# Lapita Diet in Remote Oceania: New Stable Isotope Evidence from the 3000-Year-Old Teouma Site, Efate Island, Vanuatu

Rebecca Kinaston, Hallie Buckley, Frederique Valentin, Stuart Bedford, Matthew Spriggs, Stuart Hawkins, Estelle Herrscher

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Rebecca Kinaston, Hallie Buckley, Frederique Valentin, Stuart Bedford, Matthew Spriggs, et al. Lapita Diet in Remote Oceania: New Stable Isotope Evidence from the 3000-Year-Old Teouma Site, Efate Island, Vanuatu. PLoS ONE, 2014, 9, 10.1371/journal.pone.0090376.s003. [http://dx.doi.org/10.1371/journal.pone.0090376](http://dx.doi.org/10.1371/journal.pone.0090376.s003). This is an open access article distributed under the terms of the Creative Commons Attribution 4.0 International License.

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Distributed under a Creative Commons Attribution 4.0 International License
# Lapita Diet in Remote Oceania: New Stable Isotope Evidence from the 3000-Year-Old Teouma Site, Efate Island, Vanuatu

Rebecca Kinaston¹*, Hallie Buckley¹, Frederique Valentin², Stuart Bedford³, Matthew Spriggs⁴, Stuart Hawkins⁴, Estelle Herrscher⁵

¹Department of Anatomy, University of Otago, Dunedin, New Zealand, ²CNRS, Maison de l'Archéologie et de l'Ethnologie, Nanterre, France, ³Department of Archaeology and Natural History, College of Asia and the Pacific, The Australian National University, Canberra, ACT, Australia, ⁴School of Archaeology and Anthropology, The Australian National University, Canberra, ACT, Australia, ⁵CNRS, Laboratoire Méditerranéen de Préhistoire Europe Afrique, Aix-Marseille Université, Aix-en-Provence, France

## Abstract

Remote Oceania was colonized ca. 3000 BP by populations associated with the Lapita Cultural Complex, marking a major event in the prehistoric settlement of the Pacific Islands. Although over 250 Lapita sites have been found throughout the Western Pacific, human remains associated with Lapita period sites are rare. The site of Teouma, on Efate Island, Vanuatu has yielded the largest burial assemblage (n = 68 inhumations) of Lapita period humans ever discovered, providing a unique opportunity for assessing human adaptation to the environment in a colonizing population. Stable isotope ratios (δ¹³C, δ¹⁵N, δ³⁴S) of human bone collagen from forty-nine Teouma adults were analyzed against a comprehensive dietary baseline to assess the paleodiet of some of Vanuatu's earliest inhabitants. The isotopic dietary baseline included both modern plants and animals (n = 98) and prehistoric fauna from the site (n = 71). The human stable isotope data showed that dietary protein at Teouma included a mixture of reef fish and inshore organisms and a variety of higher trophic marine (e.g. marine turtle) and terrestrial animals (e.g. domestic animals and fruit bats). The domestic pigs and chickens at Teouma primarily ate food from a C₃ terrestrial environment but their δ¹⁵N values indicated that they were eating foods from higher trophic levels than those of plants, such as insects or human fecal matter, suggesting that animal husbandry at the site may have included free range methods. The dietary interpretations for the humans suggest that broad-spectrum foraging and the consumption of domestic animals were the most important methods for procuring dietary protein at the site. Males displayed significantly higher δ¹⁵N values compared with females, possibly suggesting dietary differences associated with labor specialization or socio-cultural practices relating to food distribution.

**Citation:** Kinaston R, Buckley H, Valentin F, Bedford S, Spriggs M, et al. (2014) Lapita Diet in Remote Oceania: New Stable Isotope Evidence from the 3000-Year-Old Teouma Site, Efate Island, Vanuatu. PLoS ONE 9(3): e90376. doi:10.1371/journal.pone.0090376

**Editor:** Debbie Guatelli-Steinberg, Ohio State University, United States of America

**Received:** November 3, 2013; **Accepted:** January 28, 2014; **Published:** March 5, 2014

**Copyright:** © 2014 Kinaston et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

**Funding:** Funding of the project during 2004 and 2005 was provided by the Australian Research Council (ARC) (DP 0556874, www.arc.gov.au), Pacific Biological Foundation (PBF04-1, www.apscience.org.au). The excavations in 2006 were funded primarily through a National Geographic Scientific Research Grant (8038-06, www.nationalgeographic.com/explorers/), with further support from the ARC Discovery Grant (DP 0556874, www.arc.gov.au). Excavations from 2008 to 2010 were primarily funded by an ARC Discovery Grant (DP 0880789, www.arc.gov.au). Funding for the excavation and analysis of the humans remains, prehistoric fauna and collection and analysis of the modern plants and animals was provided by Two Royal Society of New Zealand Marsden Grants (04-UOO-007 and 09-UOO-106, http://www.royalsociety.org.nz/programmes/funds/marsden/ ) and a University of Otago Research Grant during 2009 (no number, http://www.otago.ac.nz/ research/otago004140.html). Further funding for the stable isotope analysis was provided by CNRS: Aix-Marseille Université, MCC/CNRS (UMR 7269 LAMPEA, http://lampea.cnrs.fr/) and UMR 7041 ArScAn, http://www.mae.u-paris10.fr/arscan/). The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.

**Competing Interests:** The authors have declared that no competing interests exist.

* E-mail: rebecca.kinaston@anatomy.otago.ac.nz

## Introduction

A change in diet and mode of subsistence can affect the health, demography and overall success of a population. The most well known example of a prehistoric dietary transition was the Agricultural Revolution that occurred in numerous centers across the globe, during which humans became increasingly reliant on domesticated plants and animals for food [1–3]. In the western Pacific Islands several major events can be viewed as catalysts for dietary transitions during prehistory after the initial arrival of humans in the region ca. 50,000 years ago. One significant event was the development of horticultural systems ca. 10,000 BP in the highlands of New Guinea [4–6]. Another occurred around 3300–

3000 BP, when populations with cultural and biological links to Island South East Asia (ISEA), known as Lapita, appeared in the Bismarck Archipelago and then sailed into Remote Oceania with an established suite of domesticated plants and animals, a ‘transported landscape’, which enabled the settlement of previously uninhabited Pacific islands east of the Solomon Islands chain [7–9] (fig. 1).

As the Lapita populations sailed eastward and southward from the Bismarck Archipelago they left evidence of their occupation in the form of intricately decorated dentate-stamped Lapita pottery [8,10,11]. The numerous archaeological sites containing Lapita pottery in the Reef and Santa Cruz Islands, Vanuatu, New Caledonia, Fiji, Tonga, and Samoa attest to the success of Lapita
<figure><img src="image_2.png" /><figcaption>Figure 1. Map of Near and Remote Oceania and location of Efate Island, Vanuatu.</figcaption></figure>

doi:10.1371/journal.pone.0090376.g001

colonization in Remote Oceania [7]. However, the marked decrease in biodiversity as one moves eastward across the Pacific Ocean required the initial Lapita settlers to adapt rapidly to the local ecology of each island to obtain enough food to support their fledgling communities [12–14].

A number of theories regarding the specific subsistence strategies of Lapita populations have been posited over the years. In the 1970s Groube [15] suggested that Lapita populations were Oceanic strandloopers focused primarily on gathering reef and inshore resources. Green [16] introduced the idea that domestic plants and animals transported with Lapita populations were the critical food items that facilitated the settlement of Remote Oceania [7,17]. Other hypotheses regarding Lapita subsistence have also emerged arguing for a low level of plant cultivation and animal husbandry accompanied by the broad-spectrum exploitation of nearby marine and terrestrial resources [18,19].

The presence of microfossils from exotic domestic plant species in Lapita and immediately post-Lapita sites in Remote Oceania indicates that horticulture was practiced during the early settlement of the region [20–24]. However, the extent to which the Lapita people (and their domestic animals) relied on this transported landscape compared with native flora and fauna during the initial settlement period remains uncertain [25]. A direct analysis of the diets of people from Lapita settlements and the dietary resources available to them would be ideal for addressing hypotheses regarding early Pacific island subsistence. The Teouma Lapita site, located on Efate Island, Vanuatu, provides this opportunity due to the large cemetery sample and the substantial amount of faunal material available for analysis from the site. Previous stable isotope analyses of Lapita-associated human skeletal remains has illuminated some aspects of Lapita diet [25–30], but the small nature of these samples and lack of site-specific baseline data has limited the scope of these interpretations.

The overall aim of this study is to assess human dietary adaptation in a recently colonized, pristine environment during

the earliest known Lapita settlement of Central Vanuatu, on the far western edge of Remote Oceania. To achieve this we have analyzed the carbon, nitrogen and sulfur stable isotope ratios of human bone collagen to examine the diet of individuals interred in the Lapita cemetery of Teouma (ca. 3000–2900 BP) [31]. This study builds on a previous paleodietary analysis of thirty-three individuals interred in the Teouma cemetery conducted by Valentin et al. [32] by analyzing a further sixteen individuals and using sulfur stable isotope ratios to provide additional dietary information. To ensure the most reliable interpretation of the human stable isotope data we have analyzed modern plant and animal samples from Vanuatu in addition to prehistoric faunal samples from the Teouma site in order to establish the range of isotopic variation in the local environment. The prehistoric faunal remains include native and domestic species from Lapita (~3000–2900 BP), late Lapita (2900–2800) and immediately post-Lapita (Arapus and Erueti) (~2800–2500 BP) assemblages. The analysis of prehistoric faunal material from different temporal periods can also illuminate variation in animal diets that may be related to environmental change or animal husbandry techniques connected with certain activities such as horticultural intensification over time.

Stable isotope analysis has also been used to help discern whether there were dietary differences within a prehistoric cemetery sample that may be related to sex and age [33–35]. Differential access to certain foods within a population can provide information about broader socio-cultural factors in a prehistoric population, for example gender inequalities, labor specialization, immigration, social structure, and the treatment of certain members of a community, such as children [36–40]. Throughout the Pacific Islands certain foods are considered ‘high-status’ and may be reserved for highly esteemed individuals or simply eaten in larger quantities by these people [41–44]. These ‘high-status’ foods include fatty, greasy and oily animal products such as pig (*Sus scrofa*), chicken (*Gallus gallus*), marine turtle and some types of fish,
<figure><img src="image_3.png" /><figcaption>Figure 2. Map of the location of the Teouma site on Efate Island, Vanuatu.</figcaption></figure>

doi:10.1371/journal.pone.0090376.g002

especially pelagic species [45–47]. Linguistic reconstructions have given support to the theory that Lapita social structure was ranked and formed the basis of the highly stratified societies that developed later in Polynesia [7,48–51]. Both within Polynesia and the Western Pacific, highly ranked individuals such as chiefs are traditionally male and these men usually have preferential access to high-status foods [44].

In this study we have tested two hypotheses in an attempt to address questions regarding Lapita subsistence strategies and possible differences in food consumption patterns related to sex. As people interred in the Teouma Lapita cemetery are thought to be some of the earliest colonists of Vanuatu [31] we hypothesize that the individuals from Teouma would have been more reliant on native protein resources from both marine and terrestrial

ecosystems than domestic animals and horticultural plants due to the time necessary to establish an extensive crops and animal populations. We also hypothesize that males would have been eating different foods compared to females, specifically these ‘high-status’ animal products because of the suspected ‘ranked’ nature of Lapita communities.

