In the second half of the 19th century Pleistocene faunas were discovered in two sites, Sedia del Diavolo and Monte delle Gioie, contained in deposits of the Aniene River in the area of Rome (Latium, Italy). Fieldwork by A.C. Blanc in the late 1930’s proved the association of fauna and lithic industry within fluvial deposits interbedded with volcanoclastic layers. A human femoral diaphysis and a metatarsal were later identified in the faunal assemblage from Sedia del Diavolo and evaluated as Neandertal. The lithic assemblages from these two sites were the basis of the definition of the Protopontinian by M. Taschini, which she viewed as a late Middle Pleistocene industry very similar to the later, Upper Pleistocene Pontinian industries, thought to be characteristic of the Latium Mousterian. The chronostratigraphic framework of the Aniene river deposits has been recently updated and the lithic assemblages from these two sites are now confidently dated between 295 and 290 ka, close to the transition from MIS 9 to MIS 8. They fit chronologically between the industries of layers m and d from Torre in Pietra, a site 26 km northwest of Rome. The presence of the Levallois debitage is indisputable yet it occurs within an original technical context, different from what is known in other early occurrences of the Levallois. The date confirms the proposed chronology for the early Levallois in Europe. More importantly these two assemblages demonstrate that this technology can emerge in more diversified contexts than usually described. This suggests that its dispersal in Europe may have been rapid.
Citation: Soriano S, Villa P (2017) Early Levallois and the beginning of the Middle Paleolithic in central Italy. PLoS ONE 12(10): e0186082. https://doi.org/10.1371/journal.pone.0186082
Editor: Michael D. Petraglia, Max Planck Institute for the Science of Human History, GERMANY
Received: July 26, 2017; Accepted: September 25, 2017; Published: October 20, 2017
Copyright: © 2017 Soriano, Villa. 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 data generated by this paper are within the paper and the Supporting Information files. The collections are housed in two places: Museo Nazionale Preistorico Etnografico Luigi Pigorini, Laboratorio di Paletnologia, Piazza Guglielmo Marconi 14, 00144 Rome, Italy (Sedia del Diavolo: catalogue number from 105854 to 105863; Monte delle Gioie: catalogue number from 105875 to 105915), and Istituto Italiano di Paleontologia Umana, Convitto Nazionale Regina Margherita, Piazza R. Bonghi, 2 03012 Anagni (FR), Italy. The Sedia del Diavolo and Monte delle Gioie lithics had provenience indicated but no catalogue number. We then assigned to pieces individual catalogue numbers in sequential order from PV 1 to PV 65 for Monte delle Gioie and PV 1 to PV 15 for Sedia del Diavolo. PV stands for Paola Villa. The pieces are individually bagged in zipper bags with pre-printed labels and are stored in one plastic box.
Funding: Research on the Sedia del Diavolo and Monte delle Gioie lithics was funded by National Science Foundation US (https://www.nsf.gov) Grant BCS 1118143 to PV and SS. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing interests: The authors have declared that no competing interests exist.
Monte delle Gioie (hereafter MdG; 41°56'45"N; 12°30'44"E) and Sedia del Diavolo (SdD; 41° 55'46"N; 12°31'22"E) are the two oldest known archaeological sites within the city of Rome (Latium, Italy). They are located on the same middle terrace of the Aniene River, a left bank tributary of the Tiber, on opposite sides of the valley, in the north-east suburbs of Rome (Fig 1) They were discovered late in the 19th century and further surveyed and studied by A.C. Blanc from 1935 onward [1,2]. Blanc reported in detail the stratigraphic sequences, collected fauna and artifacts from both localities and established their contemporaneity (S2 File, History of Research). At both sites, the same layer of fluvial gravels yielded fossil faunas and lithic assemblages at the time considered Rissian in age [3–6]. According to Taschini  these assemblages, made on small flint pebbles, were characterized by a high proportion of standardized sidescrapers, mostly with Quina-like retouch, the presence of blanks with facetted platforms, and centripetal cores, a few with prepared platforms. The knapping techniques were direct percussion and the bipolar technique. According to Taschini these characters showed clear similarities to the Upper Pleistocene Mousterian industries in the Latium region also made on small flint pebbles, called Pontinian (e.g. Grotta dei Moscerini, Grotta Guattari and Grotta di Sant’Agostino; Fig 1). Thus she suggested that Sedia del Diavolo and Monte delle Gioie were the direct antecedents of the Pontinian and called them Protopontinian. The absence of Levallois debitage at both sites was noted by Piperno and Biddittu . Their view was retained in the literature.
Modified from Fig 3.1 in MOUSTERIAN LITHIC TECHNOLOGY: An Ecological Perspective by Steven L. Kuhn. Princeton University Press 1995.
The stratigraphic section of Sedia del Diavolo based on work of Blanc and published by Taschini  showed the occurrence at the base of the sequence of a volcanic tuff, more than 25 m thick, called Tufo Lionato, now known to be an eruption event of the Alban Hills volcanoes, southeast of Rome (Fig 1). Above the fluvial gravels that contained fauna and lithic artifacts there was another pyroclastic flow with white pumices, now known to represent an eruptive event of the Monti Sabatini volcanoes, north of Rome. Thus two volcanic events bracket the archaeological level but their ages became known only more recently, when correlation of the local geologic terms with the Alpine sequence of glacial and interglacial periods was abandoned in favor of a more complex approach. The stratigraphic section of Monte delle Gioie is very similar to that of Sedia del Diavolo .
Since 1980 intensive research on the Middle and Upper Pleistocene structural setting and eruptive events of the Latium volcanic region developed an approach combining tectonic studies with fluvial and shallow water stratigraphy, the timing of sea-water oscillations and dating by the 40Ar/39Ar method the numerous volcanic events interbedded with other sediments. The dates show that fining-upward aggradational sequence of deposits occurred rapidly in response to sea-level changes due to glacial melting [8–14](S3 File).
The geological setting of the lower Aniene River has been recently updated [14–16]. The outcrops studied by Blanc have been buried by the urban expansion of Rome but road construction close to the course of the Aniene River (Via Mascagni) opened new exposures and allowed further observation of Pleistocene deposits in the area of SdD and correlation of the SdD sequence with the one recognized in Via Mascagni [9,17]. The Tufo Lionato at the base of the SdD sequence is dated by 40Ar/39Ar to 365 ± 4 ka while the ash flow with pumices at the top, now known as Tufo Giallo di Sacrofano, is dated to 285 ± 2 ka [18,19]. Thus the aggradational sequence of Via Mascagni, SdD and MdG is clearly older than 285 ka and correlated by [15,16] with the glacial termination of MIS 8.6 and the following onset of warmer condition (MIS 8.5) (Fig 2; S3 File). As the deposition of the basal gravel is triggered by the maximum rate of sea-level rise during the glacial termination  fluvial gravels containing the industries were deposited during a narrow time span between the glacial maximum (at 295 ka according to ) and the glacial termination around 290 ka (According to  each glacial termination is dated by the temporal midpoint between the start and end of rapid change in δ18O). Thus the SdD and MdG lithic industry and human remains are assigned a tightly constrained age between 295 and 290 ka.
1: Clay with remains of conifer, 2: Fluvial gravels, 3: Tufo Lionato, 4: Fluvial epiclastic deposits, 5: Lacustrine silts, 6: Fluvial sands, 7: Fluvial gravels (with black pumice pebbles), 8: Lacustrine yellow silty sands with travertine and tuffite, 9: Tufo giallo di Sacrofano, 10: Marl with palustrean flora, 11: Travertine, 12: Modern backfill, 13: Colluvial deposits and post-glacial soil. Modified from [3,5,17]. The fluvial aggradational sequences are correlated to the deep-sea δ18O record from  (Data available at: http://lorraine-lisiecki.com/LR04stack.txt) according to . TIV = Termination IV.
