ACTA
UNIVERSITATIS
https://doi.org/10.12775/AUNC_ARCH.2022.003
NICOLAI
COPERNICI
ARCHEOLOGIA XXXVIII, 2022, 19–34
Instytut Archeologii, Uniwersytet Mikołaja Kopernika w Toruniu
jkukawka@umk.pl
Jolanta Małecka-Kukawka
JURASSIC-CRACOW FLINT IN THE NEOLITHIC
OF THE CHEŁMNO LAND
Abstract. This paper provides an overview of the empirical results on the Jurassic-Cracow flint use by the communities of the Linear Band Pottery culture,
Late Band Pottery culture, and Funnel Beaker culture during the Neolithic in
the Chełmno Land. The picture emerging at this moment is that the Chełmno
Land did become a part of flint trading network established already in the early
Neolithic by the Linear Band Pottery communities, and running from the southern
and south-eastern flint mines located in the Holy Cross Mountains (Świeciechów
flint, ‘chocolate’ raw material), Polish Jura ( Jurassic-Cracow flint), and the Volhynian-Podolian Upland (‘Volhynian’ raw material).
Keywords: Neolithic, Chełmno Land, Jurassic-Cracow flint, distribution of flint
raw materials.
INTRODUCTION
The settlement of the Chełmno Land by the early agricultural communities
of the Balkan-Danube tradition took place in the mid-6th millennium BC.
Thanks to the research conducted since the end of the 1970s, it was established
that the Chełmno Land was the most north-eastern area of intense early Neolithic settlement – the Linear Band Pottery culture (LBK) in its European range.
As a result of surface surveys, tests and open-area excavations, about 300 sites
of this culture have been discovered to date (Kukawka, Małecka-Kukawka,
Wawrzykowska 2002, pp. 91–107; Małecka-Kukawka 2017; Kukawka, Małecka-Kukawka 2018; Fig. 1). The aforementioned research has revealed traces
of intensive settlement of the area by chronologically later Neolithic cultures,
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Jolanta Małecka-Kukawka
i.e. the Late Band Pottery cultures1 (LBPC) with nearly 400 sites, and the
Funnel Beaker culture (TRB) with around 1800 sites. The number and distribution of sites clearly indicate that there was a separate settlement region in the
Chełmno Land. Today it can be considered one of the best examined regions
in Poland. It is also worth emphasising that the Chełmno Land is considered
to be the north-eastern frontier of the European Neolithic world for over 2500
years (Kukawka, Małecka-Kukawka 2018).
The Chełmno Land, like other regions of the Polish Lowlands, is devoid
of high-quality natural silica deposits. Previous studies on Neolithic flint production have shown that this area was involved in the long-distance exchange
of raw materials of silica rocks from the south, i. e. the flint bearing margin of
the Holy Cross Mountains ( Jurassic-Cracow flint, Świeciechów flint, chocolate
flint) and the south-east, i.e. the Ukrainian Upland (‘Volhynian’ raw materials;
Małecka-Kukawka 1992; 2001; 2002; 2008; 2017).
The identification of these macroscopically different raw materials usually
does not pose any issues, especially in the case of the most characteristic ones –
chocolate flints, Świeciechów flint and striped flint. Correct identification of
the Jurassic-Cracow flint is much more problematic, especially in relation to
the variations of the chocolate colour (in the ‘Olszanica’ type), sometimes
mistakenly referred to as the ‘chocolate’ flint (see Lech 1980, p. 209; Małecka-Kukawka 2017, p. 67).
