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  • 7/30/2019 Ch5 Paul Halstead

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    Paul Halstead38

    5. Resettling the Neolithic: faunal evidence forseasons of consumption and residence at Neolithic

    sites in Greece

    Paul Halstead

    Introduction

    Had Eric Higgs lived to see the new millennium, it seems

    unlikely that the works of Julian Thomas or Alasdair

    Whittle would have been preferred reading at his Panton

    Street lair in Cambridge. And yet, on one issue, the

    palaeoeconomists of the 1970s and early 1980s could

    happily have made common cause with those who have

    sought to rethink the Neolithic in the 1990s; both groups

    emphasised the need to dismantle the traditional package

    of Neolithic material culture, farming and sedentism (e.g.

    Barker 1975; Dennell 1983; Jarman et al. 1982; Thomas

    1996; Whittle 1996a). Moreover, despite radical diff-

    erences of agenda, both groups stressed the heterogeneity

    of the European Neolithic and the desirability of

    exploring this variability in its local and regional context.

    Nonetheless, both groups have at times perhaps been

    over-zealous in their enthusiasm for discarding the

    traditional model without due attention to the local and

    regional archaeological record. At worst, the traditional

    model of a Neolithic package has been supplanted by a

    more fashionable, but equally unfounded, pan-European

    orthodoxy of gradual and piecemeal adoption ofdomesticates, sedentary life and Neolithic material

    culture.

    This chapter focuses on one particular aspect of the

    Neolithic package sedentism which is explored in

    the context of the archaeological record from what is

    today Greece. Though a rather arbitrary geographical

    unit for the Neolithic, Greece is large enough to

    encompass a range of site types of diverse date and in a

    variety of ecological settings; yet it is small enough for a

    short paper to do reasonable justice to the available

    evidence. True to the critical spirit and contextual

    sensitivities of both the palaeoeconomists and more recent

    writers on the Neolithic, it is not claimed that the results

    of this study can be extrapolated to the rest of Europe; on

    the contrary, similar empirical studies are needed for

    other areas.

    The basic argument advanced here is that the Neolithic

    of Greece is in need of resettling rather than unsettling.

    As Whittle has noted, recent discussion of Neolithic

    (im)mobility has embraced a range of temporal and

    spatial scales, ranging from seasonal to generational and

    from local to regional (Whittle 1997). Arguably, much

    recent discussion of Neolithic mobility has been muddied

    by the conflation of very different analytical scales. Beforeproceeding to argue for a largely sedentary Greek

    Neolithic, therefore, some clarification is offered as to

    the terms in which sedentism is understood here.

    Sedentism

    The primary focus of this study is on whether individual

    sites were occupied year-round or only seasonally.

    Sedentism or mobility on this time scale is a central issue

    for any attempt to explore the economic, demographic,

    social or ideological strategies of Neolithic populations.

    It is clear from ethnographic counter-examples that

    neither agriculture nor the storage of agricultural productsnecessarily ties farmers to a fixed residence. On the other

    hand, the duration and timing, as well as scale, of

    habitation in a given locality plainly constrain the range

    of viable subsistence strategies. The distinction between

    year-round and seasonal habitation may be crucial,

    therefore, in modelling Neolithic subsistence activity,

    even at the fundamental level of relative dependence on

    cultivation, animal husbandry and foraging (e.g. for the

    Neolithic of Greece: Halstead 1989). The degree of

    permanence of residence exercises an equally powerful

    influence on the nature of social interaction. While

    seasonal mobility offers a valuable safety valve for conflict

    resolution within local residential groups, year-round co-

    residence demands more active measures to maintain

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    Resettling the Neolithic: faunal evidence from Neolithic sites in Greece 39

    harmony. And, while seasonal mobility may present

    embedded opportunities for socialisation on a regional

    scale, year-round sedentism may require strategies for

    maintaining the inter-group relationships essential for

    biological and social reproduction. Likewise, sedentary

    and mobile populations are likely to have perceived thecultural landscapes that they inhabited in quite different

    terms, with far-reaching implications for resource use

    and ownership, for the nature of social relationships

    within and between local groups, and for cosmology (e.g.

    Barrett 1994; Chapman 1997; Edmonds 1999; Kotsakis

    1999; Whittle 1996b).

    It must be emphasised, however, that sedentism, in

    the sense of year-round residence, does not preclude a

    significant degree of mobility. For any Neolithic habit-

    ation site, it is assumed here that, at minimum:

    on a more or less daily basis, most inhabitants will

    have ranged off-site (within a site catchment of up to,say, one hours walk) to work fields or gardens, gather

    food and fuel, collect water, graze livestock, and so

    on;

    on a seasonal basis, at least some inhabitants will

    have ranged several hours from the site, possibly

    involving overnight absence, in pursuit of game, fruits,

    raw materials, information, and so on;

    on a seasonal or inter-annual basis, some inhabitants

    will have visited neighbouring or more distant sites,

    variously to escape conflict at home, to acquire

    resources not available locally or to socialise with kin,

    friends and exchange partners;

    on an inter-annual or generational time scale,individuals or groups of inhabitants will have taken

    up long-term residence at different sites as a result of

    exogamy, conflict and fission, or subsistence failure;

    on a generational or longer time scale, some sites

    will have been abandoned, temporarily or permanently,

    as a consequence of conflict, disease, subsistence

    failure, environmental degradation, ritual contamina-

    tion, and so on.

    It is worth noting that mobility on these temporal and

    spatial scales is probably characteristic of all modern

    Greek villages (e.g. du Boulay 1974; Karakasidou 1997;

    Sutton 2000), the majority of which would be classifiedby most Neolithic specialists as unambiguously sedentary.

    Methodological considerations

    The extent to which habitation at Neolithic sites in Greece

    was seasonal or year-round is explored here primarily

    through faunal evidence for season of death of domestic

    animals. In practice, the analysis concentrates on

    domestic animals dying in their first year or so of life, as

    only such young remains can be aged with sufficient

    accuracy to shed much light on season of death. Because

    of the relative scarcity of young cattle remains (and, even

    more so, of wild animals), the following analysis focuses

    on sheep, goats and pigs.

