1 Mitteilungen der Gesellschaft für Urgeschichte 16 (2007) 11 Economic behaviors and cognitive capacities of early hominins between 2.34 Ma and 0.70 Ma in West Turkana, Kenya Sonia Harmand Laboratoire de Préhistoire et Technologie Maison de l Archéologie et de l Ethnologie 21 allée de l Université Nanterre Cedex Abstract: In the past few years, an increasing number of discoveries of Early Stone Age sites in East Africa revealed a more complex picture of early hominins behaviors than had been documented before. However, evidence of technological elaboration and abilities among our early ancestors remains limited, and the nature of the technical change during African Lower Paleolithic is still poorly documented. This paper presents the results of a comparative techno-economic study of four rich and well-preserved Early Oldowan, Oldowan, Early Acheulean, and Acheulean lithic assemblages from a recently investigated region of East Africa, the Nachukui Formation west of Lake Turkana, Kenya. This study, spanning a wide chronological period ranging from 2.34 to 0.70 Ma, documents the antiquity of raw material provisioning strategies in very early chronological contexts in highlighting the existence for raw material selectivity and technological planning as early as 2.34 Ma. The comparative analysis demonstrates diachronic differences in patterns of resource use between the sites from the Late Pliocene, the Early Pleistocene, and the very beginning of the Middle Pleistocene. These differences are related to an improvement in technical skills throughout the Plio-Pleistocene rather than to variations in resource availability. Keywords: Early hominins, West Turkana, Kenya, Plio-Pleistocene, Raw material procurement and management, Selectivity, Technical changes Ökonomieverhalten und kognitive Fähigkeiten früher Homininen zwischen 2,34 und 0,70 Millionen Jahren vor heute in West Turkana, Kenia Zusammenfassung: In den vergangenen Jahren hat eine wachsende Zahl an Fundplätzen des Early Stone Age in Ostafrika gezeigt, dass das Bild vom Verhalten früher Homininen wesentlich komplexer ist als bisher angenommen. Nach wie vor sind jedoch die Hinweise auf die technischen Fähigkeiten unserer frühen Vorfahren überhaupt sowie auf Verbesserungen im Bereich der Technologie begrenzt, und das Ausmaß und die Art des Technologiewandels während des afrikanischen Altpaläolithikums sind immer noch unzureichend erfasst. Der Beitrag präsentiert die Ergebnisse einer vergleichenden techno-ökonomischen Untersuchung am Fundmaterial aus vier reichen und gut erhaltenen Steinartefaktkomplexen des frühen Oldowan mit einem Alter von etwa 2,34 Millionen Jahren (Lokalalei 2C), des Oldowan mit einem Alter von ca. 1,70 Millionen Jahren (Kokiselei 5), des frühen Acheuléen mit einem Alter von ca. 1,65 Millionen Jahren (Kokiselei 4) und des Acheuléen mit einem Alter von ca. 0,70 Millionen Jahren (Nadung a 4). Alle genannten Fundplätze befinden sich in einer in den vergangenen Jahren untersuchten Region in Ostafrika, der Nachukui-Formation westlich des Turkana-Sees in Kenia. Mit den genannten Alterseinstufungen umfasst das analysierte Fundmaterial einen großen zeitlichen Rahmen. Als Rohmaterialien dienten vor allem vier Haupttypen vulkanischer Gesteine, nämlich Phonolith, Basalt, Trachyt und Rhyolith, dazu kommen einige Silkatgesteine und Syenit. Durch die Untersuchungen kann gezeigt werden, wie weit in der Menschheitsentwicklung bewusste Rohmaterialbeschaffungsstrategien zurückreichen, da schon für den ältesten hier behandelten Fundkomplex von Lokalalei 2C mit einem Alter von 2,34 Millionen Jahren eine absichtliche Selektion von Steinrohmaterialien und eine Vorausplanung bei der Artefaktproduktion nachgewiesen werden können. Die vergleichende Analyse der vier Fundkomplexe offenbart diachrone Unterschiede in der Ressourcennutzung vom späten Pliozän (Lokalalei 2C) über das Altpleistozän (Kokiselei 5 und 4) bis an den Beginn des Mittelpleistozäns (Nadung a 4). Diese Unterschiede hängen eher mit einer Verbesserung der technischen Fertigkeiten im Verlaufe des Plio- Pleistozäns als mit Unterschieden in der Rohmaterialzugänglichkeit zusammen. Schlagwörter: Frühe Homininen, West Turkana, Kenia, Plio-Pleistozän, Rohmaterialversorgung und -behandlung, Vorauswahl, Technikänderungen
2 12 Sonia Harmand Introduction Issues related to raw material procurement patterns in the African Lower Paleolithic have been treated by several authors over the past four decades particularly at Olduvai Gorge, in Tanzania, and in the region of Koobi Fora, east of Lake Turkana, Kenya (e.g. Leakey 1971, 1975, 1994; Hay 1976; Isaac 1977; Isaac and Harris 1978; Jones 1979; Clark 1980; Toth 1982, 1987). Undertaken at a regional scale, these raw material studies have shown evidence of stone transport involving distances of several kilometers (up to 13 km at Olduvai: Hay, 1976; overview in Féblot-Augustins 1997) and evidence for the management of lithic resources during the Early Pleistocene (Toth 1985; Schick 1987; Isaac et al. 1997). However, the preferential use of a specific raw material from 1.9 Ma onwards is generally interpreted as a result of local abundance rather than choice on the part of the toolmakers (e.g. Merrick and Merrick 1976; Toth 1985; Schick 1987; Isaac et al. 1997). Futhermore, examples of selection patterns remain limited for the Early Stone Age (Plummer et al. 1999; Semaw 2000; Hovers et al. 2002; Stout et al. 2005; Braun et al. 2006; Goldman et al. 2006; Harmand in press a, b). Fig. 1: Map of the Lake Turkana Basin with the location of the sites mentioned in the text, modified after Roche et al
