The article presents an original analysis which combines use-wear, 3D modelling and spatial analyses to experimental archaeology in order to investigate Early Upper Palaeolithic flint-knapping gestures and techniques involving the use of macro-lithic tools. In particular, the methodological framework proposed in this paper was applied to the study of Protoaurignacian and Aurignacian macro-tools from Fumane Cave (Verona, Italy). Combining spatial analysis and use wear investigation, both at low and high magnifications, permitted the identification and detailed description of the use-related traces affecting both the hammerstones and retouchers which, at Fumane Cave, were used at different stages during flint tool production. Several experimental activities were performed including core reduction, maintenance, and blank production together with different types of edge retouching. From a methodological perspective, the protocol of analysis permitted to codify specific traces and to produce quantitative data related to their geometry and distribution over the tool’s surface, according to the activities and gestures performed. The results obtained allowed a careful investigation of the function and the gestures associated to the use of the macro-lithic tools coming from the Protoaurignacian and Aurignacian levels of Fumane Cave while providing a methodological tool for interpreting different archaeological samples.
Citation: Caricola I, Zupancich A, Moscone D, Mutri G, Falcucci A, Duches R, et al. (2018) An integrated method for understanding the function of macro-lithic tools. Use wear, 3D and spatial analyses of an Early Upper Palaeolithic assemblage from North Eastern Italy. PLoS ONE 13(12): e0207773. https://doi.org/10.1371/journal.pone.0207773
Editor: Michael D. Petraglia, Max Planck Institute for the Science of Human History, GERMANY
Received: July 29, 2018; Accepted: November 6, 2018; Published: December 12, 2018
Copyright: © 2018 Caricola et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Data Availability: All relevant data are within the manuscript.
Funding: The authors would like to acknowledge funding received for this project through the European Research Council (ERC Starting Grant Project HIDDEN FOODS, G.A. no. 639286 to E.C.).
Competing interests: The authors have declared that no competing interests exist.
Interest in the study of macro-lithic tools has increased in recent years, in relation to their potential for reconstructing the variability of adaptive human choices. First coined by Adams and colleagues , the term “macro-lithic tools” refers to a rather varied category of stone artefacts used for percussion, abrasion, polishing, cutting and grinding activities. The variability in the use of macro-tools in the past led to in-depth study of this category of artefacts, which has been analyzed from both a technological [2–6] and functional point of view, through the observation of macro and micro-traces [7–23]. There have also been important studies of the mechanical [24–26] and physical properties of the rocks , applying UBM laser profilometry methods , and of the residues [29–38]. Furthermore, the principles of tribology have made a great contribution to the study of macro-lithic tools for understanding the various processes that lead to use wear development [39–48].
So far, most of the functional data regarding macro-lithics comes from later prehistoric contexts–e.g. the Neolithic and Chalcolithic–while little information is available on the early use of such tools during the Palaeolithic and Mesolithic. Recent studies carried out on the tools found in the Bilancino site [49–52] and Grotta Paglicci , both in Italy, have emphasized the relationship between these tools and technological aspects such as plant food processing during the Upper Palaeolithic. Skills involved in the processing of different raw materials, such as plants [54–59] and minerals [60–64] have little visibility in the archaeological record. It is clear that it is necessary to intensify the functional studies on this category of artefacts, especially with regards to hunter-gatherer societies. The techno-cultural choices of these groups, for example in relation to a general evolution of human cognition and social interaction, could have been much more complex . These choices encouraged the creation or the adoption of innovative technologies combined with a series of collateral activities, such as the ability to collect raw materials, transport strategies, the complementary use of tools to produce other tools, or to process organic and inorganic raw materials .
Tools used in percussion activities, such as spheroids and anvils, are evident since the earlier phases of the Palaeolithic [67–70], being made out of different raw materials and used to process different substances.
Macro-lithic tools are also related to the production of knapped stone tools. Indeed, hammerstones and retouchers made of stone [4,21,71–73] and bone [74,75], are found in numerous contexts, especially related to the later phases of the Palaeolithic . As an example, bone retouchers have been found in different Middle and Late Pleistocene sites [76,77,78–85, 86]. Rarer are the antler billets [87–89] or wood retouchers .
To date, functional studies on this tool category are still lacking. Indeed, the use and the type of hammerstone or retoucher (e.g. hard or soft) is determined, or hypothesized, indirectly through the scrutiny of some morpho-metric features observed on the produced blanks (e.g. features of the impact point and the bulb, the internal and external platform angle, the dimensions of the striking platform and the morphology of the detachment scars or ridges of the dorsal face) or the retouched edge (e.g. features of scars and the bulb, the inclination of the retouch scars with respect to the opposed face, and the morphology of the scars). The identification of knapping techniques has usually been carried out in combination with experimental activities and numerous contributions have been published over the years [91–98], while more generic information is available for the use of hammers on bones .
Even though this type of analysis provides interesting information, some limitations do exist. Firstly, the analysis of these features focuses mainly on the knapping techniques. Secondly, it is an indirect analysis, which is exclusively based on diagnostic features on the “product”, even in those cases where the presence of hammerstones and retouchers or of ones potentially in the archaeological record would allow a detailed study of the percussion and retouching techniques. In this respect we often read about the presence of “fluvial pebbles”, which were probably used at the site as hammers, but have not been analysed by means of use wear analysis .
In this paper we present a multidisciplinary analysis of the repertoire of pebbles associated with the Protoaurignacian and Aurignacian levels of Fumane Cave. Such tools represent a valuable opportunity to detail the gestures of Early Upper Palaeolithic percussion activities, and the criteria involved in raw material selection and macro-lithic tool exploitation at the site. The combination of experimental archaeology, use wear analysis and GIS analysis allows further enhancement of the results provided by functional analysis, through the addition of quantitative data, and its potential has been already proved by the pioneering studies performed by De la Torre and colleagues , Caruana and colleagues  and more recently by Benito-Calvo and colleagues [103–105].
Our results further confirm the reliability of this combined methodology and provide new and relevant insights regarding the variety of percussion activities performed during the early Upper Palaeolithic occupation of Fumane Cave.
The archaeological context: The Protoaurignacian and Aurignacian at Fumane Cave
Fumane Cave is located in the Venetian Prealps (north-eastern Italy) (Fig 1). The cave has been under excavation since 1988 and is characterized by a high-resolution stratigraphic sequence [106,107] spanning the Mousterian , Uluzzian , Protoaurignacian [110,111], and Aurignacian . Today, it represents a key site for understanding the complex processes that led to the demise of Neanderthal populations and the spread of modern humans across Europe . Layers A2 and A1 date the appearance of the Protoaurignacian to 41.2–40.4 ky cal BP, while a combustion feature embedded in the stratigraphic complex D3 dates the youngest Aurignacian phase to 38.9–37.7 ky cal BP . A recent assessment of the Protoaurignacian [111,115] and Aurignacian  lithic technologies, has permitted an accurate narrative of the diachronic changes that occur throughout the stratigraphic sequence and enables us to critically address the techno-typological signature of the Aurignacian in northern Italy. Overall, bladelets were the first goal of the lithic production in all the studied assemblages. They were obtained from a broad range of independent reduction strategies, among which carinated technology seems to increase towards the top of the sequence. The rather standardized reduction procedures, reconstructed from the study of blanks and initial and exhausted cores, were tailored for the production of regular and frequently pointed bladelets by means of unidirectional convergent knapping progressions. Blades represented the second goal of the lithic production system and their frequency remains stable throughout the sequence. Blades were obtained from sub-prismatic cores using direct marginal percussion on flat striking platforms and were also produced during several maintenance operations carried out on bladelet cores. Unlike blades, flake production increases in the Aurignacian assemblages, where it also appears to be more standardized . Tool assemblages are dominated by retouched bladelets, with frequencies that progressively decrease from layer A2 (around 80%) to the top of layer D3 (around 50%). Modification is in most cases marginal, semi-steep, and was conducted to shape bladelets with convergent retouch and bladelets with lateral retouch . In both cases retouch delineation is regular and generally follows the initial morphology of the blank. Among common tools, laterally retouched blades and burins are more prevalent in the Protoaurignacian layers, while endscrapers significantly increase in the Aurignacian assemblages. Laterally retouched blades present unilateral or bilateral retouches. Modification is in most cases direct and, especially on the thicker blanks, has a scaled morphology. The so-called Aurignacian retouch  is instead rare. Endscrapers, both on blade and flake, display in most cases a thin working edge shaped by short lamellar removals. Some of them were made on retouched blanks. The working edge was frequently reshaped, and several wear traces were identified. Finally, thick endscrapers, such as carinated and nosed forms, were in most cases used as cores for the extraction of small and curved bladelets.
Materials and methods
The archaeological sample
The archaeological sample coming from the Protoaurignacian and the Aurignacian levels of Fumane Cave, is composed of 7 specimens, that characterize the entire assemblage (General Inventory Number VR67993) (Fig 2). These are naturally rounded pebbles originated in a fluvial sedimentary context. As suggested by previous studies  pebbles with a high degree of rounding have been collected, more likely, from fluvial deposits originating from high-energy water courses, like the Adige river which currently flows 20km south of Fumane. Indeed, they do not present any technological modification, their morphologies are rather recurrent, circular or oval with oval section. The overall dimensions are small, the average length equals to 68 mm, with an average width of 56 mm and an average weight of 322 gr.
Pebbles are made of sedimentary and metamorphic rocks: a) compact limestone, with fine texture (n 4); b) soft limestone, with a characteristic pink and white colour (n 2); c) ophicalcite, a metamorphic rock with carbonate cement veins of allochthonous origin (n 1) (Determination by Stefano Bertola).