The aggradational sequence of Via Mascagni, Sedia del Diavolo and Monte delle Gioie is not represented in the Torre in Pietra stratigraphic sequence (26 km northwest of Rome) which contains in level m at its base an Acheulian assemblage now dated by 40Ar/39Ar and U-series to MIS 10 (c. 350 ka) and higher up an early Middle Paleolithic assemblage in level d, dated to between 270 and 240 ka, at the very beginning of MIS 7 . Thus the industries from SdD and MdG are chronologically intermediate between the MIS 10 Acheulian and the early MIS 7 Middle Paleolithic of level d at Torre in Pietra. The artifacts and faunas from SdD/MdG, including two hominin remains from SdD assigned to Neandertals  (S1 File) are now confidently dated close to the transition from MIS 9 to MIS 8 between 295–290 ka and may be seen as a very old if not the oldest evidence of early Middle Paleolithic in Italy.
The objectives of this paper are (1) to describe the lithic industry recovered by A.C. Blanc at MdG and SdD; (2) to demonstrate that it is one of the earliest occurrence of Levallois in Italy; (3) to show that the Levallois method appears in a Middle Paleolithic type industry; (4) to point out that this industry is quite different from any early Levallois industry published so far and (5) to determine whether or not the industries from SdD/MdG could still be considered as Protopontinian as proposed by M. Taschini . Our results will be discussed in the broader context of emergence and diffusion of the Levallois method in Western Europe.
Material and methods
The SdD and MdG lithic assemblages are housed in the Pigorini National Museum of Prehistory and Ethnography in Rome and in the Italian Institute of Human Paleontology in the town of Anagni (Latium). Permits to study and take photos of the materials were obtained from the Soprintendenza of the Pigorini Museum (Prot. N. 212, 25.02.03/15, MBAC-S-MNPE Pigorini Cl. 25-02-04/5 and Cl. 23.03.02/1) and from Fabio Parenti, President of the Italian Institute of Human Paleontology.
Taschini inventoried 25 pieces from SdD (15 retouched pieces and 10 unretouched) and 62 retouched pieces and 30 unretouched from MdG. A single sidescraper from MdG illustrated by  was not found. In the Anagni sample from SdD, several pieces without evidence of human knapping or with dubious knapping features, with uncertain stratigraphic provenience or from later deposits were discarded. We recorded 25 pieces from SdD and 103 from MdG in our database.
As the two assemblages are small, we did not apply the sorting procedures used by us in the analysis of several assemblages from the Middle Stone Age [23–27] or the Lower and Middle Paleolithic . Only fragments without knapping features and pieces too rolled to be studied were rejected. Retouched pieces and cores are assigned individual catalog numbers, unless already assigned by the Museum or the excavator, and are individually bagged in reusable zipper bags with pre-printed labels.
We developed a technological approach to reconstruct the reduction sequences from raw material procurement to tool manufacture [28,29]. Flakes produced through debitage were categorized with reference to flake productions usually encountered in the Western European Middle Paleolithic. Due to the small amount of pieces our study is mainly based on qualitative analyses including metrical, technological and typological attributes combined with particular attention to the sequence of manufacture.
The total lithic assemblage from SdD and MdG is not large (N = 128; Table 1) but it is very diversified. Cores are frequent relative to the debitage (about 2.5 flakes per core). The frequency of retouched tools is high (56.2%) and most of them are sidescrapers. Retouched tools on flakes are dominant but 25% of them are made on cores and core fragments. Only four retouched tools are directly shaped on small pebbles or natural fragments.
Raw material and taphonomy
At MdG and SdD, flint is the dominant raw material with a single occurrence of chert or silicified limestone and 93.6% of the pieces with preserved cortical surfaces have water-worn cortex. In some later Mousterian sites from the area, active or fossil pebble beaches were the sources of flint pebbles . However flint pebbles from marine beaches are usually more regular in shape than fluvial ones while the great majority of the pebbles knapped at both site have rather irregular or angular shapes. Thus the sources of raw material were very likely fluvial deposits.
The original assemblages have been depleted of the smallest elements by winnowing in the course of fluvial transport [31–33]. In fact, objects less than 20 mm are almost completely lacking but in Middle Paleolithic studies, the sorting threshold is usually set at 20 mm as smaller elements are not very useful for chaîne opératoire reconstruction. The assemblage also includes pieces with different states of preservation but the intensity or distance of transport may have been limited because the frequency of pieces with a high degree of fluvial abrasion is low . In fact, 75.0% of the artifacts have fresh edges, without macroscopic evidence of fluvial transport and only 1.7% are very abraded (Table A in S1 File). The average size of lithic artefacts in both sites is rather similar (Table B in S1 File) indicating that the taphonomic biases and the possible recovery biases were identical on both sites. Since the goal of our study is primarily an understanding of technology we believe that the impact of taphonomic biases on our study are minor. Thus the assemblages from SdD and MdG, originating from the same fluvial deposits of the Aniene River and showing the same fluvial transport features (size sorting, degree of abrasion) were merged for the present study. Great similarities between these assemblages were emphasized by previous scholars [3,35,36].
An early Middle Paleolithic technology
At least three types of chaîne opératoire have been used to produce blanks. A fully-fledged and formalized Levallois technology is the most characteristic component of the SdD and MdG assemblages but it is not dominant. Three cores with a recurrent centripetal exploitation are undoubtedly categorized as Levallois (Fig 3A–3C). They are all fitting the criteria proposed by Boëda [37–39], Inizan et al. , Brantingham and Kuhn :
- the core is shaped by means of two intersecting flaking surfaces;
- the two surfaces are convex, asymmetrical and hierarchically related, one is the debitage surface, from which products are removed, the other constitutes the striking platform. The two surfaces are not interchangeable;
- the debitage surface is shaped so that the morphology of the product is pre-determined, which is essentially a function of the lateral and distal convexities of the surface;
- the Levallois products (filled in light grey on Fig 3) are split off along a fracture plane that is parallel or sub-parallel to the plane of intersection of the two surfaces, they are spanning the middle or most of the debitage surface;
- the convexities are shaped and maintained with short removals, centripetal and oblique with respect to the plane of intersection (filled in blue on Fig 3) and;
- the striking platform size and shape is adjusted to allow removal of flakes parallel to this plane, usually through retouch or faceting.
Cores. (A-C) Levallois cores. (D) Possible Levallois core. (B: photo by F. Naccari of the Pigorini Museum).
The chronology of removals on cores A and B clearly shows that the extraction of Levallois flakes is preceded by preparation of convexities and also at times followed by a partial re-preparation. This alternation is typical of the Levallois volumetric conception. Core C was prepared on a flake, a small portion of its of ventral surface, is still visible due to the shortness of the reduction sequence.
Two cores with hierarchically organized surfaces and centripetal removals might be Levallois but they are lacking or have a limited number of small removals to control peripheral convexities in their final condition (Fig 3D). A core fragment also has centripetal scars.
On a few flakes (N = 5) the organization of scars fits with our description of Levallois cores, thus they have been categorized as Levallois flakes (Fig 4A–4C). Short, oblique scars with respect to the ventral surface along a lateral edge are remains of convexities management. Platform preparation was typically faceted (Fig 4A) or surprisingly unprepared -a natural surface- (Fig 4B) probably because its orientation was suitable for flaking. Only marginally retouched edges have been observed on these few Levallois flakes.
Levallois and centripetal flakes. (A-C) Levallois flakes. (D-E) Centripetal flakes that might have been removed from a Levallois core. Caption and symbols used in drawings as in Fig 3. (B: photo by F. Naccari, Pigorini Museum).
