Specialized rainforest hunting by Homo sapiens ~45,000 years ago

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Oshan WedageNoel AmanoMichelle C. LangleyKaterina DoukaJames BlinkhornAlison CrowtherSiran DeraniyagalaNikos KourampasIan SimpsonNimal PereraAndrea PicinNicole BoivinMichael Petraglia & Patrick Roberts


Defining the distinctive capacities of Homo sapiens relative to other hominins is a major focus for human evolutionary studies. It has been argued that the procurement of small, difficult-to-catch, agile prey is a hallmark of complex behavior unique to our species; however, most research in this regard has been limited to the last 20,000 years in Europe and the Levant. Here, we present detailed faunal assemblage and taphonomic data from Fa-Hien Lena Cave in Sri Lanka that demonstrates specialized, sophisticated hunting of semi-arboreal and arboreal monkey and squirrel populations from ca. 45,000 years ago, in a tropical rainforest environment. Facilitated by complex osseous and microlithic technologies, we argue these data highlight that the early capture of small, elusive mammals was part of the plastic behavior of Homo sapiens that allowed it to rapidly colonize a series of extreme environments that were apparently untouched by its hominin relatives.


There is growing evidence that Homo sapiens had a unique capacity to adapt to a diversity of extreme environments, both within and beyond Africa, when compared with other members of the genus Homo1. Nevertheless, studies of migrations of our species into Europe, the Middle East, and Asia have often focused on its increased efficiency in hunting, butchering, and consuming medium-to-large game in open “savanna” settings2,3. Alternatively, coastal settings have been highlighted as providing homogeneous, protein-rich resources that stimulated human evolution as well as migration beyond Africa from the Late Pleistocene4,5. Focus on these environments has meant that small mammals have been neglected in discussions of the human colonization of new environments, despite the fact that a specialization in their procurement is often considered a feature of technological and behavioral “complexity” or “modernity” unique to our species6,7. Concentration on Europe and West Asia in this regard has linked increased usage and capture of agile, but abundant, small mammals to human population growth or climatically driven crises associated with the end of the last glacial period6. Nevertheless, the onset and behavioral context of small mammal hunting in other parts of the world, and beyond temperate environments, has remained poorly studied.

From the Late Pleistocene onwards, our species inhabited a number of diverse environments as it dispersed beyond Africa. One of these environments, tropical rainforests, has been considered a barrier to human dispersal8,9. This was mainly due to the fact that mammalian megafauna (> 44 kg10), thought to have been attractive to Late Pleistocene humans, and even driven to extinction as a result of our species’ expansion11,12, are lacking in these settings8. Nevertheless, in Sri Lanka, Southeast Asia, and Melanesia, as well as other parts of the world, the earliest evidence for human occupation is often associated with rainforest environments13,14,15,16. In Sri Lanka, stable isotope evidence has demonstrated that humans relied on rainforest resources for over 30,000 years17, perhaps aided by the complex microlith and bone toolkits found at Late Pleistocene and early Holocene sites in the region15,16,18. However, owing to a lack of detailed faunal analyses, it has remained unknown which foodstuffs sustained human populations during this time, as well as the hunting strategies employed to obtain them.

We apply new chronometric, taphonomic, archaeozoological, and artifactual analyses to the earliest dated archeological site in Sri Lanka, Fa-Hien Lena (Fig. 1), previously dated to 38,000 years ago18,19,20. Fa-Hien Lena documents the earliest fossil appearance of H. sapiens in Sri Lanka, and indeed South Asia, alongside small, quartz microlith technology, and a variety of pointed bone technologies18,19,20. Rainforest mammals, reptiles, molluscs, and plant remains have been identified at the site18,20,21. However, human exploitation of specific resources has yet to be directly demonstrated owing to a lack of systematic taphonomic study. Similarly, the early, enigmatic microlith and bone technologies discovered here and elsewhere in South Asia have undergone limited analysis, and their use and adaptive function have remained obscure19,20,22. The results of our new multidisciplinary analyses document specialized, sophisticated hunting of semi-arboreal and arboreal prey taxa from ca. 45,000 years ago, in the tropical rainforest environments of Sri Lanka.

Fig. 1
Fig. 1

Location of Fa-Hien Lena. a Map of Sri Lanka showing the location of Fa-Hien Lena and the country’s vegetation zones44,45b Excavation in Fa-Hien Lena


Stratigraphy and chronology

We divide the dates available for the site into four distinct phases based on our new, and previous, excavations19,23. The phases correspond to concentrations of charcoal, faunal remains, and artifacts, including osseous tools, shell beads, and quartz flakes (Supplementary Figure 1), and represent the major periods of human occupation of the cave. Phase D contains evidence for Late Pleistocene occupation of the cave from c. 48,000 to 34,000 cal. BP and probably included several episodes of occupation, each of which may have been relatively short-lived. Phase C spans the Terminal Pleistocene occupation from c. 13,000–12,000 cal. BP, while Phases B and A span the Early (8700 to 8000 cal. BP) and Middle (6000 to 4000 cal. BP) Holocene, respectively. One radiocarbon date falls outside these phases (29,120–27,870 cal. BP) and may represent a short-lived episode of human presence in the cave.

These phases also align with major lithostratigraphic changes (Fig. 2). The fill of Fa-Hien Lena consists of c. 170 cm of detrital sediment deposited above heavily weathered and karstified gneiss blocks. Phase D consists of pebbly loams and clayey and sandy silt deposits with laminated ash representing intermittent/episodic human occupation and colluvial inwash. The deposits yielded a variety of evidence for human activity, including heavily burned/calcined faunal remains, shell beads, bone tools, and ocher fragments, in addition to micromorphological analyses of sediments evidencing in situ burning (Supplementary Note 1). A roof fall episode appears to have contributed to the exceptional preservation of these deposits by sealing large parts of Phase D from later disturbance. Phase C, which contains the heaviest concentration of artifacts and human occupation debris in the stratigraphy, comprises of a rapidly deposited, heterogeneous mixture of dark colored, organic-rich sandy silty loams. Phases B and A are made up of light colored sandy silts and ash accumulations. For further detailed description, see Supplementary Note 1, Supplementary Tables 14, and Supplementary Figures 14.

