting this material some thousands of kilometers throughout the country and across the sea in small quantities to distant neighbors in the Kermadecs and Chatham islands. Although considerable research has been conducted on obsidian sourcing in New Zealand the complexity of geochemical source discrimination and the lack of a practical method of non-destructive geochemical analysis has hindered progress. We present the results of our use of PXRF to provide geochemical data on New Zealand obsidian sources and to compare the use of discriminant analysis and classification tree analysis to discriminate among sources and attribute archaeological samples to sources. Our research suggests that classification tree analysis is superior to discriminant analysis in sourcing studies. A large case study using an important settlement phase site (S11/20) from the Auckland region demonstrates the utility of the methods and the results support a model of high degrees of mobility and interaction during the early settlement of New Zealand.     

Microfossil evidence of land-use intensification in north Thailand

Palaeo-environmental data from accumulated lake sediments at Phayao, northwest Thailand, provide a record of vegetation and environmental change from approximately 20,000 years Before Present. This is an important region archaeologically, with claims in the 1970s for an ‘early’ transition to domestication having arisen from a number of cave sites. Multiple indices are used to determine if people had an observable impact on the natural environment, and to determine the timing and magnitude of impacts associated with the development of agricultural land use in the region. An initial increase in sedimentation rate is apparent from ca. mid-2nd C AD. Changes in phytoplankton concentrations are apparent from the late 3rd C AD, and evidence for initial forest disturbance is apparent from the 5th or 6th C AD, with impacts becoming more severe over time to reach a pre-modern maximum in the 11th to the 13th C AD. Changes in agricultural practices are apparent during the 14th C AD, with an increased emphasis on rice agriculture and incipient management of the regenerating forests. Based on these data we suggest that agricultural intensification in the early part of the 1st millennium AD destabilised catchment slopes, through clearance of dryland vegetation and swidden agriculture. There is no direct evidence for the impacts of earlier peoples on the vegetation of the area, which we take to indicate that agricultural intensification was later here than in the lowlands to the east and south.     

Critical development studies in the Anthropocene

In this short commentary, the ramifications of the Anthropocene for a broadly defined critical development studies are considered. The likely anthropogenic roots of increasing cyclonic intensity and associated impacts in the Pacific are drawn upon to propose four research agendas. The first focuses on how places are becoming connected through human‐induced changes to planetary systems. While direct causal relationships are difficult to draw, research efforts can highlight the disproportionate contributions particular development models, actors, and lifestyles are having on more distant socioecological systems. A second more conventional theme focuses on the uneven impacts of the Anthropocene on people and places, as well as on how development is practised and prioritised. A third theme explores how the Anthropocene can be used to retheorise development in creative and more‐than‐human ways, recognising non‐human agencies and the co‐production of development processes. A final agenda involves asking how critical development researchers can strategically use and repurpose the Anthropocene to pursue socially and environmentally progressive ends.     

Rethinking the Analysis of Ethnic Residential Patterns: Segregation,Isolation, or Concentration Thresholds in Auckland,New Zealand?

Data from the 1996 New Zealand Census on ethnicity in Auckland Urban Area are used to illustrate a new approach to measuring spatial separation. The traditionally employed single‐number indices are found wanting and a method based on thresholds is introduced. This provides more detailed information on the geography of ethnic groups that is consistent with the requirements for testing hypotheses regarding the relationship between social and spatial distance. The results show that (with a few exceptions) Polynesian groups were more encapsulated groups in Auckland than were Asian and European groups, and that most of the European groups—along with the “host society,” the New Zealand Europeans—were not spatially exposed to members of the Polynesian and Asian groups.     

Was there an early Polynesian ‘sky father’?∗

Abstract

There is a recurring Polynesian cosmogonic tradition whereby the primordial world was transformed into the modem world by a series of events often consisting first of vague cosmic beings (whose names and nature are not generally cognate) giving rise to a Primordial Pair who then gave rise to first order anthropomorphic gods. The Primordial Pair in Tonga were ‘Seaweed’ and ‘Sediment/Slime’ while in Nuclear Polynesian we find the female named Papa‐adj. and evidence for the male being named Papa‐adj. in Proto Nuclear Polynesian and Proto Central Eastern Polynesian as well. These are thought of as physical strata or rock in Samoa while in Central Eastern Polynesia there was commonly the notion that Papa (the female) was the earth itself and that her mate was the sky or the space between the sky and the earth. It was, however, only amongst New Zealand Maori that the male was specifically given the name ‘Sky’ although an alternative name for the male in the Marquesas is ‘Sky Parent’ but seems a (lexical) development independent of the N.Z. Maori.     

