{"id":2724,"date":"2024-04-05T12:36:23","date_gmt":"2024-04-05T10:36:23","guid":{"rendered":"https:\/\/kernsverlag.com\/the-middle-paleolithic-of-the-cote-chalonnaise-chronology-technology-and-palethnological-elements\/"},"modified":"2024-08-19T20:26:58","modified_gmt":"2024-08-19T18:26:58","slug":"the-middle-paleolithic-of-the-cote-chalonnaise-chronology-technology-and-palethnological-elements","status":"publish","type":"post","link":"https:\/\/kernsverlag.com\/de\/the-middle-paleolithic-of-the-cote-chalonnaise-chronology-technology-and-palethnological-elements\/","title":{"rendered":"The Middle Paleolithic of the C\u00f4te Chalonnaise: Chronology, Technology and Palethnological Elements"},"content":{"rendered":"<div class=\"authors-information\">\n<strong>Klaus Herkert<sup>1,3<\/sup>, Ria Litzenberg<sup>1,2,3<\/sup>, Christian Thomas Hoyer<sup>1,2<\/sup>, Jens Axel Frick<sup>1,2<\/sup>, Harald Floss<sup>1,2,3<\/sup><\/strong><\/p>\n<p><sup>1<\/sup> Institute for Pre- and Protohistory and Medieval Archaeology, Department for Early Prehistory and Quaternary Ecology, University of T\u00fcbingen, Germany<br \/>\n<sup>2<\/sup> Projet collectif de recherche (PCR) \u201cLe Pal\u00e9olithique sup\u00e9rieur ancien en Bourgogne m\u00e9ridionale\u201d associated with UMR 6298 ARTeHIS at the Universit\u00e9 de Bourgogne, Dijon, France<br \/>\n<sup>3<\/sup> DFG CRC 1070 \u201cRessourcenKulturen\u201d B01, University of T\u00fcbingen, Germany<\/p>\n<\/div>\n<h2>Zusammenfassung<\/h2>\n<p>Dieser Beitrag untersucht das technologische und allgemeine Erscheinungsbild der mittelpal\u00e4olithischen Inventare aus mehreren Fundstellen im Gebiet der C\u00f4te Chalonnaise, Burgund, Frankreich. Ausgehend von mehreren charakteristischen Merkmalen innerhalb des stratifizierten Materials der Grotte de la Verpilli\u00e8re II (Germolles), konnten die aktuellen Forschungen kongruente technologische Muster f\u00fcr eine Reihe der umliegenden Fundstellen nachweisen.<\/p>\n<p>Die wichtigsten gemeinsamen Merkmale sind das Vorhandensein von Keilmessern, mit und ohne Schneidenschlag, sowie einheitliche Produktionsstrategien, die auf dem Levallois-Konzept basieren.<\/p>\n<p>Damit liefert die vorliegende Arbeit erste Anhaltspunkte f\u00fcr ein zusammenh\u00e4ngendes Fundstellencluster in der Region. Erste Datierungsergebnisse deuten auf einen chronologischen Kontext im sp\u00e4ten Mittelpal\u00e4olithikum hin.<\/p>\n<p>Die r\u00e4umliche Verteilung der Fundstellen und die Zusammensetzung der jeweiligen Inventare erlaubt es, eine erste Hypothese zur funktionalen Organisation zwischen den Fundstellen aufzustellen. Dar\u00fcber hinaus liefern k\u00fcrzlich durchgef\u00fchrte Feldforschungen und anschlie\u00dfende Analysen Belege f\u00fcr eine fundplatzspezifische Organisation, die den mikroregionalen \u00dcberblick \u00fcber das sp\u00e4te Mittelpal\u00e4olithikum im Zusammenspiel von Technologie, Chronologie und R\u00e4umlichkeit vervollst\u00e4ndigen.<\/p>\n<h2>Introduction<\/h2>\n<p>Southern Burgundy has a long history of Paleolithic research, starting at the very beginning of archaeological research itself in the 1860s with sites such as Grotte de la Verpilli\u00e8re I, Grotte de la M\u00e8re Grand or Solutr\u00e9 (e.g., Combier 1959; Ferry and Arcelin 1868; M\u00e9ray 1869, 1876; Mortillet 1883). Over the decades, the region has also revealed a very dense Paleolithic occupation record, especially for Middle Paleolithic sites (Fig. 1) which constitute 42% of the known Paleolithic sites (Pautrat 2016). This is true for the wider Sa\u00f4ne-et-Loire Department as well as for the C\u00f4te Chalonnaise (Fig. 1).<\/p>\n<figure id=\"attachment_3322\" aria-describedby=\"caption-attachment-3322\" style=\"width: 422px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig1-422x800.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig1-422x800.jpg\" alt=\"Distribution of Middle Paleolithic sites\" width=\"422\" height=\"800\" class=\"size-large wp-image-3322\" srcset=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig1-422x800.jpg 422w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig1-158x300.jpg 158w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig1-300x569.jpg 300w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig1-600x1138.jpg 600w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig1.jpg 675w\" sizes=\"auto, (max-width: 422px) 100vw, 422px\" \/><\/a><figcaption id=\"caption-attachment-3322\" class=\"wp-caption-text\">Fig. 1: Distribution of Middle Paleolithic sites. Above: Sa\u00f4ne-et-Loire department with sites attributed to the Middle Paleolithic. The frame highlights the research area in the C\u00f4te Chalonnaise. (Map and Data: carte arch\u00e9ologique, SRA Bourgogne). Below: C\u00f4te Chalonnaise research area. Yellow stars indicate Middle Paleolithic sites mentioned in the text. From north to south, these are: Grotte de la M\u00e8re Grand &#8211; Rully, Les Griffi\u00e8res &#8211; Fontaines, La Roche &#8211; Saint-Martin-sous-Montaigu, Saint-Sulpice &#8211; Germolles, En Roche &#8211; Germolles, Grottes de la Vepilli\u00e8re I&#038;II &#8211; Germolles, Grotte des Teux Blancs &#8211; Saint-Denis-de-Vaux, La Cl\u00f4sure &#8211; Bissy-sur-Fley, La Rue Cataux &#8211; Chen\u00f4ves and Grotte de la Folati\u00e8re &#8211; Culles-les-Roches. Turquoise stars indicate Middle Paleolithic sites reported to the SRA Bourgogne. For raw material availability in the C\u00f4te Chalonnaise, dashed areas indicate deposits of argiles-\u00e0-silex (i.e., clays-with-flints), diamond symbols show the availability of various chert varieties (blue, turquoise and green), quartz (light blue) and distinct find spots of flint (violet). (Data: carte arch\u00e9ologique, SRA Bourgogne; DEM: IGN France; Raw material data: Siegeris; Map and mapping: Hoyer).<\/figcaption><\/figure>\n<p>The topography of the region, featuring narrow corridors between the Jurassic cliffs (Burgundian cuesta) that allow passage from the Sa\u00f4ne Valley in the east to the elevated hinterland in the west, might be one reason for the dense occupation of the C\u00f4te Chalonnaise (Herkert et al. 2015; Hoyer et al. 2014a). Furthermore, there is abundant lithic raw material available in close proximity to the sites (Fig. 1). The dominant siliceous material is flint from the <span class=\"fachbegriff\">argiles \u00e0 silex<\/span> (FAS; clays-with-flint), which varies greatly in quality, and various varieties of Jurassic chert (<span class=\"fachbegriff\">chaille bathonienne<\/span> and <span class=\"fachbegriff\">chaille bajocienne<\/span>, CB), which are generally more coarse-grained than the flint. Quartz, quartzite and granite are also available in primary positions, as gravels on terraces or in riverbeds (Floss 2005b; Herkert et al. 2015, 2016b; Siegeris 2014, 2020; Siegeris and Floss 2015).<\/p>\n<p>Starting with the recent fieldwork carried out at Grotte de la Verpilli\u00e8re I and II in 2006 (Floss 2007, 2008, 2009a, 2009c; Floss et al. 2013a, 2013b, 2014, 2016, 2017; Frick 2014b, 2017; Frick and Steigerwald 2016a, 2016b; Hoyer et al. 2014b), research has been expanded to include a multitude of other sites in the region; these consist of cave sites, rockshelters and open-air sites (Table 1 and Fig. 1).