Tell Nader & Tell Baqrta 2012-2-1

download Tell Nader & Tell Baqrta 2012-2-1

of 47

description

Archaeology geophysics

Transcript of Tell Nader & Tell Baqrta 2012-2-1

  • The Tell Nader and Tell Baqrta Project in the Kurdistan Region of Iraq:

    Preliminary Report of the 2011 Season.

    Konstantinos KOPANIAS, Claudia BEUGER, Tristan CARTER, Sherry FOX, Angelos HADJIKOUMIS, Georgia KOURTESSI-PHILIPPAKIS,

    Alexandra LIVARDA, John MACGINNIS

    Submitted for publication in SUBARTU - Archaeological Journal of the Kurdistan Region of Iraq (April 2012).

    Introduction .................................................................................................................................1Tell Nader Project .......................................................................................................................2

    Preparation ..............................................................................................................................2Survey .....................................................................................................................................2Principles of excavation ..........................................................................................................3Excavation...............................................................................................................................3Pottery .....................................................................................................................................7Archaeobotany and environmental sampling..........................................................................9Faunal Remains .....................................................................................................................10Human Remains ....................................................................................................................14Lithics ...................................................................................................................................15A Preliminary Report on the Tell Nader Obsidian Characterisation ....................................16

    Tell Baqrta Project ....................................................................................................................21Tell Baqrta - first reflections on its place in history .............................................................22

    Future Directions for the Tell Nader and Tell Baqrta Project ..................................................26Cited Works ..............................................................................................................................27Appendix ...................................................................................................................................31

  • 1

    IntroductionDr. Konstantinos Kopanias

    In October 2010 the University of Athens obtained permission by the Ministry of

    Municipalities and Tourism of the Kurdistan Regional Government of Iraq (KRG), the General

    Directorate of Antiquities of Kurdistan and the Directorate of Antiquities of Erbil to conduct

    excavations in two important archaeological sites: first in Tell Nader, which lies on the outskirts of

    the city of Erbil and then Tell Baqrta, approximately 28 km to the south of Erbil (Fig. 1). Tell Nader

    was discovered by Mr. Nader Babakr Muhammad, archaeologist of the General Directorate of

    Antiquities of Kurdistan and Tell Baqrta was brought to our attention by Dr. Narmen Ali Muhamad

    Amen, Professor of Archaeology at the Salahaddin University-Hawler. In November 2010 the

    University of Athens obtained written permission to conduct an excavation in both sites also by the

    Ministry of Culture of Iraq and the State Board of Antiquities and Heritage. In addition, Mr. Nawzad

    Hadi Mawlood, the Governor of the Erbil Province, invited a team of the University of Athens in

    order to examine older and new theories concerning the location of the Gaugamela battlefield.

    In April and early May 2011 a 14-member archaeological and a historical team from the

    University of Athens, under my direction, traveled to Erbil and started a systematic excavation at

    Tell Nader, conducted a preparatory survey at Tell Baqrta and a topographical survey in search of

    the Gaugamela battlefield. This has been the first Greek archaeological excavation in Mesopotamia.

    This archaeological and historical expedition was financed by the Greek Ministry of Culture

    and Tourism, by the Greek Ministry of Foreign Affairs and the University of Athens. The cost of

    the archaeobotanical and zooarchaeoloical research was financed by the University of Sheffield, UK.

    The airline Viking Hellas kindly sponsored a total of 17 airplane tickets. Also the Governorate of

    Erbil offered us inexpensive accommodation at the Iraqi Institute for the Conservation of Antiquities

    and Heritage and the company PLAISIO sponsored two laptop computers for our research.

    The work of the Archaeological and Historical Mission of the University of Athens was

    monitored by the General Directorate of Antiquities of Kurdistan (under the direction of Mr.

    Malaawat Abubaker Othman Zendin) and the Directorate of Antiquities of Erbil (under the direction

    of Mr. Haydar Hassan Hussein).

  • 2

    TellNaderProjectDr. Konstantinos Kopanias

    PreparationTell Nader lies at the fringes of Erbil (36.173148, 44.075490), approximately 6,3 km E-NE

    of the citadel and ca. 2,8 km SE of the Majidi Mall (Fig. 2-3). The diameter of this Tell is ca. 100 m.

    and its height ca. 5 m. It was located first by Mr. Nader Muhammad, an archaeologist of the General

    Directorate of Antiquities of Kurdistan, and was named accordingly after him.

    Prior to its discovery a part of it was unfortunately destroyed during construction works for

    the three adjacent city roads. Moreover, in an attempt to build a house, a bulldozer destroyed the NE

    part of the Tell and also removed part of the surface layer in its northern end (Fig. 2). The

    unauthorized excavation was brought to a halt by the Directorate of Antiquities and this Tell was

    declared an archaeological site. Despite this fact, the site remained under threat because of the very

    intensive building activity in the area. Thus, conducting a rescue excavation was imperative.

    In May 2010 Mr. Nader Muhammad and Dr. Konstantinos Kopanias conducted a preparatory

    inspection on the site. In August 2010 a jar burial was discovered during digging of a trench for a

    water pipe in the west end of the site (Fig. 4). The jar could be studied only in the photographs that

    Mr. Nader Muhammad kindly provided us, and it still remains buried in situ. According to Dr.

    Claudia Beuger (ibid.) the jar is dated probably to the Middle- rather than to the Neo-Assyrian

    period. Part of the skeleton was recovered and stored in the Erbil Civilization Museum, where it was

    studied by Dr. Sherry Fox (ibid.: TN1).

    During the first few days of our first campaign in April 2011 we purchased in Erbil digging

    tools, the necessary equipment for washing, conserving and storing the finds, as well as a tent for the

    night guard of the excavation. The Head of the Directorate of Antiquities of Erbil, Mr. Haydar

    Hussein, permitted us to use one room in his Directorate for the study of pottery and animal bones.

    Dr. Alexandra Livarda (ibid.) was able to build a sophisticated flotation system that recycles water

    for the processing of soil samples. We also prepared the excavation grid of 5x5 m squares and a

    topographic plan of the site.

    Survey Time constraints during this first campaign did not allow us to conduct an intensive survey on

    site. But, prior to the excavation, we surveyed the area, collected characteristic surface pottery and

    lithics, and noted their coordinates on the topographic plan (Fig. 5). Moreover we collected all

    surface finds from the 24 grid squares, which have been chosen as the starting point of the

  • 3

    excavation. From the surface of this 20x30 m area we collected a total of 2.956 pottery sherds with a

    total weight of 50 kg (each sherd is represented as a randomly plotted red dot on the plan) and 660

    lithics, with a total weight of 8 kg (each is represented as a randomly plotted blue dot on the plan)

    (Fig. 6). The surface finds indicate that Tell Nader was in use from the 6th millennium (Hassuna

    period) down to the late 2nd/early 1st mil. B.C. (Middle/Neo-Assyrian period). The main periods of

    site occupation, judging from the quantity of finds, seem to have been the Late Ubaid/Early Uruk1

    and the Middle-Assyrian.

    Principles of excavation It was decided to conduct the excavation at Tell Nader according to the following principles:

    all archaeological layers, including the surface layer, are excavated in a systematic way, not only the ones that were considered to be interesting,

    all pottery and lithic finds are collected, weighted, photographed and will be studied. Even the undateable finds will offer valuable statistical information,

    all architectural remains will be conserved and, if possible, preserved, palaeoenvironmental samples from every Excavation Unit will be collected and analysed, after each excavation season, all perishable architectural remains will be properly covered, in

    order to keep them protected from the weather elements.

    Excavation The main aim of the excavation at Tell Nader is to record a stratigraphy from the Late

    Neolithic down to the Middle/Neo Assyrian period, which will allow us to construct a secure dating

    system for the locally produced pottery and the lithics. Tell Nader could become a reference point for

    future research in northeastern Mesopotamia. The systematic study of the palaeoenvironmental

    material (plant and insect remains, animal and human bones etc.) will offer a valuable insight into

    daily life in the area during the above mentioned periods.

    The excavation was conducted with the assistance of 12 Kurdish workers, divided in four

    groups. In each group a Greek and a Kurdish archaeologist were responsible for the documentation.

    The Directorate of Antiquities assigned five archaeologists to our excavation (Mr. Goran

    Mohammed, Ms. Hazan Latif, Ms. Lavin Jabar, Ms. Rezna Abdulkadel and Mr. Swan Ahmed) and

    also a driver (Mr. Ramzi Hamed). All of them worked harmoniously with their Greek colleagues and

    contributed significantly to the successful outcome of this campaign. Moreover, a team of three

    students and a teaching assistant of the Department of Archaeology of the Salahaddin University- 1 Jasim 1985; Henrickson - Thuesen 1989; Bauer et al. 1998; Hammade - Yamazaki 2006; Butterlin 2009; Carter

    Philip 2010.

  • 4

    Hawler took part in the excavation, as arranged by the Head of the Department, Dr. Ahmed M.

    Mirza. Mr. Haydar Hussein and Mr. Nader Babakr Muhammed visited regularly our excavation site

    and offered us their valuable assistance in many instances.

    We opted for the open area excavation method, which meant that the excavation was done

    through natural stratigraphic layers on a larger scale without maintaining bulk walls. During the first

    season in April 2011 we began our excavation in the northern part of the Tell, where the bulldozers

    had removed the surface layers, and excavated an area of 15x15 m. (Fig. 7a-b) The excavation

    produced a total of 15.654 pottery sherds (total weight 500 kg) and 2.319 lithics (total weight 24 kg),

    mainly flint but also 68 obsidian. All finds have been collected, inventorized and stored in the Erbil

    Civilization Museum. The excavation revealed so far no buildings, although several well-baked

    bricks have been found, which indicate the existence of architectural remains in the area.