Fig. 2
Fig. 2

Stratigraphy of Fa-Hien Lena. South wall, end of the 2010 excavation. The star indicates the approximate stratigraphic location19 of the fossils described by Kennedy23

Previous excavation in Fa-Hien-lena produced the oldest human fossils so far in Sri Lanka. Remains of a 5.5–6.5 years old child, mixed with remains of at least two infants as well as a young adult female, were dated based on associated charcoal to 30,600 + 360 BP23. These remains were found in layer 4 at the rear of the cave during the 1986 excavations19 (approximately represented by context 179 during our 2010 excavations) (Fig. 2). Overall, our new data confirm Fa-Hien Lena as the oldest site with H. sapiens fossils in Sri Lanka, and wider South Asia19,20. They also indicate that Fa-Hien Lena now represents one of the earliest appearances of microlith toolkits and bone tool technocomplexes outside of Africa.

Zooarchaeology and taphonomy

Our detailed taphonomic and archaeozoological study of faunal remains at Fa-Hien Lena examined the adaptive context of the first humans on the island. We analyzed a total of 14,485 bone and tooth fragments from the site, 52.6% of which were identified to taxon (number of identified specimens, NISP = 7622). The full dataset can be found in Supplementary Note (see also Supplementary Figures 516; Supplementary Tables 542). Small mammals (i.e., weighing less than 25 kg) overwhelmingly dominate the faunal assemblage starting from the earliest phase of occupation (c. 48,000–34,000 cal. BP). These animals, including carnivores such as the civet cat, account for more than 90% of the NISP, suggesting deliberate hunting from the Late Pleistocene until the Mid-Holocene (Fig. 3) (Supplementary Note 2). Reptiles, including pythons, colubrid snakes, and water monitors, and fish (mostly catfish and carp) are also present in all phases of site occupation. Several of the specimens identified could represent fauna from natural accumulations (e.g., murids and amphibians accumulated by raptors, 1.9% of the total NISP, see Supplementary Note 2). Other specimens, including birds such as swifts and swallows and squamates such as snakes and varanids, could represent the cave’s natural faunal communities. However, the high percentage of burning (> 50% in Phase D) in squamate remains suggests that they were most likely utilized by the people that occupied the site (Supplementary Note 2).

Fig. 3
Fig. 3

Animal taxa identified in Fa-Hien Lena. Distribution of animal taxa identified in the different occupational phases of Fa-Hien Lena based on the number of identified specimens (NISP, a) and the minimum number of individuals (MNI, b). (Brown: non-mammals; orange: micromammals; green: small mammals; blue: large mammals)

There is no significant difference in the distribution of mammals based on body size from the Late Pleistocene to the Mid-Holocene (Supplementary Note 2). Large ungulates, including cervid, suid, and bovid are present throughout the stratigraphy but at very low frequencies (< 4%). Monkeys and tree squirrels overwhelmingly dominate the faunal assemblage in all phases of site occupation, accounting for more than 70% of the identified remains (or 82.4% of the total NISP discounting fauna most likely accumulated by non-human cave dwelling species). They represent 84.7% and 76.3% of the total number of identified specimens in the Terminal and Late Pleistocene layers, respectively (72.3% and 66.7% of the minimum number of individuals, MNI). Of the taxa identified in the Late Pleistocene layers, 48.7% are cercopithecoid monkeys. Deliberate targeting of monkeys continued until the Mid-Holocene, where cercopithecoids represent 61.1% of the number of identified bone and tooth fragments. Three cercopithecoid species are currently present in Sri Lanka: the cercopithecine Macaca sinica (toque macaque), the colobine monkeys Trachypithecus vetulus (purple-faced langur), and Semnopithecus priam(tufted gray langur). These species occur sympatrically and all were identified in the site. Macaques slightly outnumber the leaf monkeys in the faunal assemblage (Supplementary Note 2).

Mortality profiles based on dental eruption and wear suggest that prime-aged adults were deliberately targeted. This, and the fact that the identified monkey species are today mostly arboreal and rarely venture to the ground24,25, suggests that they were most likely captured by targeted hunting. Trapping usually results in mortality profiles similar to those found in natural populations26,27,28. The presence of bone points and microliths from the outset of site occupation hints at the possible use of projectile technology to hunt arboreal prey (see below, and Supplementary Note 3, Supplementary Figures 1719, and Supplementary Tables 43 and 44). Modern Southeast Asian hunter-gatherer communities still rely on the use of projectile weapons, including darts and blowpipes, to target arboreal and semi-arboreal taxa29,30,31. The archaeological bone points are consistent in size and breakage patterns with such uses. Regardless of method of capture, entire monkey carcasses were brought and processed in the site as revealed by the pattern of skeletal part abundance (Supplementary Note 2).

Bone fragments with anthropic modification, ranging from burning to butchery marks, were recovered in all phases of site occupation. Butchery marks were recorded on a total of 92 bone fragments (0.64%), the majority of which were from small mammals (92.2%) (Supplementary Note 2). The Late Pleistocene layers yielded a total of nine (0.7% of NISP) bone fragments with clear evidence for butchery, including squirrel, otter, and civet cat long bones from the oldest occupation deposit of the site (Fig. 4). The placement of the cutmarks, both in the shaft surface and the distal epiphyses, is suggestive of a carcass processing sequence that involved disarticulation and defleshing32. Burnt and calcined bone fragments represent 19.7% of the total specimens studied (23.9% of the Late Pleistocene assemblage). A high proportion of the small mammal (17.1%) remains identified at the site exhibit evidence for burning, including 16.1% of the monkey remains.

Fig. 4
Fig. 4

Specimens with anthropic modifications from the Late Pleistocene layers of Fa-Hien Lena. Bone fragments with evidence for butchery and osseous tools and artifacts from the earliest phase of occupation at Fa-Hien Lena. a Cutmarks on a grizzled giant squirrel (Ratufa) tibia. bCutmarks on an otter (Lutra) humerus. cd Cercopithecid monkey fibula points with evidence for shaping (ground) before high-pressure tip use. e Monkey distal fibula shaft fragment with grinding marks. f Worked monkey femur shaft fragment. g Worked macaque canine showing damage from use in cutting (on sides) and pressure/piercing on tip

Bone tool industry

Primates and giant squirrels appear to have been targeted not just for subsistence, but also for technological production. A total of 36 bone specimens with surface modifications consistent with systematic tool manufacture were recorded in the Late Pleistocene layers (Phase D) of the site (1.3% of the NISP). These consist of 10 fragments of finished implements, including proximally hafted unipoints, mesially hafted bipoints, and small geometric bipoints. The rest are fragments that represent either waste pieces or tool blanks. These specimens are characterized by the presence of heavy surface and/or edge polish and striations or grinding marks. In situ tool production accounts for the high level of fragmentation of cercopithecid bones in all levels of site occupation, but most notably in the Late Pleistocene layers (Supplementary Note 2).

