Showing posts with label Prehistoric. Show all posts
Showing posts with label Prehistoric. Show all posts

Archaeological Discoveries and Recent Rock Art in East Kalimantan, Indonesia

by Jean-Michel Chazine
CNRS-CREDO/MAP, Yogyakarta Conference 24-29 September 2005


Since 1992 a large amount of archaeological discoveries has been later gained. Being eventually and mostly involved into the survey of caves and rock shelters of East Kalimantan, a Franco-Indonesian team, has since regularly let merge some parts of the deep past of that archaeological blank area. Altogether more than 100 caves have been visited and checked, within which more than 30 contain totally unexpected and determinant Rock Art paintings.

During the last decade and more precisely, last 3 years, French and Indonesian archaeologists, assisted by cavers, have surveyed two main karstic areas, located, one North of Sangkulirang, the second Northwest of Sangatta.

These two large areas roughly spread over a 40 by 20 kms space each, appeared to be especially well enough geologically structured and rich concerning archaeological remains of all kinds. These large conic karsts, uplifted from tectonic pressure movements after the Myocene, some 60 millions years ago, have developed three geomorphological networks of cavities and galleries.

These superposed strata, located differently in the uplifted outcrops have proved to be dwelled and used differently along the time. At a broad level of description (see Chazine, 2005, for a more precise insight), the lower one has been usually used as common or daily dwelling places since oldest periods, i.e. before 10.000 years ago, at least, before the end of Pleistocene. It contains all the classical occupation remains: food remains (bones and shells), stone tools workshops with their waste piles, charcoals and fireplaces. Ceramics are often present from surface to the upper or latest levels (surface to minus 40 to 60cm), corresponding to post-Austronesian occupation phases. Within many of the adjacent cracks or crevices, funerary ceramics associated with human bones are neighbouring some late "Dayak" or similar cultural communities who have settled around in the vicinity and left their wooden mortuary coffin burials and displayed personal items.

An intermediate net of cavities, located between 50 to 150 m higher in the cliffs, has had various or composite uses. In a few cases, a punctual dwelling has happened, presenting the same occupation clues than the lower level. Nevertheless, the main use of these intermediate caves, cracks or dry rock shelters has been devoted towards succeeding funerary purposes.

There, a very large amount of earthen funerary urns presenting a large set of differenciated decorations had been regularly observed during 2001 to 2003 field sessions. During 2004' field session, while extending a new test pit in Keboboh caves complex, our colleagues Jatmiko and Udin have also unexpectedly unearthed two burials (Jatmiko et al., 2004). Once unveiled from surrounding deposits, they appeared to be in a flexed position, a feature which would correspond to a pre-Austronesian inhumation process.

The third level of cavities, practically located up to 300 m high, has not provided until now, any if almost no occupation remains but paintings. Some of these caves contain a totally specific Rock Art expression, which induces to interpret these places as having had a very specific function. We will see later in this paper, what kind of activities the particular isolation, remoteness and emptiness of these caves and rock shelters would have had in the pasts.

This natural stratigraphy which has been selectively exploited for cultural and precise goals, is one of the specificities observed in East Kalimantan's (inasmuch as Palawan's) karstic outcrops. The regularity of that distribution (29 positive cases upon a total of 32) makes it a noticeable landmark which local communities have themselves emphasied.

Amongst all dwelling and occupations remains largely found in the lowest, and -less frequently- in the median levels, comprising all kinds of lithic and bone remains (to be more precisely presented later in this paper), the earthen wares are bearing a large amount of directly readable data. As it is limited to the "Austronesian techno-culture" phase, starting around 3,500 years ago, it is too early to consider it as a general objective "leading fossil" or "chronological marker". Nevertheless, at least for East-Borneo prehistory, its main characteristics may be used for discriminating styles, periods, inasmuch as local firing processes.

Since our cooperative Franco-Indonesian program has started last 2003, implying excavations conducted in selected caves and rock shelters, findings of different kinds of earthen wares ceramics both on surface and within stratigraphied dwelling places layers, have enabled us to separate common and/or funerary items.

Broadly speaking, the display of motives and shapes of pots which have yet been sorted are very similar to those which had previously been excavated or collected in Sarawak, Sabah and even Palawan island and the North-Western part of South East island Asia. Some of them being directly similar to the basis reference "Sa Huynh-Kalanay style" analysed and proposed long ago by Pr. Solheim II (Solheim II 1964).

They show eventually not much difference with many of those which have been studied long time ago in Sarawak’, Brunei’ or Sabah’ sectors, by numerous and well known archaeologists (Harrisson, Solheim, Bellwood…,etc). In East Kalimantan, styles vary from the oldest periods (around 3,500 BP) to the most recent surviving influences (Iban or so-called communities), not older than 200 to 100 BP. Decorations vary from paddle and anvil technology using different cord, square carved, mat and granulated motives, to all the possible numerous incised decorations. Some cases
present also geometric excised designs or motives. Stamped features (including linear " grain rice-like" impressions) may also be combined within variable incised schemes. The incised motives comprise geometric, curvilinear and/or stenciled/stamped impressions. The use of specific tools, producing sinuous designs obtained from bivalves shells (cardium-like) which has been yet found only once in Sarawak (Solheim II & Tweedie, 1959), has been now also collected within two caves (Gua Tengkorak and Gua Keboboh) along the Marang river. Macro-observations show that the prints differ one from the other, indicating at least two different shells/tools and probably makers.

One amongst other cardium decorated sherds from G. Tangkorak and belonging obviously to the same pot, would be a part of a handle or prehension tag, in the shape of an animal figurine. They show a strong analogy with figurines which have been found in Lubang Angin (Datan, 1993).

Another zoomorphic figurine has just been found during our last fieldsession, a tiny and remote crack-roomy place named Gua Unak. It presents a composite feature: large horizontal ears-like protuberances and side wings or stumps. The remaining part shows that the figurine had a vertical axis of symmetry. The presence of a hole in the lower middle part, associated to the bent edge, would induce to interpret it as a probable lid handle. They should have been thus two or four located in opposite position.