However, as stressed by Bertola and colleagues  in the case of sedimentary rocks, the lithologies are various, attributable to different horizons included in the carbonatic formations cropping in the area, from Upper Cretacic Scaglia Rossa to Jurassic “Calcari Grigi”
Within the archaeological sample, 6 artefacts are intact or with perfectly reassembling parts, while 1 sample are fragmentary, along with one specimen characterised by fractures caused by a probable source of heat that caused it to expand (Table 1). No permits were required for the artefacts’ study as one of the authors (MP) is Director of the excavation at the site of Fumane Cave and responsible for the scientific activity carried out on the archaeological findings recovered from the site. Regular permits have been received (ref. DG-APAB4646) for all aspects of this work from the archaeological authority, the Soprintendenza Archeologia, Belle Arti e Paesaggio per le Province di Verona, Rovigo e Vicenza (SAPAB—VR).
US, dimensions, raw material, integrity, colour and morphology.
Use wear analysis
The artefacts were analyzed applying a functional approach along with the design and application of a dedicated experimental framework. The functional approach is based on the analysis of different aspects related to the use of macro-lithic tools.
For the study, the specimens were observed utilizing a Zeiss Axio Zoom V16 binocular stereo microscope, oculars PI 10x/23, objective 1x/0.25 FWD 56mm, with progressive magnifications ranging between 10x and 80x. This low-magnification observation allowed us to propose a hypothesis regarding the gestures and details related to the kinetics of the object. Furthermore, it allowed us to determine the nature and status of the processed matter with which the object came into contact. Topography and microtopography, grain shapes, pits, striation and fracture morphologies on experimental and archaeological artefacts have been described according to parameters already described in literature [3,20]. 3D models of the surface were produced utilizing Mountain Map Premium 7.2, which provided more information related to the evolution of the microtopography and details concerning the morphology of the identified traces.
A second level of observation consisted of the analysis of the specimens at higher magnification (50-500x) using Zeiss Scope A.1 metallographic microscope equipped with 10x oculars and with objectives ranging from 5x to 50x. This allowed the investigation of micro wear (e.g. micro-striations and micro-polishes) to achieve more information about the use of the tools. Polishes have been described by taking into account their texture, topography, distribution, extension and linkage (for more details see [23,121,122]). The surfaces have been documented using a Zeiss Axiocam 305/506 color camera and were washed with neutro phosphate detergent (Derquim) and ultrasonic cleaner AU-32 (ARGO LAB) for 15/20m.
3D Models of both experimental and archaeological samples have been created through the application of photogrammetry. Following the protocol developed by Porter and colleagues  3D models of the artefact were built using Agisoft Photoscan 1.3.4.
The tools were placed on an automatic turntable in order to produce 360° sets of each of the tool’s surfaces. Pictures of the tools were shot using a Nikon D7200 DSLR camera equipped with a Nikkor 105 Macro Lense. Each picture was taken every 15°, and at every full revolution the camera was lifted and slightly titled towards the target for a total of 72 picture per object side. A total of 144 pictures were taken per object, which were subsequently imported in Agisoft Photoscan Pro 1.3.4 to produce high quality dense point clouds and meshes.
Surface morphometric analysis
GIS analysis has been adopted to analyse the morphometric characteristics of both experimental and archaeological samples. Applying both the methodologies proposed by Caruana et al , Benito-Calvo et al  and de la Torre et al  it has been possible to analyse and quantify use wear patterns originated from both retouching and percussive activities. After the creation of 3D Models, Digital Elevation Models (DEM) featuring a resolution of 0.5mm were created in Agisoft Photoscan 1.3.4 and imported as raster files in ArcGIS 10.5.
Digital Surface Models were generated in order to analyse the topographic features characterising the tool’s surface. At first a Hillshade model of the entire surface was created. This allowed a first morphometric assessment of the surface topography that permitted the identification of the Functional Area/s (FA) of the surface which are affected by use.
Once identified, the FA of the tool was extracted from the original DEM as a new raster surface and three kinds of Digital Surface Models (DSMs) were generated to identify and interpret use wear.
Slope, which identifies the rate of change in the z-value from each of the cells composing a raster surface allows the identification of changes in the surface elevation such as depressions or pits characterising the objects FA. Subsequently, two DSMs devoted to the analysis of surface roughness were generated. Analysing surface roughness permits the analysis of the degree of homogeneity or heterogeneity characterising the tool’s surface. As already stated by Benito-Calvo and colleagues (2015) the measurement of surface roughness can lead to the identification of polished areas (low roughness) generated by use. Two methods of surface roughness measurement have been applied: Terrain Ruggedness Index (TRI) and Vector Ruggedness Measure (VRM). TRI is based on the algorithm proposed by Riley and colleagues  and calculates the sum change in elevation between a grid cell and its neighbourhood. In the resulting DSM, a TRI value of 0 represents the minimum degree of roughness (i.e. homogeneous surface). Vector Ruggedness Measure (VRM) measures roughness as the dispersion of vectors orthogonal to the surface within a specific neighbourhood. This method captures variability in slope and aspect into a single measure. A value of 0 represents no terrain variation (or lowest roughness) while a value of 1 represents a complete terrain variation (maximum roughness). In the case of the experimental replicas, 3D models and resulting DSMs were made before and after use. This allowed the mapping and quantification of the degree of variation in surface topography related to each of the experimental activities performed.
Following the methodological framework proposed by Caruana et al  the FAs of both experimental and archaeological implements were analysed through Topographic Position Index in order to identify areas of high micro topographic roughness coinciding with use related damage.
Topographic Position Index (TPI) is an elevation residual analysis which is applied to identify depressions and ridges affecting the artefacts surface topography . The DSM generated is based on the computation of the difference between the elevation of a cell and the mean elevation in a neighbourhood surrounding that cell. Neighbourhood mean elevation is calculated using a moving window centred on the cell of interest. TPI positive values indicate that the cell is higher than its neighbourhood while negative values indicate the cell is lower, corresponding to either ridges and depressions. Hot Spot Analysis (Getis-Ord GI*) was performed on the generated surface in order to identify clusters of pits and ridges highlighted by TPI and corresponding to wear caused by use. The patterns identified through Hot Spot Analysis (Getis-Ord GI*) were then transformed into polygons, which provided metric data (e.g. area, perimeter) to be statistically compared (Fig 3).
A dedicated experimental reference collection was necessary in order to understand the use of macro-lithics at Fumane cave, and to isolate specific gestures involved in percussion activities. The experimental framework consisted of different stages. Raw materials were collected according to the size and morpho-metric features of the archaeological specimens. Small and rounded pebbles (mean length 50 mm) of compact limestone were gathered along the Adige river bank, about 20 km away from Fumane. Coarse limestone pebbles were collected in a stream bed close to the site. The latter showed a pink/white colour, probably due to geochemical alterations related to the particular depositional environment.
The collected items (5 retouchers, 3 retouchers/hammerstones, 9 hammerstones, 2 anvil) were used in several experimental tests) and their surface was documented using both the stereo and metallographic microscopes before and after their use, in order to observe the modifications caused by use.
After a preliminary observation of the archaeological sample, it became clear that the Fumane macro-lithics had been used in various activities related to the processing of stone and materials of a non-organic nature. The experimental framework involved 19 pebbles used as hammers in various stages of bladelet production and retouchers, according to the technical solutions known from the analysis performed on the lithic artefacts from the Protoaurignacian and Aurignacian levels of the site, in which core reduction and maintenance are illustrated along with the morpho-technical features of the laminar products and the typology of the retouched tools [110,111,115,120].
For our experimental purposes, nodules of fine-grained flints were used. Several tests have been performed by the flint-knapper, following a precise strategy: a single hammer has been used to perform a specific action with the aim of isolating the functional traces, while others have been involved in different technical gestures to produce experimental replicas showing multi-functional surfaces (a complete list of uses has been illustrated in Table 2).
Gestures have been described following the criteria outlined by Bourguignon . The following points aim to explain the different phases and the relative technical gestures performed by the expert knapper during the experimental activities:
- cortex removal and core-shaping. The soft stone hammers (103x55mm, average dimensions) were used for opening of the nodules to remove cortical flakes in order to shape a pre-form core composed of a single flaking surface related to a single striking platform. During this step, the hammer’s marginal ends have been used as active parts, performing a punctual gesture consisting of a wide rectilinear trajectory of the arm, related to the force necessary to remove larger products. Despite their effectiveness in flake detachment (cortical and non-cortical), they broke after a reduced number of blows (conchoidal fracture along the functional end or straight fracture following the percussion axis). Therefore, their use during this stage was evaluated as not functional;
- flaking surface and striking platform configuration. After having designed the core volume, the soft hammers (50x50mm, average dimensions) were used to open a flaking surface and prepare the platform and the flaking angle through tiny flake removal. During this phase, flakes of various sizes were removed alternating with abrasion of the overhang performed with the same hammer. This latter action required consequential and rapid gestures with resting percussion, aimed to remove micro-flakes from the overhang. This resulted in a more continuous action that involved a wide contact area–usually along the flat axis or lateral along the pebble edge–between the hammer and the core face. Removals of larger maintenance flakes required slower and more precise blows with a curvilinear trajectory, variable amplitude and force related to the size of the desired flake to be removed. This action involved the use of the marginal ends of the pebble along the minor axis;
- blank production and core maintenance. After having shaped the core, we proceeded to the extraction of lamellar blanks using an organic hammer (deer antler; , p.133) and a soft stone hammer, as hypothesized in a recent revision of the bladelets’ technical attributes ( p.27). During this phase, the stone hammers (sized 50-40mm in length, average dimensions) were always used with a rectilinear trajectory on their marginal ends. They performed effectively in blade production, even though small conchoidal fractures appeared in the functional area which, however, did not lead to discarding the tool. Flake detachment and abrasion operations were also carried out, aimed at maintaining the flaking angle and the transverse and longitudinal convexities of the core;
- bipolar percussion. Due to the presence of some splintered pieces in the archaeological assemblage (, p.139) we tested the bipolar percussion by placing the core on a base, consisting of a large flat pebble selected among the collected items. At this stage, the core was of very reduced size and allowed the application of this technique despite the small size of the anvil (50x50x30 mm, average dimensions);
- retouching. Several gestures have been tested according to the different morphologies and intensity of retouching documented for Protoaurignacian and Aurignacian levels at Fumane cave. The occurrence of retouch features was strictly combined with the gesture and the technique, which involved different uses of the functional areas of the pebbles (e.g. short edge or flat face).