    The excavation has so far revealed one main stratigraphic layer. According to the preliminary

    examination of the pottery, the layer seems to be dated to the Late Ubaid/Early Uruk period. To this

    layer belong a number of simple clay constructions:

    1. An artificial concentration of small stones was unearthed in the western part of the excavation

    area (Fig. 8). The bulldozer removed here most of the surface layer, so this find was only

    0.10-0.20 m. under the surface. This stone concentration covered the interior of two simple

    clay constructions, probably ovens. After the careful removal of this layer, two almost

    circular clay constructions came to light (Fig. 9). The western one (C-1) was found partially

    destroyed. Part of its wall was apparently broken already in the antiquity and was moved

    from its original position. Nevertheless, the eastern circular construction (C-2) was not

    damaged2. Inside it there was an inhumation burial of an adult woman (TN 2: Sherry Fox,

    ibid.) (Fig. 10). Her legs were flexed, her hands positioned on her breast and belly, but,

    strangely, her body was in a prone position and also her head faced the ground3. The circular

    construction was too small for the body, so its feet stuck out. The impression we get is that

    the female was placed very carelessly inside the clay construction. Her prone position was

    intentional, as noted by Dr. Sherry Fox. Several pieces of clay were found near her head, an

    indication that the soil was shoveled very carelessly on the dead body. No funerary offerings

    were found inside the grave, with the exception of three dog teeth (all from different

    animals), which were found near the head of the dead person. With the permission of the

    Directorate of Antiquities, the skeleton was temporarily transported to Athens for further

    examination in the Wiener Laboratory of the American School of Classical Studies at 2 Dimensions: N-S 0,90-1,10 m. and E-W 1 m., preserved width of clay walls: 0,07-0,28 m. 3 For the burial customs of the Ubaid: Hole 1989. For Tepe Gawra in particular: Peasnall 2002.

  • 5

    Athens4. The anthropological study, conducted by Dr. Sherry Fox (ibid), is still in progress. A

    small sample of the bone material was sent to the University of Arizona (USA), where Dr.

    Greg Hodgins is going to conduct C-14 analysis.

    2. A similar clay circular construction (C-3) was unearthed further north of the first two ones

    (Fig. 8). Its interior remains unexcavated, so it is not yet known whether it was also used as

    grave or not. Such clay constructions with similar dimensions have been found, among other

    sites, at Tepe Gawra5, where they were used as ovens or kilns6, and also at Arpachiyah7, from

    contemporary layers with the one at Tell Nader. It seems that all three clay circular

    constructions that were discovered so far at Tell Nader were also used as ovens or kilns. After

    their abandonment, one of them was used as an improvised grave for the adult woman (TN 2).

    3. An oval shaped installation of pebbles with burnt clay in-between them was discovered in the

    northern part of the excavation area (Fig. 11). On top of this installation and also around it

    several stone tools were unearthed. Only the lower part of this construction survives. Its

    upper part was destroyed by the bulldozer, as indicated by the traces of its tires and also its

    metal plate.

    4. A two-chambered sun-dried clay construction with irregular walls also belong to this layer

    (Fig. 12). Its upper part was probably destroyed by the bulldozer. It seems to be similar with

    a two-chambered pottery kiln at Yarim Tepe I8.

    5. Near the two-chambered kiln is also an oval-shaped earthenware tannur, with a thick layer of

    ashes around it.

    6. A concentration of clay pieces, similar to the ones used for the circular constructions but not

    in situ, pottery sherds, an almost intact plate, animal bones and two animal figurines were

    also excavated (Fig. 13).

    The great bulk of finds were pottery sherds (15.654 with a total weight of ca. 500 kg) and also

    lithics (2.319 with a total weight of ca. 24 kg). The finds include many cores, flakes, blades and

    waste, so there is evidence of all stages of the reduction sequence (G. Kourtessi-Philippakis ibid.)

    (Fig. 15). A sample of the obsidian finds was sent to Dr. Tristan Carter (ibid.) at the McMaster

    4 For more information: http://www.ascsa.edu.gr/ 5 e.g. Tepe Gawra, Square 5-S, Stratum XVI: Tobler 1950, 41 pl. XLIIa. 6 For the terminology see Yasim 1985, 53: the term kiln refers to commercial installations used for pottery making;

    the term oven for those which were used for domestic purposes such as making bread; and hearth for those in the form of shallow pits used for cooking and heating.

    7 Mallowan - Cruikshank Rose 1939, 14. 8 Oates Oates 1976, 42.

  • 6

    University in Canada for a non-destructive analysis with an Energy-Dispersive XRF Spectrometer.

    The initial analysis shows that the material originates mainly from southeastern Anatolia.

    From all excavated units we collected three separate soil samples: one for archaeobotany and

    environmental sampling, one for mineralogical analysis, and one for the identification of insects. Dr.

    Alexandra Livarda built an elaborate flotation machine for the archaeobotany and environmental

    sampling (Fig. 14), probably the first one that was used for an excavation in the Kurdistan Region,

    and flotated a total of 104 bulk soil samples (Livarda ibid). The soil sieving allowed us to find 18

    tiny beads of different materials and colors. In addition, the excavation brought to light a total of 472

    animal bones, all of which were examined by Dr. Angelos Hadjikoumis. At least 137 bones could be

    identified (Hadjikoumis ibid.).

    We also found a total of five clay animal figurines, which probably served as toys and not as

    votives9. The first one (U608-BAG18-V7), possibly depicting a ram (?), clearly resembles figurines

    from the Ubaid layer at Tepe Gawra10 (Fig. 16). The second animal figurine (U35-BAG2-V1),

    possibly depicting a sheep (?), is also very similar to Ubaid finds from Tepe Gawra11 (Fig. 17).

    The excavation also produced six of the so called clay nails (Tonngel), which are very

    typical of the Ubaid period (Fig. 18). There has been some speculation about their interpretation

    (decorative wall pegs, paint grinders, sickle hand protectors, model bull's horns, nail-shaped

    mullers)12, but the matter is still unresolved. These clay nails are found in southern Mesopotamia13,

    but also in sites near Tell Nader, such as Arpachiyah14 and Tepe Gawra15.

    Another interesting find is a clay horn-shaped object (Fig. 19) and a similar cone object with

    a flattened upper end (Fig. 20). Such objects have been interpreted as tokens16 or gaming pieces17.

    Close parallels have been found in a tomb from Stratum XVIII at Tepe Gawra18. At Tell Nader we

    have also unearthed clay spindle whorls (Fig. 21), similar to those known in several north

    Mesopotamian sites19 and also Qalinj Agha20, terracotta disks perforated through the middle, which

    served as jar stoppers (Fig. 22)21, and also a stone macehead (U403-BAG8)22.

    9 Tobler 1950, 165-166. 10 Tepe Gawra: 1) Tobler 1950, 224 pl. LXXXII.c.6. 2) Tobler 1950, 224 pl. LXXXII.c.1. 3) Tobler 1950, 243 pl.

    LXXXI.b.2, pl. CLIV.12. The figurine cannot be compared with Ubaid figurines from southern Mesopotamia (e.g. from Uruk: Wrede 2003, pl. 14-22), but bears clear similarity with figurines from North Mesopotamian sites: e.g. Arpachiyah (Mallowan - Cruikshank Rose 1939, 88 fig. 48 no. 8) and Choga Mami (Oates 1969, 149 Pl. 31e).

    11 Tobler 1950, 243 pl. CLIV.18. 12 Tobler 1950, 169. 13 e.g. Uruk: Schmidt 1972, 39 pl. 59 no. 705-706 (I thank Dr. M. Van Esch for this parallel). 14 Mallowan - Cruikshank Rose 1939, 90 pl. 49.8. 15 Tobler 1950, 224 pl. LXXXIII f-g. 16 For a discussion about the tokens see Bauer et al. 1998, 46 ff. 17 Tobler 1950, 170. 18 Tobler 1950, pl. LXXXIV.c. 19 e.g. Arpachiyah: Mallowan - Cruikshank Rose 1939, 88 fig. 49 nos. 15-16.

  • 7

    PotteryDr. Claudia Beuger

    Pottery sherds,which have been collected on the surface of Tell Nader byMr.NaderBabakr Muhammed and Dr. Konstantinos Kopanias in May 2010, showed that Chalcolithicstrata should be expected on the site. In addition, the brief rescue excavation, which wasconductedbytheDirectorateofAntiquitiesofErbilinAugust2010inthewestendofthesite,revealedaMiddle/NeoAssyrianjarburial(Fig.24.5).ThefindsfromthesurveyoftheteamoftheUniversityofAthensandalsofromthefirstexcavationseasoninApril2011leadtoamoreprecise estimation of the chronological sequence in Tell Nader. Themajority of the potteryfindsfromthesitecanbedatedintheChalcolithicperiod,andconsistmainlyofpaintedEarlyNorthernUbaidpottery(Fig.23.810),aswellaspotteryoftheTransitional(Fig.23.1112)and the Gawrahorizon (Fig.23.1315). Nevertheless, isolated finds from theHassuna (Fig.23.14), Samarra (Fig.23.56) and Halaf (Fig.23.7) periods lead to the assumption that acompletestratigraphyoftheLateNeolithic/Chalcolithicisexpectedinthesite.

    Therearealsoisolatedpotteryfindsfromlaterperiods,whichindicatethatthesitewasnot abandoned altogether, namely from the Uruk period (Fig. 23.16), the early thirdmillennium (Fig. 23.1) and probably also the early second millennium. The relativelynumerousfindsofcharacteristicMiddleAssyrianpottery,whichhavebeencollectedduringthesurface survey prior to the excavation, lead to the conclusion that this site was still in useduring that time (Fig.24.24). Finally, no certain NeoAssyrian or later pottery types havebeenrecognizedyet.

    The first excavation season in Tell Nader produced a total of 18.600 pottery sherds.Duringthefirstexcavationcampaignwehaveconcentratedmainlyontheclassificationofthepotteryaccordingtoitsfabricandalsothevaseforms.Sofarwewereabletodefineatotalof43different fabric types.Thesystematicstatisticalanalysisof thepotterymaterial isnotyetconcluded, but some patterns are already visible, such as the occurrence of the OrganicTemperedFabric(F8)mainlyinMiddleAssyrianvaseshapes.Atotalofmorethan300sherdshave already been drawn, also thanks to the assistance ofMs. Hazan Latif andMs. ReznaAbdulkadel,botharchaeologistsoftheDirectorateofAntiquitiesinErbil.