## Stable isotope analysis for paleodietary reconstruction

The stable isotope analysis of carbon (δ¹³C), nitrogen (δ¹⁵N) and, more recently, sulfur (δ³S) from human skeletal and dental remains is a well-established method of reconstructing ancient diets [52–55]. Stable isotopes are measured in ratios (¹³C / ¹²C, ¹⁵N/¹⁴N, and ³S/³²S) relative to a standard (PDB for carbon, AIR for nitrogen and VCDT for sulfur), expressed in parts per
<table><caption>**Table 1.** Descriptive statistics (mean ±1 SD) for δ¹³C, δ¹⁵N and δ³⁴S values of modern plant and animals collected from Vanuatu.</caption><thead><tr><th>Sample</th><th>n</th><th>δ¹³C (‰)</th><th>±1 SD</th><th>δ¹⁵N (‰)</th><th>±1 SD</th><th>n</th><th>δ³⁴S (‰)</th><th>±1 SD</th></tr></thead><tbody><tr><td>All C<sub>3</sub> plants</td><td>62</td><td>-26.2</td><td>2.1</td><td>3.9</td><td>2.0</td><td>8</td><td>9.5</td><td>4.0</td></tr><tr><td>C<sub>3</sub> plants (no nuts)</td><td>49</td><td>-26.3</td><td>2.2</td><td>3.6</td><td>1.7</td><td>5</td><td>8.0</td><td>3.7</td></tr><tr><td>C<sub>3</sub> nuts</td><td>13</td><td>-25.6</td><td>2.0</td><td>5.1</td><td>2.4</td><td>3</td><td>11.9</td><td>3.8</td></tr><tr><td>Fruit bat bone</td><td>1</td><td>-21.7</td><td></td><td>7.1</td><td></td><td>1</td><td>11.0</td><td></td></tr><tr><td>C<sub>4</sub> plants</td><td>3</td><td>-12.5</td><td>0.1</td><td>3.9</td><td>1.0</td><td></td><td></td><td></td></tr><tr><td>Seagrass</td><td>3</td><td>-9.3</td><td>4.8</td><td>1.2</td><td>0.5</td><td>1</td><td>14.0</td><td></td></tr><tr><td>Mangrove shellfish</td><td>3</td><td>-26.1</td><td>2.5</td><td>-2.0</td><td>6.5</td><td>2</td><td>-8.7</td><td>18.0</td></tr><tr><td>Mangrove crabs</td><td>2</td><td>-24.1</td><td>0.0</td><td>2.5</td><td>0.6</td><td>1</td><td>9.4</td><td></td></tr><tr><td>Marine shellfish</td><td>15</td><td>-10.1</td><td>4.7</td><td>5.5</td><td>2.0</td><td>1</td><td>14.9</td><td></td></tr><tr><td>Sardine bone</td><td>2</td><td>-14.3</td><td>0.0</td><td>5.8</td><td>0</td><td>1</td><td>17.2</td><td></td></tr><tr><td>Sphyraenidae bone</td><td>2</td><td>-12.3</td><td>0.1</td><td>6.0</td><td>0.3</td><td></td><td></td><td></td></tr><tr><td>Parrotfish bone</td><td>2</td><td>-9.7</td><td>3.8</td><td>5.4</td><td>3.1</td><td>1</td><td>17.6</td><td></td></tr><tr><td>Tuna bone</td><td>2</td><td>-13.0</td><td>0.1</td><td>7.3</td><td>0.3</td><td>1</td><td>18.2</td><td></td></tr><tr><td>Marine turtle bone</td><td>1</td><td>-9.7</td><td></td><td>9.2</td><td></td><td>1</td><td>13.6</td><td></td></tr></tbody></table>

doi:10.1371/journal.pone.0090376.t001

<figure><img src="image_4.png" /><figcaption>**Figure 3.** Modern plant and animal δ¹³C and δ¹⁵N values from Vanuatu.</figcaption></figure>

doi:10.1371/journal.pone.0090376.g003
<figure><img src="image_5.png" /><figcaption>Figure 4. Prehistoric faunal δ¹³C and δ¹⁵N values from Teouma.</figcaption></figure>

doi:10.1371/journal.pone.0090376.g004

thousand or per mil (‰) and designated by the delta notation (δ). The rate of bone remodeling is slow for adults and therefore the stable isotope ratios of bone collagen are thought to represent at least the last 10–15 years of diet prior to death [56].

Carbon stable isotope ratios are used to address questions regarding marine and terrestrial food exploitation. Additionally, carbon stable isotope ratios are used to identify the consumption of certain types of plants that display different photosynthetic

pathways (i.e. C₃, C₄ and CAM plants). This is possible because marine systems and C₄ plants are enriched in the heavy stable isotope of carbon (¹³C) compared with terrestrial systems and C₃ plants, respectively [54,57].

There is a stepwise enrichment in ¹⁵N with every successive trophic level. Herbivores display higher δ¹⁵N values than the plants in their diet and carnivores display a subsequent enrichment in ¹⁵N in their bone collagen compared with the herbivores that

<table><caption>Table 2. Descriptive statistics (mean ±1 SD) for δ¹³C, δ¹⁵N and δ³⁴S values of the prehistoric fauna from Teouma.</caption><thead><tr><th>Animal</th><th>Layer</th><th>n</th><th>δ¹³C (‰)</th><th>±1 SD</th><th>δ¹⁵N (‰)</th><th>±1 SD</th><th>n</th><th>δ³⁴S (‰)</th><th>±1 SD</th></tr></thead><tbody><tr><td>Pig</td><td>All Layers</td><td>20</td><td>-19.6</td><td>0.7</td><td>9.6</td><td>1.1</td><td>18</td><td>10.9</td><td>0.8</td></tr><tr><td>Pig</td><td>Post-Lapita</td><td>6</td><td>-19.5</td><td>0.6</td><td>9.9</td><td>1.1</td><td>4</td><td>10.9</td><td>0.9</td></tr><tr><td>Pig</td><td>Lapita</td><td>13</td><td>-19.6</td><td>0.8</td><td>9.4</td><td>1.1</td><td>13</td><td>11.0</td><td>0.9</td></tr><tr><td>Pig</td><td>Disturbed</td><td>1</td><td>-20.5</td><td></td><td>9.3</td><td></td><td></td><td></td><td></td></tr><tr><td>Chicken</td><td>All Layers</td><td>7</td><td>-19.7</td><td>1.1</td><td>11.1</td><td>1.2</td><td>5</td><td>12.2</td><td>0.8</td></tr><tr><td>Chicken</td><td>Post-Lapita</td><td>1</td><td>-20.5</td><td></td><td>12.4</td><td></td><td></td><td></td><td></td></tr><tr><td>Chicken</td><td>Lapita</td><td>6</td><td>-19.5</td><td>1.2</td><td>10.9</td><td>1.2</td><td>3</td><td>12.2</td><td>0.8</td></tr><tr><td>Tortoise</td><td>All Layers</td><td>17</td><td>-23.4</td><td>0.5</td><td>4.9</td><td>2.8</td><td>4</td><td>11.0</td><td>0.8</td></tr><tr><td>Tortoise</td><td>Late Lapita</td><td>4</td><td>-23.4</td><td>0.5</td><td>2.7</td><td>0.8</td><td>1</td><td>10.4</td><td></td></tr><tr><td>Tortoise</td><td>Lapita</td><td>10</td><td>-23.4</td><td>0.3</td><td>5.7</td><td>2.9</td><td>1</td><td>10.4</td><td></td></tr><tr><td>Tortoise</td><td>Disturbed</td><td>3</td><td>-23.1</td><td>0.9</td><td>4.9</td><td>3.4</td><td>2</td><td>11.7</td><td>0.5</td></tr><tr><td>Marine turtle</td><td>Lapita</td><td>2</td><td>-11.2</td><td>0.6</td><td>13.1</td><td>0.1</td><td></td><td></td><td></td></tr><tr><td>Rat</td><td>Post-Lapita</td><td>2</td><td>-19.2</td><td>0.4</td><td>9.6</td><td>1.2</td><td></td><td></td><td></td></tr><tr><td>Reef fish</td><td>Post-Lapita</td><td>1</td><td>-10.9</td><td></td><td>8.1</td><td></td><td></td><td></td><td></td></tr><tr><td>Fruit bat</td><td>All Layers</td><td>22</td><td>-19.8</td><td>0.4</td><td>5.2</td><td>1.6</td><td></td><td></td><td></td></tr><tr><td>Fruit bat</td><td>Post-Lapita</td><td>11</td><td>-19.7</td><td>0.4</td><td>5.7</td><td>1.7</td><td></td><td></td><td></td></tr><tr><td>Fruit bat</td><td>Late Lapita</td><td>3</td><td>-20.0</td><td>0.3</td><td>5.5</td><td>1.9</td><td></td><td></td><td></td></tr><tr><td>Fruit bat</td><td>Lapita</td><td>8</td><td>-19.9</td><td>0.4</td><td>4.5</td><td>1.4</td><td></td><td></td><td></td></tr></tbody></table>

doi:10.1371/journal.pone.0090376.t002
<table><caption>**Table 3.** Descriptive statistics (mean ±1 SD) for δ¹³C, δ¹⁵N and δ³⁴S values of the humans from Teouma.</caption><thead><tr><th>Group</th><th>n</th><th>δ¹³C (‰)</th><th>±1 SD</th><th>δ¹⁵N (‰)</th><th>±1 SD</th><th>n</th><th>δ³⁴S (‰)</th><th>±1 SD</th></tr></thead><tbody><tr><td>All Adults</td><td>49</td><td>-15.7</td><td>1.2</td><td>12.1</td><td>1.0</td><td>14</td><td>11.3</td><td>1.3</td></tr><tr><td>Males</td><td>23</td><td>-15.8</td><td>1.3</td><td>12.7</td><td>1.1</td><td>10</td><td>11.5</td><td>1.3</td></tr><tr><td>Females</td><td>25</td><td>-15.5</td><td>1.1</td><td>11.6</td><td>0.7</td><td>4</td><td>10.9</td><td>1.1</td></tr><tr><td>Unsexed</td><td>1</td><td>-15.4</td><td></td><td>12.7</td><td></td><td></td><td></td><td></td></tr></tbody></table>

doi:10.1371/journal.pone.0090376.t003

they consume [58,59]. Nitrogen stable isotope ratios are used in conjunction with carbon stable isotope ratios to differentiate between terrestrial and aquatic dietary resources. Marine, estuarine, and freshwater systems typically exhibit more steps in their respective food chains (i.e. more trophic levels) than terrestrial systems and correspondingly display higher δ¹⁵N values [54,60–62]. Plants and organisms that utilize nitrogen-fixing bacteria such as legumes, seagrasses, mangroves, and cyanobacteria in coral reefs display low δ¹⁵N values [63–66].

Used in conjunction with carbon and nitrogen stable isotope ratios, the analysis of sulfur stable isotope ratios has become increasingly popular as a means to differentiate between aquatic and terrestrial dietary resources [27,40,67–71], and has also been used to identify migrants within a skeletal sample [72–74]. The δ³¹S value of human bone collagen is a reflection of local environmental sulfur isotope ratios [53,75]. Sulfur enters terrestrial ecosystems from a number of sources including the local geology (e.g. pyrites), microbial processes in the soil and the atmosphere (wet and dry atmospheric deposition). Inorganic sulfates enter the local food web with little fractionation after they are converted into organic forms by plants [53,73,76]. Terrestrial systems may display a wide range of δ³¹S values (–5 to +10‰) [77], depending on the underlying geology, their proximity to the ocean (discussed below), and microbial processes in the soil [78,79]. Freshwater systems display highly variable δ³¹S values (–22‰ to +20‰) [80,81] as a result of the action of anaerobic bacteria in lake and river sediments [82]. Oceanic sulfate displays a consistent mean δ³¹S value of ~20‰ [83] due to the continual mixing of oceans. Marine organisms can therefore be distinguished by their higher δ³¹S values in comparison to terrestrial organisms [80,84]. However, the δ³¹S values of coastal terrestrial food webs may be elevated as a result of marine derived precipitation and sea-spray, known as the ‘sea-spray effect’ [33,85,86].

Human and faunal bone collagen stable isotope values from one site are directly comparable, taking into account trophic level differences for carbon, nitrogen and sulfur stable isotopes. It is widely accepted that trophic differences between consumer and prey nitrogen stable isotope ratios are between 3–4‰ [59,87], although recently a larger offset of 6‰ has been suggested for humans in certain circumstances [88]. Trophic level enrichment of δ¹³C values has been found to be small, about 0–2‰, between consumer and prey collagen values [89]. The trophic enrichment of δ³¹S in bone collagen is not well established but is thought to be relatively small (<1.0‰) [53].

Nitrogen and sulfur stable isotope ratios are only representative of dietary protein as carbohydrates and lipids do not contain these elements [61]. Carbon from amino acids in dietary protein is preferentially routed to synthesize bone collagen, although some carbon from other macronutrients (e.g. lipids and carbohydrates) may also be utilized [90–93]. As a result, low protein foods (i.e. plant foods) may be underestimated in the diet when interpreting carbon stable isotope ratios [94]. The diet-tissue spacing of bone

collagen δ¹³C values has been observed to be approximately +5‰ if the diet is monoisotopic (e.g. all components are from a C₃ terrestrial ecosystem), but variations in diet-tissue spacing may occur as a result of the isotopic composition of the dietary macronutrients [90,91,95].

It is important to recognize that the interpretation of the proportions of certain foods in the diet from bone collagen isotope values is not straightforward. Establishing 100% terrestrial and 100% marine diets to use as “endpoints” is difficult because, as Müldner and Richards [96: 8] state, “uncertainty about the range of animal and plant foods consumed, their digestible protein content (which may vary according to their mode of preparation), as well as about the exact magnitude of the trophic level enrichment, means that where such end points are estimated, the likely errors involved must be considered”. The calculation of a 100% marine diet is difficult in the Pacific Islands because there are multiple sources of marine foods with a wide-range of δ¹³C values and C₄ plants such as sugar cane may also have been eaten. For these reasons we refrain from estimating exact proportions of dietary protein in this paper.

## The site and the skeletal sample

The Teouma site is located close to modern day Port Vila on Efate Island, Vanuatu. Three thousand years ago the Teouma site would have been adjacent to the sea on the edge of a large bay, but as a result of tectonic uplift the site is now located approximately 800 m from the current foreshore [97] (fig. 2). The site was first excavated in 2004 as a result of the discovery of sherds of Lapita pottery during quarrying for the construction of a prawn farm [31,97]. Sixty-eight graves, which contained single and multiple interments of around one hundred individuals, were recovered from the Lapita cemetery. All the individuals interred in the main cemetery date to the earliest phase of the Lapita settlement of Vanuatu (ca. 3000 BP) [31,98]. A complex multi-stage burial ritual has been identified at the site, involving the manipulation of the bodies after death, the removal of bones and, in one case, cremation [99,100].

