Upload
-
View
241
Download
0
Embed Size (px)
Citation preview
7/31/2019 Silex Neolit
1/19
Functional analysis of stone grinding and polishing tools fromthe earliest Neolithic of north-western Europe
Caroline Hamon
UMR 7041 ArScan, Proto histoire europeenne, Maison de larcheologie, 21 allee de l Universite, F-92023 Nant erre cedex, France
Received 7 February 2007; received in revised form 11 October 2007; accepted 26 October 2007
Abstract
This reconstruction of grinding, pounding, hammering and abrading activities in the Early Neolithic of north-western Europe (Linearband-
keramik and Villeneuve-Saint-Germain cultures, 5100e4700 BC) is based on the study of 1289 sandstone tools from 17 sites located in the main
Paris basin river valleys (Aisne, Eure, Marne, Oise, Seine, Yonne). An original method of functional identification was elaborated, relying on
observation of use-wear with a stereoscopic microscope (under120). Identification of traces of use relied on an experimental referential of 92
samples. These include (1) grinding cereals, (2) pounding temper, colourants and various plants, (3) shaping mineral, vegetal and animal objects
by polishing (schist, limestones, bone, antler, wood), (4) softening skin. A significant observation concerns the use of small handstones for grain
dehusking and larger handstones for grain grinding. Recycling is a widespread feature, with multipurpose handstones and frequent reuse of lower
grinding tools for obtaining colourants. A change in the function of tools can also be observed between the Linearbandkeramik and the
Villeneuve-Saint-Germain.
2007 Elsevier Ltd. All rights reserved.
Keywords: Neolithic; Western Europe; Grinding and abrading tools; Use-wear analysis; Experimentation
1. Introduction
The Linearbandkeramik culture, which arose in central
Europe in the middle of the 6th millennium BC, reached the
northern half of France between 5100 BC and 4900 BC.
The introduction of a neolithic economy in north-western
Europe was accompanied by important technical innovations
that impacted both dietary habits and material culture. Dietary
habits were changed by cereal grinding, which became increas-
ingly important among domestic activities. Material culturechanges affected stone tools, bone tools and ornaments made
from shell, limestone and schist that were abraded or polished
during their manufacture and included ceramic manufacturing
requirements for pounding or grinding tempering material of
bone, flint, and crushed pottery. These grinding, pounding
and abrading activities required technological developments
of the stone equipment that archaeologists have traditionally
referred to as ground stone tools and more recently are
considering them macro-lithic tools (Adams et al.,
in press).
The first systematic studies of macrolithic tools were with
Near Eastern collections, where grinding stones were consid-
ered key in the emergence of agriculture. These studies devel-
oped the first real typologies (Nierle, 1982; Wright, 1992).
Ethno-archaeological studies undertaken in the 1980s advanced
functional approaches to stone tool use (Hayden, 1987; Roux,
1985). They contributed to the development of raw materialanalyses (Pommepuy, 1999; Schoumacker, 1993; Schneider,
2002) and socio-symbolic studies (Lidstrom-Holmberg, 1998)
that provided a broader reflection of their functional signifi-
cance. Based on residue identifications and optical observations
(Adams, 1988, 2002; De Beaune, 2000; Dubreuil, 2004; Fulla-
gar and Field, 1997; Gonzalez and Ibanez, 2002; Procopiou,
1998; Risch, 2002), the relevance of macro-lithic functional
analyses is becoming widely accepted as an indicator of pre-
historic technological and economic processes (Procopiou and
Treuil, 2002). Nonetheless, with the exception of a fewE-mail address: [email protected]
0305-4403/$ - see front matter 2007 Elsevier Ltd. All rights reserved.
doi:10.1016/j.jas.2007.10.017
Journal of Archaeological Science 35 (2008) 1502e1520http://www.elsevier.com/locate/jas
mailto:[email protected]://www.elsevier.com/locate/jashttp://www.elsevier.com/locate/jasmailto:[email protected]7/31/2019 Silex Neolit
2/19
important studies (Monchablon, 2002; Pavlu, 2000; Zimmer-
mann, 1988), very little research has been conducted on Line-
arbandkeramik macro-lithic tools.
The research reported upon here is intended to place early
neolithic sandstone tools from north-western Europe in their
technological and socio-economic context. The database con-
sists of 1289 stone tools from 17 Linearbandkeramik (5100e4900 BC) and Villeneuve-Saint-Germain (4900e4700 BC)
sites in the Paris Basin and the Belgian regions of Hainaut
and Hesbaye (Fig. 1) (Hamon, 2006). Particular attention is
paid to technological and functional attributes of the tools
and to their distribution within the sites. The focus is on the
methodology and results of an analytical approach that is
primarily functional. Specifically, a use-wear analysis is elab-
orated, that relies on optical comparisons between archaeolog-
ical and experimental use-wear traces.