A complementary screening of the small cavity using a 2-4mm mesh, has not provided any complementary part. Considering that the firing of the clay, being very poor and limited to the minimum rending the whole thus very breakable and damageable, it should have normally totally disappeared. Their extreme fragility would explain why these figurines seem to be very seldom yet in SEA (Cameron, 2005).

Within an increasing number of funerary jars checked along our previous and actual surveys, one very specific was discovered in a small adjacent crevice of Gua Kairim. Considering its huge size first, around 1 meter high and 50 cm for the lip diameter, added to the unusual large geometric curvilinear incised motives, it appears to be totally different from all others. Not only in Kaltim’s set, but even in the whole Borneo Island. It displays numerous variations of alternative indented surfaces yet totally unusual in the surveyed area. Its resemblance with Lapita style ceramic was surprising enough to induce to check it with specialised colleagues. Preliminary and first glance identification confirmed a characteristic late Lapita style expression (comm. pers. Noury, in 2004’ report).

Stressing later that possible clue, a double first "lapita-like" sherd, decorated with stamped dentate motives, came to be found in Gua Batu-Aji. Unfortunately located in sub-surface of midden deposits, it could not be dated nor included in any determining process. During the 2005' Liang Jon excavations, another sherd has been found, well embeded in a regular stratigraphy. Laying at minus 40cm within a stabilized occupation layer, that dentate decorated small sherd shows the characteristic stigma of the dentate tool. In that precise case, it is totally similar to some Fijian and New Caledonian samples (Lapita Conf., 2005). It would correspond to the same period as other early earthenware witnesses, and would be thus also synchronic. According to Noury, it would correspond also to the late Lapita
period/influence, around 2800 BP (comm. pers. May 2005). For R. Green (comm. pers. Aug. 2005), it would correspond to a retroverse effect, similar to the Bukit Tangkorak data found in Sabah, by Bellwood (1989), which happened 3200-3100 years ago.

2005 excavations in Liang Jon, based upon previous researches from 2003 and their promising results, have been centred mainly upon two enlarged test pits 1,5m x 1,5m, located on one row, between the two previous surveyed areas. One (A) has been dug until a depth of 3 m, without reaching yet the terminal rock basement, while the second (B) having encountered a burial, has been stopped after a 60 cm depth.
Both of them have provided a very large set of archaeological remains including stone tools and general middens comprising various faunal bone remains and shells of different sources. More interesting, they are also apparent in distinctly separated levels, some almost complete kits related to the preparation and use of red ochre. That late group of artefacts may be related not only to specific or funerary rituals, but possibly to the ornate caves located in the direct vicinity (200 to 500m). Sophisticated physical methods of comparison should thus be employed to compare the different coloured stuffs.

Once excavated, mainly under GH. Ferrie’s supervision, the skeleton, which appeared around 60cm depth, is lying in a straight elongated position, most of its bones being in apparent connexion. The left hand is applied upon the belly. The right one, although apparent on the right side of the ribs, seems, from the position of the elbow and the missing fore-arm, to have been somehow twisted backwards. But the most strange fact, is that there is no head but a stone in place. The upper part of that stone came to sight only after a circular line of stones containing charcoals and confirming the presence of a fire structure at the previous level, had been removed. The clearing of the skeleton, which was in process, let suppose that the head would have been bent backwards and covered by that late stone. Once removed, it became clear that the corpse had been beheaded. During the extension of the scraping of the layer, some parts of skull appeared, some 60 cm away, just at the foot of the cliff wall. The clearing of that conglomerate of skull pieces has shown that they were corresponding to at least two individuals, (and possibly three). Preliminary observation of the cervical vertebra and the occipital hole(s), has not shown any blow or cutting action tracks. It would thus indicate that the splitting of the head from the body has been done after death, once the decomposition of the corpse was already enough advanced.

The similarity of formal situation is particularly striking with the recent discoveries made in Vanuatu, by Spriggs and his team (Spriggs & al. 2005). There, they unearthed some 20 burials typically belonging to the Lapita period. Some of the skeletons had been beheaded –without provoking stroke wears- and moreover, their head having also been replaced by a stone. More interestingly, some bones have been deliberately taken away, and particularly some fore-arms… From the bio-anthropologists having studied the bones assemblages, they estimate that after one year, it becomes possible, without breaking the bones remaining connexion (pers. comm. Valentin, Lapita Conf. 2005). It implies nevertheless that the body having been buried after death, the head alone had to be unearthed, using then forcibly a location marker. The position of the feet assemblage, inasmuch as the arms and hands would indicate that the body had been toughly and completely wrapped in a mat or
at least with ties (ropes, bark or tapa stripes). Hardness and consistence of the ground has been observed during the excavation process, it appeared that the body had been buried in digging a hole not much larger than the corpse in the ground and later refilled, due to the difference of flat regularity in the deposits. The coincidence of the level from which the burial has been dug and the level of the occurrence of the "lapita-like" postsherd has to be noted. Although it would not constitute yet
a real acceptable proof, it is nevertheless a clue, which has to be kept in mind.

While awaiting C14 datation results for the Liang Jon excavations, that particuliarly significant occurence, should be added to the similarity with the large Lapita inspired funerary urn from Liang Kairim. That convergence would at first and primary approach, confirms, if definitively established, that circulation of cultural items related with the Lapita periods or influence phases, has been even larger than estimated previously. Limited until now to the NE part of Borneo, mainly thanks to Sabah's investigations (see Bellwood 1989), that influence would have extended also Southwards to East Kalimantan. The exchange and circulation process including cultural items, would they be physical : like obsidian from Talasea in New Britain (see Specht 1985), transported and found in NE Sabah, or symbolic like designs or myths, would probably include also some specific decorated ceramics. Wether only
lapita-like pots or their technology, has circulated, missing until now enough identified data, remains a yet unsolved question.