3 Economic behaviors and cognitive capacities of early hominins 13 Here, the comparative study addresses the lithic procurement and exploitation patterns brought into play by hominins in four sites from the Early Oldowan, Oldowan, Early Acheulean, and Acheulean located in the recently investigated Nachukui Formation, in the West Turkana region, Kenya (Fig. 1). Owing to their chronological position, these sites offer the opportunity to provide, at a regional scale, new data on the nature of the economic organisation from 2.34 Ma onwards, and its evolution throughout the Plio-Pleistocene time-period, up to 0.70 Ma. The diachronic comparison between the four lithic assemblages and samples of cobbles available near the sites displays evidence of raw material selectivity and technological planning on the part of the toolmakers as early as 2.34 Ma, and contradicts the assumption generally made for the Early Stone Age of an opportunistic gathering of rocks. It demonstrates diachronic changes in the exploitation of rocks between the Late Pliocene and the very beginning of the Middle Pleistocene, which do not correspond to variations in raw material availability. Rather, these changes are related to an improvement in hominins technical skills throughout the Plio-Pleistocene. The Nachukui Formation The Nachukui Formation is a Plio-Pleistocene sedimentary Formation located in the northern part of Kenya, between the western shores of the lake Turkana and two volcanic escarpments, the Labur and Murua Rith. It is one of the longer and more complete geological sequences in East Africa, and it offers a set of Oldowan and Acheulean sites, aged between 2.34 and 0.70 Ma (Brown and Feibel 1988; Harris et al. 1988; Feibel et al. 1989; 1991). These sites are attributed to three Early Stone Age chronological groups and related to four cultural periods (Roche et al. 1999). So far one of the oldest sites known in Kenya, the Late Pliocene site of Lokalalei 2C (Early Oldowan), is located in the south of the Nachukui Formation (Fig. 1), and is dated at 2.34 Ma (Roche et al. 1999; Delagnes and Roche 2005; Tiercelin et al. in prep.). The Early Pleistocene site of Kokiselei 5 (Oldowan) is located in the middle of the sequence, more in the north of the Formation (Fig. 1) and dates to ca Ma (Harris et al. 1988). The Early Pleistocene site of Kokiselei 4 (Early Acheulean, Fig. 1) is one of the oldest Early Acheulean sites in Africa, ca Ma. The Acheulean site of Nadung a 4 is located in the northern part of the Nachukui Formation (Fig. 1) and correlates to the end of the Early Pleistocene or to the very beginning of the Middle Pleistocene, ca Ma (Delagnes et al. 2006). In this study, the pattern of raw material procurement and management for each of these sites was examined using the techno-economic approach to lithic analysis to reconstruct long-term trends of raw material provisioning during the Plio-Pleistocene period. The implemented methodology combined the systematic sourcing of raw materials, based on the reconstruction of the geological and geomorphological contexts of the region, and the study of the distribution and characteristics of the different types of raw materials by petrographical analysis and stone knapping tests.
4 14 Sonia Harmand Raw material characteristics in the Nachukui Formation The most common raw materials in the Nachukui Formation are fine to coarsergrained volcanic rocks, from aphyric to porphyric textures, formed in the Labur and Murua Rith volcanic escarpments. They can be found in river deposits and debris-flow outcrops in secondary position on the alluvial deposits on the west bank of Lake Turkana, at an average distance of between ten to a hundred meters from the archaeological sites (Harmand in press a). Throughout the Plio-Pleistocene in the Nachukui Formation, raw material procurement consisted of collecting and carrying volcanic rocks from these local debris-flow outcrops or dry riverbeds available in the immediate vicinity of the sites. Four major volcanic rock types were identified in the study area based on classical petrologic classification (MacKenzie and Adams 1996): phonolite, basalt, trachyte, rhyolite, and a few siliceous rocks and syenites (Fig. 2). Each of these rock types can be divided according to groundmass features (micro- to cryptocrystalline), grain-sizes (fineto coarse-grained fabrics), and textures (aphyric to porphyritic), resulting in distinct knapping and functional properties and varying initial morphologies and sizes. percentage % medium-grained phonolite = 52% Lokalalei 2C source site percentage % medium-grained phonolite = 68% Kokiselei 5 source site medium-grained phonolite = 24% medium-grained phonolite = 14% phonolites basalts trachytes rhyolites indeterm. 0 phonolites basalts trachytes rhyolites syenites silic. rocks percentage % medium-grained phonolite = 68% medium-grained phonolite = 25% Kokiselei 4 source site percentage % medium-grained phonolite = 8% medium-grained phonolite = 21% Nadung'a 4 source site phonolites basalts trachytes silic. rocks 0 phonolites basalts trachytes rhyolites other indeterm. Fig. 2: Raw material composition at geological sources and at archaeological sites in the Nachukui Formation. Lokalalei 2C: Early Oldowan (ca Ma); Kokiselei 5: Oldowan (ca Ma); Kokiselei 4: Early Acheulean (ca Ma); Nadung a 4: Acheulean (ca Ma).
