Search

Analytical ceramic studies offer the opportunity to determine cultural development and change on the basis of origin and use of raw materials. In this particular study, an archaeometric approach on ceramics in central Pisidia contributes to the discussion of contact and exchange between indigenous communities and several cultural spheres of influence on a long-term timescale (eighth to second centuries bce). Morphological data as well as mineralogical (optical microscopy; n = 273) and chemical composition (by ICP-OES/MS; n = 122) of ceramics and raw materials show distinct resource zones for the production and distribution of ceramics in this connecting region of Anatolia. The use of trace element profiles (REE, HFSE, LILE and TTE) in particular is regarded as instrumental in detailing high-resolution provenancing of ceramics. The ceramic provenance indicates different patterns of material interactions during the Archaic, Classical and Hellenistic periods. A significant increase in regional interaction occurs coinciding with the development of pottery activities at Sagalassos.

This contribution discusses the Hellenistic, Roman and early Byzantine pottery collected during archaeological survey in the Bereket valley (territory of ancient Sagalassos, southwest Turkey). This collection contains both pottery imported from as yet unknown production centres and wares produced in the Potters’ Quarter of Sagalassos. Changes in the proportions of pottery produced at Sagalassos and those produced at other locations become visible in the fourthcentury AD material and reflect the evolving relationship between the peripheral valley of Bereket and the regional centre of Sagalassos. Yet, the undiminished quantity of pottery collected suggests that human activity continued without significant changes in habitation density. However, pollen cores from the same valley show that at more or less the same time crop cultivation diminished and was largely replaced by pastoralism. This shift occured at a time when climatic conditions had become more favourable for crop cultivation. A somewhat similar decrease in crop cultivation is also observed in Gravgaz marsh. In both valleys, this shift occured about 300 years earlier than in the rest of the territory of Sagalassos. Although the reasons for these changes cannot be determined on the basis of the study of survey pottery alone, the results presented show the importance of intensive survey and the study of peripheral areas for understanding inter-regional interaction patterns.

Absorbed lipid residues from 24 seventh- to ninth-century coarseware potsherds from the major Anglo-Saxon trading centre of Hamwic (Southampton, UK) were analysed by gas chromatography – mass spectrometry (GC–MS) in order to reconstruct the dietary habits of its population. The results show that the vessels were used for preparing ruminant fats and leafy vegetables. In addition, evidence was found for a minor contribution of aquatic foods. Beeswax was found once and most probably relates to a sealing function or to honey. Remarkable features were: (i) the isomeric mixture of octadecenoic acid (C18:1 Δ7,8,9,10,11,12,13,14,15,16) and 8- to 16-hydroxyoctadecanoic acid, and (ii) the co-occurrence of C17:1, C19:1 and isoprenoid fatty acids. These features were proposed as biomarkers for ruminant and aquatic food sources, respectively. Furthermore, the carbonyl position distribution in mid-chain ketones was used to identify mixtures of animal- and plant-derived ketones. The paper highlights the difficulty in interpreting complex lipid signatures that show a mixture of various foods, as observed in the majority of the samples. This was linked to the preparation of stews or the recycling of vessels. The results are considered alongside ceramic usewear data and existing data relating to environmental remains recovered from the Hamwic excavations.

An isotopic reconstruction of human dietary patterns and livestock management practices (herding, grazing, foddering, etc.) is presented here from the sites of Düzen Tepe and Sagalassos in southwestern Turkey. Carbon and nitrogen stable isotope ratios were determined from bone collagen extracted from humans (n = 49) and animals (n = 454) from five distinct time periods: Classical-Hellenistic (400-200 BC), Early to Middle Imperial (25 BC-300 AD), Late Imperial (300-450 AD), Early Byzantine (450-600 AD), and Middle Byzantine (800-1200 AD). The humans had protein sources that were based on C(3) plants and terrestrial animals. During the Classical-Hellenistic period, all of the domestic animals had δ(13) C and δ(15) N signatures that clustered together; evidence that the animals were herded in the same area or kept in enclosures and fed on similar foods. The diachronic analysis of the isotopic trends in the dogs, cattle, pigs, sheep, and goats highlighted subtle but distinct variations in these animals. The δ(13) C values of the dogs and cattle increased (reflecting C(4) plant consumption) during the Imperial and Byzantine periods, but the pigs and the goats displayed little change and a constant C(3) plant-based diet. The sheep had a variable δ(13) C pattern reflecting periods of greater and lesser consumption of C(4) plants in the diet. In addition, the δ(15) N values of the dogs, pigs, cattle, and sheep increase substantially from the Classical-Hellenistic to the Imperial periods reflecting a possible increase in protein consumption, but the goats showed a decrease. Finally, these isotopic results are discussed in the context of zooarcheological, archeobotanical, and trace element evidence.