The aforementioned research on the Neolithic, commenced in the late
1970s, revealed a rich settlement of the Linear Band Pottery culture from
the earliest horizon of this culture’s settlement in Poland (Kirkowski 1994,
pp. 57–99). From the perspective of the ‘flint production’, the results of the research at the sites 41 and 43a in Boguszewo were particularly spectacular, since
the dominant raw material found was Jurassic-Cracow flint (Małecka-Kukawka
1992). These discoveries effectively challenged the then widely accepted vision
of the neolithisation of the Polish Lowlands (Kirkowski 1994, pp. 57–99). One
1 In the text I use the term ‘Late Band Pottery culture’, introduced by Lech Czerniak
(1980), to denote phenomena that took place after the disappearance of the Linear Band Pottery
culture. We used this term consistently in many publications concerning the Neolithic period of
the Chełmno Land. Contemporary proposals of the creator of this term introduce corrections,
narrowing the LBPC phenomenon to the Kuyavian phases I–IIa (the stage with incised elements).
L. Czerniak treats the later development stages separately, proposing to use the term ‘Brześć
Kujawski culture’ (Czerniak 2017, pp. 199–236). Since the studies on the settlement structures
after the disappearance of the LBK (for various, largely non-scientific reasons) have stalled in
the Chełmno region, I do not see the possibility of applying this new taxonomic systematics to
the sources obtained to date.
Jurassic-Cracow flint in the Neolithic of the Chełmno Land
21
had to be wary to name these findings ‘an anomaly’ due to Jurassic-Cracow
flint being discovered so far north from its point of origin. For that reason the
inventories travelled several times to the South, so that they could be examined
by the researchers of flint mines and experts in flint raw materials (I participated
in this process myself, as a young ‘flint maker’ among the team of apprentices in Igołomia under the watchful and demanding eye of Jacek Lech and
Władysław Morawski). Despite many consultations regarding the specimens
from Boguszewo, and from the sites discovered in subsequent years, issues
with unambiguous identification of raw material arose (some specimens had
‘mixed’ features – translucency, siliceous mass structure, fracture nature, cortex,
etc., which made it impossible to categorically state whether the specimen is
Jurassic-Cracow flint or chocolate flint). In such cases, I decided to place them
in the ‘undefined raw material’ category, with the possible suggestion that it is
of South Polish origin (see Małecka-Kukawka 2001, pp. 22–58).
After many years the issue of these ‘undefined’ products could be revisited
thanks to the development of various archeometric methods in cooperation
with other sciences (Werra, Siuda, Małecka-Kukawka 2018, pp. 211–224).
Petrographic and geochemical analyses showed that some of the several specimens, which I included in the group of undefined materials, can be considered as made of Jurassic-Cracow flint. However, in some cases of the analysed
specimens, the results are neither unequivocal nor satisfactory. It is hoped that
further research will contribute to increasingly better identification methods
of flint materials used in prehistory.
Researchers of Kuyavia, adjacent to the Chełmno Land, faced similar difficulties in identifying the Jurassic-Cracow flint. For example, in the publication
regarding the flint materials from site Grabie 4 from 1995, Lucyna Domańska
states that out of all 75 products, 38 (50.7%) were made of Jurassic-Cracow
flint. The rest are Baltic erratic flint or burnt specimens. This information was
repeated by Jacek Kabaciński (2010, p. 202) and me in 20172 (Table 1.46). In her
paper from 2016, L. Domańska proposes a different raw material composition
of the flint inventory from the site, with the presence of 31 Baltic erratic flint
products, 31 of Jurassic-Cracow flint, 7 of chocolate flint and 6 burnt ones
(pp. 32–33). Unfortunately, the author did not explain the reasons for the
change of raw material determination. The updated data was later used in the
2 Unfortunately, the book by L. Domańska Change and Continuity. Traditions of the Flint
Processing from the Perspective of the Tążyna River Valley came to me after the monograph was
submitted for printing.
22
Jolanta Małecka-Kukawka
publication by Joanna Pyzel and Marcin Wąs (2018, pp. 181–194). This change
is only seemingly trivial, as it concerns only seven specimens of the hitherto not
determined chocolate flint on the site, which aims to represent the earliest stage
of the Linear Band Pottery culture settlement in Kuyavia. However, it has quite
significant consequences in the interpretation of the raw material distribution
systems in the early Neolithic, which will be discussed later.