The osseous tools from the Late Pleistocene layers of the site appear to have been manufactured exclusively from cercopithecid long bone fragments, save for one worked macaque canine recorded from the earliest phase of site occupation (context 253) (Fig. 4). Tools and artifacts made from large ungulate bone, teeth, and antler only start to appear during the Terminal Pleistocene. Most of the bone points examined exhibited evidence for damage consistent with high velocity impact (four out of the five points recorded in Phase D, e.g., Fig. 4)33, which, in addition to what appears to be deliberate targeting of prime age adults, further suggests that projectile hunting, rather than trapping, was utilized in the exploitation of small semi-arboreal and arboreal game.


The consistently high percentage of arboreal small mammal taxa in all phases of occupation in Fa-Hien Lena is unheard of even among modern ethnographic groups hunting in tropical rainforest environments20,34, with perhaps one exception35. Even with access to rifle technologies and wire cord and snare traps, modern foragers never show such a bias34. Late Pleistocene hunting of arboreal primates has also been demonstrated at the Niah Caves, Borneo from 50,000 to 35,0000 years BP. However, here, in contrast to Fa-Hien Lena, humans seemingly primarily relied on large ungulates as their main source of protein28. This, alongside associated evidence from what is, to our knowledge, one of the earliest bone tool assemblages in South and Southeast Asia (contemporaneous with the bone tools from Niah Caves dated between 50,000 and 35,000 years BP33), and also one of the earliest beyond Africa, implies highly tuned hunting abilities in tropical rainforest settings upon arrival in this part of the world. Moreover, despite targeting prime age adults, these human populations were able to exploit primate and giant squirrel taxa, often considered to be rainforest game types that are among the most vulnerable to overhunting36, from ~45,000 to 4,000 years ago. This suggests close knowledge of life cycles, territories, and sustainable hunting strategies37.

Discussions of Late Pleistocene dispersals of H. sapiens beyond Africa have tended to focus on human reliance on large, mammalian megafauna that are often linked to open grassland or mixed woodland and grassland environments8,11. Alternatively, scholars have focused on reliable coastal resources as providing adaptive corridors for a rapid dispersal around the Indian Ocean, through Southeast Asia, and into Australia4,5, and also into the Americas38. Our current data, demonstrate instead that some of the earliest known H. sapiens in Sri Lanka, and indeed in the South Asian tropics, focused on the specialized hunting of small semi-arboreal and arboreal mammals in tropical rainforests. Traditionally, the use of such difficult-to-catch resources has been associated with a “broad spectrum” revolution in the face of growing populations and climate change. However, continued emphasis on prime age animals across over 40,000 years, rather than a broadening of capture strategy, implies no such stress in the tropical rainforests of Sri Lanka. Furthermore, while stable isotopic data from human and faunal tooth enamel in the Wet Zone of Sri Lanka highlights subtle environmental changes from the Late Pleistocene to the Holocene, the persistence of Wet Zone and Intermediate Zone rainforest, as well as human reliance on this forest17,39, suggests these environments did not reach carrying capacity.

As a consequence, the utilization of these energetically expensive resources developed in the absence of resource pressure, documents the behavioral and technological flexibility of H. sapiens. These complex subsistence strategies appear to be part of the adaptive ecological plasticity of our species that enabled it to inhabit diverse Late Pleistocene habitats across the world1. The primary niche of non-H. sapiens hominins within and beyond Africa appears to be diverse forest and grassland mosaics in the vicinity of rivers and lakes40,41. By contrast, following its evolution in Africa c. 300 ka42, our species came to occupy higher-elevation niches than its hominin predecessors, as well as deserts, palaeoarctic settings, and tropical rainforest habitats stretching across Asia, Melanesia, and North, Central, and South America1. Moreover, it was even able to alter and manage environments, such as tropical forests, to meet its own subsistence and cultural needs through ever-intensifying niche-construction39,43. Detailed paleoecological and archeological analysis, such as that presented here, offers to yield more insights into the variety of cultural and subsistence strategies that facilitated the eventual colonization of all of the world’s continents, and resilience to increasingly extreme Pleistocene climatic fluctuations, that left H. sapiens the last hominin standing on the face of the planet.


Chronology and thin section micromorphology

Fa-Hien Lena (80° 12’ 55” E, 6° 38’ 55” N) is located in Sri Lanka’s Wet Zone region, near the town of Bulathsinhala, some 75 km southeast of Colombo in a lowland evergreen and semi-evergreen rainforest environment44,45. The cave, on the slope of a gneiss cliff, has a c. 30 m by 20 m east-facing entrance, an interior that extends c. 10 m into the cliff, and two main chambers (termed shelters A and B). First recorded by S.U. Deraniyagala in 1968, Fa-Hien Lena was systematically excavated over several seasons from 1986 to 1988 by W.H. Wijeyapala, and from 2009 to 2012 by a team led by O. Wedage, S.U. Deraniyagala, and N. Perera. Shelter A, the larger of the cave’s chambers, was excavated to a depth of over 6 m. However, the shelter’s archaeological deposits are disturbed by recent Buddhist constructions. Shelter B, on the other hand, produced a sequence of archaeological deposits spanning from what appears to be the earliest occupation of Sri Lanka by our species (previously dated to 38,000 cal. BP19,20) through to the Middle Holocene.

This paper presents the results of the analyses of materials from 2009 to 2012 excavations. We added to existing radiocarbon dates and present a revised stratigraphy for the site. Together with dates previously published19,23,46,47, which we calibrated using OxCal 4.348, we present a total of 30 radiocarbon dates (Supplementary Tables 14) that are now available for Fa-Hien Lena, enabling detailed phasing for the site.