As a matter of fact, birth origins of "Lapita cultural complex" inspiration is still a question debated between scholars (see the numerous Lapita and IPPA Symposia held since the past decades). It broadly varies from Eastern to Western sides of New Guinea, and our late discovery is more precisely trending towards the Western origin or clustering area. Other sites from insular SEA have also provided somehow lapita-like ceramics, although not using the very specific dentate stamped technique.
Some of the most well known originate from Kalumpang area (Sulawesi) and Talaud islands, or even in and around Taiwan, have already been described by Bellwood (1997). The appearance of such ceramics in East Kalimantan, corresponding simply to the extension westwards of its possible influence, is just enlarging the probabilities area and does not present any contradiction with already established hypothesis.

The other important findings from 2005’ excavations (Gua Tebok and Liang Jon) are the numerous artefacts related to ochre uses, excavated between the upper levels and the lowest ones (2,5m deep). They comprise the complete set, from the large raw core (15cm in diameter), to the red wearings pestle, including core flakes, used pencils with wearing marks and flat to hollowed red surfaced anvils. Most of these late anvils are from calcitic-sandstone, whose provenance may be located precisely. They would come from the eastern side of the Gunung Marang itself, where sandstone
dots emerge from pure calcite deposits. It appears quite visibly intermixed in the cave named Gua "tanah lihat" (cave "where earth is visible"), at the bottom of the main cliff (see 2003' report). This complete assemblage of ochre implements, shows how its importance was noticeable. Although Gua Tebok and Liang Jon 2005’ excavations have both provided a remarkable set of ochre, Gua Tebok is presenting the advantage to contain some hand stencils (one of them right in the midle of the huge ceiling, 8m high). They may thus be with high probability directly related to them. That important use has had a lasting activity during a long lap of time because it appears in the different succeeding occupation layers. These late are still awaiting
datations sampling.

Although almost all kind of stone tools and their industry, including raw materials inasmuch as refuses, from upper until lower levels (minus 3m), no real significative change could yet be observed in lithic technology. Surface inasmuch as first 50 to 60 cm layers, which contain ceramics corresponding thus to the "Austronesian" techno-cultural phase, do not present other signature than medium to small flakes industry. Only one broken part of the cutting edge of a polished adze has yet been found during the 3 campaigns, indicating that the introduction and adoption of that new techno-cultural practice, carried by Austronesians, did not spread regularly inside all areas of Borneo. At a broad level of consideration, there is no main noticeable change in the stone tools assemblage. They are mostly flakes, whose statistical distributions appear to vary slightly. As already stressed by Julien Espagne (see 2003’ and 2004’ reports), the frequency of Kutai flakes remains
proportionally high, and lasts from buried ancient levels (yet radiocarbon undated) to sub-surface locations. Nevertheless, the main impression is confirmed that the “Pleistocene knapping technology” has lasted until very recent periods although ceramic technology was spread all over Kalimantan. It shows some seemingly contradiction concerning the acceptation or borrowing of foreign technics, by prehistoric hunter-gatherers. They have clearly conserved or adopted only what was corresponding to their needs and culturally agreeable.

A more precise description of lithic technology by J. Espagne, will appear besides, based upon his study yet in progress. The study of animal bones by HG. Ferrie being still at its beginning and in progress, only a first general draft of his preliminary interpretations is provided hereafter.

Primary and general observations concerning bone study
conducted by Jean-George Ferrié

Within the general frame of archaeological researches conducted in East Kalimantan, we have undertaken the study of faunic bones remains which have been discovered within some sites of the Marang river area.

That study has two main goals. First, it will allow to collect data concerning the different animal species, which were present in the surveyed area during different chronological phases, and to follow their evolution. Being accepted that the absence of one species in the archaeological frame would not mean its general lack in the natural environment: human communities being able to manage many choices within their accessible possibilities.

Second, as a main task, we should be able to bring out original data upon daily life of communities who have settled in this area. Thanks to a detailed taphonomic and
archaeological analyse of bone remains, it should be possible to reconstruct exploitation strategies of the natural environment managed by these populations. Once established for each site, synchronic and diachronic comparisons, for inter- and intra-locations will be performed, with the intention to search possible differences and evolutions in the managing of local animal resources.

A set of test-pits has been dug during the 2005' field session, on Gua Tebok, Liang Unak and Liang Jon sites. They have provided an important quantity of bone remains. The total weight overpasses practically 30 kg. Only Liang Jon and Gua Tebok have yet been submitted to a preliminary sorting and study. Most of the bones are highly fragmented, and depending of test-pits and layers, a large proportion of them is burnt. Within identified taxons, suidae, followed by turtles (mostly shell parts), then cervidae, constitute the main core. Some bones of primates and carnivores have also been identified in a lesser proportion in the different assemblages.

In the Test-pit B in Liang Jon, levels 24, 25 and 26 would differ from others, because of the majority proportion of cervidae. The proportion of suidae and turtles within these layers would be thus lower than cervidae, indicating an important change in the diet or food practices. These primary observations should be confirmed later with more precise observations.

The first sorting of bones has already let appear an important proportion of burnt bones. In Liang Jon, 36% of the total determined remains and 68% of undetermined fragments are burnt. These proportions are respectively 36% and 7 3% in Gua Tebok. If animals constitute an important diet resource, they are also providing an important raw material subside (long hard bones and deer antlers, inasmuch as skin and tendons). In Gua Tebok and Liang Jon, uses for non-dietary purposes have been identified thanks to the discovery of different bone points or needles.

A more detailed analyse is clearly necessary in the intention of establishing the taphonomic history of each assemblage and then in precising the acquisition and exploitation process for each species. These data will be tied and cris-crossed with those of other disciplines, the only procedure permitting to precisely describe the past way of life of the communities who have previously settled in this area. Equally important by their number inasmuch as by their contents are the ornate caves which have been discovered since 11 years in that area. Being established by now that the oldest representations are older than the end of Pleistocene (10.000 years BP), they constitute a determining core of the South East Asian prehistory.