SOURCES
This part of the text will present the information on the composition of
the raw materials of the Chełmno Land inventories analysed up to date, in
three main cultural horizons – the Linear Band Pottery culture (LBK), the
post-Linear cultures (LBPC) and the Funnel Beaker culture (TRB).
In Table 1, concerning the LBK, not only the numbers of inventories, but
also the size of the investigated area of the site is given, and there is a specific
reason behind this, namely the difference between planned and ‘rescue’ research. I have discussed the quality of research, specifically the so-called ‘large
line investments’, in my monograph from 2017. Here I will only indicate that
‘planned’ research (in the case of the Chełmno Land it is usually carried out on
a small scale) provides many times more flint material in comparison to research
performed during a ‘rescue’ excavation covering large areas. Of course, this
does not only apply to research in the Chełmno Land.
In the tabular presentation of the raw material structure of the LBK flint
materials, local erratic flints were treated jointly (varieties I and II – Pomeranian
flint, due to the occasional use of this pebble flint). Burnt and undefined flints and
other varieties of flints that occur incidentally (raw material from Świeciechów
and Volhynian flints, which appeared in the discussed collection in the total number of three specimens, which constitutes about 0.1% of all the flints considered)
were also excluded. In the ‘inventory quantity’ column, the number of all flints
from a given site is provided, therefore the sum of products from the three raw
materials included in the table may be lower than the entire inventory quantity
in the last column. This procedure makes it possible to trace the dynamics of the
inflow of southern Poland raw materials and the scale of use of local erratic flints.
The goal is to maintain the analytical comparability of the presented assemblages
(for example, 273 specimens come from site 2 in Stolno, but 144 of them are
heavily burnt, hence only the set from feature 1 was taken into account, as only
for this set the raw material analysis could be performed).
[ 23 ]
Table 1. Quantities of flint inventories of the Linear Band Pottery culture in the Chełmno Land
(after Małecka-Kukawka 1992; 2001; 2017; Osipowicz et al. 2012; Werra 2013)
Tab. 1. Liczebność inwentarzy krzemiennych ze stanowisk kultury ceramiki wstęgowej rytej
z ziemi chełmińskiej (za Małecka-Kukawka 1992; 2001; 2017; Osipowicz i in. 2012; Werra 2013)
*
No.
Phase*
Site, No.
1
2
3
4
5
6
7
8
9
10
11
12
13
13
Total
Ib
Ib
Ib
Ib
IIa1
IIa1
IIa1
IIa2
IIa2
IIa2
III
III
III
?
Boguszewo, site 41
Boguszewo, site 43a
Gruta, site 52
Klęczkowo, site 8**
Bocień, site 5**
Lisewo, site 31
Annowo, site 7
Bocień, site 5**
Ryńsk, site 42
Stolno, site 2, feature 1
Wielkie Radowiska, site 22
Wielkie Radowiska, site 24
Małe Radowiska, site 17
Nowy Dwór, site 9
Inventory
quantity
135
34
57
60
167
55
253
73
98
81
82
394
83
866
2420
Size of site’s
excavated area
355 m2
200 m2
2
6 m (test trench)
38 435 m2
9675 m2
86 m2
10 m2 (survey)
9675 m2
100 m2
160 m2
237 m2
155 m2
213,5 m2
1200 m2
Division into phases according to Werra 2013.
Pre-construction excavations of the A1 motorway.
**
Table 2. Raw material structure of the flint inventories of the Linear Band Pottery culture from
the first development phase in the Chełmno Land*
Tab. 2. Struktura surowcowa inwentarzy krzemiennych z pierwszej fazy kultury ceramiki
wstęgowej rytej na ziemi chemińskiej
No.
Phase
Site, No.
nb
cz
jp
1
2
3
4
5
Total
I
I
I
I
I
Boguszewo, site 41
Boguszewo, site 43a
Gruta, site 52
Klęczkowo, site 8
Nowy Dwór, site 9
35
2
18
31
60
146
3
–
2
9
50
64
86
29
32
20
280
447
Inventory
quantity**
135
34
57
60
405
691
Burnt and undefined specimens were excluded from the table.