    In assessing age at death, neonatal postcranial

    remains, recognisable by their distinctive surface texture

    and internal structure as well as size and gross mor-

    phology (e.g. Prummel 1987), are assumed to represent

    animals dying within one month or so of birth. Otherwise,

    assessment of age at death is based solely on eruption andwear of mandibular cheek teeth, information on which is

    available in varying detail for different sites. Both timing

    of eruption and speed of wear are subject to some

    variability. For goats and sheep, ages are assigned to

    successive stages of dental eruption and wear following

    the studies of a range of herds/flocks by Deniz and Payne

    (1982) and Jones (in press) respectively, in each case

    adopting age ranges which encompass 95% of cases. In

    the case of pigs, for which such precise information is

    not available, ages are assigned to successive stages of

    dental development following Higham (1967).

    Interpretation of these age data in terms of season(s)of death entails assumptions about the timing of lambing/

    kidding and farrowing. The peak lambing/kidding period

    in recent, unimproved sheep and goats fell during

    January-February in lowland northern Greece and a

    month or so earlier in lowland southern Greece (Halstead

    field notes). In the last few decades, herders have

    increasingly manipulated the timing of births, usually to

    take advantage of seasonal market conditions, by

    improving feeding and housing (so that females come

    into oestrus earlier) and by restricting the movements of

    breeding males. Despite archaeobotanical evidence that

    fodder was provided for livestock at Neolithic sites in

    northern Greece (Valamoti 2004), the decreasing statureof domestic animals through the course of the Neolithic,

    in Greece (e.g. von den Driesch 1987) as elsewhere,

    argues against intensive feeding on a scale sufficient to

    neutralise natural seasonal influences on the timing of

    births. Farrowing dates seem to have been rather variable

    in recent, unimproved pigs, not least because sows

    sometimes produced two litters per year (or five litters in

    three years), but there is evidence for a single farrowing

    season in one of the faunal assemblages discussed below.

    Among extensively herded pigs in woodland in northern

    Greece, the main farrowing season falls rather later than

    the peak lambing and kidding period (Halstead fieldnotes) and, given the role of the autumn glut of acorns in

    bringing pigs to peak nutritional condition and the nearly

    four-month duration of gestation, this may plausibly be

    taken as the norm for Neolithic Greece. Thus farrowing

    is assumed here to have taken place in March-April, in

    northern Greece, and in February-March, in the south. It

    must be acknowledged that such normative birth seasons

    only represent the central tendency in lambing, kidding

    and farrowing times; for a variety of reasons, some earlier

    and later births are inevitable. For the sake of simplicity,

    however, it is provisionally assumed that the faunal

    evidence reviewed is largely derived from births during

    the peak season. For the same reason, although slightly

    earlier birth dates have been assumed here for southern

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    Paul Halstead40

    than for northern Greece, a common definition is used

    for the four seasons: winter December to February,

    spring March to May, summer June to August, and

    autumn September to November.

    Interpretation of evidence for the timing of animal

    deaths in terms of season(s) of human habitation assumesthat the remains of young domesticates represent animals

    killed on-site, or introduced soon after death, rather than

    the delayed transport of preserved body parts between

    sites. This assumption seems secure, not least because

    analysis here focuses on the mandible, which is of modest

    meat utility (Binford 1978) and so unlikely to have been

    curated and transported between sites on a significant

    scale. Whether or not faunal evidence of human activity

    in all seasons of the year indicates year-round occupation

    (rather than complementary seasonal activities in

    different years) is discussed towards the end of this

    chapter. Two factors should be noted, however, thatmilitate against demonstrating activity at a given site in

    every season.

    First, the combination of a two-month birth period

    and of variability in dental development ensures that

    much of the mandibular evidence, that forms the core of

    the following analysis, could potentially be assigned to a

    range of seasons (cf. OConnor 1998). To reduce the risk

    of imprecisely aged specimens creating a spurious picture

    of occupation in all seasons, an assessment is initially

    made below of the minimum season(s) represented by the

    evidence from each site. For example, if neonatal remains

    of sheep/goats clearly indicate late winter deaths, first-

    year sheep mandibles aged more broadly to late winter-early summer and to autumn-winter may both be

    attributed to late winter. This procedure thus entails the

    rather unrealistically cautious assumption that the late

    winter-early summer specimens were fast developers,

    while the autumn-winter jaws were slow developers.

    Because the evidence for different seasons also tends to

    be of variable precision (see below), the effect of this

    procedure may well be to obscure indications of occu-

    pation in some seasons of the year.

    Secondly, it should be emphasised that the slaughter

    of young domesticates in recent, sedentary rural

    communities in Europe is often markedly seasonal, for acombination of ecological and cultural reasons (e.g.

    Cobbett 1979; cf. Halstead 1998 for some Greek

    examples). It is perfectly plausible that the slaughter of

    young livestock in the Neolithic may similarly have

    displayed some seasonality for reasons unconnected to

    temporal patterns of residence. Ironically, for this reason,

    year-round residence may be easier to demonstrate for

    Mesolithic sites in Denmark, with a diversity of wild

    animals including migratory species of restricted seasonal

    availability, than for Neolithic sites in Greece, with sparse

    evidence for hunting, fishing or fowling.

    Any archaeobotanical evidence for cereal and pulse

    grain crops is also noted for each site. It is assumed that

    such grain crops were mainly sown in mid- to late autumn

    or early winter (October-December; not spring see

    Hillman 1981, 1478) and harvested around early

    summer (June [pulses] and July [cereals] in northern

    Greece, one month earlier in southern Greece). Whether

    or not grain crops were grown in the vicinity of each site

    is discussed below. The sparse archaeobotanical evidencefor gathering of seasonally available fruits and nuts is not

    considered, because the quantities involved are too small

    to preclude the possibility of exchange between sites

    rather than collection in the vicinity of each archaeo-

    logical site.