The stratigraphy of the site is comprised of an ancient volcanic tephra covering the upraised karstic reef terrace and the former rolled-coral upper beach. Lapita burials are cut into the tephra layer, filling solution holes in the reef and upper beach. Up to 50 cm of midden associated with the Arapus and Early Erueti phases (ca. 2800–2500 BP) (Layer 2) overlies and post-dates the Lapita-associated burials (Layer 3). It is thought that this midden was deposited some time after the use of the site as a cemetery had ceased [31,97]. Capping the archaeological deposits is a black tephra-rich soil from subsequent prehistoric volcanic eruptions. The unique depositional nature of the Teouma site, with the alkaline coral reef neutralizing the potentially acidic volcanic tephra, has led to the exceptional preservation of the skeletal and faunal material.
<figure><img src="image_6.png" /><figcaption>**Figure 5.** Human δ¹³C and δ¹⁵N values in relation to the prehistoric faunal remains from Teouma. The full and dotted circles designate a trophic effect of 1.0‰ for δ¹³C and 3.0‰ for δ¹⁵N and 1.0‰ for δ¹³C and 5.0‰ for δ¹⁵N respectively.
doi:10.1371/journal.pone.0090376.g005</figcaption></figure>

Prehistoric diet at Teouma: the archaeological and ecological evidence

The Teouma site is located in an ecologically diverse area that is
near to rainforest, lagoon, coral reef, freshwater, mangroves, and
swamp ecosystems, all of which would have provided potential
food resources for the site's inhabitants [31]. The analysis of the
Teouma archaeofaunal assemblages is currently underway, but a
number of terrestrial endemic and native species have been
identified from archaeological contexts at the site and at other
contemporary habitation sites in Vanuatu. Some of these species
inhabit Vanuatu today (e.g. bats and a variety of smaller bird
species), but some taxa were hunted to extinction during
prehistory, such as a land-based crocodile (*Mekosuchus kalpokasi*), a
number of flightless birds including a large megapode, several
species of bat and a giant tortoise (? *Meiolania damelipi*) [101–103].
The extreme predation of fragile native and endemic species is a
common feature of initial human occupation of the islands of
Remote Oceania [101,104–108]. Chickens, pigs and two rat
species (*Rattus exulans* and *Rattus praetor*) comprised the domestic
and commensal animals at Teouma (S. Hawkins unpublished
data).

It remains uncertain exactly when many exotic domesticated
plant species were introduced by humans to the islands of Remote
Oceania, including Vanuatu. However, many cultivars were
established in Vanuatu prior to European contact, and it has
been speculated that a number of them were carried with the
initial Lapita colonists [109]. In terms of the plant foods available,
the tropical rainforest surrounding the Teouma site would have

provided a suitable area for swidden gardening, a process of
removing stands of rainforest for the fallow rotation of crops [109].
The underlying soil on South Efate is nutrient-rich because of the
volcanic tephra deposited before the arrival of Lapita populations
[31]. Although there is no direct evidence thus far regarding
horticulture at Teouma (the analysis of microfossils from human
dental calculus is currently underway), microfossil remains from
sites in Northern Vanuatu do provide evidence of horticulture in
Vanuatu in Lapita and post-Lapita settlements [20–22,24]. Starch
grains, phytoliths, calcium oxalate crystals and xylem cells have
been used to identify imported cultivated species including *Musa*
(banana), Araceae (aroids) and yam (*Dioscorea* spp.) in Lapita or
immediately post-Lapita layers on the islands of Uripiv and Vao
off the coast of northeast Malakula and on Epi Island. Some of
these sites also show evidence of a decrease in Arecaceae (palms)
and an increase in Poaceae (grasses), trends indicative of
vegetation clearance likely associated with human settlement and
horticultural activity [20–22].

Although there would have been some edible plants available
when people arrived in Vanuatu, the distribution and abundance
of these species is unknown [109,110]. A majority of the wild foods
probably available during the colonization of Remote Oceania
would have consisted of leafy greens, fruits and nuts [111].
Throughout the Pacific Islands, these types of food are typically
used to supplement meals, whereas starchy vegetables such as yam
and taro (in addition to breadfruit, *Artocarpus altilis*) comprise the
major constituents of meals [109,112]. Native plants used to
supplement meals in Vanuatu today include wild ferns, *Polyscias
scutellaria*, nuts including *Canarium* spp., and fruits such as *Gnetum*
<figure><img src="image_7.png" /><figcaption>**Figure 6.** Teouma human δ¹³C and δ¹⁵N values in relation to a tropical Pacific island dietary baseline. The full and dotted circles designate a trophic effect of 1.0‰ for δ¹³C and 3.0‰ for δ¹⁵N and 1.0‰ for δ¹³C and 5.0‰ for δ¹⁵N respectively. Note that the modern δ¹³C values have been corrected for the Suess effect. The asterisks (*) denote the inclusion of faunal stable isotope data from other tropical Pacific paleodietary studies (see text for references).</figcaption></figure>

doi:10.1371/journal.pone.0090376.g006

gnemon and Ficus spp. [110,113]. It must be noted that the large size of fruits and nuts and high yields of arboricultural crops found today throughout the Pacific are a result of thousands of years of selection and cultivation by humans [113]. Remains of coconut (Cocos nucifera) dating to ca. 5000 BP have been found on Aneityum Island in the south of Vanuatu [114] and coconut would likely have also been present on Efate when Lapita populations first arrived. Vanuatu was also the center of domestication of kava (Piper methysticum), but this plant is used for its medicinal and psychoactive properties and is not a food item [115]. Of the numerous starchy root vegetables eaten regularly in Vanuatu, the five-finger yam (Dioscorea pentaphylla) is the only edible tuber suggested to be endemic to the island group and is not a major dietary item anywhere today [109]. Certain non-native plants used for medicinal purposes or eaten infrequently today in Vanuatu (e.g. in times of famine or severe food shortage), such as cycas (Cycas seemannii), sago (Metroxylon sp.), kudzu (Pueraria lobata), wild yam (Dioscorea nummularia), and Cordyline spp. may have been consumed more regularly during prehistory [111, 116, 117] but were replaced when less labor intensive, higher yielding crops were established.

## Materials and Methods

### Ethics Statement

All necessary permits were obtained for the described study, which complied with all relevant regulations. Research agreements were signed between S. Bedford and M. Spriggs, the Vanuatu

Kaljoral Senta and the Vanuatu Cultural Council, which included permission to excavate the Lapita site at Teouma, Efate Island, Vanuatu. The permits for exporting the human and faunal remains from the Teouma archaeological site were issued by the Vanuatu Kaljoral Senta and the Vanuatu Cultural Council (export permit numbers 11/VLI/04, 04/VLI/05, 14/VLI/06, 17/VLI/08, 08/VLI/09 and 09/VLI/2010). The prehistoric human remains are currently curated at the Vanuatu Kaljoral Senta, Port Vila, Vanuatu. The prehistoric faunal assemblage is curated by the School of Archaeology and Anthropology at the Australian National University, Canberra, Australia with the exception of the excess bone left over from stable isotope analysis (n = 73), which is stored in the Department of Anatomy, University of Otago, Dunedin, New Zealand. Modern plant and animal samples from Vanuatu were collected on private land with permission from private landowners and chiefs. Only modern wild animals (no domestic species) were sampled and no protected species were collected. All samples imported from Vanuatu (modern) or Australia (prehistoric) to the transitional facility at the University of Otago, Dunedin, New Zealand, were sent under the MAF (Biosecurity New Zealand Ministry of Agriculture and Forestry) Permit to Import Restricted Biological Products of Animal Origin (2011 permit number 2011041970) and the Permit to Import Laboratory Specimens (2011 permit number 2011041930). The modern plant and animal material is currently stored in a PC2 laboratory at the Department of Anatomy, University of Otago, Dunedin, New Zealand. All specimen numbers are detailed in full in Tables S1, S2 and S3.
<figure><img src="image_8.png" /><figcaption>**Figure 7.** Teouma human, faunal, and floral δ¹³C and δ³⁴S (A) and δ¹⁵N and δ³⁴S (B) values. Note that the modern δ¹³C values have been corrected for the Suess effect.
doi:10.1371/journal.pone.0090376.g007</figcaption></figure>

## Materials and Methods

Cortical bone was sampled from fifty-one adult individuals from Teouma. The carbon and nitrogen stable isotope values from thirty-three of these individuals have been previously reported in Valentin et al. [32] (Table S1). The age and sex of the Teouma

adults were estimated using standards found in Buikstra and Ubelaker [118].

Prehistoric faunal samples from pig (*Sus scrofa*, n = 18), chicken (*Gallus gallus*, n = 5), tortoise (? *Meiolania damelipi*, n = 16), sea turtle (n = 3), and fruit bat (Pteropodidae, n = 20) were analyzed to create the prehistoric dietary baseline for this study. In addition to
the samples collected for this study, previously published stable isotope data from eleven prehistoric animals from Teouma (n = 2 pigs, n = 2 chickens, n = 2 tortoises, n = 2 rats, n = 2 fruit bats, and n = 1 reef fish) were also included in the dietary baseline to increase the sample size [32,102,119] (Table S2). Additionally, modern plants (n = 68) and animals (n = 30) were collected from Efate Island and northeast Malakula, Vanuatu (Table S3), and analyzed for carbon, nitrogen, and sulfur stable isotope ratios to provide further environmental baseline data. To account for the global decrease in ¹³C after the Industrial Revolution (i.e. the Suess effect), modern Pacific island plant and animal δ¹³C values within the baseline data were corrected by +1.5‰ for terrestrial and +.86‰ for marine systems [26,120]. Very few aquatic animals from Vanuatu could be sampled for this study; therefore, published isotope values of Pacific island marine fish bones, seaweed (macroalgae), marine turtle bones and freshwater organisms were also included in the dietary baseline [27,30,94,121–125].

Modern bone, plant, and shellfish flesh samples were rinsed in distilled water and defatted in methanol and chloroform (2:1 v/v) until lipids were removed at the University of Otago (Dunedin, New Zealand) [126]. Plant and flesh samples were then lyophilized and weighed before isotopic analysis. The method used to extract the collagen from the bone samples prepared at the University of Otago followed the Longin [127] method modified by Brown et al. [128] and Collins and Galley [129] described in detail in Kinaston et al. [33]. Collagen was purified from the bone samples prepared at Aix-Marseille University (Marseille, France) using the Longin [127] method modified by and described in Bocherens et al. [130]. The purified “collagen” was analyzed by EA-IRMS at Iso-Trace (Dunedin, New Zealand) or Iso-Analytical (Cheshire,

United Kingdom) (cf. Table S1). Analytical error was routinely ±0.10‰ for δ¹³C, ±0.20‰ for δ¹⁵N, and ±0.30‰ for δ³S.

## Results and Discussion

The following sections present the stable isotope data, offering interpretations of the isotope values within the context of what is known about Vanuatu island ecology, in addition to addressing the hypotheses.

### Preservation of archaeological samples

An initial crucial step in the interpretation of these data was to assess the quality of the collagen to determine which samples could be included in subsequent analyses. In contrast to Valentin et al. [32] – who excluded ten individuals from their statistical analyses and dietary interpretations because the samples did not reach specific collagen quality indicators (i.e. wt %C higher than 30.0%, wt%N higher than 11.0%) [131] although their C:N ratios were between 2.9 and 3.6 described by DeNiro [132] as well-preserved – we have only rejected the two individuals (burials 63 and 64) with C:N values outside of 2.9 and 3.6. As outlined in White and Schwarcz [133] a significant correlation between C:N ratios and 1) δ¹³C values and 2) δ¹⁵N values may be indicative of post-depositional diagenetic alteration of collagen. No significant correlations between these variables were observed for the ten individuals removed by Valentin et al. [32] and burials 51 and 53 from the later analyses (n = 12; Spearman's r = 0.233, p = 0.469; Spearman's r = -0.201, p = 0.531, respectively) or the other ‘well-preserved’ individuals (n = 44; Spearman's r = -0.004, p = 0.978; Spearman's r = 0.269, p = 0.078). Thus, the adequate C:N ratios and the lack of a significant correlation between these variables in addition to the fact that any ‘outlier’ displayed wt %C over 30%

<figure><img src="image_9.png" /><figcaption>**Figure 8.** Comparison of Teouma δ¹³C and δ¹⁵N with other Pacific paleodietary studies (see text for references). Spearman's correlation of δ¹³C and δ¹⁵N values of adult humans from Teouma, Vanuatu (n = 49, r = -0.210, p = 0.148), Taumako, Solomon Islands (n = 96, r = 0.541, p < 0.001), Cikobia, Fiji Islands (n = 8, r = 0.651, p = 0.081), Rota, Mariana Islands (n = 10, r = 0.838, p = 0.002), and Saipan, Mariana Islands (n = 8, r = 0.723, p = 0.043).</figcaption></figure>

doi:10.1371/journal.pone.0090376.g008
and wt %N over 11% [131] suggest that the collagen of all the individuals except two (burials 63 and 64) was not affected by diagenetic alteration or post-depositional contamination. (Table S1). Ten of the human collagen samples analyzed for sulfur stable isotope ratios did not reach the sulfur collagen quality criteria outlined in Nehlich and Richards [134] (C:S ratio of 600±300, a N:S ratio of 200±100 and a wt %S lower than 60%) and were removed from subsequent analyses.