<\/p>\n<p>All of the sites have yielded lithic artifacts attributable to the Middle Paleolithic, but the assemblages derive either from older excavations or from surface collections. In order to widen the focus, and to enable comparative studies, the various collections have been re-examined (Dutkiewicz 2011; Frick 2010; Herkert 2016, 2017; Herkert et al. 2016a, 2015; Macioszczyk and Donguy 2014; Sikner 2014) and some of this work is still ongoing (see Herkert and Frick 2020). Over the course of more than 150 years of research, which has been primarily based on typological criteria, the various assemblages in question have been interpreted quite differently and thus have been attributed to various classic Middle Paleolithic techno-complexes or facies (cf. Frick 2014a; Herkert and Frick 2020). To cite but a few examples, the material from Grotte de la M\u00e8re Grand in Rully has been identified as <span class=\"fachbegriff\">Micoquien final<\/span> (Combier and Ayroles 1976), La Roche at Saint-Martin-sous-Montaigu as <span class=\"fachbegriff\">Moust\u00e9rien type Quina<\/span> (Combier and Ayroles 1976) or as <span class=\"fachbegriff\">Moust\u00e9rien groupe Quina rhodanien<\/span> (Pouliquen 1983), and Saint Sulpice at Germolles as <span class=\"fachbegriff\">Moust\u00e9rien typique de faci\u00e8s levalloisien<\/span> (Colb\u00e8re 1979). The assemblage from Grotte de la Verpilli\u00e8re I has been ascribed to a <span class=\"fachbegriff\">Moust\u00e9rien de tradition acheul\u00e9nne<\/span> (Combier and Ayroles 1976; Desbrosse et al. 1976) and that from La Closure at Bissy-sur-Fley to a <span class=\"fachbegriff\">Charentien de type Ferrassie<\/span> (Desbrosse and Texier 1973; Parriat 1956).<\/p>\n<p>This diversity in attribution suggests a panoply of different Middle Paleolithic groups. However, as we will see, these different industries have much more in common than the given attributions might suggest. With this contribution, we are beginning to fill in the gaps in comparative analysis in the region, a lacuna that was already criticized 35 years ago: \u201c<q lang=\"fr\">Malheureusement, pour l\u2019instant, le manque de travaux r\u00e9gionaux dans cette partie de la Bourgogne nous prive de r\u00e9f\u00e9rences sur les traits g\u00e9n\u00e9raux et particuliers des faci\u00e8s en pr\u00e9sence, avec leurs \u00e9ventuelles ramifications g\u00e9ographiques<\/q>\u201d (Pouliquen 1983: 206).<\/p>\n<figure id=\"attachment_3325\" aria-describedby=\"caption-attachment-3325\" style=\"width: 800px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table1-800x429.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table1-800x429.jpg\" alt=\"table of relevant Sites in the C\u00f4te Chalonnaise mentioned in the text\" width=\"800\" height=\"429\" class=\"size-large wp-image-3325\" srcset=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table1-800x429.jpg 800w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table1-300x161.jpg 300w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table1-768x412.jpg 768w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table1-1536x824.jpg 1536w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table1-2048x1099.jpg 2048w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table1-600x322.jpg 600w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\" \/><\/a><figcaption id=\"caption-attachment-3325\" class=\"wp-caption-text\">Table 1: Relevant Sites in the C\u00f4te Chalonnaise mentioned in the text. Research history and literature are only outlined and not exhaustive (see also: Herkert 2020 or Herkert et al. 2015).<\/figcaption><\/figure>\n<h2>The Characteristics of Middle Paleolithic Assemblages<\/h2>\n<h3>Raw materials used<\/h3>\n<p>With regard to the economic aspects of raw material supply and use strategy, we note that local flint predominates in all Middle Paleolithic assemblages. However, a significant amount of chert is always present (Fig. 2). For example, as regards artifacts from the recently excavated layer GH 3 of Verpilli\u00e8re II, 74% are made of flint from the <span class=\"fachbegriff\">argiles \u00e0 silex<\/span> while only 2% are of chert. In comparison, 85% of the artifacts from the open-air site of La Roche in Saint-Martin-sous-Montaigu are made of flint and 12% are made of chert. The highest proportion of chert recognized thus far comes from Grotte de la M\u00e8re Grand in Rully, which contains 32% chert artifacts compared to 67% flint artifacts when all pieces are taken into account; indeed, if only the strictly Middle Paleolithic pieces (n=145) are considered, chert use actually increases to 41%. All in all, an average of around 80% of the Middle Paleolithic artifacts are made of locally available flint, and raw material provisioning relies almost exclusively on local or regional sources within a maximum range of 25 km (Fig. 1). Nevertheless, certain specific pieces also suggest long distance imports to the sites. For example, at Verpilli\u00e8re II, at least four pieces can be attributed to raw material sources in the Mont-l\u00e8s-Etrelles region (Floss 2008, 2009a, 2009b) situated about 110 km to the north-east in the direction of south-western Germany and within the traditional range of the <span class=\"fachbegriff\">Keilmessergruppen<\/span> (Frick 2016a).<\/p>\n<figure id=\"attachment_3327\" aria-describedby=\"caption-attachment-3327\" style=\"width: 800px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig2-800x294.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig2-800x294.jpg\" alt=\"Raw material used (percentage values) within the assemblages of Verpilli\u00e8re I, Verpilli\u00e8re II, En Roche, La Roche and La M\u00e8re Grand\" width=\"800\" height=\"294\" class=\"size-large wp-image-3327\" srcset=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig2-800x294.jpg 800w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig2-300x110.jpg 300w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig2-768x282.jpg 768w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig2-600x220.jpg 600w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig2.jpg 1280w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\" \/><\/a><figcaption id=\"caption-attachment-3327\" class=\"wp-caption-text\">Fig. 2: Raw material used (percentage values) within the assemblages of Verpilli\u00e8re I, Verpilli\u00e8re II, En Roche, La Roche and La M\u00e8re Grand. Data for VPI: Dutkiewicz (2011); Data for VPII: Frick (2016a).<\/figcaption><\/figure>\n<h3>Assemblage characteristics<\/h3>\n<p>In the detailed analysis of recently excavated Late Middle Paleolithic stratified assemblages from Verpilli\u00e8re II at Germolles (e.g., Frick and Floss 2015), Frick (2016a: 657\u201358) concludes with a list of technological and general features that characterize the studied material:<\/p>\n<ul>\n<li>Presence of <span class=\"fachbegriff\">Keilmesser<\/span> with and without tranchet blow modification (for this feature, see especially Frick et al. this volume)<\/li>\n<li>Great diversity in the morphology of bifacial objects with a preference for asymmetrical morphologies<\/li>\n<li>Prevalent use of Levallois reduction for a wide range of blank shapes (from oval to rectangular blanks, triangular and deltoid points and blades)<\/li>\n<li>Almost no evidence for other elaborate reduction concepts, such as Quina or Discoidal<\/li>\n<li>In addition to Levallois reduction there is evidence for opportunistic reduction processes to obtain blanks<\/li>\n<li>Use of ventral reduction on blanks for the configuration of Levallois cores and bulb reduction on tools<\/li>\n<li>Occasional presence of blades<\/li>\n<li>Blank tools are made from a wide range of blank morphologies, such as cortical, configuration and target blanks<\/li>\n<li>Tools can be made on blanks and cores<\/li>\n<li>Minor presence of <span class=\"fachbegriff\">Groszaki<\/span><\/li>\n<li>Minor