    Seasons of consumption and residence at

    Neolithic tell sites in Thessaly, northern

    Greece

    The depth of occupation debris at Neolithic tell sites in

    Thessaly provides striking evidence for habitation ofconsiderable duration and was regarded by Childe (1957,

    60) as indicative of sedentism and an advanced farming

    regime (cf. Kotsakis this volume). Strictly speaking,

    however, tell formation indicates recurrent building

    activity on a generational or longer time scale, rather

    than year-round residence. Moreover, tell formation is a

    cumulative process and so impressive mounds might well

    conceal the remains of very transient early occupation, as

    Whittle has argued with reference to thin early levels at

    Thessalian tells such as Sesklo and Akhillion (Whittle

    1996a). Until recently, groups of transhumant or nomadic

    shepherds from the surrounding mountains over-wintered

    in the immediate vicinity of many lowland Thessalian

    tell sites and a similar pattern of regular seasonal

    movements has been suggested for the Neolithic (Jarman

    et al. 1982, 1501). A third possibility should also be

    considered that the Neolithic inhabitants of Thessaly

    moved on a more irregular basis, occupying individual

    sites at different seasons in different years.

    Middle Neolithic late Neolithic Plateia Magoula

    Zarkou

    The idea of seasonally mobile Neolithic settlement

    received apparent support from geoarchaeological

    investigations around the tell site at Plateia MagoulaZarkou, on the northern edge of the flat, west Thessalian

    basin (Fig. 5.1) and close to the Pinios, one of the largest

    rivers in Greece. Coring suggested that early occupation

    was located in an active floodplain, subject to annual

    inundation in winter-spring until river incision, perhaps

    from the later middle Neolithic onwards, reduced the

    risk of flooding; as a result, it has been argued, early

    Neolithic and middle Neolithic human occupation at

    Plateia Magoula Zarkou would necessarily have been

    seasonal (van Andel et al. 1995; van Andel and Runnels

    1995; Whittle 1996b, 17). As van Andel et al. (1995,

    138) make clear, however, they were unable to determine

    the frequency of flooding, leaving open the possibility

    that the early Neolithic-middle Neolithic settlement was

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    Resettling the Neolithic: faunal evidence from Neolithic sites in Greece 41

    flooded no more frequently than such major and long-

    established European cities as Athens and Prague.

    Modest assemblages of faunal remains (overwhelm-

    ingly of domestic mammals) are reported from both

    middle Neolithic (Becker 1999) and late Neolithic

    (Becker 1991) levels at Plateia Magoula Zarkou. Neonatalsheep/goat are reported from both levels (Becker 1999,

    12 table 4; 1991, 20 table 5), implying a human presence

    around or up to a month after the suggested lambing/

    kidding season of January-February, thus in mid-winter

    to early spring. Dental data for age at death of sheep and

    goats are not published in a format compatible with that

    used below for other sites, but young pig mandibles (Table

    5.1) imply deaths in early spring to early summer and in

    mid-autumn to mid-winter during the middle Neolithic;

    and in late spring to late summer, in mid-autumn to mid-

    winter and in early winter to mid-spring during the late

    Neolithic. The neonatal sheep/goats thus indicate human

    habitation at middle Neolithic and late Neolithic Plateia

    Magoula Zarkou firmly in the middle of the winter-spring

    period, when flooding supposedly drove people away from

    the site. Most of the young pig deaths are potentiallycompatible with this same period, but additional late

    Neolithic activity is implied at some less precisely

    identifiable stage(s) of the remaining mid-spring to early

    winter period. Information on the timing of deaths of

    first-year lambs and kids might further fill in the seasonal

    cycle, while middle Neolithic caches of bitter vetch, Vicia

    ervilia (Kroll cited in Becker 1991, 77 table 14; Jones

    and Halstead 1993), if cultivated locally, would confirm

    a human presence in mid-autumn to early winter (for

    sowing) and in early summer (for harvesting).

    Figure 5.1 Map of Greece, showing the location of sites discussed in the text.

    Key: 1. Plateia Magoula Zarkou, 2. Prodromos 12 and 3, 3. Akhillion, 4. Ag. Sofia, 5. Dimini, 6. Doliana, 7. Cave

    of Zas, 8. Makriyalos.

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    Paul Halstead42

    Table5

    .1AgesandsuggestedseasonsofdeathofpigsatENProdromos1-2and3,MNandLNPlateiaMagoulaZa

    rkou,LNAg.Sofia,LNDimini,LNM

    akriyalos(Pit

    212),F

    NCaveofZasandFNDoliana.

    SuggestedagesfordentalstagesafterHigh

    am(1967).Assumingbirthseasons

    ofMarch-April(NGreece)andFeb

    ruary-March

    (SGreece).MortalitydataforProdromos1-2and3fromHalsteadandJones(1980,99fig.3;andunpublishedre

    cords),forPlateia

    MagoulaZarkoufromBecker(1991,24table8),forAgiaSofiafromvondenDrieschandEnderle(1976,44table

    11),forDimini,

    Makriyalos,CaveofZasandDolianafrom

    authorsunpublishedrecords.

    Key:d4fourthdeciduouspremolar,M1firstmolar,M2secondmolar,U

    unerupted,E-erupting,Winw

    ear

    Prodromos

    1-2

    3

    PlateiaMago

    ula

    Zarkou

    Agia

    Sofia

    Dimini

    Makri-

    yalos

    Caveof

    Zas

    Doliana

    Age

    stage

    Agein

    months

    EN

    EN

    MN

    LN

    LN

    LN

    LNPit

    212

    FN

    FN

    Neo-

    natal

    0-1

    -

    -

    -

    -

    March-

    May

    -

    March-

    May

    Feb-

    April

    March-

    May

    d4E

    0-2

    -

    -

    March-

    June

    -

    -

    -

    -

    -

    -

    d4W

    M1U

    2-4

    May-

    Aug

    -

    -

    M

    ay-

    Aug

    May-

    Aug

    May-

    Aug

    May-

    Aug

    -

    -

    M1E

    4-7

    July-N

    ov

    -

    -

    -

    -

    July-Nov

    July-Nov

    -

    July-Nov

    M1W

    M2U

    7-9

    Oct-Jan

    Oct-Jan

    Oct-Jan

    Oct-Jan

    Oct-Jan

    Oct-Jan

    Oct-Jan

    Sept-Dec

    Oct-Jan

    M2E

    9-12

    -

    Dec-

    April

    -

    D

    ec-

    A

    pril

    Dec-

    April

    -

    Dec-

    April

    Nov-

    March

    Dec-

    April

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    Resettling the Neolithic: faunal evidence from Neolithic sites in Greece 43

    Early Neolithic Prodromos 13

    A cluster of Neolithic sites at Prodromos in the southern

    part of the west Thessalian basin lies close to the margin

    of recent marsh. Prodromos 3 forms an impressively tall

    tell, topped by Bronze Age and historical deposits.