Mainly characterized by a high number of negative hand prints, it shows also different manners of using not only combinations but also overpainted hand stencils. That late characteristic let it differs from all surrounding cultural expressions, and even of all worldwide examples. Its origins are not yet clearly established but analyses have proved to be dated from more than late Pleistocene (10.000 BP). Being unique in that part of the world, and presenting more links with its far neighbours from Australia, than with the closest islands (Sulawesi, Moluccas and Western New Guinea, mainly described by Kosasih, Setiawan, O’Connor, Delanghe & Arifin) this would induce to consider differently the settlement and cultural diffusion of Rock
Art in that large area. One new hypothesis would be that before the end of Pleistocene (10.000 years ago) and during its move towards Australia, a group would have settled –or escaped- in that remote area of East Kalimantan and locally kept that painting tradition and its former usages. The fact is that there is no apparent aesthetic, neither figurative link, between the rock art painted in these caves and any ethnographic "Dayak" style figurations.

Although the presumption of a specific "austronesian" origin has been proposed and would for many cases fit there with the local "prehistory of history", mainly in East Nusantara, by some scholars (Balard, 1992), that explanation does not match observations for East Kalimantan. The presence of a few general figures in some caves, presents some analogies, with some common symbolic "ideograms", in frequent use in South East Asia. For instance, the arborescent feature found in Gua Tewet linking a minimum of 7 differenciated negative hand prints, may evoke possibly the "tree of life" scheme. Another hypothesis is prefering the "visual language" approach and its logical interpretations, is supported by P. Setiawan, our everlasting global partner since 1995.

Apart that possible reference with some "Dayak" cultural expression, it would possibly also be perceptible in what seems to represent the large bees hive and the "honey tree" painted in Kerim cave. It is known from ethnography (Van Geddes, 1959, Hopes, 1997) that much respect was paid to any honey tree and a specific dance used to be performed by communities, after or against bad or difficult events or periods. Would these representations ("tree of life/honey tree") and customs (honey tree dance) pre-exist before the arrival of Austronesians, followed themselves later by generic Dayak cultures, is still a possible hypothesis. This late one, is forming the bulk of possible eventually consequences of the contacts between Pleistocene populations, long time settled in South East Asia. Samples from Niah or Tabon, show that peoples -Homo sapiens sapienswere already living there since 40 to 50.000 years, compared to newcomers like Austronesians, some 5.000 years ago only. What kind of exchanges or inter-influences have thus and then happened, and in which directions, is still a puzzling question, breeding discussions between specialists.
The investigations conducted in Gunung Marang cluster have began to nourish the gap of knowledge still remaining in that large area. Completing –or confronting- other data gathered not only in Eastern Kalimantan, but also the complete Eastern side of Island Borneo, archaeological results converging from all disciplines would provide a determining clue for interpreting the role that this precisely “in the between” location, would have played in the past.

Concerns towards its proper study but also its efficient protection should therefore be strongly linked for future generations. Note on the economico-cultural environment of the Gunung Marang Reserve situation (JM. Chazine/Kalimanthrope) The state of protection of that huge and determinant patrimony is eventually almost null. The burial sites and the painted caves, had remained until recent decades under a traditional and implicit protection. Local communities, mainly Dayak and their more slightly episodic Punan contacts were the only ones to settle within that area. Some caves had thus been devoted to keep funerary remains, jars for older times, and wooden coffins for more recent, like in Gua Lungun or Gua Tengkorak. The dramatic 1997’ hazes, have left nothing but charcoals from these wooden items. The whole area had anyway already been abandoned some decades ago, under common pressure of the Government and the logging companies attractive salaries. Only bird nest collectors, ancient residents or newcomers from the Transmigrasi process, were rovering from caves to caves. Pressure was not that much important, based upon a low and temporary mean human presence. Conditions and incomes produced by some caves has strongly increased and time length during which a new population remains on the spots has totally changed also. Being reduced from 45 days of minimal maturation, it has dropped down to 42 if not 40, decreasing dramatically the natural stock for reproduction. Bands of 6 to 10 men stay all the time near the caves to collect and protect the “goldmine” and consequently predate everything still living around. Large areas are now under a huge and almost wild threaten from free scavengers and logging gangs. Protection and information actions have now to be organised and coordinated, in accordance with the local authorities demands and intentions. Discoveries and findings already gained in that specific area are important enough to help settle local showroom and exhibitions actions for enhancing cultural awareness.

At another level, the groups exploiting the natural resources of these remote and desertified areas do not belong to the new created local culture, i.e. the " Kutai". A neologism which has the advantage to integrate as many people as needed, as long as they have been resident since enough time or generations. It permits also to include in a new generic, common and neutral term, Dayaks or assimilated communities and overpass the cultural complex of inferiority which has been and still is prevalent. A rather little number of "real new Kutai" are permanently involved in logging or forestry industries, inasmuch as bird nest collecting. They use to come there to get a harsh but speed, amount of money and behave just like simple or other predators. They do not feel any cultural, historical neither emotional link with those who have left the archaeological remains that archaeologists excavate and exhume from the ground and the caves. They have in no case their ancestors buried there and will never have. Thus cultural links between previous inhabitants and local authorities do not yet exist at all. Understanding and protection measures are totally foreign constraints for these new scavengers, inasmuch as there is no support for the Administration on the spot. That gap is not the smallest problem which has to be managed and solved to attempt to protect and maybe enhance the cultural consciousness of a morally and geographically distancied population.

Bibliography (quoted in the text only):

Balard, 1992: "Painted Rock Art sites in Western Melanesia: locational evidence for an "Austronesian" tradition", in J. McDonald & L.P. Haskovecs (eds.), Occas. AURA
papers 4, p.94-105.

Bellwood, 1988: "Archaeological research in South-Eastern Sabah". Sabah Mus. Monogr. 2.

Bellwood, 1997 (revised ed.): "Prehistory of Indo-Malaysian Archipelago". Univ. of Hawaii Press.

Burley, (ed) : " Lapita Conference in Tonga". Pre-proceedings papers abstract, Aug.
2005.

Cameron, 2005: "Pottery figurines in the archaeological record of South China, South
East Asia and the Pacific". Lapita Conf. Tonga, Aug. 2005.