A second, very distinctive and original, chaîne opératoire, between debitage and shaping, was used at SdD and MdG. Small rounded flint blocks or cobbles were split in half by means of a strong and very internal percussion with a hard hammer (Fig 5). Nevertheless the mode of fracture remains conchoidal in most of the cases and one can distinguish a ‘core-like’ piece (negative blank) with a single invasive negative scar and an entirely cortical thick ‘flake’ (positive blank). Bipolar percussion on an anvil was not used because the fracture is clearly conchoidal without any crushing and splintering on the distal end [25,41–44]. The aim is to obtain two blanks, almost equal in size, as large as the initial raw material volume and with a flat surface almost as large as the pebble itself. Structurally the two blanks are similar.
At MdG and SdD both flake and core resulting from this chaîne opératoire were considered suitable blanks. Once produced they were systematically retouched as sidescrapers (or convergent scrapers) and no blanks from this production seem to have been left unretouched. ‘Cores’ of that type were easy to identify (N = 11; 15.2% of retouched tools) because the retouched edge was commonly opposed (Fig 6A and 6B; Fig 7A and 7C) or adjacent (Fig 7B) to the negative of the bulbar scar. In some cases, especially highly reduced tools, the negatives of bulbar scar have been removed by one or two retouched edges (Fig 6C; Fig 7D). These scrapers are variable in size, especially thickness, from very thick (Fig 7B) to thinner ones (Fig 7C) in relation to their length and width. Flakes produced through this chaîne opératoire are much more difficult to identify with confidence because they are just totally cortical flakes and because their proximal part has been frequently removed due to reduction (Fig 8). They might also be thinner than cores.
Retouched core-like pieces. (A-C) « Core-like » pieces with a single invasive removal used as blanks for sidescrapers (A, B) or convergent scraper (C). (A, B: photos by F. Naccari, Pigorini Museum). Line drawings A and C modified after .
Retouched core-like pieces. (A-D) « Core-like » pieces with a single invasive removal used as blanks for sidescrapers. Line drawings modified after .
Scrapers on cortical flakes. (A-C) Cortical flakes [transformed in sidescrapers (A, B) or déjeté scraper (C)] that are possible complements of « Core-like » pieces with a single invasive removal. The platform was removed on A and B. Line drawings A and B modified after .
Blanks produced through this method are totally different from Levallois blanks and probably functionally complementary. They are significantly thicker than Levallois blanks (Fig 9) and consequently several of the sidescrapers made from these blanks bear a scaled retouch close to the classical sidescrapers of the Quina Mousterian. Superposition of many cycles of retouch is responsible for the stepped morphology of some scrapers’ edges (Fig 6C and Fig 7D).
Levallois flakes are thin blanks whose size variations are proportional (their thickness/width ratio varies little). Negative or positive blanks from the ‘core-like’ production system are thicker (nearly as thick as wide for heavily retouched ones) but much more variable in size.
This chaîne opératoire was never described before. We failed to find in the literature an exactly similar way to produce and modify two thick cortical blanks per nodule. At Les Tares, an Early Middle Paleolithic site in South-Western France, an experimental study has shown that a very internal percussion performed with hard hammer when the contact of the hammer with the core is not through a rounded end but rather through a longer edge of the hammer, produces very thick flakes, as large as the raw material volume, but the fracture was almost non-conchoidal  and usually several flakes were produced per nodule.
In assemblages of the Lower and Middle Paleolithic of the Latium a few small tools were made by using direct hard hammer percussion to flake a pebble with a large, unique and invasive removal. The large surface of the removal on the "core" or the "flake" was used as a striking platform for retouch. In the Italian Acheulian from Castel di Guido a few tools were made on core-like blanks (negative blanks in : fig 20) but they are irregularly modified with steep retouch. They are lacking in the Acheulian from Torre in Pietra level m. In Middle Paleolithic industries from Torre in Pietra level d (: fig 24) and Grotta dei Moscerini these core-like blanks are also present but do not occur frequently (respectively 3.3% and 2.5% of retouched tools). They are more finely retouched (sidescrapers) than at Castel di Guido. At Torre in Pietra level d invasive removals were produced by direct freehand percussion (conchoidal fracture) whereas at Moscerini both conchoidal and non-conchoidal fracture (on anvil) occur. Core-like pieces were more commonly produced and used as blanks for retouched tools by the flintknappers of SdD and MdG than in the sites listed above.
A third reduction sequence documented by end-products with scars of successive series of unidirectional parallel removals (Figs 10 and 11) indicates a more conventional scheme to produce blanks (N = 14). Series of removals were flaked from unprepared cores (Fig 11A and 11B) hence remains of cortex or natural surfaces appear on most blanks (Fig 10, Fig 11C and 11D). This scheme can induce high variations in core morphology depending on how the series of removals are organized (: fig 10). Here, in most of the cases, a single platform or two opposed platforms were used according to the organization of scars on the blanks. Among the few cores (N = 4) a single one has three series of unidirectional removal scars and older negatives with unclear pattern are also visible (Fig 11A) whereas the others have a simpler pattern or were exploited with a shorter chaîne opératoire (Fig 11B). Twelve of the fourteen blanks have been retouched mostly as sidescrapers.
Retouched end-products with scars of successive series of unidirectional parallel removals. Line drawings modified after .
Cores (A, B) and retouched end-products (C, D) with scars of successive series of unidirectional parallel removals. Caption and symbols used in drawings as in Fig 10. Line drawings C and D modified after .
The repeated use of secondary flaking (called ‘ramification’ in French [46,47]) is one of the features that defines the SdD and MdG industry as Middle Paleolithic. Secondary flaking is not an exclusive feature of the Middle Paleolithic as it was already described in earlier industries [46,48]. Nevertheless, secondary flaking is a form of blank production that occurs more frequently in the Middle Paleolithic echoing the diversification of flaking methods . In the industry from High-Lodge, now considered to be early Middle Paleolithic in age , N. Ashton  concludes that in the majority of cases the flaked flakes should be regarded as tools whereas secondary flakes were very rarely retouched. Secondary flakes of so-called Le Pucheuil-type  from the early Middle Paleolithic site of Le Pucheuil in Normandy (France) were also unretouched but use-wear analysis shows that they were used for multiple purposes . Secondary flaking to produce supplementary blanks for retouched or unretouched tools has been documented in numerous though not all Middle Paleolithic industries of Western Europe. In Quina Mousterian industries scrapers with scaled retouch (Quina-type retouch) were frequently re-flaked to produce small blanks themselves retouched as side or transverse scrapers [46,54,55].
Six artifacts from SdD/MdG show evidence of secondary flaking according to two different modalities (Fig 12). In each case the blanks produced in this manner were retouched. The first modality, called Kombewa (Modality 1 in ), consist in extracting a flake, more or less invasive, from the ventral face of a primary flake (Fig 12A1–12A5). This secondary flake (2 artifacts in our case) as well as the secondary core (i.e. the flake used as core; 1 artifact) were retouched as sidescrapers or denticulates. The second modality involves the core-like pieces produced by the second reduction sequence described above (Fig 12B1–12B5; Fig 13). A percussion applied to one of the retouched edges of a scraper extracts a flake from the flat surface of the core-like piece. Note that the secondary flake and even the already retouched core-like piece were retouched afterward. In a single case a secondary flake was extracted from the dorsal face of a first flake (Nahr-Ibrahim modality, Modality 2 in ). As in the previous case, the primary flake was retouched prior to the extraction of the secondary flake and was retouched again afterward. As could be expected four cases of secondary flaking concern a reddish-brown flint which has the finest texture in the assemblage.
(A1-A5) First modality. Secondary flaking on a flake (Kombewa modality). (B1-B5) second modality. Secondary flaking on a core-like scraper. In both modalities, cores and flakes were retouched as sidescrapers.
Retouched (sidescraper) secondary core made from a sidescraper shaped on a primary core-like piece.
The shaping of small pebbles to directly make retouched tools is the least represented reduction sequence at SdD/MdG. Three artifacts were produced in this manner (Fig 14) but only one has a regularly retouched edge (Fig 14A).
