The following is adapted from:
Parkinson, William A. 1999. "The Social Organization of Early Copper Age Tribes on
the Great Hungarian Plain." Ph.D. Dissertation. University of Michigan, Ann Arbor.
The Archaeological Setting
The complex geomorphological history of the Great Hungarian Plain has
left behind a region that is, in many ways, ideal for archaeological research.
The Carpathian Basin forms a topographically discrete unit within the
European landscape and the Great Hungarian Plain forms an even more discrete
geomorphological region within that basin. Separated from the rolling
hills of Transdanubia by the Danube and Tisza rivers, the rich alluvial
soils of the Great Hungarian Plain are surrounded by imposing geographic
boundaries, creating an almost insular environment that to this day is
considered a distinct cultural area with more affinities to the east and
south, in Romanian Transylvania and the Yugoslavian Banat, than with the
west and north.
The extensive deposition of wind-blown loess during the end of the Pleistocene
and the beginning of the Holocene, combined with the successive movement
of several active streambeds across the Plains soft loess surface,
left behind a surface landscape largely devoid of the raw materials that
prehistoric people were so fond of using, thus transforming the Plain
into a virtual laboratory for prehistoric archaeologists. Since the prehistoric
inhabitants were forced to look elsewhere for metal and stone, which occur
in abundance in the surrounding mountainous areas, the presence of materials
such as obsidian, chert, copper, and gold in different archaeological
contexts provides the prehistorian with the ability to identify patterns
of exchange in a manner unparalleled in most other parts of the world.
While these various geological events have created a region that in many
other respects offers benefits that can be found in only a few other parts
of the world, these same geomorphological processes have obscured much
of the early prehistory of the Plain, leaving a picture of the past that
fades to black sometime during the Mesolithic.
Upper Paleolithic, Epipaleolithic, and Mesolithic
The earliest prehistory of Hungary can be traced to the Lower Paleolithic
at Vértesszölös (see Kretzoi and Dobosi 1990), and several Middle
Paleolithic sites have been documented throughout Transdanubia and in
the Bükk Mountains, but the earliest prehistory of the Great Hungarian
Plain begins sometime during the Upper Paleolithic. As Kertész
(1996:5) has recently noted,
the Great Hungarian Plain (the
Alföld) remained a terra incognita until recently with regard to
the Palaeolithic and Mesolithic.
Although some Upper Paleolithic and Mesolithic sites had been identified
on the Plain during the early decades of this century (e.g., Szeged-Öthalom,
Hugyaj/Érpatak, Tószeg-Áldozó, see Banner
1936; Hillebrand 1925; Sümeghy 1944), the cultural makeup of the
region prior to the Neolithic remained largely unknown. As a result, reconstructions
of these earlier periods were therefore subject to much speculation (for
a recent discussion, see Makkay 1996). In recent years, however, new evidence
regarding the later Pleistocene and early Holocene habitation of the Plain
is beginning to emerge, thus clarifying the relationship between the early
Neolithic agriculturalists and their hunting and gathering predecessors.
Of particular interest in this regard is the work of Kertész (1996),
who has identified several Upper Paleolithic, Epipaleolithic, and Mesolithic
sites in the northwestern corner of the Plain, in the Jászság
area. Kertész notes that Upper Paleolithic and Epipaleolithic sites
in the Jászság tend to be located on Pleistocene alluvial
fans. In contrast, Upper Paleolithic sites in the center of the Plain
tend to be covered with thick Quaternary deposits. For example, Kertész
(1996:12) notes that the cultural layer at the Szeged-Öthalom campsite
was found at a depth of 4.5 m, while at Madaras-Téglaveto‡ it was
between 6.5 and 7 m deep. The depth of deposits on top of these early
sites precludes their systematic investigation at the center of the Plain.
Mesolithic sites, on the other hand, are located in a wider variety of
geological contexts in the Jászság, and can therefore be
expected in different contexts throughout the Plain. These range from
marginal subsidences and alluvial fans in the northern Alföld to
the sandy plain between the Danube and the Tisza (Kertész 1996:16-17).