A set of undisturbed sediment samples were collected from the excavated profile in clear polyurethane boxes. Sample boxes were labeled, photographed, and plotted on the profile drawing before removal from the profile. Four of these samples, all from Phase D sediments, were selected for micromorphological analysis (Supplementary Figure 2), aiming to understand the depositional history and to access the taphonomic integrity of these earliest occupation deposits. Sample processing, at the Thin Section Micromorphology Laboratory, University of Stirling included air-drying and impregnation with polyester (polylite) resin (http://www.thin.stir.ac.uk/). c. 30-μm thick, covered, large format thin sections (7.5 × 11 cm) were manufactured from the hardened impregnated blocks (sample code FH). Thin sections were observed with a polarizing microscope at magnifications of ×12.5 to ×400, using plain polarized (PPL), cross-polarised (XPL), and oblique incident light (OIL). The relative abundance of sediment components was estimated using standard semi-quantitative estimation charts49,50.

Zooarchaeology and taphonomy

We analyzed faunal remains recovered from the 2009 and 2012 excavations of Fa-Hien Lena. All bone fragments from sedimentary contexts with secure radiocarbon dates (including those from deposits sandwiched by dated layers) were included in the analysis. All specimens, including diaphyses and rib shafts, were sorted, counted, and measured (length, width, and thickness) using a digital caliper (Mitutoyo 500–463). Identified specimens were recorded in detail using codes for anatomic zones51 (e.g., Supplementary Figure 5) that allow the description of bone preservation/fragmentation patterns. Diagnostic dental and skeletal elements were identified to the highest possible taxonomic level using vertebrate comparative collections from the Laboratory of Comparative Anatomy of the Muséum national d’Histoire naturelle (MNHN) in Paris and photographs from the mammalian collections of the Field Museum of Natural History and American Museum of Natural History. Following von den Driesch52, individual dental specimens and specific anatomical features of diagnostic skeletal elements were measured to differentiate between closely related taxa. The naming of identified taxa follows the nomenclature for mammalian species of Wilson and Reeder53. The taxa identified in the sites were assigned to size class based on live weight (modified from refs. 54,55): (a) micromammals: 100 g to1 kg, (b) small mammals: 1 kg to 25 kg, (c) large mammals class 1: 25 kg to 200 kg, (d) large mammals class 2: 200 kg to 1000 kg, and (e) large mammals class 3: > 1000 kg.

All fragments were examined for natural, animal, and anthropic modifications, including weathering56,57, abrasion58, burning, staining, and butchery marks32. Bone surface modifications were recorded/observed using an Olympus BX53 light microscope and a Keyence VHX-6000 digital microscope. Burnt bone fragments were identified based on color59,60,61. They were distinguished into different classes based on the degree of burning56: (1) partially burnt, (2) charred (blackened), and (3) calcined (partial and complete calcination). Burnt bones were quantified by determining the percentage of the total bone fragments that is comprised of burnt specimens62,63.

The minimum number of element (MNE) and minimum number of individual (MNI) counts were calculated following a modification of Dobney and Rielly’s51 zonation system. This system is based on the recording of morphologically distinct zones in a skeletal element. The MNE was taken as the total number of non-repeatable zones (i.e., greater than 50% of the diagnostic zone present) for every skeletal element of a taxon. The highest MNE value, considering side and age (epiphyseal fusion and dental wear64), was used to estimate the MNI. The MNE counts were converted to minimum animal unit (MAU) values by taking into account the number of times the element occurs in the skeleton. The normed MAU values (% MAU) were used to compare skeletal part representation in the different phases of cave occupation65.

The length and circumference of long bone fragments were also recorded in relation to complete specimens to measure the extent of bone fragmentation in the assemblage. Long bone fragments were assigned the following fragment circumference and length scores66,67: (1) fragments with less than half of the circumference/length of the complete specimen, (2) fragments with more than half of the circumference/length of the complete specimen, and (3) fragments with the complete circumference/length of the complete specimen.

Artifact analysis

The technological study of the lithic assemblages of Fa-Hien Lena was carried out following the chaîne opératoire concept68,69, a methodological framework that defines the reconstruction of the various processes of flake production from the procurement of raw materials, through the phases of manufacture and utilization until the final discard. The chaîne opératoire concept provides systematic sequences of the flaking activities in which is possible to determine the temporal phase and the position of the artifact produced70. The lithic material is composed of 5070 items (Supplementary Tables 4344). The predominant raw material is quartz, which is abundantly available in the streams nearby.

Few chert blanks were also found and include: a siret flake fragment in context 131 (Phase A); two flakes and a fragment in context 136 (Phase B); a flake fragment in context 141; and one flake and one blade from context 248 (Phase C).

For the analysis of osseous artifacts, the materials were examined using a Zeiss Stemi 508 stereomicroscope fitted with an AxioCam 105 camera. Taphonomic and anthropogenic alterations were identified based on published works58,71,72,73,74,75,76,77,78 and mapped onto photographs taken with a Canon digital SLR camera.

Reporting summary

Further information on research design is available in the Nature Research Reporting Summary linked to this article.

Data availability

The authors declare that all data supporting the findings of this study are available upon request from the authors. The artifacts and faunal remains from the Fa-Hien Lena excavations are curated at the Department of Archeology, Government of Sri Lanka, under the site code BYP and the suffixes 10, 11, and 12 (denoting the year of excavation). Some materials remained housed at the Max Planck Institute for the Science of Human History to be returned to the Department of Archeology, Government of Sri Lanka by the end of 2019. All of the data reported in the paper are presented in the main text or in the Supplementary Notes, Tables, and Figures.

Additional information

Journal peer review informationNature Communications thanks Melinda A. Zeder and the other anonymous reviewer for their contribution to the peer review of this work. Peer reviewer reports are available.