presence of dorsal reduction<\/li>\n<li>Minor presence of Janus flakes<\/li>\n<li>Major presence of evidence for hafting processes of a wide range of tools<\/li>\n<li>\u201cUpper Paleolithic\u201d tool types are more or less non-existent<\/li>\n<\/ul>\n<p>As listed above, the work of Frick revealed several characteristic features including, among others, the presence of <span class=\"fachbegriff\">Keilmesser<\/span> (especially those with a tranchet blow modification) and, in addition, a variety of other bifacial elements such as bifaces of different shape and size or bifacially worked objects (Frick and Floss 2017). With regard to blank production, the predominant use of the Levallois concept is attested, using nodules as well as blanks as core matrices. Very little evidence was observed of other explicit production concepts, such as Discoid or Quina reduction for instance, but there is evidence for a degree of opportunistic production. Bulb reduction was recognizable both on tools, and also in the sense of Kombewa or Levallois-like production. Concerning the general characteristics of the assemblage from Verpilli\u00e8re II, a certain amount of blade production was observed. Furthermore, there are a wide variety of tools made from target blanks but also from cortical or configuration blanks. There is minor evidence for <span class=\"fachbegriff\">Groszaki<\/span> pieces and considerable evidence for hafting and re-working of tools. Classic Upper Paleolithic tools (such as burins and endscrapers) are virtually absent from the assemblage.<\/p>\n<p>Using these characteristics of the Verpilli\u00e8re II assemblage as a basis, several surrounding sites have been re-evaluated, and others continue to be reviewed as part of our ongoing research. Frick et al. (this volume) have already pointed out that one major common feature is the presence of Keilmesser, with and without a tranchet blow modification, in at least five of the assemblages (La Roche in Saint-Martin-sous-Montaigu, La Closure in Bissy-sur-Fley, La Rue Cataux in Chen\u00f4ves and the Grottes de la Verpilli\u00e8re I and II). Other bifacial objects are also present at these sites (see Frick et al. this volume). Apart from these Keilmesser-yielding sites, the Middle Paleolithic assemblages of Grotte de la M\u00e8re Grand in Rully and En Roche in Germolles provide some additional bifacial objects (n=8 each), and at Saint-Sulpice 10 of these objects were found (Herkert 2020). As regards the site of La Roche, the presence of bifacial tools had already attracted attention at the beginning of the 1980s: \u201c<q lang=\"fr\">Mais l\u2019originalit\u00e9 de La Roche tient dans la fr\u00e9quence des objets bifaces<\/q>\u201d [But the originality of La Roche lies in the frequency of bifacial objects] (Pouliquen 1983: 206).<\/p>\n<h3>Levallois production<\/h3>\n<p>While examining blank production in these assemblages, a similar emphasis on Levallois production became evident. The Levallois concept completely dominates the recognizable production strategies. Other concepts like the Discoidal or the Quina concepts are only evidenced in a very limited number of pieces or not at all. In comparison to the identified Discoidal cores, Levallois cores represent between 88 and 100% of the Middle Paleolithic cores (Table 2). Due to uncertain chronological attribution, simple opportunistic flake cores have been excluded from our analysis. Otherwise, exclusively Middle Paleolithic assemblages like Bissy-sur-Fley, for example, or the GH 3 of Grotte de la Verpilli\u00e8re II, contain 37% and 23% Levallois cores, respectively.<\/p>\n<figure id=\"attachment_3329\" aria-describedby=\"caption-attachment-3329\" style=\"width: 800px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table2-800x342.png\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table2-800x342.png\" alt=\"Identified reduction concepts within the Middle Paleolithic assemblages (table)\" width=\"800\" height=\"342\" class=\"size-large wp-image-3329\" srcset=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table2-800x342.png 800w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table2-300x128.png 300w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table2-768x328.png 768w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table2-600x256.png 600w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table2.png 1048w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\" \/><\/a><figcaption id=\"caption-attachment-3329\" class=\"wp-caption-text\">Table 2: Identified reduction concepts within the Middle Paleolithic assemblages. Data: Herkert (2020) except data for VPI taken from Dutkiewicz (2011) and data for VPII from Frick (2016a).<\/figcaption><\/figure>\n<p>While there was a concentration on Levallois production (e.g., Bo\u00ebda 1993; Bo\u00ebda et al. 1990; Richter 1997), no dominant production mode is recognizable. In fact, several modes are present to a greater or lesser degree (Fig. 3). The reduction strategies have so far been analyzed for seven assemblages (e.g., Herkert 2020) which provide between n=11 and n=71 Levallois cores for which the mode could be identified (Table 3). As Figure 4 shows, preferential and centripetal reduction are the most dominant modes with means of 30.6% and 34.9%, respectively (Table 3). Repeated unidirectional or bidirectional reduction follows with 13.6% and 13.4%, respectively, while the occurrence of convergent or orthogonal reduction is very limited (mean of 7.6%). This distribution is similar for all analyzed assemblages. Only Verpilli\u00e8re II displays higher values for the repeated uni- and bidirectional reduction (each at 19%), and therefore less preferential (23.8%) and centripetal (28.6%) reduction. In addition, the site of Saint-Sulpice shows a clear peak for repeated unidirectional reduction (25.8%), while preferential reduction was only observed in 19.7% of the pieces; this marks the minimum encountered in all of the assemblages. The minimum values for orthogonal or convergent reduction occur at La Roche where only 2.4% of the cores follow this mode. Here, centripetal reduction was very common (46.3%).<\/p>\n<figure id=\"attachment_3331\" aria-describedby=\"caption-attachment-3331\" style=\"width: 800px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table3-800x424.png\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table3-800x424.png\" alt=\"Quantitative distribution of the various Levallois reduction modes observed at different sites (table)\" width=\"800\" height=\"424\" class=\"size-large wp-image-3331\" srcset=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table3-800x424.png 800w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table3-300x159.png 300w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table3-768x407.png 768w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table3-600x318.png 600w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table3.png 1048w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\" \/><\/a><figcaption id=\"caption-attachment-3331\" class=\"wp-caption-text\">Table 3: Quantitative distribution of the various Levallois reduction modes observed at different sites. Data: Herkert (2020), except data for VPII taken from Frick (2016a).