5 Economic behaviors and cognitive capacities of early hominins 15 Among phonolites, the homogeneous and medium-grained type is a high-grade rock most suitable in terms of flaking quality. This raw material displays a parallel mineral orientation that gives the rock a natural foliation and has the mechanical advantage of breaking easily along the foliation plane when direct hard hammer percussion is used. It therefore offers a measure of predictability in terms of fracture orientation (Harmand 2004, 2005). The medium-grained phonolite is also very suitable for obtaining potentially functional active edges (sharp cutting edges). The presence of numerous phenocrystals within the dark black porphyric basalts (phenocrystals of olivine and pyroxene) and the dark gray porphyric phonolites significantly lessens the predictability of flake sizes and morphologies. Poorer quality cobbles of light brown medium-grained trachytes and dark black fine-grained aphyric basalts are usually hard and difficult to break and also display low fracture predictability. The resistance and the roundness of these rocks appear to be appropriate for percussion. Fine-grained red and green rhyolites are very suitable rocks for obtaining hard-wearing and potentially functional active edges despite the fact that these rocks frequently occur as small diaclasic and angular blocks, less compact and less homogeneous than phonolites and basalts owing to frequent internal fissures. Behavioral continuity in raw material procurement patterns in the Nachukui Formation during Plio-Pleistocene With regard to petrography from the Early Oldowan (ca Ma) to the Acheulean (ca Ma), hominins selected good quality rocks (medium grained phonolites, rhyolites) over coarse-grained or porphyric basalts and trachytes for knapping (Harmand in press a). Rock type frequency distributions show differences between the lithic assemblages and samples of cobbles from the area of the sites (Fig. 2). The frequencies underline the preferential selection of cobbles of a medium grained phonolite until the Early Acheulean (the frequency of medium-grained phonolite is higher in the assemblages than in the local conglomerates, Fig. 2), and of angular blocks of red and green rhyolite at the Acheulean site of Nadung a 4, a rock quite uncommon in the conglomerates sampled in the vicinity of the site (Fig. 2). At Nadung a 4, the medium-grained phonolite was also used although it is very rare at the sources (Fig. 2). From the Early Oldowan to the Acheulean, the selectivity towards raw material quality can also be inferred from the avoidance of poorer quality rocks including trachytes and basalts, which are higher in the local conglomerates than in the assemblages (Fig. 2). Diachronic changes in raw material procurement patterns during Plio-Pleistocene While the same good quality raw material was predominantly used during the Early Oldowan, the Oldowan, and the Early Acheulean, substantial diachronic changes in patterns of raw material procurement and management can be seen during Plio-Pleistocene in the Nachukui Formation, related to the selection for raw material sizes and morphologies, as well as to the way raw material was processed.
6 16 Sonia Harmand Fig. 3: Lokalalei 2C, Early Oldowan (ca Ma). Three refitted complexes showing organized reduction of deliberately selected cobbles. Modified after Harmand The study of the relationship between raw materials at sites and raw materials at sources highlights a high degree of planning and foresight as early as 2.34 Ma. This is testified to by the careful selection of good quality rocks with naturally serviceable striking platforms, for the purpose of carrying out long reduction processes according to the level of skill the Lokalalei 2C (Fig. 3 and 4) knappers have mastered (see Delagnes and Roche 2005; Harmand in press b). To a lesser extent, debitage was struck from poorer quality cobbles or fragments of cobbles of aphyritic or porphyritic basalts (Fig. 2). A series of heavy and medium-sized rounded cobbles of a resistant medium-grained trachyte were selected for use as hammerstones and few unmodified cobbles of mediumgrained trachyte or fine-grained basalt were also brought to the site and probably stockpiled as manuports.
7 Economic behaviors and cognitive capacities of early hominins 17 Fig. 4: Lokalalei 2C, Early Oldowan (ca Ma). Three refitted complexes showing organized reduction of cobbles. Modified after Harmand 2005.