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  1. Roberts, P. & Stewart, B. A. Defining the ‘generalist specialist’ niche for Pleistocene Homo sapiensNatHum. Behav. 2, 542–550 (2018).
  2. Finlayson, C. Neanderthals and Modern Humans: An Ecological and Evolutionary Perspective. (Cambridge Univ. Press, Cambridge, 2004).
  3. Domínguez-Rodrigo, M. Is the “Savanna Hypothesis” a dead concept for explaining the emergence of the earliest hominins? Curr. Anthropol. 55, 59–81 (2014).
  4. Mellars, P. Going east: new genetic and archaeological perspectives on the modern human colonization of Eurasia. Science 313, 796–800 (2006).
  5. Marean, C. The transition to foraging for dense and predictable resources and its impact on the evolution of modern humans. Philos. Trans. Roy. Soc. B 371, 1698 (2016).
  6. Stiner, M. C. Thirty years on the “Broad Spectrum Revolution” and paleolithic demography. PNAS 98, 6993–6998 (2001).
  7. Shea, J. J. Homo sapiens is as Homo sapiens was: behavioral variability versus “behavioral modernity” in Paleolithic archaeology. Curr. Anthropol. 52, 1–35 (2011).
  8. Bird, M. I., Taylor, D. & Hunt, C. Palaeoenvironments of insular Southeast Asia during the Last Glacial Period: a savanna corridor in Sundaland? Quat. Sci. Rev. 24, 2228–2242 (2005).
  9. Boivin, N., Fuller, D. Q., Dennell, R., Allaby, R. & Petraglia, M. D. Human Dispersal across Diverse Environments of Asia during the Upper Pleistocene. Quat. Int 300, 32–47 (2013).
  10. Martin, P. S. & Klein, R. G. Quaternary Extinctions: A Prehistoric Revolution (University of Arizona Press, Tucson, 1984).
  11. Rule, S. et al. The aftermath of megafaunal extinction: ecosystem transformation in Pleistocene Australia. Science 355, 1483–1486 (2012).
  12. Sandom, C., Faurby, S., Sandel, B. & Svenning, J.-C. Global late quaternary megafauna extinctions linked to humans, not climate change. Philos. Trans. Roy. Soc. B 28, 20133254 (2014).
  13. Barker, G. & Farr, L. (eds) Archaeological Investigations in the Niah Caves, Sarawak (McDonald Institute for Archaeological Research, Cambridge, 2016).
  14. Summerhayes, G. R. et al. Human adaptation and plant use in highland New Guinea 49,000 to 44,000 Years Ago. Science 330, 78–81 (2010).
  15. Perera, N. et al. People of the ancient rainforest: Late Pleistocene foragers at the Batadomba-lena rockshelter. J. Hum. Evol. 61, 254–269 (2011).
  16. Roberts, P. & Petraglia, M. D. Pleistocene rainforests: barriers or attractive environments for early human foragers? World Archaeol. 47, 718–739 (2015).
  17. Roberts, P. et al. Direct evidence for human reliance on rainforest resources in late Pleistocene Sri Lanka. Science 347, 1246–1249 (2015).
  18. Deraniyagala, S. U. The Prehistory of Sri Lanka: An Ecological Perspective 2nd edn, (Department of Archaeological Survey, Colombo, 1992).
  19. Wijeyapala, W. H. New Light on the Prehistory of Sri Lanka in the Context of Recent Investigations at Cave Sites (University of Peradeniya, Sri Lanka,1997).
  20. Roberts, P., Boivin, N. & Petraglia, M. D. The Sri Lankan ‘Microlithic’ tradition c. 38,000 to 3000 years ago: Tropical technologies and adaptations of Homo sapiens at the southern edge of Asia. J. World Prehist. 28, 69–112 (2015).
  21. Perera, N. Prehistoric Sri Lanka: Late Pleistocene Rockshelters and an Open Air Site. (British Archaeological Reports International Series, Archaeopress, Oxford, 2010).
  22. Perera, N., Roberts, P. & Petraglia, M. Bone Technology from Late Pleistocene Caves and Rockshelters of Sri Lanka. In Osseous Projectile Weaponry. Towards an Understanding of Pleistocene Cultural Variability (ed. Langley, M. C.) 173–188 (Springer-Verlag, New York, 2016).
  23. Kennedy, K. A. R. God-apes and Fossil Men. (University of Michigan Press, Ann Arbor, MI, 2000).
  24. Dittus. W. P. J. Population dynamics of the toque monkey, Macaca sinica. In Socioecology and Psychology of Primates (ed. R. H. Tuttle) 125–151 (World Anthropology Series, The Hague, 1975).
  25. Dittus, W. P. J. The socioecological basis for the conservation of the Toque monkey (Macaca sinica). In Primate Conservation (eds. Rainier III & Bourne, G. H.) 237–265 (Academic Press, New York, 1977).
  26. Stiner, M. C. The use of mortality patterns in archaeological studies of hominid predatory adaptations. J. Anthropol. Archaeol.9, 305–351 (1990).
  27. Cranbrook, E. & Labang, D. Bearded pigs (Sus barbatus): tooth-wear and aging wild populations in Sarawak. Sarawak MuseumJournal 58, 163–182 (2003).
  28. Piper, P. J. & Rabett, R. J. Vertebrate fauna from the Niah Caves. In Archaeological Investigations in the Niah Caves, Sarawak (eds. Barker, G. & Farr, L.) 401–438 (McDonald Institute for Archaeological Research, Cambridge, 2016).
  29. Brandt, J. H. The Southeast Asian Negrito: further notes on the Negrito of South Thailand. J. Siam. Soc. 53, 27–43 (1965).
  30. Kuchikura, Y. Efficiency and focus of blowpipe hunting among Semaq Beri hunter-gatherers of Peninsular Malaysia. Hum. Ecol.16, 271–305 (1988).
  31. Endicott, K. Batek. In The Cambridge Encyclopedia of Hunters and Gatherers (eds. Lee, R. B. & Daly, R.) 298–306 (Cambridge University Press, Cambridge, 1999).
  32. Fernandez-Jalvo, Y. & Andrews, P. Atlas of Taphonomic Identifications (Springer, New York, 2016).
  33. Rabett, R. J. Bone and tusk tools from the West Mouth and Lobang Hangus. In Archaeological Investigations in the Niah Caves, Sarawak (eds. Barker, G. & Farr, L.) 301–324 (McDonald Institute for Archaeological Research, Cambridge, 2016).
  34. Peres, C. A. & Dolman, P. Density compensation in Neotropical primate communities: Evidence from 56 hunted and non‐hunted Amazonian forests of varying productivity. Oecologia 122, 175–189 (2000).
  35. Fortier, J. The ethnography of south Asian foragers. Ann. Rev. Anthropol. 38, 99–114 (2009).
  36. Mittermeier, R. A. Effects of hunting on rain forest primates. In Primate Conservation in the Tropical Rainforest (eds. Marsh, C. W. & Mittermeier, R. A.) 109–146 (Liss, New York, 1987).
  37. van Vliet, N., Milner-Gulland, E. J., Bousquet, F., Saqalli, M. & Nasi, R. Effect of small-scale heterogeneity of prey and hunter distributions on the sustainability of bushmeat hunting. Conserv. Biol. 24, 1327–1337 (2010).
  38. Erlandson, J. M. et al. The kelp highway hypothesis: marine ecology, the coastal migration theory, and the peopling of the Americas. J. Isl. Coast. Archaeol. 2, 161–174 (2007).
  39. Roberts, P. et al. Fruits of the forest: Human stable isotope ecology and rainforest adaptations in Late Pleistocene and Holocene (~36 to 3 ka) Sri Lanka. J. Hum. Evol106, 102–118.