<\/figcaption><\/figure>\n<p>In addition to nodules, which dominate the range of matrices used, blanks were also selected and transformed into Levallois cores; generally, advantage was taken of the existing general shape and the convexities of the blank (e.g., Fig. 3.4 and 3.9). Although the studied assemblages did not attain the same level of blank use as observed at Verpilli\u00e8re II, where n=9 blanks were identifiable as core matrices out of a total of n=24 Levallois cores, using blanks as core matrices is nonetheless an observable strategy present in the other collections. For Saint-Sulpice, there are n=5 Levallois cores which could be identified as blanks. At La Roche, n=3 cores on blanks could be detected within the studied material, and at En Roche at least n=1 of the n=11 cores were configured on a blank.<\/p>\n<figure id=\"attachment_3333\" aria-describedby=\"caption-attachment-3333\" style=\"width: 800px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig3-800x766.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig3-800x766.jpg\" alt=\"Levallois cores from La Roche and Saint-Sulpice showing the variability of reduction modes\" width=\"800\" height=\"766\" class=\"size-large wp-image-3333\" srcset=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig3-800x766.jpg 800w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig3-300x287.jpg 300w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig3-768x735.jpg 768w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig3-600x574.jpg 600w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig3.jpg 1280w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\" \/><\/a><figcaption id=\"caption-attachment-3333\" class=\"wp-caption-text\">Fig. 3: Levallois cores from La Roche (1-6 &#038; 9) and Saint-Sulpice (7 &#038; 8) showing the variability of reduction modes. If present, grey shades indicate the succession of reduction from light to dark. 1-3) Preferential reduction (FAS); 4-6) Centripetal reduction (4: on blank; 4 &#038; 5: FAS; 6: rose chert); 7) Bidirectional reduction (FAS); 8) Repeated unidirectional reduction (FAS); 9) Orthogonal reduction (on blank) (photos: Herkert and Huber; image: Herkert).<\/figcaption><\/figure>\n<h3>Levallois products<\/h3>\n<p>As for products linked to Levallois production, we observe quite a similar situation within the assemblages. As Frick pointed out for the Levallois products from Verpilli\u00e8re II, elongated forms (Levallois blades) are usually present. A similar observation has been made for the assemblage from Saint-Sulpice in Germolles, where Colb\u00e8re (1979: 33) already noted that one of the characteristics of the industry is its laminar component.<\/p>\n<figure id=\"attachment_3335\" aria-describedby=\"caption-attachment-3335\" style=\"width: 800px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig4-800x621.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig4-800x621.jpg\" alt=\"Net graph showing the distribution of the various Levallois reduction modes observed at different sites\" width=\"800\" height=\"621\" class=\"size-large wp-image-3335\" srcset=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig4-800x621.jpg 800w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig4-300x233.jpg 300w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig4-768x596.jpg 768w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig4-600x466.jpg 600w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig4.jpg 1280w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\" \/><\/a><figcaption id=\"caption-attachment-3335\" class=\"wp-caption-text\">Fig. 4: Net graph showing the distribution of the various Levallois reduction modes observed at different sites. Values are percentage values based on the total amount of identifiable Levallois cores per site. Data: Herkert (2020), except data for VPII taken from Frick (2016a).<\/figcaption><\/figure>\n<p>With the exception of Culles-les-Roches, all other assemblages contain a certain amount of Levallois blades (Fig. 5) and Levallois points. Data are available for eight sites (Table 4). As illustrated in Figure 6, Levallois flakes always dominate the spectrum with a mean of nearly 70%. Levallois blades on average represent about 17% of artifacts that fall within the spectrum of Levallois blanks and reach a maximum at Bissy-sur-Fley (35.2%). For the assemblage from Saint-Sulpice, 27.5% of its Levallois products are comprised of blades. In addition to Culles-les-Roches, where no blades have been identified so far, a minimum is provided at En Roche (Germolles), where only 7.1% of the Levallois products could be identified as blades. Triangular forms, in the sense of Levallois points (and pseudo-Levallois points), reach a mean of almost 14%. Perceptible peaks can be observed for Chenoves and Culles-les-Roches, where the proportion of points reaches 26.5% and 22.9%, respectively.<\/p>\n<figure id=\"attachment_3337\" aria-describedby=\"caption-attachment-3337\" style=\"width: 800px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table4-800x245.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table4-800x245.jpg\" alt=\"Absolute and percentage quantitative distribution of Levallois cores and Levallois blanks (table)\" width=\"800\" height=\"245\" class=\"size-large wp-image-3337\" srcset=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table4-800x245.jpg 800w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table4-300x92.jpg 300w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table4-768x236.jpg 768w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table4-1536x471.jpg 1536w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table4-600x184.jpg 600w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table4.jpg 2028w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\" \/><\/a><figcaption id=\"caption-attachment-3337\" class=\"wp-caption-text\">Table 4: Absolute and percentage quantitative distribution of Levallois cores and Levallois blanks, subdivided into flakes, blades and points, within the different Middle Paleolithic assemblages. Data: Herkert (2020), except data for VPII taken from Frick (2016a).<\/figcaption><\/figure>\n<p>For the preparation of the detachment of Levallois products, flat and facetted butts are clearly preferred (Table 5 and Fig. 7). At La Roche, more than 86% of the identified butts fall into these two categories. The same is true for En Roche, where flat and facetted butts together reach 83%, with a slightly different emphasis than that observed at La Roche. At Verpilli\u00e8re II, there is also a distinct preference for flat and facetted platforms, while the majority of the blanks show facetted butts. This phenomenon has also been observed for the entire lithic blank production from GH 3 at Verpilli\u00e8re II (Frick 2016a: 609\u201310). A similar picture emerges where recent data are available for the Levallois core platforms. The n=11 cores from En Roche show either a flat striking platform (n=5) or a facetted one (n=6). La Roche, in contrast, provides almost exclusively facetted core platforms (n=38 to n=3 flat platforms), which does not in fact correlate with the image of the corresponding blanks but at the same time does not entirely contradict it. Furthermore, there seems to be no further correlation or preference for one or other of these two platform styles in terms of, for example, ongoing reduction, in regards to either core or to blank sizes.<\/p>\n<figure id=\"attachment_3339\" aria-describedby=\"caption-attachment-3339\" style=\"width: 800px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig5-800x316.