The terminal Pleistocene/Holocene boundary (approximately 12–8 thousand years ago) represented a major ecological threshold for humans, both as a significant climate transition and due to the emergence of agriculture around this time. In the highlands of New Guinea, climatic and environmental changes across this period have been highlighted as potential drivers of one of the earliest domestication processes in the world. We present a terminal Pleistocene/Holocene palaeoenvironmental record (12–0 thousand years ago ) of carbon and oxygen isotopes in small mammal tooth enamel from the site of Kiowa. The results show that tropical highland forest and open mosaics, and the human subsistence focused on these environments, remained stable throughout the period in which agriculture emerged at nearby Kuk Swamp. This suggests the persistence of tropical forest foraging among highland New Guinea groups and highlights that agriculture in the region was not adopted as a unilinear or dramatic, forced event but was locally and historically contingent.
The transition from the terminal Pleistocene to the Holocene witnessed increasingly intensive human manipulation of plant and animal resources that resulted in genetic and phenotypic changes in various species as part of what has been termed the ‘origins of agriculture’ 1 . This process has been cited as one of the most significant ecological moments in human evolutionary history 2,3 , representing a shift in human interactions with the natural world that was to have global environmental ramifications 4,5 . The emergence of this new form of subsistence has elsewhere been linked to dramatic climatic and environmental processes witnessed across the terminal Pleistocene/Holocene transition and into the Holocene 6,7 , yet the horticulture-style cultivation seen in the tropics is often ignored in such discussions. This is despite the fact that active human manipulation of plants and animals, including deliberate anthropogenic burning of forests to encourage plant growth 8,9 and the deliberate translocation of small mammals 10 , occurred in tropical forest environments as early as 45 thousand years ago (ka) and 20 ka, respectively.
It is now evident that one of the clearest and earliest examples of the mutualistic relationship between humans and their plant-foods comes from Kuk Swamp in the tropical highlands of New Guinea 1,11,12 . Here, in a montane tropical rainforest and grassland ecotone, terminal Pleistocene human foragers moved and tended the tropical plants of yam (Dioscorea sp.), banana (Musa sp.) and taro (Colocasia sp.) taxa until these species were fully ‘domesticated’ during the Early–Middle Holocene 1,11,13 . Although decades of research has described the archaeological sequence of Kuk Swamp, little is known of foraging behaviour elsewhere in the New Guinea Highlands and the drivers behind the intensification of tropical plant manipulation at this time. As in other regions, it has been suggested that this process was stimulated by climatic fluctuation across the Pleistocene/Holocene boundary 1,14 . However, there are currently no detailed, well-dated, ‘on-site’ palaeoenvironmental records, directly associated with forager behaviour, in this region to support or refute such hypotheses.
We applied stable carbon and oxygen isotope analysis to small mammal tooth enamel from the archaeological site of Kiowa (Supplementary Text 1 and Supplementary Tables 1 and 2), which is located at a similar ecological and altitudinal position to Kuk Swamp in the Central Highlands of New Guinea (Figs 1 and 2), to produce a well-dated, palaeoenvironmental sequence associated with terminal Pleistocene/Holocene forager behaviour (12–0 ka) (Supplementary Table 1)
Isotope analysis of archaeological small mammalian fauna such as those identified at Kiowa is an increasingly popular method of local palaeoenvironmental reconstruction due to their high frequency (and therefore large sample sizes), small home ranges and high habitat discrimination
. Stable carbon isotopes of mammalian faunal enamel primarily reflect the proportions of C3 and C4 biomass in the diet in the tropics and subtropics; low faunal δ13C indicates reliance on 13C-depleted C3 resources relative to 13C-enriched C4 resources available in open areas
The δ13C values covered a wide range (−14.5‰ to −8.7‰). Based on a comparison with stable isotope analysis of modern faunal tooth enamel (corrected for the fossil fuel effect 31 ), the data showed an environmental range from closed forest environments (≤−14.0‰) to open-woodland mosaic C3 habitats (approximately −12.0‰ to −9.0‰) 21,22,32,33 . This range fits with the modern ecological preferences of the faunal groups sampled (Supplementary Text 2). The δ13C range remained broadly consistent across the terminal Pleistocene and Holocene levels at the site with some elements of dense forest habitat and more open C3 environments present throughout the period of human occupation. Analysis of variance (ANOVA) testing indicated that there was no difference in overall faunal δ13C values between the levels (F(6,130) = 1.61, P > 0.05) (Supplementary Table 4).