- Direct percussion. A rapid and consequential gesture was performed: the knapper’s arm moved following an oblique dragging trajectory against the blank’s edge, striking it very quickly using the tool’s flat face along the apical area. This movement allowed the removal of tiny flakes and was particularly effective for delineating straight cutting edges with marginal and abrupt retouch on thinner edges, due to the limited contact area between the hammer and the blank edge of a wide spectrum of blank morphologies from simple flakes to blades sharing a consistent thickness (Figs 4A and 5B). We noted that this type of retouch can also be performed with different trajectories (e.g. perpendicular to the blank axis). This technique was also used to delineate the front of carinated end-scrapers and of some thin scrapers, even though the short edge of the retoucher was used. This allowed the removal of tiny bladelets and elongated flakes by adopting a marginal percussion (cfr. ). A more punctual gesture produced a more invasive retouch of a scaled type (Figs 4B and 5A), due to a larger contact area between the hammer flat face and the blank to be retouched. This action followed a perpendicular trajectory, with respect to the blank edge, with a movement from the top to the bottom of the arm and a final flexion downwards. This type of retouch has been performed on blades for delineating the front of the end-scrapers (cfr. [111,120]).
- Direct percussion on anvil (Fig 6). This technique was aimed at retouching tiny bladelets: a flat pebble was used as anvil on which the blank edge was modified through the use of a retoucher by percussion ([98,126,127]). The trajectory was found to be variable depending on the position of the blank to be retouched on the anvil: in a central position a perpendicular trajectory was adopted, while when slightly inclined in proximity of the lateral edge of the anvil an oblique trajectory was adopted. In both cases, the short edges of the retoucher were used.
- Edge abrasion (or égrisage, ). The bladelet edge was modified by rubbing against the pebble with the aim of delineating a straight edge (Fig 4C). This reciprocal contact permitted the detachment of micro-flakes.
(a) Production of marginal and abrupt retouch; (b) production of scaled retouch on the lateral edge of a laminar flake; (c) blank retouch through edge abrasion.
(a) The marginal and abrupt retouch: a rapid and consequential gesture was performed. The knapper’s arm moved following an oblique dragging trajectory against the blank’s edge, striking it very quickly using the tool’s flat face along the apical area; (b) the scaled retouch: this action followed a perpendicular trajectory, with respect to the blank edge, with a movement from the top to the bottom of the arm and a final flexion downwards(drawings by Giulia Formichella).
(a) Bipolar percussion for flake production; (b) hinged laminar flake retouch on anvil adopting a rectilinear trajectory; (c) bladelet retouch on anvil adopting an oblique trajectory.
The replicas used during the experimental protocol comprised: a) hammerstones, used for removing cortex and shaping cores, abrasion of core edges and detachment of flakes and bladelets (n.9); b) retouchers, used to produce different types of retouch (n.5); c) anvil, used as a passive base for detaching flakes (n.2); hammerstones/retouchers used with mixed activity (n.3).
The types of use-wear observed on the hammerstones were:
- during cortex removal and core-shaping large longitudinal flake scars (50mm) located along the short edge were produced. In association with these scars there were residual surfaces with pits, similar to the deep scales, of around 6mm in size, with a triangular section. Micro-polishes were absent.
- Overhang abrasion activity produced long, deep striations alternated with more superficial striations, with different orientations, often associated with the configuration of the striking platform. These striations were located on the flat and/or on the long edge of the tool and showed polishing on the bottom with a rough texture when observed at the metallographic microscope (Fig 7).
(a) Macro-traces (30x) long, deep striations alternate with more superficial striations, with different orientations. They are located on the flat and/or on the long edge of the instrument; (b) micro-traces (200x), striations with polishes on the bottom, with rough texture; (c) 3D microtopography of the unused surface and profile; (d) 3D microtopography of the used surface and profile.
- During the configuration of the striking platform of the core, the removal of small flakes produced small pits with sub-oval morphology. The pits often overlapped short superficial striation. These traces were located on the short edges of the tool; if this is circular, use-wear traces were distributed all around its perimeter. A micro-polish was observed, extended on the top of the grains, with a smooth texture, flat topography, uniformly oriented striations, with concentrated-separated distribution (Fig 8).
(a) Macro-traces (30x) highlight the presence of overlapping pits with sub-oval morphology, located all around the marginal perimeter of the object; (b) micro-traces (200x) are extended onto the top of the grains, with smooth texture, flat topography, striation with the same orientation, and concentrated-separated distribution; (c) 3D microtopography of the unused surface and profile; (d) 3D microtopography of the used surface and profile.
- During blank production and core maintenance small sub-circular pits overlapping with small striations and chaotic orientation were produced; flake scars (20/30mm) due to the blow for the extraction of the blank were also observed. The mechanical levelling led to the production of short strips and sporadic polishing with loose-separated distribution on the top of the grains, with deep striation with the same orientation, and a rough texture and domed topography. The traces were located on the short edge of the hammerstone.
Pits produced by the trimming of the striking platform and the production of blanks and core maintenance looked very similar in their distribution and morphology. Often overlapping, pits were not well defined, but polishes looked different. In particular, the trimming of the striking platform produced polishing as a consequence of repeated contact between the hammer and the edge of the flint tool. On the contrary, the detachment of the blades/bladelets consisted of a more precise blow.
Bipolar percussion makes large pits with sub-quadrangular/triangular morphology located in the central area of the flat surface of the tool. The texture grains appear fractured, polishes are absent (Fig 9).
(a) Macro-traces (40x) consisted of large pits with sub-quadrangular/triangular morphology, grains appeared fractured, located in the central area of the flat surface of the pebble; (b) the micro-traces (200x) are absent, the bottom of the pits appear rough; (c) 3D microtopography of the unused surface and profile; (d) 3D microtopography of the used surface and profile.
Retouchers presented different types of use-wear. In detail, the scaled retouch generated a series of contiguous pits of a linear form (reduced half-moon) with a rough bottom and an asymmetric triangular section, localised on the flat surfaces of the tool concentrated near the apices. There were also striations: short, more sporadic and superficial (Fig 10). The micro-polishes were probably absent because the traces resulted from a punctual contact between the retoucher and the edge of the flint tool (the dragged gesture is absent).
(a) Macro-traces (30x), contiguous pits of linear form (half-moon), with rough bottom, and triangular section; the traces are located in the centre of the apical area; (b) polishes (200x) are absent; (c) 3D microtopography of the unused surface and profile; (d) 3D microtopography of the used surface and profile.
Marginal retouch led to an association of small circular pits and dense long parallel striations. Use-wear traces concentrated over the apical area of the flat surface, with oblique orientations. Bands of polishing with striations were present, with covered-closed distribution, a rough texture and domed topography. The dragging movement (oblique trajectory) related to the marginal retouch, produced a mechanical levelling of the surface where the polishes were present (Fig 11).
(a) Macro-traces highlight area characterized by a concentration of micro-pits (25x) with sub-circular morphology; (b) long striation (20x) associated with the pits and with the same orientations; the traces are located in apical top with oblique orientation; (c) micro-traces (200x), band of polishes with striations, covered-closed distribution, rough texture and domed topography; (d) 3D microtopography of the unused surface and profile; (e) 3D microtopography of the used surface and profile (striations and pits).
Other types of retouching were tested, including edge abrasion. This activity produced traces located in a small area between the short edge and the apical area of the retoucher. The traces consisted of small pits with sub-quadrangular morphology and short striations. The rough polishes were present.
Retouching on an anvil produced, on the passive base, superficial small pits with a sub-circular morphology and short striation. The use wear was located on the flat surface. The polishes were absent. The same traces were present on the active retoucher but located on the short edge (Fig 12).
Description of activities, macro and micro traces, use wear localisation and pictures.
On the experimental samples, prehension traces were visible at high magnification. Macroscopically, the prehensive area was smoothed, with several patches of smooth/flat polishing, affecting the top of the grains. Polishes visible between 20x and 50x developed on the flat and central portion of the tool, favoured by a type of prehension in which a large portion of the finger (fingertip) was in contact with the flat surface of the tool. Polishing was not observed in cases where the hammer or the retoucher was gripped by the short margins (tridigital prehensions) and the contact occurred with a reduced portion of the finger (Fig 13).
(a-b) Patch of polishing visible through the metallographic microscope (100x), localised on the top of the grain; (c-d) smooth/flat patch of polishing visible through the metallographic microscope (200x).
GIS analysis—Experimental sample
Overall, the raw material characterising the experimental sample presented in this work was homogeneous. This led to minimal modifications of the tools surfaces in particular concerning their roughness. On the other hand, the analysis of slope revealed several differences between the activities performed (Fig 14).
Digital Surface Maps of Slope, TRI and VRM respectively.