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig5-800x316.jpg\" alt=\"Examples of Levallois blades from the sites of La M\u00e8re Grand, La Roche and En Roche\" width=\"800\" height=\"316\" class=\"size-large wp-image-3339\" srcset=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig5-800x316.jpg 800w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig5-300x119.jpg 300w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig5-768x304.jpg 768w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig5-600x237.jpg 600w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig5.jpg 1280w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\" \/><\/a><figcaption id=\"caption-attachment-3339\" class=\"wp-caption-text\">Fig. 5: Examples of Levallois blades from the sites of La M\u00e8re Grand (1-3), La Roche (4-7) and En Roche (8). All blades are made of flint, except no. 3, which is made of chert (photos: Frick, Herkert and Huber; illustration: Herkert).<\/figcaption><\/figure>\n<figure id=\"attachment_3341\" aria-describedby=\"caption-attachment-3341\" style=\"width: 800px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig6-800x407.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig6-800x407.jpg\" alt=\"Bar graph of the percentage distribution of Levallois blank types within the different assemblages\" width=\"800\" height=\"407\" class=\"size-large wp-image-3341\" srcset=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig6-800x407.jpg 800w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig6-300x153.jpg 300w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig6-768x391.jpg 768w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig6-600x305.jpg 600w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig6.jpg 1280w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\" \/><\/a><figcaption id=\"caption-attachment-3341\" class=\"wp-caption-text\">Fig. 6: Bar graph of the percentage distribution of Levallois blank types within the different assemblages. Blue: Levallois flakes; Green: Levallois blades; Yellow: Levallois points.<\/figcaption><\/figure>\n<figure id=\"attachment_3343\" aria-describedby=\"caption-attachment-3343\" style=\"width: 794px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table5.png\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table5.png\" alt=\"Quantitative distribution of platform configuration on Levallois blanks from En Roche, La Roche and Verpilli\u00e8re II (table)\" width=\"794\" height=\"358\" class=\"size-full wp-image-3343\" srcset=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table5.png 794w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table5-300x135.png 300w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table5-768x346.png 768w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table5-600x271.png 600w\" sizes=\"auto, (max-width: 794px) 100vw, 794px\" \/><\/a><figcaption id=\"caption-attachment-3343\" class=\"wp-caption-text\">Table 5: Quantitative distribution of platform configuration on Levallois blanks from En Roche, La Roche and Verpilli\u00e8re II. Data: Herkert (2020), except data for VPII taken from Frick (2016a).<\/figcaption><\/figure>\n<h3>General appearance<\/h3>\n<p>Within the more general appearance of the assemblages, further common features can be observed. At most of the sites, tool production is not restricted to target blanks, as is the case at Verpilli\u00e8re II. In fact, tools are made from a huge variety of blanks, including, next to target blanks, configuration blanks and initialization blanks (i.e., cortical blanks). Where sufficient data are available, this pattern could be observed for all of the assemblages studied. La Closure, where studies are still in progress, is an exception. This type of opportunistic matrix selection for tool production could be related to economic strategies governing raw material use patterns.<\/p>\n<figure id=\"attachment_3345\" aria-describedby=\"caption-attachment-3345\" style=\"width: 800px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig7-800x624.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig7-800x624.jpg\" alt=\"Bar graph showing the percentage distribution of butt configuration on Levallois blanks from En Roche, La Roche and Verpilli\u00e8re II\" width=\"800\" height=\"624\" class=\"size-large wp-image-3345\" srcset=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig7-800x624.jpg 800w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig7-300x234.jpg 300w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig7-768x599.jpg 768w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig7-600x468.jpg 600w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig7.jpg 1280w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\" \/><\/a><figcaption id=\"caption-attachment-3345\" class=\"wp-caption-text\">Fig. 7: Bar graph showing the percentage distribution of butt configuration on Levallois blanks from En Roche, La Roche and Verpilli\u00e8re II. A clear emphasis is to be noted for flat and facetted butts.<\/figcaption><\/figure>\n<p>Another commonly observable trait is the intentional removal of bulbs on many tools (Table 6). Even though not extensively applied, this feature concerns 5.5% of the modified blanks at La Roche and 6.8% of those at En Roche, respectively. The studied material from Verpilli\u00e8re II reaches a value of 4.5% for bulb reduction within the spectrum of modified blanks. Bulb reduction on tools has also been observed within the assemblages of some other surrounding sites, although quantitative data are lacking (e.g., Verpilli\u00e8re I, La M\u00e8re Grand, Saint-Sulpice and La Folati\u00e8re).<\/p>\n<figure id=\"attachment_3347\" aria-describedby=\"caption-attachment-3347\" style=\"width: 756px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table6.png\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table6.png\" alt=\"Quantitative distribution of modified blanks with bulb removal (ventral flattening) from La Roche, En Roche and Verpilli\u00e8re II (table)\" width=\"756\" height=\"280\" class=\"size-full wp-image-3347\" srcset=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table6.png 756w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table6-300x111.png 300w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table6-600x222.png 600w\" sizes=\"auto, (max-width: 756px) 100vw, 756px\" \/><\/a><figcaption id=\"caption-attachment-3347\" class=\"wp-caption-text\">Table 6: Quantitative distribution of modified blanks with bulb removal (ventral flattening) from La Roche, En Roche and Verpilli\u00e8re II. Data: Herkert (2020), except data for VPII taken from Frick (2016a).<\/figcaption><\/figure>\n<p>The removal of bulbs might be related to, among others, the manipulation or hafting of the tools concerned (Banks 2004; Rots 2010, 2016). Furthermore, there are other \u201cmorphological adjustments\u201d evident on the tools that provide \u201cindirect arguments\u201d (Rots 2016: 168) for the practice of hafting. In addition to bulb removal (or ventral face flattening), we observe opposite lateral notches as well as uni- and bifacial retouch on one or both of the edges (Fig. 8). These observations also provide evidence for specific activities carried out on site, such as re-working and rehafting of tools. While edge-modified basal fragments, for example, represent the hafting remains of supposed composite tools, there are also, as Frick (2016a) demonstrated, fragments that only display a modified active edge (tool tips). Such tool tips complement the hafting evidence.<\/p>\n<figure id=\"attachment_3349\" aria-describedby=\"caption-attachment-3349\" style=\"width: 729px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig8-729x800.