Interestingly, despite the relatively high density of Mesolithic sites,
Kertész did not discover any Early Neolithic (Körös Culture)
sites in the Jászság. The closest Early Neolithic sites
are located in the Middle Tisza valley. This led Kertész to suggest
that differences in site location are likely the result of, on the one
hand, geological, hydrological, and climatic considerations; and, on the
other, the differing ecological demands of hunters and gatherers (i.e.,
Mesolithic populations) as opposed to farmers (i.e., Early Neolithic populations):
The Mesolithic sites in the Alföld lie on the well-watered alluvial
plain (the Jászság area) and in sand regions on the dune
ridges associated with marginal floodplains and water-courses (the sandy
plain between the Danube and the Tisza as well as the Nyírség
area). In other words, the Mesolithic sites lie in ecological niches which
were rejected by the Körös culture. The Körös culture
preferred levees suitable for agriculture. This is the main reason why
Mesolithic and Early Neolithic Körös groups lived side by side
for a long period of time in the Alföld (Kertész 1996:25).
Kertészs recent research is beginning to shed light upon
a much-disputed topic in Hungarian archaeology the origins of the
Neolithic.
Early and Middle Neolithic
The Neolithic of the Great Hungarian Plain is characterized by a trend
towards increasing regional differentiation in ceramic styles, settlement
patterning, and resource exploitation. This trend began with the intrusion
of the earliest farmers onto the Plain during the Early Neolithic (Körös
Culture; see Figure 1 and Figure 2).
It gained pace gradually throughout the
Middle Neolithic (Alföldi Vonaldiszes Kerámia, or Alföld
Linear-Decorated Pottery - AVK), and finally reached its most heightened
and regionally differentiated level during the Late Neolithic (Tisza-Herpály-Csöszhalom
Complex).
The Early Neolithic Körös Culture
The earliest agriculturalists on the Great Hungarian Plain, known as the
Körös Culture, appeared sometime during towards the end of the
seventh millennium BC (cal.), shortly after the Neolithic became well-established
in the southern Balkans. Unlike their southern contemporaries in the Thessalian
Plain of northern Greece (see Demoule and Perlès 1993), wherein
domesticates regularly make up 90-95% of faunal assemblages, there are
generally fewer domesticates in the Early Neolithic Körös sites
(ca. 75%; see Bökönyi 1988; see also Tringham 1971:92). The
Körös culture is traditionally discussed as part of a much larger
cultural complex that encompasses the Great Hungarian Plain and eastern
Romania known as the Körös-Cris, complex (see Bognár-Kutzián
1944; Tringham 1971:91-96). Sometimes the northern Yugoslavian Early Neolithic
variant (Starcûevo) is also included, thus creating the Körös-Starcûevo-Cris,
complex (see Makkay 1996 for a recent discussion). Kalicz and Makkay (1977)
assigned a few sites in the northeastern Carpathian Basin to a sub-group
of Körös the Szatmár group since these
sites were spatially distinct and appeared to be contemporary with the
later phases of Körös. However, more recent research (see Makkay
1996) has demonstrated that these sites should be considered transitional
between Körös and AVK, or even early AVK (e.g., Kalicz 1998).
As is the case with the Early Neolithic throughout all of Europe, the
process of Neolithization within the region has received much
attention. Two questions have dominated research into the Hungarian Early
Neolithic. The first concerns how the region came to be occupied by ceramic-
and food-producing groups. The second addresses how those ostensibly invasive
groups related to indigenous Mesolithic hunting and gathering populations.
Until the recent work of Kertész (see above) in the Jászság
area the relationship of the Early Neolithic agriculturalists to their
Mesolithic predecessors, and contemporaries, has remained the subject
of speculation.
In a recent discussion of the topic, Makkay (1996:35) noted:
Traditionally, research of the Körös-Starcûevo-Cris, (KS or
KSC if the Transylvanian distribution of the culture is also involved)
has been mainly concerned with regional chronologies, typological nuances,
and the refinement of the internal chronology of the culture complex.