Chazine, 2000: " Découvertess de peintures rupestres à Bornéo", in " L'Anthropologie", 104, p.459-471.

Chazine, 2002: "Rock Art and ceramics in East Borneo: logical discovery or new cornerstone?", in "Pacific archaeology: Assessments and prospects", Sand (ed.), Noumea, p.43-52.

Chazine, 2005: "Rock Art, burials and habitations: caves in East Kalimantan", in Asian Perspectives, 44:2, p.219-230.

Chazine, 2005: "Ceramics from East Kalimantan and the Lapita connexion". Lapita Conf.
Tonga, Aug. 2005.

Chazine, Fage & Setiawan, 2002: "The Rock Art of Kalimantan in Indonesian Borneo", in
" Ligabue Magazine", Anno XXI, n°41, p.146-166.

Datan, 1993: "Excavations from G. Sireh and L. Angin". Sarawak Mus. Journal Vol XLV
n°66.

Delanghe & Arifin, 2004: Rock Art in West Papua, Paris, UNESCO.

Geddes, 1973: "Nine Dayak nights". Oxford University Press, New York.

Hopes, 1997: "Ilmu, magic and divination amongst the Benuaq and Tunjung Dayak", Puspa Swara & Rio Tinto Foundation, Jakarta.

Jatmiko, Nazruddin & Bambang, 2004: "Explorasi situs gua dan hunian Prasejarah di pegunungan Marang kabupaten Kutai Timur, Kalimantan Timur", Laporan Penilitian Arkeologi, Puslit Arkenas, Jakarta.

Kosasih, E.A, (1991) "Rock Art in Indonesia", in Bahn, P & Rosenfeld, A (eds), Rock Art and Prehistory:papers presented to Symposium G of the AURA Congress, Darwin,
1988, Oxbow Books, Monograph 10.

O'Connor, S (2003) "Nine new painted Rock Art sites from East Timor in the context of
the Western Pacific Region", in AP Vol.34, No 1, 2003.

Setiawan, 2003: " Alih pengetatuhan pada nelayan tradisional Pelabuhan Ratu (Thesis).
Progr Pasca Sarjana Antropologi, FISIP, UI, Depok.

Setiawan, 2004: "kawasan Kars Sangkulirang.:Antropologi dan Arkeologi. Research
Report of "The Nature Conservancy", Samarinda, Kaltim.

Solheim II, 1965: "The prehistoric earthenware of Tanjung Kubor, Santubong", in
Sarawak Museum Journal 12 (25-26), p.1-62.

Spriggs & alii, 2005: " Lapita pots and the people: results of two field seasons at the

Teouma site, central Vanuatu". Lapita Conf. Tonga, Aug. 2005.

Valentin, 2005: "Teouma human remains: first descriptions of metric and non-metric
features". Lapita Conf. Tonga, Aug. 2005.
Read More..

Archaeology of the Flores Man Site: Liang Bua Cave, Indonesia

By K. Kris Hirst

Liang Bua is located in the Wae Racang Valley on the western end of the tiny island of Flores in Indonesia. Liang Bua is the name of the karst limestone cave from which Flores Man (a.k.a. the Hobbit) was found. The stratified site deposits are 12 meters in depth, and within the deposits have been found both modern humans and the hominin remains somewhat controversially called "Homo floresiensis".

Liang Bua Cave Formation

The cave was created by karst action nearly 400,000 years ago, but evidence suggests that it was invisible from the surface until about 190,000 years ago. Homo erectus appears on Flores Island beginning 840,000 years ago. Homo sapiens first appeared in the region circa 55,000-35,000 years ago.

Liang Bua's Hominin Remains

Hominin remains recovered from the site include LB1 (the original Flores Man, dated ca 18,000 years old), and elements from eight other individuals (dated between 12,000 years and 95,000 years ago. Modern human skeletal remains recovered from Liang Bua are all within Holocene levels (i.e., within the past 11-12,000 years or so). None of the bones recovered from Pleistocene deposits in Liang Bua cave appear to be modern H. sapiens.

Artifact Assemblages at Liang Bua

The artifact assemblages from Liang Bua include a fairly sophisticated suite of stone tools attributed to H. floresiensis, particularly within a level dated to ca. 74,000 years ago (+14/-12 ka) that contains stone artifacts with evidence of hard-hammer stone tool production. Raw material for the stone tools was mostly volcanic glass, with some marine limestone. The reconstructed stone tool manufacturing process is similar to sites of the same age found throughout Southeast Asia: a combination of off-site production of large stone blanks and on-site blank reduction. These methods were used by all hominids in southeast Asia around at the time: H. erectus, H. sapiens, and (assuming Flores is a separate species) H. floresiensis.

Sources

Argue, Debbie, Denise Donlon, Colin Groves, and Richard Wright. 2007. Homo floresiensis: Microcephalic, pygmoid, Australopithecus, or Homo? Journal of Human Evolution 51(4):360-374.
Brown, Peter, T. Sutikna, M. J. Morwood, R. P. Soejono, Jatmiko, E. Wayhu Saptomo & Rokus Awe Due. 2004 A new small-bodied hominin from the Late Pleistocene of Flores, Indonesia. Nature 431:1056–1061
Morwood, Michael J. et el. 2004. Archaeology and age of a new hominin from Flores in eastern Indonesia. Nature 431:1087–1091
Morwood, Michael J., et al. 2005. Further evidence for small-bodied hominins from the Late Pleistocene of Flores, Indonesia. Nature 437:1012-1017.
Westaway, K.E., M.J. Morwood, R.G. Roberts, J.-x. Zhao, T. Sutikna, E.W. Saptomo and W.J. Rink. 2007. Establishing the time of initial human occupation of Liang Bua, western Flores, Indonesia. Quaternary Geochronology: in press
Read More..