    Prodromos 1 and 2 may represent two closely spaced low

    mounds, but with the benefit of hindsight might be

    interpreted as parts of a disturbed flat-extended site (see

    below). The deposits of Prodomos 12 and the lower

    levels of Prodromos 3 were assigned to early Neolithic

    and the transition to middle Neolithic.

    First-year pig mandibles from Prodromos 12 are

    assignable to deaths in late spring to late summer, in

    mid-summer to late autumn and in mid-autumn to mid-

    winter; specimens from Prodromos 3 are assignable to

    deaths in mid-autumn to mid-winter and in early winter

    to mid-spring (Table 5.1). This evidence could be

    accommodated to short periods of human presence inlate summer to mid-autumn at Prodromos 12 and in

    early or mid-winter at Prodromos 3, but is more likely to

    represent activity extending earlier and later at both sites.

    First-year mandibles of sheep/goats, assigned broadly to

    the periods between mid- or late summer and mid-winter

    (both sites) and between mid-autumn and mid-spring

    (Prodromos 12 only), are compatible with the evidence

    from young pig deaths (Table 5.2). Samples of cereal and

    pulse grains (Halstead and Jones 1980, 115 table 8), if

    derived from local cultivation, would favour an extended

    human presence at Prodromos 12, from harvest time in

    early and mid-summer until sowing time in mid-autumn

    to early winter. The apparent late winter to mid-spring

    gap at Prodromos 12, reflecting the lack of records of

    neonatal remains or of very young mandibles, should be

    treated with particular caution for two reasons. First, this

    site was excavated under rescue conditions, so that

    retrieval of small specimens may be worse than at the

    other tells discussed here. Secondly, neonatal bones were

    not distinguished as a separate category during recording

    of the Prodomos assemblages, but might be included

    among the lamb/kid specimens represented by unfused

    scapula, pelvis, distal humerus and proximal radius

    recorded at both sites (Halstead and Jones 1980, 112

    table 4c).

    Early Neolithic-middle Neolithic Akhillion

    The tell site of Akhillion is located in the rolling hills on

    the southern edge of the Thessalian lowlands and is thus

    safe from the risk of flooding. Published mortality data

    do not distinguish between early Neolithic and middle

    Neolithic material (Bknyi 1989, 323 table 13.8), but

    newborn specimens of sheep/goat and pig suggest deaths

    of livestock and a human presence in mid-winter to early

    spring and in spring, respectively. The use of very coarse

    age categories (juvenile, subadult) precludes dis-

    cussion of faunal evidence for the rest of the annual cycle.Sparse finds of cereal and pulse grains from both early

    Neolithic and middle Neolithic levels (Renfrew 1989),

    however, if derived from crops grown locally, would again

    entail a human presence in mid-autumn to early winter

    (sowing) and early to mid-summer (harvesting). Despite

    the paucity of relevant data, therefore, there is some

    evidence for occupation in all seasons of the year.

    Late Neolithic Agia Sofia

    The Agia Sofia mound is located in the slightly elevated

    north-eastern part of the Thessalian plain. The man-

    dibular evidence for age at death of young un-

    differentiated sheep/goats (probably mostly sheep) and

    young pigs is published in reasonable detail for the late

    Neolithic Agia Sofia assemblage (von den Driesch and

    Enderle 1976). First-year pigs died in spring, in late

    spring to late summer, in mid-autumn to mid-winter,

    and in early winter to mid-spring (Table 5.1), implying

    activity at the site during spring and also later in the year

    at minimum in early or mid-winter. First-year sheep(/goat) deaths in late winter to late spring, in early spring

    to mid-summer, between mid-spring and mid-winter, and

    between mid-autumn and mid-spring (Table 5.2) are

    consistent with the evidence of young pigs, suggesting

    activity at the site at least during (and probably extending

    beyond) spring.

    Late Neolithic Dimini

    Dimini occupies a slight rise on the edge of the coastal

    plain of Volos and the modest sample of young sheep and

    goat mandibles (Halstead 1992 and original records)

    documents deaths in late winter to mid-spring, in mid- tolate spring, in early spring to mid-summer, in mid-

    summer to early winter, in late summer or early autumn

    to mid-winter, and in mid-autumn to early or mid-spring

    (Table 5.2). The few jaws from first-year pigs suggest

    deaths at least during late spring to late summer, during

    mid-summer to late autumn, and during mid-autumn to

    mid-winter (Table 5.1). Young sheep/goat and pig deaths

    thus concur in indicating occupation at least during late

    winter or spring and also, less precisely, during summer

    to mid-winter (minimally mid- to late autumn, but

    probably longer). Caches of both cereals and pulses (Kroll

    1979), if grown locally, would indicate a human presence

    during mid-autumn to early winter (sowing) and early to

    mid-summer (harvesting) and so strengthen the evidence

    for activity in all seasons.

    Discussion: going nowhere in Neolithic Thessaly?

    For none of these Thessalian tells can occupation be

    demonstrated for all seasons of the year, but this may

    well be an artefact of the nature of the available evidence.