Considerably less effort has been devoted to a better understanding of
the Körös distribution, or the research of its settlement patterns
and even less to the explanation of large-scale patterns of historical
development.
Makkay has for a long time commented on the interesting fact that the
distribution of the Early Neolithic Körös Culture did not extend
to the alluvial fan of the Great Eastern River, nor into the Upper Tisza
valley (cf. Makkay 1982 for discussion). This has led him to suggest:
that the northern expansion of the Körös culture in the
Tisza valley was blocked not by geographic factors, but rather by an ancestral
(and, possibly, linguistic) border which in the Neolithic did not coincide
with any major natural geographic boundary, but which might easily have
coincided with an earlier, Mesolithic, or even Pleistocene geographic
boundary or area and, also, with a corresponding cultural boundary which
must already have existed in the Mesolithic. (Makkay 1996:41)
The northern part of the Alföld also follows the boundary between
the continental and Mediterranean climatic regimes, and it may therefore
have been less suitable to growing vernalized crops, such as winter wheat,
perhaps providing another explanation for the distribution. Nevertheless,
the overall pattern of site distribution recently has been bolstered by
Kertészs research in the Jászság area (see
above), where he located almost one hundred Middle and Late Mesolithic
sites in an area of approximately 100 km2 (see Kertész 1994; Kertész
et al. 1994; Kertész 1996). This evidence for a rather intensive
occupation of the northeastern Plain during the later Mesolithic, combined
with the contemporary lacuna of sites between the Jászság
area and the distribution of Körös sites further to the south,
have led Makkay to suggest that:
the Körös culture did not penetrate further north partly
because it was repelled by the heavy, water-logged clay of the low wet
backswamps and partly because the area was inhabited by a Late Mesolithic
indigenous population. Which for some reason or other, resisted Neolithization
in spite of the fact that for some time it lived beside the northern border
of the Körös culture. And when this Mesolithic population finally
accepted the Neolithic way of life, it did so on its own terms. By this
time, however, the decisive element was not the geographic boundary and
environment, but rather the different ethnic background. (Makkay 1996:41).
The relationship between Late Mesolithic hunters and gatherers and Early
Neolithic farming populations has been the topic of much discussion in
European prehistory (e.g., Keeley 1992; Price and Gebauer 1992; Whittle
1996:43-71, 1997). It is likely that future research in the Great Hungarian
Plain will further elucidate the particular means by which Neolithization
occurred via different processes of diffusion, acculturation, and migration
throughout different parts of the continent.
The Middle Neolithic Alföld Linear Pottery Culture (AVK)
The Middle Neolithic of the Great Hungarian Plain is known by a variety
of different names and acronyms in the literature Alföld Linear
Pottery Culture (ALP, or ALPC) in English, Alföldi Vonaldíszes
Kerámia (AVK) in Hungarian (see Figure 3). All of these terms attempt
to differentiate this Linear Pottery Culture from its Central and Northern
European successors, the Linienbandkeramik (LBK) and Stichbandkeramik
(SBK).
The AVK apparently developed in situ within the Great Hungarian Plain,
directly out of its Early Neolithic (Körös and Szatmár)
predecessors (Kalicz and Makkay 1977; Makkay 1982), sometime during the
middle of the sixth millennium BC. Roughly contemporary with the transition
from Starcûevo to Vincûa further south in Yugoslavia, the transition from
Körös to AVK in the Plain is also characterized by ceramic changes.
In the Great Hungarian Plain, this period is marked by the appearance
of incised, linear decoration on open-shaped vessels. While AVK pottery
is typically decorated with white paint, the early Vincûa pottery is typically
dark and burnished. Roughly simultaneous with this development in the
eastern Carpathian Basin, the LBK appears in Transdanubia (for a recent
synthesis of the Neolithic in Transdanubia, see Kalicz 1998). Makkay (1982:42-43)
suggests that the AVK developed out of the Szatmár II group in
eastern Hungary, and the LBK from the Bicske Group.