Alluvial and colluvial sediment deposition provide a vital record of environmental change during the Holocene. Firm chronological control on these archives is necessary to enable us to relate sediment dynamics to human activity and climate variability. In the Eastern Mediterranean, such relationships are hard to establish due to the lack of spatially well-distributed sediment archives with good chronological control. This scarcity is problematic with respect to regional-scale reconstructions of the temporal variation of sediment dynamics. Here, we present a radiocarbon database (n ¼ 178) of geomorphological activity collected from multiple distinct sediment archives within the territory of Sagalassos in south-western Turkey. The data were grouped according to their sedimentary facies for analysis using cumulative probability distributions (CPDs) and sedimentation rate (SR) modelling. Two small-scale colluvial valleys, where chronological information was abundant, were investigated in more detail. Results show that sedimentation chronology differs between individual, nearby cores, as it depends strongly on the local geomorphic situation. A generalizing approach combining multiple core results yields more widely valid conclusions. High sedimentation rates coincided with the initial major anthropogenic disturbance of the landscape and decreased afterwards, probably due to hillslope soil depletion. CPD and SR analysis indicates that in general colluvial sedimentation rates did not change much from 2000 BC onwards. River floodplain sedimentation, in contrast, increased markedly during the first millennium BC and during recent times, and a significant time lag in enhanced sediment deposition between the upper and lower reaches of the river valleys was observed. Copyright # 2012 John Wiley & Sons, Ltd.

A well-dated pollen diagram from Gravgaz marsh, near the archaeological site of Sagalassos (western Taurus Mountains, Turkey), provides the first detailed record of vegetation change in southwest Turkey during the last two millennia. A newly developed numerical analysis disentangles the climatic and anthropogenic influences on vegetation and reveals for the first time for southwest Turkey the timing and influence of late-Holocene climate change. Results show that sudden vegetation changes, driven by changes in moisture availability, co-occurred with well-defined European climate shifts. A trend towards dry conditions, from c. ad 640 to 940, coincides with the cold early Middle Ages in Europe. During this period, human presence in the region diminished and agricultural activity switched focus from crop cultivation to pastoralism while signs of cereal cultivation temporarily ceased. This period was followed by a return to moister conditions from ad 940 to 1280, coinciding with the ‘Medieval Climate Anomaly’. During this period there was a resurgence of human activity in the basin. Another trend towards dry conditions occurred at c. ad 1280, corresponding with the start of the ‘Little Ice Age’ in Europe and another disappearance of cereal pollen until the present day. The numerical analyses suggest that human impact around Gravgaz during the last two millennia is primarily driven by climatic changes.

For over a decade, multi-element chemical analysis of floor sediments in archaeological contexts has been a tool to identify and interpret anthropogenic chemical residues and activities. For the current study, a multi-element chemical analysis was applied to floor samples from a Classical-Hellenistic courtyard building at Duzen Tepe (SW Turkey). Among a series of 19 elements analyzed, K, Mg, Fe, P and Sr are thought to directly reflect anthropogenic chemical residues. The elements Cr, Mg, Ni, Pb and Ti are considered to reflect the geological background of the site, yet their contents seem to vary over different chemical residue zones, making them a suitable tool for delineating activity areas. Overall, the sampling and analysis techniques applied at Duzen Tepe – mild acid sample extraction and ICP-OES analysis – have proven to be fit for this kind of study. The analyses allow human activity zones within the study area to be identified and interpreted and deliver insights into the archaeological contexts that could not be obtained by archaeological research alone.

Past vegetation change and the influence of climate change and anthropogenic pressure during the Holocene is constructed from a series of palynological records sampled from three locations within the territory of the antique site of Sagalassos. The disappearance of the original deciduous oak woodlands and increases in anthropogenic indicator species around 5300 and 4300 b.c. correspond with an increase in settlements in the region. A period of drought following the deforestation may have hampered the recovery of deciduous oak. The timing of the onset of the Beysehir Occupation Phase (BO-Phase) in the territory differs between locations, estimates ranging from ca. 1000–800 b.c. to the start of the Hellenistic period (334 b.c.). The most intense period of arboriculture coincides with the Roman and late-Roman periods. Increases in human pressure on the landscape as reflected in the pollen record correspond with an increased rate of sedimentation and fire activity. The timing of the end of the BO-Phase again differs between locations. Estimates range from the 4th century a.d. to the mid 7th century a.d., when a region-wide shift to dry environmental conditions is observed. Numerical analyses show that post BO-Phase vegetation change is largely driven by climate and displays a succession of dry and wet periods that coincided with well-defined European climate shifts, including the Medieval Climate Anomaly and the Little Ice Age. Current agricultural activities in the region are of a very recent (20th century) origin.