2. Stone tool classification
2.1. Some remarks about terminology
The terminologies used for stone tool classification (also la-
belled macrolithic tools, grinding stones, ground stone
implements or non-flaked tools) are as numerous as their
geographical and cultural contexts of discovery (Table 1). As
for grinding tools, American terminology is inspired by the
Spanish term mano for a hand-held grinder and a modified
American Indian term metate to label the stationary stone
on which the mano was used (see for example Adams, 2002,
pp. 99e127). The same tools are designated in English litera-
ture as handstones or grinders for the hand-held tools
and querns or slabs for their stationary counterparts,
and these labels are used in most of the classifications pro-
posed for Near-Eastern tools (Wright, 1992). The German
school uses terminology that combines tool use and morphol-ogy to define Mahlsteine including Laufer for the hand-
held tool and Unterlieger for the stationary counterpart
(see for example Zimmermann, 1988). In France, the impact
of Leroi-Gourhans work (Leroi-Gourhan, 1945) led to the inte-
gration of macrolithic tools in a broader system of artefact clas-
sification: meules for the stationary tool and molettes for
the hand-held tool used for cereal grinding (De Beaune, 2000;
Hamon, 2006). Similar terminological and linguistic correla-
tions could be made for all the categories of tools.
2.2. Proposed classification for the early Neolithic
of the Paris Basin
The 1170 stone tools from the Paris basin included in this
study are typically classified as grinding tools such as querns
and grinders, multifunctional tools such as netherstones, crush-
ing tools such as anvils, hammerstones and broyons (defini-
tion below) and abrading and polishing tools. Interestingly, so
far neither pestles nor mortars have been found in the Paris
Basin (Table 2, Fig. 2).
N
km
Villeneuve-Saint-Germain - BlicquyLinearbandkeramik
Aisne
Marne
Seine
Yonne
Ois
e
Fig. 1. Map of the Paris Basin and south Belgium in the Linearbandkeramik sphere: 17 sites studied in the Aisne, Eure, Marne, Seine and Yonne valleys.
1503C. Hamon / Journal of Archaeological Science 35 (2008) 1502e1520
7/31/2019 Silex Neolit
3/19
Linearbandkeramik grinders are loaf-shaped and manipu-
lated with two hands in reciprocal strokes. They are compati-
ble with large square or oval querns that have varyingly
concave working surfaces. Three categories of dimensions co-
exist.1
The shaping of Linearbandkeramik grinders was quiteelaborate with pre-forming accomplished first by flaking, fol-
lowed by pecking and with some items finished by smoothing.
Hammerstones include tools with obvious impact fractures
from forceful strokes on their ends and faces. Similar impact
fractures can occur on the upper surfaces of netherstones,
along with cuts, incisions and polished areas.
One type of tool has to be considered separately and is la-
belled here by the term broyon. Broyons were used inter-
changeably as crushers and grinders. Crushing strokes create
a pattern of dense fine impact fractures on the edges, whereas
grinding strokes create abrasion and sheen on the broad sur-
face. Far from a secondary use, this tool was purposefullyshaped to be used in a two-step task of crushing and grinding
substances.
Linearbandkeramik abrading and polishing tools have been
sorted into three main categories including polishers, hand-
abraders, and grooved abraders. Polishers served as working
surfaces for shaping objects (Adams, 2002, pp. 143e145).
The upper surfaces of Linearbandkeramik polishers are
slightly concave, uniformly smooth and have a continuous
sheen. Linearbandkeramik hand-abraders are less than 10 cm
long and can be used either in an active or passive position.
Made of coarse and porous sandstones, their surfaces are
covered with abrasive scratches.
Some grooved abraders have narrow grooves with v-shapedcross sections, and others have wider grooves with deep
u-shaped cross sections. Within the groove, the rock grains
are levelled.
Another category of handstones manipulated with only one
hand is particularly interesting for understanding Linearband-
keramik technological development. Despite having standard-
ized dimensions and shapes, they were clearly used in a wide
variety of tasks and made from a variety of rock types. They
were used with multidirectional strokes, circular and linear,
to grind, pound or soften all kind of materials. They complete
the general stone toolkit found in the lateral pits of the Linear-
bandkeramik longhouses.
This proposed classification constitutes a first and necessarystep for the understanding of the use of macrolithic tools from
the Early Neolithic of the Paris Basin. However, the develop-
ment of use-wear analysis techniques based on petrographic
determinations and on experimental comparative collections
is essential to determine the exact function and role of macro-
lithic tools in the activities that took place in Linearband-
keramik houses and villages.