Bifacial tools shaped on small flint pebbles. (A) Bifacial sidecraper. A flat surface is first shaped then the opposite one is retouched. (B-C) Bifacially retouched tools. Line drawing of B modified after .
The distribution of tools types at MdG and SdD (Table 2) is in agreement with Middle Paleolithic patterns. Simple scrapers dominate the tool-kit followed by pieces with irregular retouch (abrupt retouch, short or marginally retouched edges), tools with denticulated edges and tools with convergent retouched edges (convergent and déjeté scrapers, Tayac point). It was considered that the high frequency of retouched tools (56.2%, i.e. 72/128 in Table 1), especially scrapers (Table 2), was a recovery bias . It is now explained by the original chaîne opératoire described here which produces two cortical blanks for scrapers without any byproducts.
Blanks of retouched tools.
Fifty years after the publication of Sedia del Diavolo and Monte delle Gioie by Mariella Taschini  our research has allowed us to describe the technological structure of the two assemblages and to show their originality. Clearly it is the Levallois technology that distinguishes these assemblages from earlier ones, whether the Acheulian of Torre in Pietra level m  or assemblages without bifaces, such as La Polledrara [57–59].
The appearance of the Levallois technology
We agree with White et al.  that focusing discussions on Levallois technology may bring us to underestimate the role and importance of other prepared core technologies, but confident identification of Levallois is still a key point for the study of the emergence of Middle Paleolithic traditions. As pointed by Malinsky-Buller , in Lower and Middle Paleolithic industries some cores can be confused with Levallois cores because they share some but not all characters. Such cases have been rightly described as ‘simple prepared-core technology’  and these cores can be encountered in assemblages predating the appearance of Levallois, as for instance at Cagny-la-Garenne  or in association with the earliest Levallois cores. This may explain persistent discrepancies in publications about the timing of appearance of the Levallois technology.
The chronology of the appearance of Levallois production in Western Europe have been recently reviewed in several papers [64–68]. Pre-MIS 9 occurrences of the Levallois method listed in these papers are usually considered dubious for two reasons: (1) Levallois-like items are very rare and might result from technical convergence and/or (2) their chronology is insecure. SdD/MdG fits with a dozen of convincing West-European sites with Early Levallois spanning from (late?) MIS 9 to early MIS 8.
The archaeological record from Spain is a case in point. Occurrence of the Levallois method has been reported from the middle stratigraphic unit of Ambrona comprising layers excavated by F.C. Howell and L. Freeman between 1960 and 1983 (called Upper Complex in the central and eastern sector of the site) and layers excavated by M. Santonja and A. Pérez-González between 1993 and 2000 in the Middle Stratigraphic Member, unit AS6 in the eastern sector [69,70]. Levallois cores are recorded for the Howell and Freeman's series and Levallois flakes but no cores are reported for the smaller series of the Santonja and Pérez-González's excavation. The industry of the Middle Stratigraphic member is in marked contrast with the Lower Complex where there is no evidence of the use of the Levallois method [70,71]. ESR and U-series combined on horse teeth from AS6 have produced two date: 366 +55/-51 and 314 +48/-45 ka . For the lower levels (AS1 and AS2 of the Lower Stratigraphic Complex) dates are much too young. The problems created by environmental conditions resulting in unacceptable dates for the Acheulian of the Lower Complex are discussed in [73,74] who suggests a date, based on a mean value, of 350 ka for AS6, equivalent to MIS 10. This chronology is also supported by morphostratigraphic position of the site, and with other dates obtained in nearby localities . Such an early age would seem to require further discussion as it predates most if not all confident occurrence of Levallois debitage in Western Europe.
In Italy, secure evidence of Levallois production is recorded at San Bernardino Cave at the end of MIS 7  and earlier at Torre in Pietra layer d now dated to the early part of MIS 7 between 270 and 240 ka . At Cave dall’Olio, the MIS 9 age of Levallois finds buried in a thick fluvial terrace is argued through correlation with the long paleosoil-sedimentary record from the Po Plain  but this chronological framework is not supported by any geochronological dating and must be considered with caution. The site from Guado San Nicola is claimed to have the earliest occurrence of Levallois technology in Italy within an Acheulian industry of late MIS 11 age  thus pushing back of almost an entire glacial cycle the appearance of Levallois technology in Italy [65,76] and more widely in Western Europe . According to  the transition from the Lower to the Middle Paleolithic would have occurred significantly earlier than generally considered and this is challenging our results on SdD and MdG. Clearly the identification of Levallois technology is a key point in the debate.
At a first level of reading, the organization of removals on the cores from Guado San Nicola classified as Levallois (7.58% of the cores) by Peretto et al. (: figs 5 and 6) suggest that they could match with the definition of Levallois debitage proposed by Boëda (1994, 1995). They have two asymmetric and hierarchized surfaces and most of these cores have been exploited centripetally or preferentially. With a closer observation of the published materials, the presence of Levallois debitage in the industry from Guado San Nicola appears doubtful. First, there is no step by step presentation of arguments, necessary to support the hypothesis of such an early occurrence of Levallois. For instance, on the schemes of these hypothetical Levallois cores (: fig 6), negatives of flakes on the debitage surface are not distinguished according to their status and orientation, that is, whether they are secant removals shaping the convexities or are subparallel Levallois products and alternation in the flaking chronology between these two types of removals is not documented. It seems that no or limited preparation/maintenance of convexities occurred on these cores. Second, another element defining the Levallois debitage (Boëda, 1994, 1995) but often omitted by researchers is missing here: the management of the striking platform. This surface must allow the extraction of flakes with secant orientation for the preparation or maintenance of convexities and also Levallois flakes parallel/sub-parallel to the core surface (Fig 15). It implies an alternation on the platform between two types of removals. Large oblique flakes (angle of ~45–65° with the debitage surface) will create suitable platforms to extract short flakes with secant orientation to prepare or maintain the convexities. Small and narrow flakes will increase locally up to 80–85° the angle of the platform with the debitage surface to prepare facetted platforms of forthcoming Levallois flakes. This is a key parameter to control the location of the percussion, the transmission of the energy from the hammerstone and the size of the Levallois flake. On Guado San Nicolas cores this alternation is not visible and the angle between the striking platform and the debitage surface seems to be constant and always close to 70–85° (: Fig 5:2, Fig 6:2–4). Thus two of the important criteria of the Levallois debitage are missing on the Guado San Nicola cores. These cores are in fact by-products of a less elaborate centripetal debitage with two hierarchically organised surfaces. For similar reasons, White and Ashton  have considered that cores from Purfleet, Botany Pit, dating to either late MIS 9 or early MIS 8, and previously described as ‘proto- or reduced Levallois’ don’t match all the criteria defining Levallois production. We believe that the presence of Levallois debitage in the late MIS 11 Acheulian industry of Guado San Nicola is not conclusively demonstrated.
Levallois platform must allow both the extraction of flakes oblique with respect to the plane of intersection to prepare and maintain convexities and Levallois flakes parallel or sub-parallel to the plane of intersection of the two surfaces. This is a key criterion to distinguish Levallois and non-Levallois cores.