Kosse (1979) noted that AVK sites occupy a much wider range of environments
than sites of the preceding Körös Culture, penetrating into
forest zones hitherto unoccupied during the Neolithic. Correlated with
this shift in settlement expansion, Kosse (1979:150-151) recorded a shift
towards the more intensive exploitation of locally available domesticated
animals and cultivars:
In the Linear Pottery culture, the wheat-sheep-aquatic/wild resource economic
pattern of the Körös culture underwent several changes, the
best documented of which is the shift to locally available domesticated
animals. Cattle replaced sheep as the most important species, and pigs,
which had been almost negligible at the Körös sites, became
equally or more important than sheep. Aurochs and wild swine are both
indigenous to much of temperate Europe, and the increase in the number
of their domesticated counterparts at the Linear Pottery sites was without
doubt the result of local domestication (Kosse 1979:150-51).
This basic trend has been explored further by Vörös (1994),
who documented a shift in the relative number of domestic to wild animal
bones in AVK sites (94-98% domestic vs. 2-6% wild), and in later AVK/early
Tisza sites (63-78% domestic vs. 22-37% wild). A wider range of domesticated
plants, cereals, and legumes, began to be utilized during this period.
In addition to the Early Neolithic complex of einkorn and emmer wheat,
two-row hulled barley and millet, breadwheat and lentils also began to
be cultivated.
Towards the end of the Middle Neolithic, about 5,100 BC, the previously
homogeneous AVK cultural assemblage gave way to more spatially-discrete
ceramic groupings within the Great Hungarian Plain (Bognár-Kutzián
1966; Kalicz and Makkay 1977). As Sherratt (1997b:280) noted:
On the lower and middle Tisza and along the Körös, the Szakálhát
group is distinguished by pottery ornamented with paint outlined by incised
decoration. To the north of this the Esztár group occupied a wide
territory on the Nyírség, Szamos and upper Berettyó,
in which pottery with dark painted ornament was used. Various smaller
groups emerged on the fringes of the northern mountains: Szilmeg in the
Bükk foothills, Tiszadob in the Sajó valley, and Bükk
in the mountains themselves, with exceptionally fine incised and occasionally
painted pottery. All of these groups are distinguished by their characteristic
finewares, which occur in smaller quantities as imports in each others
areas.
Sherratt attributed this small-scale cultural distinctiveness to economic
differentiation, and to increased trade between the obsidian-bearing regions
in the mountainous Tokaj region and the Plain.
The Late Neolithic Tisza-Herpály-Csöszhalom Complex
The trend towards regional differentiation that began initially with the
sub-division of the Carpathian Basin into two discrete cultural complexes
AVK (on the Plain) and DVK (Dunatúl Vonaldiszes Kerámia,
or Transdanubian Linear Pottery) continued throughout the Middle
Neolithic in the Great Hungarian Plain (e.g., Szakálhát,
Esztár; Tiszadob). This resulted in the division of the region
into three discrete cultural groups during the Late Neolithic,
known as the Tisza-Hérpály-Cso‡szhalom complex (see Figure
4). Within the wider context of central, eastern, and southeastern Europe,
this complex is roughly contemporary with Lengyel (I-II) in Transdanubia,
and the Petres,ti culture in Transylvania (for discussions see Kalicz
and Raczky 1987a:25-27; Raczky 1988).
In their recent synthesis of Late Neolithic research on the Plain, Kalicz
and Raczky (1987a) traced the concept of a younger, final, phase of the
Neolithic to Tompas (1929) influential article:
[Tompa] assigned the Lengyel culture of Transdanubia to the younger, second
phase of the Tisza culture, and traced its development to the Transdanubian
expansion of the Tisza population. In fact, Tompa had correctly identified
the culture complexes that are even today regarded as the main representatives
of the Late Neolithic in Hungary (Kalicz and Raczky 1987a:11).