Of the most recently analyzed prehistoric faunal samples, all the animals reached the quality collagen indicators used in previous publications with the exception of two animals (a tortoise and a sea turtle), which displayed C:N ratios higher than 3.6 and were removed from the following analyses. The pig (*Sus scrofa*) and reef fish (*Scaridae*) that were removed from the Valentin et al. [32] study because they did not meet the collagen quality criteria were included in this study as their C:N ratios were between 2.9 and 3.6. All of the samples analyzed for sulfur stable isotope ratios reached the collagen quality indicators outlined in Nehlich and Richards [134] and described above. It must be noted that non-mammalian (e.g. tortoise) and mammalian bone collagen may display naturally differing collagen wt %C, wt %N and wt %S compositions. Therefore collagen quality indicators may be species-dependent [131,134,135].

## Dietary baseline: modern plants and animals

The stable isotope ratios of modern plants and animals found in the local food web were used to develop a dietary baseline to interpret the potential diet of the human and prehistoric fauna. The collection location, raw data and the summary statistics for the carbon, nitrogen and sulfur stable isotope ratios of the modern floral and faunal samples analyzed in this study are located in Supplementary Table S3 and Table 1 respectively.

Figure 3 details the carbon and nitrogen stable isotope values of the modern plants and animals from Vanuatu that were analyzed for this study. The modern δ¹³C and δ¹⁵N values of C₃ and C₄ plants from Vanuatu are similar to those found in the Marianas [94] and the Cook Islands [121]. Using a two-sample t-test assuming unequal variance (Levene's test *p* = 0.037), there was a tendency for δ¹⁵N values of the nuts to be higher than the non-nut C₃ plant species (diff 1.5‰, *p* = 0.053). The δ¹³C and δ¹⁵N values of the modern fruit bat confirm that this animal ate fruits, flowers, nectar and insects from a C₃-based terrestrial environment.

Seagrass δ¹³C and δ¹⁵N values were similar to those observed by Fry et al. [136] and Keegan and DeNiro [63]. Some C₃ marine plants, including seagrasses and coral reef algae, have demonstrated δ¹³C values similar to plants with a C₄ photosynthetic pathway and this is the case for the *Thalassia hemprichii* and *Syringodium isoetifolium* species analyzed in this study [64,137,138]. Coral reef, seagrass and mangrove ecosystems display low δ¹⁵N values as a result of a prevalence of N₂-fixing bacteria in these environments [60,63,64]. Accordingly, the shellfish (n = 3) and crabs endemic to mangroves (n = 2) displayed low average δ¹⁵N values ranging from -9.5‰ to 2.9‰ but, as a result of their C₃ mangrove environment, exhibited terrestrial δ¹³C values ranging from -28.9‰ to -24.1‰.

The δ¹³C values of the marine shellfish from environments outside the mangroves (n = 15) were, on average, lower than the δ¹³C values of limited number (n = 7) of tropical species analyzed in other studies, although their δ¹⁵N values were similar [26,125]. The variation between studies is likely a result of the small number of samples analyzed, species-specific isotope variation, environmental factors and differences in defatting protocols. Eight marine fish (two reef fish, two fish with variable feeding areas, two pelagic tuna and two pelagic sardines) were sampled. On average, the reef

fish and low trophic level pelagic species (sardines) displayed the lowest δ¹⁵N values; the higher trophic level deep-water species (tuna) displayed the highest δ¹⁵N values; and the species that utilized both environments displayed intermediate values. It must be noted that the pelagic fish in this study (all tuna) displayed lower δ¹⁵N values compared with pelagic fish and sea mammals analyzed in other studies [27,30,94,123], likely a reflection of the specific taxa, fish size and feeding environment. Otherwise, the carbon and nitrogen stable isotope values of the marine fish species analyzed in this study generally agreed with those observed by other Pacific island stable isotope studies that analyzed tropical fish bone [26,27,30,121–123]. It is difficult to compare the isotope values of the modern turtle bone with those presented by other studies because of the potential isotopic variation resulting from age-specific foraging strategies and migratory patterns of species such as *Chelonia mydas* (green turtle) and *Eretmochelys imbricate* (hawksbill turtle) [139,140]. The high δ¹³C values of the modern marine turtle bone (-9.7‰) in this study indicate that this animal likely fed in ¹³C enriched environments, such as seagrass meadows and coral reefs.

The average δ³⁴S value of the modern terrestrial plants ranged from 3.7‰ to 15.7‰ (average 9.5‰±4.0‰). As previously mentioned, marine-derived precipitation and sea-spray can raise the δ³⁴S values of terrestrial plants and animals, an effect of marine sulfates (averaging ~21.0‰) entering coastal food webs [53,83]. The elevated δ³⁴S values of the modern Vanuatu plants are likely a result of this sea-spray effect. The large variation in terrestrial δ³⁴S values is most likely associated with garden location, with the plants displaying the low δ³⁴S values originating from inland gardens further away from the coast. The δ³⁴S value of the modern fruit bat (11.0‰) further indicates that marine-derived sulfates have affected the local terrestrial food web as these animals consume purely terrestrial resources. Elevated terrestrial plant and animal δ³⁴S values have been observed in other Pacific island paleodietary studies [26,27], indicating that sea-spray may influence terrestrial sulfur stable isotope ratios and thus potentially affect subsequent dietary interpretations.

Primary producers at the base of marine food webs exhibit δ³⁴S values ranging from +17‰ to +21‰ [80,84]. All of the modern fish analyzed for sulfur stable isotope ratios fell within this range. The lower δ³⁴S values of the seagrass (14.0‰), marine turtle (13.6‰), marine shellfish (14.9‰), crab (9.4‰) and mangrove shellfish (average -8.7‰) analyzed in the current study are likely a result of environmental conditions such as the proximity to mangroves and the effect of terrestrial detritus [141,142]. Plants living in anaerobic sediments found in mangroves and seagrass meadows utilize ³⁴S-depleted sulfides and display low δ³⁴S values [143] and the action of sulfate-reducing bacteria in anoxic marine sediments has been suggested as a reason for low δ³⁴S values of marine mammals in northern Europe [141]. The exceptionally low δ³⁴S value of one species of mangrove bivalve (*Anodonta philippiana*) (-21.5‰) is likely a reflection of its chemosymbiotic relationship with sulfide-oxidizing bacteria living in its gills [144] and, as these species are widespread [145], should be taken into consideration when assessing diet using sulfur stable isotope ratios where relevant. We do not believe that modern pollutants have influenced the marine or terrestrial δ³⁴S values [86] as the areas of Vanuatu where these samples were collected are not industrialized.

## Dietary baseline: Prehistoric fauna

The stable isotope values of the prehistoric fauna analyzed from the site of Teouma provide further baseline information about the foods available to the humans living in the settlement. An
<figure><img src="image_10.png" /><figcaption>**Figure 9.** Teouma male and female δ¹³C and δ¹⁵N values. Spearman's correlation of δ¹³C and δ¹⁵N values of adult males (black line, n=23, r=-0.500, p=0.015) and females (dotted line, n=25, r=0.161, p=0.443) from Teouma.
doi:10.1371/journal.pone.0090376.g009</figcaption></figure>

assessment of the diet of domesticated animals also has the potential to provide information about the management of these species, especially pigs, and about how the humans and animals interacted within their shared environment. A potential outcome of analyzing the wild faunal resources is that their isotope values are a reflection of the ecological niches in which they live that may vary over time partly as a consequence of human impact on the environment.

The isotope results for the fauna from Teouma are located in Supplementary Table S2 and Figure 4. Summary statistics for the prehistoric animals from Teouma are presented in Table 2. The mean (±1 SD) δ¹³C value of the prehistoric fruit bats (−19.8‰±0.4‰, n = 22) confirmed that these animals were primarily eating foods from C₃-based environments [146]. The prehistoric fruit bat values are in agreement with other studies that suggest the δ¹³C value of a purely terrestrial diet to be ~20.0‰±1.0‰ [35,123]. There was a large variation in fruit bat δ¹⁵N values, ranging from 3.0‰–8.4‰ which may be the result of specific feeding strategies as some environments, such a mangroves, can exhibit variable δ¹³C and δ¹⁵N values depending on their location relative to the coast [147]. However, we suggest that a likely cause of the observed variation in δ¹⁵N values is the result of the inclusion of insect-eating bats in our study. Megabats (Pteropodidae) commonly feed on fruit, nectar and flowers but are also known to be insectivorous [146,148]. There are twelve species of bat found throughout Vanuatu today, three of which are megabats [149,150]. However, several distinct and as yet unidentified fruit bat species from the Pteropodidae family have been identified from the Teouma, Uripiv and Vao (northeast Malakula, Vanuatu) archaeological sites. Now-extinct species are most certainly present in these assemblages and variations in bat δ¹⁵N values could reflect differences in ecological adaptations from these various bat species (S. Hawkins, unpublished data).

The average δ¹⁵N values of the fruit bats increased by 1.0‰ from the Lapita to late Lapita period, but only 0.2‰ between the

late Lapita and the post-Lapita periods (note that the sample sizes were too small to conduct statistical analyses). These differences may be a result of the human establishment of fruit-bearing arboricultural species with different δ¹⁵N values compared to native trees, vegetation change resulting from climate change or human disturbance [151], or it may just be that more insectivorous bats were present in the later assemblages. The presence of nursing or juvenile individuals in the sample, which would result in the enrichment of ¹⁵N in the infant bats' tissues, could also be responsible for the observed variation of δ¹⁵N values in these animals [148,152].

The average δ¹³C values of the tortoise, another purely terrestrial species, are 3.6‰ lower compared with the average fruit bat δ¹³C values, which may be related to the ecological zones they utilized or possibly a physiological effect. Plants that grow under the forest canopy display low δ¹³C values as a result of recycling ¹³C-depleted CO₂ from decomposing forest floor litter during photosynthesis, a phenomenon known as the 'canopy effect' [153,154]. Thus, the consumption of plants under the rainforest canopy by tortoises may account for their low δ¹³C values. Nine of the tortoises displayed δ¹⁵N values lower than 4.0‰ (n = 3/10 from the Lapita assemblage, n = 4/4 from the late Lapita assemblage and n = 2/3 from the disturbed assemblage), whereas the other eight tortoises displayed values higher than 5.5‰ (n = 7/10 from the Lapita assemblage and n = 1/3 from disturbed layers). Although the sample sizes are small, this trend may be indicative of changing environmental conditions as a result of human settlement. The δ¹³C values of all tortoises were very similar (−23.4‰±0.5‰, n = 17) and therefore the variation in δ¹⁵N values is likely a result of the regular consumption of foods from different trophic levels. Higher trophic level foods could have included insects and freshwater organisms such as crustaceans, mollusks and freshwater fish. The tortoises that displayed the lowest δ¹⁵N values may have utilized the mangrove environment for food as their values were similar to mangrove shellfish and
crabs. It is difficult to extrapolate on the dietary breadth of these
extinct animals, but the variation in δ¹³N values may point
towards age-related dietary variations or diverse foraging envi-
ronments. Evidence from the ongoing faunal studies suggests that
the Teouma human population was forced to target ever more-
distant tortoise populations as high levels of predation led to
depletion of resources closer to the site (S. Hawkins, unpublished
data).

The domestic and commensal species displayed δ¹³C values that indicate that their diets were highly terrestrial (pig = −19.6‰±0.7‰, n = 20, chicken = −19.7‰±1.1‰, n = 7 and rat = −19.2‰±0.4‰, n = 2), although some animals displayed a minor marine signal. These values suggest that they were either fed C₃ terrestrial foods by humans, such as cultivated plants, or allowed to forage for food in the C₃ environments surrounding Teouma, such as the rainforest. The limited marine input into both the Lapita and immediately post-Lapita domestic animal diets at Teouma may be indicative of some type of controlled feeding (even of wild resources) or penning away from the settlement, meaning they were unable to access marine food scraps. Another interpretation is that the marine foods consumed by humans such as shellfish and soft-shelled crustaceans left few edible remains.