The experimental replicas utilised to produce scaled retouch recorded the development of depressions exhibiting a mean slope value of 9.94°. Surface ruggedness measured through TRI and VRM appeared low with a mean TRI value of (0.0015) and a VRM mean value of (0.001). Most of the variability was concentrated over the apices of the tool. Scaled retouch (Fig 15I, Table 3) led to the development of use-related wear on the apical portion of the tool. Wear features were characterised by an average perimeter and an area of 8.6 mm and 1.5 mm2 respectively. The average distance of the wear feature from the centre of the tool was 16 mm while the average from its edge was 13 mm. Traces are concentrated over the central portion of the tool apex as suggested by the standard deviational ellipse elongation value (0.87 ad). As in the case of scaled retouch, use wear generated by marginal retouch (Fig 15II, Table 3) also affected the apical portion of the retoucher. The depression caused by use featured a slope mean value of 18.8°. The surface showed an overall homogeneity as indicated by the recorded TRI (0.0015) and VRM (0.0023) mean values, with most of the surface variability localised on the tool apical areas. Use related wear exhibited an average perimeter of 9 mm and a mean area of 1 mm2 along with an average distance from the tool centre and edge of 15 mm and 12 mm respectively. Traces generated by marginal retouch were well spread over the retoucher apical portion as suggested by the standard deviational ellipse elongation value (1.7 ad), higher than the value observed on the experimental replica used in scaled retouching.
(a) Spatial distribution of the identified wear; (b) slope; (c) terrain roughness index; (d) vector roughness measure.
In detail, scaled retouch (FSR-1), marginal retouch (FRP-1), bipolar percussion (FA-8), striking platform maintenance (FSPM-13) and bladelet removal (FBR-2).
Passive percussion (Fig 16I, Table 3) led to the development of wear over the central area of the tool used as anvil, where depressions developed featuring a mean slope value of 11.2°. The surface was overall homogeneous (TRI mean value 0.007) with a low topographic variability (VRM mean value 0,0009) mostly at the bottom of the produced wear. Use marks generated by passive percussion featured a mean perimeter of 7.2 mm and an average area of 1 mm2. Traces were localised near the centre of the tool, with an average distance from the centre of 9 mm, while their average distance from the edges averaged 21mm. Traces were concentrated on the tool surface centre as indicated by the standard deviational ellipse elongation value of 0.7 ad.
(a) Spatial distribution of the identified wear; (b) slope; (c) terrain roughness index; (d) vector roughness measure.
Adjustment of core ridges (Fig 16II, Table 3) led to the development of use wear over the apical portion of the tool and in a minimal part over its inner areas. Depressions caused by use featured a mean slope value of 14°, while the TRI and VRM mean values, 0.0011 and 0.0034 respectively, suggest an overall homogeneous surface topography with its higher topographic variability localised over the outer portion of the tool apical area. Marks generated by use were relatively large given their average perimeter of 14 mm and mean area of 3 mm2. While the inner area of the object was also affected, most of the traces generated by the adjustment of core ridges were located near the tool edge (average distance 10 mm) rather than its centre (mean distance 20 mm). Use related damage was well spread over the affected area of the tool as indicated by the standard deviational ellipse elongation value of 1.2 ad.
For the purpose of bladelets production (Fig 17, Table 3), the short edge of the experimental replicas was used rather than its surface. Over the used portion the depressions generated by use were characterised by an average slope value of 23.7°. The used area of the tool was characterised by a higher degree of heterogeneity when compared to the other experimental samples presented in this work, as indicated by TRI (mean value 0,0025) and VRM (mean value 0,0067). Of particular interest is the fact that surface roughness was lower in proximity to the centre of the used surface area, where the bigger traces were located. Wear generated by bladelets production featured an average perimeter of 3.8 mm and a mean area of 1 mm2. Damage affected most of the used area of the tool as indicated by the standard deviational ellipse elongation value (2.3ad) (Fig 18, Table 3).
(a) Spatial distribution of the identified wear; (b) slope; (c) terrain roughness index; (d) vector roughness measure.
(a) Dimensions of the wear identified over the utilized areas of the experimental replicas; (b) mean distance of the identified wear from the object centre; (c) mean distance of the identified wear from the object edge; (d) dispersion of the identified wear over the tool surface defined by the elongation of the standard deviational ellipse.
Use wear analysis.
In the archaeological sample, traces of use were identified on 7 objects. These allowed the determination of the use of the tools at Fumane cave as: a) hammerstones (n. 3, RF37, RF138, RF73); b) retouchers (n.2, RF80 and RF67); c) hammerstone/retoucher (n.1, RF127); anvil/retoucher (n.1, RF92). The artefacts showed a general rounding due to post-depositional alteration, probably of chemical nature. Invasive patinas or concretions were visible in one case (RF73 around the edge) (Table 4).
In four cases (RF127, RF73, RF138, RF37) pits and flake scars were localized on the short edges of the tool, namely on the opposing short margins or, if the instrument presents a sub-circular shape, all around its perimeter. Small pits overlapped, often associated with short and chaotic striations (RF127) (Fig 19). Polishing was not present, probably due to the overall rounding of the surface caused by post-depositional alterations. For the same reason, the pits morphologies were not well defined. However, they shared characteristics similar to those observed on wear produced during core maintenance, related to the detachment of small flakes observed during the experimental knapping of bladelets. One hammerstone (RF138) was characterised by pits associated with negative flake scars (average dimensions 25mm) localised on the short edge of the tool. Deep, long striations were localised on the flat surface, or on the long edge (RF73 and RF37). The flake scars looked very similar to the experimental ones produced during bladelet removal and in overhang abrasions during core management. In one case (RF73) there was an association between the pits, in the marginal extremities, and long and deep striations on the flat surface (Fig 20). Moreover, on RF127 polishing was observed associated with intense rounding of the grains over the central area of the flat surface. These latter patches of polish, affecting the top of the grains were characterised by a flat topography and a smooth texture similar to that observed on the experimental sample and related to prehension (Fig 21).
(a) Macro-traces (25x), overlaid pits with sub-circular morphology; (b) macro-traces (10x), pits located around the short edge of the artefact; (c) 3D microtopography of the used surface and profile.
(a) Macro-traces (20x), long striations with different orientations located on the flat surfaces in the central area; (b) pits (20x) on the marginal surface, overlapping, covered by the patina. The artefact is affected by dissolution; (c) 3D microtopography of the used surface and profile.
(a) Polishing (100x) affecting the top of the grains; (b) patch of polish characterised by a flat topography and smooth texture (200x).
Artefact RF92 featured pits with sub-triangular morphology over its central area. These had a rough bottom with microcracks visible over the grains. Polishing was not present. The observed functional patterns were similar to the experimental sample used as a passive anvil for flake detachment (Fig 22).
(a) Macro-traces (20x), micro-pits with sub-circular morphology associated with long parallel striations, located in the apical top with oblique orientation; (b) micro-traces (200x) are absent, a general rounding is visible; (c) macro-traces (20x), pits with triangular morphology, located in the centre area of the flat surface; (d) polishing is absent (200x); (e) 3D microtopography and profile of the used surface related to (a-b); (f) microtopography and profile of the used surface related to (a-b).
Macro-traces observed at the stereo-microscope were represented by pits and striations. However, the pits displayed differences in morphology and location. In two cases (RF67 and RF127) the pits were located on the apices opposite to the flat surfaces (on one or both surfaces). The morphology of the pits was linear (reduced half-moon), with a triangular section. Polishing was not present (Figs 23 and 24).
(a) Macro-traces (10x), contiguous pits of linear form (half-moon), with rough bottom and triangular section, located on the centre of apical area; (b) micro-traces (200x) are absent; (c) 3D microtopography of the used surface and profile.
(a) Macro-traces (30x), contiguous pits of linear form (half-moon), with rough bottom, located on the centre of apical area; (b) pits with rough bottom (200x); (c) 3D microtopography of the used surface.
In two other cases (RF80 and RF92) (Fig 25) pits were always located on the flat surfaces of the tool over the apices and were characterized by circular morphology, associated with the presence of long, parallel, superficial and overlapped striations. These traces were very similar to ones observed in the experimental replica used for marginal retouching.
(a) Macro-traces (20x), small circular pits associated with long parallel striations, located in apical top with oblique orientation; (b) micro-traces (200x), polishing is absent, a general rounding of the artefact can be observed; (c) 3D microtopography of the used surface.
GIS analysis—Archaeological sample.
As in the case of the experimental replicas, the raw material characterising the archaeological specimens presented in this work was of a homogeneous nature overall.
Specimen RF67 was interpreted through use wear analysis as likely to be a retoucher used to produce scaled retouching based on the presence of traces of use over its apical area, where depressions characterised by a mean slope value of 9.8° were present. The topography of the surface was homogeneous overall with a low to medium degree of surface roughness (TRI mean value 0.00138) along with a low degree of topographic variation as indicated by the VRM mean value (0.0032). Wear generated by use featured a mean perimeter of 9 mm and mean area of 1 mm2. As observed on the experimental replica, use related traces were located towards the artefact edge (mean distance 12mm), while their average distance from the tools centre was 20mm. Wear results were well dispersed over the apical area of the retoucher as indicated by the standard deviational ellipse elongation value (1.6 ad).
Use wear identified on artefact RF80 (Fig 26II, Table 5) allowed us to interpret its function as a retoucher utilised for marginal retouching. As in the case of artefact RF67 (Fig 26I, Table 5) wear was located over the apical area of the object, where depressions bearing a mean slope value of (13.8°) were visible. The utilised area was characterised by a rough surface (TRI mean value 0.0021) becoming smoother towards the centre of the tool. The same pattern was evinced from VRM (mean value 0.0016), with a higher degree of topographic variation towards the outer portion of the tool apical area and lower values characterising its inner portion. This phenomenon can be explained by the fact that the outer area of the tool’s apex suffered a higher degree of surface crushing compared to its inner area. The traces observed on RF-80 were relatively small with an average perimeter of 2.8 mm and an average area of 0.33 mm2. Use related damage was localised nearer the edge of the retoucher (average distance 11 mm) than its centre (mean distance 14 mm). Use wear appeared dispersed over the apical area of the tool as indicated by the standard deviational ellipse value (1.3 ad).
(a) Spatial distribution of the identified wear; (b) slope; (c) terrain roughness index; (d) vector roughness measure.