Today, the Late Neolithic of the Great Hungarian Plain is understood to
be represented by three regionally-discrete cultures, as they
are known in Hungarian literature. These sub-groups Tisza, Herpály
and Cso‡szhalom were initially identified by differences in ceramic
styles, and have more recently received support by the identification
of regional differences in settlement patterns and subsistence (Kalicz
and Raczky 1987a:13-14).
The Early Copper Age Tiszapolgár Culture
In stark contrast to the Late Neolithic of the Great Hungarian Plain,
which has occupied the main focus of Hungarian prehistorians for the last
thirty years, the succeeding Early Copper Age has received significantly
less attention. With a few exceptions, the vast majority of information
regarding the Early Copper Age Tiszapolgár culture has been collected
from cemeteries. To date, only a handful of Tiszapolgár settlement
sites have been even partially excavated (see Szabó 1934; Bognár-Kutzián
1972:164-171; Goldman 1977; Siklódi 1982, 1983; Skomal 1983). The
comment made decades ago by Bognár-Kutzián (1963:15) remains
almost as true today as it was then, [T]he Early Copper Age is one
of the most neglected fields of prehistoric research in Hungary.
Compared to the three relatively distinct ceramic groups that characterized
the Great Hungarian Plain during the end of the Neolithic, Early Copper
Age Tiszapolgár pottery is remarkably homogeneous across the entire
Plain. Characterized by unpainted and usually polished surfaces, Tiszapolgár
vessels frequently are decorated with knobs (also called bosses) and lugs
that are sometimes pierced, or semi-pierced. In her initial typological
analysis of the pottery from Basatanya, Bognár-Kutzián (1963:236-99)
identified thirteen different vessel types, ranging from small tumblers
(type A) to large storage jars (type D) and cooking pots (type G). Each
of these types (A-M), was then sub-divided into variants (e.g., C3) and
subvariants (e.g., C3c), each of which referred to only a handful of specific
vessels (see Bognár-Kutzian 1963:figures 1-10). The most diagnostic
vessel types of the Early Copper Age have hollow-pedastalled bases, which
are frequently pierced (Bognár-Kutziáns types H, I
and J), and often quite large. In a subsequent synthetic publication,
Bognár-Kutzián (1972) added an additional three types to
the thirteen she identified at Basatanya (types N,O, and P), creating
an explicit, if cumbersome method of classification.
The area occupied by the Tiszapolgár culture extended from the
Banat in northern Yugoslavia, across the entire Hungarian Plain, into
the foothills of Transylvania, and into the mountains of southern Slovakia
(see Figure 5). This area corresponded roughly to the area that previously
had been occupied by the Tisza-Herpály-Cso‡szhalom groups during
the Late Neolithic, but extended to slightly higher elevations in the
east and north. Bognár-Kutzián (1963, 1972) envisioned the
Tiszapolgár culture as a direct cultural extension of these preceding
Late Neolithic groups, as do most other researchers working in the region.
The Middle Copper Age Bodrogkeresztúr Culture
Bodrogkeresztúr is generally understood to be a direct temporal
extension of Tiszapolgár into the Middle Copper Age. Continuity
between the two periods is supported both by continual habitation at settlement
sites (e.g., Vészto‡-Mágor) and cemeteries (e.g., Tiszapolgár-Basatanya),
and also by overlapping radiocarbon dates, which suggest that the two
periods overlapped considerably (see also Forenbaher 1993). The break
between the two periods is therefore somewhat arbitrary, and generally
corresponds to minor changes in ceramic vessel form and decoration. In
contrast to Tiszpolgár, Bodrogkeresztúr ceramics are characterized
by closed vessel types (especially milk jars) and by incised
squares decoration within meandric bands. Other decorative techniques
of the period include tight combinations of dotted and linear incisions
with white encrustation. These additional elements are added to those
of the Tiszapolgár ceramic tradition.
The geographic extent of Bodrogkeresztúr generally continues that
of the Tiszapolgár, but for the first time some sites are located
on the sandy interfluvial zone between the Danube and the Tisza (see Figure
6). In addition, the area between the Jászág and the Danube
bend, which previously had been occupied by Lengyel sites, became incorporated
into the Bodrogkeresztúr sphere (see Banffy 1994:294). Sherratt
(1997c) suggests that the center of the Plain became depopulated during
this time, as settlements became more concentrated on the edge of the
Plain.