A 12th-13th-century A.D. ceramic assemblage from Alexander's Hill at Sagalassos in southwestern Turkey provides new evidence for the typochronological study of Byzantine pottery. A functional analysis of the assemblage, along with textual and iconographic evidence, archaeozoological and palynological analyses, and chemical analysis of cooking-pot residues, contributes to the reconstruction of diet and cooking practices in Anatolia. While baked fish, vegetables, pulses, and bread are usually regarded as the staples of Byzantine peasant cuisine, diners at Sagalassos were enjoying beef stews before the Fourth Crusade, when the technique of stewing meat was allegedly introduced to the eastern Mediterranean from the West. © The American School of Classical Studies at Athens. ispartof: Hesperia vol:79 issue:3 pages:423-464 status: published

When sampling white marble for INAA, using a diamond core drill and circular saw the inevitable contamination can be removed by etching the samples with HNO3 (1N). Samples are etched for five minutes, first immediately after extraction and a second time after irradiation. For cooling the drill and saw, distilled water must be used whereas pro analysi acid is shown to be sufficiently pure to prepare the etchant with.

Assessment of the wild or cultivated origin of Olea europaea L. during the middle to late Holocene according to pollen analyses is of palaeoecological and evolutionary interest as olive is thought to be one of the earliest cultivated trees and is still one of the most important fruit trees of the eastern Mediterranean. This paper considers data from the Bronze—Iron Age harbour-town, Tell Tweini, of the Ugarit Kingdom, in the Syrian coastal lowland near Jableh (17 m a.s.l.) and from the Hellenistic—Roman Moatra-Bereket (1410 m a.s.l.), in the territory of Sagalassos, in Turkey’s western Taurus Mountains. Both of these sites have recorded the rise and collapse of early eastern Mediterranean urban systems from 4200 to 1600 cal. yr BP. The Syrian data suggest that the Olea pollen-type originated from wild varieties during the Bronze and Iron Ages despite archaeological evidence for olive cultivation in the northern Levant. For Turkey, the results of the pollen-numerical analyses support the existing archaeological evidence of a wealthy oleoculture in Hellenistic and Roman Anatolia and suggest important anthropogenic pressures on local ecosystems.

This paper compares and evaluates the significance of spectral characteristics and pixel resolution of the very high spatial resolution satellite systems (VHSRS) Quickbird-2 and Ikonos-2 for automatic extraction of ancient features on one archaeological site, the antique town Sagalassos (southwest-Turkey). The evaluation of the spectral characteristics is based on a band-by-band comparison. Pixel- and object-based classification techniques are compared with visual analyses to assess the effects of different image characteristics. The analysis reveals that Quickbird-2 is outperforming Ikonos-2 for the visual identification of ancient remains. Its augmented spatial resolution however does not necessarily result in a better automatic classification. For Sagalassos, maximum likelihood classification on Ikonos-2 gives the best results. The accuracy of automatic extraction depends on the type and characteristics of the VHSRS data, the classification method and on on-site parameters. Site characteristics appear ...

Microwear analysis of pig teeth from the classical site of Sagalassos (SW Turkey) is undertaken to obtain insight into pig management strategies in this region from the 1st to 7th centuries AD. Earlier research on modern pigs revealed significant differences in microwear patterns between stall-fed and free-ranging, rooting individuals. A comparison of the microwear data of the Sagalassos pig with those from archaeological and modern pigs with a known or presumed type of management shows that the microwear of the Sagalassos pigs is very different. It is suggested that the Sagalassos pigs had a very soft, non-abrasive diet, that in the first instance cannot be attributed to either management type. Therefore, the nature of the substrate on which the animals were foraging and its impact on microwear are considered and the microwear data are compared with the results of previous archaeozoological research carried out at the site. Further, diachronic changes in microwear patterns are investigated.

Pitch compounds are frequently identified inside archaeological ceramic vessels. As their presence might affect the permeation of oil or wine into the ceramic fabric, experiments were conducted in which the diffusion of lipids or polyphenols into pitched and non-pitched modern vessels was followed by chemical analysis. Results show that the polyphenols of wine can intrude into the ceramics even through a pitch layer. Consequently, the absence of polyphenols in archaeological sherds is not due to their inability to reach the ceramic matrix under the pitch layer. By contrast, a pitch layer is quite effective to avoid oil intrusion into the ceramic matrix. Thus, it seems logical that oil amphorae would have been coated with pitch at the inside prior to use. Experiments in which the pitched ceramic was simultaneously exposed to oil and wine, show that the wine makes the pitch more permeable for the lipid compounds. These experimental data are confronted with residue analysis results obtained on amphorae fragments excavated in Sagalassos, Turkey. Pitch and oil were frequently found together. Based on a polyphenol test, indications for wine storage could only be obtained for two vessels. Against this background, the possible uses of the Sagalassos amphorae are discussed, and the traditional association of pine pitch with wine storage in archaeological amphorae is critically assessed.