3. Methodology for a use-wear analysis of stone tools
The methods chosen for functional analysis of macrolithic
tools are based on macroscopic and microscopic observationsof use-wear traces on working surfaces and of patterns that in-
dicate motor habits involved with tool use (Hamon, 2003). The
traces were first defined on experimental tools and then com-
pared to traces on archaeological material in order to define
their function in terms of the tasks in which they were used
and their manner of use. Microscopic observations were at
low power (less than 120) magnification, using a stereoscopic
microscope. Archaeological and experimental tools were
cleaned with demineralized water or, in the case of surfaces
with grease or colorant, with alcohol.
3.1. Raw material properties
Grinding and abrading tools are made of different types of
sandstones. Sandstones are sedimentary rocks composed of
quartz grains, together with rock fragments and feldspar grains.
Grain morphology and roundness are key to determining a
rocks geologic origin, transportation distance and transporta-
tion conditions (Foucault and Raoult, 1980). The classification
of sandstones is based on the proportion of each component
and on the nature of the cement (Folk, 1974). The rock matrix
can be composed of iron oxides, silicate, glauconie or calcium
carbonate and is different from cement which crystallizes
among the interstitial spaces after the formation of the rock.
Table 1
Terminological comparisons between French, English, American, German and Spanish terms used to designate grinding tools
Term Grinder Handstone Molette Laufer Mano
Language English English French German Spanish
Bibliography Wright, 1992 Leroi-Gourhan, 1945 Zimmermann, 1988 Adams, 2002; Hayden, 1987;
Mauldin. 1993
Term Quern Grinding slabs Meule Unterlieger Metate
Language English English French German American Indian
Bibliography David, 1998 Wright, 1992 Leroi-Gourhan, 1945 Zimmermann, 1988 Adams, 2002; Hayden, 1987;
Mauldin, 1993
Term Grinding equipment Grinding stones Moulin Mahlsteine Milling equipment
Language American American/English French German American
Bibliography David, 1998; Smith, 1986 Fullagar and Field, 1997;
Lidstrom-Holmberg, 1998
Leroi-Gourhan, 1945 Zimmermann, 1988 Schneider, 1996
1Querns: 30 15, 35 22 and 23 12 cm; grinders: 10 8, 18 12,
23 12 cm.
1504 C. Hamon / Journal of Archaeological Science 35 (2008) 1502e1520
7/31/2019 Silex Neolit
4/19
Table 2
Composition of the toolkit by site, with counts of the number of houses and cultural affiliation (LBK, Linearbandkeramik; VSG, Villeneuve-Saint-Germain, Cerny
Site Cuiry-les-
Chaudardes
les
Fontinette
Berry-au-
Bac le
Vieux
Tordoir
Bucy-le-
Long
la
Fosselle
Etigny
le
Brassot-
est
Villeneuve-
la-Guyard
les
Falaises
de Prepoux
Reims-
Tinqueux
la
Haubette
Passy
Sablonniere
Trosly-
Breuil
les
Obeaux
Pontpoint
le Fond
de
Rambourg
Poses
Sur
la
Mare
Bucy-le-
Long le
Fond du
Petit
Marais
Bucy-le-
Long la
Fosse
Tounise
Vignely
la
Porte
aux
Bergers
Culture Lbk Lbk Lbk Lbk VSG VSG VSG VSG VSG VSG VSG VSG VSG
Number of
houses
33 6 15 6 4 3 6 4 3 10 6 5 5
Grinder 8 5 2 2 9 1 2 15 79 8 3 1 8
Quern 39 10 21 5 7 2 12 21 64 28 7 6 9
Broyon 1 20 1 1 1
Anvil 1 6 1 4 1
Hammerstone 27 5 43 1 4 4 15 6 13 1
Netherstone 6 1 1 2 1 1 6
Hand polisher 7 1 8 3 3 4 1
Groovedpolisher
7 31 1 1 1 8 3 4 2
Small
handstones
10 4 3 1 6 159 23 1
Polished items 47 1 25
Undetermined 9 16 77 7 5 16 84 12 14 5
Grinder.
hammerstone
3
Quern
hammerstone
9 2
Quern anvil 2
Mortar
indeterminate
1
Small handstone
indeterminate
5
Lower grooved
abrader
1
Netherstone.
handstone
1
Total 131 41 252 10 31 12 28 75 387 105 36 42 32
7/31/2019 Silex Neolit
5/19
The cementation process affects the porosity and durability of
the rock (Adams et al., 1994).