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig8-729x800.jpg\" alt=\"Artifacts from La Roche with hafting evidence\" width=\"729\" height=\"800\" class=\"size-large wp-image-3349\" srcset=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig8-729x800.jpg 729w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig8-273x300.jpg 273w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig8-768x843.jpg 768w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig8-300x329.jpg 300w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig8-600x659.jpg 600w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig8.jpg 1166w\" sizes=\"auto, (max-width: 729px) 100vw, 729px\" \/><\/a><figcaption id=\"caption-attachment-3349\" class=\"wp-caption-text\">Fig. 8: Artifacts from La Roche with hafting evidence. Dotted lines: Active edge; Dashed lines: modification for hafting purposes (retouch and\/or notches); grey lines: techno-functional separation between transmitting part (hafted section) and transformative part (active section) (e.g., Bo\u00ebda 2013; Frick and Herkert 2014).<br \/>1-3) Scrapers (flint from argiles \u00e0 silex) showing different reduction stages (1: Bonnotte collection, 2-3 Donguy collection); 4) Heavily reduced scraper (rose chert, Donguy collection); 5) Scraper (flint from argiles \u00e0 silex) with two proposals of hafting (Denon collection), a: hafting with rounded active edge; b: hafting as regular scraper; 6) Point or convergent scraper (grey chert, Donguy collection); 7) Point or convergent scraper (flint from argiles \u00e0 silex, Denon collection); 8) Rounded end scraper (rose chert, Donguy collection) on Levallois blade; 9) Rounded end scraper (rose chert, Donguy collection); 10) End scraper (brown flint, Donguy collection); 11) End scraper (pale chert, Denon collection) on Levallois blade; 12-15) Basal fragments of Levallois blades (flint from argiles \u00e0 silex) with lateral retouch or notches (Bonnotte collection); 16) Basal blank fragment (flint from argiles \u00e0 silex) with lateral retouch (Donguy collection) (photos: Herkert and Huber; image: Herkert).<\/figcaption><\/figure>\n<h3>Technological cluster<\/h3>\n<p>Concerning the other general features set out by Frick (2016a), analysis is still in progress (see also Herkert and Frick 2020); in some cases the lack of stratigraphical contexts for the pieces prevents further clarification. Nevertheless, the initial overview of the assemblages appears quite homogeneous (Table 7), which leads us to the hypothesis of a technological cluster on these sites. The major common feature on which this assumption is based is the presence of various bifacial objects including Keilmesser with and without tranchet blow (see also Frick et al. this volume) as well as a homogeneous pattern of lithic production evident in the prevalent use of the Levallois concept, on the one hand, and the almost complete absence of other specific reduction concepts, on the other hand. Furthermore, these technological traits are accompanied by a general homogeneous \u2018habitus\u2019 in the assemblages, composed of laminar blanks, opportunistic tool manufacturing on a multitude of blanks (including target blanks and other debitage blanks), bulb reduction on tools and further indications for tool hafting.<\/p>\n<figure id=\"attachment_3351\" aria-describedby=\"caption-attachment-3351\" style=\"width: 800px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table7-800x366.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table7-800x366.jpg\" alt=\"Cross table with the technological and general assemblage characteristics after Frick (2016a) (lines) and the various Middle Paleolithic assemblages (rows)\" width=\"800\" height=\"366\" class=\"size-large wp-image-3351\" srcset=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table7-800x366.jpg 800w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table7-300x137.jpg 300w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table7-768x352.jpg 768w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table7-1536x703.jpg 1536w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table7-2048x938.jpg 2048w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_table7-600x275.jpg 600w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\" \/><\/a><figcaption id=\"caption-attachment-3351\" class=\"wp-caption-text\">Table 7: Cross table with the technological and general assemblage characteristics after Frick (2016a) (lines) and the various Middle Paleolithic assemblages (rows). Given, that most of the assemblages derive from surface collection or older excavations, it was not always possible to determine whether a criterion is fulfilled or not and analysis is in progress, but in most cases, a similar pattern is noticeable. Dark green: presence confirmed; Light green: present in small quantities; Dark red: absence confirmed; Light red: absence indicated after first overview; Yellow: (chronological) attribution unclear; Grey: no reliable data yet.<\/figcaption><\/figure>\n<p>Thus far, radiometric dates obtained by IRSL, ESR and AMS-<sup>14<\/sup>C have been used to establish a chronological framework for Verpilli\u00e8re I (GH 15) and Verpilli\u00e8re II (GH 3 and 4) (Heckel et al. 2016; Richard et al. 2016; Z\u00f6ller and Schmidt 2016). These dates place the Middle Paleolithic assemblages of these two neighboring sites within the probability range between 62 and 42 ka BP (Fig. 9). On the basis of the technological traits, we presume that the other assemblages fall within the same chronological bracket, but further work is required and is currently in progress. Nevertheless, especially within the context of an affiliation of these industries to the Keilmessergruppen (Frick 2016a; Frick and Floss 2017; Frick et al. intra), it seems likely that the other assemblages also belong to the Late Middle Paleolithic (Frick et al. 2017).<\/p>\n<figure id=\"attachment_3353\" aria-describedby=\"caption-attachment-3353\" style=\"width: 411px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig9-411x800.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig9-411x800.jpg\" alt=\"Results of initial radiometric dating of the Middle Paleolithic at Verpilli\u00e8re I and II using IRSL, ESR and AMS-14C\" width=\"411\" height=\"800\" class=\"size-large wp-image-3353\" srcset=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig9-411x800.jpg 411w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig9-154x300.jpg 154w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig9-300x584.jpg 300w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig9-600x1169.jpg 600w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig9.jpg 657w\" sizes=\"auto, (max-width: 411px) 100vw, 411px\" \/><\/a><figcaption id=\"caption-attachment-3353\" class=\"wp-caption-text\">Fig. 9: Results of initial radiometric dating of the Middle Paleolithic at Verpilli\u00e8re I and II using IRSL, ESR and AMS-14C. For Verpilli\u00e8re I, the dates of GH 15 can be seen as termini ante quem for the underlying intact GH 16. Data: Heckel et al. (2016), Richard et al. (2016) and Z\u00f6ller and Schmidt (2016); illustration: modified according to Frick.<\/figcaption><\/figure>\n<h2>Spatial Organization<\/h2>\n<p>In the context of the observed technological correlation between the assemblages and given that \u201c[s]ite patterning in both within-place and between-place contexts is a property of the archaeological record\u201d (Binford 1982: 6), recent research in the C\u00f4te Chalonnaise region provides further evidence of potential regional inter-site organization of late Middle Paleolithic land-use patterns as well as of high resolution intra-site spatial distribution patterns.