Two distinctive functional areas were identified on artefact RF92 (Fig 27I, Table 5), one localised at the centre of the object and one corresponding to its apical area. The wear identified on each of the FAs was related to two different activities, passive percussion (RF-92a) and marginal retouching (RF92b). RF-92a was characterised by the presence of depressions with a mean slope value of 22.6°, while more gentle slopes (mean value 15.6°) characterised the depressions identified over RF92b. The surfaces of both the functional areas exhibited a medium to high degree of roughness, with RF92a exhibiting a TRI mean value of 0.0022 and RF-92b featuring a TRI mean value of 0.0029. A difference between the two surfaces was found in their topographic variability. While RF92a was characterised by a low VRM mean value (0.0008), with the higher values corresponding to the bottom of the traces generated by use, a higher variability characterised RF-92b (VRM mean value 0.0023) where higher values were spread over the entire used surface. Traces observed on the central area exhibited a mean perimeter of 7mm and an average area of 1mm2. The damage was located close to the centre of the tool (mean distance 10 mm) and were concentrated, as indicated by the standard deviational ellipse elongation value of 0.7ad.
(a) Spatial distribution of the identified wear; (b) slope; (c) terrain roughness index; (d) vector roughness measure.
Use related damage identified on RF92b featured a mean perimeter of 7mm and an average area of 1 mm2. Traces were localised in proximity of the tool’s edge (average distance 12mm) and were dispersed over the utilised area (stde elongation 2 ad).
Use wear associated with the adjustment of the core ridges was identified over artefact RF73 (Fig 27II, Table 5). The utilised area of the tool was characterised by depressions bearing a mean slope value of 9.6°. Overall the surface topography was characterised by a medium to high degree of roughness (TRI mean value 0.0021) along with a low to medium degree of topographic variability (VRM mean value 0.0014). Traces related to use featured an average perimeter of 7 mm and an average area of 1 mm2. Damage was localised near the artefact’s centre (mean distance 10mm) and was moderately dispersed over the used surface (stde elongation 1.3ad).
Three functional areas were identified on artefact RF127, corresponding to its apices (RF127a; RF127b) (Fig 28I, Table 5) and its short edge (RF-127c) (Fig 28II, Table 5). The wear identified on the apical area was associated with the production of scaled retouching, while the traces affecting its short edge were related to percussion activity involving the production of blank and core management. The apical area of the tool was characterised by a medium degree of surface roughness: TRI mean value 0.0015 (apical top) and TRI mean value 0.0021 (apical bottom). Both the apices were characterised by a low degree of topographic variability as indicated by the VRM mean values of 0.0012 (apical top) and 0.0011 (apical bottom). Use related damage affecting the top apical area featured a mean perimeter of 6.3 mm and an average area of 1 mm2. Similar dimensions were recorded within the traces located on the bottom apical area of the tool (average perimeter 6.7 mm and mean area 1 mm2). On both functional areas use related damage was dispersed over the surface as indicated by the recorded standard deviational ellipse value of 1.3 ad. The short edge of RF127 was instead characterised by slightly steeper depressions (mean value 20°) compared to the ones observed over its flat surface. The topography of the surface was moderately rough (TRI mean value of 0.0021) with the lower values coinciding with the area of the edge mostly affected by use related damage. The surface topographic variability was low, given the VRM mean value of 0.0006. The traces identified on the short edge of RF127 exhibited a mean perimeter of 2.7 mm and an average area of 1 mm2. They appeared highly dispersed over the utilised surface, as indicated by the high standard deviational ellipse elongation value of 2.5 ad (Fig 29, Table 5).
The surface of the tool (I) has been used in retouch activities while its edge (II) was used to produce bladelets/core adjustment. (a) Spatial distribution of the identified wear; (b) slope; (c) terrain roughness index; (d) vector roughness measure.
(a) Dimension of the wear identified over the utilized areas; (b) mean distance of the identified wear from the object centre; (c) mean distance of the identified wear from the object edge; (d) dispersion of the identified wear over the tool surface defined by the elongation of the standard deviational ellipse.
Through the application of a dedicated experimental framework we were able to test the usage, and suitability for the task, of different areas of the hammerstone or retoucher. Use wear analysis, performed at low and high magnification, permitted the definition of the morphological characteristics of wear associated with each of the performed activities. In the study of archaeological samples from Fumane Cave, macro-trace analysis, performed at low magnification, resulted to be more indicative than the observation of micro wear at high magnification, due to the fact that in some cases chemical alteration had prevented the preservation of the micro traces. GIS analysis allowed the investigation of the macro-traces from a quantitative point of view, analysing aspects such as dimensions and spatial distribution of the wear generated by each activity. Moreover, it permitted the collection of data concerning the topographic characteristics (e.g. slope, roughness and topographic variability) of the utilised area of the tool.
Overall, the dedicated experimental framework allowed the isolation of both qualitative and quantitative features concerning use wear deriving from both percussion and retouching activities. The microscopic analysis of the surfaces provided qualitative aspects such as development of polish, micro-striations etc. GIS analysis revealed quantitative data (distance from centre, distance from edge and wear dispersion, this latter defined by the standard deviational ellipse elongation value) concerning the morphometry of use related damage associated to retouching activity, bipolar percussion and core maintenance activities.
Comparing the experimental and archaeological datasets provided positive results (Figs 30, 31 and 32), supporting interpretation derived from use wear analysis. However, on this matter, a note of caution needs to be made. When the dimensions of damage were compared, those of the wear on the experimental replicas resulted to be much larger than those observed on the archaeological materials. This is due to the post depositional alteration affecting the archaeological specimens and leading to an overall rounding and modification of the wear morphology, suggesting that dimensions alone cannot be considered as a diagnostic feature in the interpretation of tool use.
In detail, crosses = retouch activities; diamonds = bipolar percussion; triangles = striking platform management; square = bladelets production).
Within the Fumane Cave macro-lithic sample, several implements exhibited use patterns resembling the ones recorded on the experimental replicas used in scaled and marginal retouching. In particular, artefacts RF67 and RF127 have been interpreted as retouchers used for scaled retouching, while the apical area of artefact RF92 and RF80 exhibited use wear features which led to their interpretation as retouchers used to produce marginal retouching. On 4 archaeological artefacts coming from Fumane Cave, the presence of overlapping pits over the short edges of the tools (RF127, RF138) and of deep long striations affecting the flat surface of the implements (RF73, RF37) led to the interpretation of the artefacts as hammerstones used in both blank production and core maintenance activities. Wear patterns similar to the ones associated with bipolar percussion have been identified on the central surface area of artefact RF92 leading to the interpretation of the use of its central area as an anvil (Fig 33). Our results enabled the identification of specific functional patterns related to the use of hammerstones and retouchers at Fumane Cave. We have been able to isolate specific patterns both regarding the morphology of the wear, its spatial distribution and the topography of the used area associated with each of the activities performed. This permitted the placing of the Protoaurignacian and Aurignacian macro-tools of Fumane Cave into specific stages of the production process of chipped tools. Our analysis underlined the high efficiency of the Fumane cave macro-tools in activities concerning core maintenance, blank production and tool retouching. The use of these implements in advanced stages of core maintenance and blank production is suggested by the absence of artefacts bearing traces associated with the initial stage of core reduction. Furthermore, the analysis of the retouchers suggests relevant behavioural insights regarding the choice of objects with specific features (i.e. different types of limestones, soft or compact; the morphological features that favours the success of the product;). Moreover, the analysis of wear from a morphological and spatial point of view permitted to formulate a preliminary hypothesis, that will be confirmed in the future, under which the archaeological tools were used employing two preferential gestures, perpendicular and oblique, involved in the production of scaled, marginal and abrupt retouches. The experimental results showed how, adopting a scaled retouch, it was possible not only to package or maintain formal tools such as end-scrapers, but also to delineate the lateral edges of some thicker blades. On the contrary, marginal and abrupt retouch was mainly used to transform the flake/blade edges. Retouching on an anvil, and edge abrasion techniques aimed at bladelet retouching, currently do not match with the archaeological traces and, following our results, it was difficult to use the flat surface of the retoucher to perform the former activity. The absence of these types of use wear does not exclude that other raw materials and techniques have been used in the production of the Dufour and pointed bladelets at Fumane Cave.
(a) Experimental striations (10x) related to the overhang abrasion, localised (b) on the flat surface of the pebble; (c) archaeological striations (10x), localised (d) on the flat surface of the sample; (e) experimental pits (15x) related to core maintenance/bladelets removal, with sub-oval morphology, localised (f) around the short edge of the pebble; (g) archaeological pits (10x) with sub-oval morphology, (h) localised around the short edge of the sample; (i) experimental pits (40x) related to scaled retouching, with linear (half-moon) morphology, rough bottom, localised (l) on the apices of the flat surface; (m) archaeological pits (40x) with linear (half-moon) morphology, rough bottom, localised (n) on the apices of the flat surface; (o) experimental pits (20x), related to the anvil used for the flakes detachment, with sub-triangular morphology, localised (p) in the centre of the pebble; (q) archaeological pits (20x), with sub-triangular morphology, localised (r) in the centre of sample; (s) experimental circular pits associated with the striations (20x), related to marginal retouching, localised (t) on the apices of the flat surface with oblique orientation; (u) archaeological circular pits and striations associated (20x), localised on the apices of the flat surface with oblique orientation.
Given the lack of functional studies focused on the uses of hammerstones and retouchers, the combined approach presented here enhances our current knowledge of this specific kind of tool. This approach provides data not only related to the use of the tools at the site (e.g. ) but also involving the gestures and ergonomic choices characterising the Protoaurignacian and Aurignacian human groups of Fumane Cave. As emphasized by Bracco et al.  the reconstruction of gesture plays a major role within the analysis of technical processes. The traces of prehension observed and documented during the experimental phase, and evidenced in the archaeological sample, reveal that in Fumane Cave there were different ways of handling the objects. However, it is evident that the study of the variables on the modalities of prehension requires the formulation of a specific experimental protocol.