Until recently, late antique quotidian objects were relegated to the domain of specialist studies and information relating to the context or assemblage within which the objects were found was rarely retained. The objects were studied as individual examples of form or type, rather than as part of an assemblage. The ability of archaeological evidence to contribute to the study of human behaviour largely derives from patterns in the dispersal of artefacts, however, and not simply from the objects themselves. A full description of the archaeological context of particular objects is thus required in order to maximise the recovery of data about the past. Contextual analysis, as it has been developed at Sagalassos, is used to identify human activities and their social and economic implications by carefully delineating the distribution of archaeological material, taking surrounding architecture and the process of context formation into account.

Two concentrations of animal bones, almost exclusively from small mammals and wild birds, were found within the destruction debris of a Roman bath complex in Sagalassos (SW Turkey). The overall species spectrum, skeletal element representation, fragmentation and preservation condition of the bones indicate that they represent the prey remains of a large nocturnal avian predator, more precisely the eagle owl (Bubo bubo). Differences in skeletal element representation and in prey species' spectrum show that the two bone clusters derive from pellets deposited near a nest site and a roost site, respectively. Radiocarbon dates obtained from the bones indicate that eagle owls lived in the collapsing bath complex during the second half of the 6th to the beginning of the 7th century AD, before the final abandonment of the town. The MNI of the prey animals found at the nest site, confronted with the daily dietary needs of a female eagle owl and its young, indicates repetitive use of the same place during several years. Copyright © 2008 John Wiley & Sons, Ltd.

The 800 cm long sequence from the Bereket provides the first detailed fire history in the western Taurus Mountains for the last three millennia. The main disturbances occurred during the Beyşehir Occupation Phase (BO Phase), a period of intensive polyculture and dated at Bereket from ca. 2230 to 1550 cal yr BP. Four phases of local and extra-local fire periods have been recorded at 2320–2240, 1985–1970, 1865–1820 cal yr BP and post-AD 1950. The fire history established for the BO Phase is complex, with fire periods alternating with periods without local fires, as is the case for the late BO Phase from 1820 until 1550 cal yr BP. It is suggested that the past agricultural practices including fires cause a higher soil erodibility than agricultural practices without fires. A climatic shift towards aridity during Roman times may have triggered the observed change in fire regime but local processes, mainly human disturbances, appear to be the proximal cause of all recorded changes. In the Bereket surroundings, fires led to a simplification of the vegetation structure, favouring soil erosion, pastures and intensive cultivation.

Burned greasy deposits were found inside shells of the large Nile bivalve Chambardia rubens, excavated in an eight- to tenth- century AD church of the Coptic monastery of Bawit, Egypt, and supposedly used as oil lamps. The residues were subjected to a combination of chromatographic residue analysis techniques. The rather high concentrations of unsaturated fatty acids, as analysed by gas chromatography (GC) in the methylated extract, suggest the presence of a vegetal oil. Analysis of the stable carbon isotopes (delta C-13 values) of the methyl esters also favoured plants over animals as the lipid source. In the search for biomarkers by GC coupled to mass spectrometry on a silylated extract, a range of diacids together with high concentrations of 13,14-dihydroxydocosanoate and 11,12-dihydroxyeicosanoate were found. These compounds are oxidation products of erucic acid and gondoic acid, which are abundantly present in seeds of Brassicaceae plants. Liquid chromatography coupled to mass spectrometry analysis showed low concentrations of unaltered triglycerides, but revealed sizeable amounts of triglycerides with at least one dihydroxylated acyl chain. The unusual preservation of dihydroxylated triglycerides and alpha,omega-dicarboxylic acids can be related to the dry preservation conditions. Analysis of the stereoisomers of the dihydroxylated fatty acids allows one to determine whether oxidation took place during burning of the fuel or afterwards. The results prove that the oil of rapeseed (Brassica napus L.) or radish (Raphanus sativus L.) was used as illuminant in early Islamic Egypt, and that not only ceramic lamps but also mollusk shells were used as fuel containers. ispartof: Analytical and Bioanalytical Chemistry vol:390 issue:2 pages:783-793 ispartof: location:Germany status: published