The inventory quantity takes into account all flints from a given site (including burnt and
undefined in raw material terms).
nb – Baltic Erratic flint, cz – Chocolate flint, jp – Jurrasic-Cracow flint
*
**
24
Jolanta Małecka-Kukawka
The first phase of the settlement of the Chełmno Land by the LBK population
(Fig. 1), which is distinguished by the analyses of pottery materials and further
supported by other analyses (including radiocarbon dating), is within the oldest
horizon of settlement of Polish lands in general (Małecka-Kukawka 2017; Werra
2013). The most characteristic feature of flint materials, considering the earliest
settlements, is a very high proportion of Jurassic-Cracow flint. Artifacts made
from this type of flint constitute from about 60% to over 90% of all specimens from
individual sites determined in terms of raw materials, which gives an average of
about 70%. The second largest group of used flint in the analysed inventories is the
local Cretaceous erratic flint (slightly over 20% on average), while the chocolate
flints (of various provenance, see Małecka-Kukawka 2017, p. 45) constitute the
least numerous group of products, on average a little less than 10%.
Fig. 1.
Distribution of the Linear Band Pottery culture sites in the Chełmno Land. The sites
of the stage I of development are marked in red: 1. Boguszewo, site 41; 2. Boguszewo,
site 43a; 3. Gruta, site 52; 4. Klęczkowo, site 8; 5. Nowy Dwór, site 9 (based on Werra
2013, graphic design by Ł. Kowalski)
Ryc. 1. Rozmieszczenie stanowisk kultury ceramiki wstęgowej rytej na ziemi chełmińskiej. Na
czerwono zaznaczono stanowiska I fazy rozwoju: 1. Boguszewo, stan. 41; 2. Boguszewo,
stan. 43a; 3. Gruta, stan. 52; 4. Klęczkowo, stan. 8; 5. Nowy Dwór, stan. 9 (na podstawie
Werra 2013, opracowanie graficzne Ł. Kowalski)
25
Jurassic-Cracow flint in the Neolithic of the Chełmno Land
Table 3. Raw material structure of the flint inventories of the Linear Band Pottery culture from
the second and third development phases in the Chełmno Land*
Tab. 3. Struktura surowcowa inwentarzy krzemiennych z drugiej i trzeciej fazy kultury ceramiki
wstęgowej rytej na ziemi chełmińskiej
No.
Phase
Site, No.
nb
cz
jp
1
2
3
4
5
6
7
8
9
10
Total
II (?)
IIa1
IIa1
IIa1
IIa2
IIa2
IIa2
III
III
III
Nowy Dwór, site 9
Bocień, site 5
Lisewo, site 31
Annowo, site 7
Bocień, site 5
Ryńsk, site 42
Stolno, site 2, feature 1
Wielkie Radowiska, site 22
Wielkie Radowiska, site 24
Małe Radowiska site 17
165
27
22
16
43
30
72
4
101
33
513
165
93
17
168
42
39
7
74
226
39
870
81
1
4
4
2
1
–
–
13
4
110
Inventory
quantity**
461
132
55
253
90
98
81
82
394
83
1729
Burnt and undefined specimens were excluded from the table.
The inventory quantity takes into account all flints from a given site (including burnt and
undefined in raw material terms).
nb – Baltic Erratic flint, cz – Chocolate flint, jp – Jurrasic-Cracow flint
*
**
In the following, distinguished phases of settlement of the Chełmno Land
(II and III) there is a clear change in the raw material composition of the
analysed inventories, according to the source data. The most numerous are
products made of chocolate flints (nearly 60% on average), the second most
frequent is Baltic erratic flint (on average nearly 35%), and the share of products
made of Jurassic flint is approximately 7% on average.