The δ¹⁵N values of the domestic and commensal species are higher compared with the values of tortoises and fruit bats, suggesting consumption of these local animals (e.g. from human food scraps) or other terrestrial organisms such as insects [155], native animals such as small lizards and snakes [149] or human feces. Pigs practice caecotrophy and the regular consumption of human feces could result in the elevation of pig δ¹⁵N values [156]. The pigs from the immediately post-Lapita assemblage displayed slightly higher δ¹³C values (0.1‰) and higher δ¹⁵N values (0.5‰) compared with the same taxa in the Lapita assemblage. This dietary variation suggests that the pig population consumed resources from higher trophic levels in the later period. The post-Lapita chicken displayed a δ¹⁵N value that was 1.5‰ higher and a δ¹³C value that was 1.0‰ higher than the chickens (n = 6) from the Lapita period, although it is noted that these sample sizes are very small, preventing us from making meaningful inferences regarding temporal changes in chicken diet.

The prehistoric fauna from Teouma displayed a trend in δ³⁴S value similar to the modern terrestrial plants and fruit bats. The land-based tortoise, a species undoubtedly consuming a terrestrial-based diet, exhibited δ³⁴S values indicative of the sea-spray effect (11.0‰±0.8‰, n = 4). The δ³⁴S values of the domestic species (pigs and chickens) all ranged between 9.7‰ and 13.0‰. The δ¹³C values of the domestic animals are representative of a predominately terrestrial-based diet, further supporting the suggestion that the sea-spray effect influenced their δ³⁴S values. As the site was directly on the coast, this result is not entirely surprising, but does indicate that all species were affected similarly.

The δ¹⁵N values of the domestic animals are comparable with the highest values for the bats or are elevated compared to the bats indicating they were eating terrestrial resources from higher trophic levels. The domestic animal isotope data may be indicative of controlled feeding of C₃ horticultural foods and terrestrial animal remains as hypothesized by Valentin et al. [32] but could also suggest that pigs and chickens relied heavily on foraging for wild foods, especially insects, and human feces. If the latter is the case, the data support the proposition by Clark et al. [157: 9] that during colonization the low population density and limited established garden areas would allow for "the presence of a free range scavenging pig population under benign environmental conditions".

The presence of pigs at Lapita sites has previously been used as a proxy for horticulture [158,159], but depending on the size of the pig and human populations horticulture is not necessarily a prerequisite for keeping pigs due to their ability to forage [160,161]. Feral pig populations survive throughout Vanuatu, including on Efate Island, indicating that if released, pigs could have survived without the assistance of humans [149]. In New Guinea, pig husbandry methods range from the complete control of pig fodder by humans (sometimes dedicating a large proportion of vegetable crops to pigs) to completely relying on pigs to forage for their own food [161].

Human diet at Teouma

The isotope data and demographic information for the humans are located in Supplementary Table S1. Summary statistics for the human data are located in Table 3. Figures 5 and 6 detail the human isotope values (δ¹³C and δ¹⁵N) in relation to the prehistoric faunal remains from Teouma and a wider Pacific dietary baseline, including the modern Vanuatu data.

It is generally accepted there is a trophic increase between 0–2.0‰ for δ¹³C and 3.0–6.0‰ for δ¹⁵N values between predator/prey bone collagen [88,89]. The average human δ¹³C values were 3.9‰ higher compared with the δ¹³C values of the combined commensal species (pigs, rats and chickens) from all layers, indicating that they were eating these domestic species. A similar difference in δ¹³C values was observed between the humans and the endemic fruit bats (humans 4.1‰ higher), but this difference was much larger between the human and the tortoises (humans 7.7‰ higher). The average human δ¹⁵N values were 2.2‰ higher compared with the commensal species and much higher compared with the native species (humans 6.9‰ higher for the fruit bats and 7.2‰ higher for the tortoises). The low δ¹³C and δ¹⁵N values of the tortoise compared with the stable isotope values of the humans indicate these animals did not constitute a major dietary resource at Teouma during the cemetery phase.

It has previously been posited that land-based tortoises were hunted in preference to the marine turtles until their disappearance some 300 or so years after initial settlement as a result of human predation [102]. In fact, further faunal analysis has now shown that fruit bats, marine turtles, and tortoises were initially heavily targeted in close proximity to the site resulting in resource depletion and the subsequent subsistence change towards more mobile foraging tortoises (S. Hawkins, unpublished data). The δ¹³C and δ¹⁵N values of the humans support the faunal analysis evidence, specifically that the commensal animals and fruit bats constituted the major terrestrial protein resources at Teouma in the early cemetery phase.

The higher δ¹³C values of the humans compared to the commensal and native species indicates that ¹³C-enriched protein resources were also being consumed, most likely from the marine environment. Comparison with the dietary baseline data suggests that the people at Teouma were likely accessing resources from the reef in addition to sea turtle and possibly deeper-water species of fish. Inshore organisms are also likely to have been eaten, but their contribution is most visible when a larger trophic offset for δ¹⁵N (5.0‰) is used to interpret the human diet. The consumption of inshore organisms is typical of early Lapita sites, indicating foraging for nearby, easily accessible resources [7,8,162,163]. In addition, reef and inshore species of fish are well-represented in Lapita middens across the western Pacific [30,164]. Few remains of pelagic species or of deep-sea trolling fishhooks are found at Lapita sites (including Teouma), supporting the suggestion that the elevated δ¹³C and δ¹⁵N values are more likely a result of the consumption of marine turtle than deep-water fish.
The identification of sea turtle exploitation is difficult because of the large variation in stable isotope values for these animals [discussed in 32]. However, the consumption of marine turtle likely contributed to the elevated δ¹³C and δ¹⁵N values of the humans as these animals are well-represented in some early Vanuatu faunal assemblages [162,165], including Teouma (S. Hawkins unpublished data).

Mangrove, freshwater and C₄ plant resources (i.e. sugarcane) cannot be ruled out of the dietary interpretations but do not appear to contribute substantially to the diet at Teouma. Freshwater species display similar δ¹³C values to terrestrial ecosystems but higher δ¹⁵N values [125]. The freshwater stream running adjacent to the site may have provided access to freshwater fish, shellfish and other aquatic organisms [31], although, as a result of geographic isolation, both freshwater and mangrove species diversity is limited in Vanuatu [166,167]. To address this issue it would be necessary to analyze modern freshwater organisms in the Teouma area.

Sugarcane (Saccharum officinarum), the only C₄ terrestrial domesticated plant known in the Pacific Islands, or *Portulaca lutea*, an edible indigenous CAM/C₄ plant [121,168], may have also influenced the δ¹³C values observed in the Teouma sample. However, because sugarcane has a high carbohydrate and low protein content its consumption may not be well reflected in bone collagen stable isotope values [169].

The human sulfur isotope data are presented in Figure 7. The human δ³⁴S values were 0.1‰ higher compared with the commensal species and 0.3‰ higher compared with the tortoise values. The δ³⁴S values of the humans and fauna from Teouma are not consistent with the dietary patterns observed in the carbon and nitrogen stable isotope results. Confirming previous suggestions [26,27], the δ³⁴S values of the terrestrial plants and animals (both modern and prehistoric) in addition to the similarity of human and faunal isotopic values strongly indicate that the local food web was influenced by the sea-spray effect. As a result of this effect and large variations in the local ecosystem's δ³⁴S values (e.g. mangrove organisms), it is difficult to use sulfur stable isotope ratios to differentiate between marine and terrestrial dietary components for the Teouma individuals and more generally for skeletal populations residing in coastal areas.

The range in human δ¹³C and δ¹⁵N values in addition to the lack of any significant positive correlation for the sample (n = 49, Spearman's r = -0.210, p = 0.148) suggest that the population was subsisting on marine and terrestrial protein resources from similar trophic levels as one another, a different dietary pattern from that observed in later prehistoric Pacific island populations. For example, a statistically significant positive correlation between the δ¹³C and δ¹⁵N values of humans from the Polynesian outlier site of Taumako in the Solomon Islands (n = 96, Spearman's r = 0.541, p < 0.001) and the range of δ¹³C and δ¹⁵N values (–16.4‰ ± 0.6‰ and 11.5‰ ± 0.9‰) indicated that their diet consisted of low trophic level plants (likely starchy root vegetables) and higher trophic level marine resources [33]. Similar dietary interpretations were posited for eight prehistoric/historic adult individuals from Cikobia in the Fiji Group, who exhibited low δ¹³C and δ¹⁵N values (–17.2‰ ± 0.4‰ and 9.6‰ ± 0.4‰ respectively), but maintained a positive, albeit insignificant, correlation between δ¹³C and δ¹⁵N values (n = 8, Spearman's r = 0.651, p = 0.081) [35]. In the Mariana Islands, the strong positive correlation between the bone collagen δ¹³C and δ¹⁵N values of the inhabitants of Rota (–18.1‰ ± 1.1‰ and 9.0‰ ± 1.3‰, n = 10, Spearman's r = 0.838, p = 0.002) and Siapan (–18.6‰ ± 0.3‰ and 7.8‰ ± 0.9‰, n = 8, Spearman's r = 0.723, p = 0.043) indicated that their protein diet consisted of a high

proportion of starchy root vegetables and a lesser amount of marine protein [94] (fig. 8). Based on the analysis of the bone carbonate of the Marianas individuals it was suggested that C₄ plants such as sugar cane or seaweeds were also consumed but these plant foods could not be identified using the stable isotope analysis of bone collagen because of their low protein content [94,170].

The results from the human isotopic analyses support the interpretation of the dietary pattern proposed by Valentin et al. [32], specifically that the Lapita people from Teouma were primarily subsisting on reef foods, some higher trophic level marine animals (likely marine turtle), some inshore organisms and terrestrial animal protein resources, most importantly commensals and fruit bats. Comparison of the human isotope values with those of the fruit bat δ¹³C values (representing a purely C₃ plant and insect diet) indicates that C₃ plant foods did not constitute a major protein resource for the humans at Teouma. The lack of significant amounts of C₃ plants in the human diet supports the assumption that horticulture was likely being established at this early stage and was less important to the overall diet compared with populations later in prehistory. The first hypothesis – that the people from Teouma were eating more local wild resources compared to domestic species and horticultural plants – is not falsified. However, in addition to these wild resources, domestic animals are also likely to have been important protein resources. The stable isotope data suggest that the subsistence strategy at the site was focused on foraging for wild marine and terrestrial resources while raising and eating domestic animals. These domestic species may have been raised using a free-range system of animal husbandry, reducing the competition between pigs and humans for the limited horticultural plant foods likely being grown at the time.

## Sexual differences in diet

Summary statistics for the males and females are presented in Table 3.

Compared with the females, the males displayed a larger range of both δ¹³C and δ¹⁵N values (female δ¹³C range –18.6‰ to –13.6‰ and male δ¹³C range –19.3‰ to –13.8‰, female δ¹⁵N range 10.4‰ to 13.0‰ and male δ¹⁵N range 11.0‰ to 16.1‰) (fig. 9). Using a two-sample t-test assuming equal variance (Levene's test *p* = 0.206), males displayed significantly higher δ¹⁵N values compared to females (12.7‰ vs. 11.6‰, *p* < 0.001, male n = 23, female n = 25), but no significant differences were observed between the sexes in δ¹³C or δ³⁴S values. Similar results were observed in Kinaston et al. [171], but the analysis of a larger sample of individuals from the site confirms that this dietary difference between the sexes is very important for understanding possible socio-cultural practices at this Lapita site.

Therefore, the stable isotope evidence supports the second hypothesis, that males and females had different diets. The stable isotope analysis indicates that males were consuming a more variable diet and higher trophic level protein resources than women. This trend suggests sexual differences in food consumption patterns. These dietary patterns may be representative of the differential roles of food acquisition between the sexes, with the males hunting and fishing while the women primarily gathered foods and foraged in the inshore environment. These gendered patterns of food acquisition have been observed in modern-day Pacific island communities [44,112,163,172–174] and in late prehistoric populations from Papua New Guinea through to Polynesia [33,40].

Alternatively, the observable difference between male and female diets may indicate that food distribution was culturally
moderated and may suggest preferential treatment of males in the society, at least with regard to food access. In modern-day Pacific island cultures protein-rich animal foods are highly valued. Choice cuts of pig and chicken and relatively scarce marine foods (e.g. turtle and shark) are traditionally restricted to high status men within many communities [43,47,112,163,172]. It is possible that males at Teouma were considered of a higher status and thus receiving differential treatment to the women, expressed here in the unequal distribution of food resources, perhaps supporting the premise that Lapita societies were ranked in some way.

## Conclusions

The stable isotope analysis of the Teouma cemetery sample presented here constitutes the largest paleodietary study of Lapita period humans to date. In conjunction with the stable isotope values of the modern plants and animals and prehistoric fauna, these data collectively represent the most comprehensive assemblage of information on the diet and subsistence strategies of these enigmatic colonizers.

The interpretation of the paleodiet at Teouma in the context of a comprehensive dietary baseline has assisted in clarifying food procurement strategies during the initial Lapita colonization of Efate. The dietary pattern observed at Teouma supports a mixed subsistence strategy which included broad-spectrum marine resource foraging, the consumption of wild animals, especially fruit bats, and animal husbandry. These data indicate that the protein resources eaten by these early colonists were procured by a 'strandlooping' mode of subsistence, but also that domestic animals were important at the site and were likely reared using a low-cost free-range system of animal husbandry. This interpretation does not discount the fact that horticultural foods were likely grown and eaten at Teouma, but rather suggests that these plants were not heavily relied upon during the earliest settlement phase in Vanuatu's prehistory.