Aim To investigate the human impact on eastern Mediterranean ecosystems in a subhumid to semi-arid region of the Near East. Location This paper considers data from Bereket (1410-1440 m a.s.l.), an intramontane basin surrounded by the Kokayamk Tepe (1830 m a.s.l.) and the Besparmak Daglari (2280 m a.s.l.), in the western Taurus Mountains of south-west Turkey. Methods Late Holocene samples were collected along an 800-cm-deep sediment profile cored in the secondary valley of the Bereket basin. Descriptive vegetation data and modern pollen samples (moss polsters) were collected at elevational intervals of c. 15 m along an altitudinal transect from the Bereket basin (over Tepe Duzen, 1600 m a.s.l.) to Aglasun Dagi (1700 m a.s.l.). Information about the spatial distribution of the present land cover was obtained from ASTER satellite imagery. Digital elevation-derived data and geological information were used to examine the relationship between actual land cover and other environmental variables. Results The well dated Bereket sequence provides a unique record of biennial-to-decadal landscape changes driven primarily by intensive human impact from 360 cal. yr BC to 650 cal. yr AD. Since 360 cal. yr BC, over-exploitation of the land has led to altitudinal variation of tree lines, a destruction of the natural forest ecosystems (Pinus-Quercus cerris mixed forest), and an extensive spread of forest-steppe in the highlands. The present-day distribution of vegetation in the basin area shows that human activities remain the major factor influencing the character of modern ecosystems. Main conclusions This research demonstrates the long-term local destructive effects of human impacts on the mountainous ecosystems in a small Anatolian intramontane basin since 360 cal. yr BC, and the capacity of these ecosystems to recover during periods of reduced human impact. The late Holocene history and modern vegetation characteristics show that the past and present-day distribution and composition of vegetation are influenced primarily by human activity, and that substrate, elevation, slope and orientation are of secondary significance.

Three lipid analysis methods were applied to extracts of archaeological potsherds from the ancient city of Sagalassos, south-west Turkey. In the fatty acid methyl ester fraction, obtained by selective transesterification of acylglycerols, the ratio of methyl palmitate to methyl stearate was determined. Secondly, by means of gas chromatography‐ combustion‐isotope ratio mass spectrometry (GC‐C‐IRMS), stable carbon isotope ratios were measured for the same methyl esters. Finally, triglyceride composition was determined via high-performance liquid chromatography‐mass spectrometry (HPLC‐MS). All three methods can be used to trace the origin of animal fat. Agreement between them is reasonable, especially in recognizing ruminant adipose fat. One sample was found to be of dairy origin using both GC‐C‐IRMS and HPLC‐MS. The advantages of the various methods are discussed. Variations in lipid composition were observed between samples from different periods and excavated in diverse areas within the city of Sagalassos.

The existence of a local glass workshop is known at Sagalassos through archaeological and chemical analysis. In test soundings in the monumental city, an enigmatic ceramic cane was found attached to a chunk of green glass. This remarkable object is thought to be a pontil rod, more specifically a mandril. This study illustrates the use of ceramic tools in the glass craft as a readily available and cheap solution to the technical problems a glass-worker encountered. © 2007 The Authors; Journal compilation © 2007 Blackwell Publishing Ltd. ispartof: Oxford Journal of Archaeology vol:26 issue:2 pages:193-200 status: published

Archaeological research in the territory of Sagalassos is a multidisciplinary project covering scientific disciplines traditionally linked to archaeology and also new technologies such as very high-resolution remote sensing with sufficient radiometric and spatial resolution (

Lead and strontium isotope analyses were performed by thermal ionization mass spectrometry (TIMS) on Roman to Byzantine iron artefacts and iron ores from the territory of ancient Sagalassos (south-west Turkey), to evaluate Pb and Sr isotopes for provenance determination of ores for local iron production. It can be demonstrated that for early Roman artefacts and hematite iron ore processed in early Roman times from Sagalassos proper, as well as for magnetite placer sands and early Byzantine raw iron from the territory of the city, Sr isotopes are much less ambiguous than Pb isotopes in providing clearly coherent signatures for ore and related iron objects. Late Roman iron objects were produced from iron ores that as yet remain unidentified. Early Byzantine iron artefacts display more scatter in both their Pb and Sr isotope signatures, indicating that many different ore sources may have been used. Our study demonstrates that iron objects can be precisely analysed for their Sr isotopic composition, which, compared to Pb isotopes, appears to be a much more powerful tool for distinguishing between chronological groups and determining the provenance of raw materials.

The archaeological site of Sagalassos (SW Turkey) is located in a region characterized by the absence of any significant recent seismic activity, contrary to adjacent regions. However, the assessment of earthquake-related damage at the site suggests that the earthquakes that have been demonstrated to have struck this Pisidian city in ca. AD 500 and in the middle or second half of the 7th century AD are characterized by an MSK intensity of at least VIII and occurred on a fault very close to the city. Different investigation techniques (archaeoseismology, remote sensing and geomorphology, surface geology and structural data, 2D resistivity imaging and palaeoseismological trenching) have been applied at the archaeological site and its direct surroundings in search for the causative fault of these earthquakes. This multidisciplinary approach shows that each of the different approaches independently provides only partial, non-conclusive information with respect to the fault identification. Integration is imperative to give a conclusive answer in the search for the causative fault. This study has, indeed, revealed the existence of a to date unknown active normal fault system passing underneath ancient Sagalassos, i.e. the Sagalassos fault. A historical coseismic surface rupture event on this fault could be identified. This event possibly corresponds to the devastating Sagalassos earthquakes of ca. AD 500 and the middle or second half of the 7th century AD. Finally, this study demonstrates that in the particular geodynamic setting of SW Turkey archaeological sites with extensive earthquake-related damage form an important tool in any attempt to asses the seismic hazard.

