Shell tool use by early members of Homo erectus in Sangiran,central Java,Indonesia: cut mark evidence

Sangiran has been known as a source of fossil Homo erectus but is better known for the absence of archaeological tools. Cut mark analysis of Pleistocene mammalian fossils documents 18 cut marks inflicted by tools of thick clamshell flakes on two bovid bones created during butchery at the Pucangan Formation in Sangiran between 1.6 and 1.5 million years ago. These cut marks document the use of the first tools in Sangiran and the oldest evidence of shell tool use in the world.     

The significance of the fossil hominid skull from Petralona,Greece

Evidence is accumulating that the hominid cranium found in the Petralona cave in 1960 is associated with cave deposits of middle Pleistocene age. If this is so, the fossil is the most complete middle Pleistocene cranium yet discovered and provides important morphological, metrical and radiographic information on the possible evolutionary transition from Homo erectus to Homo sapiens. The classification of the specimen is discussed and it is suggested that a grade system within Homo spaiens should be erected. The Petralona fossil would be allocated to Homo sapiens grade 1 rather than to Homo erectus or to a subspecies of Homo sapiens.     

Middle pleistocene adaptations in Central Europe

The biological evolution documented in the fossil and archaeological record of Central Europe between about 700,000 and 100,000 years ago reflects the transition fromHomo erectus to the earliestHomo sapiens. These populations created different types of industries, ranging from assemblages of small artifacts and industries with simple pebble tools to standardized units such as the Evolved Acheulean and the Early Mousterian. The industries of the Last Interglacial (Taubachian) show some regression in technological standardization and a reappearance of small artifacts. Other aspects of cultural adaptation (settlements, dwellings, hunting activity, symbolic and aesthetic expressions) are also summarized. It is suggested that the impact of climate and climatic changes on human settlement and behavior was greater in Central Europe (where two glaciations advanced from both north and south) than in the Mediterranean and Western Europe. The general trend of cultural veolution was toward greater technological and social complexity, but its course was not unilinear.     

Vault thickness in two Pleistocene Australian crania

This study examines vault thickness in two Pleistocene crania at the centre of discussions about the evolution of Indigenous Australians and competing scenarios about modern human origins: Willandra Lakes Human (WLH) 3 and WLH 50. We estimated total vault thickness and thickness of the diploë, external and internal table on CT-scans, and undertook a quantitative comparison of them. We found that they differ significantly in absolute thickness, but are similar in terms of the relative contribution to thickness made by the diploic space and total table. They also differ significantly in terms of relative variation in thickness, and in several instances, WLH 50 shows greater variability than WLH 3. This finding undermines pathology as an explanation for thickness in the former cranium. Among later hominins, WLH 50 is highly unusual in possessing an extremely thick vault at bregma. We show, however, that vault thickness at this landmark is positively allometrically scaled in Indigenous Australians, but negatively scaled in Ngandong Homo erectus. Thus, vault thickness is mostly explained by the extremely large size of WLH 50: one of the largest hominin crania ever found. Moreover, its extreme thickness firmly establishes its affinities with modern humans rather than the Ngandong group. Despite the important role played by epigenesis in the development of the cranial vault, similarities between WLH 3 and WLH 50 indicate some canalisation in the extent to which the various vault components contribute to total thickness.     

The phylogenetic significance of the Middle Pleistocene Narmada hominin cranium from central India

A parsimony analysis of the Narmada cranium from central India and a number of other demes and species of Homo concludes that the Narmada hominin shares a closer relationship with the European Steinheim specimen, than with Asian H. erectus or H. pekinensis. This suggests that the population represented by the Narmada cranium is likely to have had its origins in Europe rather than in Asia. Overall the available evidence supports an ‘Out of Africa’ scenario, as the early Asian hominins belong to a distinct clade which has no extant descendants and thus appear to represent an evolutionary ‘dead end’. The later African and European hominins are defined by a clade including early H. sapiens from Africa. The main difference between these two distinct clades is that the H. erectus lineage is defined by increasing degrees of neuro‐orbital disjunction associated with increased anterior cranial base extension, while the lineage leading to early H. sapiens is characterized by the opposite condition of reduced neuro‐orbital disjunction associated with increased anterior cranial base flexion. While there is also evidence of differential patterns of head and neck musculature between these two clades, they are of secondary importance. Preliminary dating of bovid remains found in association with the hominin cranium by the gamma spectrometric U‐series dating technique suggests a tentative minimum age of not less than 236,000 years. This is in agreement with evidence from biostratigraphical studies of the Boulder Conglomerate, which place these deposits in the Middle Pleistocene. Copyright © 2004 John Wiley & Sons, Ltd.     