The Late Band Pottery culture
Despite the discovery of a significant number of sites within the AZP (Archaeological Map of Poland), related to the LBPC settlements (about 400),
further research is needed, since excavation research was carried out on only
a few sites. Promising research on the multicultural site 12 in Zelgno, where
traces of six or seven (depending on the interpretation of the ditch’s direction) trapezoidal houses were discovered, was not published up to date (see
Małecka-Kukawka 2017, pp. 13–15). Hence, the knowledge of flint production
is modest, as it was based only on the results of analyses from a very limited
26
Jolanta Małecka-Kukawka
number of sites. Furthermore, the analysis considered only few selected features: Firlus, site 8; Radzyń Wieś, site 21; Linowo, site 20; Świecie nad Osą,
site 26 (Małecka-Kukawka 1992; 2001); Trzciano, site 40 (Osipowicz et al.
2015, pp. 139–164); Małe Radowiska, site 17, feature 53 (Osipowicz 2016,
pp. 237–258). There are numerous sites with pottery related to this horizon.
However, the issue at hand is that they are usually multicultural objects, often
in the palimpsest ‘Neolithic’ sequence of settlement. Hence, it is not possible
to unambiguously assign flints to any of the cultures.
In general, on sites related to the LBPC, we can observe an almost complete
disappearance of the inflow of southern Poland raw materials, including the
Jurassic-Cracow flint. Only on the site 8 in Firlus, representing the early horizon
of the LBPC with incised ornaments, chocolate flint products account for less
than 20% of the total inventory (after excluding burnt and undefined specimens,
Małecka-Kukawka 2001, p. 51). In addition, it is worth noticing that the LBPC
population often used a pebble variety of erratic flint (‘swallow breads’).
The Funnel Beaker culture
The raw material structure of the vast majority of flint inventories related to the Funnel Beaker culture was published in the volume Krzemień
świeciechowski w pradziejach (Małecka-Kukawka 2002, pp. 155–175). Raw
materials of southern Poland origins (chocolate flints, Świeciechowski flint,
incidentally striped flint) and from the Ukrainian Upland (Volhynian flints)
were discovered in the Chełmno Land. The products made from Jurassic flint
were identified only on three sites: Wełcz Wielki, site 10B, Mgoszcz, site 2
and Niemczyk-Wrocławki, site 1. One type of specimen was found on each
of the sites (Małecka-Kukawka 2002, Plate 1). In terms of morphology, these
are blades (Wełcz Wielki 10B and Mgoszcz 2, Małecka-Kukawka 2001, Plates
26:5; 29:3) and a fragment of retouched blade (Niemczyk-Wrocławki 1, Plate
26:11).
Due to the popularity of this flint in the LBK, it cannot be ruled out that
the products were made from material which was local for the TRB population,
they could have simply been found on the surface (reuse). This remark may
also apply to a number of products made of chocolate flints, which is difficult
to estimate.
Jurassic-Cracow flint in the Neolithic of the Chełmno Land
27
DISCUSSION
The Jurassic-Cracow flint is an inseparable component of the material
equipment of the oldest farmers in the Chełmno Land. The obtained source
data shows that the first migrants (the fact that they were migrants, according
to the latest research, including genetic studies, is undisputed) from the South
(i.e. historical region of Lesser Poland, pol. Małopolska) came to the Chełmno
Land bringing the Jurassic-Cracow flint, which was most probably necessary in
their culture (everyday life). Site 9 in Nowy Dwór, Kowalewo Pomorskie commune, seems to be of the key importance for understanding the flint production
phenomenon, to which I devoted a significant part of my monograph from
2017. The analyses show that the oldest part of the remains of the settlement is
undoubtedly feature 26 with the richest inventory from the site. These are 185
products (several dozen chips below 10 mm in diameter have been omitted)
and 82% of all products were made from the Jurassic-Cracow flint, 12.3% from
chocolate flints. The remaining less than 5% is made up of erratic and burnt flint
products (Małecka-Kukawka 2017, Plate 1.15.). The stratigraphy of this feature
is also important: 95% of the discovered materials were found in the bottom
layers, covered with an almost sterile layer with a laminated structure, which
suggests a natural way of backfilling the feature after cessation of activity in its
surroundings. This pit played the role of a ‘dump’ of waste from the processing
of flint, mainly the Jurassic-Cracow one, as evidenced by the presence of flint
cores and several dozen very fine chips, 113 flakes and waste, including 99 from
Jurassic flint (Małecka-Kukawka 2017, Plate 1.28, pp. 42–43).