Economic re-colonisation: Financialisation,indigeneity and the epistemic violence of resolution

The 1998 Ngāi Tahu-Crown Te Tiriti o Waitangi-Treaty of Waitangi settlement represents a long battle for justice concerning Te Waipounamu (South Island) of Aotearoa, New Zealand. We focus on the resolution practices of the New Zealand Government and the impacts of financialising historic harm as economic techniques dominate the articulation of resolution. The paper challenges three main ideas. First, it illustrates a logical impossibility in a process of ‘resolution’ determined by the Crown. Second, it challenges the financialisation rhetoric applied in ‘resolving’ harm caused. Third, it challenges the imposition of economic control in requiring Ngāi Tahu to establish a corporate structure to be eligible to receive settlement. These three elements constitute ‘economic re-colonisation’ by denying alternative approaches to resolution and knowledge and consequently, the rhetoric of resolution constitutes ‘epistemic violence’.     

Ta‘isi O.F. Nelson and Sir Maui Pomare Samoans and Māori Reunited

ABSTRACT

This paper unearths the friendship between Samoan nationalist leader Ta‘isi Olaf Frederick Nelson and Māori politician Sir Maui Pomare during the early period of New Zealand's administration of Samoa. It examines the role this friendship played – especially as a line of communication between the Samoan protest movement or Mau, of which Nelson was a leader, and the highest echelons of the New Zealand government – in those years of fraught relations between Samoa and New Zealand. It also explores the significant historical connections that were made, or remade, through this friendship. The relationship between these two men brought Polynesian peoples together in new ways and also directly linked Parihaka, a 19th-century Māori community known for its non-violent resistance against European colonialism, with the later Samoan Mau.     

The boat grave studies of Sutton Hoo and Vendel ‐ A Palaeoenvironmental study

This study is part of the project ‘Vegetational development and land use during the pre‐Viking period. A comparative study of environmental history in northern Uppland, Sweden, and East Anglia, England’. The main aim of the project is to reconstruct the palaeoenvironments within the catchment areas of Lake Vendelsjön, northern Uppland, and the river Deben, East Anglia. The project employs a variety of palaeoecological methods such as sedimentation processes and rates, erosion levels, changes in sea level and climatic influences, the effects of land uplift and changes in land use. The time period covered by the project is the last 3000 years.     

Advances in Polynesian Prehistory: A Review and Assessment of the Past Decade (1993–2004)

The pace of archaeological research in Polynesia has intensified in recent years, resulting in more than 500 new literature citations over the past decade. Fieldwork has continued in such previously well-studied archipelagoes as Tonga and Samoa in Western Polynesia, and Hawai’i and New Zealand in Eastern Polynesia, and has expanded into previously neglected islands including Niue, the Equatorial Islands, the Austral Islands, and Mangareva. The emergence of Ancestral Polynesian culture out of its Eastern Lapita predecessor is increasingly well understood, and the chronology of Polynesian dispersal and expansion into Eastern Polynesia has engaged several researchers. Aside from these fundamental issues of origins and chronology, major research themes over the past decade include (1) defining the nature, extent, and timing of long-distance interaction spheres, particularly in Eastern Polynesia; (2) the impacts of human colonization and settlement on island ecosystems; (3) variation in Polynesian economic systems and their transformations over time; and (4) sociopolitical change, especially as viewed through the lens of household or microscale archaeology. Also noteworthy is the rapidly evolving nature of interactions between archaeologists and native communities, a critical aspect of archaeological practice in the region.

Pollen evidence for major shifts in forest composition since the mid‐nineteenth‐century in the vicinity of Sudbury,Ontario

Numerous anthropogenic stressors have impacted the region surrounding Sudbury, Ontario, leading to pronounced vegetation and landscape change. Few long‐term records exist to understand the nature or timing of this change. We use pollen analysis from radiometrically dated sediments of Clearwater Lake to compare pre‐ and post‐settlement vegetation. Beginning ～1850 CE, the record shows major shifts in forest composition, coincident with settlement and the beginnings of lumbering. These changes are unprecedented for the past ～5000 years, and consist of increases in diversity and abundance of deciduous tree taxa and herbaceous disturbance indicators. While evidence of mining appears as early as 1900 CE, little effect is seen in the pollen record until ～1930 CE, when sedimentation rates increased and acidification of the lake also began. At this time, further increases in palynological disturbance indicators and minimum sediment organic matter levels indicate the period of maximum vegetation loss. As a result of reduced emissions since the 1970s, water quality began to improve in Clearwater Lake and there are some decreases in the abundances of shade‐intolerant disturbance indicators in the pollen record. However, the fact that the pollen assemblages do not resemble those prior to 1850 suggests lasting vegetation changes.     