The preliminary study conducted here showed the potentials of an integrated method applied to the study of prehistoric macro-lithic tools, which can be successfully increased in the future with the support of a broader experimental collection. Our results emphasize the importance of the combination of qualitative (use wear) and quantitative (GIS analysis) approaches which can be applied to a variety of tool categories, providing new data enhancing not only our knowledge regarding the use of ancient Palaeolithic or Mesolithic tools but also, in a broader way, our understanding of ancient human behaviour.
We are grateful to Giulia Formichella for the drawing in Fig 6 and to the two anonymous reviewers for their careful reading of the manuscript and constructive comments, which helped us to improve the first version of the article.
Adams J, Delgado S, Dubreuil L, Hamon C, Plisson H, Risch R. Functional Analysis of Macro-Lithic Artefacts: A Focus On Working Surfaces. In: Stenke F, Eigeland L, Costa L-J editors. Non-flint raw material use in prehistory: Old prejudices and new directions. Oxford: BAR International Series; 2009.
Adams JL. Ground stone analysis: a technological approach. University of Utah Press; 2014.
Adams JL. Understanding grinding technology through experimentation. Designing Experimental Research in Archaeology, Examining Technology through Production and Use. University Press of Colorado, Boulder; 2010. pp. 129–151.
DeBeaune S. Nonflint Stone Tools of the Early Upper Paleolithic. CRC Press Inc., Boca Raton, Florida; 1993.
- 5. DeBeaune SA, Davidson I, Hardy B, McGrew W, Marchant L, Reader S, et al. The invention of technology: prehistory and cognition. Curr Anthropol. The University of Chicago Press; 2004;45: 139–162.
- 6. Schiffer M, Skibo J. Theory and Experiment in the Study of Technological Change. Curr Anthropol. 1987;28: 595–622. http://dx.doi.org/10.1086/203601
- 7. Adams JL. Mechanisms of wear on ground stone surfaces. Pacific Coast Archaeol Soc Q. 1993;29: 61–74.
- 8. Adams JL. Refocusing the Role of Food-Grinding Tools as Correlates for Subsistence Strategies in the U.S. Southwest. Am Antiq. 1999;64: 475–498.
- 9. Astruc L, Vargiolu R, Zahouani H. Wear assessments of prehistoric instruments. Wear. 2003;255: 341–347.
- 10. Bofill M. Quantitative analysis of use-wear patterns: a functional approach to study grinding stone tools. Broadening Horizons 3, Conference of young researchers working in the Ancient Near East. 2012. pp. 63–84.
- 11. Bofill M, Procopiou H, Vargiolu R, Zahouani H. Use-wear analysis of near eastern prehistoric grinding stones. Regards croisés sur les Outil liés au Trav des végétaux. 2013; 225–242.
Conte IC, Fernández TL, Astruc L, Rodriguez AC. Use-wear analysis of nonflint lithic raw materials: the cases of quartz/quartzite and obsidian. Use-wear and residue analysis in Archaeology. Springer; 2015. pp. 59–81.
DeBeaune S. Les galets utilisés au Paléolithique supérieur: approche archéologique et expérimentale. CNRS; 1997.
- 14. Dubreuil L, Savage D. Ground stones: A synthesis of the use-wear approach. J Archaeol Sci. Elsevier Ltd; 2014;48: 139–153.
Dubreuil L, Savage D, Delgado-Raack S, Plisson H, Stephenson B, de la Torre I. Current analytical frameworks for studies of use—wear on ground stone tools. Use-wear and residue analysis in archaeology. Springer; 2015. pp. 105–158.
- 16. Dubreuil L, Nadel D. The development of plant food processing in the Levant: insights from use-wear analysis of Early Epipalaeolithic ground stone tools. Philos Trans R Soc London B Biol Sci. 2015;370: 20140357–. pmid:26483535
- 17. Fullagar R, Hayes E, Stephenson B, Field J, Matheson C, Stern N, et al. Evidence for P leistocene seed grinding at L ake M ungo, south-eastern A ustralia. Archaeol Ocean. Wiley Online Library; 2015;50: 3–19.
- 18. Hamon C. Functional analysis of stone grinding and polishing tools from the earliest Neolithic of north-western Europe. J Archaeol Sci. 2008;35: 1502–1520.
- 19. Hamon C. Le statut des outils de broyage et d’abrasion dans l’espace domestique au Néolithique ancien en Bassin parisien. Notae Praehistoricae. 2004;24: 117–128.
- 20. Hamon C. Broyage et abrasion au néolithique ancien: caractérisation technique et fonctionnelle de l’outillage en grès du bassin parisien. BAR International Series. 2004. 1551.2006
- 21. Hayes E, Pardoe C, Fullagar R. Sandstone grinding/pounding tools: Use-trace reference libraries and Australian archaeological applications. J Archaeol Sci Reports. Elsevier; 2018;20: 97–114.
Plisson H. Etude fonctionnelle d’outillages lithiques préhistoriques par l’analyse des micro-usures: recherche méthodologique et archéologique. Université de Paris I. 1985.
Caricola I. La funzione dei macro lithic tools e lo sfruttamento delle risorse minerarie durante la Preistoria recente nel Mediterraneoo Occidentale. Sapienza Università di Roma. 2017.
- 24. Delgado-Raack S, Gómez-Gras D, Risch R. The mechanical properties of macrolithic artifacts: a methodological background for functional analysis. J Archaeol Sci. 2009;36: 1823–1831.
- 25. Domanski M, Webb JA, Boland J. Mechanical properties of stone artefact materials and the effect of heat treatment. Archaeometry. Wiley Online Library; 1994;36: 177–208.
Jackson MJ, Hitchiner MP. High performance grinding and advanced cutting tools. Springer Science & Business Media; 2012.
- 27. Lerner H, Du X, Costopoulos A, Ostoja-Starzewski M. Lithic raw material physical properties and use-wear accrual. J Archaeol Sci. 2007;34: 711–722.
- 28. Stemp WJ, Stemp M. Documenting stages of polish development on experimental stone tools: surface characterization by fractal geometry using UBM laser profilometry. J Archaeol Sci. Academic Press; 2003;30: 287–296.
- 29. Byrne L, Ollé A, Vergès JM. Under the hammer: Residues resulting from production and microwear on experimental stone tools. Archaeometry. 2006;48: 549–564.
- 30. Buonasera T. Investigating the presence of ancient absorbed organic residues in groundstone using GC-MS and other analytical techniques: a residue study of several prehistoric milling tools from central California. J Archaeol Sci. 2007;34: 1379–1390.
Buonasera TY. Expanding archaeological approaches to ground stone: Modeling manufacturing costs, analyzing absorbed organic residues, and exploring social dimensions of milling tools. The University of Arizona. 2012.
- 32. Buonasera TY. More than acorns and small seeds: A diachronic analysis of mortuary associated ground stone from the south San Francisco Bay area. J Anthropol Archaeol. Elsevier Inc.; 2013;32: 190–211.
- 33. Fullagar R, Liu L, Bestel S, Jones D, Ge W, Wilson A, et al. Stone tool-use experiments to determine the function of grinding stones and denticulate sickles. Bullettin Indo-Pacific Prehistory Assoc. 2012;32: 29–44.
Bicho N, Marreiros J, Gibaja JF. Use-Wear and Residue Analysis in Archeology. Use-wear and residue analysis in archaeology. Springer; 2015. pp. 1–4.
- 35. Pearsall DM, Chandler-Ezell K, Zeidler JA. Maize in ancient Ecuador: Results of residue analysis of stone tools from the Real Alto site. J Archaeol Sci. 2004;31: 423–442.
- 36. Piperno DR, Ranere AJ, Holst I, Iriarte J, Dickau R. Starch grain and phytolith evidence for early ninth millennium B.P. maize from the Central Balsas River Valley, Mexico. Proc Natl Acad Sci U S A. 2009;106: 5019–5024. pmid:19307570
Portillo M, Bofill M, Molist M, Albert RM. Phytolith and use-wear functional evidence for grinding stones from the Near East. Regards croisés sur les Outil liés au Trav des végétaux An Interdiscip Focus plant-working tools. Éditions APDCA Antibes; 2013; 205–218.
- 38. Yang X, Yu J, Lü H, Cui T, Guo J, Ge Q. Starch grain analysis reveals function of grinding stone tools at Shangzhai site, Beijing. Sci China Ser D Earth Sci. Springer; 2009;52: 1164–1171.
- 39. Anderson PC, Georges JM, Vargiolu R, Zahouani H. Insights from a tribological analysis of the tribulum. J Archaeol Sci. 2006;33: 1559–1568.
- 40. Bhushan B, Israelachvili JN, Landman U. Nanotribology: friction, wear and lubrication at the atomic scale. Nature. Nature Publishing Group; 1995;374: 607.
Bhushan B. Modern tribology handbook, two volume set. CRC press; 2000.
Bhushan B. Introduction to tribology. John Wiley & Sons; 2013.
Bhushan B, Gupta BK. Handbook of tribology: materials, coatings, and surface treatments. McGraw-Hill, New York, NY (United States); 1991;
Czichos H. Tribology: a systems approach to the science and technology of friction, lubrication, and wear. Elsevier; 2009.
Dowson D. History of tribology. Addison-Wesley Longman Limited; 1979.
Halling J. The tribology of surface films. Thin Solid Films. Elsevier; 1983;108: 103–115.
Arnold E. Tribology: Friction and Wear of Engineering Materials. IM Hutchins. 1992;
Quinn T. Oxidative Wear Mechanisms. Conference of Chemical Effects at Bearing Surfaces. Swansea; 1971.
- 49. Aranguren B, Becattini R, Lippi MM, Revedin A. Grinding flour in Upper Palaeolithic Europe (25000 years bp). Antiquity. Cambridge University Press; 2007;81: 845–855.