Getting “Out of Africa”: Sea Crossings,Land Crossings and Culture in the Hominin Migrations

Palaeoanthropologists and archaeologists have advanced a wide range of explanatory narratives for the various movements of Homo erectus/Homo ergaster, and the first modern Homo sapiens, “Out of Africa”—or even back again. The application of Occam's razor—a parsimonious approach to causes—gives a more cautious approach. There is nothing in the available evidence that would require the ability for a human water crossing from Africa before the later Pleistocene, whether across the Strait of Gibraltar, the Sicilian Channel or the southern Red Sea (Bab el-Mandab). A parsimonious narrative is consistent with movements across the Sinai peninsula. The continuous arid zone from northern Africa to western Asia allowed both occupation and transit during wet phases of the Pleistocene; there is no requirement for a “sponge” model of absorption followed by expulsion of human groups. The Nile Valley as a possible transit route from East Africa has a geological chronology that could fit well much current evidence for the timing of human migration. The limited spatial and temporal opportunities for movements “Out of Africa,” or back again, also puts particular difficulties in the way of the gene flow required for the multiregional hypothesis of the development of modern Homo sapiens.     

Significance of diadematid echinoid ossicles in micropalaeontological samples,Miocene–Pliocene of Indonesia

Fragments of diadematoid echinoids from the early and middle Miocene, and late Miocene–Pliocene, respectively, of Java, Kalimantan and Sulawesi, Indonesia, are identified as diadematid spp. indet. (radioles from all sites) and Centrostephanus sp. (an interambulacral plate; early Miocene, Java). The radioles are probably a mixture of Diadema ± Centrostephanus ± Echinothrix. This is the first report of identifiable fossil diadematoid remains from Indonesia and demonstrates that these echinoids, so common in modern reef environments, were present in the Neogene of the region. Even though classified in open nomenclature, Centrostephanus sp. nevertheless provides further evidence for the Cenozoic record of a genus in which the only nominal species are of Late Cretaceous and Holocene age.     

Kariandusi: Acheulean morphology and the question of allometry

Allometry, or size-related variation, is shown to be an important factor in the bifaces of two separate assemblages from the Acheulean site of Kariandusi in Kenya. Such variation has functional and possibly stylistic implications. The paper gives a review of the archaeology of Kariandusi, and then investigates the question of size and shape variation in bifaces. The Upper Sites at Kariandusi, first investigated by L. S. B. Leakey, have yielded many obsidian bifaces which can be dated to approximately 0.7–1.0 myr ago. Material from the Lower Site, including many lava bifaces, is judged to be stratigraphically younger but probably in the same time range. We show by making comparisons with the neighbouring Acheulean sites of Kilombe and the Kapthurin Formation that allometry is present in biface assemblages at least 0.5 myr different in date; that similar principles of allometry operate in all the assemblages; and that where there are differences of allometric pattern, within-site variation is sometimes greater than variation between distant sites. We conclude that the size of a biface at least partly determines the shape in which it was made, and that sites in the time range ofHomo erectus and earlyHomo sapiens show surprisingly similar allometric patterns.

