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130

Transition to Settled Life

on average, was used to produce 69 per cent of the total lithic assemblage. Even so, the main concentration of Arteni obsidian was found at the northern sites (Aratashen,Ada Blur, Mashtots Blur, and Masis Blur), with villages in the south-eastern area of the Ararat Plain preferring Gutansar and Hatis obsidian. Most of the obsidian in Georgia derives from the Chikiani source, except in the case of the Alazani valley, where communities also exploited Armenian sources.Analyses have also shown that the inhabitants of Alikemek Tepesi used Kelbadzhar obsidian from some 300 km away.

This pattern changed during the Early Bronze Age. Hatis obsidian was increasingly exploited by villagers in the Ararat Plain, with a commensurate drop in the utilisation of the Arteni. In the southern part of the Ararat Plain, however, the picture is more varied, with communities acquiring obsidian from Geghasar as well. In the Shirak Plateau,Arteni remained the main source overall and amongst the southern sites, although at the northern site of Keti villagers obtained most of their obsidian (66.7 per cent) from the unidentified TCUNK 1 source.136 About 2,000 years later, in the early Iron Age, Arteni obsidian is the predominant type across the Shirak region.The sites of Berdshen (settlement) and Verin Naver (cemetery), situated no more than 4 km from each other, clearly reveal that sites in close proximity did not necessarily share similar resources.The deceased were buried atVerin Naver with tools primarily knapped from Arteni obsidian (40 per cent), whereas the Berdshen villagers exploited the Damlik and Ttvakar sources from the Tsaghkuniats volcano. On the fringes of Lake Sevan, inhabitants of sites preferred sources along the Gegham ridge.

CONCLUSION

A feature of the Neolithic of the Caucasus is the careful siting of settlements to take advantage of soils for cultivation and grazing.With no apparent local antecedents, the agrarian groups of the Kura-Araxes interfluve reflect their Near Eastern origins – they built mud-brick or pisé architecture, they cultivated domesticated cereals and practised animal husbandry, and they manufactured a range of tools – such as ground stone objects – that are commonly associated with farming communities.Although these pioneers have long been viewed as immigrants from further south, in northern Mesopotamia or Iran, the degree to which they might have interacted with the indigenous Late Mesolithic communities is a matter for future research to determine. Likewise, the discussion of the Pre-Pottery Neolithic must await more detailed evidence.

Evidence for interconnectivity in the Late Neolithic periods is growing. The interplay that existed in Anatolia between the polities south of the Taurus Mountains and settlements located along the Turkish Upper Euphrates and its

136 Badalyan 2010: 31.

Conclusion

131

tributaries is well known.137 It is quite likely that the southern Caucasus was drawn into this network of trade and interaction, even though the nature of the interaction has yet to be determined. In Upper Mesopotamia, craft production flourished to satisfy the demands of an emerging elite. Long-distance trade networks and a formative organisational system, reflected in the use of seals, were established to cope with the demand for raw materials.These systems were by no means as uniform and intensive as those that were to appear later in the Uruk period, but they were nonetheless far-flung.To what extent the southern Caucasus was part of this network is not clear.Although present evidence does not indicate that Armenian obsidian travelled to distant lands, its rich sources were a desirable target for communities in the immediate environs.We can say that contact between Anatolia and the south Caucasus would not have crossed over the highlands of north-eastern Anatolia, because there is a singular lack of evidence along that route, but instead people followed the arc of theTaurus Mountains and then turned northwards towards Armenia and Azerbaijan.The earliest firm link with surrounding regions is represented by fragments of unequivocally Halaf pottery.

Conceptually, these south Caucasian Neolithic settlements call to mind the ‘keyhole plan’ of the Middle Halaf, leading some to conjecture a northern origin for the Upper Mesopotamian round house tradition.138 The eventual evolution from round to rectilinear houses is significant because it is not simply one of shape and design, but the change also underpins shifting social behaviour and altered economic structures.At its core are different approaches to risk management. Initially, each individual in the Neolithic south Caucasus probably had a round hut, and preferred to share food and store commodities in a communal area; as a community, they shouldered rewards and risks together. Rectilinear dwellings that were already in use in Anatolia, on the other hand, focused on the nuclear family within a closed house plan and private storage facilities were the norm.

137Sagona and Zimansky 2009: 125–7; Castro Gessner 2011.

138Dzhavakhishvili 1973; Mellaart 1975: 203.