There is an overall agreement that in Western Europe the Levallois method appears in association with the first manifestations of the Middle Paleolithic. The SdD and MdG occurrence introduces a new degree of diversity within the context of emergence of Levallois production because the industry is significantly different from any one ever described in Western Europe from MIS 9 to the end of MIS 8. The first manifestations of the Levallois technology not only show a variety of methods (recurrent centripetal, recurrent parallel, preferential) but more curiously occur within quite variable industries. In Southwestern France (at Les Bosses about 300 ka or at Raspide 2) the Levallois method (of the recurrent centripetal variety) is less common than other core types (discoidal, simple unprepared cores) and of tools such as bifaces and other large tools (cleavers, choppers) [78,79]. At Orgnac 3, Levallois technology is dominating from level 3 upward with different methods but it is still associated with a few handaxes and pebble tools [80,81]. In England at Baker’s Hole the Levallois debitage from the base of the sequence, dated to the end of MIS 8 and beginning of MIS 7 , is represented by the preferential method, occasionally by the recurrent method and is not associated to any biface (except for specimens reworked from older deposits) [83,84]. At Kesselt Op-de-Schans (Belgium), in a level at the transition from MIS 9 to MIS 8, the industry from the ODS1 and ODS2 concentrations is only characterised by recurrent centripetal Levallois debitage incorrectly described as ‘sophisticated discoid technology’ by [85,86]. In Southwestern France, at Petit Bost, in level 2 dated to the end of MIS 9 or early MIS 8, different methods of Levallois debitage, including recurrent parallel uni- or bidirectional, are associated with a few handaxes but also with several cases of Quina debitage [67,87]. These examples suggest that in Western Europe early Levallois occurs in variable technological context. Interestingly the sudden and concomitant emergence of the Levallois method in several European sites in association with a variety of technical repertories -of which SdD and MdG are a clear example- strongly suggest a rapid diffusion over wide geographic spaces of this innovation adopted by groups of different technical traditions thus entering a new technological phase which we call Middle Paleolithic. The SdD and MdG industries are a record of this process.
The SdD/MdG artifact assemblages should no longer be considered as “Protopontinian” even if they share some typological features (a moderately high Quina retouch, Levallois always present but rare, an abundance of sidescrapers) with the so-called Pontinian industries  which are dated to the Upper Pleistocene. The structure of the lithic production at SdD/MdG is widely different from the lithic technology of Pontinian assemblages such as Grotta Guattari [30,88,89] whose layers 5, 4 base and 4 are dated to MIS 5, Grotta di Sant’Agostino  dated to MIS 3 and Grotta dei Moscerini [30,91] whose sequence spans 123–74 ka (MIS 5) .
Our analyses indicate that all three “Pontinian” assemblages are characterized by the frequent use of a particular variant of the bipolar technique, which is absent at SdD and MdG. The bipolar technique (or hammer and anvil technique) consists in resting a pebble (or a block or a flake) on anvil and striking it with a hammer. This flaking technique can be used to split a pebble in two blanks to be further worked or as a reduction method for producing quantities of flakes and flake fragments from small nodules [25,42–44]. Flakes produced with this technique are characterized by a non-conchoidal fracture, a flat ventral face, a crushed or concave or no bulb of percussion, no measurable platform and an opposing bulb or shattering at the distal end (Fig 16A).
(A) With the classical bipolar flaking the development of the counterblow results in the formation of an opposing bulb and/or crushing and splintering. (B) With a soft anvil the counterblow doesn’t generate any feature on flakes or cores. (C) Two ‘flat’ flakes from ‘Pontinian’ anvil flaking (Grotta di Sant’Agostino).
However the flakes of several Pontinian assemblages do not show some features expected on bipolar flakes, such as an opposing bulb, or crushing and splintering at the distal end (Fig 16C). Experiments show that the lack of opposing bulb or other traces at the distal end is due to the use of a soft anvil (e.g. wood) or more simply by resting the pebble on the ground and maintaining it in a vertical position [30,45]. This very specific variant of the bipolar technique (Fig 16B) would result in producing cortical and semicortical flakes with an undamaged distal edge, a significant feature in very small products. We call these flakes “flat” flakes using a terminology first used at the Acheulian site of Terra Amata . However at Terra Amata the limestone pebbles yielding flat flakes were large flat ovals that could be easily held in the hand and experiments  show that flat flakes were produced by hand-held vertical percussion on anvil, a mode of production quite different from the knapping of the small flint pebbles of the Latium sites. Flakes without opposing bulb or other counterblow features are also obtained experimentally when a stone anvil is used in bipolar flaking  but always in association with bipolar products with blow and counterblow features.
A good proportion of the typical Pontinian sidescrapers were made on flat flakes and sometime on cores with one or several of these flat removals. The ventral face of flat flakes and the flat scars of cores offered a flat and uniform knapping surface. As yet, there are no known antecedents to the Pontinian variant of the bipolar technique in this region. The first use of this particular technique occurs at Grotta dei Moscerini (Table 3).
Present data shows that the SdD/MdG assemblage, securely dated to 295–290 ka, that is close to the time of transition from MIS 9 to MIS 8, is one of the oldest, if not the oldest record of Levallois production in Italy. Despite the small size of the lithic assemblage from SdD and Mdg, most if not all the characters defining the Middle Paleolithic have been identified. Sidescrapers dominate the tool-kit and at least three main chaîne opératoires, including the fully developed Levallois one, have been used to produce blanks of different size, shape and technical properties (involving length and sharpness of retouched or unretouched cutting edges): thin and regular Levallois flakes, slightly elongated flakes and thick ‘core-like’ half pebbles. The Levallois method is clearly associated with a Middle Paleolithic technological context. Direct shaping of unifacial or bifacial tools on small flint pebbles (i.e. chopping tools) is a minor component of the industry and the bipolar percussion is absent. Thus we cannot agree with Picin et al.  who believes that the Sedia del Diavolo and Monte delle Gioie industry show a continuity of archaic elements.
The industries from SdD/MdG can no longer be considered as Proto-Pontinian because several technological differences distinguish them from later, Würmian, industries of the so-called Pontinian type and also from the Early Middle Paleolithic from Torre in Pietra level d. However a degree of technological continuity can be seen in the selection and use of small flint pebbles and core-like pieces as blanks for retouched small tools.
The SdD and MdG industries show significant differences with broadly contemporaneous industries of the initial Middle Paleolithic with early evidences of Levallois technology such as Orgnac 3, Mesvin IV, Kesselt Op-de-Schans, Petit-Bost, and even with Torre in Pietra level d which is more recent and yet geographically very close. Not only the role of the Levallois debitage in the lithic production of SdD/MdG is minor by comparison with those industries; more importantly, the industries of those two sites are characterized by an original debitage method that is actually mid-way between blank production and shaping of a single tool, and intended to produce specific blanks for thick sidescrapers. This technology has never been described before yet is part and parcel of a regional trend to make tools directly from small volumes of raw material -commonly small flint pebbles- as we described it for the Lower Paleolithic industries of Torre in Pietra level m and Castel di Guido. This habit indicates a degree of technical continuity between Acheulian industries and Middle Paleolithic industries of the region, including Torre in Pietra level d. It is in this context that the Levallois technology was introduced from abroad and successfully integrated in the local technological background on the way to the Middle Paleolithic.
S1 File. Human remains from Sedia del Diavolo and supplementary tables.
S2 File. History of research at Sedia del Diavolo and Monte delle Gioie.
S3 File. Fluvial aggradational cycles in the Aniene River Valley.
Stratigraphy and chronology of Sedia del Diavolo and Monte delle Gioie.
S4 File. Permissions from copyright holders.
We thank the Pigorini Museum and the Italian Institute of Human Paleontology for access to the collections and facilities during analysis. Fabio Parenti, President of the Italian Institute of Human Paleontology and Luciano Bruni very graciously allowed us complete access to the lithic material of Sedia del Diavolo and Monte delle Gioie and its transport from the town of Anagni to the Zoology Museum in Rome and keep it there for the duration of this study. We thank Francesco di Gennaro and Mario Mineo of the Pigorini Museum in Rome for permission to take photos of the materials and allowing us to use the skills of Fabio Naccari for photography. We thank Fabrizio Marra for enlightening discussions about the geomorphology and chronology of Pleistocene continental deposits around Roma. We thank Luca Bondioli for permission to take photos of the human fossils from Sedia del Diavolo. We are particularly grateful to Mario Amore of the Pigorini Museum and the staff of the Zoology Museum in Rome for the good humor and quick access to the Museum facilities (including the indispensable coffee machines). We thank two anonymous reviewers for their helpful and constructive comments. PV wishes to thank the University of Colorado Interlibrary Loan Service for their efficient and rapid deliveries and the University of Colorado Museum of Natural History for covering the publication cost. We thank Stefano Grimaldi the new President of the Italian Institute of Human Paleontology for granting us permission to use in modified form several drawings from the 1967 M. Taschini paper (S4 File).