    Activity can be firmly documented at some sites in late

    winter-early spring and/or spring because neonatal and

    infant remains are very distinctive and can be aged very

    precisely, but such remains are subject to acute preser-

    vation and retrieval biases and so their absence may shed

    no light on season(s) of human activity. As animals

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    Paul Halstead44

    Prodromos

    1-2

    3

    Agia

    Sofia

    Dimini

    Makriyalos

    CaveofZas

    Doli-

    ana

    Ageinmonths

    EN

    EN

    LN

    LN

    LNPit212

    LN

    FN

    FN

    A

    ge

    stage

    Sheep

    Goat

    Sh/G

    t

    Sh/Gt

    Sh/Gt

    Sheep

    Goat

    Sheep

    Goat

    Sheep

    Goat

    Sheep

    Goat

    Sheep

    N

    eo-

    natal

    0-1

    0-1

    -

    -

    -

    -

    Jan-March

    Dec-Feb

    Dec-Feb

    Jan-

    March

    d4W

    M

    1U

    1-2

    1-3

    -

    -

    Feb-

    May

    Feb-

    April

    -

    Feb-

    April

    -

    -

    -

    Jan-

    March

    -

    -

    M

    1E

    3

    2-5

    -

    -

    March-

    July

    April-

    May

    March-

    July

    April-

    May

    March-

    July

    -

    Feb-

    June

    March-

    April

    -

    -

    M

    1W

    M

    2U

    (C1-2)

    3-6

    4-6

    -

    -

    -

    -

    April-

    Aug

    May-

    Aug

    -

    April-

    July

    -

    April-

    July

    April-

    Aug

    M

    1W

    M

    2U

    (C3-4)

    5-9

    5-8

    -

    -

    -

    -

    June-

    Nov

    -

    -

    May-

    Sept

    May-

    Oct

    May-

    Sept

    -

    M

    1W

    M

    2U

    (C5)

    6-10

    6-11

    July

    -

    Jan

    -

    July-

    Dec

    -

    July-

    Dec

    July-

    Jan

    -

    -

    -

    June-

    Dec

    July-

    Dec

    M

    1W

    M

    2U

    (C6+)

    8-11

    7-11

    Aug

    -

    Jan

    Aug-

    Jan

    April

    -Jan

    Sept-

    Jan

    Aug-

    Jan

    Sept-

    Jan

    Aug-

    Jan

    Aug-

    Dec

    -

    Aug-

    Dec

    July-

    Dec

    Sept-

    Jan

    M

    2E

    9-13

    9-14

    Oct-

    Apr

    il

    -

    Oct-

    April

    Oct-

    March

    Oct-

    April

    Oct-

    March

    Oct-

    April

    -

    -

    -

    Sept-

    March

    -

    Table5

    .2Agesandsuggestedseason(s)ofd

    eathofsheepandgoatsatENProdromos1-2and3,LNAgiaSofia,LN

    Dimini,LNMakriyalos(Pit212),LN

    andFNCave

    ofZas,

    andFNDoliana.

    SuggestedagesfordentalstagesafterJones(inpress),forsheep,andDeniza

    ndPayne(1982),forgoat;Jonessub-stageC6+modifiedtoexcludespecimenswith

    eruptingM2.AssumingbirthseasonsofJa

    nuary-February(NGreece)andDe

    cember-January(SGreece).MortalitydataforAgiaSofiafromvonde

    nDrieschand

    Enderle(1976,39table8),forDiminifrom

    Halstead(1992,46fig.7;andunpu

    blishedrecords),forProdromos1-2

    and3,Makriyalos,CaveofZasandDolianafrom

    author

    sunpublishedrecords.

    Key:se

    eTable7.1.

    Paul Halstead

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    Resettling the Neolithic: faunal evidence from Neolithic sites in Greece 45

    progress through the first year, their mandibles become

    increasingly robust (e.g. Munson and Garniewicz 2003)

    and also larger, greatly enhancing the likelihood of both

    survival and retrieval; at the same time, because of

    variability in the timing of tooth eruption and, especially,

    in the speed of tooth wear, the precision of agedetermination declines (cf. OConnor 1998). As a result,

    although later first-year animals are well represented in

    at least some of these assemblages, human activity tends

    to be identified for rather broad periods (summer-autumn,

    autumn-winter) rather than for single seasons. The

    clearest seasonal gaps in the evidence for human presence

    can plausibly be attributed to coarse analytical methods

    (e.g. late winter to mid-spring at Prodromos 12, summer

    to early winter at Akhillion), insufficient detail in

    published records (e.g. mid-spring to early winter at

    middle Neolithic Plateia Magoula Zarkou), or small

    sample size (e.g. late winter to early autumn at Prodomos3).

    Figure 5.2 offers a simplified overview of the evidence

    for seasons of occupation discussed in detail above.

    Faunal evidence is distinguished as very strong, strong

    or moderate (i.e. deaths assigned to a period of two-three

    months, four months or five months, respectively); weak

    evidence (deaths assigned to a period of six or more

    months) is treated in Figure 5.2 in the same way as an

    absence of evidence. In addition, the times of year are

    highlighted at which reported crop remains would if

    grown locally require a human presence for sowing and

    harvesting.

    With due allowance for variation in sample size,retrieval standards, and the precision of recording or

    reporting relevant data, the faunal evidence consistently

    indicates a human presence in winter and/or spring,

    probably extending into more or less of the summer-

    autumn period. Other than the very unreliable absence of

    evidence for late winter-spring activity at Prodromos 1

    2, there is no hint that different sites occupied com-

    plementary positions in a system of regular seasonal

    movements. Nor is there any support for the claim that

    the inhabitants of Plateia Magoula Zarkou were driven

    away from the site in winter-spring by flooding. If

    Neolithic tells were abandoned, therefore, in the contextof regular seasonal movements, it seems that their

    inhabitants must have moved to un-recognized sites of a

    different type and/or located outside the Thessalian

    lowlands. Seasonal movement with livestock to summer

    pastures at high altitude, as practised by recent specialised

    pastoralists, is compatible with the faunal evidence, but

    as yet there is no evidence in favour of this practice nor

    would it necessarily have involved movement of the entire

    human population of a tell settlement. Moreover, the

    window for such an absence is narrowed if cereals and

    pulses were grown in the vicinity of these sites, implying

    habitation at least during the June-July harvest season,

    and perhaps later if crops required processing for storage

    on a large scale. Local cultivation cannot be demon-

    strated, but cereal and pulse grains seem to be encountered

    in all tell excavations (Kroll 1981), despite the lack of

    systematic sampling. Crops must have been grown round

    at least some of these sites, therefore, unless we posit the

    importing of cereals and pulses from sites that, again,

    remain to be discovered.Consideration of the extent and probable number of

    inhabitants of known sites leaves little room for doubt

    that cereals and pulses were grown in significant

    quantities around all Neolithic tells in Thessaly (Halstead

    1989). When the practical implications of local crop

    husbandry are also taken into account (Fig. 5.2), the case

    is further strengthened for occupation of these sites in all

    seasons of the year. Given the longevity and coarse

    chronological resolution of these tell sites, it must be

    acknowledged that the faunal and archaeobotanical

    assemblages are compatible with a pattern of irregular

    seasonal mobility, in which individual sites were occupiedat different seasons in different years. Such opportunistic