    20 Al-Soof 1966; 1968 ; 1969; al-Soof Es-Siwwani 1967; Hijara 1973; Gut 1996. 21 e.g. Arpachiyah: Mallowan - Cruikshank Rose 1939, 90 fig.49 no. 22. 22 Tepe Gawra: Speiser 1935, 86-87 pl. XLII no. 4; Rothmann 2002, pl 66 no. 629 (Level XIA/B), pl. 66 no. 1181

    (Level XI/XA).

  • 8

    Fig. No.

    Fabric, Decoration Date Reference Reference context

    23.1 buff, very fine clay with some fine lime and several bigger lime pieces, some black and red minerals, some fine organic temper, decoration incised

    Hassuna Gut 1995, tab. 4 nos. 38, 40

    Nineveh

    23.2 light brown, very fine clay with some fine organic temper and some fine mica, decoration incised

    Hassuna Gut 1995, tab. 4 nos. 45 Nineveh

    23.3 light brown, fine clay with a lot of coarse organic temper, some bigger pieces of lime, decoration impressed

    Hassuna husking tray

    Gut 1995, tab. 5 no. 58 Nineveh

    23.4 buff, very fine clay with some-plenty organic temper, plenty of very fine and some bigger pieces of lime, some fine minerals, some polish, reddish brown paint

    Hasuna Gut 1995, tab. 8 no. 91, 92, 95

    Nineveh

    23.5 light buff, very fine clay with plenty of minerals (mostly black and white) and lime, some fine organic temper, smooth surface with reddish brown paint

    Samarra Gut 1995, tab. 26 no. 441, tab. 27 no. 450

    Nineveh

    23.6 buff, fine clay with plenty of black minerals, plenty of fine lime, some fine mica, surface with light slip and some polish, reddish brown paint

    Samarra Gut 1995, tab. 24 no. 427, Table 31, no. 491, tab. 33 no. 518, tab. 42 no. 621

    Nineveh

    23.7 light brown, very fine clay with very fine lime, some fine black minerals, inside and outside very fine polish, black paint

    Halaf Gut 1995, tab. 44 no. 689, tab. 47 no. 723, tab. 48

    no. 736

    Nineveh

    23.8 buff, very fine clay with some fine organic temper, very hard (almost metallic), some polish, black paint

    Early Northern Ubaid (Gawra

    XIX-XVII)

    Akkermans 1988, 137 fig. 2.12

    Hammam et-Turkman IVA

    23.9 greenish, very fine clay with some fine lime, some black and red minerals, some organic temper, black paint

    Early Northern Ubaid

    (Gawra XIX-XVII)

    Akkermans 1988, 138 fig. 3.32+36

    Hammam et-Turkman IVA

    23.10 buff, very fine clay with some fine lime and several bigger lime pieces, some black and red minerals, some fine organic temper, dark brown-grey paint

    Early Northern Ubaid

    (Gawra XIX-XVII)

    Gut 1995, tab. 52 no. 788 Akkermans 1988, 138 fig.

    3.35

    Nineveh

    Hammam et-Turkman IVA

    23.11 light buff, fine-very fine clay with plenty of fine and bigger lime pieces and minerals (red, black, white), some bigger organic temper

    Late Ubaid-Gawra B

    (Gawra XII-IX)

    Matthews 2003, fig. 3.15:15

    Tell Brak HS6 level 3

    23.12 buff, very fine clay with some fine lime and several bigger lime pieces, some black and red minerals, some fine organic temper, reddish brown paint

    Late Ubaid/trans.

    Ubaid

    Rothman 2002, pl. 7 nos. 320, 324

    Gawra level XII/XIIA

    23.13 light buff, fine clay with a lot of fine and bigger lime pieces, plenty of organic temper (sometimes not completely burned), reddish brown paint

    Gawra XIA-XI = Gawra A

    Akkermans 1988, 141 fig. 6.87

    Hammam et-Turkman VA

    23.14 buff, very fine clay with some fine lime and several bigger lime pieces, some black and red minerals, some fine organic temper

    Gawra A Rothman 2002, pl. 9 nos. 723, 750

    Gawra level XIA/B

    23.15 buff, very fine clay with some fine lime and several bigger lime pieces, some black and red minerals, some fine organic temper, decoration painted

    Gawra A Rothman 2002, pl. 9 no. 790

    Gawra level XIA/B

    23.16 greenish-buff, fine clay with very fine lime and minerals (black, red, white), some bigger lime

    Early Middle Southern Uruk

    Matthews 2003, fig. 4.18:4-5

    Tell Brak HS1 level 6

  • 9

    pieces (Gawra VIII) 24.1 buff (greenish), fine clay with a lot of very fine

    minerals, lime and organic temper, some mica, black paint

    Ninivite 5 Gut 1995, tab. 83 no. 1183

    Nineveh

    24.2 buff, fine clay with plenty coarse organic temper and fine lime

    Middle/Neo-Assyrian

    Beuger 2007, 189 fig. 99 Assur

    24.3 buff, fine clay with plenty coarse organic temper and fine lime

    Middle Assyrian

    Beuger 2007, 127 fig. 60 Assur

    24.4 buff, fine clay with plenty coarse organic temper and fine lime

    Middle Assyrian

    Beuger 2007, 127 fig. 61 Assur

    Archaeobotany and environmental sampling Dr. Alexandra Livarda, Dr. Mike Charles, Dr. Amy Bogaard

    The priorities of the environmental team during the first excavation season were to devise and

    implement a systematic soil sampling strategy and create the installations for the processing of

    samples. Systematic sampling allows detection of both presence and absence patterns across space

    and time, and therefore, reliable identification of any activity areas. In total 104 bulk soil samples

    were collected from all excavated units, excluding the top soil layers. The samples were processed in

    a York-style flotation machine, adapted to recycle water in an attempt to minimize wastage and

    respect the limited water resources of the area (Fig. 14). A 1mm aperture mesh was used to retain the

    heavy residues while the flots were being collected in a very fine piece of cloth.

    Forty-seven of the heavy residues were sorted in their entirety for all categories of material

    during the April-May 2011 field season. Most samples had small numbers of animal bone and shells

    fragments and worked flint/stones. In addition, 40 of the samples contained small amounts of

    charcoal fragments. Also, 17 small beads of various colors (black, white, grey and green) were found

    in 12 samples.

    Processing of the flots was carried out at the University of Sheffield during the summer

    (2011) and their analysis is ongoing. The preliminary results indicated the sporadic presence of plant

    macrofossils in 47 samples, including cereals, such as bread wheat (Triticum aestivum L.) and barley

    (Hordeum vulgare L.), possibly pea and wild species, mainly grasses (Poaceae) and mineralised

    seeds of Lithospermum sp.

  • 10

    Faunal Remains Dr. Angelos Hadjikoumis

    The overall aim of zooarchaeology at Tell Nader is to study and follow the evolution of all

    human-animal interactions at the site. This includes many specific aims revolving around general

    themes such as hunting, animal husbandry, the cultural role of animals, the surrounding environment

    and its exploitation, cuisine and many others. Due to the small size of the assemblage, its bad

    preservation condition and the currently crude chronology, this first faunal report remains on a

    general level.

    The faunal assemblage was recovered through hand collection and dry sieving (1mm aperture

    mesh). It consisted of 472 specimens but from these, only 137 recordable elements could be

    identified to species or genus. The assemblage was washed, studied and recorded at the Erbil

    Civilization Museum in May 2011 by the author. The majority of specimens were not identifiable

    due to severe fragmentation (mostly in the past), erosion of bone surface and, most importantly, the

    cement-like crust in which they were enveloped. Even among identified bones erosion and

    concretions were very common with a 77% affected by erosion or concretions or both. Halsteads23

    recording protocol was used with few additions and changes. Identification was aided only by

    anatomical atlantes24 as no reference collection was available in Erbil.

    At least six species of mammal and one species of bird are represented in the assemblage.

    Before proceeding to the most abundant species, issues concerning rare or intrusive species are

    briefly addressed. Such species at Tell Nader include an equid (horse/donkey), a bird and a rodent.

    The equid is represented only by a heavily worn permanent maxillary premolar/molar and

    unfortunately it cannot be determined with certainty whether it belonged to the original

    archaeological assemblage or it was incorporated in it recently. Birds are represented by 4

    specimens. Two left tibiotarsi fragments are compatible with a medium-sized member of the

    Accipitridae family25 (diurnal birds of prey) though this should be confirmed or refuted through

    comparisons with modern reference specimens. A femur of a small/medium-sized bird was also

    recorded but not identified, as was another long bone fragment. Lastly, the remains of rodents

    include a near-complete skeleton of a rodent and a maxilla belonging to another individual. The

    23 Halstead 2011: 741-749 24 Barone 1976; Pales and Garcia 1982; Schmidt 1972 25 I would like to thank my colleague Lionel Gourichon for giving me his opinion on these specimens. Any mistakes

    remain mine.

  • 11

    remains belong to a species of the genus Spalax26, probably Spalax ehrenbergi, although there still

    considerable confusion in mole rat taxonomy in the Middle East. Irrespective of species, members of

    the genus Spalax in the Middle East are the commonest burrowers in the region27 and hence, most

    probably of intrusive origin in the upper strata of archaeological sites.

    The bulk of mammalian remains belong to cattle, sheep/goat, pig and dog (Table. 1). It has to

    be clarified that the possibility of the presence of jackal remains in the category dog is open simply

    due to the diachronic presence of the dog/wolf-sized golden jackal (Canis aureus) in the Middle East

    and despite the absence of any indication for it. According to the Maximum Anatomical Units

    (MaxAU) count, the most abundant species is sheep/goat (47%) followed closely by the pig (39%),

    while cattle, also taking into account their large size, are also significant with 11%. A canid (most

    probably dog) is also present in the assemblage in low numbers (3%). An interesting result

    concerning the sheep/goat category is that no sheep has been identified and goat contributed 14% to

    the total 47% of the category.

    Table 1: Main animal species in the 2011 Tell Nader assemblage.

    26 I would like to thank my colleagues Katerina Papayiannis, Miriam Belmaker and Paul Halstead for their opinions. Any

    mistakes remain mine. 27 E.g. Reed 1958

  • 12

    Data on the age-at-death are scarce and should thus be reconsidered in the future with more data.