Fossil Finds of Flores Man, Indonesia

By K. Kris Hirst

The scientific world was rocked by reports of the discovery of the preserved skeleton of a previously unknown hominin species in 2004. Tentatively named Homo floresiensis, or Flores Man, the hominin became known to the world press as the Little Lady of Flores or the Hobbit. Most of a female individual of Flores Man was discovered by a joint international research team led by R.P Soejono from the Indonesia Centre for Archaeology and Michael Morwood from the University of New England Armidale. The research team discovered Flores Man six meters deep within the deposits of the Liang Bua site, a limestone cave on the island of Flores in Indonesia. The hominin was very small in stature, no more than a meter in height and as small as those of the shortest human beings ever known, but the brain capacity of the creature was much smaller than in modern humans. Further, the form of the skull and lower skeleton suggested to Soejono, Morwood and colleagues that the Little Lady was a form of Homo erectus, and not Homo sapiens. Flores Man caused quite a stir, not the least because she appeared to have survived as recently as 18,000 years ago, far later than any other Homo erectus known on the planet.


H. floresiensis skull, Liang Bua Cave, Indonesia. (by Peter Brown)

The resultant furor over the original Flores Man findings brought a competing theory, not yet published, that the skeleton is of a microcephalic (diseased) modern human pygmy. Further problems developed when the skeletal material was damaged during analysis by another researcher.

Morwood and colleagues continued excavations in Liang Bua cave through 2004, and discovered partial remains of eight additional individuals, one a subadult. These new finds were reported in the journal Nature on October 13, 2005. The recovery of so many examples has allowed for a more complete consideration of the form of H. floresiensis as a group, rather than the single individual. All of the specimens (with the exception of the child) appear to have been about 1 meter in height. In general, the skull shape and body form are most similar to Homo erectus, but H. floresiensis has longer arms and a smaller brain capacity than H. erectus normally has, in fact closer to Australopithecus or gorilla than H. erectus. Recent investigations of the Dmanisi H. erectus fossils in Georgia and those at Olduvai in Kenya suggest that there was more diversity in H. erectus than has been previously identified, a fact surely epitomized here.


Comparison of mandibles from Laetoli Australopithecus afarensis LH4 and Homo floresiensis LB6. (by Nature)

Further information was also found about the behavior of the little hominin: butchered pygmy Stegodon (a primitive type of elephant) and Komodo dragon have been found at Liang Bua, as have clusters of fire-cracked rock and charred bone in levels containing H. floresiensis skeletal materials, suggesting the hominin knew how to control fire. Stone tools recovered from the site evidence a sophisticated grasp of lithic knapping.


Homo floresiensis (Liang Bua Cave, Indonesia) and a modern human skull. (by Peter Brown)

The late date of the appearance of H. floresiensis is also confirmed. Using thermo-luminescence dating of the strata in which the skeletons lie, the oldest appear to have been dated to about 94,000 years ago, and the most recent 12,000 years ago. None of these materials are fossilized, and DNA testing and radiocarbon dating of the hominid skeletons themselves does not seem to be possible, given the condition of the material. Morwood hopes that additional skeletal materials may allow these forms of testing.

Whatever species the little hominin is, Homo erectus or something quite different, they are certainly not human. The appearance of a different hominin species dated to 12,000 years ago is quite remarkable, given that the last known Homo erectus found to have been living on planet earth died out about 120,000 years ago; and the most recent Neanderthal form of Homo sapiens was gone by 28,000 years ago.

Sources and Furthern information

Read the latest information about the Flores individual: Is Flores a Deformed Homo sapiens?
Lieberman, Daniel E. 2005 Further fossil finds from Flores. Nature 437(October 13, 2005):957-958.
Morwood, M. J., et al. 2004 Archaeology and age of a new hominin from Flores in eastern Indonesia. Nature 431:1087-1091.
Morwood, Michael J., et al. 2005 Further evidence for small-bodied hominins from the Late Pleistocene of Flores, Indonesia. Nature 437(13 October 2005):1012-1017.
Read More..

Artifacts, Archaeology and Cabeza De Vaca (Part III)

Summary
Museum material culture appropriate to Cabeza de Vaca during his "trader" phase and his journey thence to the Rio Grande would include: arrow points (likely Perdiz, and perhaps Caracara at Falcon Lake), bone-tempered pottery (including restored or partially restored vessels at TARL and, from Choke Canyon, at the Center for Archaeologica Research at The University of Texas at San Antonio, "hide scrapers" (end scrapers) and beveled knives (bison processing equipment), large trade bifaces, manos and metates, mats (as among the Cuchendado, use Lower Pecos examples), bows and arrows, digging sticks, etc. (also derived from Lower Pecos collections but surely identical to what was in the south Texas interior). Photographs of the wooden mortars and pestles reported by Collins (1968) and Prewitt (1981) would be very appropriate, given Cabeza de Vaca's description of mesquite bean processing (the Collins and Hester specimen is from the Lower Pecos, and had prickly pear seeds in the mortar) on the Rio Grande. He clearly describes pestles, and mentions a "jar" which sounds much like the mortars that have been reported. Cabeza de Vaca in Northeastern Mexico.

When Cabeza de Vaca moves west from the Rio Grande, he entered territory that is still very poorly known archaeologically‹especially in Late Prehistoric times. No major excavations or studies have dealt with this terminal portion of the culture sequence in the region, and those that have, usually involved rockshelters (cf Hester et al. 1994)‹not part of Cabeza de Vaca's chronicle. Cabeza de Vaca's reference to rabbit-hunting sticks clearly refer to the "rabbit sticks" present in museum collections at the Witte and at TARL, from the lower Pecos and western Texas; doubtless, they are the same as he recorded in northeastern Mexico. However, there is a much discussed incident involving material culture that I would like to touch upon. This is the "copper" bell or rattle (described as "squat and wide;" M. Wade, personal communication, 1996) given to Dorante "at the base of the mountains" (Covey 1961:110; Ketchum 1988; Epstein 1991). Cabeza de Vaca relates that the gift-givers had obtained the artifact from the "north." This has led many to speculate that it is derived from Casas Grandes, the great trading and craft production center in Chihuahua studied by Di Peso (cf. Di Peso l974, who notes Casas Grandes trade networks reaching to La Junta de los Rios and other northern Mexico locales). It may have indeed come from there, but I suggest an alternate scenario. If the Krieger map is correct (cf Chipman 1987:143), this event probably took place south of Monterrey. This is only 250 miles from the Pavon site, on the Rio Panuco, in the Huastecan culture area. At this site, Ekholm (1944:478-479) reports and illustrates large copper bells (including one strikingly similar to a specimen from Casas Grandes, DiPeso 1974 510), and notes several others, including one in the form of a turtle (the one given Dorante apparently had a "face" or image on it) in the Huasteca. Indeed, Huastecan outposts in the Sierra de Tamaulipas, occupied at the time of Cabeza de Vaca (the Mesoamerican Late Postclassic) were within 100 miles! The Huastecans were very active traders, as seen in their interaction with the hunters and gatherers of the Brownsville complex in the Rio Grande delta, where obsidian, pottery, and jade is documented (see Hester 1995 for a detailed review). Further, despite all the ruminations in the various translations, could the "South Sea" and its riches not be the Pacific or the Bay of California . . . but the Gulf of Mexico with its Huastecan towns and traders?