It is known that Lapita populations brought with them a number of exotic domestic plants and animals as part of a 'transported landscape' that was necessary for the establishment of new settlements, but these early colonizers also had to adapt to increasingly sparse conditions as they moved eastward across the Pacific Ocean [7,175,176]. The ecology of each specific island, the type of domestic plant and animal species brought by the colonists and later arrivals, the time necessary to establish each crop type and the overall size of the settlement would all have been important factors affecting the success of horticulture and animal husbandry at each site. Depending on the type and number of cultivars brought to Efate initially and through trade or return voyaging after settlement, the establishment and production of imported plant foods (root crops and arboricultural species) would have taken time before yielding enough food to adequately provide for a fledgling community and their domestic animals. The stable isotope evidence may actually be the first direct evidence of a "low-cost free-range system" of animal husbandry as has been posited by Clark et al. [157: 9].

## References

1. Cohen MN (1989) Health and the Rise of Civilization. New Haven: Yale University Press.

2. Cohen MN, Armelagos GJ, editors (1984) Paleopathology at the Origins of Agriculture. Orlando: Academic Press.

3. Steckel R, Rose J (2002) The Backbone of History: Health and Nutrition in the Western Hemisphere. Cambridge: Cambridge University Press.

4. Denham T (2004) Early agriculture in the Highlands of New Guinea: an assessment of Phase 1 (c. 9000 bp) at Kuk Swamp. In: Attenbrow VJ, Fullagar R, editors. A Pacific Odyssey: Archaeology and Anthropology in the Western Pacific Papers in Honour of Jim Specht Records of the Australian Museum 29. Sydney: Australian Museum. 47-57.

The lack of a significant positive correlation between carbon and nitrogen isotope ratios for the overall sample in addition to the range of values observed for the Teouma humans is very different from the dietary patterns observed at sites later in prehistory where horticulture was heavily relied on, thus supporting the interpretation that these people were a truly colonizing group in Vanuatu. The finding of sex-related dietary variation has also added to the linguistic data by illuminating possible social-cultural factors affecting diet during the heretofore-enigmatic Lapita period of human colonization.

## Supporting Information

<caption>**Table S1** Demographic data, bone collagen δ¹³C, δ¹⁵N and δ³⁴S values, collagen quality indicators and laboratory specifics for the humans from Teouma.
(DOCX)</caption>

<caption>**Table S2** Bone collagen δ¹³C, δ¹⁵N and δ³⁴S values, temporal period and collagen quality indicators for the prehistoric fauna from Teouma.
(DOCX)</caption>

<caption>**Table S3** Modern plant and animal δ¹³C, δ¹⁵N and δ³⁴S values and area of collection in Vanuatu.
(DOCX)</caption>

## Acknowledgments

The Teouma Archaeological Project was a joint initiative of the Vanuatu National Museum and the Australian National University (ANU) directed by Dr. Stuart Bedford and Professor Matthew Spriggs of ANU and Mr. Ralph Regenvanu and Mr. Marcelin Abong the former and current Director of the Vanuatu Cultural Centre (VVC). We thank the chiefs, landowners and inhabitants of Eratap Village for their permission and support during the excavations. Many *filwokas* (fieldworkers) and staff at the VCC were essential in organizing and assisting with the excavations, in addition to disseminating information about the archaeology to the wider community. For this we are especially thankful to Richard Shing. *Tankyu tumas* to Kela Allen and Silas Alben for their invaluable assistance collecting the modern plant and animal samples and to the numerous chiefs and villagers from Efate Island and northeast Malakula who allowed access to their gardens for collection purposes. We would like to pay our respects to two important team members who have passed away: 'wan man blong droing' illustrator Fidel Yoringmal and Vanuatu Cultural Centre staff member Willy Damelip. We are indebted to the two anonymous reviewers who provided excellent feedback for the improvement of this paper. Special thanks go to Andy Brown and Aimee Foster for the permission to use the map of the Pacific Islands for Figure 1 and Lydia White for assistance with editing the final draft of this manuscript.

## Author Contributions

Conceived and designed the experiments: RLK HRB EH FV. Performed the experiments: RLK EH. Analyzed the data: RLK EH. Contributed reagents/materials/analysis tools: RLK HRB EH SB MS SH FV. Wrote the paper: RLK HRB SB MS SH EH FV.

5. Denham TP, Haberle SG, Lentfer C, Fullagar R, Field J, et al. (2003) Origins of agriculture at Kuk Swamp in the Highlands of New Guinea. Science 301: 189-193.

6. Golson J (1990) Kuk and the development of agriculture in New Guinea: retrospection and introspection. In: Yen DE, Mummery JMJ, editors. Pacific Production Systems: Approaches to Economic Prehistory. Canberra: Australian National University. 139-147.

7. Kirch PV (1997) The Lapita Peoples: Ancestors of the Oceanic World. Oxford: Blackwell.

8. Spriggs M (1997) The Island Melanesians: the Peoples of South-East Asia and the Pacific. Cornwall: Blackwell.
9. Summerhayes GR (2001) Defining the chronology of Lapita in the Bismarck Archipelago. In: Clark GR, Anderson AJ, Sorovi-Vunidilo T, editors. The Archaeology of Lapita Dispersal in Oceania, Terra Australis 17. Canberra: Pandanus Books. 25-38.

10. Bedford S, Sand C (2007) Lapita and Western Pacific settlement: progress, prospects and persistent problems. In: Bedford S, Sand C, Connaughton SP, editors. Oceanic explorations: Lapita and Western Pacific Settlement. Canberra: ANU Press. 1-15.

11. Summerhayes GR (2001) Lapita in the Far West: recent developments. Archaeology in Oceania 36: 53-63.

12. Green RC (1991) Near and Remote Oceania - Disestablishing 'Melanesia' in Culture History. In: Pawley A, editor Man and a Half: Essays in Pacific Anthropology and Ethnobiology in Honour of Ralph Bulmer. Auckland: The Polynesian Society. 491-502.

13. Yen DE (1990) Environment, agriculture and the colonisation of the Pacific In: Yen DE, Mummery JMj, editors. Pacific Production Systems. Canberra: Department of Prehistory, Research School of Pacific Studies. The Australian National University. 258-277.

14. Spriggs M (1993) Island Melanesia: The Last 10,000 Years. In: Spriggs M, Yen DE, Ambrose W, Jones R, Thorne A, et al., editors. A Community of Culture The People and Prehistory of the Pacific. Canberra: Australian National University. 187-205.

15. Groube LM (1971) Tonga, Lapita pottery, and Polynesian origins. Journal of the Polynesian Society 80: 278-316.

16. Green RC (1976) Lapita sites in the Santa Cruz Group. In: Green RC, Cresswell MM, editors. Southeast Solomon Island Cultural History: A Preliminary Survey Bulletin of the Royal Society of New Zealand no 11. Wellington: Bryce Francis Ltd. 245-265.

17. Kirch PV (2000) On the Road of the Winds: An Archaeological History of the Pacific Islands before European Contact. Berkeley: University of California Press.

18. Burley DV, Dickinson WR, Barton A, Shutler Jr R (2001) Lapita on the periphery: new data on old problems in the Kingdom of Tonga. Archaeology in Oceania 36: 89-104.

19. Kennett D, Andersen AJ, Winterhalder B (2006) The ideal free distribution, food production, and the colonization of Oceania. In: Kennett DJ, Winterhalder B, editors. Behavioral Ecology and the Transition to Agriculture. Berkeley: University of California Press. 265-288.

20. Horrocks M, Bedford S (2005) Microfossil analysis of Lapita deposits in Vanuatu reveals introduced Araceae (aroids). Archaeology in Oceania 39: 67-74.

21. Horrocks M, Bedford S (2010) Introduced *Dioscorea* spp. starch in Lapita and later deposits, Voa Island, Vanuatu. New Zealand Journal of Botany 48: 179-183.

22. Horrocks M, Bedford S, Spriggs M (2009) A short note on banana (*Musa*) phytoliths in Lapita, immediately Post-Lapita and modern period archaeological deposits from Vanuatu. Journal of Archaeological Science 36: 2048-2054.

23. Horrocks M, Nunn PD (2007) Evidence for introduced taro (*Colocasia esculenta*) and lesser yam (*Dioscorea esculenta*) in Lapita-era (c. 3050-2500 cal. yr BP) deposits from Bourewa, southwest Viti Levu Island, Fiji. Journal of Archaeological Science 34: 739-748.

24. Horrocks M, Nieuwoudt MK, Kinston RL, Buckley H, Bedford S (In Press) Microfossil and Fourier Transform InfraRed analyses of Lapita and post-Lapita human dental calculus from Vanuatu, Southwest Pacific. Royal Society of New Zealand DOI: 10.1080/03036758.2013.842177.

25. Davidson J, Leach F (2001) The Strandlooper concept and economic naivety. In: Clark GR, Anderson AJ, Sorovi-Vunidilo T, editors. The Archaeology of Lapita Dispersal in Oceania, Terra Australis 17. Canberra: Pandanus Books. 115-123.

26. Beavan-Athfield N, Green R, Craig JC, McFadgen B, Bickler S (2008) Influence of marine sources on ¹⁴C ages: isotopic data from Watom Island, Papua New Guinea inhumations and pig teeth in light of new dietary standards. Journal of the Royal Society of New Zealand 38: 1-23.

27. Leach BF, Quinn CJ, Morrison J, Lyon GL (2003) The use of multiple isotope signatures in reconstructing prehistoric human diet from archaeological bone from the Pacific and New Zealand. New Zealand Journal of Archaeology 23: 31-98.

28. Petchey F, Green R (2005) Use of three isotopes to calibrate human bone radiocarbon determinations from Kainapirina (SAC), Watom Island, Papua New Guinea. Radiocarbon 47: 181-192.

29. Petchey F, Spriggs M, Leach BF, Seed M, Sand C, et al. (2011) Testing the human factor: radiocarbon dating the first peoples of the South Pacific. Journal of Archaeological Science 38: 29-44.

30. Jones S, Quinn RL (2009) Prehistoric Fijian diet and subsistence: integration of faunal, ethnographic, and stable isotopic evidence from the Lau Island Group. Journal of Archaeological Science 36: 2742-2754.

31. Bedford S, Spriggs M, Buckley HR, Valentin F, Regenvanu R (2009) The Teouma Lapita site, South Efate, Vanuatu: a summary of three field seasons (2004-2006). In: Sheppard P, Thomas T, Summerhayes GR, editors. Lapita: Ancestors and Descendants. Auckland: New Zealand Archaeological Association Monograph 28. 215-234.

32. Valentin F, Buckley HR, Herrscher E, Kinston RL, Bedford S, et al. (2010) Lapita subsistence strategies and food consumption patterns in the community of Teouma (Efate, Vanuatu). Journal of Archaeological Science 37: 1820-1829.

33. Kinaston RL, Buckley HR, Gray A (2013) Diet and social status on Taumako, a Polynesian outlier in the Southeastern Solomon Islands. American Journal of Physical Anthropology 151: 589-603.

34. Privat KL, O'Connell TC, Richards MP (2002) Stable isotope analysis of human and faunal remains from the Anglo-Saxon cemetery at Berinsfield, Oxfordshire: dietary and social implications. Journal of Archaeological Science 29: 779-790.

35. Valentin F, Bocherens H, Gratuze B, Sand C (2006) Dietary patterns during the late prehistoric/historic period in Cikobia island (Fiji): insights from stable isotopes and dental pathologies. Journal of Archaeological Science 33: 1396-1410.

36. Ambrose SH, Buikstra J, Krueger HW (2003) Status and gender differences in diet at Mound 72, Cahokia, revealed by isotopic analysis of bone. Journal of Anthropological Archaeology 22: 217-226.

37. Keenleyside A, Schwarz H, Stirling L, Ben Lazreg N (2009) Stable isotopic evidence for diet in a Roman and Late Roman population from Leptiminus, Tunisia. Journal of Archaeological Science 36: 51-63.

38. Le Huray JD, Schutkowski H (2005) Diet and social status during the La Tène period in Bohemia: carbon and nitrogen stable isotope analysis of bone collagen from Kutná Hora-Karlov and Radovesice. Journal of Anthropological Archaeology 24: 135-147.

39. Ubelaker DH, Katzenberg MA, Doyon LG (1995) Status and diet in precontact highland Ecuador. American Journal of Physical Anthropology 97: 403-411.

40. Kinaston RL, Buckley HR, Gray A, Shaw B, Mandui H (2013) Exploring subsistence and cultural complexes on the south coast of Papua New Guinea using palaeodietary analyses. Journal of Archaeological Science 40: 904-913.

41. Bell FL (1931) The place of food in the social life of central Polynesia. Oceania 2: 117-135.

42. Firth R (1967) The Work of the Gods in Tikopia. New York: Humanities Press.

43. Leach H (2003) Did East Polynesians have a concept of luxury foods? World Archaeology 34: 442-457.

44. Oliver DL (1989) Oceania: The Native Cultures of Australia and the Pacific Islands. Honolulu: University of Hawaii Press.