    Based on tooth eruption and wear of mandibular teeth, the general tendency for sheep/goat is low

    mortality in the first year, high in the second and moderate from the third year onwards (Table 2).

    Concerning pigs, data are pointing towards high mortality in the second half of the first year and

    some in the second year with very few animals surviving beyond the third (Table 3). No cattle teeth

    were identified in the assemblage, while dog was represented by the teeth of at least two animals.

    One was a 1-2 month-old puppy represented by an unworn mandibular dP4. The other was an

    unworn upper M1, representing also a young animal, most probably younger than 6 months old. Both

    these teeth, along with a permanent lower incisor, were found near the head of a human burial but

    without any reliable evidence of association with it. This should be clarified in following seasons

    when more burials are excavated.

    Table 2: Sheep/Goat age-at death based on mandibular eruption and wear data.

  • 13

    Table 3: Pig age-at death based on mandibular eruption and wear data.

    Analyses are still under way and more results and discussion will appear in the literature soon,

    especially when more material comes to light for zooarchaeological study in the second excavation

    season scheduled for September-October 2012.

  • 14

    Human Remains Dr. Sherry C. Fox

    The human skeletal remains from two primary inhumation burials have been recovered, to

    date, from the archaeological site of Tell Nader. Recovery of the human skeletal material from TN 1

    had been directed by the eponymous Mr. Nader Babakr Muhammed prior to the University of

    Athens excavations in April/May 2011. TN 1 is currently stored at the Erbil Civilization Museum.

    Temporary transfer was granted of the human and animal bone within Erbil to the Iraqi Institute for

    Conservation of Antiquities and Heritage where the author began examination of the human remains

    representing TN 1 on April 25th. TN 1 was recovered from a broken jar with the legs in a hyper-

    flexed position (Fig. 4). It is posited that the skeleton was bound prior to placement in the jar. The

    individual is largely incomplete and in a fair-to-poor state of preservation. The bones were dry-

    brushed prior to analyses and some elements were reconstructed with UHU brand wood glue. The

    sex of the individual is indeterminate at present, but future study could help elucidate the sex. The

    age-at-death of the individual is estimated to have been 36 years + 10 years. Ten teeth have been

    recovered from TN 1 that require further analysis. There are non-metric traits recorded for this

    individual along with a possible pathology. Stature reconstruction was not attempted as no complete

    long bones were recovered from TN 1. Aside from the jar, no other artifacts are associated with TN 1.

    It is hoped that more of TN 1 will be recovered from excavations during the coming field season.

    The second skeleton (TN 2) was found in situ on April 27th within a circular burial cist grave

    from Unit 621 (Fig. 9-10). The virtually circularly shaped enclosure, measured approximately 110

    cm x 90 cm at its greatest diameter and 85 cm x 75 cm at the inside diameter with an apparent

    channel running along the outside circumference, near both a large ceramic sherd and on either side

    of two tile fragments. The cranium of TN 2 was abutting the inside circumference of the burial

    enclosure comprised of clay and tiles. The cranium was positioned slightly on its left side, facing

    down (inferiorly) toward the west, and along with the remainder of the skeleton, it appears to have

    been interred in a prone position with the arms and legs flexed to the left such that the right hip was

    likely inferior. Prone burials are not that common, from the authors experience. The femora were

    positioned toward the east of the cist grave. Although the human skeleton from within this circular

    enclosure was primarily interred, it appears to have been slightly disturbed. Once again, the

    preservation of the human remains is fair-to-poor. The age of this individual appears to be adult,

    although a more precise age-at-death remains to be estimated and the individuals sex remains to be

    determined. This material requires further study in a laboratory setting and the remains have been

  • 15

    temporarily transferred to the Wiener Laboratory of the American School of Classical Studies at

    Athens. At present, there are no known pathological lesions nor non-metric traits preserved.

    Reconstruction of adult living stature has not been attempted at this time for this individual either.

    There were very few grave goods associated with TN 2 in this rather simple grave. Future analyses

    should help provide greater information about this individual.

    LithicsDr. Georgia Kourtesi-Philippaki

    The first excavation season in Tell Nader produced 2.979 lithics with a total weight of 32.2

    kg. The raw materials mainly used for the production of the lithic tools were flint (94%, i.e. ca. 2.800

    finds in total) and obsidian (2.28%, i.e. 68 finds) (Fig. 15). An untrimmed stone and also a flake

    were produced in quartz.

    Several varieties of flint of many different colors were used. From the technological point of

    view there is evidence of all stages of the reduction sequence (chaine operatoire), since the finds

    include many cores, flakes, blades and waste. The flint tools are relatively few, in relation to the

    volume of lithic debitage. There is a tendency to use blades as blanks. We also find a certain type of

    borers.

    The examination of a sample of obsidian finds from the 2011 excavation season showed the

    existence of two stone types: a black opaque obsidian and also an almost entirely transparent greyish

    one. Both varieties were used for the production of blades, in most part with the pressure flaking

    method. Among the finds are also two cores, which are very suitable for the production of micro-

    blades. Micro-blades, as well as cores, make up a significant percentage of the total count of the

    lithic products. Some blades show traces of use, while one obsidian blade has a deniculate edge.

  • 16

    APreliminaryReportontheTellNaderObsidianCharacterisationDr. Tristan Carter, Dr. Renee Ford and Dr. Sarah Grant28

    Introduction While the Tell Nader chipped stone assemblage is dominated by local raw materials (see

    Kourtessi-Philippakis, ibid.), it also includes a small quantity of implements manufactured from

    obsidian (n=68, 2%), a volcanic glass razor sharp when freshly knapped whose nearest sources

    lay some 300km to the north in south-eastern Anatolia (Fig. 26). Although only a minority

    component, the obsidian is an important data-set, as scientific techniques developed over the past 50

    years have enabled us to determine with great accuracy where these raw materials came from, thus

    shedding light on a communitys regional and supra-regional connections (Chataigner 1998;

    Renfrew et al 1966). The methodological basis of these sourcing studies, is that (a) the obsidian of

    each volcanic source is remarkably homogenous with regard to its chemical composition (far more

    so than flint), (b) each of these source materials is chemically distinct, and can thus be analytically

    discriminated from one another (c) using the same analytical techniques one can then match the

    chemical fingerprint of an obsidian artefact with that of a source specimen in order to elucidate

    provenance (Pollard and Heron 2008: 75-97). While complications can arise in the process (see

    below), it remains that an obsidian characterisation study represents a powerful means of

    reconstructing the various socio-economic networks within which members of the Tell Nader

    community participated.

    Sampling and analysis In 2011 thirteen obsidian artefacts were selected for elemental characterisation (19% of total

    assemblage), the pieces chosen to represent the raw material variability in the assemblage with

    regard to colour, texture and opacity. All bar one of the artefact is in the form of fragmentary

    pressure-flaked blades / microblades, plus a single non-cortical flake (Fig. 27). While no cores were

    included in this analysis, two obsidian microblade nuclei are reported from the 2011 excavation (see

    Kourtessi-Philippakis, this report). The material is all considered to date to the Late Ubaid/Early

    Uruk Period, specifically the 5th/4th mil. B.C. (Kopanias, this report). The artefacts were analyzed

    whole and non-destructively at the McMaster Archaeological XRF Laboratory [MAX Lab] using a

    28 McMaster Archaeological XRF Lab / Department of Anthropology, McMaster University, Chester New Hall, 524, 1280 Main Street West, Hamilton, ON L8S 4L9, Canada.

  • 17

    Thermo Scientific ARL QuantX energy-dispersive x-ray fluorescence spectrometer [EDXRF], each

    piece having first been cleaned in an ultrasonic tank with distilled water for ten minutes. The analysis

    recorded three major and twelve trace elements, their concentrations estimated through reference to

    various geo-standards of known composition purchased from the US Geological Service and

    Geological Survey of Japan. The analytical protocols and methods follow those devised by Shackley

    (2005, appendix; Poupeau et al 2010: 2711); full details will be provided in our final report.

    In attempting to provenance these artefacts raw materials, we compared their chemical

    signatures with those of source samples run by the MAX Lab under the same analytical conditions.

    In choosing which geological products to compare with the Tell Nader data, it makes sense to first

    consider the results of previous obsidian characterisation studies from nearby sites of similar dates,

    i.e. mid-6th/4th millennium cal BC, Periods 8-9 in the Maison de lOrient scheme (Hours et al 1994).

    Some of the most commonly recognised raw materials from excavations of the period east of the

    Tigris in the Zagros or Iranian Highlands are the highly distinctive peralkaline products of Bingl

    and/or Nemrut Da in eastern Anatolia, a distance of up to 2000 km away (Blackman 1984; Chataigner 1998: 310-311, Fig. 16a-b; Mahdavi and Bovington 1976; Renfrew et al 1966). We thus

    included in our analyses geological samples from the major sources of the Lake Van region and

    those from further to the north (Fig. 28), namely Bingl, Meydan Da, Mu, Nemrut Da, Pasinler and Suphan Da (Poidevin 1998).

    We also included data from the central Anatolian sources of Acgl, Gll Da and Nenezi Da (Fig. 28); while Cappadocian products are rarely attested east of the Syrian desert (Renfrew et al 1966: 48), small quantities have allegedly been documented at Chalcolithic (Period 9) sites as far

    east as Mashnaqa in north-east Syria and Tepe Sabz in Irans Deh Luran plain (Chataigner 1998:

    290; Renfrew 1977), plus Jaffarabad and Susa in the lower Zagros of south-western Iran (Mahdavi

    and Bovington 1976).

    From here on matters become more complicated, as characterisation studies of Iraqi and

    Iranian have almost always generated data from artefacts that could neither be matched to central or

    eastern Anatolian sources. In these cases the likelihood is that either (a) not all pertinent Anatolian

    obsidian was included in the analyses, (b) the artefacts were in fact made of obsidian from other

    regions, likely either those located in Armenia, for which we have an increasing number of recent

    studies (Blackman et al 1998; Cherry et al 2010; Chataigner et al 2003), or from northern Iran,

    whose sources remain largely unexplored (though see Niknami et al 2010).