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Résumé Il est démontré que l'allométrie ou variation dimensionnelle, est un facteur important des bifaces de deux collections séparées du site acheuléen de Kariandusi au Kénya. Une telle variation a des implications fonctionnelles et peut-être aussi stylistiques. Cet article examine l'archéologie de Kariandusi, puis étudie la question des variations de dimensions et de formes dans les bifaces. Les sites plus élevés de Kariandusi, que L.S.B. Leakey a été le premier à fouiller, ont donné de nombreux bifaces d'obsidienne que l'on peut dater d'environ 0,7–1,0 million d'années. Le matériel obtenu dans le site inférieur, y compris de nombreux bifaces en lave, est jugé plus récent stratigraphiquement, mais probablement de la même période. En faisant des comparaisons avec les sites acheuléens voisins de Kilombe et de la Formation Kapthurine, nous démontrons que l'allométrie est présente dans des collections de bifaces dont les dates diffèrent d'au moins 0,5 million d'années; que des principes d'allométrie similaires s'appliquent à toutes les collections; et que lorsqu'il y a des différences de schéma allométrique, la variation au sein d'un même site est souvent plus importante que la variation entre des sites distants. Nous concluons que la dimension d'un biface détermine au moins partiellement sa forme, et que les sites de la période de l'Homo erectus et du début de la période de l'Homo sapiens présentent des schémas allométriques étonamment semblables.

     

Entry points for local tourism in developing countries: evidence from Yogyakarta, Indonesia

International tourism is an increasingly important source of income and employment for many developing countries with over 690 million annual international arrivals (World Tourism Organisation data). This paper considers the impact of tourism in the city of Yogyakarta, in Java, Indonesia, and asks whether one subsector of international tourism, namely backpacker tourism, provides a way for local people to enter this globalised industry. The paper examines the emergence of small‐scale, bottom‐ up tourism and its transformatory effect upon a previously poor kampung (urban village). It is suggested that the nature of small‐scale, locally owned tourism businesses, particularly their minimal capital requirements, may be seen as a form of ‘pro‐poor tourism’ and may provide a useful component of local economic development strategies for poor communities. Further, smallscale tourism development may also be seen as an effective local response to some of the effects of globalisation, specifically increasing flows of international tourists to developing countries.     

Evidence of Stress Fracture in a Homo antecessor Metatarsal from Gran Dolina Site (Atapuerca,Spain)

We present the palaeopathological analysis of a right fourth metatarsal (ATD6‐124) recovered from the Atapuerca–Gran Dolina site (Spain). This fossil, ca. 1 Ma, belongs to Homo antecessor, the earliest known European hominin species. The metatarsal exhibits a proliferative lesion on its medial periosteal surface. Periosteal reaction can be the bone response to a wide number of injurious processes. We describe a lesion on the basis of macroscopic and microscopic analyses, including microtomography and scanning electron microscopy. Externally, the osteoblastic lesion presents a highly porotic and disorganised morphology. Internally, we observe a series of micro‐fractures on the compact bone that do not affect the medullary canal. We provide a differential diagnosis and suggest that the ATD6‐124 lesion could correspond to a pedal stress fracture, also known as fatigue or march fracture. Stress fractures have been related to a load increase and muscular fatigue. This type of fracture has been widely reported in the foot of soldiers and athletes, which are usually engaged in strenuous, excessive or prolonged locomotive activities. Despite its high frequency in these groups, stress fractures have not been reported as such in fossil collections, with the exception of a metatarsal belonging to the Sima de los Huesos site (Atapuerca). Copyright © 2013 John Wiley & Sons, Ltd.     

Pleistocene connexions between Africa and Southwest Asia: an archaeological perspective

This paper investigates the archaeological evidence for direct prehistoric connexions between Southwest Asia and Africa during the Palaeolithic period. The importance of the ‘Levantine Corridor’ bridging the two continents is stressed in describing the dispersal ofHomo erectus. The continental bridge could have been through the Nile Valley during the Late Acheulian and the emergence of earlyHomo sapiens. Upper Palaeolithic and especially Epi-Palaeolithic dispersal during the terminal Pleistocene are discussed. The role of Egyptian-Levantine connexions in the context of the complex situation which led to sedentism is stressed.     

Book review

Herman C. Kemp. Annotated bibliography of bibliographies on Indonesia. xvii, 433pp. Leiden: KITLV Press, 1990. (Koninklijk Instituut voor Taal‐, Land‐ en Volkenkunde. Bibliographical series, 17.) Guilders 70.     