If the findings regarding the dynamics of the settlement of the site in Nowy
Dwór are correct (and they were based only on the analysis of flint materials,
planigraphy and features’ stratigraphy, Małecka-Kukawka 2017, pp. 14–15),
it can be suggested that the settlers brought the necessary flints, including
the Jurassic-Cracow (which they processed, as evidenced by the materials
from feature 26) and a few products made of chocolate flint. In the course of
the settlement’s growth, the raw material structure changed, the number of
products made of the Jurassic-Cracow flint decreased significantly in favour of
chocolate flints (from various outcrops), and the number of products made from
local raw materials also increased (Małecka-Kukawka 2017, pp. 13–105).
Comparing the data on the raw material structure of the flint inventories
of the oldest phase of the LBK settlement in the Chełmno Land, it can be
stated that the Jurassic-Cracow flint was of a significant importance for the
first settlers. However, in almost every case, products made from this flint were
28
Jolanta Małecka-Kukawka
accompanied, albeit in small numbers, by specimens made of chocolate flints.
Local erratic flints were also used from the very beginning.
I will return now to the issue of raw material identification (especially
the Jurassic-Cracow flint) in relation to the neighbouring Kuyavia region.
According to previous publications, on two of the four sites, which are used to
define the oldest horizon of the LBK settlement in Kuyavia, the only ‘imported’
flint raw material was the Jurassic-Cracow flint (site 4 in Miechowice, Grygiel
2004, p. 361 ff.; site 4 in Grabie, Domańska 1995). This could suggest that these
first migrants did not know the chocolate flint outcrops yet, but were aware
of the places where the Jurassic-Cracow flint occurred. The structure of the
raw materials recently published (Domańska 2016) shows that, apart from the
Jurassic-Cracow flint, these oldest LBK settlers had various southern Poland
resources in their flint equipment.
Examples from the Chełmno Land, especially materials from Nowy Dwór,
show that from the beginning of the LBK settlement, the settlers ‘preferred’
the Jurassic-Cracow flint, but they also knew and used other south Poland flint
raw materials. They exploited local flints for their needs, which they collected
in the places where they decided to settle.
Compared to the stage I of the LBK development in the Chełmno Land,
chocolate flints clearly dominate in the subsequent stages of settlement, although their frequency is lower than that of the Jurassic-Cracow flint in the
older phase. It is also worth paying attention to the constant presence of various
products made of local erratic flints, from the oldest stage of settlement until
the end of the LBK existence. The share of local raw materials varies from site
to site. For example: in materials from site 2 in Stolno, the Baltic erratic flint
accounts for about 91% of the inventory, and the chocolate flint is only about
9%, while in the case of the inventory from site 22 in Wielkie Radowiska the
situation is the opposite – 95% of total products are made of chocolate flint,
while 5% of specimens are made of erratic raw materials.
The indicated differences are probably a result of many factors, of which – I believe – the important role is played by factors related to the method of obtaining
the material (circumstances of the research, soil type, weather conditions, etc.).
However, in the case of the two sites in question, the excavations were conducted
by one researcher, Ryszard Kirkowski, using the same methodology of excavation
works. On both sites, small areas were examined (see Table 1), which may indicate
the randomness of such studies. Perhaps features with different functions within
the settlement were excavated. Unfortunately, we do not know the structure of
the remains of the LBK settlement on these sites.