45. Kirch P (2001) Polynesian feasting in ethnohistoric, ethnographic and archaeological contexts: a comparison of three societies. In: Dietler M, Hayden B, editors. Feasts: Archaeological and Ethnographic Perpectives on Food, Politics, and Power. Washington: Smithsonian Institution Press. 168-184.

46. Kirch P, O'Day SJ (2003) New archaeological insights into food and status: a case study from pre-contact Hawaii. World Archaeology 34: 484-497.

47. Pollock N (1986) Food classification in three Pacific societies: Fiji, Hawaii, and Tahiti. Ethnology 25: 107-117.

48. Bellwood P (1996) Hierarchy, founder ideology and Austronesian expansion. In: Fox JJ, Sather C, editors. Origins, Ancestry and Alliance: Explorations in Austronesian Ethnography. Canberra: Australian National University Press. 19-40.

49. Currie TE, Greenhill SJ, Gray RD, Hasegawa T, Mace R (2010) Rise and fall of political complexity in island South-East Asia and the Pacific. Nature 467: 801-804.

50. Hage P (1999) Reconstructing ancestral Oceanic society. Asian Perspectives 38: 200-228.

51. Hayden B (1983) Social characteristics of early Austronesian colonisers. Bulletin of the Indo-Pacific Prehistory Association 4: 123-134.

52. Katzenberg MA (2008) Stable isotope analysis: a tool for studying past diet, demography, and life history. In: Katzenberg MA, Saunders S, editors. Biological Anthropology of the Human Skeleton. Hoboken, New Jersey: Wiley-Liss. 413-441.

53. Richards MP, Fuller BT, Sponheimer M, Robinson T, Ayliffe L (2003) Sulphur isotopes in palaeodietary studies: a review and results from a controlled feeding experiment. International Journal of Osteoarchaeology 13: 37-45.

54. Schwarz HP, Schoeninger MJ (1991) Stable isotope analyses in human nutritional ecology. Yearbook of Physical Anthropology 34: 283-321.

55. Sealy J (2001) Body tissue chemistry and palaeodiet. In: Brothwell D, Pollard AM, editors. Handbook of Archaeological Sciences. Chichester: John Wiley and Sons. 269-279.

56. Hedges REM, Clement JG, Thomas CDL, O'Connell TC (2007) Collagen turnover in the adult femoral mid-shaft: modeled from anthropogenic radiocarbon tracer measurements. American Journal of Physical Anthropology 133: 808-816.

57. DeNiro MJ, Epstein S (1978) Influence of diet on the distribution of carbon isotopes in animals. Geochimica et Cosmochimica Acta 42: 495-506.

58. DeNiro MJ, Epstein S (1981) Influence of diet on the distribution of nitrogen isotopes in animals. Geochimica et Cosmochimica Acta 45: 341-351.

59. Minagawa M, Wada E (1984) Stepwise enrichment of ¹⁵N along food chains: further evidence and the relation between δ¹⁵N and animal age. Geochimica et Cosmochimica Acta 48: 1135-1140.

60. Schoeninger MJ, DeNiro MJ, Tauber H (1983) Stable nitrogen isotope ratios of bone collagen reflect marine and terrestrial components of prehistoric human diet. Science 220: 1381-1383.

61. Ambrose SH (1993) Isotopic analysis of paleodiets: methodological and interpretive considerations. In: Sandford MK, editor. Investigations of Ancient Human Tissue: Chemical Analyses in Anthropology. Philadelphia: Gordon and Breach. 59-130.
62. Katzenberg MA, McKenzie HG, Losey RJ, Goriunova OI, Weber A (2012) Prehistoric dietary adaptations among hunter-fisher-gatherers from the Little Sea of Lake Baikal, Siberia, Russian Federation. Journal of Archaeological Science 39: 2612-2626.

63. Keegan WF, DeNiro MJ (1988) Stable carbon and nitrogen isotope ratios of bone collagen used to study coral reef and terrestrial components of prehistoric Bahamian diet. American Antiquity 53: 320-336.

64. Yamamuro M, Kayanne H, Minagawa M (1995) Carbon and nitrogen stable isotopes of primary producers in coral reef ecosystems. Limnology and Oceanography 40: 617-621.

65. Schoeninger MJ, Moore K (1992) Bone stable isotope studies in archaeology. Journal of World Prehistory 6: 247-296.

66. Bashan Y, Holguin G (2002) Plant growth-promoting bacteria: a potential tool for arid mangrove reforestation. Trees 16: 159-166.

67. Craig OE, Biazzo M, Colonese AC, Di Giuseppe Z, Martinez-Labarga C, et al. (2010) Stable isotope analysis of Late Upper Palaeolithic human and faunal remains from Grotta del Romito (Cosenza), Italy. Journal of Archaeological Science 37: 2504-2512.

68. Nehlich O, Boric D, Stefanovic S, Richards MP (2010) Sulphur isotope evidence for freshwater fish consumption: a case study from the Danube Gorges, SE Europe. Journal of Archaeological Science 37: 1131-1139.

69. Nehlich O, Fuller BT, Jay M, Mora A, Nicholson RA, et al. (2011) Application of sulphur isotope ratios to examine weaning patterns and freshwater fish consumption in Roman Oxfordshire, UK. Geochimica et Cosmochimica Acta 75: 4963-4977.

70. Oelze VM, Koch JK, Kupke K, Nehlich O, Zäuner S, et al. (2012) Multi-isotopic analysis reveals individual mobility and diet at the Early Iron Age monumental tumulus of Magdalenenberg, Germany. American Journal of Physical Anthropology 148: 406-421.

71. Leach BF, Quinn CJ, Lyon GL (1996) A stochastic approach to the reconstruction of prehistoric human diet in the Pacific region from bone isotope signatures. Tuhinga: Records of the Museum of New Zealand Te Papa Tongarewa 8: 1-54.

72. Vika E (2009) Strangers in the grave? Investigating local provenance in a Greek Bronze Age mass burial using δ34S analysis. Journal of Archaeological Science 36: 2024-2028.

73. Nehlich O, Fuller BT, Márquez-Grant N, Richards MP (2012) Investigation of diachronic dietary patterns on the islands of Ibiza and Formentera, Spain: evidence from sulfur stable isotope ratio analysis. American Journal of Physical Anthropology 149: 115-124.

74. Linderholm A, Jonson CH, Svensk O, Lidén K (2008) Diet and status in Birká: stable isotopes and grave goods compared. Antiquity 82: 446-461.

75. Krouse HR, Levinson AA, Piggott D, Ueda A (1987) Further stable isotope investigations of human urinary stones: comparison with other body components. Applied Geochemistry 2: 205-211.

76. Trust BA, Fry B (1992) Stable sulfur isotopes in plants: a review. Plant, Cell, and Environment 15: 1105-1110.

77. Nriagu J, Rees CE, Mekhtiyeva VL, Lein AY, Fritz P, et al. (1991) Hydrosphere. In: Krouse HR, Grinenko VA, editors. Stable isotopes: natural and anthropogenic sulphur in the environment. Chichester: Wiley. 177-265.

78. Faure G (1977) Principles of Isotope Geology. New York: Wiley.

79. Peterson BJ, Howarth RW, Garritt RH (1985) Multiple stable isotopes used to trace the flow of organic matter in estuarine food webs. Science 227: 1361-1363.

80. Peterson BJ, Fry B (1987) Stable isotopes in ecosystem studies. Annual Review of Ecosystem and Systematics 18: 293-320.

81. Mekhtiyeva VL, Pankina RG, Gavrilov YY (1976) Distributions and isotopic compositions of forms of sulfur in water, animals, and plants. Geochemistry International 13: 82-87.

82. Canfield DE (2001) Biogeochemistry of sulphur isotopes. Review of Mineral Geochemistry 43: 607-636.

83. Rees CE, Jenkins WJ, Monster J (1978) The sulphur isotopic composition of ocean water sulphate. Geochimica et Cosmochimica Acta 42: 377-381.

84. Krouse HR, Herbert MK (1988) Sulphur and carbon isotope studies of food webs. In: Kennedy BV, LeMoine GM, editors. Diet and Subsistence: Current Archaeological Perspectives. Calgary: University of Calgary Archaeological Association. 315-322.

85. Kusakabe M, Rafter TA, Stout JD, Collie TW (1976) Sulphur isotope variations in nature. New Zealand Journal of Science 19: 433-440.

86. Richards MP, Fuller BT, Hedges REM (2001) Sulphur isotopic variation in ancient bone collagen from Europe: implications for human palaeodiet, residence mobility, and modern pollutant studies. Earth and Planetary Science Letters 191: 185-190.

87. Schoeninger MJ, DeNiro MJ (1984) Nitrogen and carbon isotopic composition of bone collagen from marine and terrestrial animals. Geochimica et Cosmochimica Acta 48: 625-639.

88. O'Connell TC, Kneale CJ, Tasevska N, Kuhne GGC (2012) The diet-body offset in human nitrogen isotopic values: a controlled dietary study. American Journal of Physical Anthropology 149: 426-434.

89. Bocherens H, Drucker D (2003) Trophic level isotopic enrichment of carbon and nitrogen in bone collagen: case studies from recent and ancient terrestrial ecosystems. International Journal of Osteoarchaeology 13: 46-53.

90. Ambrose SH, Norr L (1993) Experimental evidence for the relationship of the carbon isotope ratios of whole diet and dietary protein to those of bone collagen

and carbonate. In: Lambert JB, Grupe G, editors. Prehistoric Human Bone: Archaeology at the Molecular Level. Berlin: Springer-Verlag. 1-37.

91. Froehle AW, Kellner CM, Schoeninger MJ (2010) FOCUS: effect of diet and protein source on carbon stable isotope ratios in collagen: follow up to Warinner and Tüross (2009). Journal of Archaeological Science 37: 2662-2670.

92. Jim S, Ambrose SH, Evershed RP (2004) Stable carbon isotopic evidence for differences in the dietary origin of bone cholesterol, collagen and apatite: Implications for their use in palaeodietary reconstruction. Geochimica et Cosmochimica Acta 68: 61-72.

93. Kellner CM, Schoeninger MJ (2007) A simple carbon isotope model for reconstructing prehistoric human diet. American Journal of Physical Anthropology 133: 1112-1127.

94. Ambrose SH, Butler BM, Hanson DB, Hunter-Anderson RL, Krueger HW (1997) Stable isotopic analysis of human diet in the Marianas Archipelago, Western Pacific. American Journal of Physical Anthropology 104: 343-361.

95. Tieszen LL, Fagre T (1993) Effect of diet quality and composition on the isotopic composition of respiratory CO₂, bone collagen, bioapatite, and soft tissues. In: Lambert JB, Grupe G, editors. Prehistoric Human Bone: Archaeology at the Molecular Level. Berlin: Springer-Verlag. 121-155.

96. Mündler G, Richards MP (2007) Stable isotope evidence for 1500 years of human diet at the city of York, UK. American Journal of Physical Anthropology 133: 682-697.

97. Bedford S, Spriggs M, Regenvanu R (2006) The Teouma Lapita site and the early human settlement of the Pacific Islands. Antiquity 80: 812-828.

98. Bedford S, Spriggs M, Buckley H, Valentin F, Regenvanu R, et al. (2011) A cemetery of first settlement: the site of Teouma, South Efate, Vanuatu. In: Sand C, Bedford S, editors. Lapita: Oceanic Ancestors 141-161.

99. Scott RM, Buckley HR, Spriggs M, Valentin F, Bedford S (2010) Identification of the first reported Lapita cremation in the Pacific Islands using archaeological, forensic and contemporary burning evidence. Journal of Archaeological Science 37: 901-909.

100. Valentin F, Bedford S, Buckley H, Spriggs M (2010) Inhumations, exhumations and bone treatment in a Lapita community as reflected at the Teouma burial ground, Vanuatu. Journal of Island and Coastal Archaeology In press.

101. Steadman DW (2006) Extinction and Biogeography of Tropical Pacific Birds. Chicago: The University of Chicago Press.

102. White AW, Worthy TH, Hawkins S, Bedford S, Spriggs M (2010) Megafaunal meiolanid horned turtles survived until early human settlement in Vanuatu, Southwest Pacific. Proceedings of the National Academy of Sciences 107: 15512-15516.

103. Mead JI, Steadman DW, Bedford SH, Bell CJ, Spriggs M (2002) New extinct *Mekosuchus* crocodile from Vanuatu, South Pacific. Copeia 2002: 632-641.

104. Anderson A (2002) Faunal collapse, landscape change and settlement history in Remote Oceania. World Archaeology 33: 375-390.

105. Steadman DW (1993) Biogeography of Tongan birds before and after human impact. Proceedings of the National Academy of Sciences 90: 818-822.

106. Steadman DW (1995) Prehistoric extinctions of Pacific Island birds: biodiversity meets zooarchaeology. Science 267: 1123-1131.

