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Introduction to Pacific Islands Archaeology
by Patrick V. Kirch
(in .pdf format)
The Pacific
Islands, also known as Oceania, have been subdivided traditionally by
anthropologists into three main geographic regions: Melanesia,
Micronesia, and Polynesia.
Following Green (1991), prehistorians now stress the division between
Near Oceania in the west (including the Bismarck Archipelago and the Solomon
Islands), and Remote Oceania (which includes all of island Melanesia southeast
of the Solomons, along with Polynesia and Micronesia). This latter distinction
recognizes the Pleistocene settlement of Near Oceania, whereas the widely
dispersed islands of Remote Oceania were discovered and settled only within
the past 4,000 years. Archaeological research in Oceania has a long history,
but modern efforts emphasizing stratigraphic excavations did not begin
until after World War II (Kirch 2000), and have revealed the main chronological
sequence for human settlement. This sequence is summarized here, followed
by reviews of the development of complex societies in Oceania, and of
human impact on island environments.
1. Early
Human Settlement of Near Oceania
The
oldest known occupation sites are radiocarbon dated to ca. 36,000 years
ago (the late Pleistocene), on the large island of New Guinea and in the
adjacent Bismarck Archipelago (Allen 1996). At several times during the
Pleistocene, New Guinea was joined to Australia as a single land mass
(known as Sahul), and human entry into and expansion throughout this vast
Australasian region occurred rapidly. Late Pleistocene sites in the Admiralty
Islands, New Ireland, and Buka (Solomons), all would have required open
ocean transport, suggesting the presence of some form of watercraft (possibly
rafts, bark boats, or dugouts) (Irwin 1992).
Early human colonists in Near Oceania were hunters-and-gatherers, who
exploited tropical rainforests as well as inshore marine resources (see
Hunter-Gatherer Societies, Archaeology of). Long-distance communication
and exchange is indicated by the movement of obsidian between islands.
By the early Holocene period (after 8,000 B.C.), there is archaeobotanical
evidence for domestication of tree, root, and tuber crops (such as the
Canarium almond, and various aroids) within Near Oceania. Archaeological
evidence for cultivation of swamplands at Kuk in the Highlands of New
Guinea commences as early as 7,000 B.C. (Golson 1988). These archaeological
indications confirm the long-held ethnobotanical hypothesis that Near
Oceania was one of several independent centers for the origins of tropical
horticulture.
2. Austronesian
Expansion and Lapita
During
the early Holocene, the southeastern Solomon Islands marked the limit
of human expansion. Beginning around 2,000 B.C., a major expansion or
diaspora of people speaking languages belonging to the Austronesian language
family commenced (Blust 1995). Their immediate homeland has generally
been regarded as comprising the island of Taiwan (and perhaps adjacent
areas of mainland China). The ability of early Austronesians to disperse
rapidly has been attributed to their invention of the outrigger sailing
canoe (Pawley and Ross 1993). The Austronesians were horticulturalists
who transported root, tuber, and tree crops via their canoes, along with
breeding stocks of domestic pigs, dog, and chickens.
The Austronesian diaspora rapidly encompassed the major archipelagoes
of island Southeast Asia; one branch of Austronesian-speakers expanded
along the north coast of New Guinea into the Bismarck Archipelago. This
branch is known to linguists as Oceanic, and the Oceanic languages (numbering
about 450 modern languages) include most of those spoken throughout the
Pacific. The great exception is New Guinea, where roughly 750 Non-Austronesian
languages are spoken.
Archaeological evidence for the initial Austronesian dispersal into the
Pacific comes from both western Micronesia (the Marianas and Palau archipelagoes),
and from the Bismarck Archipelago. In western Micronesia, early sites
contain red-slipped pottery, some of which is decorated with lime-filled,
impressed designs (Rainbird 1994). These sites, along with radiocarbon-dated
sediment cores exhibiting signals of human presence (e.g., high influxes
of microscopic charcoal resulting from anthropogenic burning) suggest
that humans settled Marianas and Palau no later than 1500 B.C., and possibly
as early as 2000 B.C.