The secondary production (working) of glass from imperial to early Byzantine times has been proven at the ancient city of Sagalassos (SW Turkey) by the existence of glass chunks, fuel ash slag and kiln fragments related to glass processing. It had been previously suggested that local green glass might have been recycled from two other locally found glass types (blue glass vessels and chunks and HIMT glass chunks). This paper provides analytical evidence for the recycling of glass next to the use of imported raw glass. The heterogeneous lead isotopic composition of the green and HIMT vessel glass at Sagalassos, with as end members on the one hand the isotopic composition of local blue glass vessels and chunks and on the other hand that of the HIMT glass chunks, could indicate the production of ‘recycled’ glass, although heterogeneous raw materials could have been used. However, the use of Sr-mixing lines confirms local recycling. It is clear that the Sr in the green and HIMT vessels is a mixture of the Sr in the aforementioned end members. It cannot be proved whether the green ‘recycled’ glass was produced from a mixture of chunks alone, or from a mixture of cullet and chunks. Suggestions are made towards the possible origin of the raw materials for the blue and HIMT glass on the basis of Sr isotopic signatures and absolute Sr contents in the glass.

The town of Sagalassos, located in south-western Turkey, was an important regional centre from the Hellenistic period to Late Antiquity. Since the 1990s, the site has been the subject of systematic interdisciplinary research focusing on industrial, commercial, and residential areas of the town. The aim of this paper is to present the results of the excavations of two residential complexes in the town, including a palatial mansion to the north of the Roman Baths and a late antique house/shop encroaching upon the east portico of the lower agora. These housing complexes provide evidence for the living conditions of both the upper and middle classes in Late Antiquity.

Using a large assemblage of domestic fowl bones from a classical site, a methodology is presented that allows the recognition of breeds. The approach differs from previous research in which tarsometatarsi were used exclusively. In the present paper, frequency histograms of long bone lengths and mixture analysis were combined with observations on medullary bone development. By concentrating on the analysis of bones with medullary bone, only the securely sexed part of the population (the females) is considered, thereby avoiding problems related to the use of spur development in tarsometatarsi. Three breeds of different sizes could be recognized, of which the smallest shows a high incidence of spurred females.

The Sagalassos Fault is one of the candidate faults for the devastating earthquakes that struck the ancient Pisidian town of Sagalassos, situated some 10 km SSW of Isparta (SW Turkey), early in the 6th century a.d . and in the middle or during the second half of the 7th century a.d . The Sagalassos Fault is an at least 150-m wide and ∼10 km long active normal fault zone, passing through and behind the ancient town. The southern base of the limestone cliff at the northwestern extremity of Sagalassos is believed to represent the strongly degraded master fault. The Sagalassos Fault Necropolis -trench, exposing this limestone face and its hanging wall deposits, reveals a fresh normal fault slip plane. Fault breccia, dip-slip frictional-wear striae, tool tracks, spall marks, dilational fractures and a flowstone are present on the excavated limestone face. Moreover, in the excavated part of the hanging wall, evidence of historical reactivation of the main fault has been inferred within anthropogenic deposits. The main argument is a 20-cm thick shear zone against the limestone face. This shear zone affects a man-made dump of the Early Imperial Period (ca. 25 b.c .–100 a.d .). The shear zone has an indurated and compact aspect, a parallel alignment of ceramic and limestone fragments, dip-slip striae and a vertical displacement of layers within the dump. The new findings of this study suggest that the surface-rupturing event identified may very well correspond to the 6th or 7th century earthquake, thus identifying a to date unknown seismically active and potentially hazardous fault in the Burdur–Isparta area.

The finding of glass chunks together with fuel ash slag and kiln fragments related to glass processing strongly suggests local secondary production (working) of glass at Sagalassos (SW Turkey) from imperial to early Byzantine times. Chemical evidence shows that different silica raw materials were used in imperial and early Byzantine times for blue and green glass found locally. Colourless glass shows no clear difference in chemical composition and hence in silica raw materials between late Roman and early Byzantine times. Locally found early Byzantine yellow-green glass and chunks correspond to the previously defined Byzantine HIMT glass type. The chemical composition of the glass chunks found, identical to that of the contemporary glass of the same colour, strongly indicates that these chunks were used for the manufacture of early Byzantine green, colourless and yellow-green glass at Sagalassos. The homogenous lead isotopic composition of the chronological groups of blue glass, suggests the use of two distinct but homogenous silica raw materials for the manufacture of this glass. In view of this homogeneity, it is likely that contemporary blue glass was produced at a single location. The linear trend of the heterogeneous lead isotopic composition of the green and colourless glass is a strong indication of recycling effects in the glass composition. The end members of this trend are formed by the isotopic composition of the blue glass on the one hand, and of the yellow-green (HIMT) glass on the other hand. The heterogeneous lead isotopic composition of the yellow-green glass at Sagalassos is probably the result of recycling of this glass, reflecting mixtures of the original lead isotopic signatures of the broken glass and the original HIMT glass chunks. It should be noted that the two main raw materials for primary glass production (silica and soda) were available on the territory of Sagalassos. Moreover, the lead isotopic composition of quartz pebbles sampled from the artisanal quarter of Sagalassos, is similar to that of the local blue glass.