8 18 Sonia Harmand Fig. 5: Kokiselei 5, Oldowan (ca Ma). Phonolite core showing alternating production of blanks. Ctx = cortex, n = negative; the numbers indicate the sequence of reduction, arrows indicate the striking direction. Modified after Harmand While evidence of selectivity at Lokalalei 2C was largely determined by the knappers technological limitations, the procurement and exploitation strategies at Early Pleistocene underscore a higher degree of selectivity. At the site of Kokiselei 5, ca Ma, and later on, at the site of Kokiselei 4, ca Ma, the medium-grained phonolite accounts for a higher proportion of the on-site raw materials than at Lokalalei 2C (Fig. 2). Moreover, selection at the sources within the phonolite group was more important at Kokiselei 5 and Kokiselei 4, since the medium-grained type of phonolite is rare in both cases (Fig. 2). Furthermore, at the Oldowan site of Kokiselei 5 (Fig. 5), the debitage systems appear less constrained by the initial morphology of the raw materials available at the sources, and the knappers display for the first time the ability to modify the initial morphology of the raw material by creating new striking platforms (Texier et al. 2004, 2006). Finally, the study of the relationship between raw materials and artifacts at Kokiselei 5 highlights evidence for distinct provisioning patterns in relation with distinct morphological and functional goals. Two types of production, flakes and heavy-duty tools (sensu M. Leakey 1971), are identified, each of them involving the selection of specific sizes of clasts at the nearby raw material sources. Small to medium-sized cobbles of the medium-grained phonolite were preferably exploited for debitage reduction sequences to obtain flakes, while larger blocks of medium-grained phonolite were selected for the manufacture of heavy-duty tools (Harmand in press a). To a lesser extent, debitage was also conducted on lower quality cobbles of basalts, trachytes and syenites (Fig. 2).
9 Economic behaviors and cognitive capacities of early hominins 19 Fig. 6: Kokiselei 4, Early Acheulean (ca Ma). Proto-handaxes made of phonolite. Modified after Harmand 2005.
10 20 Sonia Harmand At the Early Acheulean site of Kokiselei 4, new volumes are exploited to create specific tools, large handaxes, proto-handaxes (Fig. 6) and picks, through a shaping reduction system (Texier et al. 2006; Fig. 2). This reduction system involves a measure of anticipation in the selection of large flat and elongated slabs of a medium-grained phonolite poorly represented in the nearby conglomerates (Fig. 2) but suitable for maximizing tool sizes and producing large handaxes and picks with long sharp cutting edges. The patterns of raw material procurement and management become more sophisticated at the Acheulean site of Nadung a 4, ca Ma. A wider range of raw materials has been exploited, without an increase in procurement possibilities. Along with the medium-grained phonolites, rhyolites were also preferentially exploited (Fig. 2), although they were rarely exploited in the preceding time-periods (Late Pliocene and Early Pleistocene). Furthermore, the selection of different types of rocks appears very closely linked to specific types of products, for the purpose of carrying out various processing tasks, probably partly connected with the presence of an elephant carcass in the site (Delagnes et al. 2006; Harmand in press a). Red or green rhyolite was exclusively used to produce sharp flakes and obtain cutting edges (Fig. 7). The medium-grained phonolite was used for flake production according to the same principles of debitage documented for rhyolite, as well as for manufacturing some heavy-duty tools by simple shaping (Fig. 2). The remaining rocks at the site are large and compact cobbles of fine-grained phonolite, basalt or trachyte used as heavy-duty tools. Fig. 7: Nadung a 4, Acheulean (ca Ma). Notched and denticulate tools made of red and green rhyolite. Modified after Harmand 2005.
11 Economic behaviors and cognitive capacities of early hominins 21 Conclusion The archaeological record in the Nachukui Formation reveals evidence of raw material selectivity and technological planning on the part of the toolmakers as early as 2.34 Ma. It contradicts the assumption generally made for the Oldowan of an opportunistic gathering of rocks and the notion of artifacts being made in an immediate and rudimentary way. These patterns lend strong support to recent investigations on plio-pleistocene lithic productions which reveal a much more complex panorama of the first technical systems and their related behaviors (Plummer et al. 1999; Roche 2000; de la Torre et al. 2003; de la Torre 2004; Plummer 2004; Stout et al. 2005; Delagnes and Roche 2005; Goldman et al. 2006). The present study also demonstrates that the observed behavioral changes in raw material procurement and exploitation patterns from Early Oldowan to Acheulean are related to the qualities and morphologies of the raw materials selected as well as to the way they were processed, rather than to variations in raw material availability. These temporal changes could reflect a gradual improvement in technical skills throughout the Plio-Pleistocene, and could possibly be related to distinct hominin species or genera (Paranthropus, Homo aff. habilis, Homo erectus). Acknowledgements I am grateful to ratiopharm, Ulm, and the Tübingen Prize Jury for awarding me the 2007 Tübingen Prize for Early Prehistory and Quaternary Ecology. I would like to express a special thank to Nicolas Conard for making my stay in Tübingen so pleasant. Many thanks in particular to Miriam Haidle, Michael Bolus, Harald Floss, Maria Malina, and Luc Moreau for welcoming me at the Institute of Prehistory of the University of Tübingen