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Blombos Cave

Blombos Cave is an archaeological site located in Blombos Private Nature Reserve, about 300 km east of Cape Town on the Southern Cape coastline, South Africa. The cave contains Middle Stone Age (MSA) deposits currently dated at between c. 100,000 and 70,000 years Before Present (BP), and a Late Stone Age sequence dated at between 2000 and 300 years BP. The cave site was first excavated in 1991 and field work has been conducted there on a regular basis since 1997, and is ongoing.

Excavation history and research context
in Blombos Cave Blombos Cave was first excavated in 1991–1992 as a part of Professor Christopher S. Henshilwood's (1995) doctoral thesis. at the University of Cambridge: Holocene archaeology of the coastal Garcia State Forest, southern Cape, South Africa. Blombos Cave was originally one of nine Holocene Later Stone Age sites that Henshilwood excavated and it was first given the acronym GSF8 (Garcia State Forest, site no. 8). In 1997 GSF8 was renamed Blombos Cave and given its current acronym: BBC. at the University of Bergen and the University of the Witwatersrand, South Africa, together with Professor Francesco d'Errico from the University of Bordeaux 1, France. The aim of TRACSYMBOLS project is to examine how key behavioural innovations emerged among Homo sapiens and Homo neanderthalensis in southern Africa and Europe respectively, and to explore whether and how environmental variability influenced this development between 180,000 – 25,000 years ago, primarily by combining archaeological results, original multi-proxy palaeoenvironmental data and climatic simulations for two continents. From 2017 the cave site continues to be excavated by many of the same researchers under the newly funded Centre for Early Sapiens Behaviour (SapienCE) at the University of Bergen, Norway. The centre is formed in cooperation with Witwatersrand University, Royal Holloway University of London, Université de Bordeaux, Eberhard Karls Universität Tübingen and UNI research, Bergen, Norway. The aim is to follow an even broader multi-disciplinary approach, and the 10-year programme include cognitive studies, neuroscience, geoscience, climate modelling and reconstruction, fauna etc. == Site description ==
Site description
The cave is in a south-facing cliff face 34.5 meters above sea level, ca. 100 meters from the present-day shoreline. The cave formation is set in calcretes of the Wankoe Formation, and the geological setting indicates that the cave was formed by wave action sometime during the Plio-Pleistocene. The interior of Blombos Cave consists of a single main chamber, and the entire (accessible) interior cave floor is about 39 m2 behind the drip line. West of the cave's main chamber, the anthropogenic deposit extends inwardly 3–5 meters. In this area, however, the cave ceiling lowers to a point where it falls in level with the surface, preventing access to the deposit beneath. In the area north-east of the main chamber, the deposit expands into a low laying ante-chamber of unknown extent due to the sand filling it. By the end of the 2011 field season about 19.5 m2 of interior cave has been dug during the Blombos Cave excavations. Blombos Cave's outer talus forms a gently sloping platform of about 23 m2 that extends 4–5 meters southwards, before the terrain abruptly drops down towards the shoreline that lies some 34.5 meters below the cave entrance. The talus, which primarily consists of Middle Stone Age deposit, rock fall and unconsolidated sediments, is stabilized by an area of large, exposed blocks (14 m2). At some stage – and in between the prehistoric occupation of the cave site – these blocks have fallen down from the rock face above, effectively preventing site erosion and allowing sediments to stabilize and accumulate in front of the cave's drip line. Calcium carbonate (CaCO3) rich ground water seeps in from the cave roof and percolates through the interior sediments, resulting in an alkaline environment with good preservation conditions. The excavated Middle Stone Age deposit in Blombos Cave consists of aeolian (wind-borne) dune sand, blown in through the cave entrance, and roof spall from the cave ceiling. Intermixed with these sandy matrices are decomposed marine and terrestrial faunal remains (fish, shellfish, egg shell, and animal bones) and organic material. Large combustion features, small basin-shaped hearths and carbonized horizons are recorded throughout the whole MSA sequence. ==Stratigraphy and dating==