The lower paleolithic of the Near East

The Near East forms the geographic crossroads between Africa, Asia and Europe and was certainly a main route for the dispersal of Homo erectusinto Eurasia. The study of Lower Paleolithic sites in this region and in the neighboring Caucasus area sheds some light on several potential colonization events. Sites such as Ubeidiya (Jordan Valley) and Dmanisi (Georgia) suggest the early sorties took place around 1.4-1.0 Ma. Despite the lack of radiometric dates, sequences of raised beaches, marine deposits, river terraces, and paleolake formations have enabled various investigators to identify several series of major aggradation and erosion periods within the Pleistocene. Lithic assemblages derived from a few systematic excavations and collections from stratigraphically dated outcrops led to a threefold subdivision of the Acheulian sequence into the Lower, Middle, and Upper Acheulian. The study of nonbiface assemblages, however, has not resolved the question of whether these assemblages deserve inclusion as separate entities or should be viewed as sites within the Acheulian settlement pattern. While the typotechnological definitions of each major phase can be compared to what is known from other regions of the Old World, the Acheulo-Yabrudian (or the Mugharan Tradition) is seen as a local entity. Rare human remains and scarce data concerning subsistence activities do not warrant a comparative discussion with what is known from African and some European sites.     

Book reviews

Pieter van de Velde (ed.). Prehistoric Indonesia: a reader. vii, 404 pp. Dordrecht: Foris Publications, 1984. (Verhandelingen van het Koninklijk Instituut voor Taal‐, Land‐ en Volkenkunde, 104.)

B.J. Boland and I. Farjon. Islam in Indonesia: a bibliographical survey 1600–1942, with post‐1945 addenda. xxii, 173 pp. Dordrecht: Foris Publications, 1983. (Koninklijk Instituut voor Taal‐, Land‐ en Volken‐kunde. Bibliographical Series, 14.) Guilders 40.

Anthony J. Whitten and others. The ecology of Sumatra. [By] Anthony J. Whitten, Sengli J. Damanik, Jazanul Anwar, Nazaruddin Hisyam. xvii, 583pp., 64 plates. Yogyakarta: Gadjah Mada University Press, 1984. $20.

Jan Breman. Control of land and labour in colonial Java: a case study of agrarian crisis and reform in the region of Cirebon during the first decades of the 20th century. xii, 159 pp. Dordrecht: Foris Publications, 1983. (Verhandelingen van het Koninklijk Instituut voor Taal‐, Land‐ en Volkenkunde, 101.)     

From Islamism to nationalism in Aceh,Indonesia

ABSTRACT. This article analyses a dramatic political transformation in Indonesia's Aceh province. In the 1950s, an Islamic rebellion (Darul Islam) aimed not to separate Aceh from Indonesia, but rather to make Indonesia an Islamic state. A successor movement from the 1970s was GAM, the Free Aceh Movement. GAM, however, was essentially secular‐nationalist in orientation, sought Aceh's complete independence and did not espouse formal Islamic goals. The transformation is explained by various factors, but the key argument concerns the relationship between Islam and nationalism. The defeat of Darul Islam had caused Aceh's Islamic leaders to focus on what they could achieve in Aceh alone, ultimately giving rise to Acehnese nationalism and the secessionist goal. However, Islam remained a point of commonality with, rather than difference from, majority‐Muslim Indonesia. The logic of nationalist identity construction and differentiation thus caused Aceh's separatist leaders, despite being personally devout, to increasingly downplay Islamic symbols and ideology.     

Cultural Resource Management for a Majapahit Kingdom Site in Trowulan,East Java,Indonesia

Abstract

The Kingdom of Majapahit located in East Java, Indonesia, was established in 1293 ce and lasted until its destruction in the sixteenth century. At its peak, the Kingdom covered the modern-day region of Indonesia and the Malay Peninsula. Archaeological remains from the Majapahit era have been discovered in several places, including Java, Bali, and Sumatra, but the most important site is located in the small town of Trowulan in East Java. Trowulan has been researched since the beginning of nineteenth century, with most of the work concerned with the study and preservation of the archaeological remains; little research has taken place regarding the archaeological remains in the relation to the local community. Archaeologists and the government agree that the inhabitants of Trowulan have violated regulations related to the protection of the monuments and that their activities have damaged the site. Until now neither the neither archaeologists nor the government have conducted any research into the reasons behind the local community’s actions. Understanding the local communities’ perspectives and aspiration is essential in order to develop relevant recommendations regarding the protection and management Trowulan’s cultural heritage. This research has been undertaken using qualitative methods, including observations, in-depth interviews, and Focus Group discussions.     