and for the interesting discussions we shared together. Special thanks also to Nicolas Teyssandier. Data presented here were collected during the completion of my dissertation at the Université de Paris X-Nanterre. I would like to thank the Office of the President of Kenya and the National Museums of Kenya for the excavation and research permits and I am grateful to the West Turkana Archaeological Project co-directed by Hélène Roche (Mission Préhistorique au Kenya) and Mzalendo Kibunjia (National Museums of Kenya) and funded by the French Ministry of Foreign Affairs (sous-direction de la Recherche) and the CNRS/INSU (ECLIPSE Program). This research was partly supported by the French Ministry of Foreign Affairs, EGIDE (bourse Lavoisier). References Braun, D., Plummer, T., Bishop, L., Ditchfield, P., and Ferraro, J. 2006: Kanjera South: Pliocene technological diversity. Paper presented in the Interdisciplinary approaches to the Oldowan Symposium, organized by D. Braun and E. Hovers, at the 71 st Annual Meeting of the Society for American Archaeology, Puerto Rico (USA), April Brown, F. H. and Feibel, C. S. 1988: Robust hominids and Plio-Pleistocene paleogeography of the Turkana Basin, Kenya and Ethiopia. In: Grine, F. E. (ed.), Evolutionary History of the Robust Australopithecines. New York: Aldine de Gruyter,
12 22 Sonia Harmand Clark, J. D. 1980: Raw material and African lithic technology. Man and Environment 4, de la Torre, I., Mora, R., Dominguez-Rodrigo, M., Luque, L., and Alcala, L. 2003: The Oldowan industry of Peninj and its bearing on the reconstruction of the technological skills of Lower Pleistocene hominids. Journal of Human Evolution 44, de la Torre, I. 2004: Omo Revisited. Evaluating the technological skills of Pliocene Hominids. Current Anthropology 45, Delagnes, A. and Roche, H. 2005: Late Pliocene hominid knapping skills: the case of Lokalalei 2C, West Turkana, Kenya. Journal of Human Evolution 48, Delagnes, A., Brugal, J.-Ph., Harmand, S., Lenoble, A., Prat, S., Tiercelin, J.-J., and Roche, H. 2006: Interpreting pachyderm single carcass sites in the African Middle Pleistocene record: a multidisciplinary approach in the site of Nadung a 4 (Kenya). Journal of Anthropological Archaeology 25, Féblot-Augustins, J. 1997: La circulation des matières premières au Paléolithique. Synthèse des données. Perspectives comportementales. ERAUL 75, Liège: Université de Liège. Feibel, C. S., Brown, F. H., and McDougall, I. 1989: Stratigraphic context of fossil hominids from the Omo group deposits: northern Turkana Basin, Kenya and Ethiopia. American Journal of Physical Anthropology 78, Feibel, C. S., Harris, J. M., and Brown, F. H. 1991: Paleoenvironmental context for the Late Neogene of the Turkana Basin. In: Harris J. M. (ed.), Koobi Fora Research Project, vol. 3, The fossil ungulates: geology, fossil artiodactyls, and palaeoenvironments. Oxford: Clarendon Press, Goldman, T., Feibel, C., Hovers, E. 2006: Lithic raw material selection at the Late Pliocene site AL 894 (Hadar, Ethiopia). Paper presented in the Interdisciplinary approaches to the Oldowan Symposium, organized by D. Braun, and E. Hovers, at the 71 st Annual Meeting of the Society for American Archaeology, Puerto Rico (USA), April Harmand, S. 2004: Raw materials and economic behaviour of Late Pliocene Hominids: the case of Lokalalei 2C and Lokalalei 1 sites, West Turkana (Kenya). Poster presented at the Paleoanthropology Society Annual Meeting, Montreal (Canada), March 30-31st. Harmand, S. 2005: Matières premières lithiques et comportements techno-économiques des homininés pliopléistocènes du Turkana occidental, Kenya. Thèse, Université Paris X-Nanterre. Harmand S. in press a: Raw material and economic behaviours at Oldowan and Acheulean in the West Turkana region, Kenya. In: Adams, B. and Blades, B. (eds), Lithic Materials and Paleolithic Societies. Blackwell Publishing. Harmand S. in press b: Variability in raw material selectivity and techno-economic behaviors in the Early Oldowan: evidence from the Late Pliocene sites of Lokalalei, West Turkana, Kenya. In: Delson, E. and MacPhee, R. (eds.), Vertebrate Paleobiology and Paleoanthropology Book Series. New York: American Museum of Natural History. Harris, J. M., Brown, F. H., and Leakey, M. G. 1988: Stratigraphy and paleontology of pliocene and pleistocene localities west of Lake Turkana, Kenya. Nat. Hist. Mus. Los Angeles, Contrib. Sci. 399, Hay, R. L. 1976: Geology of the Olduvai Gorge: a study of sedimentation in a semi-arid basin. Berkeley: University of California Press. Hovers, E., Schollmeyer, K., Goldman, T., Eck, G., Reed, K. E., Johanson, D. C. and Kimbel, W. H. 2002: Late Pliocene archaeological sites in Hadar, Ethiopia. Journal of Human Evolution 42, Isaac, G. L. 1977: Olorgesailie: archaeological studies of a Middle Pleistocene lake basin in Kenya. Chicago: University of Chicago Press. Isaac, G. L., and Harris, J. W. K. 1978: Archaeology. In: Leakey, M. G. and Leakey, R. E. (ed.), Koobi Fora Research Project. The fossil hominids and an introduction to their context, Oxford: Clarendon Press, Isaac, G. L., Harris, J. W. K., and Kroll, E. 1997: The stone artifact assemblages: a comparative study. In: Isaac, G. L. (ed.), Koobi Fora Research Project, vol. 5: Plio-Pleistocene archaeology. Oxford: Clarendon Press, Jones, P. 1979: Effects of raw material on biface manufacture. Science 204, Leakey, M. D. 1971: Olduvai Gorge: Excavations in Beds I and II, , vol. III. Cambridge: Cambridge University Press. Leakey, M. D. 1975: Cultural patterns in the Olduvai sequence. In: Butzer, K. W. and Isaac, G. L. (ed.), After the Australopithecines. Mouton, Leakey, M. D. 1994: Olduvai Gorge: Excavations in Beds III, IV and the Masek Beds, , vol. V. Cambridge: Cambridge University Press.