- 50. Aranguren B, Longo L, Mariotti Lippi M, Revedin A. Evidence of edible plant exploitation. Pavlov 2007–2011, Dolni Vestonice Stud. 2012;18: 170e179.
- 51. Revedin A, Aranguren B, Becattini R, Longo L, Marconi E, Lippi MM, et al. Thirty thousand-year-old evidence of plant food processing. Proc Natl Acad Sci U S A. 2010;107: 18815–18819. pmid:20956317
- 52. Aranguren B, Revedin A. Bilancino settlement: Integrated methodological approaches for the historical reconstruction. Hum Evol. 2011;25: 97–105.
- 53. Mariotti Lippi M, Foggi B, Aranguren B, Ronchitelli A, Revedin A. Multistep food plant processing at Grotta Paglicci (Southern Italy) around 32,600 cal B.P. Proc Natl Acad Sci U S A. 2015;112: 12075–12080. pmid:26351674
- 54. Liu L, Field J, Weisskopf A, Webb J, Jiang L, Wang H, et al. The exploitation of acorn and rice in early Holocene Lower Yangzi River, China. Acta Anthropol Sin. 2010;29.
- 55. Liu L, Ge W, Bestel S, Jones D, Shi J, Song Y, et al. Plant exploitation of the last foragers at Shizitan in the Middle Yellow River Valley China: Evidence from grinding stones. J Archaeol Sci. Elsevier Ltd; 2011;38: 3524–3532.
- 56. Nadel D, Piperno DR, Holst I, Snir A. New evidence for the processing of wild cereal grains at Ohalo II, a 23 000-year- old campsite on the shore of the Sea of Galilee, Israel. Antiquity. 2012;86: 990–1003.
- 57. Valamoti SM, Chondrou D, Papadopoulou L. Plant food processing and ground stone equipment in prehistoric Greece: An experimental investigation using seeds of einkorn and grass-pea. Regards croisés sur les Outil liés au Trav des végétaux An Interdiscip Focus plant-working tools. 2013; 169–187.
- 58. Wright K. A Classification System for Ground Stone Tools from the Prehistoric Levant. Paléorient. 1992;18: 53–81.
- 59. Šajnerová-Dušková A, Fridrich J, Sýkorová I. Pitted and grinding stones from Middle Palaeolithic settlements in Bohemia: a functional study. Non-Flint Raw Mater Use Prehistory Old Prejud new Dir. 2009; 145–151.
- 60. d’Errico F, Salomon H, Vignaud C, Stringer C. Pigments from the Middle Palaeolithic levels of Es-Skhul (Mount Carmel, Israel). J Archaeol Sci. 2010;37: 3099–3110.
- 61. Dubreuil L, Grosman L. Ochre and hide-working at a Natufian burial place. Antiquity. 2009;83: 935–954.
- 62. Hamon C, Billard C, Bosquet D, Constantin C, Jadin I. Usages et transformation de l’hématite dans le Néolithique ancien d’Europe du Nord-Ouest. Antropol Praehist. 2016;125: 45–61.
- 63. Henshilwood CS, D’Errico F, Van Niekerk KL, Coquinot Y, Jacobs Z, Lauritzen M-E, et al. A 100,000-year-old ochre-processing workshop at Blombos Cave, South Africa. Science (80-). American Association for the Advancement of Science; 2011;334: 219–222.
- 64. Salomon H. Les matières colorantes au début du Paléolithique supérieur: sources, transformations et fonctions. Bordeaux 1. 2009.
- 65. Henrich J. Cultural group selection, coevolutionary processes and large-scale cooperation. J Econ Behav Organ. Elsevier; 2004;53: 3–35.
- 66. Stout D, Chaminade T. Stone tools, language and the brain in human evolution. Philos Trans R Soc B Biol Sci. 2012;367: 75–87. pmid:22106428
- 67. Arroyo A, de la Torre I. Pounding tools in HWK EE and EF-HR (Olduvai Gorge, Tanzania): Percussive activities in the Oldowan-Acheulean transition. J Hum Evol. Elsevier; 2017;
- 68. Barkai R, Gopher A. On anachronism: The curious presence of Spheroids and Polyhedrons at Acheulo—Yabrudian Qesem Cave, Israel. Quat Int. Elsevier; 2016;398: 118–128.
- 69. Malinsky-Buller A, Hovers E, Marder O. Making time: “Living floors”, “palimpsests” and site formation processes—A perspective from the open-air Lower Paleolithic site of Revadim Quarry, Israel. J Anthropol Archaeol. Elsevier Inc.; 2011;30: 89–101.
Raynal J-P, Sbihi-Alaoui F. Le Macro-Outillage de Percussion. In: Raynal J-P, Abderrahim M, editors. Préhistoire de Casablanca 1- La Grotte des Rhinocéros (fouilles 1991 et 1996). Rabat; 2016.
- 71. Navarro C, Pérez SD, Bustos-Pérez G, Monteagudo F, Navas C, Preysler JB. Experimental study on flint hammerstone use in Discoid-Levallois technologies: A comparison with the workshop assemblages of the central Iberian Peninsula. J Lithic Stud. 2016;3.
- 72. Pop E, Charalampopoulos D, Arps CS, Verbaas A, Roebroeks W, Gaudzinski-Windheuser S, et al. Middle Palaeolithic Percussive Tools from the Last Interglacial Site Neumark-Nord 2/2 (Germany) and the Visibility of Such Tools in the Archaeological Record. J Paleolit Archaeol. Springer; 2018; 1–26.
- 73. Veselsky AP. Kabazi V, Sub-Unit III/1: The Starosele Facie of Micoquian. Kabazi V Interstratification Micoquian Levallois-Mousterian Camp Sites Palaeolithic sites Crimea. 2008;3: 129–179.
- 74. David É, Sørensen M. First insights into the identification of bone and antler tools used in the indirect percussion and pressure techniques during the early postglacial. Quat Int. Elsevier; 2016;423: 123–142.
- 75. Chase PG. Tool-making tools and Middle Paleolithic behavior. Curr Anthropol. University of Chicago Press; 1990;31: 443–447.
- 76. Abrams G, Bello SM, Di Modica K, Pirson S, Bonjean D. When Neanderthals used cave bear (Ursus spelaeus) remains: Bone retouchers from unit 5 of Scladina Cave (Belgium). Quat Int. Elsevier; 2014;326: 274–287.
- 77. Blasco R, Rosell J, Cuartero F, Peris JF, Gopher A, Barkai R. Using bones to shape stones: MIS 9 bone retouchers at both edges of the Mediterranean Sea. PLoS One. Public Library of Science; 2013;8: e76780. pmid:24146928
- 78. Bourguignon L. Apports de l’expérimentation et de l’analyse techno-morpho-fonctionnelle à la reconnaissance du processus d’aménagement de la retouche Quina. Préhistoire Approch expérimentale. Editions MM Montagnac Paris; 2001; 35–66.
- 79. Costamagno S, Bourguignon L, Soulier M-C, Meignen L, Beauval C, Rendu W, et al. Bone Retouchers and Site Function in the Quina Mousterian: the case of Les Pradelles (Marillac—Le—Franc, France). The Origins of Bone Tool Technologies. 2018. pp. 1–31.
- 80. Daujeard C, Moncel M-H, Fiore I, Tagliacozzo A, Bindon P, Raynal J-P. Middle Paleolithic bone retouchers in Southeastern France: Variability and functionality. Quat Int. Elsevier; 2014;326: 492–518.
- 81. Karavanić I, Šokec T. The Middle Paleolithic percussion or pressure flaking tools? The comparison of experimental and archaeological material from Croatia. Pril Instituta za Arheol u Zagreb. Institut za arheologiju; 2003;20: 5–14.
- 82. Jéquier C, Romandini M, Peresani M, Others. Ritoccatori in materie dure animali, confronto tra Musteriano finale (44ky cal. BP) e Uluzziano (42ky cal. BP) in Nord Italia, il caso di Grotta di Fumane (VR). Ann dell’Università di Ferrara Museol Sci e Nat. Annali dell’Università degli Studi di Ferrara; 2012;8: 15.
- 83. Mallye J-B, Thiébaut C, Mourre V, Costamagno S, Claud É, Weisbecker P. The Mousterian bone retouchers of Noisetier Cave: experimentation and identification of marks. J Archaeol Sci. Elsevier; 2012;39: 1131–1142.
- 84. Mozota Holgueras M. Un análisis tecno-funcional de los retocadores óseos musterienses del norte de la Penìnsula Ibérica, y su aplicación al estudio de los grupos neandertales. Munibe Antrol Arkeol. Sociedad de Ciencias Aranzadi; 2015;66: 5–21.
- 85. Tejero M-M, Yeshurun R, Barzilai O, Goder-Goldberger M, Hershkovitz I, Lavi R, et al. The osseous industry from Manot Cave (Western Galilee, Israel): Technical and conceptual behaviours of bone and antler exploitation in the Levantine Aurignacian. Quat Int. Elsevier; 2016;403: 90–106.
- 86. Yeshurun R, Tejero M-M, Barzilai O, Hershkovitz I, Marder O. Upper Palaeolithic bone retouchers from Manot Cave (Israel): A preliminary analysis of a (yet) rare phenomenon in the Levant. Orig Bone Tool Technol. Römish-Germanisches Zentralmuseums; 2017; 1–9.
- 87. Averbouh A. Un fragment de percuteur sur partie basilaire de la grotte magdalénienne d’Enlène (Ariège). Bull la Société préhistorique française. JSTOR; 1999; 497–504.
- 88. Bello SM, Parfitt SA, De Groote I, Kennaway G. Investigating experimental knapping damage on an antler hammer: a pilot-study using high-resolution imaging and analytical techniques. J Archaeol Sci. Elsevier; 2013;40: 4528–4537.
- 89. Goutas N. From stone flaking to grinding: Three original Pavlovian antler tools from Moravia (Pavlov I, Czech Republic). Quat Int. Elsevier; 2015;359: 240–260.