  40. Gamble, C. Timewalkers: The Prehistory of Global Colonization. (Alan Sutton Press, Gloucester UK, 1993).
  41. Gamble, C. Settling the Earth: The Archaeology of Deep Human History. (Cambridge University Press, Cambridge, 2013).
  42. Hublin, J.-J. et al. New fossils from Jebel Irhoud, Morocco and the pan-African origin of Homo sapiensNature 546, 289–292 (2017).
  43. Boivin, N. et al. Ecological consequences of human niche construction: examining long-term anthropogenic shaping of global species distributions. PNAS 113, 6388–6396 (2016).
  44. Ashton, P. S. & Gunatilleke, C. V. S. New light on the plant geography of Ceylon. I. historical plant geography. J. Biogeogr. 14, 249–285 (1987).
  45. Erdelen, W. Forest ecosystems and nature conservation in Sri Lanka. Biol. Conserv. 43, 115–135 (1988).
  46. Premathilake, R., Hunt, C. O., Perera, N. & Wedage, O. Late Pleistocene humans used rice in Sri Lanka: phytolith investigation of the deposits at Fa Hien Rock Shelter. Global J. Human-Soc. Sci.D17, 19–30 (2017).
  47. Premathilake, R., Hunt, C. O. Earliest Musa banana from the late Quaternary sequence at Fa Hien Rock Shelter in Sri Lanka. J. Quat. Sci33, 624–638 (2018).
  48. OxCal version 4.3.2 (2017).
  49. Bullock, P., Fedoroff, N., Jongerius, A., Stoops, G. & Tursina, T. Handbook for Soil Thin Section Description (Waine Research, Wolverhampton, UK, 1985).
  50. Stoops, G. Guidelines For Analysis and Description of Soil and Regolith Thin Sections (Soil Science Society of America Inc., Madison, USA, 2003).
  51. Dobney, K. & Reilly, K. A method for recording archaeological animal bones: the use of diagnostic zones. Circaea 5, 79–96 (1988).
  52. von den Driesch, A. A Guide to the Measurement of Animal Bones from Archaeological Sites. (Harvard University Press, Cambridge, MA, 1976).
  53. Wilson, D. E. & Reeder, D. M. Mammal Species of the World (John Hopkins University Press, Baltimore, MD, 2005).
  54. Thomas, D. H. Great basin hunting patterns: a quantitative method for treating faunal remains. Am. Antiq. 34, 392–401 (1969).
  55. Grayson, D. K. Quantitative Zooarchaeology: Topics in the Analysis of Archaeological Faunas. (Studies in Archaeology, Academic Press, Cambridge, MA, 1984).
  56. Behrensmeyer, A. K. Taphonomic and ecologic information from bone weathering. Paleobiology 4, 150–162 (1978).
  57. Andrews, P. Experiments in taphonomy. J. Arch. Sci. 22, 147–153 (1995).
  58. Shipman, P. & Rose, J. Bone tools: an experimental approach. In Scanning Electron Microscopy in Archaeology (ed. Olsen, S. L.) 303–335 (British Archaeological Reports International Series, Archaeopress, Oxford, 1988).
  59. Shipman, P., Foster, G. & Schoeninger, M. Burnt bones and teeth: an experimental study of color, morphology, crystal structure and shrinkage. J. Arch. Sci. 11, 307–325 (1984).
  60. Johnson, E. Human modified bones from early southern Plains Sites. In Bone Modification (eds. Bonnichsen, R. & Sorg, M.) 431–471 (Center for the Study of First Americans, Orono, ME, 1989).
  61. Brain, C. K. The Hunters or the Hunted? An Introduction to African Cave Taphonomy. (Chicago University Press, Chicago, IL, 1981).
  62. Cain, C. R. Using burned animal bone to look at middle stone age occupation and behavior. J. Arch. Sci. 32, 873–884 (2005).
  63. Bar‐Oz, G., Belfer‐Cohen, A., Meshveliani, T., Djakeli, N. & Bar‐Yosef, O. Taphonomy and zooarchaeology of the Upper Palaeolithic cave of Dzudzuana, Republic of Georgia. Int J. Osteoarch 18, 131–151 (2008).
  64. Klein, R. G. & Cruz-Uribe, K. The Analysis of Animal Bones from Archeological Sites. (Chicago University Press, Chicago, IL, 1984).
  65. Lyman, R. L. Vertebrate Taphonomy. (Cambridge Manuals in Archaeology, Cambridge University Press, Cambridge, UK, 1994).
  66. Bunn, H. T. Comparative analysis of modern bone assemblages from a San hunter-gatherer camp in the Kalahari Desert camp, Botswana, and from a spotted hyena den near Nairobi, Kenya. (British Archaeological Reports International Series, Archaeopress, Oxford, 1983).
  67. Marean, C. W., Dominguez-Rodrigo, M. & Pickering, T. R. Skeletal element equifinality in zooarchaeology begins with method: the evolution and status of the “shaft critique”. J. Taphon. 2, 69–98 (2004).
  68. Pelegrin, J., Karlin, C. & Bodu, P. Chaînes opératoires: un outil pour le préhistorien. Technol. préhistorique 25, 55–62 (1988).
  69. Lemonnier, P. The study of material culture today: toward an anthropology of technical systems. J. Anthropol. Archaeol. 5, 147–186 (1986).
  70. Inizan, M.-L., Roche, H. & Tixier, J. Technology of Knapped Stone. Prehistoire de la pierre taillée, Vol. 3 (CREP, Meudon, 1992).
  71. Backwell, L., d’Errico, F. & Wadley, L. Middle stone age bone tools from Howiesons Poort layers, Sibudu Cave, South Africa. J. Arch. Sci. 35, 1566–1580 (2008).
  72. Blasco, R., Rosell, J., Fernández Peris, J., Caceres, I. & María Vergès, J. A new element of trampling: an experimental application on the Level XII faunal record of Bloomer Cave (Valencia, Spain). J. Arch. Sci. 35, 1605–1618 (2008).
  73. Bradfield, J. & Brand, T. Results of utilitarian and accidental breakage experiments on bone points. Archaeol. Anthropol. Sci. 7, 27–38 (2015).
  74. Buc, N. Experimental series and use-wear in bone tools. J. Arch. Sci. 38, 546–557 (2011).
  75. Buc, N. & Loponte, D. Bone tool types and micro wear patterns: Some examples from the Pampa Region, South America. In Bones as Tools: Current Methods and Interpretations in Worked Bone Studies (eds. Gates St-Pierre, C., Walker, R. B.) 143–147 (British Archaeological Reports International Series, Archaeopress, Oxford, 2007).
  76. Gates St-Pierre, C. 2007. Bone awls of the St. Lawrence Iroquoians: A micro wear analysis. In Bones as Tools: Current Methods and Interpretations in Worked Bone Studies (eds. Gates St-Pierre, C., Walker, R. B.) 107–118 (British Archaeological Reports International Series, Archaeopress, Oxford, 2007).
  77. Langley, M. C., O’Connor, S. & Aplin, K. A>46,000-year-old macropod bone implement from Carpenter’s Gap 1: Challenging past perspectives of Pleistocene Australia. Quat. Sci. Rev. 154, 199–213 (2016).
  78. Legrand, A. & Sidéra, I. Methods, means, and results when studying European bone industries. In Bones as Tools: Current Methods and Interpretations in Worked Bone Studies (eds. Gates St-Pierre, C., Walker, R. B.) 67–79 (British Archaeological Reports International Series, Archaeopress, Oxford, 2007).