13 Economic behaviors and cognitive capacities of early hominins 23 MacKenzie, W. S. and Adams, A. E. 1996: Atlas d initiation à la petrographie. Paris: Masson. Merrick, H. V. and Merrick, J. P. S. 1976: Recent archaeological occurrences of earlier Pleistocene age from the Shungura Formation. In: Coppens, Y., Howell, F. C., Isaac, G. L., and Leakey, R. E. (ed.), Earliest man and environments in the Lake Rudolf Basin. Chicago: Chicago University Press, Plummer, T. 2004: Flaked stones and old bones: biological and cultural evolution at the dawn of technology. Yearbook of Physical Anthropology 47, Plummer, T., Bishop, L. C., Ditchfield, P., and Hicks, J. 1999: Research on Late Pliocene Oldowan sites at Kanjera South, Kenya. Journal of Human Evolution 36, Roche, H. 2000: Variability of Pliocene lithic productions in East Africa. Acta Archaeologica Sinica sup. Vol. 19, Roche, H., Delagnes, A., Brugal, J.-Ph., Feibel, C. S., Kibunjia, M., Mourre, V., and Texier, P.-J. 1999: Early hominid stone tool production and knapping skill 2.34 Myr ago in West Turkana. Nature 399, Roche, H., Brugal, J.-Ph., Delagnes, A., Feibel, C., Harmand, S., Kibunjia, M., Prat, S., and Texier, P.-J. 2003: Les sites archéologiques plio-pléistocènes de la formation de Nachukui, Ouest-Turkana, Kenya: bilan synthétique Comptes Rendus Palevol 2, Schick, K. 1987: Modelling the Formation of Early Sone Age artifact concentrations. Journal of Human Evolution 16, Semaw, S. 2000: The world s oldest stone artifacts from Gona, Ethiopia: their implications for understanding stone technology and patterns of human evolution between million years ago. Journal of Archaeological Science 27, Stout, D., Quade, J., Semaw, S., Rogers, M., and Levin, N. 2005: Raw material selectivity of the earliest stone toolmakers at Gona, Afar, Ethiopia. Journal of Human Evolution 48, Tiercelin, J.-J., Schuster, M., Roche, H., Thuo, P., Brugal, J.-Ph, Trentesaux, A., Barrat, J.-A., Bohn, M., Prat, S., Harmand, S., Davtian, G., and Texier, P.-J. in prep.: Stratigraphy and paleoenvironments of the Myr Lokalalei archaeological sites, Nachukui Formation,West Turkana, Northern Kenya Rift. Texier, P.-J., Roche, H., and Harmand, S. 2006: Kokiselei 5, formation de Nachukui, Ouest Turkana, Kenya: un témoignage de la variabilité ou de l évolution des comportements techniques au Pléistocène ancien? Actes du XIV ème Congrès de l Union Internationale des Sciences Préhistoriques et Protohistoriques, Liège, 2-8 Septembre Toth, N. 1982: The stone technologies of early hominids at Koobi Fora, Kenya: an experimental approach. Ph.D. dissertation, University of California, Berkeley. Toth, N. 1985: The oldowan reassessed: a close look at early stone artifacts. Journal of Archaeological Science 12, Toth, N. 1987: Behavioral inferences from early stone artifact assemblages: an experimental model. Journal of Human Evolution 16,
Journal of Human Evolution 48 (2005) 365e380 Raw material selectivity of the earliest stone toolmakers at Gona, Afar, Ethiopia Dietrich Stout a, *, Jay Quade b, Sileshi Semaw a, Michael J. Rogers c, Naomi
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A reprint from American Scientist the magazine of Sigma Xi, The Scientific Research Society This reprint is provided for personal and noncommercial use. For any other use, please send a request to Permissions,
Rocks: Materials of the Solid Earth Presentation modified from: Instructor Resource Center on CD-ROM, Foundations of Earth Science, 4 th Edition, Lutgens/Tarbuck, Rock Cycle Shows the interrelationships
Las Rocas Nos Cuentan Su Historia worksheet answer key (English). Study the samples provided by your instructor. Complete each step as explained in the instructions. Answer discussion questions in your
Name: Rocks & Minerals 1 KEY CONCEPT #1: What is a mineral? It is a, substance which has a What would be the opposite of this? KEY CONCEPT #2: What causes minerals to have different physical properties?