Finally, I want to close with some observations on the material culture related to the famed "mouse-teeth" scarification event (Covey 1961: 113). It is hard to say where this took place, though Krieger's route suggests it could have been in the Big Bend area. Of particular relevance here is a basket and contents found at site 41VV171 in the 1930s and in the collections at TARL (see Figure 2). This has never been fully published, though it is sometimes called a "shaman's kit" or a "medicine kit." Among the contents are mescal beans (known hallucinogens) and a number of rodent (rabbit) mandibles. It is not hard to imagine these latter items being used for this type of scarification, especially in the scene described in the Cabeza de Vaca case. Though Cabeza de Vaca describes the event as one of parents' punishing a crying infant, one suspects that it is related to curing rituals. If so, such scarification appears not to have been the domain solely of a "shaman," (cf Ricklis 1994:416) but could be done by anyone. I do not want to stretch this too much, but simply point to this kit (or a photograph of it, again due to Native American concerns) as a possible exhibit item, given the mention of the scarification event and, of course, Cabeza de Vaca's role as a healer during much of his time in Texas and Mexico. (This text initially appeared in Windows to the Unknown: Cabeza de Vaca's Journey to the Southwest. An interdisciplinary symposium hosted by the Center for the Study of the Southwest at Southwest Texas State University, San Marcos.
Read More..

New Dinosaur of Canada

A candidate geologist stumbled a group of bone in north of British Columbia more than three decades then. He is insane that the bones possibly came from a new species. What is interesting, the identity of the dinosaur still mysterious now.

Gathering of bone collected covers seven jaws, arm, and feet bone, and fragment of skull. Based on form and bone measure, the paleontologist anticipates it is a dinosaur in small to medium size, possibly a pachycephalosaurus or ornithopoda. But this specimen only called as dinosaur Sustut because found in Sustut Basin in Middle-North of British Columbia, Canada.

Kenny Larsen found the fossil by 1971 when looking for thorium, of a kind element of radioactivity. When working in field, his instrument caught a level of certain radiation, which actually came from bone. Larsen then collected the separated bones, and donated to Dalhousie University in Halifax, Nova Scotia, at 2004.

The bones then studied by Victoria Arbour which soon realized that the goods were rareness finding. The bones is conserved carefully and is most dinosaur specimen complete which was found in the existing finite British Columbia.

Unfortunately, the Larsen’s note of field is lost, so that the researchers had difficulties to find the precise location of the fossil grave, and made the fossils were difficult to be known by the age. But based on stone patching at some fragment, Arbour and her partners anticipating the specimen’s age is around 70 million last year, precisely from the end of Cretaceous era.

Fragment of Bone identified that the fossils came from small dinosaur of biped herbivore. Some the bones were alike with pachycephalosaurus, which was running with two feet, and has dome-shaped skull. While some parts again looked like ornithopoda, eater of grass run with two feet and had horns snout.

There are some resemblances with two other dinosaur types though there are also arm bone which we have never seen before all, said Arbour. Possible Sustut Dinosaur was new species but we didn't know sure until other fossils are found.
Read More..

The Earliest Inhabitants

Black and White photo by Abbott of bridge with water flowing under it [SPEC].
The earliest visitors to Sabino Canyon are believed to be hunter-gatherers of the Clovis culture. [Guide, p.2] They hunted big game, such as bison, Columbian mammoth, and other large mammals that lived in southern Arizona when the climate was cooler and more moist. Later, as the climate changed, the Cochise culture became dominant. The Cochise hunted small game and gathered edible plants. With the climate warming and water becoming less plentiful, the mountain canyon would have been an attractive place to see food and shelter. Archaeologists believe that they have correctly identified flat grindstones, called metates, stone points and other tools left behind in Lower Sabino Canyon by these people. [Lazaroff, p.80] The Clovis hunters could have come to the canyon as early as 12000 to 15000 years ago. The Cochise were most likely visitors closer to 8000 B.C.

The Hohokam became the predominant people in this area after the Cochise. The peak of their culture occurred around 1100 AD. [Guide, p.2] We are not sure where the Hohokam came from, whether they were descendants of the Cochise, or were migrants who came to Southern Arizona from Central America. The Hohokam were farmers, known for their use of irrigation systems to maintain their crops. The Hohokam built villages along Tucson's rivers and foothills. Archaeologists have found evidence of small dams west of the canyon. [Lazaroff, p.80-1] These check dams caught rainwater and soil. On the canyon floor there are indentations worn in the rock where the Hohokam ground beans. Hohokam pot sherds have also been found. By 1300 the population of the Tucson basin began to decrease, leading to the collapse of the Hohokam culture around AD 1450. No one is certain what caused the disappearance of this group: climatic changes, disease, social problems.