En 2002, les vestiges bien preserves d'un hammam ont ete decouverts dans le village d'Aglasun (province de Burdur, Turquie). Il s'agit d'une construction de petite taille, precedee d'un espace semi-ouvert donnant acces a quatre salles. A considerer son plan et ses caracteristiques techniques et decoratives, il est comparable a des edifices similaires bâtis en Turquie durant la premiere moitie du XIIP siecle ap. J.-C. La plupart de ces hammams etaient partie integrante d'un caravanserail. Or, certaines indications laissent a penser que c'etait egalement le cas du hammam d'Aglasun. Cette hypothese est notamment favorisee par le fait que le village et son hammam se situent a mi-chemin entre incir Han et Egidir, a proximite de l'ancienne route caravaniere. Le fait que le caravanserail se situe le long de la meme route que trois autres structures similaires (Kirgoz Han, Susuz Han et Incir Han) datees du regne de Giyaseddin Kayhosrau II (1237-1246 ap. J.-C.), rend probable une datation a la meme periode, comme indique par la date proposee pour la construction du hammam.

Through chemical analysis of ancient animal bone found at the archaeological site of Sagalassos, and through comparison of the analytical data with that from modern bone and feed from the same location, conclusions on the ancient livestock are made. Samples of ancient and modern goat bone as well as Quercus coccifera were analyzed using Inductively Coupled Plasma–Mass Spectrometry (ICP‐MS). After evaluation of the consistency of the chemical characteristics of different types of modern bone in one individual, it is decided to use the trace element data of long bone for statistical treatment. After evaluation of the degree and effects of diagenesis in the fossil bone, it is concluded that trace element data are useful indicators for anthropogenic palaeoenvironmental pollution, as a distinction could be made between elements that occur naturally in the bedrock and those that can be linked to industrial pollution. The occurrence or depletion of the latter elements in fossil bone, show diachronic cha...

Lipid extracts of different types of pottery from the archaeological site Sagalassos (southwest Turkey) were investigated using several analytical techniques. The usefulness of lipid analysis in the functional analysis of a broad spectrum of pottery from one archaeological site was evaluated. The results establish indeed a relationship between vessel use and form. Based on the analyses a determination table could be drawn relating vessel use and form and separating the different types of vessels. This research shows that lipid analysis can be a valuable contribution to classify different ceramic pots.

The ancient Pisidian town of Sagalassos (southwest Turkey) was struck by several earthquakes during Roman and early Byzantine times and was abandoned around the middle of the seventh century AD, partly as the result of a devastating earthquake. A nearby epicentre is postulated, although the causative fault has not yet been identified. The identification of such an active fault is, however, important with respect to the assessment of the seismic hazard of the area. Two-dimensional resistivity imaging has been used to detect the presence of an active normal fault passing underneath Sagalassos, as evidenced by geological, geomorphological and archaeoseismological observations. The resistivity profiles reveal the presence of five stratigraphical layers, i.e. from bottom to top: the bedrock composed of either limestone or ophiolitic me lange, the weathered top of this bedrock, old colluvial material, recent colluvial material that covers archaeological structures and recent scree deposits. The presence of active normal faults is, moreover, indicated by the displacement of the bedrock and the colluvial material on top of it. Offsets of archaeological structures at Sagalassos are likely to be the result of historical reactivations of these faults. The limestone front, overlooking Sagalassos from the north, probably corresponds to the degraded fault plane of the detected fault zone. Sagalassos was thus built on the hanging wall of an active normal fault. Two-dimensional resistivity imaging proved to be an efficient tool in archaeoseismology. Copyright © 2003 John Wiley & Sons, Ltd.

Different types of builing stones have been macro-scopically and petrographically characterized at the ancient city of Sagalassos (SW Turkey). The natural building stones include limestone, conglomerate, breccia, marble, travertine, granite and sand-to siltstone of different qualities. The provenance of most of the building stones may be related to local lithological units, both in the immediate area of the city and on its territory. Also, some stone types were clearly imported from considerable distance. Throughout the history of the city, local beige and pink good quality limestone remained the most important building stone. Both the high quality white limestone from the territory of the city and the marbles imported from a distance of 250 km, represent only a small fraction of the total amount of building stones used. While the use of the white limestone can be considered to form a clear but limited trend from the Trajanic period (98–117 AD) onwards, the import of the marbles must be considered as a rare event. The selection of building stone went hand in hand with the appreciation for structural strength and suitability for carving complex architectural decoration, together with the desire to obtain a polychrome architecture.