- 1. Blanc AC. Notizie sui trovamenti e sul giacimento di Saccopastore e sulla sua posizione nel Pleistocene laziale. Palaeontographia Italica. 1948;XLII (Nuova Serie, XII): 1–24.
- 2. Blanc AC. Ricerche sul quaternario laziale. III–Avifauna artica, crioturbazioni e testimonianze di soliflussi nel Pleistocene medio-superiore di Roma e di Torre in Pietra. Il Periodo Glaciale Nomentano nel quadro della serie di glaciazioni riconosciute nel Lazio. Quaternaria. 1955;2: 187–200.
- 3. Taschini M. Il “Protopontiniano” rissiano di Sedia del Diavolo e di Monte delle Gioie (Roma). Quaternaria. 1967;9: 301–319.
Piperno M, Segre A. The transition from Lower to Middle Palaeolithic in Central Italy: an example from Latium. In: Ronen A, editor. The Transition from Lower to Middle Palaeolithic and the origin of modern man. Oxford: B.A.R; 1982. pp. 203–221.
Segre AG, Segre-Naldini E. 96. Sedia del Diavolo, Lazio. 97. Monte delle Gioie, Lazio. I Primi abitanti d’Europa: 1 500 000–100 000 anni Catalogo della mostra, Museo Nazionale Preistorico Etnografico “Luigi Pigorini”, Roma, marzo-luglio 1984. Roma: De Luca Editore; 1984. pp. 200–202.
- 6. Caloi L, Palombo MR, Petronio C. La fauna quaternaria di Sedia del Diavolo (Roma). Quaternaria. 1980; 177–209.
- 7. Piperno M, Biddittu I. Studio tipologico ed interpretazione dell’industria acheuleana e pre-musteriana dei livelli m e d di Torre in Pietra (Roma) in Torre in Pietra (Roma). Quaternaria. 1978;20: 441–536.
- 8. Conato V, Esu D, Malatesta A, Zarlenga F. New data on the Pleistocene of Rome. Quaternaria. 1980; 131–176.
- 9. Marra F, Rosa C. Stratigrafia e assetto geologico dell’area romana. Memorie Descrittive della Carta Geologica d’Italia. 1995;50: 49–118.
- 10. Karner DB, Renne PR. 40Ar/39Ar geochronology of Roman volcanic province tephra in the Tiber River valley: Age calibration of middle Pleistocene sea-level changes. Geol Soc Am Bull. 1998;110: 740–747.
- 11. Karner DB, Marra F. Correlation of fluviodeltaic aggradational sections with glacial climate history: A revision of the Pleistocene stratigraphy of Rome. Geol Soc Am Bull. 1998;110: 748–758. https://doi.org/10.1130/0016-7606(1998)110<0748:COFASW>2.3.CO;2
- 12. Marra F, Florindo F. The subsurface geology of Rome: Sedimentary processes, sea-level changes and astronomical forcing. Earth Sci Rev. 2014;136: 1–20.
- 13. Marra F, Pandolfi L, Petronio C, Di Stefano G, Gaeta M, Salari L. Reassessing the sedimentary deposits and vertebrate assemblages from Ponte Galeria area (Rome, central Italy): An archive for the Middle Pleistocene faunas of Europe. Earth Sci Rev. 2014;139: 104–122.
- 14. Marra F, Rohling EJ, Florindo F, Jicha B, Nomade S, Pereira A, et al. Independent 40Ar/39Ar and 14C age constraints on the last five glacial terminations from the aggradational successions of the Tiber River, Rome (Italy). Earth Planet Sci Lett. 2016;449: 105–117.
- 15. Marra F, Ceruleo P, Jicha B, Pandolfi L, Petronio C, Salari L. A new age within MIS 7 for the Homo neanderthalensis of Saccopastore in the glacio-eustatically forced sedimentary successions of the Aniene River Valley, Rome. Quat Sci Rev. 2015;129: 260–274.
- 16. Marra F, Ceruleo P, Pandolfi L, Petronio C, Rolfo MF, Salari L. The Aggradational Successions of the Aniene River Valley in Rome: Age Constraints to Early Neanderthal Presence in Europe. PLoS One. 2017;12: e0170434. pmid:28125602
- 17. Palombo MR, Milli S, Rosa C. Remarks on the biochronology of the late Middle Pleistocene mammalian faunal complexes of the Campagna Romana (Latium, Italy). Geologica Romana. 2004;37: 135–143.
- 18. Karner DB, Marra F, Renne PR. The history of the Monti Sabatini and Alban Hills volcanoes: groundwork for assessing volcanic-tectonic hazards for Rome. Journal of Volcanology and Geothermal Research. 2001;107: 185–215.
- 19. Marra F, Karner DB, Freda C, Gaeta M, Renne P. Large mafic eruptions at Alban Hills Volcanic District (Central Italy): Chronostratigraphy, petrography and eruptive behavior. Journal of Volcanology and Geothermal Research. 2009;179: 217–232.
- 20. Lisiecki LE, Raymo ME. A Pliocene‐Pleistocene stack of 57 globally distributed benthic δ18O records. Paleoceanography. 2005;20.
- 21. Villa P, Soriano S, Grün R, Marra F, Nomade S, Pereira A, et al. The Acheulian and Early Middle Paleolithic in Latium (Italy): Stability and Innovation. PLoS One. 2016;11: e0160516. pmid:27525705
- 22. Mallegni F. Les restes humains du gisement de Sedia del Diavolo (Rome) au Riss final. L’Anthropologie. 1986;90: 539–553.
- 23. Villa P, Delagnes A, Wadley L. A late Middle Stone Age artifact assemblage from Sibudu (KwaZulu-Natal): comparisons with the European Middle Paleolithic. J Archaeol Sci. 2005;32: 399–422.
- 24. Villa P, Soriano S, Teyssandier N, Wurz S. The Howiesons Poort and MSA III at Klasies River main site, cave 1A. J Archaeol Sci. 2010;37: 630–655.
- 25. Villa P, Soriano S, Tsanova T, Degano I, Higham TF, d’Errico F, et al. Border Cave and the beginning of the Later Stone Age in South Africa. Proc Natl Acad Sci U S A. 2012;109: 13208–13213. pmid:22847432
- 26. Soriano S, Villa P, Wadley L. Blade technology and tool forms in the Middle Stone Age of South Africa: the Howiesons Poort and post-Howiesons Poort at Rose Cottage Cave. J Archaeol Sci. 2007;34: 681–703.
- 27. Soriano S, Villa P, Delagnes A, Degano I, Pollarolo L, Lucejko JJ, et al. The Still Bay and Howiesons Poort at Sibudu and Blombos: Understanding Middle Stone Age Technologies. PLoS One. 2015;10: e0131127. pmid:26161665
- 28. Boëda E, Geneste J-M, Meignen L. Identification des chaînes opératoires lithiques du Paléolithique ancien et moyen. Paléo. 1990;2: 43–80.
Inizan M-L, Reduron-Ballinger M, Roche H, Tixier J. Technology and Terminology of Knapped Stone. Nanterre: Cercle de Recherches et d’Etudes Préhistoriques; 1999.
Kuhn SL. Mousterian Lithic Technology. Princeton: Princeton University Press; 1995.
Harding P, Gibbard PL, Lewin J, Macklin MG, Moss EH. The transport and abrasion of flint handaxes in a gravel-bed river. In: Sieveking G de G, Newcomer M, editors. The Human Uses of Flint and Chert. Cambridge, UK: Cambridge University Press; 1987. pp. 115–126.