Stratigraphy and dating
When the excavation started at Blombos Cave in 1992 the cave entrance was partially sealed by dune sand, and about 20 cm of sterile aeolian deposit covered the interior Later Stone Age deposit. Underneath the aeolian sand surface, seven main phases of occupation have been identified in the 2.5–3 meter deep Blombos Cave stratigraphic sequence, three in the Later Stone Age (L1–L3) and four in the Middle Stone Age (M1, Upper M2, Lower M2 and M3). These phases are further divided into finer lenses and sub-lenses, most of them less than 10 cm thick. The Later Stone Age and Middle Stone Age levels are separated by a 5–50 cm thick, sterile unit named 'Hiatus' or 'DUN'. The Hiatus consists of yellow aeolian sand that blew into the cave at about 68,000–70,000 years BP, and shows little disturbance from the overlying Later Stone Age units. Humans have briefly and sporadically occupied Blombos Cave throughout the Middle Stone Age (101,000–70,000 years BP) and in the latter parts of the Later Stone Age (2,000–300 years BP). The occupational hiatus between ca. 68,000 and 2,000 years BP, combined with the geological evidence, indicates that the cave site was sealed off by aeolian sand during this period. uranium-thorium series (U/Th) The lowest levels of the M3 phase has a preliminary age of greater than 130,000 years ago, while the unexcavated sediments below these levels remain undated (June 2013). Dating the Middle Stone Age sequence (detailed review) The hiatus level (DUN) composed of undisturbed aeolian sand overlying the M1 phase is dated by OSL to 69,000 ± 5,000 and 70,000 ± 5000 years BP, while OSL ages ranging from 74,900 ± 4,300 to 72,500 ± 4,600 years BP have been obtained for the upper part of the M1 phase, i.e. the units associated with the Still Bay techno-tradition. (see next paragraphs). TL ages for the M1 phase are 74,000 ± 5,000 and 78,000 ± 6,000 years BP. raised towards the luminescence-based Middle Stone Age chronology established by Jacobs et al. 2008 on methodological grounds related to errors in the manipulation of the luminescence data and estimation of uncertainties in the dose rates. The Middle Stone Age chronology for Blombos Cave derived from optically stimulated luminescence (OSL) ages is, nonetheless, consistent with the ages obtained through alternative methods (TL, ESR, U/Th), and remains uncontested. ==Archaeological remains and material culture from the Middle Stone Age levels==
Archaeological remains and material culture from the Middle Stone Age levels
Still Bay bifacial points '' at Blombos Cave (M3 phase, MIS 5), Southern Cape, South Africa (c. 105 – 90 Ka) The most extensive and well-documented sample of so-called Still Bay points in southern Africa comes from the Still Bay sequence in the Blombos Cave. Still Bay points have bifacially retouched sides, are elliptic to lanceolate shaped and most often they have two pointed apices. Since the excavation in Blombos Cave began, more than 500 points or point fragments have been recovered, of which 352 have been described in detail. While hard hammer and direct percussion was used in the initial reduction phase (phase 1), followed by soft hammer and marginal percussion (phase 2), pressure flaking was only used during the final retouch phase (3), and a few points were also reworked by hard hammer percussion (phase 4). or both. Some researchers have suggested that the seeming concern for the appearance of the finished point may represent evidence for social and stylistic elaboration during the MSA. similar to the ones observed ethnographically. Högberg and Larsson 2011 hypothesise that blanks and unfinished Still Bay points were purposely left behind in Hollow Rock Shelter, perhaps for use at a later stage or as an act of solidarity with other hunter-gatherer groups. According to the research published in the journal Nature, the find was "a prime indicator of modern cognition" in our species and an ochre crayon was used by early African Homo sapiens inscribed onto the stone. "The abrupt termination of all lines on the fragment edges indicates that the pattern originally extended over a larger surface," said archaeologist and lead author of the study Christopher Henshilwood. Ochre – an iron-rich mineral – is regularly found at Stone Age sites throughout southern Africa, and has also been recovered from the Middle Stone Age levels in Blombos Cave. More than 8,000 pieces of ochre-like material, of which more than 1500 are 10 mm or more in length, have been recovered from the Middle Stone Age levels of Blombos Cave. Many of them show use-wear traces from intentional use and processing. In 2002 the recovery of two finely engraved ochre pieces – both deriving from the Still Bay units (M1 phase) – was reported in Science Magazine. Wonderwerk Cave and Klasies River Cave 1. Arguably, these engraved pieces of ochre represent – together with the engraved ostrich egg shells from Diepkloof – the earliest forms of abstract representation and conventional design tradition hitherto recorded. Geometric or iconographic representations have traditionally been archaeological categories associated with modern human behaviour and cognitive complexity. The evidence from Blombos Cave – and from sites like Klasies River, Diepkloof Rock Shelter, Klein Kliphuis and Wonderwerk cave – implies that abstract representations were made in southern Africa at least 30,000 years earlier than in Europe and that stylistic elaboration and symbolic traditions were common in southern Africa 70,000–100,000 years ago. The incised ochre pieces recovered from Blombos Cave and various other Middle Stone Age sites indicates that there was a spatial and temporal continuity in the production and use of conventional symbols in the region. The soft, iron-rich ochre would have been ground to powder and turned into a reddish paint, perhaps for cave or body painting. Shell beads and bone tools found alongside the ochre stones support the idea that the early humans using this cave were interested in ornamentation. Ochre processing workshop In 2008 an ochre processing workshop consisting of two toolkits was uncovered in the 100,000-year-old levels at Blombos Cave, South Africa. In addition to conventional bone tools, a modified bone fragment marked with eight parallel lines has also been recovered from the Still Bay phase. Most academics now believe that marine shells were used as beads in the Near East, North Africa, and Sub-Saharan Africa at least 30,000 years earlier than their first use in Europe. Besides Blombos Cave, there are a number of African and Middle East sites that all have yielded strong evidence for the early use of personal ornaments: Skul and Qafzeh, Israel, Oued Djebbana, Algeria, Human remains No skeletal remains have been found in Blombos Cave and the amount of other types of recovered human material from the Middle Stone Age units amounts only to seven teeth. The crown diameters of at least some of these teeth are morphometric "modern" in terms of tooth size reduction, implying that the humans occupying Blombos Cave were anatomically modern. This conclusion is supported by similar evidence from a nearby archaeological site, Klasies River Caves, that dates to a similar time period. Faunal remains At Blombos Cave a great variety of terrestrial and marine faunal remains are consistently found throughout the Later Stone Age and Middle Stone age phases. Fish remains are present, but not abundant, in all phases at Blombos Cave. Fish are more abundant in the Later Stone Age but a wider range of species are present in the Middle Stone Age sequence. Chemical analysis of fish bone from the Later Stone Age and Middle Stone Age levels, using the carbon/nitrogen method, confirms the antiquity of the Middle Stone Age specimens. Most of the species present are not known to wash up after cold water upwelling events, hence scavenging of wash-ups was not the primary source of fish. No artefacts that appear to be obvious fishing equipment have been found, but the range and sizes of species present indicate that a number of methods must have been employed. These may have included: baited hooks, spearing and tidal traps. Where the same fish species have survived in both Later Stone Age and Middle Stone Age levels, analysis of relative bone element occurrence show a significant deficit in the Middle Stone Age. In other words, age-related taphonomic processes have resulted in the loss of many fish bones, and it is likely that more fish were originally deposited in the Middle Stone Age levels than have been recovered through archaeological excavations. Fish