CHAPTER 4

FAR - FLUNG NETWORKS : THE CHALCOLITHIC (50 0 0/ 48 0 0 – 350 0 BC)

Two decades or so ago, the Chalcolithic period in the Caucasus was difficult to grasp. It was an elusive period, characterised by fuzzy concepts, multiple traditions,and an array of patchy evidence weakly glued together by a small number of radiocarbon readings.Added to this were some striking differences in character between the northern and southern Caucasus sequences.1 To the south of the Caucasus ridge, regional expressions, represented mostly by settlements, chronologically sandwiched between the earliest farming communities and the appearance of the well-known Kura-Araxes complex, were ‘fl at-planed’ into a segment of time with little sense of connectivity. Our understanding of the northern Caucasus and its spectacular Maikop culture fared little better. In contrast to southern Caucasia, the drainage basin of the Kuban and Terek rivers, the heartland of Maikop culture province, was represented through scores of tomb assemblages that overshadowed the importance of its typically shallow and indistinct settlements. This combination of a tomb-dominated northern Caucasus and a settlement-focused southern region resulted in a vacillating and uncertain chronology.

Regional perspectives further complicated the dilemma: should the northern Caucasus be coupled primarily to the Near East, or to Eastern Europe? We are still grappling with this quandary that sets arguments in favour of art historical connections with the literate societies in Mesopotamia against presumed parallels with the Russian steppes. Soviet archaeologists referred to this stretch of fifteen centuries or more in the Caucasus as the Aeneolithic or Eneolithic period, a term still widely used in south-eastern Europe to denote a period when copper metallurgy was adopted by cultures essentially Neolithic

1For regional overviews of this prehistoric interlude, referred to by some as Chalcolithic and by others as the Early Bronze Age, see Munchaev 1982, 1994b; Chataigner 1995; Ivanova 2013: 50–129;Wilkinson 2014a.

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133

in character.Terminology remains a problem, with the Maikop culture often attributed to the Early Bronze Age. I have assigned Maikop to the Chalcolithic because its oft-cited links to north-eastern Mesopotamia and neighbouring lands belong to Chalcolithic sequences of those regions. To do otherwise would put it radically out of kilter.

A burgeoning quantity of precise information from both sides of the Caucasus is showing us that this Chalcolithic interlude is far more complex than had formerly been appreciated. Trustworthy contexts accompanied by absolute readings have initiated a paradigm shift in our thinking. In terms of chronology, we now have a skeletal framework, which has placed the region’s far-reaching and salient dynamics into a more coherent picture. It now appears that communities in the Caucasus during the late fifth and fourth millennia BC were involved in the subtle interplay of cultural stimuli that served, at one time or another, to create conditions favourable for development on an impressive scale. Following sporadic and subdued foreign contacts during the south Caucasian Neolithic, social and economic networks emerged that stretched from the Kuban region and south-eastern Caucasia across the highlands of eastern Anatolia and southwards, over the Taurus Mountains, into the north Mesopotamian Plain. The long arm of communication even stretched far into central Asia.These new data have also opened our eyes to a metallurgical precociousness and distinctiveness that is still only partially understood.

There is a general consensus that the Chalcolithic in the southern Caucasus can be split into two broad phases: early (5000/4800–4000 BC) and late (4000– 3500 BC).2 In the northern Caucasus, the early phase is roughly comparable to the pre-Maikop Early Chalcolithic period, whereas the late phase is coeval with the Maikop Culture, which when coupled with its late (Novosvobodnaia) phase extends even further to about 2800 BC.3

Three broad and distinctly different cultural traditions define the Chalcolithic (Figures 4.1 and 4.2). Two are local and derive from late Neolithic groups, while one was clearly shaped by intrusive influences. From north to south the traditions are as follows:

•The Maikop culture: known also as the Maikop-Novosvobodnaia CultureHistorical Community, emphasising its two developmental stages, this dominant northern Caucasian tradition is an indigenous cultural expression with far-flung connections. Known mostly from tomb assemblages, some exceptionally wealthy, its phases are yet to be articulated precisely. Recent radiocarbon dates have gone some way in defining an absolute chronology for the Maikop phase that stretched across much of

2 Kiguradze 2000; Lyonnet 2007a.

3Korenevskii 2004; Ivanova 2007; Chernykh 2011; Rezepkin 2012; Kohl and Trifonov 2014. Lyonnet (2007) assigns an end date of 2600 BC for the developed Novosvobodnaia phase.

134

N

Black Sea

 

River

Halys

Arslantepe

 

 

Malatya

 

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u

 

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Amuq

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a

 

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Krasnodar

 

River

 

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Kislovodsk

Sokhumi

Caspian

 

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Kura

 

Tbilisi

 

Chobareti

Chalcolithic

Sioni

Maikop

Chaff Ware

Dolmen

Archaeological site Modern city

 

Yerevan

Lake

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Erzurum

 

 

Sevan

 

 

 

Araxes

River

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Murat

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Van

 

Tabriz

 

 

 

Tigris

 

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Urmia

 

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Mosul

Baku

0100 km

Figure 4.1. Map showing the cultural boundaries of the Maikop, Chaff-Faced Ware, and the Sioni traditions.The dolmen area shows its relationship with Maikop, even though many dolmens were constructed after Maikop (drawn by C. Jayasuriya).