Geology Minerals: We will begin our study of the land with a study of the basic building blocks of rocks: Minerals. Definition of a Mineral To be defined as a mineral in the geologic sense, a substance
Kari A. Kinnunen FRACTURED SILTSTONES IN SUSIVUORI ESKER CLOSE TO SUSILUOLA CAVE, KARIJOKI, FINLAND Kari A. Kinnunen, Hietalahdenkatu 18 D 98, 00180 Helsinki, Finland Email: email@example.com INTRODUCTION
ROCK PICTIONARY ROCK TYPES IGNEOUS ROCKS Rocks formed when magma (molten material beneath the earth s surface) or lava (molten material on the earth s surface) cools and becomes solid. SEDIMENTARY ROCKS
QUATERNARY DATING METHODS 1: RELATIVE DATING TECHNIQUES Objectives: In this lab we will examine relative dating methods used to date Quaternary glacial deposits. After this lab you should be able to: 1)
Kalambo Falls Site A and Site C of Kalambo Falls is of particular interest to our study of the Middle Stone Age in two respects. The evidence of this site demonstrates the Levalloisian technique of stone
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World Beneath Our Feet Lesson Plan 2: Rock Identification Learning Objective Time required Learning Outcomes Materials (provided) Materials (Teacher supplied) background Suggested Procedure Students will
Study Abroad in Kenya at the Turkana Basin Institute s ENVIRONMENTAL CHANGE & SUSTAINABILITY FIELD SCHOOL Lessons from the Past, Solutions for the Future TURKANA BASIN INSTITUTE F I ELD SCHOOLS A UNIQUE
Chapter 4 Practice Test Multiple Choice Identify the letter of the choice that best completes the statement or answers the question. 1. The process in which water, wind, ice, and heat break down rock is
Lecture Outlines PowerPoint Chapter 3 Earth Science 11e Tarbuck/Lutgens 2006 Pearson Prentice Hall This work is protected by United States copyright laws and is provided solely for the use of instructors
Kenya, Truly the Cradle of Mankind A publication of Kenya Tourist Board Issue No 001 Kenya, Truly the Cradle of Mankind The Lake Turkana National Parks is unique and is amongst the six World Heritage Sites
THE FLAKE Stepchild of Lithic Analysis Tony Baker November 21, 2006 Daddy is this an arrowhead? No, that s just a flake. (circa 1963: conversation between Ele Baker and myself) As the reader can see from
The Story of Human Evolution Part 1: From ape-like ancestors to modern humans Slide 1 The Story of Human Evolution This powerpoint presentation tells the story of who we are and where we came from - how
Liz LaRosa http://www.middleschoolscience.com 2010 Images from Geology.com unless otherwise noted A rock is a naturally occurring solid mixture of one or more minerals, or organic matter Rocks are classified
Liz LaRosa http://www.middleschoolscience.com 2010 Images from Geology.com unless otherwise noted A rock is a naturally occurring solid mixture of one or more minerals, or organic matter Rocks are classified
Minerals & Rocks Minerals 5 Characteristics: Naturally occurring Formed from elements or compounds Inorganic Found as a solid in nature Definite chemical make up and regular atomic structure A. Minerals
Characteristics of Sedimentary Rocks Deposited at the earth s surface by wind, water, glacier ice, or biochemical processes Typically deposited in strata (layers) under cool surface conditions. This is
EXERCISE 5D SEDIMENTARY ROCK IDENTIFICATION 1 PURPOSE: To learn the SYSTEMATIC PROCEDURE for sedimentary rock identification. To learn to recognize the TEXTURE and COMPOSITION of the sedimentary rocks.
FROM SEDIMENT INTO SEDIMENTARY ROCK Objectives Identify three types of sediments. Explain where and how chemical and biogenic sediments form. Explain three processes that lead to the lithification of sediments.
Earth Materials: 1 The three major categories of rocks Fig 3.1 Understanding Earth 2 Intro to rocks & Igneous rocks Three main categories of rocks: Igneous Sedimentary Metamorphic The most common minerals
stone age institute publication series Series Editors Kathy Schick and Nicholas Toth Stone Age Institute Gosport, Indiana and Indiana University, Bloomington, Indiana Number 1. THE OLDOWAN: Case Studies
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Joannea Geol. Paläont. 11: 132-136 (2011) Recent ostracods from the Azores archipelago Ricardo P. MEIRELES, Antonio FRIAS MARTINS & Sérgio ÁVILA The Azores is an archipelago in the Atlantic Ocean between
Sedimentary Rocks Practice Questions and Answers Revised September 2007 1. Clastic sedimentary rocks are composed of and derived from pre-existing material. 2. What is physical weathering? 3. What is chemical
MEETINGS A 3- day workshop was held in China to discuss coastal ocean processes, the biogeochemistry of large river- dominated ocean margins ( RiOMars), and climate change and variability studies; to formulate
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Please read chapters 10 and 5 CHAPTER 5 Sedimentary Rocks 1) Sedimentary rocks A) form by compaction and cementation of loose sediment. B) are widespread on the continents and ocean floor. C) are common
Eötvös Loránd University Department of Geophysics HUNGARY 1117 Budapest Pázmány Péter sétány 1/C Tel: +36-1-3812191 Fax: +36-1-3812192 E-mail: firstname.lastname@example.org PALEOENVIRONMENTS OF THE LAKE BALATON
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Project 1: Sedimentology of the Jackfork Group, DeGray spillway near Caddo Gap, Arkansas Due: September 30, 2003 Over the next month or so, we will use the Pennsylvanian age Jackfork Group (JFG) to get