are seldom reported from other southern African MSA sites, and by implication, it was thought that Middle Stone Age people were incapable of exploiting coastal resources efficiently. The evidence for fishing at Blombos Cave and Klasies River contradicts this theory. The huge variety of faunal and the shellfish remains recovered from all parts of the Blombos Cave Middle Stone Age sequence demonstrate that people during this period practiced a diverse set of subsistence and procurements strategies and were able to effectively hunt, trap and collect coastal, as well as terrestrial, resources. The subsistence behaviour inferred from the faunal assemblages can hardly be distinguished from the remains and behaviour seen in more recent Later Stone Age contexts. Thus, the overall subsistence pattern at Blombos Cave signifies that no clear distinction can be made between Later Stone Age and Middle Stone Age subsistence behaviour at the site. ==Palaeoenvironment==
Palaeoenvironment
Episodes of past environmental change are typically defined by marine oxygen isotope stages (MIS) that are derived from oxygen isotope signals in planktonic foraminifera found in marine cores. The climatic fluctuations documented from MIS 6 through to MIS 3 spans the duration of the southern African MSA. These stages are therefore most pertinent. In the archaeological context, environmental proxies typically come from a broad range of sources such as microfauna, macrofauna, fossil pollen, dune sediments and speleothems. In recent years, there has been a growing interest in improving our understanding of the environments in which MSA peoples lived and interacted with each other. This is because aspects of MSA behaviours related to artefact production, subsistence, pigment use and migration patterns are increasingly being linked to periods of climatic, and by extension environmental change. Establishing a link, if any, between MSA lifeways and the environmental context in which MSA behaviours developed is complex. While some researchers argue for links between extreme climate change and social change there is some debate. The aim of current research efforts focusing on MSA environments is therefore two-fold. Firstly, improving the temporal resolution of proxies by applying suitable dating methods such as radiocarbon, uranium-series, luminescence, etc. Secondly and most importantly, is to refine the available proxy database so that ambiguous and often, conflicting interpretations can be re-assessed as new information emerges. In light of this, two key studies have emerged, Jacobs and Roberts who evaluate and synthesise the dates for the Still Bay and Howiesons Poort periods across southern Africa and Chase who addresses the issues about MIS 4 environments and the role of climate forcing during this period. A current synthesis of environmental proxy evidence associated with MIS 4 indicates that the Still Bay and Howiesons Poort occurred during relatively humid conditions. It is however not clear what environmental conditions during earlier periods of the MSA (i.e. MSA I, II, III & MSA 2) were like. These early MSA periods are broadly correlated with MIS 6 and MIS 5 (b, c, d, e) but have not been investigated in any detail. ==Provincial Heritage Site==
Provincial Heritage Site
Blombos Cave was declared a provincial heritage site by Heritage Western Cape on 29 May 2015 in terms of Section 27 of the National Heritage Resources Act. ==See also==
Further reading and media productions
Publications in peer-reviewed journals and books • Henshilwood, C. & d'Errico, F. (editors). 2011. Homo symbolicus: The dawn of language, imagination and spirituality. Amsterdam, Benjamins. • Henshilwood, C. S. 2008. Holocene prehistory of the southern Cape, South Africa: excavations at Blombos Cave and the Blombosfontein Nature Reserve. BAR S1860, Cambridge: Cambridge Monographs in African Archaeology 75: 1- 171. Publications in peer-reviewed journals and books • Henshilwood, C.S. & Lombard, M. 2013. Becoming human: Archaeology of the sub-Saharan Middle Stone Age. In: Renfrew, C. & Bahn, P.