In the Bismarck Archipelago, the initial
Austronesian incursion has been correlated with the appearance of a distinctive
suite of sites, also containing pottery with lime-infilled decorations,
but with motifs made largely by a technique of dentate-stamping. These
sites and the associated artifacts (such as Tridacna-shell adzes and Trochus-shell
fishhooks, as well as ornaments) represent the earliest known phase of
the Lapita cultural complex, dating to ca. 1500-1300 B.C. (Gosden et al.
1989; Spriggs 1997). Early Lapita sites were frequently hamlets or villages
consisting of houses elevated on posts or stilts, situated over tidal
reef flats or along shorelines. Excavated plant and animal remains indicated
a mixed economy with horticulture and marine exploitation. Substantial
quantities of obsidian, chert, pottery, shell artifacts and other materials
were exchanged between communities (Kirch 1997).
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Correlations among archaeological assemblages, language groups, and human
biological populations are often complex, and need not be isomorphic.
However, a strong consensus is emerging among scholars in several disciplines
that the initial phase of the Lapita cultural complex can be correlated
with the Proto Oceanic interstage of the Austronesian language family.
Moreover, genetic evidence (such as mtDNA and hemoglobin markers) supports
the view that the Lapita phenomenon reflects a substantial population
intrusion into the Bismarck Archipelago, deriving out of island Southeast
Asia (Hill and Serjeantson 1989). At the same time, the Proto Oceanic
speakers undoubtedly had considerable interaction (cultural, linguistic,
and genetic) with the indigenous Non-Austronesian speaking populations
who already occupied the Bismarck region in the mid-Holocene. Thus the
Lapita cultural complex is seen as an outcome of cultural processes of
intrusion, integration, and innovation.
3. Human
Colonization of Remote Oceania
Beginning
ca. 1300 B.C., the Lapita
pottery-makers expanded rapidly beyond the Solomons and into the southwestern
archipelagoes of Remote Oceania: Vanuatu, the Loyalty Islands, New Caledonia,
Fiji, Tonga, and Samoa. Numerous radiocarbon-dated archaeological sites
document that Lapita sites in all of these archipelagoes no later than
900 B.C.
We have already noted that the westernmost islands of Micronesia were
colonized directly out of island Southeast Asia by Austronesian speakers
ca. 2000-1500 B.C. Around 2,000 years ago, Oceanic speakers who made plainware
pottery (a late form of Lapita) and who used shell adzes, fishhooks, and
other implements, founded settlements on several volcanic islands of central
Micronesia (Chuuk, Pohnpei, and Kosrae). The atolls of the Marshall Islands
were also colonized at this time.
The final stage in the human settlement of the Pacific Islands began after
500 B.C., with the Polynesian dispersals eastwards out of Tonga and Samoa.
Ancestral Polynesian culture and Proto Polynesian language themselves
had developed in this Tonga-Samoa region between ca. 900-500 B.C. in this
homeland region, directly out of the founding Lapita cultural complex
(Kirch 2000; Kirch and Green, in press). While archaeologists debate the
exact chronology and sequence of Polynesian dispersals, most agree that
the central Eastern Polynesian archipelagoes (such as the Society Islands,
Cook Islands, and Marquesas Islands) were settled first, no later than
A.D. 300 and perhaps some centuries earlier (Rolett 1998). Remote Easter
Island was discovered by A.D. 800-900 (Van Tilburg 1994), while the Hawaiian
Islands were also well settled by this date. The twin large, temperate
islands of New Zealand were colonized by Polynesians around A.D. 1200
(Anderson 1989; Davidson 1984). Critical to the success of this unprecedented
diaspora was the double-hulled sailing canoe, capable of carrying 40-60
people on voyages lasting one month or longer (Irwin 1992). That the Polynesians
reached South America and returned is suggested by preserved remains of
the sweet potato (Ipomoea batatas), a South American domesticate, in several
prehistoric Polynesian sites.