Jurassic-Cracow flint in the Neolithic of the Chełmno Land
29
However, despite the aforementioned differences, based on the raw material analysis of flint sources, it can be concluded that the Jurassic-Cracow flint
dominated during the earliest stages of settlement of the Chełmno Land, as
well as the Kuyavia region, and was later ‘replaced’ by chocolate flints.
CONCLUSIONS
The presented raw material structure of flint materials from sites associated
with the Linear Band Pottery culture, Late Band Pottery culture, and Funnel
Beaker culture allows for the identification of significant differences when
it comes to the inflow of the Jurassic-Cracow raw material (and others, of
southern Poland and south-eastern origin).
The most intense inflow of this raw material took place during the first
agricultural communities, and, at least in the Chełmno Land, it refers to the
early period of the LBK settlement (Table 2). It is worth noting that almost
three times more specimens made from the discussed raw material (nearly 600)
come from the sites located in the Chełmno Land than from Kuyavia (less than
250, Małecka-Kukawka 2017, Plate 1.46). Based on the unique flint cores found
on site 41 in Boguszewo, with a characteristic black coating (Figs. 2 and 3), it
can be assumed that the LBK communities began flint deposits exploitation in
the area of the Jura Ojcowska (Lech 2006, pp. 400–401, 423).
In subsequent stages of development, until the noticeable disappearance of
this culture, the intensity of the inflow of chocolate flints increases. Although
the Jurassic-Cracow flint appears in materials from sites with later chronology,
their number clearly decreases. On some sites only a single artifact made of
the Jurassic-Cracow flint can be found, on other sites no presence of this flint
was recorded at all.
After the disappearance of the LBK, the distribution of mine raw materials
changed dramatically. Apart from a single site, from the early (incised) phase
of the LBPC, where almost 20% share of chocolate flints was recorded, there
are virtually no raw materials of southern origin on other sites. The collapse
of the raw material distribution system after the disappearance of the LBK is
observed not only in the Chełmno Land. A similar phenomenon took place
in Kuyavia and Silesia (Kabaciński 2010, pp. 184–186, further references
there).
In the Funnel Beaker culture, the Jurassic-Cracow flint was not distributed,
the few identified specimens (two blades and a fragment of retouched blade)
Fig. 2.
Boguszewo, Grudziądz district, site 41. Core made of Jurassic-Cracow flint
(photo by W. Ochotny)
Ryc. 2. Boguszewo, pow. grudziądzki, stan. 41. Rdzeń z krzemienia jurajskiego podkrakowskiego (fot. W. Ochotny)
Fig. 3.
Boguszewo, Grudziądz district, site 41. Slight close-up of the core of Jurassic-Cracow flint with visible black mine coating (photo by W. Ochotny)
Ryc. 3. Boguszewo, pow. grudziądzki, stan. 41. Niewielkie powiększenie rdzenia
z krzemienia jurajskiego podkrakowskiego z widocznym czarnym nalotem
pochodzenia kopalnianego (fot. W. Ochotny)
Jurassic-Cracow flint in the Neolithic of the Chełmno Land
31
should rather be associated with the Linear Band Pottery culture. Most likely
they were found on the surface and reused by the TRB communities.
The presented rhythm of changes in the distribution of the Jurassic-Cracow
flint is of course a generalisation and, in a sense, a simplification. Probably, the
system of exchange of raw materials was a much more complicated process.
Nevertheless, it reflects the dynamics of changes that took place during the
functioning of the early and middle Neolithic communities in the Chełmno
Land. It also confirms the existence of an extensive and multidirectional Jurassic
flint exchange network among the oldest agricultural communities (see Lech
2006, p. 402).
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KRZEMIEŃ JURAJSKI PODKRAKOWSKI W NEOLICIE
ZIEMI CHEŁMIŃSKIEJ
Słowa kluczowe: neolit, ziemia chełmińska, krzemień jurajski podkrakowski,
dystrybucja surowców krzemiennych.