The Hohokam were replaced by the Pima and Tohono O'odham Indians, who still inhabit the Tucson area today. Both of these peoples were primarily farmers. They were well established, living in villages near Tucson's rivers, when the first Europeans came to this area in 1539. Padre Eusebio Francisco Kino named the village of San Cosme de Tucson and the Santa Catalina Mountains when he visited the area at the end of the seventeenth century. The Pima, Tohono O'odham, and Apache all probably used the canyon for access to water and as a cool refuge from the desert heat.
Early Tucson

Horseback rides in Sabino Creek, circa 1920s [SPEC].
Arizona became part of the United States with the ratification of the Gadsden Purchase in 1854. Bill Kirkland built a ranch house on Sabino Creek south of the canyon in the late 1850's. [Lazaroff, p.85] In 1873 this ranch was purchased by one of Tucson's wealthiest entrepreneurs, Leopoldo Carrillo. With city dwellers beginning to travel to Sabino Canyon for recreation, Carrillo intended to build a hotel and baths on the ranch property. He died without carrying out this plan, and a hotel was not be built near the canyon for another century.

In 1887, an earthquake centered in northern Mexico shook Southern Arizona. Tucson citizens reported seeing great clouds of dust rising from the Santa Catalina Mountains, the result of large boulders tumbling down the canyon walls into the valley. The results of this quake are plainly visible in Sabino's streambed today, and it is not difficult to imagine what would happen to some of the delicately balanced rocks lining the canyon walls should a similar earthquake occur today.

In the late 19th and early 20th centuries, visitors rode to Sabino Canyon on horseback, or came in horse-drawn carriages and wagons. [Lazaroff, p.88] A popular destination was the picnic grounds [SPEC] at the junction of Rattlesnake and Sabino creeks.

Picnicing in Sabino Canyon, circa 1920s [SPEC].
A dirt track lead to this area from the canyon entrance, much as the paved road leads to this area today. Beyond the picnic ground was a horse trail called Sabino Canyon Trail or Apache Trail, which led to high country. These trails were mainly used by pack animals to carry supplies to summer residents and temporary army camps, and to supply forest fighting teams. [Guide, p.3] Another popular destination was the dirt track to Lower Sabino. Congress established the Catalina Forest Reserve in 1902, which included Sabino Canyon

Col. Charles P. Sykes and a small group of associates staked claims to five gold mines near the mouth of Rattlesnake Canyon in 1892. [Lazaroff, p.90] By 1897, the group had formed the Sabino Gold Mining Company and had expanded its holdings to ten mines. The mines never panned out but the short tunnels dug into the canyon walls by this group can still be seen today.

Sabino Creek also figured into some early Tucson water-supply plans. [Lazaroff, p.93] As the city grew, citizens began to realize that they would need additional sources of water to supply the population. Many thought Sabino Creek would provide a likely source and devised elaborate schemes to deliver the water to Tucson. One plan was originally devised by a young University of Arizona professor, Sherman M. Woodward. He proposed a huge dam more than 3 miles upstream from the mouth of the canyon (1 mile beyond the current end of the paved road). Woodward moved from Tucson before he could put his plan into action. Another group, however, adopted his idea and formed the Great Western Power Company. By 1907, this groups' plan had grown to include a second dam in Bear Canyon, and a system of pipes and generating stations to supply both water and electric power to the city.

Fortunately for current Sabino Canyon visitors, these plans collapsed because of disputes over water rights, and a drought which showed that the reservoir would have been nearly dry had it been built. [Lazaroff, p.95] The dams were never built. One visible reminder of this period of the canyon's history, however, is the trail on the eastern slope of the Canyon wall. The Plat Rail Trail had been built to carry men and materials up to the site of the proposed dam. By 1912, a telephone line had been strung beside it. The trail in now called the Phoneline Train, and you can see the remnants of poles and wire today, along with an uncompleted diversion tunnel which penetrates 125 feet into the canyon wall.

The Depression

The 1930's brought improvements to Sabino Canyon. Tucson's citizens now envisioned a large dam at the canyon which would provide a great lake capable of supporting boating, fishing, camping and other recreational activities. [Lazaroff, p.95-7] The lake would be accessed via a winding road that would cross Sabino creek nine times over stone bridges. In the fall of 1934, the Emergency Relief Administration had crews in the canyon to build the new road beyond the old Rattlesnake Canyon picnic ground. By fall of 1935, 4 bridges had been built. The Works Progress Administration then assumed responsibility for the project, building the remaining bridges and laying the road up the wall of the canyon to approach the proposed dam site. When the WPA [26K] took over the road project in the upper canyon, the ERA crews began working on Lower Sabino Canyon, building roads and campgrounds. The Civilian Conservation Corps also worked on campgrounds, picnic tables, outhouses, grills, retaining walls, and the Lowell Ranger Station west of the canyon in Lower Sabino [Henry, p.77].

The dam in lower Sabino Canyon.
In June of 1937, funding had still not been secured to build the proposed dam in Upper Sabino Canyon and the road project was halted. [Lazaroff, p.99] The ERA's crews turned their attention to building a smaller dam in lower Sabino Canyon. The tiny lake formed by the ERA dam was enormously popular with Tucson's citizens, providing opportunities for swimming and fishing. Today the dam is still one of Sabino's most popular attractions, although the lake has long since been filled in with silt and plant life. The shaded, shallow pond and water falling over the small dam are frequented by picnickers, birdwatchers, and hikers. By 1940, the facilities in Upper and Lower Sabino Canyon were completed.

The Canyon Today

The Forest Service patrols the trails on horseback.
Sabino Canyon continued to grow in popularity over the next decades as Tucson's population grew. The Forest Service constructed the road into Lower Bear Canyon in 1960, and a Visitor's Center in 1963. [Guide, p.3] Eventually, overnight camping and private cars were banned in the canyon. A shuttlebus service began in 1978 to replace private cars. [Lazaroff, p.101] Today, locals and tourists take this narrated excursion to reach popular swimming areas in the upper canyon as well as to learn more about the natural history of the canyon.

Currently, Sabino Canyon has over 1 million visitors every year. Facilities continue to be improve, through the efforts of the USDA Forest Service and a local service group, the Friends of Sabino Canyon.
Read More..

 

ArchaeologyWorld

Recent Comments