Because it was the last sector of Remote Oceania to be settled, and because
its populations represent a single radiation or diaspora, Polynesia constitutes
a monophyletic cultural and linguistic group. Thus, Polynesia has often
been regarded as an ideal region for testing models of cultural differentiation
from a common ancestor (e.g., Kirch 1984; Kirch and Green, in press).
4. Development
of Complex Societies
When
the 18th-19th century European voyages of discovery inspired by the Enlightenment
encountered Pacific island societies, they frequently encountered large,
dense populations organized into complex, hierarchical sociopolitical
formations. With populations often numbering into the tens or hundreds
of thousands, such societies had two to three decision-making levels,
and hereditary leaders who enjoyed elite privileges and status markers.
Anthropologists classify such sociopolitical formations as chiefdoms,
and indeed, the Polynesian chiefdoms are often considered the archetypal
model.
The origins, development, and elaboration of Pacific island chiefdoms
have been a major topic of archaeological research (e.g., Davidson 1984;
Kirch 1984; Rainbird 1994; Sand 1995; Spriggs 1997). Based on linguistic
and archaeological evidence, early Austronesian societies were characterized
by some degree of internal ranking (especially between senior and junior
branches of a descent line), but were probably heterarchical rather than
hierarchical in structure. However, heterarchic competition (in such social
arenas as marriage and exchange, as well as competition for land) between
social groups provided the basis for true hierarchy (and eventually, in
the largest societies, class stratification) to emerge.
Archaeologists have identified several factors and processes that were
significant in the rise of Oceanic chiefdom societies. Many of these were
closely linked, and should not be considered unicausal variables. For
example, population growth leading to large, high-density populations
can be identified as a necessary, but probably not sufficient, cause underlying
sociopolitical complexity (Kirch 2000; Sand 1995). The human populations
of the volcanic islands typically reached densities of between 100-250
persons per square kilometer prior to European contact, resulting in intense
competition for arable land and other resources. Such conditions encouraged
centralized, hierarchic control, as well as providing incentives for militaristic
aggression.
A second process linked to population growth and to increased hierarchy
was intensification of production, including agricultural systems and
other forms of production or resource extraction, as well as economic
specialization (e.g., in pottery production and trade). On many islands,
large-scale irrigation works or dryland field systems were developed during
late prehistory. Although population increases may have initially spurred
intensification, once in place such intensive production systems provided
a means for surplus extraction by chiefs and other leaders, thus encouraging
hierarchy. Often culturally marked as tribute, such surpluses were the
economic foundation of an emergent elite, including not only hereditary
chiefs, but priests, warriors, craft specialists, and others.
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Ideology likewise played a key role in Pacific island societies, with
the elite cadres of the larger and most complex societies actively employing
ideological control as a means of legitimation. The origins of Oceanic
ritual systems can be traced back to common Austronesian concepts of the
sacredness of ancestors; these concepts later became elaborated as cults
in which the highest chiefs were seen as directly descended from powerful
gods, and hence essential to the continued well-being of the society at
large. Archaeologically, the rise of elite-dominated ideological systems
is particularly reflected in monumental architecture, of which the most
impressive examples are the giant statue-bearing temples of Easter Island,
and the site of Nan Msadol on Pohnpei. Other forms of monumental architecture,
however, are ubiquitous throughout Pacific islands chiefdoms. Even when
monumental architecture is absent, material signs of ideological control
can be quite striking, as in the multiple sacrificial interments associated
with the burial of Roy Mata, a chief of Vanuatu (Garanger 1972).