A petrographic analysis of the sandstones used by neolithic
people throughout the Paris Basin was conducted in collabora-
tion with the Geological Department of the University of
Reims and Lyon (see Blanchet et al., 1989; Hamon, 2006).
It focused on the identification of tertiary sandstones exploited
in the Aisne valley, such as the Auversien, Cuisien and Spar-
nacien layers for grinding tools (Table 3). Within the Paris Ba-
sin, the sandstone selected for tool manufacture is local with
sources located less than 5 km from each site.
Sandstone blocks were chosen for experimentation based
on petrographic distinctions and by comparisons between the
natural blocks from alluvial deposits and stone tools from ar-
chaeological sites in the Aisne Valley. Considering the impor-
tant vertical and lateral variations that affect the texture and
cementation of different types of sandstones, this comparison
could not rely entirely on the accuracy of source identification.
The physical properties (texture and cohesion) of each sand-
stone were also taken into account when choosing the proper
blocks for experimental tools. Ultimately, several qualities of
sandstone were recognized as functional. Fine-grained, well-
cemented and quartzitic sandstone was preferred for cereal
grinding because they are characterized by a high proportion
of durable quartz grains and bonded by well-developed sili-
ceous cement (arkoses or sub-arkoses) which inhibits flour
contamination by loosened rock grains. Poorly cemented, po-
rous and coarse sandstone rocks were suitable for abrading
tasks and were mainly glauconious sandstone although some
ferruginous sandstone rocks (graywacke) were also used. Con-
sequently, a range of sandstone rocks, with varying degrees ofcohesiveness and porosity, were used for grinding, pounding,
abrading and softening tasks by Neolithic people.
3.2. Use-wear definition and observation
Following a macroscopic level of analysis and according to
previous experimental and archaeological observations, use-
wear on macrolithic tools consists of striations, percussion im-
pacts and sheen or polish. The use-wear analysis discussed
here on sandstone is based on three main types of traces visi-
ble with low magnification (Hamon, 2003):
(1) Levelling of the microtopography is caused by abrasion of
the grains and removal of loosely cemented grains. Such
damage is visible at very low magnifications (less than
10). The more the levelling, the more melted or contig-
uous the rock grains appear.
(2) Modifications of the interstitial spaces between grains can be
observed with magnifications between 10 and 40. On
porous rocks, grains are detached from the rock during
work. On well-cemented rocks, the interstitial space can
become filled with a specific type of residue, or reaction
product (Adams, 2002, p. 31). It can be described as a trans-
lucid fluid substance, distinct from the matrix or cement,
which covers thewhole surface or develops only on the facesof the grains.
(3) Modifications of the angles, edges, profiles and faces of the
grains can be observed at magnifications above 60 and are
described as fractures, edge rounding and abrasion.
3.3. Discussion about hypotheses of use-wear formation
How can the formation of use-wear traces be explained
(Fig. 3)? Macroscopic observations alone cannot give a true
image of the interacting mechanisms. Tribologists have recog-
nized that both mechanical and tribochemical actions2 contrib-
ute to the creation of use-wear traces, some of which are onlyvisible with high power magnification (Adams, 1988, 2002;
Fullagar and Field, 1997; Procopiou et al., 1996). Surface
levelling, grain rounding and fracturing and grain removal
are mainly mechanical actions. Tribochemical actions may
play a greater role in the formation of surficial residues that
are visible to us as sheen or polish (Adams, 1988, 2002). Pol-
ish could be created by interactions among processed sub-
stances and the rock, and by chemical interactions between
water and silica contained in the processed cereals and in
Cereal grinding
Softening
Crushing / grinding
grinder
handstones
anvil / slab
broyon
Abrading / Polishing
abrader / polisher
quern
broyon
anvil / slab
Grinding
anvil / slab
handstones
Fig. 2. Schematic of strokes used with stone tools for grinding, pounding, soft-
ening and abrading activities.
2Tribologists study friction, lubrication and wear on surfaces that are in rel-
ative motion.
1506 C. Hamon / Journal of Archaeological Science 35 (2008) 1502e1520
7/31/2019 Silex Neolit
6/19
Table 3
Petrographical analysis of geological and archaeological samples from the Aisne valley
Site/no. inv./M2 Type Macro-scopic
description
Grain size
(mm)
Minerals Structure,
sorting
and grains
morphology
Matrix/cement
Feldspar Plagio-clases Rock
fragments
Other Si Ca Silt/
micaceous
Quartz
over-
growth
%
1 Trosly-
Breuil
(VSG)
Quern
fragment
Fine well-
cemented
Over 0.5 x e x Black
minerals
Well-sorted
sub-rounded
x
around
10%
x
around
5%
x