Two pollen sequences from the Classical city of Sagalassos (Pisidia, southwest Turkey) show that the hills just north of the city were forested during the main occupation period of the city (late Hellenistic to early Byzantine). They demonstrate that there was a mixed needle-leaved forest of Pinus, Cedrus libani and Abies cilicica. The platform on which the city sat was already deforested, as is indicated by the presence of pollen from various light demanding herbs. Furthermore, there is evidence that grapevines (Vitis) were cultivated, indicating that much of the land below the city was already exploited for agricultural purposes. Walnut trees were also cultivated near the city. It is probable that suburban farmsteads were present close to the city. The pollen sequences show that man-made deposits from high altitudes may contain important information on the former natural and cultural vegetation of mountain sites in Anatolia. Archaeologists and palynologists should draw more attention to these pollen rich man-made contexts.

The excavations of Roman and Early Byzantine contexts at the town of Sagalassos (Turkey) yielded fish remains belonging to species that do not occur near the site. The modern geographical distribution of the identified fish indicates trade with various regions of Anatolia, the Mediterranean coast, Egypt and/or the Levant. Trade with Levant and Egypt is evident throughout the period by the presence of Clarias, a catfish living amongst others in the Nile and Levant. Mitochondrial DNA analysis was successfully carried out on modern populations of this species from Turkey, Syria, Israel and Egypt. Several variable regions were discovered on the mitochondrial control region containing polymorphisms that distinguish the haplotypes. Primer sets were designed to amplify small fragments of ancient DNA containing these informative regions. Ancient fish DNA could be successfully extracted, amplified and sequenced. The analyses indicate that the catfish bones belong to Clarias gariepinus and that they originated from the lower Nile. In addition, this study sheds light on the understanding of the modern distribution of C. gariepinus in Anatolia.

Fault- and joint-related calcite precipitates are investigated to reconstruct the neotectonic activity in the northwesternextremity of the Isparta Angle (SW Turkey). A preliminary palaeostress analysis allows us to frame the observed fault activity and joint development in the neotectonic history of SW Turkey. The mineralogical and geochemical study of the fault-related calcites indicates that fluids with a long residence time in the Lycean limestone were responsible for their precipitation. The joints, on the contrary, were passively filled with calcites precipitated from infiltrating near-surface meteoric water.

Aim To study the present-day olive stands and their ecology in the eastern part of the territory of the ancient city of Sagalassos, to study the variation of olive pollen production and dispersal near the olive stands, to establish a modern pollen reference model, and to compare Hellenistic–Roman pollen data from two wetlands with this modern reference model. Location Eastern part of the territory of the ancient city of Sagalassos, western Taurus mountain range in south-west Turkey. Methods The study is based on field survey, pollen analysis of surface samples, multivariate statistics of modern pollen data and the use of ‘modern analogues’ in comparison with Hellenistic–Roman pollen samples. Results A field survey revealed the presence of 35 olive stands in the study area. These are mainly small-scale stands. The olive pollen representation in the surface samples is highly variable. Two groups of modern ‘olive’ pollen spectra could be distinguished: (1) a group representing mainly olive stands from lush and moist mixed orchards; and (2) a group representing mainly olive stands from open small-scale olive stands in combination with annual crop agriculture. Although no ‘perfect’ modern analogue was found for the Hellenistic–Roman pollen data, the fossil pollen data show similarities with modern spectra from the second group, due to the presence of relatively high pollen values for secondary anthropogenic indicators. Main conclusion A well-organized and diverse, but time- and energy-consuming, agricultural system was maintained nearby the wetlands of Canakli soils, presumably to maximize the yields in both valleys.

The extensive territory of the ancient (Hellenistic to Byzantine) city of Sagalassos (SW Turkey) offered a rich variety in natural mineral resources. The frequent occurrence of iron slag in the excavations at the site proved the local working of metal. A geochemical prospection campaign was done in the territory of the ancient city in order to identify or discard the city and its territory as a self-sustaining metallurgical centre. Secondly, the geochemical impact of ancient metallurgy was investigated. Geochemical anomalies identified in stream sediments are explained by the presence of mineralised deposits and ancient metal working. Mg, Cr, Co and Ni anomalies point to chromite and chrysotile-magnetite deposits related to the basic rocks of the Lycian nappes in the area. Fe, V and Ti anomalies indicate the presence of iron mineralisations, which have been worked for iron production in ancient times. Finally, the association of P, Cu, Ph, Mn, As and Ag anomalies are an indicator of human activity at archaeological sites'. Within the framework of this geochemical prospection, a metal working site apart from the city of Sagalassos was identified. Here, ore was both extracted and processed to workable iron. (C) 2002 Elsevier Science B.V All rights reserved. ispartof: Journal of geochemical exploration vol:77 issue:1 pages:65-80 status: published