Finally, competition, conflict, and warfare also characterized many of
the complex societies of the Pacific, especially following the rise of
large and dense populations. Archaeologically, warfare is marked by a
diversity of kinds of fortifications, such as the pallisaded pa
volcanic cones and headlands of New Zealand, or the ring-ditch fortified
villages of Fiji. Another, more gruesome signal of the levels that inter-societal
aggression reached on some islands is cannibalism (or para-cannibalistic
treatment of enemies, such as dismembering, roasting, and non-funerary
discard of skeletal remains). Although some anthropologists have expressed
skepticism regarding European voyagers’ accounts of cannibalism
in the Pacific, there is now direct archaeological evidence for cannibalistic
or para-cannibalistic practices in late prehistory on Easter Island, the
Marquesas, New Zealand, Mangaia, and Fiji.
5. Human
Impacts to Island Ecosystems
The
islands of Remote Oceania, due to isolation and related factors, provide
model conditions for studying the effects of human colonization and land
use on pristine ecosystems. Interdisciplinary research among archaeologists
and natural scientists over the past three decades has amplified our understanding
of such human-ecosystem interactions (Kirch and Hunt, eds., 1997).
Because of the substantial open-ocean distances isolating them from continents
as well as other islands, and the difficulty of dispersal to islands,
prior to human arrival oceanic ecosystems were typically characterized
by: high species-level endemicity, but lower diversity in higher-level
(generic and family) taxa; lowered competition; survival of archaic forms;
and vulnerability to disturbance from outside agents. Larger vertebrates
such as marsupials (wombats, cuscus) and rats, snakes, frogs, and most
lizards were restricted primarily to Near Oceania, with only a handful
of species declining in numbers eastwards to Fiji and Samoa. (The reef
and marine resources of Pacific islands also display a west-to-east decline
in species diversity.) Throughout most of Remote Oceania, pre-human vertebrate
faunas were dominated by birds (including many flightless forms which
had evolved in situ from flighted ancestors). Prior to human arrival,
these bird populations lacked large vertebrate predators, and presumably
also a typical predator avoidance strategy. They must have been extremely
easy prey for the first humans to step foot on islands.
When humans first arrived in Remote Oceania, they typically found the
islands to be forested, and inhabited by a range of largely endemic species,
dominated by birds, along with invertebrates such as landsnails and insects.
Oceanic peoples possessed a successful colonization strategy that allowed
them to exist on isolated islands, by: (1) transporting in their sailing
canoes stocks of horticultural crop plants, along with domestic pigs,
dog, and chickens (rats came along, presumably as “stowaways”);
(2) clearing areas of rainforest for garden land; and, (3) intensively
exploiting the abundant natural avifaunal and marine resources.
This colonization strategy had several consequences for island ecosystems,
all of which are increasingly well documented through both archaeological
and paleoenvironmental indicators. Forest clearance on many islands is
signaled in changing pollen spectra from sediment cores, with tree taxa
rapidly giving away to ferns and grasses; also characteristic are sharp
increases in microscopic charcoal influxes, indicating human-induced burning,
in most cases probably associated with shifting cultivation. On some islands,
forest clearance led to increased erosion rates, along with alluviation
of valley bottoms or along coastal plains. The exploitation of natural
resources is particularly evident in the zooarchaeological assemblages
from early settlement sites, which are characterized by high numbers of
land and seabirds, many of them representing now extinct or extirpated
species (Steadman 1995). A dramatic case of avifaunal extinctions on Pacific
islands is that of the moa, a group of 13 species of large, flightless
birds which became totally extinct in New Zealand during the brief period
of Polynesian occupation (Anderson 1989).
Cumulative effects of human actions on islands led to irreversible changes,
such as dramatic declines in biodiversity, and the conversion of natural
rainforests to intensively-managed, anthropogenic landscapes. The consequences
for human populations themselves were undoubtedly mixed. The replacement
of natural ecosystems with intensive food production systems enabled the
growth of large and dense human populations. At the same time, reduction
or depletion of natural resources, coupled with the necessity for intensive
land use, encouraged highly complex sociopolitical systems which at times
competed fiercely for control of land and the means of production.
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References Cited
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