Dating bog bodies by means of 14C-AMS

We have made efforts to date a substantial number of bodies from northwest European peat bogs by means of ¹⁴C. In our research, we compared materials such as skin, hair, bone, textile, leather and wood where available. Most of the bodies we investigated were found to date from the Late Iron Age/Roman period (c. 2nd century BC–4th century AD). Our data set shows that bog bodies in general can indeed be successfully dated by means of ¹⁴C analysis. Our results contradict comments in the literature (e.g. C.S. Briggs, Did they fall or were they pushed? Some unresolved questions about bog bodies, in: R.C. Turner, R.G. Scaife (Eds.), Bog Bodies—New Discoveries and New Perspectives, British Museum Press, London, 1995, pp. 168–182) to the effect that ‘peat bogs can age corpses so as to distort completely the usefulness of Radiocarbon’.     

Evolution of Polynesian bark cloth and factors influencing cultural change

The origin and dispersal of the first human inhabitants of the Polynesian Triangle have been studied from many perspectives and significant progress in our understanding of Polynesian prehistory has derived from an intermingling of linguistics, archaeology, and genetics. Contributions from the ethnographic record, however, have been limited by the dearth of comparative methods that are useful for reconstructing prehistory and identifying and analyzing cross-cultural trends. For more than fifty years, cladistic phylogenetic methods have been used to reconstruct the evolutionary history of biological systems from contemporary trait distributions. These rigorous methods are applied herein to reconstruct the prehistoric evolution and dispersal of Polynesian bark cloth, using ethnographic data recorded since European contact with Polynesian cultures. Contrary to expectation given the earlier settlement of Western Polynesia, the Eastern Polynesian bark cloth traditions retained many ancestral features. In contrast, a suite of innovations appear in the Western Polynesian bark cloth traditions and it is asserted herein that the distribution of these traits may be associated with the rise of the Tongan maritime Empire. Within Eastern Polynesia, the pattern of diversification of bark cloth traditions is consistent with the breakdown of interaction spheres late in the settlement era.     

The Varying Role of Vertebrae in Pacific Fishbone Analysis: Comparing Tropical Versus Temperate Midden Assemblages

Archaeologists working in the tropical Pacific have demonstrated the feasibility and value of including fish vertebrae in midden analyses, and recent New Zealand studies draw similar conclusions. This work provides an illustrated guide to the identification of vertebrae from key New Zealand fish taxa and shows the effects of including vertebrae on a large fishbone assemblage from southern New Zealand. We note major differences between New Zealand and tropical Pacific assemblages resulting from the inclusion of vertebrae. Unlike the Indo‐Pacific taxa of the tropical Pacific, no New Zealand species have been shown to be sensitive to the inclusion of vertebrae. In both places, including vertebrae results in changes in relative abundance and rank order; but in New Zealand, this is a function of processing practices, not fishing behaviours. This work serves to highlight changes in the Polynesian fishing adaption following the colonisation of New Zealand. Copyright © 2017 John Wiley & Sons, Ltd.     

OPTICAL DATING OF ANTHROPOGENIC SEDIMENTS AT THE ARCHAEOLOGICAL SITE OF HERRENBRUNNENBUCKEL,BRETTEN-BAUERBACH (GERMANY)*

Optical dating was applied to natural and anthropogenic silts at an Iron Age settlement in southern Germany. The natural sediments were dated accurately and allowed study of the human impact on the landscape. The studied anthropogenic sediments were infills of cellars and ditches. Again, deposits derived from soil erosion proved to be datable using infrared-optically stimulated luminescence. However, optical dating of fine grained sediments was at its limits when sediments consisted of a mixture of bleached and unbleached grains. This is shown on sediments of known age originating from cellar infills. Improvements were obtained when using the 560 nm emission and a partial bleach approach. Experimental evidence shows that the D_E versus shine-time plot discloses insufficient bleaching only in cases in which all grains are insufficiently bleached to the same degree.     

Origins of Procellariidae Hunting in the Southwest Pacific

Small procellariids, mainly petrels, prions and shearwaters, were hunted at their rookeries in various parts of the southwest Pacific during the early historical era. The industries, some of which continue, arose from both traditional, indigenous, practices of prehistoric origin and subsistence necessity in early European settlements. The history and main features of the Tasmanian and southern New Zealand ‘muttonbird’ industries are described, together with brief summaries of those on Chatham, Raoul and Norfolk islands. Procellariid hunting occurred in two different situations, on isolated tropical islands, where its impact was often devastating, and on temperate islands associated with the East Australian Current, a western boundary current like the Gulf Stream. In the latter case, procellariid populations were very large and resilient to predation. In Tasmania, muttonbirds were taken for immediate consumption, but in New Zealand and other Polynesian islands there was preservation for storage. However, a common feature seems to have been the late development of systematic procellariid hunting, possibly because of the relative costs of access to the resource, although other explanations cannot be ruled out.     