<\/p>\n<h3>Inter-site functionality: a hypothesis<\/h3>\n<p>Given that the research area constitutes a dense micro-regional concentration of caves, rockshelters and open-air sites with different raw materials available in close proximity (Fig. 1), the assemblages differ in terms of qualitative and quantitative composition (e.g., tool frequencies). Due to these differences, and with regard to the geographical distribution, the topological position, and the extent of the sites, we propose a hypothetical regional functional model (Fig. 10).<\/p>\n<p>Both Verpilli\u00e8re sites have been interpreted as base camps (Fig. 10a) with extensive assemblages, which have produced evidence for in-situ lithic production as well as recycling and re-working of tools and abundant food waste (Frick 2016a, 2016b; Frick and Floss 2015; Herkert et al. 2015; Litzenberg 2015).<\/p>\n<p>At Saint-Sulpice in Germolles and Les Griffi\u00e8res in Fontaines, two probable workshops (Fig. 10b) with extensive lithic production are situated on flint outcrops (Colb\u00e8re 1979; Pascal 2013; Sikner 2014).<\/p>\n<p>La Roche at Saint-Martin-sous-Montaigu is a very large open-air site (Herkert 2020; Herkert et al. 2015; Pouliquen 1982, 1983). Lithic production is in evidence here, but with a focus on scraper production (constituting nearly 40% of the known Middle Paleolithic material), which might indicate a specialized processing site (Fig. 10c).<\/p>\n<p>Finally, there are smaller satellite sites in the surrounding area (Fig. 10d) that have yielded smaller assemblages. Particularly noteworthy are the small cave sites of La M\u00e8re Grand in Rully and Les Teux Blancs in Saint-Denis-de-Vaux whose elevated locations provide a very good overview over the whole region. In contrast, En Roche is situated on the plain.<\/p>\n<figure id=\"attachment_3355\" aria-describedby=\"caption-attachment-3355\" style=\"width: 800px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig10-800x707.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig10-800x707.jpg\" alt=\"Distribution of Middle Paleolithic sites around the Grottes de la Verpilli\u00e8re I &amp; II with indications of their suggested function within the micro-regional site cluster\" width=\"800\" height=\"707\" class=\"size-large wp-image-3355\" srcset=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig10-800x707.jpg 800w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig10-300x265.jpg 300w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig10-768x679.jpg 768w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig10-600x530.jpg 600w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig10.jpg 1280w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\" \/><\/a><figcaption id=\"caption-attachment-3355\" class=\"wp-caption-text\">Fig. 10: Distribution of Middle Paleolithic sites around the Grottes de la Verpilli\u00e8re I &#038; II with indications of their suggested function within the micro-regional site cluster. a) Base camps: Grottes de la Verpilli\u00e8re I &#038; II (circle with dot); b) Workshops: Les Griffi\u00e8res and Saint-Sulpice (squares); c) Specialized processing site: La Roche (pentagon); d) Smaller satellite camps in elevated positions: Grotte de la M\u00e8re Grand and Grotte des Teux Blancs (crosses) and smaller satellite camps on the plain: En Roche on the plain (cross). (DEM: IGN France; map and mapping: Hoyer).<\/figcaption><\/figure>\n<h3>Intra-site organization<\/h3>\n<h4>GH 16 at Verpilli\u00e8re I<\/h4>\n<p>During the excavation of Verpilli\u00e8re I, preserved parts of an intact Middle Paleolithic layer (GH 16) were detected between 2010 and 2015 in the inner part of the cave (Floss 2011, 2012; Floss et al. 2013b, 2014, 2016). The area makes up 15 m\u00b2 of the excavation grid (Fig. 11). The character of the lithic industry, although quantitatively limited, is not without analogies to those from Verpilli\u00e8re II or other surrounding sites. In addition to opportunistic flake cores, Levallois production has been observed. The spectrum also comprises elongated forms as well as a quantity of bifacial objects (Litzenberg 2015). Radiometric dating (AMS-14C and ESR\/U-Th) of the overlying GH 15 provides indications for a terminus ante quem at around 48 ka BP (Heckel et al. 2016; Richard et al. 2016). Faunal remains that include deer (<span class=\"fachbegriff\">Cervus elaphus<\/span> and <span class=\"fachbegriff\">Megalocerus giganteus<\/span>), reindeer (<span class=\"fachbegriff\">Rangifer tarandus<\/span>), horse (<span class=\"fachbegriff\">Equus ferus<\/span>), bison (<span class=\"fachbegriff\">Bison priscus<\/span>), fox (<span class=\"fachbegriff\">Vulpes vulpes<\/span>), and lynx (<span class=\"fachbegriff\">Lynx spelaea<\/span>) support a chronological attribution to between MIS4 and early MIS3, within a temperate phase of the early or middle Weichselian glaciation.<\/p>\n<p>Despite the limited extent of the preserved area, the analysis of the find distribution provides initial evidence for distinct concentrations and thus for spatial organization within the various occupation events. As Litzenberg (2015) points out, the main concentrations of lithic artifacts and faunal remains overlap each other. Nevertheless, indications for anthropogenic zonal structuring are present, especially in the case of the distribution of cores and raw pieces (Fig. 11). Cores and raw pieces are mainly concentrated in an area covering only half a square meter (square number 191\/097), with cores generally found in the southern part of the area and raw pieces in the northern part. The spatial distribution of blanks does not indicate primary knapping events in this part of the site, although quartzitic hammerstones have also been found. Furthermore, given that the rear of the former rockshelter is not the most suitable place for knapping activities, the deposition of the pieces can instead be interpreted as the storage of raw materials for use in future re-visits to the site within a pattern of repeated seasonal migration (e.g., Binford 1980, 1982) or as \u201cinsurance gear\u201d (Binford 1979). This indicates economic organization on the part of late Middle Paleolithic Neanderthals in the region.<\/p>\n<figure id=\"attachment_3357\" aria-describedby=\"caption-attachment-3357\" style=\"width: 800px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig11-800x501.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig11-800x501.jpg\" alt=\"GH 16 at Verpilli\u00e8re I\" width=\"800\" height=\"501\" class=\"size-large wp-image-3357\" srcset=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig11-800x501.jpg 800w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig11-300x188.jpg 300w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig11-768x481.jpg 768w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig11-600x376.jpg 600w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig11.jpg 1280w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\" \/><\/a><figcaption id=\"caption-attachment-3357\" class=\"wp-caption-text\">Fig. 11: GH 16 at Verpilli\u00e8re I. Left: Plan of Verpilli\u00e8re I with location of the sediment unit GH 16 in the north-western part of the cave (red shaded) (Mapping: Hoyer). Right: Distribution of single find measurements of lithic objects within GH 16, showing the concentration of cores and raw pieces in square number 191\/097. Modified according to Litzenberg (2015).