  • 18

    Preliminary results In a Zirconium vs. Strontium contents plot, the artefacts are clearly discriminated into two

    groups (Fig. 29). The largest set, comprising nine artefacts (eight blades and a flake [Fig. 27, 1-9]),

    are highly distinctive on the basis of their green colour and high Zr values (>1000 ppm); their

    elemental profiles match those of geological samples from the eastern Anatolian (Lake Van region)

    sources of Bingl and Nemrut Da. While these volcanoes are separated by 150km, their peralkaline products (Bingl also has the more common black, calc-alkaline obsidian) have often been difficult

    to discriminate due to many of their trace elements having similar values, whereby many studies

    assign these artefacts to a Bingl A / Nemrut Da group (though see Chataigner 1994; Frahm 2012). Focusing purely on these peralkaline obsidians and using an Ti/Mn v. Fe/Mn ratio plot, we

    achieve a high level but not complete discrimination between our Bingl A and Nemrut Da geological samples, with the Tell Nader artefact signatures more closely approximating those from

    Nemrut Da (Fig. 30). We are continuing to work on this issue of discriminating these important eastern Anatolian sources and to test our working hypothesis that these nine artefacts are largely, if

    not exclusively made of obsidian from the Bingl massif.

    The remaining four pressure-flaked blades / bladelets (Fig. 27, 10-13) are made of translucent

    purple-grey obsidian whose chemical signatures do not match any source exactly, but most closely

    approximate the southern Cappadocian source materials from Gll Da and Suphan Da on the north coast of Lake Van (Fig. 26). If one contrasts thee source products elemental composition in a

    bivariate Y vs. Rb plot, then one clearly appreciates that the Tell Nader artefacts composition far

    more closely approximates those from Suphan Da (Fig. 30), though once again the data do not match exactly. Our preliminary claim is that these four artefacts are made from obsidian procured

    from an outcrop on the flanks of Suphan Da that has yet to be located. If our interpretation is correct, then this would be only the second time that this raw material was found on an

    archaeological site, having allegedly been first documented from Late Chalcolithic Arslantepe, over

    300km west of the source (Chataigner 1998: 308; Fornaseri et al 1975-1977). The final point to note,

    is that while these four artefacts Sr values tightly cluster (24-27ppm), as to a slightly lesser extent do

    their Zr contents (92-113ppm), they display a significant variability in their Zn concentrations (53-

    362ppm), suggesting that these pieces may represent more than one source.

    The Tell Nader results in context Over the past 50 years there have been numerous obsidian characterization studies undertaken

    on assemblages of broadly similar date to the Tell Nader material and from the larger region, i.e.

    Mesopotamia, the Levant and south-eastern Anatolia (cf. Chataigner 1998; Frahm 200x, inter alia).

  • 19

    We here focus specifically on data from the 5th/4th millennium B.C., i.e. contemporary with the

    material under consideration, the Early Northern Ubaid, Transitional and the Gawra-horizon, or

    Periods 8-9 in the chronological scheme of the Maison de lOrient (Hours et al 1994).

    Taking this broader perspective, one immediately appreciates that the people of Tell Nader

    were only one of a great many communities at this time who were accessing peralkaline obsidians

    from the Lake Van region. Artefacts characterized as being made of Bingl A / Nemrut Da obsidian (or having the visually distinctive green appearance) have been documented from numerous sites

    throughout the larger region (Fig. 26), including nearby Arpachiyah and Pisdeli, and further south at

    Choga Mami and Tepe Sabz in the Deh Luran, then Suse, Ouelli and Ubaid down in southern

    Mesopotamia (Chataigner 1998: 310, Fig. 11b; Forster and Grave 2012; Healy 2010; Renfrew 1977).

    The consumption of these eastern Anatolian raw materials by populations in Iraqi Kurdistan in fact

    forms part of a very long-term tradition, used by populations of the Zagros and northern Syria from

    some 30,000 BP, as attested by small quantities of peralkaline obsidian from in Upper Palaeolithic

    strata of the Shanidar Cave (c. 100km to the NE of Tell Nader) and Epi-Palaeolithic deposits at the

    nearby Zarzi cave (Cauvin and Chataigner 1998: 329; Renfrew et al 1966: 40-41, Fig. 4a). During

    the Ubaid period one might view the movement in terms of In terms of the actual routes by which

    this material moved, then one can likely talk in terms of a cross-land caravan route to the Tigris and

    thereafter water-borne transport southwards.

    It is not entirely clear at this point as to the specific means by which these Bingl and/or

    Nemrut Da products reached the inhabitants of Tell Nader; ideally we need to view a larger assemblage to see if there is evidence for the on-site working of obsidian, or whether the community

    was reliant upon others for access to ready-made implements. The idea of gateway communities

    (cf. Hirth 1978) who served as the primary points of access into the obsidian source region and as

    production and redistribution centres, is a long established one. There are a number of sites, of

    various periods, such as Halafian Tilki Tepe ([Wright and Gordus 1969: 76) and Hurrian Tell Brak

    and Tell Mozan (Frahm 2010: 724-729), whose mass of obsidian working including the reduction

    of large raw blocks is taken to indicate a level of production above and beyond the needs of the

    immediate community, with preformed cores and/or pressure-flaked blades then being traded to

    populations further away. Late Chalcolithic Tell Hamoukar in north-eastern Syria is another such

    site, occupying a nodal position on both east-west and north-south trade routes, with good evidence

    for local blade manufacture (from the Southern Extension part of the site in particular), with rough

    outs, flake debris and a number of blade cores, with all those analysed shown to come from the

    Bingl sources (Khalidi et al 2009). Closer to Tell Nader is Tell Arpachiyah, where thousands of

    pieces of flint and obsidian cores and chips were found in the well-known late Halafian Burnt

  • 20

    House (Mallowan and Rose 1935: 105). The concentration of this material along with other

    commodities and a number of seals has been viewed as evidence for the accumulation and

    redistribution of obsidian blades within a system of formalised central exchange (Campbell 2000).

    Certainly the Tell Arpachiyah assemblage is anomalous with so much material (including >200

    cores) given its distance from the sources, indicating that members of this community were well

    connected within larger regional trade networks. One might have thus expected that nearby

    communities such as Tell Nader were dependent upon the Tell Arpachiyah craftspeople for their

    obsidian blades, but the early impressions from the site with the blade cores suggest that this may not

    be the case (we await clear evidence of their contemporaneity). Might we ultimately view the sites as

    inter-dependent partners, i.e. acting as gateway communities / central-place pair, supplying

    populations further to the east and south, as for example has recently been suggested for the

    relationship between Bronze Age Tell Mozan and Tell Brak (Frahm 2010: 650-651).

    At both Tell Arpachiyah and Tell Nader green peralkaline obsidian is dominant (Campbell

    2000: 21-22), indicating that Bingl and/or Nemrut Da were the primary sources being exploited at this time. As noted above, this fits the general contemporary pattern and forms part of a much

    longer-term history of these sources products by Mesopotamian populations (Cauvin and Chataigner

    1998).

    Future directions Ultimately there are a number of different strategies we need to follow to successfully

    complete this study. Firstly, we need to find a better match for our four alleged Suphan Da pieces. Secondly, in keeping with our other lab projects, we need to fully integrate our chemical data with an

    artefacts techno-typological attributes and specific archaeological findspot, i.e. to move away from a

    focus on compositional analysis to an integrated contextual / chane opratoire analytical framework

    (cf. Carter et al 2006; Carter and Kilikoglou 2007). This will help us maximise our potential to use

    characterisation studies as a means to further shedding light on Tell Naders local, regional and

    supra-regional connections and its place within the larger socio-economic structures of the Ubaid and

    other periods (cf. Healey 2010).

    Acknowledgements The MAX Lab was established by a Canada Foundation for Innovation - Leaders Opportunity Fund,

    while the research project within which the Tell Nader artefacts were analysed was paid for by a

  • 21

    Social Sciences and Humanities Research Council - Standard Research Grant (both awarded to T.

    Carter). We thank Danica Mihailovi for the line illustrations and map.

    TellBaqrtaProjectDr. Konstantinos Kopanias

    Tell Baqrta is located 28 km south of Erbil, near the village Minara, on the road to Makhmour

    (Fig. 1). It is one of the largest archaeological sites of the Erbil region (Fig. 23-25). It measures ca.

    220 m in diameter and 20 m in height. This so far unknown site was brought to our attention by Dr.

    Narmen Ali Muhamad Amen, Professor of Archaeology at the Salahaddin University-Hawler. The

    University of Athens received a permit to excavate this Tell, which will be conducted after the

    conclusion of the Tell Nader Project. We have visited the site in October 2010, accompanied by Mr.

    Nader Babakr Muhammad (General Directorate of Antiquities) and Mr. Saber Hasan Hussein

    (Directorate of Antiquities of Erbil), and also in April 2011, accompanied by Mr. Goran Mohammed

    (Directorate of Antiquities of Erbil), Dr. Athanasios Sideris and Dr. Claudia Beuger.

    This site lies on the road that connected Arbela with middle Mesopotamia and controls an

    important pass on the hill chain south of Erbil. On the surface lie thousands of pottery sherds and

    hundreds of lithics, which indicate that the site was in use from the Chalcolithic down to the Parthian

    and Islamic period, but not during later periods. Tell Baqrta was probably walled during some

    periods of its long history, and had two main access points, which are still visible.

    During our visit an unexpected find was made by Dr. Athanasios Sideris: an Attic Late

    Classical sherd, probably from the first half of the 4th century B.C. Although this find could have

    arrived to the site through trade, it could also be connected with the march of Xenophon's Ten

    Thousand. In 401 B.C., on their way back from Cunaxa (ca. 70 km north of Babylon), they crossed

    the Great Zab river just a few kilometers west of Tell Baqrta. Hopefully, the excavation is going to

    produce more finds that will shed some light on this question.