    residential mobility, however, seems far less likely than

    year-round habitation to have led to the accumulation (or

    even purposive creation cf. Chapman 1997; Kotsakis

    1999) of monumental tell sites. Arguably the most

    parsimonious interpretation of the available evidence

    (from early Neolithic, middle Neolithic and late Neolithic

    levels alike) is that these Thessalian tell sites were

    occupied year-round by at least some of their in-

    habitants.

    Seasonality of consumption and residence atnon-tell Neolithic sites in Greece

    In addition to the impressive tells, known in largest

    numbers in lowland central and northern Greece, at least

    three other types of Neolithic site are now well docu-

    mented in Greece: small and short-lived open sites,

    located in large numbers by survey projects in southern

    Greece, but also found in northern Greece; caves,

    frequently used in the later Neolithic, especially in

    southern Greece; and flat-extended open sites, recently

    recognized in northern Greece. The small open sites and,

    for obvious geological reasons, the caves are often located

    in agriculturally marginal locations, and inter alia havebeen interpreted as seasonal herding camps. The flat-

    extended sites are, like the tells, found in the fertile

    lowlands, but represent a radically different form of

    spatial organization, with habitation traces drifting

    laterally through time rather than building up vertically

    on the same spot (Kotsakis 1999). Ditches encircling the

    flat-extended site of Makriyalos (Pappa and Besios 1999)

    are somewhat reminiscent of Neolithic enclosures in

    north-west Europe and perhaps invite speculation that

    these sites represent seasonal gathering places, rather

    than an alternative form of long-term residential site.

    The bioarchaeological evidence for seasonality of human

    activity is reviewed here for one site in each of these

    three non-tell categories (Fig. 5.3).

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    Paul Halstead46

    Figure 5.2 Evidence for season(s) of Neolithic human activity at tell sites in Thessaly.

    Key: Dark fill very strong faunal evidence (deaths within period of 23 months);

    Medium fill strong faunal evidence (deaths within period of 4 months);

    Light fill moderate faunal evidence (deaths within period of 5 months);

    Unfilled weak (deaths within period of 6+ months) or no faunal evidence;

    Bold outline probable harvest and sowing periods for cereal and pulse crops;SG3 etc type of faunal evidence for activity in any month (e.g., S2, SG3, P4, G5 = sheep, sheep/goat, pig and goat deaths

    attributed to periods of 2, 3, 4 and 5 months, respectively).

    EN-MN Akhillion

    July

    August

    September

    October

    November

    December

    May

    P3

    April

    P3

    March

    SG3, P3

    February

    SG3

    January

    SG3

    June

    Autumn

    (Sept-Nov)

    Summer

    (June-Aug)

    Spring

    (March-May)

    Winter

    (Dec - Feb)

    EN Prodromos 1-2

    February

    March

    April

    December

    P4

    January

    P4

    May

    P4June

    P4

    July

    P4, P5

    August

    P4, P5

    September

    P5

    October

    P4, P5

    November

    P4, P5

    EN Prodromos 3

    May

    JuneJuly

    August

    September

    November

    P4

    October

    P4

    April

    P5

    March

    P5

    February

    P5

    January

    P4, P5December

    P4, P5

    MN Plateia Magoula Zarkou

    August

    September

    December

    P4

    November

    P4

    October

    P4

    July June

    P4

    May

    P4

    April

    P4

    March

    SG3, P4

    February

    SG3

    January

    SG3, P4

    LN Plateia Magoula Zarkou

    March SG3,

    P5

    April P5

    May P4

    September

    June

    P4

    July

    P4

    August

    P4

    October

    P4

    November

    P4

    December

    P4, P5

    January

    SG3, P4, P5February

    SG3, P5

    LN Ag Sofia

    September

    December

    P4, P5

    November

    P4

    October

    P4

    August

    P4

    July

    P4, SG5June

    P4, SG5

    May

    SG4, P3, P4,

    SG5

    April

    SG4, P3, P5,

    SG5

    March

    SG4, P3, P5,

    SG5

    February

    P4, P5

    January

    P4, P5

    LN Dimini

    October

    P4, S5, P5

    September

    S5, P5

    August

    P4, P5

    July

    P4, G5, P5June

    P4, G5

    May

    S2, P4, G5

    April

    S2, S3, G5

    March

    S3, G5

    February

    S3

    January

    P4, S5

    November

    P4, S5, P5

    December

    P4, S5

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    Resettling the Neolithic: faunal evidence from Neolithic sites in Greece 47

    Final Neolithic Doliana, Ipiros

    Rescue work uncovered a small, short-lived open site of

    final Neolithic date in the Doliana basin, at 400m altitude

    on the western flank of the Pindos Mountains of north-

    west Greece. The brevity of occupation and lack of

    building remains other than two successive hut floors

    favoured interpretation as a seasonal herding camp

    (Dousougli 1996); a nearby pollen core has also been

    interpreted in terms of seasonal herding (Willis 1997). A

    modest faunal assemblage (Halstead et al. in preparation)

    included neonatal remains of sheep/goats and pigs,

    suggesting activity in mid-winter to early spring and in

    spring, respectively. Young mandibles indicate first-year

    deaths of sheep in mid-spring to late summer, in mid-

    summer to early winter, and in early autumn to mid-

    winter (Table 5.2), and first-year deaths of pigs in mid-

    summer to late autumn, in mid-autumn to mid-winter,

    and in early winter to mid-spring (Table 5.1). Themandibular evidence thus implies further human activity

    at some stage(s) between early summer and early winter

    at minimum, during mid- to late summer (sheep) and

    during mid- to late autumn (pigs). Although seasonal

    abandonment of the site cannot be ruled out, inter-

    pretation in terms of year-round activity would perhaps

    require less special pleading.