- 90. Vitezović S. Retouching Tools from Osseous Raw Materials in the Starčevo Culture. Haemus J. 2013;2: 31–32.
- 91. Bietti A, Cancellieri E, Corinaldesi C, Grimaldi S, Spinapolice E. La percussion sur enclume en Italie centrale Tyrrhénienne. Paléo. Société des amis du Musée national de préhistoire et de la recherche archéologique (SAMRA); 2010; 143–180.
- 92. Dibble HL, Pelcin A. The effect of hammer mass and velocity on flake mass. J Archaeol Sci. Academic Press; 1995;22: 429–439.
- 93. Driscoll K, Garc$\$’$\$ia-Rojas M. Their lips are sealed: identifying hard stone, soft stone, and antler hammer direct percussion in Palaeolithic prismatic blade production. J Archaeol Sci. Elsevier; 2014;47: 134–141.
- 94. Mourre V. Le débitage sur enclume au Paléolithique moyen dans le Sud-Ouest de la France. BAR Int Ser. TEMPUS REPARATSM; 2004;1239: 29–38.
- 95. Inizan M-L, Pelegrin J. Débitage par pression et expérimentation: une question de méthodologie. Paléorient. JSTOR; 2002; 105–108.
- 96. Pelegrin J, Texier P-J. Les techniques de taille de la pierre. Les dossiers d’archeologie. 2004; 26–33.
- 97. Roussel M, Bourguignon L, Soressi M. Identification par l’expérimentation de la percussion au percuteur de calcaire au Paléolithique moyen: le cas du façonnage des racloirs bifaciaux Quina de Chez Pinaud (Jonzac, Charente-Maritime). Bull la Société préhistorique française. JSTOR; 2009; 219–238.
- 98. Duches R, Peresani M, Pasetti P. Success of a flexible behavior. Considerations on the manufacture of Late Epigravettian lithic projectile implements according to experimental tests. Archaeol Anthropol Sci. Springer; 2017; 1–27.
- 99. Crezzini J. Studio della distribuzione delle tracce antropiche sui resti di ungulati del Gravettiano antico di Grotta Paglicci (Rignano Garganico-FG): Il trattamento delle frazioni distali degli arti di Bos primigenius. Ann dell’Università degli Stud di Ferrara. 2007;1824: 2707.
- 100. Belluomini G, Calderoni G, Collina C, Fedi M, Fiore I, Gallotti R, et al. La Grotta di Roccia San Sebastiano (Mondragone, Caserta). Atti della XL Riun Sci dell’Istituto Ital di Preist e Protostoria, Strateg di insediamento fra Lazio e Camp età Preist e protostorica, Roma, Napoli, Pompei. 2007;30: 319–331.
- 101. de la Torre I, Benito-Calvo A, Arroyo A, Zupancich A, Proffitt T. Experimental protocols for the study of battered stone anvils from Olduvai Gorge (Tanzania). J Archaeol Sci. Elsevier Ltd; 2013;40: 313–332.
- 102. Caruana M V, Carvalho S, Braun DR, Presnyakova D, Haslam M, Archer W, et al. Quantifying traces of tool use: a novel morphometric analysis of damage patterns on percussive tools. PLoS One. Public Library of Science; 2014;9: e113856. pmid:25415303
- 103. Benito-Calvo A, Carvalho S, Arroyo A, Matsuzawa T, de la Torre I. First GIS analysis of modern stone tools used by wild chimpanzees (Pan troglodytes verus) in Bossou, Guinea, West Africa. PLoS One. Public Library of Science; 2015;10: e0121613. pmid:25793642
- 104. Benito-Calvo A, Crittenden AN, Livengood S V, Sánchez-Romero L, Martínez-Fernández A, De La Torre I, et al. 3D 360° surface morphometric analysis of pounding stone tools used by Hadza foragers of Tanzania: A new methodological approach for studying percussive stone artefacts. J Archaeol Sci Reports. 2018;20: 611–621.
- 105. Benito-Calvo A, Arroyo A, Sánchez-Romero L, Pante M, de la Torre I. Quantifying 3D Micro-Surface Changes on Experimental Stones Used to Break Bones and Their Implications for the Analysis of Early Stone Age Pounding Tools. Archaeometry. 2017;
- 106. Martini M, Sibilia E, Croci S, Cremaschi M. Thermoluminescence (TL) dating of burnt flints: problems, perspectives and some examples of application. J Cult Herit. Elsevier; 2001;2: 179–190.
- 107. López-Garc$\$’$\$ia JM, dalla Valle C, Cremaschi M, Peresani M. Reconstruction of the Neanderthal and Modern Human landscape and climate from the Fumane cave sequence (Verona, Italy) using small-mammal assemblages. Quat Sci Rev. Elsevier; 2015;128: 1–13.
- 108. Peresani M. Fifty thousand years of flint knapping and tool shaping across the Mousterian and Uluzzian sequence of Fumane cave. Quat Int. Elsevier; 2012;247: 125–150.
- 109. Peresani M, Cristiani E, Romandini M. The Uluzzian technology of Grotta di Fumane and its implication for reconstructing cultural dynamics in the Middle—Upper Palaeolithic transition of Western Eurasia. J Hum Evol. Elsevier; 2016;91: 36–56. pmid:26852812
- 110. Broglio A, Bertola S, De Stefani M, Marini D, Lemorini C, Rossetti P, et al. La production lamellaire et les armatures lamellaires de l’ aurignacien ancien de la Grotte de Fumane (Monts Lessini, Vénétie). Arch ologiques; 2005;
- 111. Falcucci A, Conard NJ, Peresani M. A critical assessment of the Protoaurignacian lithic technology at Fumane Cave and its implications for the definition of the earliest Aurignacian. PLoS One. Public Library of Science; 2017;12: e0189241. pmid:29216284
- 112. Bartolomei G, Broglio A, Cassoli P f, Castelletti L, Cremaschi M, Giacobini G, et al. La Grotte-Abri de Fumane. Un site Aurignacien au Sud des Alps. Preist Alp. 1992;28: 131–179.
- 113. Benazzi S, Slon V, Talamo S, Negrino F, Peresani M, Bailey SE, et al. The makers of the Protoaurignacian and implications for Neandertal extinction. Science (80-). American Association for the Advancement of Science; 2015; aaa2773.
- 114. Higham T, Brock F, Peresani M, Broglio A, Wood R, Douka K. Problems with radiocarbon dating the Middle to Upper Palaeolithic transition in Italy. Quat Sci Rev. Elsevier; 2009;28: 1257–1267.
- 115. Falcucci A, Peresani M, Roussel M, Normand C, Soressi M. What’s the point? Retouched bladelet variability in the Protoaurignacian. Results from Fumane, Isturitz, and Les Cottés. Archaeol Anthropol Sci. Springer; 2018;10: 539–554.
- 116. Falcucci A., Conard N.J., Peresani M. The chrono-cultural narrative of the Fumanian Aurignacian supports the inapplicability of the Aquitaine Model on a supra-regional scale. PESHE. 2018. p. 62.
- 117. De Stefani M, Dini M, Klempererova H, Peresani M, Ranaldo F, Ronchitelli A, et al. Continuity and replacement in flake production across the Middle-Upper Palaeolithic transition: a view over the Italian Peninsula. Flakes Not Bl Role Flake Prod Onset Up Palaeolithic Eur Mettmann. 2012; 135–151.
- 118. Falcucci A, Peresani M. Protoaurignacian core reduction procedures: blade and bladelet technologies at Fumane Cave. Lithic Technol. Taylor & Francis; 2018;43: 125–140.
- 119. de Sonneville-Bordes D, Piveteau J. Le paléolithique supérieur en Périgord. Imprimeries Delmas; 1960.
- 120. Bertola S, Broglio A, Cristiani E, De Stefani M, Gurioli F, Negrino F, et al. La diffusione del primo Aurignaziano a sud dell’arco alpino. Preist Alp. 2013;47: 17–30.
Keeley LH. Experimental determination of stone tool uses: a microwear analysis. University of Chicago Press; 1980.
- 122. Van Gijn A. Functional differentiation of late neolithic settlements in the Dutch coastal area. Interpret possibilities microwear Stud. Uppsala, Sweden; 1990;
- 123. Porter ST, Huber N, Hoyer C, Floss H. Portable and low-cost solutions to the imaging of Paleolithic art objects: A comparison of photogrammetry and reflectance transformation imaging. J Archaeol Sci Reports. Elsevier Ltd; 2016;10: 859–863.
- 124. Riley S, Degloria S, Elliot S. A Terrain Ruggedness Index that Quantifies Topographic Heterogeneity. Intermt J Sci. 1999;5: 23–27.
- 125. Lucas G. Production expérimentale de lamelles torses: approche préliminaire. Bull la Société préhistorique française. JSTOR; 1999; 145–151.
- 126. Fasser N, Visentin D, Fontana F, Barbaza M, Fat-Cheung C. Variabilità e modalità di confezione delle punte a dorso nel Tardoglaciale: i casi studi di Riparo Tagliente (VR, Italia) e Troubat (Hautes-Pyrénées, Francia). Sez di Museol Sci e Nat. 2018;13: 106–108.
Pelegrin J. Sur les techniques de retouche des armatures de projectile. CNRS Editions; 2004.
- 128. Arrighi S, Borgia V, D’Errico F, Ronchitelli A. I ciottoli decorati di Paglicci: raffigurazioni e utilizzo. Riv di Sci Preist. Istituto italiano di preistoria e protostoria; 2008;58: 39–58.
- 129. Bracco J-P, Dutour O, Chernokian R, Defleur A. Gestes techniques et debitage experimental. Elements de reflexion et potentialites de recherches dans l’etude du geste en prehistoire. Treballs d’Arqueologia. 1991;1: 163–172.