  • 22

    TellBaqrtafirstreflectionsonitsplaceinhistoryDr. John MacGinnis

    The site of Tell Baqrta lies 28 km SSW of Erbil in the plain of Makhmur, an area of Iraq

    which until recently had received very little in the way of archaeological attention. In 1948 Mallowan

    and El Amin carried out a campaign of exploration in the Makhmur plain, carrying out soundings in

    the sites of Kaula Kandal (8 miles southwest of Dibega on the road running from Erbil to the Tigris),

    Tell Aqrah (18 km east of the Tigris at the northeastern end of the Qaraj) and Tell Ibrahim Bayis (Old

    Makhmur). These sites produced material from the Halaf period onwards and they all also had

    Assyrian remains, including evidence for an Assyrian temple at Old Makhmur. Other important

    Assyrian sites in the vicinity reported by Mallowan and El Amin included Pir Daoud (12 miles from

    Erbil) and Dibega (on the western flank of the Avanah Dagh hills)29. These forays amply

    demonstrated that the plain of Makhmur is host to an astonishingly collection of archaeological sites,

    investigation of which can be expected to produce rich results. It is therefore very satisfying to see

    such operations commencing, firstly with the work of the French team at Qasr Shemamok and now

    with that of the Greek team at Tell Baqrta.

    We set out here to give a concise outline of the historical phases which we might expect to

    find represented at the site, concentrating on the ancient Mesopotamian periods up until the coming

    of Alexander. These are only preliminary remarks. More detailed observations will follow in a

    subsequent contribution. As yet the ancient name of the site has not been identified. This of course

    greatly hampers the degree to which its history can be reconstructed, but it does not entirely frustrate

    such an endeavour as it is still possible to articulate a more general understanding of the region in

    which Tell Baqrta lies. A recurring theme is the degree and times at which Tell Baqrta was dependent

    on other cities; particularly in the earlier periods, there is simply not enough evidence to say whether

    or not it was the capital of an independent polity. Thus, through the third and the first part of the

    second millennium Tell Baqrta might have been dependent on Erbil. Later, when it unquestionably

    lay within the core territory of the Assyrian empire, it will also have had connections with other

    major cities such as Assur, Balawat, Kilizu, Nineveh and Nimrud.

    Surface ceramics have already demonstrated that the plain of Makhmur was host to a

    presence in the Half and Ubaid periods. Numerous sites have produced ceramics of these dates and it

    is likely that future research will establish that that there were flourishing occupations in these

    periods. For present purposes however we will commence our reflections with the Uruk period

    29 Amin & Mallowan 1949, 146.

  • 23

    (4000-3000 BC) as this is the earliest date at which something approaching history may be

    considered. To my knowledge no texts of this period have as yet been discovered in the region. It is

    however conceivable, even likely, that early administrative literacy will have also had a place here

    and that texts of this date will in due course be discovered. Nor do we as yet have any texts from the

    region from the Early Dynastic Period (3000-2334 BC) or, as far as we can tell, references to the

    region in texts from that date. The same is essentially also true with regard to the Akkadian Period

    (2334-2193 BC) with one difference, however: the region must have either been incorporated in the

    empire of Sargon of Akkad or at least lain close on the borders - we know that Sargon took control of

    Assur and Nineveh though not - as far as we can tell - Erbil. The Akkadian administration must

    certainly have been aware of the region's existence and importance30.

    The region actually enters history in the Gutian Period (2193-2120 BC) when Erbil (Urbilum)

    became the objective of a military campaign of a certain Erridu-Pizir, a king of the Gutium who

    probably ruled in the interval between the end of the Akkadian empire and the foundation of the Ur

    III state; a more exact placing of this king cannot be given at present. It has been suggested that

    Urbilum in fact lay within the state of Lullubum but this is far from certain. Nor is it known whether

    or not Tell Baqrta came within the administrative control of Erbil. Nevertheless it is clear that the site

    must have been caught up in the convulsions that marked the transition from the Akkadian Empire to

    Gutian dominance and it is not unlikely that excavation will eventually cast light on this.

    Whatever the eventual conclusion, there is no doubt that Tell Baqrta then came under the

    control of the Ur III Empire. The period of Gutian domination came to an end with the

    reestablishment of Sumerian control over Mesopotamia. The first steps were taken by Utu-hegal

    when he expelled the Gutians from the land. His period of dominance was however short lived as he

    was in his turn ousted by one of his own officials, Ur-Nammu, who thereby initiated the Third

    Dynasty of Ur and went on to create the Neo-Sumerian empire. Two kings of the Third Dynasty

    besieged and took Erbil - Shulgi in his forty-fifth year and Amar-Sin in his second year. In addition to

    booty taken from Erbil itself, an annual tribute was imposed and will certainly have been levied on

    the whole land; Tell Baqrta was certainly incorporated within the Ur III empire, most likely as part of

    the province of Urbilum, and will have been affected by this tax.

    The fall of the Ur III state led to a major reconfiguration of the political geography of

    Mesopotamia. In the north the city of Assur regained its independence, leading to the emergence of a

    nascent Assyrian state. Little is known of the region at this time. Erbil - now written Urbel - will also

    30 The statue found in 1975 at Bassetki on the highway between Zakho and Mosul (Ayish 1976) attests to the fact that that the sway of Naram-Sin extended at least that far north, but we have no evidence at present how far it extended to the east of the Tigris at this point.

  • 24

    have regained its independence, at least temporarily, and once again an important question will be to

    consider whether Tell Baqrta was itself independent, dependent on Erbil, or part of some other

    political configuration. The site will however have next come within the sphere of the empire of

    Shamshi-Adad I after he joined up with Dadusha of Eshnunna and campaigned against and took

    Erbil, an event recorded in stelae of each of these kings. Erbil itself may have previously been part of

    the kingdom of Qabra though this is not certain nor is it known whether Tell Baqrta also fell within

    the control of Qabra. In any case when the Turukkean rebellion broke out Shamshi-Adad and his sons

    were not able to keep hold of the region.

    Once more, though for the last time, we face the question of whether Tell Baqrta was

    dependent on Erbil or was the capital of its own polity, but this long history of punctuated autonomy

    finally comes to an end with the rise of Mittanni and then of the Middle Assyrian empire. To take the

    first of these, it is not known when the site came under Mittanni domination - though it must be no

    later than the reign of Saustatar, by which time Arrapha was under Mittanni control - nor is it known

    at what point control was wrested away by the kings of Assyria. Broadly though it is probably fair to

    say that Tell Baqrta will have been subject to Mittanni rule over something like 1430-1350 BC. The

    next change came with the rise of the Middle Assyrian empire in the fourteenth century BC. By the

    reign of Shalmaneser I (1273-1244 BC) at the latest the region had come to be included within the

    core territory of Assyria, a situation which then essentially lasted till the end of the Assyrian empire

    in 612 BC although there may have been occasions, for example during the reign of Aur-resa-ii

    (1133-1115 BC), when this control was lost.

    The Neo-Assyrian period (1000-612 BC) is likely to have been a highpoint in the history of

    Tell Baqrta. It is becoming increasingly clear that settlement of the countryside of Assyria was

    intensified by the importation of colonies of deportees from throughout the empire. Combined with

    the construction of massive hydraulic projects this laid the ground for an explosion in agricultural

    productivity. Consequently Tell Baqrta is likely to have become a wealthy regional centre. However

    this prosperity came to an end at the end of the seventh century BC with the invasion and overthrow

    of the Assyrian empire. What happened next, in the Post-Assyrian period (612-539 BC), is not known

    and will be of extreme interest. Firstly, it is not known for sure to which part of the coalition which

    overthrew Assyria the region of Tell Baqrta was assigned, the Medes or the Babylonians. The latter is

    perhaps more likely but there is no concrete evidence. Secondly, it is not known what happened to the

    population of the region. Were many killed? Were they enslaved? Did they join the invading armies?

    Did they return to their homelands? Did they flee? Eventual elucidation of these questions is one of

    the key questions in Assyrian studies.

    Moving on, one event we do know of, from an entry in the Neo-Babylonian Chronicle, is that

  • 25

    at the outset of his campaign in 547 BC Cyrus crossed the Zab below Erbil. The army must

    consequently have passed within the vicinity of Tell Baqrta. Shortly afterwards, with the conquest of

    Babylonia and the overthrow of the Neo-Babylonian empire, northern Mesopotamia passed into the

    control of the Achaemenid empire (539-330 BC). This unquestionably included the region of Tell

    Baqrta, which was probably part of the province of Erbil. Very likely this was a flourishing province

    but little more is known than that. According to the inscription of Behistun, Darius I chased down and

    impaled the rebel Shitrantakhma (Titrantaechmes) in Erbil so it is not improbable that Tell Baqrta

    may have witnessed some of these hostilities. From the end of the 5th century BC the "Passport of

    Nehtihor", an official permit written on leather in Aramaic, attests to the passage through the region

    of an official of the Persian magnate Arsames. Around the same time Xenophon passed by on his

    famous march up to the sea. Seventy years later, as the Achaemenid Empire in its turn came to an

    end, Guagamela, the decisive battle against Darius III, was fought in the plains northwest of Erbil.

    Once again Tell Baqrta is not so far away and it must have witnessed or participated in these world-

    shaping events.

    It is interesting to give some thought to the population of the region over this great stretch of

    time. We have, as yet, no knowledge of the nature of the population prior to the advent of historical

    sources - this is something upon which genetics might, eventually, cast some light - but as literacy

    dawns over the horizon of prehistory the first ethnic group whom we know to have inhabited the

    region are the Hurrians. This is not to say there were not other groups. There almost certainly were.

    Texts over these millennia relating to the eastern frontiers of Mesopotamia (for instance Ur III

    administrative documents and the Shemshara archives) contain a large number of personal names

    whose linguistic affiliation has not yet been established and it is, in my view, probable that parent

    languages will one be day be recognised and reconstructed for at least some of them. Be that as it

    may, the Hurrians are the earliest definable group for whose presence in the region we currently have

    evidence; followed closely by the Sumerians. After this Babylonians, Assyrians, Mittanni, Arameans,

    Medes, Kurds, Greeks and Persians all played their part in the region. Later on came Arabs, Turks

    and Armenians. All these will have left their mark.