The δ18O data from the Kiowa fauna showed a similarly large range (−12.6‰ to −6.4‰). Low δ18O is expected in the tropics as a result of the high intensity of rainfall 28 . All of the fauna analysed were obligate drinkers and therefore this range is probably indicative of variability in precipitation values, in open drinking water sources in the vicinity of the site, and in food. The faunal groups sampled had varying reliance on open water sources, while; cuscus, ringtail possums and bats are known to drink nocturnally, which probably contributed to the size of this range (Supplementary Text 2). As with δ13C, the δ18O values and range also remained consistent across the terminal Pleistocene and Holocene periods of site activity, suggesting little change in the influences that governed hydrological isotope values in the tropics during human occupation at the site 19,34,35 . An ANOVA test demonstrated that there was no significant difference between overall fauna δ18O values from the different levels (F(6,130) = 1.008, P > 0.05) (Supplementary Table 5).
There were, however, consistent δ13C distinctions evident between the faunal groups sampled (F(3,130) = 30.79, P < 0.05; ANOVA) (Supplementary Table 4). When post hoc Tukey pairwise testing was applied, statistically significant differences were found between macropods and bats, ringtail possums and bats, macropods and cuscus, and ringtail possums and cuscus (Supplementary Table 6). Bat and cuscus δ13C values were at the higher end of the δ13C range, relative to the ringtail possums, while macropods spanned the whole range (Supplementary Fig. 3). As bats are known to travel large distances to obtain food 36,37 , the contribution of resources from open C3 environments is unsurprising. The distinction between the cuscus and both the ringtail possums and macropods may suggest that cuscus could survive in more open forest mosaics than these other taxa (Supplementary Text 2). ANOVA testing also demonstrated differences in δ18O values between the groups of taxa sampled (F(3,130) = 6.015, P < 0.05; Supplementary Table 5). When post hoc Tukey pairwise testing was applied, statistically significant differences were observed between macropods and bats, and ringtail possums and macropods (Supplementary Table 7). These differences may be linked to the nocturnal habits of bats and ringtail possums, compared with the diurnal feeding and drinking habits of macropods (Supplementary Text 2).
There was no variation in δ13C and δ18O values between stratigraphic levels when ANOVA tests were performed on individual faunal groups (Fig. 4). Ringtail possums showed no variation in δ13C (F(6,28) = 0.860, P > 0.05; Supplementary Table 8) or δ18O (F(6,28) = 1.582, P > 0.05; Supplementary Table 9) by level. The same was true for cuscus (δ13C: F(6,28) = 0.738, P > 0.05, Supplementary Table 10; δ18O: F(6,28) = 2.127, P > 0.05, Supplementary Table 11) and bats (δ13C: F(6,29) = 1.568, P > 0.05, Supplementary Table 12; δ18O: F(6,29) = 1.273, P > 0.05, Supplementary Table 13). No variation in δ13C by level was found for macropods (F(6,27) = 0.710, P > 0.05; Supplementary Table 14). However, there was a significant difference in macropod δ18O by level (F(6,27) = 2.636, P < 0.05; Supplementary Table 15). This may be a result of macropods feeding and drinking diurnally, and therefore more strongly reflecting palaeoenvironmental evapotranspiration-linked changes in δ18O, compared with the other taxa sampled. That said, when post hoc Tukey pairwise testing was applied, no specific inter-level δ18O differences were found for the taxon group (Supplementary Table 16).
Overall, the results indicate stability in faunal diets and drinking water sources, and their associated environments, from the terminal Pleistocene into the Holocene in the vicinity of Kiowa. The data presented here are consistent with other palaeoenvironmental evidence from South Asia
, Southeast Asia
and the New Guinea Highlands themselves
that suggest the persistence of tropical forests, albeit of varying structure, in this part of the world between 12 and 0 ka. Significant, rapid climate fluctuations, particularly in the form of submontane tropical forest encroachment under the warmer conditions of the Holocene, have been argued for in the highlands of New Guinea across the terminal Pleistocene boundary
The lack of marked climate and environmental shifts in our data suggest that plant manipulation and domestication at Kuk Swamp is best seen as active anthropogenic modification of the landscape, rather than an environmental response. It could be argued that other reasons, including demographic change or an increase in social network densities 46,47 , should be used to explain one of the earliest global experiments with ‘agriculture’. However, given the paucity of evidence elsewhere in the region for ‘domestication’ processes at this time 15,48 , it is perhaps best to see Kuk Swamp as part of a diversity of stable, successful tropical forest foraging adaptations in the region that extend back to 45 ka 8,48 , through the Last Glacial Maximum 49,50 and into the Holocene 1,13 . Evidence for an increasingly intensive relationship between human foragers and tropical forests across the terminal Pleistocene/Holocene transition in Sahul includes an increase in burning to stimulate plant growth 51 and the deliberate translocation of animal protein between tropical forest islands 10 . Instead of a dramatic forced event, plant management at Kuk Swamp is part of the long-term relationships between hunter–gatherer communities and tropical forest habitats that have characterized this part of the world from the Late Pleistocene.