    Late Neolithic-final Neolithic cave of Zas,

    Cyclades

    The cave of Zas is located at 600m altitude on the

    limestone mountain that dominates the island of Naxos.

    The cave is small and dark enough to cast doubt on its

    use as a habitation site, while an abundance of metal

    finds perhaps suggests a ceremonial or symbolic function

    (Broodbank 2000, 165). Either way, an agriculturally

    marginal location perhaps invites suggestions of use by

    seasonally mobile herders (Zachos 1999). The late

    Neolithic and final Neolithic faunal assemblage from this

    cave has benefited from strikingly better preservation

    (carnivore attrition was negligible) and retrieval (deposits

    were systematically and intensively sieved) than all other

    sites discussed in this chapter. In addition, the present

    author (with collaborators) recorded this assemblage (and

    those from Doliana and Makriyalos) recently, and thushas access to records far more detailed than would be

    tolerated by most publishers.

    Remains of newborn sheep/goats (both late Neolithic

    and final Neolithic) and newborn pigs (final Neolithic)

    imply activity at the cave in winter and in late winter to

    mid-spring, respectively, that is at the time of year when

    seasonally mobile herders might have been expected to

    be absent from the vicinity. At this site, sheep and goats

    are almost equally represented, but the latter exhibit more

    first-year deaths. In the larger final Neolithic assemblage,

    mandibles of lambs and kids suggest deaths in mid-winter

    to early spring, in early to mid-spring, in mid-spring tomid-summer, in late spring to early or mid-autumn, in

    early or mid- or late summer to early winter, and in early

    autumn to early spring (Table 5.2); pigs are rare, but late

    first-year mandibles imply deaths at least in early autumn

    to early winter and in late autumn to early spring (Table

    5.1). The smaller late Neolithic sample provides a less

    continuous, but broadly similar, record of deaths of first-

    year lambs and kids. Although only securely demon-strable for winter-spring, human activity in all seasons is

    the most parsimonious reading of the faunal data,

    especially for the larger final Neolithic assemblage.

    Cereal and pulse grains were found in considerable

    numbers in both the late Neolithic and final Neolithic

    levels (Zachos 1999, 1567) and, if grown locally, would

    strengthen the case for a human presence nearby in late

    spring-early summer (harvest) and mid-autumn to early

    winter (sowing). Whatever the function of the cave,

    therefore, it seems more likely to have been used by people

    from a nearby and relatively sedentary settlement than as

    a shelter for mobile herders taking advantage of summerpasture on Mt. Zas.

    Late Neolithic Makriyalos, Central Macedonia

    The flat-extended site of Makriyalos is located on gentle

    slopes close to the sea. Extensive excavation of enclosure

    ditches, borrow pits and huts of early late Neolithic and

    late late Neolithic date yielded one of the largest faunal

    assemblages from prehistoric Greece. Unlike Zas, the

    assemblage did not avoid carnivore attrition, nor did

    rescue excavation permit the same high standards of

    retrieval, but again recent and detailed dental records are

    available. Analysis is restricted here to a single short-

    lived context, in order to reduce the risk that apparent

    evidence for year-round activity might in fact represent

    the conflation of numerous seasonal visits, the timing of

    which varied from year to year or even from century to

    century. The early late Neolithic Pit 212, with a diameter

    of 30m, produced the remains of at least several hundred

    domestic animals and a wealth of pottery, both apparently

    deposited rapidly over a period of months or just a handful

    of years and interpreted as the remains of large-scale

    collective feasting (Pappa et al. 2004, 1644). It should

    be noted that the evidence for seasonality from Pit 212

    seems to be very similar to that for the rest of the early

    late Neolithic assemblage.Remains of newborn sheep/goats and pigs indicate

    deaths in mid-winter to early spring and in spring,

    respectively. Young mandibles of sheep and goats suggest

    deaths in late winter to mid-spring, in mid- to late spring,

    in early spring to mid-summer, in mid- or late spring to

    late summer, in early summer to late autumn, in mid-

    summer to early or mid-winter, in late summer or early

    autumn to mid-winter, and in mid-autumn to early or

    mid-spring. Young mandibles of pigs suggest deaths in

    late spring to late summer, in mid-summer to late autumn,

    in mid-autumn to mid-winter, and in early winter to mid-

    spring. Pit 212 provides the strongest faunal evidence yetconsidered for human activity in all seasons and this is

    strengthened by two further considerations. First, pre-

  • 7/30/2019 Ch5 Paul Halstead

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    Paul Halstead48

    liminary results from a study of enamel hypoplasia in the

    pig mandibles (cf. Dobney et al. 2002) provide empirical

    support for a single farrowing season (U. Albarella and

    K. Dobney pers. comm .); this makes it unlikely that the

    observed range of ages at death of young pigs represents

    seasonal slaughter of animals born at different times ofyear. Secondly, in the case of sheep, every stage of first-

    year dental development is represented - and the same is

    almost true of pigs and largely so of goats; thus the

    argument for slaughter in every season of the year is

    independent of the assumptions made here as to the

    timing (absolute or relative) of lambing, kidding and

    farrowing. In addition, Pit 212 yielded archaeobotanical

    samples rich in cereal chaff and these crop remains, if

    grown locally, provide supporting evidence for human

    activity at Makriyalos in mid-autumn to early winter

    (sowing) and in mid-summer (harvesting). Finally, as

    noted above, Pit 212 represents a relatively shortdepositional episode, probably spanning at most a

    handful of years; the record of deaths in all seasons,

    therefore, is highly unlikely to be an artefact of com-

    plementary seasonal episodes of slaughter in different

    years. Pit 212 surely results from year-round slaughter

    and consumption at late Neolithic Makriyalos.

    Discussion: going nowhere in Neolithic Greece?