    A final consideration concerns the identification of the site in antiquity. Textual evidence

    relating to the plain of Makhmur is scarce but there are some leads to follow; it may of course be

    hoped that in the fullness of time fieldwork at Tell Baqrta will itself yield material germane to these

    discussions. Nevertheless, according to our present, somewhat scanty knowledge the two principal

    towns believed to have been in the region are Sare and Baqar/Baqarru, the former putatively on the

    Zab at the place (on the northern bank) where the river was crossed by the road from Arrapha to

  • 26

    Erbil, the latter halfway between this point and Erbil31. This location is strikingly close to the

    location of present day Tell Baqrta, The closeness of the names is no less striking. I would therefore

    propose that Tell Baqrta in fact represents the remains of ancient Baqar. Further to this Deller has

    suggested that Baqara is to be equated with Old Babylonian Qabra (Deller 1990), locating it 15-20

    km northwest of Altn Kpr. It must therefore be suggested that Tell Baqrta also equates to ancient

    Qabra. If correct this identification will be of the first importance. Obviously this proposition

    requires further investigation and a more detailed analysis of the textual evidence will form the

    subject of my next communication.

    FutureDirectionsfortheTellNaderandTellBaqrtaProjectKonstantinos Kopanias

    The results of the first excavation season in Tell Nader are very promising. This site could

    produce a complete stratigraphy not only for the Late Neolithic/Chalcolithic, but also for later

    periods (3rd-early 1st mil. B.C.), thus becoming an important reference point for the archaeology of

    the northeastern Mesopotamia. It will also offer a better understanding of the important finds at the

    nearby site Qalinj Agha, which was excavated in the 60s and early 70s, but still remains unpublished

    in corpore32.

    Tell Baqrta is also a very promising site, especially if future finds confirm its identification

    with the town Baqar/Baqarru of the Neo-Assyrian and Qabra of the Old-Babylonian period

    (MacGinnis ibid.).

    The next excavation season is scheduled to take place in August - October 2012. We plan to

    continue the excavation in Tell Nader, refine its stratigraphy and study the finds, but also dig a small

    test trench in Tell Baqrta. A geophysical investigation of both sites is planned for 2013.

    31 Note that the Helsinki Atlas puts Baqarru at Tell Ya'qub: Parpola & Porter 2001, 7. 32 Al-Soof 1966; 1968 ; 1969; al-Soof Es-Siwwani 1967; Hijara 1973; Gut 1996.

  • 27

    CitedWorks

    Akkermans, P.M.M.G. 1988. An Updated Chronology for the Northern Ubaid and Late

    Chalcolithic Periods in Syria: New Evidence from Tell Hammam et-Turkman. Iraq 50: 109-146.

    al-Soof, A. 1966. Short Sounding at Tell Qalinj Agha. Sumer 22/1-2: 77-82. ______. 1968. Distribution of Uruk, Jamdat Nasr and Ninevite V Pottery as Revealed by Field

    Survey Work in Iraq. Iraq 30: 74-86. ______. 1969. Excavations at Tell Qalinj Agha (Erbil). Sumer 25/1-2: 3-42. al-Soof, A. - S. Es-Siwwani 1967. More Soundings at Tell Qalinj Agha (Erbil). Sumer 32/1-2: 69- 75. Ayish, A.H. 1976. "Bassetki Statue with an Old Akkadian Inscription of Naram-Sin of Agade (B.C. 2291-2255)." Sumer 32: 63-75. Barone, R. 1976. Anatomie compare des mammifres domestiques. Paris: Vigot Freres. Bauer, J., R.K. Englund and M. Krebernik 1998. Mesopotamien. Spturuk-Zeit und Frhdynastische Zeit. Orbis biblicus et orientalis 160-1. Freiburg, Schweiz: Universittsverlag, Gttingen, Vandenhoeck und Ruprecht. Beuger, C. 2007. Keramik der sptfrhdynastischen bis sptassyrischen Zeit aus Assur, Eine Bearbeitung unter chronologischen Gesichtspunkten (http://www.diss.fuberlin.de/ diss/receive/FUDISS_thesis_000000003202). Blackman, M.J. 1984. Provenance studies of Middle Eastern obsidian from sites in Highland

    Iran. In Archaeological Chemistry III, edited by J.B. Lambert: 19-50. Advances in Chemistry Series 205. Washington: American Chemical Society.

    Blackman, M.J., R. Badaljan, Z. Kikodze, and P. Kohl. 1998. Chemical characterization of Caucasian obsidian geological sources. In LObsidienne au Proche et Moyen Orient: Du Volcan lOutil, edited by M.-C. Cauvin, A. Gourgaud, B. Gratuze, N. Arnaud, G. Poupeau, J.-L. Poidevin, and C. Chataigner : 205-31. BAR International Series 738. Oxford: Archaeopress.

    Butterlin, P. ed. 2009. A propos de Tepe Gawra, le monde proto-urbain de Msopotamie. Subartu XXIII. Turnhout: Brepols. Campbell, S. 2000. The Burnt House at Arpachiyah: A re-examination. Bulletin of the

    American Schools of Oriental Research 318: 1-40. Carter, T., and V. Kilikoglou. 2007. From reactor to royalty? Aegean and Anatolian obsidians

    from Quartier Mu, Malia (Crete). Journal of Mediterranean Archaeology 20(1): 115-43. Carter, T., G. Poupeau, C. Bressy, and N.J.G. Pearce. 2006. A new programme of obsidian

    characterization at atalhyk, Turkey. Journal of Archaeological Science 33(7): 893-909. Carter, R.A. - G. Philip 2010. Beyond the Ubaid. Transformation and Integration in the Late

    Prehistoric Societies of the Middle East. Papers from The Ubaid Expansion? Cultural Meaning, Identity and the Lead-uo to Urbanism. International Workshop held at Grey College, University of Durham 20-22 April 2006. Studies in Ancient Oriental Civilization 63. Chicago: The Oriental Institute of the University of Chicago.

    Charpin, D. 2004. "Chroniques bibliographiques 3. Donnes nouvelles sur la rgion du Petit Zab au XVIIIe sicle." RA 98: 151-78. Charpin, D., O. Edzard, and M. Stol. 2004. Mesopotamien. Die altbabylonische Zeit. Orbis Biblicus

    et Orientalis 160/4. Gttingen: Universittsverlag, Gttingen, Vandenhoeck und Ruprecht. Chataigner, C. 1994. Les proprits gochimiques des obsidiennes et la distinction des sources

    de Bingl et Nemrut Da. Palorient 20(2): 9-17. ______. 1998. Sources des artefacts nolithiques. In LObsidienne au Proche et Moyen Orient:

  • 28

    Du Volcan lOutil, edited by M.-C. Cauvin, A. Gourgaud, B. Gratuze, N. Arnaud, G. Poupeau, J.-L. Poidevin, and C. Chataigner: 273-324. BAR International Series 738. Oxford: Archaeopress.

    Chataigner, C., R. Badalian, G. Bigazzi, M.-C. Cauvin, R. Jrbashian, S.G. Karapetian, P. Norelli, M. Oddone, and J.-L. Poidevin. 2003. Provenance studies of obsidian artefacts from Armenian archaeological sites using the fission-track dating method. Journal of Non-Crystalline Solids 323: 167-71.

    Cherry, J.F., E.Z. Faro, and L. Minc. 2010. Field survey and geochemical characterization of the South Armenian obsidian sources. Journal of Field Archaeology 35(2): 147-63. Deller, K.-H., 1990/3. "Eine Erwgung zur Lokalisierung des aB ON Qabr/Qabar." NABU 84: 62-

    3. Eidem, J. 1992. The Shemshara Archives 2: The Administrative Texts. Copenhagen: Det Kongelige

    Danske videnskabernes selskab. El Amin, M., and M. Mallowan. 1949. "Soundings in the Makhmur Plain, Part 1." Sumer 5: 145-53. ______. 1950. "Soundings in the Makhmur Plain, Part 2." Sumer 6: 55-89. Ess, M. van 2006. Gefe mit Hohlmaangabe aus Mesopotamien? Baghdader Mitteilungen 37:

    69-90. Finkelstein, J.J. 1953. "Cuneiform Texts from Tell Billah." JCS 7: 111-76. Fornaseri, M., L. Malpieri, A.M. Palmieri, and A. Taddeucci. 1975-77. Analysis of

    obsidians from the Late Chalcolithic levels of Arslantepe (Malatya). Palorient 3: 231-46. Frahm, E. 2010. The Bronze-Age Obsidian Industry at Tell Mozan (Ancient Urkesh), Syria:

    Redeveloping Electron Microprobe Analysis for 21st-Century Sourcing Research and the Implications for Obsidian Use and Exchange in Northern Mesopotamia after the Neolithic. Unpublished PhD thesis, Department of Anthropology, University of Minnesota.

    Frahm, E. Forthcoming (a). Distinguishing Nemrut Da and Bingl A obsidians: geochemical and landscape differences and the archaeological implications. Journal of Archaeological Science [2012].

    Frahm, E. Forthcoming (b). Non-destructive sourcing of Bronze Age Near Eastern obsidian artefacts: Redeveloping and reassessing electron microprobe analysis for obsidian sourcing. Archaeometry [2012].

    Furlarni, G. 1934. "Sarcofaghi partici de Kakzu." Iraq 1: 90-4. Glassner, J.-J. 1993. Chroniques msopotamiennes. Paris: Les Belles Lettres. Gut, R. 1995. Das prhistorische Ninive. Zur relativen Chronologie der frhen Perioden Nordmesopotamiens. Baghdader Forschungen 19. Mainz: von Zabern. ______. 1969. Zur Datierung der Proto-Ninive 5-Ware von Qalinj Agha. Baghdader Mitteilungen 27: 1-12. Halstead, P. 2011. The faunal remains. In The Early Bronze Age Village on Tsoungiza Hill, edited

    by D. J. Pullen: 741-800. Princeton: American School of Classical Studies at Athens. Hammade, H. - Y. Yamazaki 2006. Tell al-Abr (Syria). Ubaid and Uruk Periods. Association pour

    la Promotion de l'Histoire et de l'Archologie Orientales. Mmoires 4. Louvain: Peeters. Healey, E. 2010. Ubaid lithics revisited: Their significance for the interpretation of Ubaid

    Society. In Carter and Phillip 2010, 163-81. Henrickson, E.F. - I. Thuesen eds. 1989. Upon this Foundation The Ubaid Reconsidered. Proceedings from the ubaid Symposium Elsinore, May 30th-June 1st 1988. Copenhagen: University of Copenhagen/Museum Tusculanum Press. Hijara, I. 1973. Excavations at Tell Qalinj Agha (Erbil), 4th Season.: Sumer 29:13-35. Hirth, K.G. 1978. Inter-regional trade and the formation of prehistoric gateway communities.