Tropical forests are currently undergoing a rehabilitation in the archaeological and anthropological literature as productive environments for human foraging
We sampled molar teeth from small mammal taxa that made up a consistently high portion of the mammalian assemblage throughout the archaeological sequence of Kiowa (Supplementary Text 1)
The taxa sampled represented a diversity of environments, ecological niches and altitudinal zones (Supplementary Text 2), enabling a more detailed picture of local environmental change relevant to human hunters to be produced throughout the sequence. Cuscus (P. carmelitae) is a nocturnal inhabitant of primary tropical forest approximately 1,350–3,800 m above sea level (a.s.l.) and the possums (P. cupreus, P. corinnae and P. forbesi) are nocturnal and come mainly from undisturbed primary forest approximately 2,000 m a.s.l. and higher. The bat species sampled (D. magna) is abundant in tropical forest up to 2,700 m a.s.l. but is also known to range to savannah woodland at lower altitudes (Supplementary Text 2). Finally, the larger macropod individuals come from a diversity of forest habitats at different altitudes and include a mixture of nocturnal and diurnal feeders (Supplementary Text 2).
Despite primarily being nocturnal, these taxa are extensively documented in ethnographic and archaeological hunting assemblages
To avoid the nursing or weaning effect67, second and third molars were preferred as representing the ‘adult’ period of enamel formation and diet for bats, cuscus, ringtail possums, and macropods. Exterior surfaces of the teeth were cleaned using air-abrasion to remove any adhering external material. The roots of the molar teeth were removed and each tooth was sectioned to remove dirt from inside the tooth. Due to their small sizes, each tooth was crushed using an agate mortar and pestle 19,35 . An attempt was made to remove dentine from enamel where possible. However, as per ref. 19 , given the relatively short formation times for these teeth, we assumed that dentine apatite and enamel apatite represented the same period and conditions.
All enamel powder was pretreated using a consistent technique to remove any organic or secondary carbonate contaminants 68,69 . This consisted of a series of washes in 1.5% sodium hypochlorite for 60 min, followed by three rinses in purified H2O and centrifugation, before 0.1 M acetic acid was added for 10 min, followed by another three rinses in purified H2O. Following reaction of the samples with 100% phosphoric acid, the gases evolved were analysed to identify the stable carbon and oxygen isotopic composition using a Gas Bench II (ThermoFisher) connected to a Delta V Advantage Mass Spectrometer (ThermoFisher). Carbon and oxygen isotope values were compared against an international standard registered by the International Atomic Energy Agency (NBS 19) and an in-house standard (MERCK). Replicate analysis of ostrich eggshell (OES) standards indicated that the machine measurement error was approximately ± 0.1‰ for δ13C and ± 0.2‰ for δ18O.
All δ13C and δ18O datasets were tested for normality using the Shapiro–Wilks test and histogram observations before statistical analysis. ANOVA tests were performed on faunal enamel δ13C and δ18O values from Kiowa to determine the influence of species and stratigraphic level on isotopic variation overall and for each faunal group (namely ringtail possums, cuscus, bats and macropods). Where variance was found to be significant, this was combined with a post hoc Tukey pairwise comparison to determine which taxa or stratigraphic levels were significantly different from each other, in terms of δ13C and δ18O values. Where data were non-normal a Kruskal–Wallis test was applied in addition to the parametric analyses described. In all cases, the results of the parametric and non-parametric analyses supported each other. We consequently only report the results of the ANOVA and, where relevant, post hoc Tukey pairwise comparison tests for consistency across the datasets. All statistical analyses were conducted using the software ‘R’ 70.
The authors declare that the data supporting the findings of this study are available within the paper and its supplementary information files.
How to cite this article: Roberts, P., Gaffney, D., Lee-Thorp, J. & Summerhayes, G. Persistent foraging in the highlands of terminal Pleistocene/Holocene New Guinea. Nat. Ecol. Evol. 1, 0044 (2017).
This project was funded by grants from the Natural Environmental Research Council and the Boise Fund, University of Oxford (to P.R.). We also thank the National Museum and Art Gallery of Papua New Guinea for supporting this research. J. Menzies provided helpful insight into the zoology. Finally, a special thanks goes to Sue Bulmer and her family for providing us with access to the materials and field notes for the site of Kiowa. We dedicate this paper to Sue, who sadly passed away during the writing of this paper—her legacy in Pacific archaeology and at the site of Kiowa remains.
Supplementary Text; Supplementary Figures 1–3; Supplementary Tables 1–16; Supplementary References