Continue reading Specialized rainforest hunting by Homo sapiens ~45,000 years ago


Dancing in the darkness of a climate crisis

Source – Link

By Vidhura Ralapanawe

Globally, Sri Lanka ranks as the sixth most vulnerable to climate change. But this reality has not taken hold in Sri Lankan polity. This is partly because we do not have sufficient analysis of climate change impacts nor a communication strategy to help public and policymakers understand it better.

When many countries are planning large-scale interventions based on specific localised impact assessments, we are literally dancing in the dark.

The four years from 2015 to 2018 were the warmest globally since records began in 1880, a trend mirrored in Sri Lanka. This country saw a sharper rise in temperature between 1960 and 2000 than the global trend while 2016 was the highest recorded. The impact has been substantial. Continue reading Dancing in the darkness of a climate crisis

Becoming Greta: ‘Invisible Girl’ to Global Climate Activist, With Bumps Along the Way

Source – Link

By Somini Sengupta

Greta Thunberg, center, skips school on Fridays to demonstrate for climate action at the Swedish Parliament in Stockholm. Elisabeth Ubbe for The New York Times

STOCKHOLM — It’s complicated being Greta.

Small, shy, survivor of crippling depression, Greta Thunberg, the 16-year-old Swedish girl skipping school to shame the world into addressing climate change, drew a parade of fans one Friday in February on a frozen square in Stockholm.

Six Swiss students had traveled 26 hours by train to seek her support for their petition for a tougher Swiss carbon emissions law. An Italian scientist told her she reminded him of his younger, activist self. A television news crew hovered around her. Women from an anti-smoking group came to give her a T-shirt.

Greta nodded, whispered, “Thanks,” posed for pictures. Made exactly zero small talk.

All this attention, she said out of earshot of the others, is great. It means “people are listening.” But then, a knife-blade flash of rage revealed itself.

“It’s sometimes annoying when people say, ‘Oh you children, you young people are the hope. You will save the world’” she said, after several grown-ups had told her just that. “I think it would be helpful if you could help us just a little bit.”

This is signature Greta. Wry. Blunt. Sometimes sarcastic. The opposite of sweet.

It surfaced again on Friday, when Prime Minister Theresa May’s office dismissed school walkouts in Britain as a distraction that “wastes lesson time.” Greta swiftly struck back on Twitter: “But then again, political leaders have wasted 30 yrs of inaction. And that is slightly worse.”

Continue reading Becoming Greta: ‘Invisible Girl’ to Global Climate Activist, With Bumps Along the Way

Count the birds: Public urged to join global initiative

Source – Link

As the annual initiative, Great Backyard Bird Count (GBBC) from February 15-18–where birdwatchers around the world are invited to count and report details of birds in the area in which they live– marks its last day tomorrow, a veteran ornithologist here has said it was important to keep a tab on what are regarded as common birds too.

Prof. Sarath Kotagama says that while many are concerned about the declining numbers of rare birds, the numbers of common birds, too, could dip towards extinction without anyone realizing it and, therefore, it was important to take a count of those birds too.

The latest ‘State of the World Birds’ report published by BirdLife International reveals that while highly threatened species continue to go extinct, what were once considered common and widespread species too are in sharp decline. At least 40% of bird species worldwide (3,967) have declining populations, compared with 44% that are stable (4,393) according to the report. Continue reading Count the birds: Public urged to join global initiative

Artificial rain: Climatologist urges Govt. to conduct a trial first

Source: Link

A senior climatologist in the committee that studied a proposal to produce artificial rain for hydropower generation has urged the Government to conduct a thorough cost-benefit analysis and environmental impact study before taking the project beyond its trial stage.

The Ceylon Electricity Board (CEB) and the Sri Lanka Air Force (SLAF) this week signed an agreement to facilitate the rainmaking initiative with technical expertise from the Thai Government. The project is expected to benefit Sri Lanka in periods of drought to avoid buying expensive power from independent power producers, Power and Energy Minister Ravi Karunanayake was quoted as saying.

But Ranjith Punyawardena, Principal Climatologist of the Department of Agriculture, expressed caution, saying the Government must not go beyond a pilot project before analysing whether the high cost initiative would have the required result of producing sufficient rainfall for hydropower generation.

Rainmaking here will involve the use of the chemicals calcium chloride, calcium oxide, sodium chloride and urea. There are three steps. The first is cloud “triggering” where sodium chloride is sprayed into small clouds or cumulus. Several hours later, there is cloud “fattening” or the application of calcium chloride and calcium oxide to the clouds.