Provenience,age and associations of archaic Homo sapiens crania from Lake Eyasi,Tanzania

Fifty years ago, an ethnographic expedition found primitive human fossils at Lake Eyasi, Tanzania. Subsequent emphasis has centered almost exclusively on cranial morphology, neglecting the discovery site and associated finds. Fauna has been deemed “essentially modern” and racemization dates suggest a late Pleistocene age for the hominid remains; these assessments have been advanced as consistent with a “terminal Middle Stone Age” antiquity. Based on recent observations at the site and new sediment analyses, a provisional sequence is now proposed: an earlier formation, the Eyasi Beds, is distinguished from later Pleistocene deposits, the Mumba Beds, the latter being partially calibrated by uranium series and radiocarbon dates. This evidence indicates that the Eyasi Beds, the probable source of the human fossils, are older than 130,000 years, and the fauna may include seven extinct large mammal species. Documented Eyasi Beds artifacts are mostly unspecialized Middle Stone Age types; no typological or technical features suggest later MSA specializations or innovations foreshadowing Later Stone Age industries. A series of core tools from the lakeshore suggests an industry of Sangoan aspect. All lines of evidence from the locality contradict the young amino acid racemization dates; artifacts and fauna, including archaic Homo sapiens remains, are of probable Middle Pleistocene age.     

First large‐scale provenance study of pigments reveals new complex behavioural patterns during the Upper Palaeolithic of south‐western Germany

The use of red iron‐based earth pigments, or ochre, is a key component of early symbolic behaviours for anatomically modern humans and possibly Neanderthals. We present the first ochre provenance study in Central Europe showing long‐term selection strategies by inhabitants of cave sites in south‐western Germany during the Upper Palaeolithic (43–14.5 ka). Ochre artefacts from Hohle Fels, Geißenklösterle and Vogelherd, and local and extra‐local sources, were investigated using neutron activation analysis (NAA), X‐ray diffraction (XRD) and scanning electron microscopy (SEM). The results show that local ochre sources were continuously and systematically accessed for c.29 500 years, with periodic events of long‐distance (about > 300 km) ochre acquisition during the Aurignacian (c.35–43 ka), suggesting higher mobility than previously suspected. The results reveal previously unknown long‐term, complex spatio‐temporal behavioural patterns during the earliest presence of Homo sapiens in Europe.     

A 6000 Year‐old Fossil Dugong from Botany Bay: Inferences about Changes in Sydney's Climate,Sea Levels and Waterways

The excavation in the 1890s of a skeleton of the warm‐water marine mammal Dugong dugon, associated with Aboriginal artefacts, from a Botany Bay salt marsh, marked the beginning of speculation about climate and sea level change in Australia over the period of human occupation. The dugong bones have recently been dated, giving a conventional ¹⁴C age of 5520±70 years BP, which is consistent with three older ¹⁴C dates for a layer of buried trees that underlies much of the north Botany sediments. The carefully drawn cross‐sections of depositional strata produced by the original discoverers allow further interpretation of the pattern of Holocene sea‐level fluctuations in the Sydney region. Layers of estuarine sediment, such as the one containing the dugong skeleton, are inter‐bedded with peat layers containing in situ roots and stumps, suggesting that the site alternated between sub‐aerial exposure and submergence throughout the Holocene. The presence of the dugong is suggestive of warmer conditions, and its inland location indicates a more extensive Botany Bay in the recent past. This is in agreement with other work from southern New South Wales describing both warm‐water marine species and higher sea levels several thousand years ago.

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MATHEMATICS,STATISTICS AND ARCHAEOMETRY: THE PAST 50 YEARS OR SO*

This review of developments in the use of mathematics and statistics in archaeometry over the past 50 years is partial, personal and ‘broad‐brush’. The view is expressed that it is in the past 30 years or so that the major developments have taken place. The view is also expressed that, with the exception of methods for analysing radiocarbon dates and increased computational power, mathematical and statistical methods that are currently used, and found to be useful in widespread areas of application such as provenance studies, don't differ fundamentally from what was being done 30 years ago.