Similar to the preceding period, the vast majority of information for
the period is known from the excavation of large cemeteries, in particular
Tiszapolgár-Basatanya (Bognár-Kutzián 1963) and Tiszavalk-Kenderföld
(Patay 1978a,b). The separation of settlement from cemetery, already established
during the Early Copper Age, continued. In addition to the grave goods
commonly associated with Tiszapolgár burials, copper axes begin
to be found in increasing regularity in burials and also as stray finds
(see Sherratt 1997b:294).
It generally is assumed that Bodrogkeresztúr populations continued
the subsistence practices of their Tiszapolgár predecessors. Settlements
during the Middle Copper Age are similar to those of the preceding period
they tend to be small, and dispersed. One anomalous settlement,
Szarvas 38 (Makkay 1983), contains a large roundel reminiscent of Lengyel
sites and may be indicative of increasing contact between the Great Hungarian
Plain and Transdanubia (i.e., the Balaton-Lasinja culture) during this
time. Increasing contact throughout the Carpathian Basin is also indicated
by the presence of sites in the previously uninhabited frontier zone between
the Danube and the Tisza.
The Late Copper Age BolerázBaden, Pécel, and Kurgan
Cultures
The Late Copper Age in the Great Hungarian Plain marks the incorporation
of the region into a larger sphere of interaction that extends throughout
most of central Europe, ca. 4,000-3,000 BC. On the Alföld, this time
period corresponds to the Boleráz and Baden, or Pécel cultures.
Baden sites are distributed throughout Hungary, westernmost Romania, eastern
Austria and southern Slovakia. The settlement pattern indicates increased
movement into upland regions, and into the sandy interfluve between the
Danube and Tisza rivers. The pottery is characterized by handled jugs
and cups, which suggest affinities with Bulgaria, northern Greece, and
the Aegean. The ceramic types bear formal affinities that link it closely
with neighboring archaeological cultures, such as Cot,ofeni in western
Romania, Ezero in the south, and Cernavoda in the Danube/Dobrogea area.
Several of the cultural practices that had begun during the Early and
Middle Copper Age persist throughout the later Copper Age, including the
tradition of placing the dead into large, formal cemeteries, such as Alsónémedi
(cf. Korek 1951; Némeskeri 1951; Bökönyi 1951).
While certain cultural features suggest a high degree of continuity with
the previous period, others suggest that several of those features that
had been adopted at the beginning of the Copper Age began to assume a
different social role during the later Copper Age. For example, cattle,
which had begun to dominate faunal assemblages during Tiszapolgár
times, occur in several Baden burials throughout the Plain (see Whittle
1996:122-126), suggesting an increased emphasis in their role probably
as producers of secondary products (see Sherratt 1983a).
Another feature that characterizes the later Copper Age is the multitude
of pit-grave kurgans (i.e., mounded tumuli) that dot the relatively flat
landscape of the Plain (see Ecsedy 1979). The burials found in such tumuli
are frequently covered in red ocher and the associated ceramics suggest
affinities with cultures further to the east, on the south Russian steppe
(Yamna Culture). Although the chronological relationship between the kurgans
and the Baden sites remains unclear, Sherratt (1997b:310) has noted that
the distribution of the kurgans in the Körös basin are spatially
exclusive of the Baden sites. This led him to suggest that the kurgan
builders may have been an intrusive group from the east that selectively
inhabited those areas that were unoccupied by indigenous Baden agricultural
groups (see also Ecsedy 1979).
The vast majority of later Copper Age settlement sites consist only of
a few pits. As a result, it is nearly impossible to draw conclusions regarding
the relationship between the Baden and kurgan burial traditions based
upon information from settlements. This is unfortunate, given the various
social changes that occur at the beginning of the Bronze Age in the region
(see OShea 1996).
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