107. Steadman DW (1999) The prehistoric extinction of South Pacific birds: catastrophy versus attrition. In: Galipaud J, Lilley I, editors. The Pacific from 5000 to 2000 BP: Colonisation and Transformations. Paris: IRD Publications. 375-386.

108. Pregill GK, Steadman DW (2004) South Pacific iguanas: human impacts and a new species. Journal of Herpetology 38: 15-21.

109. Walter A, Lebot V (2007) Gardens of Oceania. ACIAR Monograph No. 122. Canberra: Australian Centre for International Agricultural Research.

110. Walter A (2002) Fruits of Oceania. Canberra: Australian Centre for Agricultural Research.

111. McClatchey WC (2012) Wild food plants of Remote Oceania. Acta Societatis Botanicorum Poloniae 81: 371-380.

112. Pollock NJ (1992) These Roots Remain: Food Habits in Islands of the Central and Eastern Pacific since Western Contact. Honolulu: University of Hawaii Press.

113. Walter A, Sam C (1993) A variety collection of nut trees and fruit trees in Vanuatu. Société, Urbanisation, Développement, Notes Techniques No. 15.: ORSTOM.

114. Spriggs M (1984) Early coconut remains from the South Pacific Journal of the Polynesian Society 93: 71-76.

115. Lebot V, Merlin M, Lindstrom L (1997) Kava the Pacific Elixir: the definitive guide to it's ethnobotany, history, and chemistry. Rochester: Healing Arts Press.

116. Barrau J (1965) Witnesses of the past: notes on some food plants of Oceania. Ethnology 4: 282-294.

117. Keppel G, Hodgskiss PD, Plunkett GM (2008) Cycads in the insular South-west Pacific: dispersal or vicariance? Journal of Biogeography 35: 1004-1015.

118. Buikstra JE, Ubelaker DH (1994) Standards for Data Collection from Human Skeletal Remains. Fayetteville: Arkansas Archaeological Survey.

119. Storey AA, Spriggs M, Bedford S, Hawkins SC, Robins JH, et al. (2010) Mitochondrial DNA from 3000-year old chickens at the Teouma site, Vanuatu. Journal of Archaeological Science 37: 2459-2468.

120. Tieszen LL (1991) Natural variations in the carbon isotope values of plants: implications for archaeology, ecology, and paleoecology. Journal of Archaeological Science 18: 227-248.
121. Allen MS, Craig JA (2009) Dynamics of Polynesian subsistence: insights from archaeofauna and stable isotope studies, Aitutaki, Southern Cook Islands. Pacific Science 63: 477-506.

122. Field JS, Cochrane EE, Greenlee DM (2009) Dietary change in Fijian prehistory: isotopic analyses of human and animal skeletal material, Journal of Archaeological Science 36: 1547-1556.

123. Richards MP, West E, Rolett B, Dobney K (2009) Isotope analysis of human and animal diets from the Hanamiai archaeological site (French Polynesia). Archaeology in Oceania 44: 29-37.

124. Casu D, Ceccherelli G, Sechi N, Rumolo P, Sarà G (2009) *Caulerpa racemosa* var. *cylindracea* as a potential source of organic matter for benthic consumers: evidences from a stable isotope analysis. Aquatic Ecology 43: 1023-1029.

125. Yoshinaga J, Minagawa M, Suzuki T, Ohtsuka R, Kawabe T, et al. (1991) Carbon and nitrogen isotopic characterization for Papua New Guinea foods. Ecology of Food and Nutrition 26: 17-25.

126. O'Connell TC, Hedges REM, Healey MA, Simpson A (2001) Isotopic comparison of hair, nail and bone: modern analyses. Journal of Archaeological Science 28: 1247-1255.

127. Longin R (1971) New method of collagen extraction for radiocarbon dating. Nature 230: 241-242.

128. Brown TA, Nelson DE, Vogel JS, Southon JR (1988) Improved collagen extraction by modified Longin method. Radiocarbon 30: 171-177.

129. Collins MJ, Galley P (1998) Towards an optimal method of archaeological collagen extraction: the influence of pH and grinding. Ancient Biomolecules 2: 209-222.

130. Bocherens H, Fizet M, Mariotti A, Lange-Badre B, Vandermeersch B, et al. (1991) Isotopic biogeochemistry (δ13C, δ15N) of fossil vertebrate collagen: application to the study of a past food web including Neandertal man. Journal of Human Evolution 20: 481-492.

131. van Klinken GJ (1999) Bone collagen quality indicators for palaeodietary and radiocarbon measurements. Journal of Archaeological Science 26: 687-695.

132. DeNiro MJ (1985) Postmortem preservation and alteration of *in vivo* bone collagen isotope ratios in relation to palaeodietary reconstruction. Nature 317: 806-809.

133. White CD, Schwarcz HP (1994) Temporal trends in stable isotopes for Nubian mummy tissues. American Journal of Physical Anthropology 93: 165-187.

134. Nehlich O, Richards MP (2009) Establishing collagen quality criteria for sulphur isotope analysis of archaeological bone collagen. Archaeological and Anthropological Sciences 1: 59-75.

135. Privat KL, O'Connell TC, Hedges REM (2007) The distinction between freshwater-and terrestrial-based diets: methodological concerns and archaeological applications of sulphur stable isotope analysis. Journal of Archaeological Science 34: 1197-1204.

136. Fry B, Scalan RS, Parker PL (1983) $^{13}$C/$^{12}$C ratios in marine food webs of the Torres Strait, Queensland. Australian Journal of Marine and Freshwater Research 34: 707-715.

137. Abel KM (1984) Inorganic carbon source for photosynthesis in the seagrass *Thalassia hemprichii* (Ehrenb.) Aschers. Plant Physiology: 776-781.

138. Beer S, Waisel Y (1979) Some photosynthetic carbon fixation properties of sea-grasses. Aquatic Botany 7: 129-138.

139. Arthur K, Boyle M, Limpus C (2008) Ontogenetic changes in diet and habitat use in green sea turtle (*Chelonia mydas*) life history. Marine Ecology Progress Series 362: 303-311.

140. Biasatti DM (2004) Stable carbon isotopic profiles of sea turtle humeri: implications for ecology and physiology. Palaeogeography, Palaeoclimatology, Palaeoecology 206: 203-216.

141. Craig OE, Ross R, Andersen SH, Milner N, Bailey GN (2006) Focus: sulphur isotope variation in archaeological marine fauna from northern Europe. Journal of Archaeological Science 33: 1642-1646.

142. Krouse HR (1989) Sulphur isotope studies of the pedosphere and biosphere In: Rundel PW, Ehleringer JR, Nagy KA, editors. Stable Isotopes in Ecological Research. New York: Springer-Verlag. 424-444.

143. Fry B, Scalan RS, Winters JK, Parker PL (1982) Sulphur uptake by salt grasses, mangroves, and seagrasses in anaerobic sediments. Geochimica et Cosmochimica Acta 46: 1121-1124.

144. Meyer E, Nilkerd B, Glover EA, Taylor JD (2008) Ecological importance of chemoautotrophic Lucinid bivalves in a peri-mangrove community in eastern Thailand. Raffles Bulletin of Zoology, Supplement 18: 41-55.

145. Taylor JD, Glover EA (2010) Chemosymbiotic bivalves. In: Kiel S, editor The Vent and Sea Biota: Aspects from Microbes to Ecosystems. Heidelberg: Springer. 107-135.

146. Banack SA (1998) Diet selection and resource use by flying foxes (genus *Pteropus*). Ecology 79: 1949-1967.

147. Muzuka ANN, Shunula JP (2006) Stable isotope compositions of organic carbon and nitrogen of two mangrove stands along the Tanzanian coastal zone. Estuarine, Coastal and Shelf Science 66: 447-458.

148. Scanlon AT, Petit S, Sternberg L (2013) Insectivory in Fijian flying foxes (*Pteropodidae*). Aust J Zool 61: 342-349.

149. Medway L, Marshall AG (1975) Terrestrial vertebrates of the New Hebrides: origin and distribution. Philosophical Transactions of the Royal Society of London B, Biological Sciences 272: 423-465.

150. Flannery T (1995) Mammals of the Southwest Pacific and Moluccan Islands. Ithaca: Cornell University Press.

151. Nelson SL, Miller MA, Heske EJ, Fahey GC (2000) Nutritional consequences of a change in diet from native to agricultural fruits for the Samoan fruit bat. Ecography 23: 393-401.

152. Jenkins S, Partridge S, Stephenson T, Farley S, Robbins C (2001) Nitrogen and carbon isotope fractionation between mothers, neonates, and nursing offspring. Oecologia 129: 336-341.

153. van der Merwe NJ, Medina E (1989) Photosynthesis and 13C/12C ratios in Amazonian rain forests. Geochimica et Cosmochimica Acta 53: 1091-1094.

154. van der Merwe NJ, Medina E (1991) The canopy effect, carbon isotope ratios and foodwebs in Amazonia. Journal of Archaeological Science 18: 249-259.

155. Gross GF (1975) The land invertebrates of the New Hebrides and their relationships. Philosophical Transactions of the Royal Society of London B, Biological Sciences 272: 391-421.

156. Guiry EJ (2012) Dogs as analogs in stable isotope-based human paleodietary reconstructions: a review and considerations for future use. Journal of Archaeological Method and Theory 19: 351-376.

157. Clark G, Petchey F, Hawkins S, Reepmeyer C, Smith I, et al. (2013) Distribution and extirpation of pigs in Pacific Islands: a case study from Palau. Archaeology in Oceania 48: 141-153.

158. Green RC (1979) Lapita. In: Jennings JD, editor The Prehistory of Polynesia. Cambridge: Harvard University Press. 27-60.

159. Green RC (1974) Sites with Lapita pottery: importing and voyaging. Mankind 9: 253-259.

160. Davidson J (2012) Intrusion, integration and innovation on small and not-so-small islands with particular reference to Samoa. Archaeology in Oceania 47: 1-13.

161. Hide R (2003) Pig husbandry in New Guinea: a literature review and bibliography. ACIAR Monograph No.108. Canberra: Australian Centre for international Agricultural Research.

162. Bedford S (2006) Pieces of the Vanuatu Puzzle: Archaeology of the North, South and Centre. Canberra: Pandanus Books.

163. Kirch PV, Dye T (1979) Ethno-archaeology and the development of Polynesian fishing strategies. The Journal of the Polynesian Society 88: 53-76.

164. Davidson J, Leach BF, Sand C (2002) Three thousand years of fishing in New Caledonia and the Loyalty Islands. In: Bedford S, Sand C, Burley D, editors. Fifty years in the field: essays in honour and celebration of R Shutler Jr's archaeological career. Auckland: New Zealand Archaeological Association Monograph. 153-164.

165. Galipaud JC (2000) The Lapita site of Atanoasao, Malo, Vanuatu. World Archaeological Bulletin 12: 41-55.

166. Marshall AG, Medway L (1976) A mangrove community in the New Hebrides, south-west Pacific. Biological Journal of the Linnean Society 8: 319-336.

167. Nimoho LT (2000) Freshwater Fish and Crustaceans of Vanuatu. Port Vila: Vanuatu Environmental Unit.

168. Voznesenskaya EV, Koteyeva NK, Edwards GE, Ocampo G (2010) Revealing diversity in structural and biochemical forms of C4 photosynthesis and a C3-C4 intermediate in genus Portulaca L. (Portulacaceae). Journal of Experimental Botany 61: 3647-3662.

169. Katzenberg MA, Pfeiffer S (1995) Nitrogen isotope evidence for weaning age in a Nineteenth Century Canadian skeletal sample. In: Grauer AL, editor Bodies of Evidence. New York: Wiley-Liss. 221-235.

170. Froehle AW, Kellner CM, Schoeninger MJ (2012) Multivariate carbon and nitrogen stable isotope model for the reconstruction of prehistoric human diet. American Journal of Physical Anthropology 147: 352-369.

171. Kinaston RL, Buckley HR, Halcrow SE, Spriggs MJT, Bedford S, et al. (2009) Investigating foetal and perinatal mortality in prehistoric skeletal samples: a case study from a 3000-year-old Pacific Island cemetery site. Journal of Archaeological Science 36: 2780-2787.

172. Oomen H, Malcolm SH (1958) Nutrition and the Papuan Child: A Study in Human Welfare. Noumea, New Caledonia: South Pacific Commission, Technical Paper No. 118.

173. Oliver DL (2002) Polynesia in Early Historic Times. Honolulu, Hawaii: Bess Press.

174. Parslow BH (1993) Pre-Contact Polynesian Fishing: a gender perspective. Unpublished Masters Thesis: Department of Anthropology. University of Otago, Dunedin.

175. Sheppard P (2011) Into the great ocean: Lapita movement in Remote Oceania. In: Sand C, Bedford S, editors. Lapita: Oceanic Ancestors 105-117.

176. Green RC (1997) Linguistic, biological and cultural origins of the initial inhabitants of Remote Oceania. New Zealand Journal of Archaeology 17: 5-27.