The final stage is cloud “attacking” where one aircraft sprays sodium chloride from above the cloud while the other sprays urea from the base, both at the same time. This is called a “sandwich operation” as there are two planes going through the cloud. The exercise will be expensive for Sri Lanka. Thailand’s Royal Rainmaking Agency has 24 aircraft and hangars dedicated and especially maintained for the purpose of cloud seeding. However, Sri Lanka will use its limited SLAF planes, risking corrosion from long-term exposure to salt.

Dr Punyawardena was part of a committee that included representatives of the CEB, the SLAF, the Power and Energy Ministry, the Mahaweli Authority, the Irrigation Department, the Central Environmental Authority, the Met Department and the Department of Agriculture. With 30 years of experience in climate science, he was also doubtful that this exercise would produce the required amount of rainfall. For that reason, he insisted that it must be done as a pilot project, to be up-scaled if successful.

“Even if the trial succeeds, it must be replicated several times because atmospheric stability changes from time to time depending on the global ocean atmospheric circulation from time to time,” Dr Punyawardena said.

The initiative will be monitored by the Ministry, the CEB and the committee, said a spokesman for the utility. After some runs were conducted last year, water samples were collected from the ground and found to be affected to a “negligible level” by scientists, he said. This was still at pre-feasibility stage, he added. If implemented, formal procedures such as an Environmental Impact Assessment (EIA) may need to be conducted.
“The amount of chemicals they are going to use in this mission may be insignificant compared to the area they will spray,” said Dr Punyawardena. “But if we are to keep on spraying regularly, there could be an accumulation of salt in the soil and water bodies. It all depends on how it is practised.”

There are concerns, too, about how effective the exercise would be in Sri Lankan conditions. Cloud seeding will be done when there is no rain. But at such times, climatologists say, the atmosphere over Sri Lanka is “highly stable” and it could be futile to apply chemicals to a stable atmosphere as it will not bring on precipitation.

Cloud seeding was done with Thai technology even in the early to mid-70s during the Sirimavo Bandaranaike government. It produced some rain, not a significant amount. What is needed, observes said, were proactive approaches–not reactive ones, such as a rainmaking through artificial means. These include conserving the Central highlands, forestation and reforestation and soil conservation.

Experts have also called for sound practices to ensure the country puts to good use the rainfall it does receive. Pakistan, with between 300-400mm annual rainfall, is managing its water. However, Sri Lanka gets 800-1,500mm of rainfall per year but does not manage it well enough to maximise use.

The committee had agreed that cloud seeding will take place just before the onset of convectional rain. This means, when the land warms up, it heats the air above it, causing the air to expand and rise. As the air rises it cools and condenses. If this process continues, there will be rain.
“The sun is directly overhead Sri Lanka in March and early April and somewhere in September and October,” explained Dr Punyawardena. “This is when convectional activity is intense, just before the Yala and Maha rains. That is the time they will try this, to trigger the rainfall. I’m not sure how much it will bring down and whether there will be a gain for the amount spent on it. That has to studied.”

Weather monitoring: Equipment worth Rs. 72m gone with the wind

By Sandun Jayawardana

Sri Lanka has abandoned an initiative to use satellite technology during natural disasters, leaving Rs 72 million worth of equipment unused for four years before finally dismantling it, the Auditor General (AG) has found. The project was initiated in 2011 and given up despite the country facing severe natural disasters in previous years, states the latest report of the AG on the Disaster Management Centre (DMC). The DMC found out that the satellite technology equipment was not compatible with its other systems, only when the full system was installed.

The DMC Director General admitted to the AG that the equipment was bought without first conducting a proper study. The project’s nerve centre was an Information Communication Centre (ICC) established in Padukka under the International Centre for Emergency Techniques based in the Netherlands. Continue reading Weather monitoring: Equipment worth Rs. 72m gone with the wind

Pollution: 300 million children breathing toxic air – UNICEF report

Original article

NEW YORK 31 October 2016 – Almost one in seven of the world’s children, 300 million, live in areas with the most toxic levels of outdoor air pollution – six or more times higher than international guidelines – reveals a new UNICEF report.

Residents in Lagos,Nigeria,navigate the polluted waters of Makoko,a fishing community mostly made up of structures on stilts above Lagos Lagoon,as smoke from a nearby house spills out over the canals

Clear the Air for Children uses satellite imagery to show for the first time how many children are exposed to outdoor pollution that exceeds global guidelines set by the World Health Organization (WHO), and where they live across the globe.

The findings come a week ahead of the COP 22 in Marrakesh, Morocco, where UNICEF is calling on world leaders to take urgent action to cut air pollution in their countries. Continue reading Pollution: 300 million children breathing toxic air – UNICEF report

Sri Lanka committee to look in to Norochcholai environmental issues


Norochcholai power station

Sep 21, 2016 (LBO) – Sri Lanka’s Public Utilities Commission (PUCSL) has appointed a 7 member committee to look at the environmental damage allegations that have been leveled against the Norochcholai power station.

“We have received several complaints about this so we appointed a committee that is qualified to look into this matter,” Damitha Kumarasinghe, director general, Public Utilities Commission of Sri Lanka (PUCSL) told Lanka Business Online. Continue reading Sri Lanka committee to look in to Norochcholai environmental issues

Mass bleaching of Sri Lanka coral reefs

Friday, July 1, 2016

Originally Published in ECONOMYNEXT


Higher than normal ocean temperatures off Sri Lanka’s coast is threatening to damage the best coral reefs in the island, according to surveys done by marine scientists of the National Aquatic Resources Research and Development Agency (NARA).

“Underwater surveys shows widespread bleaching or whitening along the reefs, especially in shallow depths (of less than 10 meters) in the south and south west coast and also reported in Jaffna and Bar Reef in Kalpitiya,” a statement said.
Continue reading Mass bleaching of Sri Lanka coral reefs

Flood control system to be set up in Colombo

Thursday, June 02, 2016

Originally Published in the Sunday Times

A flood and drainage management system aimed at preventing flooding in the Colombo city and its outskirts costing more than Rs. 21 billion will get off the ground early next year, a senior official said.

The design for the project which is already prepared following an extensive study on the flooding situation in the city and its outskirts includes introduction of new canal systems, underground tunnels for the flow of water and pumping stations to discharge excess water, Secretary to the Ministry of Megapolis and Western Development, Nihal Rupasinghe told the Sunday Times.

Continue reading Flood control system to be set up in Colombo


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