(eds.) The Cambridge World Prehistory, Volume 1. Cambridge: Cambridge University Press. • Henshilwood, C.S. 2013. Origins of symbolic behaviour. In: McGraw-Hill Yearbook of Science & Technology. California, McGraw-Hill. • Dubreuil, B. & Henshilwood, C.S. 2013. Archeology and the language-ready brain. Language & Cognition 5 (2/3). • Henshilwood, C. S. 2012. The Still Bay and Howiesons Poort: 'Palaeolithic' techno-traditions in southern Africa. Journal of World Prehistory 25:205–237. • Henshilwood, C., & Dubreuil, B. 2012. Response to Shea. Current Anthropology53 (1):1–3. • d'Errico, F., Vanhaeren, M., Henshilwood, C., Lawson, G., Maureille, B., Gambier, D., Tillier, A. Soressi, M & van Niekerk, K. 2009. From the origin of language to the diversification of languages: What can archaeology and palaeoanthropology say? In F. d'Errico & J.-M. Hombert (eds.), Becoming Eloquent: Advances in the emergence of language, human cognition, and modern cultures. Amsterdam: John Benjamins Publishing Company: 13–68. • Henshilwood, C.S. 2009. The origins of symbolism, spirituality & shamans: exploring Middle Stone Age material culture in South Africa. In Becoming human: innovation in prehistoric material and spiritual cultures, (eds. C. Renfrew & I. Morley), Cambridge, Cambridge University Press: 29–49. • Henshilwood, C.S. & Dubreuil, B. 2009. Reading the artefacts: Gleaning language skills from the Middle Stone Age in southern Africa. In: (eds. R. Botha & C. Knight), The Cradle of Language, Oxford: Oxford University Press: 41–60 . • Henshilwood, C.S. 2008. Winds of change: palaeoenvironments, material culture and human behaviour in the Late Pleistocene (c. 77 – 48 ka) in the Western Cape Province, South Africa. South African Archaeological Bulletin, Goodwin volume, Current Themes in Middle Stone Age Research 10: 35–51. • Henshilwood, C.S. 2007. Fully symbolic sapiens behaviour: Innovation in the Middle Stone Age at Blombos Cave, South Africa. In: Rethinking the Human Revolution: New Behavioural and Biological Perspectives on the Origins and Dispersal of Modern Humans,. (eds.C. Stringer & P. Mellars), MacDonald Institute Research Monograph series: Cambridge, University of Cambridge Press: 123–132 1. • Henshilwood, C.S. 2006. Modern humans and symbolic behaviour: Evidence from Blombos Cave, South Africa. In Origins (ed. G. Blundell). Cape Town: Double Storey: 78–83 • Henshilwood, C.S. 2004. The Origins of Modern Human Behaviour – Exploring the African evidence. In Combining the Past and the Present: Archaeological perspectives on society. Edited by Terje Oestegaard, Nils Anfinset and Tore Saetersdal. BAR *International Series 1210: 95–106. • Henshilwood, C.S. 1997 Identifying the collector: Evidence for human consumption of the Cape dune mole-rat, Bathyergus suillus, from Blombos Cave, southern Cape, South Africa. Journal of Archaeological Science 24:659–662. • Henshilwood, C. S. 1996. A revised chronology for the arrival of pastoralism in southernmost Africa: new evidence of sheep at ca. 2000 b.p. from Blombos Cave, South Africa. Antiquity 70:945–949. • Henshilwood, C.S., Nilssen, P. & Parkington, J. 1994. Mussel drying and food storage in the Late Holocene, sw Cape, South Africa. Journal of Field Archaeology 21:103–109. • Lombard, M., et al. (2012) South African and Lesotho Stone Age sequence updated. South African Archaeological Bulletin. Popular articles • Henshilwood, C. & van Niekerk, K. 2012. Middle Stone Age Chemists: A 100,000 Year Old Pigment Processing Workshop at Blombos Cave, South Africa. The Digging Stick. • Tollefson, Jeff 2012. Human evolution: Cultural roots. Nature: News Feature. • Voght, Henrik 2012. Her så vi lyset. Aftenposten A-magasinet. Television 2008–2013 (selected sample) • 2013 – CNN Inside Africa: African beads rewrite the human story? • 2012 – NHK Japanese Television Special Human Series. Presenter: Tatsuya Fujiwara narration (narrator): Seiko Nakajo • 2010 – NHK Japanese Broadcasting Corporation: Film for TV made with Henshilwood at Blombos Cave • 2010 – Film made at Cape Point Nature Reserve with Henshilwood on the 'Origins of H. sapiens' for Foster Brother Film Productions, South Africa. • 2009 – TV film made with Henshilwood at Blombos Cave for the Swedish Broadcasting Society Directed by Martin Widman and presented by Lasse Berg • 2008 – Film made at Blombos Cave with Henshilwood in March, 2008 for display in the 'Anne & Bernard Spitzer Hall of Human Origins', American Museum of Natural History, New York. • 2008 – Film made at De Hoop Nature Reserve with Henshilwood directed by Alan Wilcox on Human Evolution in Africa. SABC Production. ==External links==
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