Streszczenie
Artykuł prezentuje dane dotyczące materiałów krzemiennych z surowca jurajskiego
podkrakowskiego w inwentarzach kultury ceramiki wstęgowej rytej, kultury późnej ceramiki wstęgowej i kultury pucharów lejkowatych. Dotychczasowe studia nad krzemieniarstwem
neolitycznym wykazały, że obszar ten był włączony w dalekosiężną wymianę surowców ze
skał krzemionkowych pochodzących z południa – z krzemienionośnego obrzeżenia Gór
Świętokrzyskich (krzemień jurajski podkrakowski, krzemień świeciechowski, krzemienie
czekoladowe) i południowego wschodu – Wyżyny Ukraińskiej (surowce „wołyńskie”).
Kultura ceramiki wstęgowej rytej
Pierwsza faza zasiedlenia ziemi chełmińskiej przez ludność KCWR mieści się w najstarszym horyzoncie zasiedlenia ziem polskich w ogóle. Najbardziej charakterystyczną cechą
materiałów z tej fazy jest bardzo wysoki udział krzemienia jurajskiego podkrakowskiego.
Wytwory z tego krzemienia stanowią od około 60% do ponad 90% wszystkich określonych
surowcowo okazów z poszczególnych stanowisk. Drugą co do liczebności grupę wytworów
stanowi lokalny krzemień narzutowy wieku kredowego (średnio nieco ponad 20%). Krzemienie czekoladowe (o różnej proweniencji) to najmniej liczna grupa wytworów, średnio
niewiele poniżej 10%.
W kolejnych fazach zasiedlenia ziemi chełmińskiej (II i III) następuje wyraźna zmiana
składu surowcowego analizowanych inwentarzy. Najliczniejsze są wytwory z krzemieni
czekoladowych (średnio blisko 60%), drugi co do frekwencji jest krzemień narzutowy
bałtycki (średnio blisko 35%), a udział wytworów z krzemienia jurajskiego wynosi średnio
około 7%.
Kultura późnej ceramiki wstęgowej
Stan rozpoznania tego etapu zasiedlenia ziemi chełmińskiej nie jest zadowalający.
Badania wykopaliskowe przeprowadzono zaledwie na kilku stanowiskach. Stąd też i wiedza
o krzemieniarstwie jest skromna, oparta na wynikach analiz materiałów z zaledwie kilku
34
Jolanta Małecka-Kukawka
stanowisk, a raczej kilku obiektów z nich pochodzących. Na stanowiskach wiązanych
z KPCW obserwuje się niemal całkowity zanik napływu surowców południowopolskich,
w tym także i krzemienia jurajskiego podkrakowskiego.
Kultura pucharów lejkowatych
W trakcie trwania kultury pucharów lejkowatych na ziemię chełmińską docierały
surowce pochodzenia południowopolskiego (krzemienie czekoladowe, krzemień
świeciechowski, incydentalnie krzemień pasiasty) oraz z Wyżyny Ukraińskiej (krzemienie
wołyńskie). Wytwory z krzemienia jurajskiego zidentyfikowano w materiałach z zaledwie trzech stanowisk – są to dwa wióry oraz fragment wióra retuszowanego. Nie można
wykluczyć, że wytwory z tego surowca dla populacji KPL mogły mieć charakter lokalny
(wtórne użytkowanie).
Najbardziej intensywny napływ krzemienia jurajskiego podkrakowskiego nastąpił
w czasie trwania pierwszych społeczności rolniczych i odnosi się do wczesnego okresu
osadnictwa KCWR. W kolejnych fazach rozwoju KCWR wzrasta intensywność napływu
krzemieni czekoladowych. Krzemień jurajski podkrakowski pojawia się w materiałach ze
stanowisk o późniejszej chronologii, jednak jego frekwencja wyraźnie spada.
Przedstawiona struktura surowcowa potwierdza istnienie rozległej i wielokierunkowej
sieci wymiany krzemienia jurajskiego wśród najstarszych społeczności rolniczych.