- 32. Soriano S, Huysecom E. Lithic industry as an indicator of ceramic diffusion in the Early Neolithic of West Africa: A case study at Ounjougou. Journal of African Archaeology. 2012;10: 85–101.
- 33. Chambers JC. Like a Rolling Stone? The Identification of Fluvial Transportation Damage Signatures on Secondary Context Bifaces. Lithics–The Journal of the Lithic Studies Society. 2003;24: 66.
- 34. Chu W, Thompson C, Hosfield R. Micro-abrasion of flint artifacts by mobile sediments: a taphonomic approach. Archaeol Anthropol Sci. 2015;7: 3–11.
Piperno M, Segre AG, Biddittu I. Il Paleolitico inferiore nel Lazio, nella Basilicata e in Sicilia. Atti della XXIII Riunione Scientifica dell’Istituto Italiano di Preistoria e Protostoria. Firenze, 7–9 mai 1980; 1982.
Palma di Cesnola A. Le Paléolithique inférieur et moyen en Italie. Grenoble: Ed. Jérôme Millon; 1996.
- 37. Boëda E. Le débitage discoïde et le débitage Levallois récurrent centripète. Bulletin de la Société Préhistorique Française. 1993;90: 392–404.
Boëda E. Le concept Levallois: variabilité des méthodes. Paris: CNRS éditions; 1994.
Boëda E. Levallois: A Volumetric Construction, Methods, A Technique. In: Dibble HL, Bar-Yosef O, editors. The Definition and Interpretation of Levallois Technology. Madison: Prehistory Press; 1995. pp. 41–68.
- 40. Brantingham PJ, Kuhn SL. Constraints on Levallois Core Technology: A Mathematical Model. J Archaeol Sci. 2001;28: 747–761.
- 41. Cotterell B, Kamminga J. The Formation of Flakes. Am Antiq. 1987;52: 675–708.
Mourre V, Jarry M, editors. “Entre le marteau et l’enclume”: la percussion directe au percuteur dur et la diversité de ses modalités d’application. Les Eyzies-de-Tayac: SAMRA; 2011.
Soriano S, Robert A, Huysecom E. Percussion bipolaire sur enclume: choix ou contrainte? L’exemple du Paléolithique d’Ounjougou (Pays dogon, Mali). In: Mourre V, Jarry M, editors. « Entre le marteau et l’enclume. » La percussion directe au percuteur dur et la diversité de ses modalités d’application. Les Eyzies: SAMRA; 2011. pp. 123–132.
- 44. Knight J. Technological analysis of the anvil (bipolar) technique. Lithics–The Journal of the Lithic Studies Society. 1991; 57–87.
Faivre J-P, Geneste J-M, Turq A. La fracturation en split, une technique de production dans l’industrie lithique des Tares (Sourzac, Dordogne). In: Mourre V, Jarry M, editors. « Entre le marteau et l’enclume. » La percussion directe au percuteur dur et la diversité de ses modalités d’application. Les Eyzies: SAMRA; 2011. pp. 133–142. Available: http://paleo.revues.org/1944
- 46. Bourguignon L, Faivre J-P, Turq A. Ramification des chaînes opératoires: une spécificité du Moustérien. Paléo. 2004;16: 37–48.
- 47. Turq A, Roebroeks W, Bourguignon L, Faivre J-P. The fragmented character of Middle Palaeolithic stone tool technology. J Hum Evol. 2013;65: 641–655. pmid:24074611
- 48. Parush Y, Assaf E, Slon V, Gopher A, Barkai R. Looking for sharp edges: Modes of flint recycling at Middle Pleistocene Qesem Cave, Israel. Quaternary International. 2015;361: 61–87.
Delagnes A, Meignen L. Diversity of lithic production systems during the Middle Paleolithic in France: Are there any chronological trends. In: Hovers E, Kuhn SL, editors. Transitions before the Transition. New York: Plenum/Kluwer; 2006. pp. 85–107.
- 50. West RG, Gibbard PL, Boreham S, Rolfe C. Geology and geomorphology of the Palaeolithic site at High Lodge, Mildenhall, Suffolk, England. Proceedings of the Yorkshire Geological Society. 2014;60: 99–121.
- 51. Ashton N, Dean P, McNabb J. Flaked flakes: what, when and why? Lithics–The Journal of the Lithic Studies Society. 1991;12: 1–11.
- 52. Delagnes A. Un mode de production inédit au Paléolithique moyen dans l’industrie du niveau 6e du Pucheuil (Seine-Maritime). Paléo. 1993;5: 111–120.
- 53. Lazuén T, Delagnes A. Lithic tool management in the Early Middle Paleolithic: an integrated techno-functional approach applied to Le Pucheuil-type production (Le Pucheuil, northwestern France). J Archaeol Sci. 2014;52: 337–353.
Faivre J-P. Organisation techno-économique des systèmes de production dans le Paléolithique moyen récent du Nord-est Aquitain: Combe-Grenal et les Fieux. Thèse de Doctorat, Université de Bordeaux 1. 2008. Available: http://www.theses.fr/2008BOR13597
- 55. Faivre J-P. Le « Moustérien à denticulés » de la couche 20 de Combe-Grenal: implications techniques, économiques et fonctionnelles au sein du système de production Quina en Périgord. Paléo. 2011;21: 135–162.
- 56. Tixier J, Turq A. Kombewa et alii. Paléo. 1999;11: 135–144.
- 57. Anzidei AP, Bulgarelli GM, Catalano P, Cerilli E, Gallotti R, Lemorini C, et al. Ongoing research at the late Middle Pleistocene site of La Polledrara di Cecanibbio (central Italy), with emphasis on human–elephant relationships. Quat Int. 2012;255: 171–187.
- 58. Santucci E, Marano F, Cerilli E, Fiore I, Lemorini C, Palombo MR, et al. Palaeoloxodon exploitation at the Middle Pleistocene site of La Polledrara di Cecanibbio (Rome, Italy). Quat Int. 2016;406: 169–182.
- 59. Pereira A, Nomade S, Falguères C, Bahain J- J, Tombret O, Garcia T, et al. 40Ar/39Ar and ESR/U-series data for the La Polledrara di Cecanibbio archaeological site (Lazio, Italy). J Archaeol Sci Rep. 2017;15: 20–29.
White M, Ashton N, Scott B. The emergence, diversity and significance of the Mode 3 (prepared core) technologies. In: Ashton N, Lewis SG, Stringer CB, editors. The ancient human occupation of Britain. Amsterdam: Elsevier; 2011. pp. 53–66.
- 61. Malinsky-Buller A. Lost and found: Technological trajectories within Lower/Middle Paleolithic transition in Western Europe, North of the Pyrenees. Quat Int. 2016;409, Part B: 104–148.
- 62. White MJ, Ashton NM. Lower Palaeolithic core technology and the origins of the Levallois method in North-Western Europe. Curr Anthropol. 2003;44: 598–609.
Tuffreau A, Antoine P. The earliest occupation of Europe: Continental Northwestern Europe. In: Roebroeks W, Kolfschoten T van, editors. The earliest occupation of Europe. Leiden: University of Leiden, Publications of the Institute of Prehistory; 1995. pp. 147–163.
- 64. Fontana F, Nenzioni G, Peretto C. The southern Po plain area (Italy) in the mid-late Pleistocene: Human occupation and technical behaviours. Quat Int. 2010;223–224: 465–471.