    If tell sites have long been equated with sedentary

    occupation, the reverse has often been assumed for

    Neolithic caves and small open sites and, more

    tentatively, for flat-extended sites. Contrary to these

    expectations, bioarchaeological evidence from the small

    open site of Doliana, from the Cave of Zas and from the

    flat-extended site of Makriyalos, is, in each case, more or

    less strongly suggestive of year-round human activity

    (Fig. 5.3). These three sites cannot be treated as typical

    of all such sites, but nor is there any reason to imagine

    that they are unusual other than in the quantity and/or

    quality of available bioarchaeological data.

    Conclusions

    While bioarchaeological evidence for year-round activity

    at Neolithic sites in Greece is of variable strength, it mustbe underlined that several of the assemblages discussed

    are small and that most are of coarse chronological

    resolution, while most publications of data sets from tells

    address different research questions and so provide

    insufficient detail for assessment of seasonality. More-

    over, almost any set of dental data could be accommodated

    Figure 5.3 Evidence for season(s) of Neolithic human activity at non-tell sites in Greece. Key: see Figure 5.2.

    LN M akriyalos Pit 2 12

    December

    P4, P5, S5

    November

    P4, P5, S5

    October

    P4, P5, S5

    September

    P5, S5

    August

    G4, P4, P5,

    G5 July

    P4, P5, G4,

    G5, G5

    June

    G4, P4, G5,

    G5

    May

    S2, P4, G4,

    G5, G5

    Apr il

    S2, P3, S3,

    P5, G5, G5

    March

    P3, SG3,

    S3, P5, G5

    February

    SG3, S3, P5

    January

    SG3, P4, P5,

    S5

    FN Doliana

    January

    S3, P4, P5,

    S5

    February

    S3, P5

    March

    S3, P3, P5

    April

    P3, P5, S5

    May

    P3, S5June

    S5

    July

    P5, S5

    August

    P5, S5

    September

    P5, S5

    October

    P4, P5, S5

    November

    P4, P5, S5

    December

    P4, P5, S5

    LN Zas

    November

    S5

    October

    S5

    September

    G5, S5

    August

    G5, S5

    July

    G4, G5

    June

    G4, G5, G5

    May

    G4, G5, G5

    April

    G4, G5

    March

    G5

    February

    SG3, G5

    January

    SG3

    December

    SG3, S5

    FN Zas

    November

    P4, S5, P5

    October

    P4, S5

    September

    P4, G5, S5

    August

    G5, S5July

    G4, G5

    June

    G4, G5

    May

    G4, G5

    April

    S2, P3, G4,

    March

    S2, S3, P3,

    P5

    February

    SG3, S3, P3,

    P5

    January

    SG3, S3, P5

    December

    SG3, P4, S5,

    P5

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    Resettling the Neolithic: faunal evidence from Neolithic sites in Greece 49

    to seasonal slaughter by assuming the appropriate

    combination of early or late birth, precocious or tardy

    tooth eruption, and fast or slow tooth wear. On the other

    hand, it is striking that the strength of the evidence for

    year-round activity is related not to the type, location or

    date of each site, but to sample size and preservation,retrieval standards, the level of detail of available dental

    records, and the chronological resolution of each

    excavation. The most parsimonious interpretation of the

    evidence is that all of these sites were used more or less

    year-round.

    As has already been stressed, human activity in the

    Neolithic of Greece must have taken place off-site (i.e.

    away from archaeologically recognizable sites). It is also

    highly likely that known archaeological sites include loci

    (e.g. some of the ephemeral scatters of Neolithic material

    located by several survey projects in southern Greece)

    used on only a seasonal or shorter-term basis. It seems,however, that most excavated Neolithic sites, including

    tells, flat-extended sites and at least some caves and small

    open-air sites, were used more or less year-round by at

    least some of their occupants. Although uncomfortably

    close to traditional assumptions of a sedentary Neolithic,

    this conclusion poses some interesting questions:

    how did local aggregations maintain communal

    solidarity in the face of the tensions inevitably arising

    from long-term co-residence and despite the divisive

    tendencies implied on most open sites by domestic

    architecture?

    how did neighbouring sites (often close enough for

    regular contact in herding, gathering, hunting, etc)interact and how did they avoid (or win) conflicts?

    how did communities, or individuals, maintain the

    distant social relationships needed to find marriage

    partners and implied by exotic objects and long-

    distance stylistic similarities?

    Answers to these questions are beyond the scope of

    this chapter, but the wealth of fine, often decorated

    tablewares in Neolithic ceramic assemblages from Greece

    suggests that the consumption of food and drink (and,

    perhaps, other stimulants) was of fundamental social, as

    well as nutritional, significance (Halstead 1995; Kotsakis

    1983; Sherratt 1991; Vitelli 1989). Faunal evidence most dramatically, the massive assemblage from Pit 212

    at Makriyalos suggests that consumption of the meat of

    domestic animals played a major role in such commensal

    politics (Pappa et al. 2004, 1644).

    While the recurring desire to question the link between

    farming and sedentism is undoubtedly healthy, the

    available evidence for the Neolithic of Greece favours a

    largely sedentary pattern of settlement, which in turn

    poses some important and interesting questions con-

    cerning social reproduction in the early farming pop-

    ulations of this region. Faunal remains both provide

    evidence for sedentary habitation and offer some hints as

    to how the attendant stresses on social life may have been

    resolved.

    Acknowledgements

    I am grateful to Doug Bailey and Alasdair Whittle, for

    encouraging dissent, and to Amy Bogaard and Valasia

    Isaakidou, for comments on drafts of this paper. For

    access to faunal material discussed here, I am indebted toGiorgos Hourmouziadis (Prodromos and Dimini),

    Angelika Dousougli (Doliana), Kostas Zachos (Zas), and

    Maria Pappa and Manthos Besios (Makriyalos). I also

    thank Pat Collins and Valasia Isaakidou, for helping to

    record the Doliana, Zas and Makriyalos assemblages;

    Umberto Albarella and Keith Dobney, for preliminary

    results of their analysis of enamel hypoplasia in the

    Makriyalos pigs; and Gill Jones, for access in advance of

    publication to her study of sheep tooth eruption and wear.

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