A Rocky World How are rocks classified? A combination of one or more minerals or organic matter is called rock. Scientists divide rock into three classes: igneous, sedimentary, and metamorphic. Each class
Name: Class: _ Date: _ Rocks and Plate Tectonics Multiple Choice Identify the choice that best completes the statement or answers the question. 1. What is a naturally occurring, solid mass of mineral or
Grant-in-Aid of Research, Artistry and Scholarship Investigating Neanderthal Stone Tool Functions by Residue Analysis using SEM-EDS PI: G. Monnier, Anthropology, University of Minnesota, Twin Cities Abstract
Gert STEINKELLNER, Austria Key words: University Curriculum, Advanced Technical College, Civil Engineer, Assistant Surveyor. ABSTRACT In Austria was a substantial change of surveying education during the
Metamorphic Rocks Rocks that recrystallize without melting (solid state) at high temps and pressures Caused by changes in T, P or pore fluids New environment often = new minerals Growing minerals create
WILLOCHRA BASIN GROUNDWATER STATUS REPORT 2009-10 SUMMARY 2009-10 The Willochra Basin is situated in the southern Flinders Ranges in the Mid-North of South Australia, approximately 50 km east of Port Augusta
Sedimentary Rocks, Processes, and Environments Sediments are loose grains and chemical residues of earth materials, which include things such as rock fragments, mineral grains, part of plants or animals,
RHYOLITE BIFACIAL PREFORM PRODUCTION AT EL PULGUERO: A PREHISTORIC QUARRY AND WORKSHOP SITE IN THE CAPE REGION OF BAJA CALIFORNIA HARUMI FUJITA CENTRO INAH BAJA CALIFORNIA SUR Rhyolite is the most abundant
Metamorphism and Metamorphic Rocks Earth - Chapter 8 Metamorphism Transition of one rock into another by temperatures and/or pressures unlike those in which it formed Metamorphic rocks are produced from:
Presents the Rock Test Study Resource Created by Simone Markus Published by EngLinks 1 Preface This is a free resource provided by EngLinks for students in APSC 151. This presentation is a supplementary
6 LUCY & THE LEAKEYS BIOGRAPHY 770L LUCY & THE LEAKEYS HOMININE FOSSILS AND PALEOARCHAEOLOGISTS Louis Leakey Mary Leakey Lucy c. 3.2 MYA Afar, Ethiopia Born August 7, 1903 Kabete, Kenya Died October 1,
Liz LaRosa http://www.middleschoolscience.com 2010 Images from Geology.com unless otherwise noted A rock is a naturally occurring solid mixture of one or more minerals, or organic matter Rocks are classified
The Hot Rocks of ASU GPH 111 Laboratory Stop: LS (Law School) Feel the gritty, sandy texture on broken surfaces Look at the bedding planes Clastic Sedimentary Rock Sandstone Walking by the Southeast of
Scientific Insights into the Evolution of the Universe and of Life Pontifical Academy of Sciences, Acta 20, 2009 www.pas.va/content/dam/accademia/pdf/acta20/acta20-coppens.pdf THE BUNCH OF PREHUMANS AND
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EARTH SCIENCE 110 INTRODUCTION to GEOLOGY DR. WOLTEMADE NAME: SECTION: MINERALS & ROCKS LABORATORY INTRODUCTION The identification of minerals and rocks is an integral part of understanding our physical
Geology Administered by the Department of Physical Sciences within the College of Arts and Sciences. The Bachelor of Science degree in Geology prepares students for entry-level positions in Earth- Science-related
Name: The purpose of this laboratory experiment is to have students interact in multiple ways with rocks and minerals. They are asked to conduct observations and make inferences about the rocks they are
UNIT 3 EXAM ROCKS AND MINERALS NAME: BLOCK: DATE: 1. Base your answer to the following question on on the photographs and news article below. Old Man s Loss Felt in New Hampshire FRANCONIA, N.H. Crowds
UNIT 7: Metamorphic Rocks Chapter Summary Metamorphism is the transformation of one rock type into another. Metamorphic rocks form from preexisting rocks (either igneous, sedimentary, or other metamorphic
Paleoenvironmental Time Slice Reconstructions, Glaciated North America Arthur S. Dyke Geological Survey of Canada Paleoenvironmental conditions in northern North America for the period from the Last Glacial
WC-1 archaeologist artifact A scientist who studies the life and culture of ancient people. An object, such as a tool, made by humans. WC-1 climate climate zone The weather in an area averaged over a long
Learning Series: Basic Rockhound Knowledge Metamorphic Rocks Transformation at Work Metamorphic rocks are one of the three types of rock classifications, the other two being igneous and sedimentary. Rocks
2016 DRIMOLEN FIELD SCHOOL SOUTH AFRICA 24 th JUNE 15 th JULY The Drimolen Field School provides students with a unique opportunity to work at a UNESCO World Heritage fossil site in the Cradle of Humankind,
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Types of Metamorphic Rocks Metamorphic rocks can be subdivided into two main groups - and Groups are distinguished on the basis of:, and Foliation (Latin root folium meaning ), refers to the in a metamorphic
Exercise 1 Rock Review The purpose of this lab exercise is to help refresh your memory of igneous, metamorphic and sedimentary rock types. Rocks are the physical record of past events in Earth s history.
Chapter 3 Rocks Section 1 The Rock Cycle Key Concepts What is a rock? What are the three major types of rocks? How do igneous, sedimentary, and metamorphic rocks differ? What is the rock cycle? What powers