The Difficult Place of Deserted Coasts in Archaeology: New Archaeological Research on Cooks Beach (Pukaki), Coromandel Peninsula,New Zealand

Sites which have been occupied semi-continuously in the past present some inherent difficulties for archaeology. Here we present new research from a coastal site on the North Island of New Zealand at Cooks Beach where anthropogenic vegetation changes are seen using microfossil analysis of obsidian tools, sediments and pit fill. The results indicate the initial presence of people in AD 1300–1400 followed by subsequent periods of disuse or abandonment and sweet potato (Ipomoea batatas) cultivation. Around the time of initial settlement, obsidian from this location is found at sites across the country. After AD 1400 the area appears to be deserted for a century or more, after which we see evidence for the cultivation of sweet potato in AD 1500 as evidenced by extensive soil modification and numerous storage pits. There is no evidence of a permanent settlement at the site. The geographic distribution of Cooks Beach obsidian was constricted while the site was used for sweet potato cultivation, a pattern often attributed to increased warfare. It appears cultivation was abandoned after AD 1650 marking a second secession of use, a fact confirmed in AD 1769 when Captain Cook visited the area. We consider the possible drivers for the late abandonment of cultivation at Cooks Beach.     

Settlement and environmental history of a multilayered settlement mound in Niederröblingen (central Germany) – a multi-proxy approach

A multi-disciplinary palaeoecological approach on a sequence of dated archaeosediments was accomplished. The sediments derive from a multilayered prehistoric settlement mound in central Germany, representing the remnants of a prehistoric village. Based on the analysis of biological remains and geochemical/physical analysis of the settlement layers its environment was reconstructed. There is a trend to increasing anthropogenic activities and impact on the environment represented through a rise of indicators for productive surplus from the Early Neolithic (5300–4900 BC) until the Roman Times (400 AD). During the Early Neolithic, shifting flat settlements were situated in a locally opened landscape. The immediate surrounding of the floodplain was used by the settlers for their economic requirements (e.g. wood from the riparian forest). After a hiatus of ca. 1900 years, a multilayered settlement mount rose from Late Neolithic Times (3000 BC) to Roman Times. Since the Middle Bronze Age (approximately 1500 BC) the riparian forest was obviously replaced by agricultural fields and meadows and henceforward the hinterland used by the settlers probably grew in size. The continuing demand of wood was maintained by the acquisition of more distant sources. The onset of house constructions substituting wood by loam (wattle and daub) might be a possible societal response to this shortfall. This is reflected in the growing thickness and composition of the settlement layers, as well as in the archaeological record (e.g. tumbled wattle and daub house walls). The rising of the groundwater table and the start of severe floods of the adjacent river Helme during pre-Roman Iron Age (approx. 800–100 BC) might reflect a geomorphological response to the increased land use intensity at a regional scale.     

CONTRASTING SUBSISTENCE STRATEGIES IN THE EARLY IRON AGE? – NEW RESULTS FROM THE ALFÖLD PLAIN,HUNGARY, AND THE THRACIAN PLAIN,BULGARIA

Summary. What can students of the past do to establish the predominant land‐use and settlement practices of populations who leave little or no artefactual discard as a testament to their lifeways? The traditional answer, especially in Eastern Europe, is to invoke often exogenous nomadic pastoralists whose dwelling in perpetuo mobile was based on yurts, minimal local ceramic production and high curation levels of wooden and metal containers. Such a lacuna of understanding settlement structure and environmental impacts typifies Early Iron Age (henceforth ‘EIA’) settlements in both Bulgaria and eastern Hungary – a period when the inception of the use of iron in Central and South‐East Europe has a profound effect on the flourishing regional bronze industries of the Late Bronze Age (henceforth ‘LBA’). The methodological proposal in this paper is the high value of palynological research for subsistence strategies and human impacts in any area with a poor settlement record. This proposal is illustrated by two new lowland pollen diagrams – Ezero, south‐east Bulgaria, and Sarló‐hát, north‐east Hungary – which provide new insights into this research question. In the Thracian valley, there is a disjunction between an area of high arable potential, the small size and short‐lived nature of most LBA and EIA settlements and the strong human impact from the LBA and EIA periods in the Ezero diagram. In the Hungarian Plain, the pollen record suggests that, during the LBA–EIA, extensive grazing meadows were established in the alluvial plain, with the inception of woodland clearance on a massive scale from c.800 cal BC, that contradicts the apparent decline in human population in this area. An attempted explanation of these results comprises the exploration of three general positions – the indigenist thesis, the exogenous thesis and the interactionist thesis. Neither of these results fits well with the traditional view of EIA populations as incoming steppe nomadic pastoralists. Instead, this study seeks to explore the tensions between local productivity and the wider exchange networks in which they are entangled.