    American Antiquity 43: 25-45. Hole, F. 1989. Patterns of Burial in the Fifth Millennium. In Henrickson Thuesen

    1989, 149-180.

  • 29

    Hours, F., O. Aurenche, J. Cauvin, M.-C. Cauvin, L. Copeland, and P. Sanlaville. 1994. Atlas des Sites du Proche Orient (14.000-5.700 BP). Lyon: Travaux de la Maison de lOrient.

    Hubbard, N.L. 1980. Halafian Agriculture and Environment at Arpachiyah. Iraq 42(2):153-154.

    Ismail, B.K., and A. Cavigneaux. 2003. "Dduas Siegesstele IM 95200 aus Enunna. Die Inschrift." BaM 34: 129-56.

    Jasim, S.A. 1985. The Ubaid Period in Iraq. Recent Excavations in the Hamrin region. BAR 267 (i). Oxford: BAR International Series.

    Khalidi, L., B. Gratuze, and S. Boucetta. 2009. Provenance of obsidian excavated from Late Chalcolithic levels at the sites of Tell Hamoukar and Tell Brak, Syria. Archaeometry 51(6): 879-93.

    Levine, L.D. 1989. "K.4675+. The Zamua Itinerary." SAAB 3: 75-92. MacGinnis, J.D.A. 2012. Erbil in the Cuneiform Sources. Erbil. Mahdavi, A. and C. Bovington. 1972. Neutron activation analysis of some obsidian samples from geological and archaeological sites. Iran 10: 148-51. Mallowan, M.E.L., and J.C. Rose. 1935. Excavations at Tell Arpachiyah, 1933. Iraq 2: 1-178. Mallowan, M.E.L. - J.C. Rose 1935. Prehistoric Assyria. The Excavations at Tall Arpachiyah 1933.

    London: Oxford University Press. Matthews, D.M. (ed.) 2003: Excavations at Tell Brak - Vol. 4: Exploring an Upper Mesopotamian

    Regional Centre, 1994-1996. London : British School of Archaeology in Iraq/Cambridge : McDonald Institute for Archaeological Research.

    Miglus, P. 2003. "Die Siegesstele des Knigs Dduas von Enunna und ihre Stellung in der Kunst Mesopotamien und der Nachbargebiete." AOAT 306: 397-420.

    Niknami, K.A., A.C. Amirkhiz, and M.D. Glascock. 2010. Provenance studies of Chalcolithic obsidian artefacts from near Lake Urmia, Northwestern Iran using WDXRF analysis. Archaeometry 52(1): 19-30.

    Oates, D. 1968. Studies in the Ancient History of Northern Iraq. London: Oxford University Press. Oates, J. 1969. Choga Mami 1967-68: A Preliminary Report. Iraq 31: 115-152. Oates, D. - J. Oates 1976. The Rise of Civilization. Oxford: Elsevier-Phaidon. Pales, L. and Garcia, M. 1981. Atlas ostologique pour servir lidentification des mammifres du

    Quaternaire. Paris: CNRS. Parker, B. 1961. "Administrative Tablets from the North-west Palace, Nimrud." Iraq 23: 15-67. Parpola. S., and M. Porter. 2001. The Helsinki Atlas of the Near East in the Neo-Assyrian Period.

    Helsinki: Casco Bay Assyriological Institute. Peasnall, B.L. 2002. Burials from Tepe Gawra, Levels VIII to XIA/B. In Rothmann 2002, 171-

    254. Poidevin, J.-L. 1998. Les gisements dobsidienne de Turquie et de Transcaucasie: gologie,

    gochimie et chronomtrie. In LObsidienne au Proche et Moyen Orient: Du Volcan lOutil, edited by M.-C. Cauvin, A. Gourgaud, B. Gratuze, N. Arnaud, G. Poupeau, J.-L. Poidevin, and C. Chataigner: 105-203. BAR International Series 738. Oxford: Archaeopress.

    Pollard, M.A., and C. Heron. 2008. Archaeological Chemistry. Cambridge: RSC Publishing. Poupeau, G., F.-X. Le Bourdonnec, T. Carter, S. Delerue, M.S. Shackley, J.A. Barrat,

    S. Dubernet, P. Moretto, T. Calligaro, M. Mili, and K. Kobayashi. 2010. The use of SEM-EDS, PIXE and EDXRF for obsidian provenance studies in the Near East: A case study from Neolithic atalhyk (central Anatolia). Journal of Archaeological Science 37(11): 2705-20.

    Reed, C. A. 1958. Observations on the burrowing rodent Spalax in Iraq. Journal of Mammalogy 39 (3): 386-389.

    Renfrew, C., J.E. Dixon, and J.R. Cann. 1966. Obsidian and early culture contact in the Near East. Proceedings of the Prehistoric Society 32: 30-72.

  • 30

    Renfrew, C. 1977. The later obsidian of Deh Luran the evidence of Chagha Sefid. In Studies of the Archaeological History of the Deh Luran Plain: The Excavation of Chagha Sefid, edited by F. Hole: 289-311. Ann Arbor: Museum of Anthropology, University of Michigan.

    Rothman, M.S. 2002. The Evolution of a small, prehistoric center in northern Iraq. University Museum Monograph 112. Philadelphia: University of Philadelphia.

    Schmidt, J. 1972. XXVI. und XXVII. vorlufiger Bericht ber die von dem Deutschen Archologischen Institut und der Deutschen Orient-Gesellschaft unternommenen Ausgrabungen in Uruk-Warka. 1968 und 1969. Abhandlungen der Deutschen Orient-Gesellschaft 16. Berlin: Gebr. Mann Verlag.

    Schmid, E. 1972. Atlas of animal bones. New York: Elsevier. Shackley, M.S. 2005. Obsidian: Geology and Archaeology in the North American Southwest.

    Tucson: University of Arizona Press. Speiser, E.A. 1935. Excavations at Tepe Gawra. vol I: Levels I-VIII. Philadelphia: University of

    Pennsylvania Press. Tenu, A. 2009. L'expansion mdio-assyrienne: Approche archologique. BAR International Series

    1906. Oxford: Hadrian Books. Tobler, A.J. 1950. Excavations at Tepe Gawra. Vol. II: Levels IX-XX. Museum Monographs 4.

    Philadelphia: University of Pennsylvania Press, London: Oxford University Press.

    Wrede, N. 2003. Uruk. Terrakotten I. Von der Ubaid- bis zur altbabylonischen Zeit. Ausgrabungen in Uruk-Warka - Endberichte 25. Mainz am Rhein: Verlag Philipp

    von Zabern. Wright, G.A., and A.A. Gordus. 1969. Distribution and utilization of obsidian from Lake Van

    sources between 7500 and 3500 B.C. AJA 73(1): 75-7.

  • 31

    Appendix

    List of members of the archaeological research team Dr. Konstantinos Kopanias Principal director of the Archaeological Mission

    Lecturer for Prehistoric Archaeology, University of Athens, Greece

    Dr. Claudia Beuger Pottery Lecturer for Near Eastern Archaeology, University of Halle-Wittenberg, Germany

    Dr. Amy Bogaard Archaeobotany Lecturer in Neolithic and Bronze Age Archaeology, University of Oxford, UK

    Dr. Tristan Carter Obsidian analysis Assistant Professor, McMaster University, Canada

    Dr. Mike Charles Archaeobotany Reader in Environmental Archaeology, University of Sheffield, UK

    Dr. Sherry Fox Human Remains Director of the Wiener Laboratory of the American School of Classical Studies at Athens, Greece

    Dr. Angelos Hadjikoumis Animal Bones Researcher, University of Sheffield, UK

    Dr. Paul Halstead Animal Bones Professor of Archaeology, University of Sheffield, UK

    Dr. Chrysanthos Kanellopoulos

    Architecture Lecturer for Classical Archaeology, University of Athens, Greece

    Dr. Lilian Karali Shells Professor for Environmental Archaeology, University of Athens, Greece

    Dr. Georgia Kourtesi-Philippaki

    Lithics Assistant Professor for Prehistoric Archaeology, University of Athens, Greece

    Dr. Alexandra Livarda Archaeobotany Lecturer in Archaeobotany, University of Nottingham, UK

  • 32

    Dr. John MacGinnis Assyrian Inscriptions

    Research Fellow, University of Cambridge, UK

    Dr. Eva Panagitakopoulou Insects Lecturer in Palaeoecology, University of Edinburgh, UK

    Michel Roggenbucke Senior Conservator Department of History and Archaeology, University of Athens, Greece

    Maria Koutsoumpou Excavation Assistant 21th Ephorate of Prehistoric and Classical Antiquities, Greece

    Katerina Glaraki Excavation Assistant M.A. Student, University of Athens, Greece

    Eva Karantoni Excavation Assistant B.A. Student, University of Athens, Greece

    George Mavronanos Excavation Assistant B.A. Student, University of Athens, Greece

    ntonis Papadopoulos Excavation Assistant B.A. Student, University of Athens, Greece

    Phoivos Michos-Rammos Inventory of Lithics B.A. Student, University of Athens, Greece

    List of members of the historical research team Dr. Konstantinos Bourazelis

    Advisor of the Historical Team Professor for Ancient History, University of Athens, Greece

    Dr. Konstantinos Kopanias

    Project Coordinator Lecturer for Prehistoric Archaeology, University of Athens

    Dr. Athanasios Sideris Survey Director of the Archaeological Department of the Foundation of the Hellenic World, Greece

    Kleanthis Zouboulakis Survey Ph.D. Student, University of Athens, Greece

    Dr. Sophia Aneziri Inscriptions Assistant Professor for Ancient History, University of Athens, Greece

    Dr. Selini Psoma Coins Assistant Professor for Ancient History, University of Athens

  • Fig. 1: Tell Nader an