- 65. Picin A, Peresani M, Falguères C, Gruppioni G, Bahain J-J. San Bernardino Cave (Italy) and the Appearance of Levallois Technology in Europe: Results of a Radiometric and Technological Reassessment. PLoS one. 2013;8: e76182. pmid:24146836
- 66. Adler DS, Wilkinson KN, Blockley S, Mark DF, Pinhasi R, Schmidt-Magee BA, et al. Early Levallois technology and the Lower to Middle Paleolithic transition in the Southern Caucasus. Science. 2014;345: 1609–1613. pmid:25258079
Brenet M, Bourguignon L, Colonge D, Folgado M, Jarry M, Lelouvier L-A, et al. Les techno-complexes au début du Paléolithique moyen en Aquitaine septentrionale: complexité, complémentarité des productions de débitage et de façonnage et implications comportementales. In: Jaubert J, Fourment N, Depaepe P, editors. Transitions, ruptures et continuité en Préhistoire Vol 2: Paléolithique et Mésolithique. Paris: Société Préhistorique Française; 2014. pp. 81–101.
- 68. Hérisson D, Brenet M, Cliquet D, Moncel M- H, Richter J, Scott B, et al. The emergence of the Middle Palaeolithic in north-western Europe and its southern fringes. Quat Int. 2016;411, Part A: 233–283.
Santonja M, Panera J, Rubio-Jara S, Pérez-González A. La industria lítica de Ambrona. Características generales y contexto estratigrafico. In: Santonja M, Pérez-González A, editors. Los yacimientos paleolíticos de Ambrona y Torralba (Soria) Un siglo de investigaciones arqueologicas. Alcalá de Henares (Madrid): Museo Arqueológico Regional; 2005. pp. 306–332.
- 70. Santonja M, Pérez-González A. Mid-Pleistocene Acheulean industrial complex in the Iberian Peninsula. Quaternary International. 2010;223: 154–161.
- 71. Santonja M, Rubio-Jara S, Panera J, Sánchez-Romero L, Tarriño A, Pérez-González A. Ambrona revisited: The Acheulean lithic industry in the Lower Stratigraphic Complex. Quat Int. 2017;
- 72. Falguères C, Bahain J-J, Pérez-González A, Mercier N, Santonja M, Dolo J-M. The Lower Acheulian site of Ambrona, Soria (Spain): ages derived from a combined ESR/U-series model. J Archaeol Sci. 2006;33: 149–157.
- 73. Falguères C, Bahain J-J, Dolo J-M, Mercier N, Valladas H. On the interest and the limits of using combined ESR/U-series model in the case of very late uranium uptake. Quat Geochronol. 2007;2: 403–408.
- 74. Falguères C, Bahain J-J, Duval M, Shao Q, Han F, Lebon M, et al. A 300–600ka ESR/U-series chronology of Acheulian sites in Western Europe. Quaternary International. 2010;223: 293–298.
Santonja M, Pérez-González A, Panera J, Rubio-Jara S, Sesé C, Soto E, et al. Ambrona and Torralba archaeological and palaeontological sites, Soria Province. In: Sala Ramos R, editor. Pleistocene and Holocene hunter-gatherers in Iberia and the Gibraltar strait: the current archaeological record. Burgos: Universidad de Burgos, Fundación Atapuerca; 2014. pp. 517–527.
- 76. Fontana F, Moncel M-H, Nenzioni G, Onorevoli G, Peretto C, Combier J. Widespread diffusion of technical innovations around 300,000 years ago in Europe as a reflection of anthropological and social transformations? New comparative data from the western Mediterranean sites of Orgnac (France) and Cave dall’Olio (Italy). J Anthropol Archaeol. 2013;32: 478–498.
- 77. Peretto C, Arzarello M, Bahain J-J, Boulbes N, Dolo J-M, Douville E, et al. The Middle Pleistocene site of Guado San Nicola (Monteroduni, Central Italy) on the Lower/Middle Palaeolithic transition. Quat Int. 2016;411, Part B: 301–315.
Jarry M, Colonge D, Lelouvier L- A, Mourre V. Les Bosses 1, Lamagdelaine (Lot): un gisement paléolithique moyen antérieur à l’avant-dernier Interglaciaire sur la moyenne terrasse du Lot [Internet]. Paris: Société Préhistorique Française; 2007.
- 79. Colonge D, Jarry M, Delfour G, Fondeville C, Arnoux T, Berthet A-L. De la transition paléolithique inférieur-moyen dans la vallée de la Garonne: l’Acheuléen supérieur de Raspide 2 (Blagnac, Haute-Garonne). Bulletin de la Société préhistorique française. 2010;107: 205–225.
Moncel M-H. Les assemblages lithiques du site pléistocène moyen d’Orgnac 3 (Ardèche, Moyenne vallée du Rhône, France). Liège: Université de Liège; 1999.
- 81. Moncel M-H, Moigne A-M, Combier J. Towards the Middle Palaeolithic in Western Europe: The case of Orgnac 3 (southeastern France). J Hum Evol. 2012;63: 653–666. pmid:23040107
Bridgland DR. Quaternary of the Thames. London: Chapman and Hall; 1994.
Scott B. Becoming Neanderthals: the earlier British middle Palaeolithic. Oxford; Oakville: Oxbow books; 2010.
- 84. Scott B, Ashton N, Penkman KEH, Preece RC, White M. The position and context of Middle Palaeolithic industries from the Ebbsfleet Valley, Kent, UK. J Quat Sci. 2010;25: 931–944.
- 85. Van Baelen A, Meijs EPM, Van Peer P, de Warrimont J-P, De Bie M. An early Middle Palaeolithic site of Kesselt—Op de Schans (Belgian Limburg). Preliminary results. Notae Praehistoricae. 2007;27: 19–26.
- 86. Van Baelen A, Meijs EPM, Van Peer P, de Warrimont J-P, De Bie M. The early Middle Palaeolithic site of Kesselt—Op de Schans (Belgian Limburg). Excavation campaign 2008. Notae Praehistoricae. 2008;28: 5–9.
Bourguignon L, Djema H, Bertran P, Lahaye C, Guibert P. Le gisement Saalien de Petit-Bost (Neuvic, Dordogne) à l’origine du Moustérien d’Aquitaine. In: Jaubert J, Bordes J-G, Ortega I Cordelat I, editors. Les Sociétés Paléolithiques d’un Grand Sud-Ouest: Nouveaux Gisements, Nouvelles Méthodes, Nouveaux Résultats. Paris: Société Préhistorique Française; 2008. pp. 41–55.
- 88. Taschini M. L’industrie lithique de Grotta Guattari au Mont Circé (Latium): définition culturelle, typologique et chronologique du Pontinien. Quaternaria. 1979;21: 179–247.
- 89. Bietti A, Grimaldi S. Small flint pebbles and Mousterian reduction chains: The case of Southern Latium (Italy). Quaternaria Nova. 1996;6: 237–260.
- 90. Tozzi C. La Grotta di S. Agostino (Gaeta). Rivista di Scienze Preistoriche. 1970;25: 3–87.
Vitagliano S. Nota sul Pontiniano della Grotta dei Moscerini, Gaeta (Latina). XXIV Riunione Scientifica dell’Istituto Italiano di Preistoria e Protostoria Nel Lazio, 8–11 Oct 1982. Firenze: Istituto Italiano di Preistoria et Protostoria; 1984. pp. 155–164.
- 92. Schwarcz HP, Bietti A, Buhay WM, Stiner MC, Grun R, Segre A. On the Reexamination of Grotta Guattari: Uranium-Series and Electron-Spin-Resonance Dates. Curr Anthropol. 1991;32: 313–316.
Villa P. Terra Amata and the middle Pleistocene archaeological record of southern France. Berkley, Los Angeles, London: University of California Press; 1983.
Fournier R-A. Les Outils sur galets du site Mindelien de Terra-Amata: Nice, Alpes-Maritimes. Thèse de Doctorat, Université de Provence. 1973.
Bietti A, Cancellieri E, Corinaldesi C, Grimaldi S, Spinapolice EE. La percussion sur enclume en Italie centrale tyrrhénienne. In: Mourre V, Jarry M, editors. « Entre le marteau et l’enclume. » La percussion directe au percuteur dur et la diversité de ses modalités d’application. Les Eyzies: SAMRA; 2011. pp. 143–180.