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Sioni tradition

32Kviriatskali

33Damisvari Gora

34Sioni

35Tospi

36Sos Höyük

37Sarıgül

38Cetenli

 

Chaff tradition

 

39

Berikldeebi

 

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Kavtiskhevi

 

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Boyuk Kesik

 

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Mentesh Tepe

 

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Leila Tepe

 

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Alikemek

 

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Ovçular Tepe

 

46

Hanago

 

47

Colpan

 

48

As Tepe

 

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Uzub Tepe

Halys

50

Kultepe

51

Baruj Tepe

 

52

Basmandj

 

53

Qara Buru Tepe

 

54

Geoy Tepe

 

55

Kalecik

 

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Hasan Abad

 

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Gol Tepe

 

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Tastepe

 

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Sa'in Qaleh

 

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Kuma

 

 

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Murat

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Van

 

 

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Tigris

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0100 km

Maikop tradition

Burial

Settlement

1 Poluostrov Fontan

2 Sennaia

3 Temriuk

4 Rassvet

5 Raevskaia

6 Diurso 1

7 Obshchestvennoe 2

8 Timashevskaia

9 Baturinskaia

10Staromyshastovskaia

11Psekupekoe

12Chishkho

13Pshish

14Svobodnoe

15Novolabinskaia

16Temizbbekskaia

17Sereginskoe

18Maikop (BMK)

19Lasenova Poliana

20Novosvobodnaia (Klady)

21Meshoko

22Ust’-Dzheguta

23Vorovskolesskaia

24Ipatovo

25Kisloslovodsk

26Chograi ı

27Nal’chik

28Myshtulagtylagat

29Sunzha

30Galiugai ı-6

31Bachi-Iurt

Figure 4.2. Map showing the key sites of the Maikop, Sioni and Chaff-Faced traditions (drawn by C. Jayasuriya).

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Far-Flung Networks

the fourth millennium BC (ca. 3800–3000 cal BC). Novosvobodnaia dolmens, on the other hand, straddle the fourth–third millennia (3300–2800 cal BC). This places them at the tail end of the Maikop, while also overlapping with the beginning of west Caucasian dolmens (Chapter 6).4 The pre-Maikop phase is represented by a handful of sites, including Nal’chik and Meshoko, that belong mostly to the second half of the fifth and the early fourth millennia BC.

•Chaff -Faced Ware horizon: well known in Syro-Mesopotamia as Amuq F, this tradition has been found in a considerable number of locations in the southern part of south Caucasia. In Azerbaijan, the Chaff-Faced Ware horizon is referred to as the ‘Leilatepe culture’, which is not an exact mirror image of its Syro-Mesopotamian counterpart. South of the Taurus Mountains, this horizon, comprised of mostly coarse wares, has been placed in the first half of the fourth millennium BC. Chronometric dates from the southern Caucasus generally concur with these dates, though it has been argued that the Azerbaijani sequences may point to an even slightly earlier origin.5

•The Sioni horizon: this local south Caucasian tradition is the most prob-

lematic. We do not have as yet a single clearly articulated settlement – its namesake, located in Georgia, is badly disturbed by later Bronze Age activity. Despite imprecise data, we can track its material culture, mostly pottery, in regions beyond the boundaries of Neolithic occupation.‘Sioni’ ceramics are found mostly in the south-eastern Caucasus – eastern Georgia, Armenia, and Azerbaijan – and on the Iranian side of the middle Araxes Valley, as well as in easternmost Anatolia.6 Its stone tool technology differs from the Neolithic tradition, too, but has yet to be studied in any detail.A few recent absolute dates and loose typologies help bracket this elusive horizon within the fifth through mid-fourth millennia cal BC, though its beginning date is quite blurry: early phase (5000–4000 BC) and late phase (4000–3500 BC).

With this mix of indigenous and foreign communities, northern and southern elements, many questions spring to mind. What was the nature of cultural interaction at this time across the Caucasian ridge, and how intense was the level of communication? Does the apparent hybridity that certain material

4 Trifonov et al. 2014.

5 Marro 2010.

6Sagona 2014a. For an earlier and now outdated summation with copious illustrations, see Kiguradze and Sagona 2003.The Sioni tradition has occasionally been nuanced even further, largely on the basis of ceramic typology. For instance, it is sometimes split to create a sub-group termed ‘Tsopi-Ginchi’ (Chikovani 1999; Chikovani et al. 2010: 95), a division that does not seem warranted at this stage.