<\/figcaption><\/figure>\n<h4>GH 3 at Verpilli\u00e8re II<\/h4>\n<p>Another reliable source for intra-site organization, spatial patterning and the identification of occupation features dating to the late Middle Paleolithic in southern Burgundy concerns the stratified deposits of GH 3 at Verpilli\u00e8re II (Frick 2016a, 2016b).<\/p>\n<p>The identification of several distinct charcoal lenses in the otherwise very homogeneous deposits of GH 3 (Fig. 12a) not only indicates homogeneous, low-energy, proximate aeolian sedimentation, resulting in the transportation of lighter burnt material from presumed hearths located at the entrance of the former rockshelter into the interior (Frick 2016b: 707), but also suggests that several repeated occupation events, which would have included the use of fire, occurred over the course of this period of constant sedimentation. Furthermore, the charcoal concentrations are clearly separate from the recorded limestone fragments (Fig. 12b).<\/p>\n<p>A second detected pattern at Verpilli\u00e8re II concerns the spatial distribution of lithic artifacts and faunal remains. As already presented elsewhere (Frick 2016a, 2016b), these two categories display a clear spatial separation from each other (Fig. 12c). While lithic artifacts are primarily scattered towards the eastern part of the excavation area and thus also towards the former opening of the ancient rockshelter, the faunal remains, in contrast, are mostly concentrated in the inner part of the cavity in the west and south of the excavated area.<\/p>\n<figure id=\"attachment_3359\" aria-describedby=\"caption-attachment-3359\" style=\"width: 566px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig12-566x800.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig12-566x800.jpg\" alt=\"Find distribution plots from Verpilli\u00e8re II (GH 3) with top view (north up) and profile views on the left and 3D view on the right\" width=\"566\" height=\"800\" class=\"size-large wp-image-3359\" srcset=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig12-566x800.jpg 566w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig12-212x300.jpg 212w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig12-768x1086.jpg 768w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig12-300x424.jpg 300w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig12-600x849.jpg 600w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig12.jpg 905w\" sizes=\"auto, (max-width: 566px) 100vw, 566px\" \/><\/a><figcaption id=\"caption-attachment-3359\" class=\"wp-caption-text\">Fig. 12: Find distribution plots from Verpilli\u00e8re II (GH 3) with top view (north up) and profile views on the left and 3D view on the right. a) Elements with evidence for heat (fire), showing distinct lenses of charcoal particles. b) Distinct separation of charcoal particles and limestone fragments. c) Distribution of lithic artifacts and faunal remains in GH 3, showing a clear zonation of the latter in the west and in the south of the interior part of the cave. Illustrations: Frick (2016a: 636).<\/figcaption><\/figure>\n<p>Comparable observations have been made on other sites, such as Abric Roman\u00ed or Kebara Cave (Carbonell i Roura 2012; Speth et al. 2012). \u201cIf we assume that the main occupation occurred under the rock shelter, the far interior of the shelter and the area of the cave tunnel make logical areas for toss-zones and rubbish dumping, further from the active occupation area and less likely to attract carnivores\u201d (Frick 2016b: 708).<\/p>\n<p>These observations are, to a certain extent, in contrast to those made for Verpilli\u00e8re I (GH 16). On the one hand, no separation between fauna and lithics has been observed here; on the other hand, there are no deposit-like features in Verpilli\u00e8re II.<\/p>\n<h2>Discussion<\/h2>\n<p>The Middle Paleolithic archaeological record of the C\u00f4te Chalonnaise region allows multifocal analyses on a regional scale. The recently conducted excavations at Verpilli\u00e8re I and II provide high resolution data for microscale intra-site analysis that may serve as a reliable reference and starting point for further investigation. As demonstrated, the stratified assemblages contribute significantly to our understanding of the technological particularities within an observable variability. Initial radiometric dating provides further evidence for a chronological position in the late Middle Paleolithic, around the end of MIS 4 and the beginning of MIS 3.<\/p>\n<p>The comparative studies of neighboring sites in the area, which we have recently commenced, reveal a multitude of common features despite the lack of stratigraphical context. Such mesoscopic regional research is crucial for understanding the structuring of late Middle Paleolithic settlement. The homogeneous patterning discovered contrasts with the former fairly heterogeneous image of the Middle Paleolithic record that emerged through typological assignments. In this context, we have to once again stress the identification of several assemblages containing <span class=\"fachbegriff\">Keilmesser<\/span> with and without tranchet blow (Frick et al. 2018; Frick et al. 2017, also this volume; Herkert et al. 2015). Despite all of the production variability observed, this litho-technological correspondence within the industries links them to a plausible site cluster present in a region which is on the margins of the traditional circumjacent late Middle Paleolithic techno-complexes or facies (Fig. 13). This comparative regional analysis is an indispensable step for macroscopic considerations.<\/p>\n<figure id=\"attachment_3361\" aria-describedby=\"caption-attachment-3361\" style=\"width: 800px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig13-800x771.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig13-800x771.jpg\" alt=\"Schematic extent of different late Middle Paleolithic technocomplexes as indicated by different authors\" width=\"800\" height=\"771\" class=\"size-large wp-image-3361\" srcset=\"https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig13-800x771.jpg 800w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig13-300x289.jpg 300w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig13-768x740.jpg 768w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig13-600x578.jpg 600w, https:\/\/kernsverlag.com\/wp-content\/uploads\/2024\/04\/herkert_fig13.jpg 1280w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\" \/><\/a><figcaption id=\"caption-attachment-3361\" class=\"wp-caption-text\">Fig. 13: Schematic extent of different late Middle Paleolithic technocomplexes as indicated by different authors. MTA (Mousterian of Acheulean Tradition): bright yellow according to Soressi and Roussel (2014), light yellow according to Ruebens (2013); MBT (Mousterian with Bifacial Tools): according to Ruebens (2013); KMG (Keilmessergruppe): according to Ruebens (2013); Charentian (with Micoquian influence): according to Koehler (2009); N\u00e9ronien: according to Koehler (2009); Rhodanien: according to Koehler (2009). The red spot indicates the location of the C\u00f4te Chalonnaise region. (map: wikipedia.org; mapping: Herkert).<\/figcaption><\/figure>\n<p>Our research has only just begun, and the identified presence of <span class=\"fachbegriff\">Keilmesser<\/span> already enlarges the traditional extent of the central-eastern European <span class=\"fachbegriff\">Keilmessergruppen<\/span> complex further to the west. Other lithic elements, such as various bifacial objects, have already led to other attributions for the Verpilli\u00e8re I assemblage, such as a Charentian with Micoquian influence, or, in a broader scale, to a Mousterian with Bifacial Tools (MBT) with affinities even to a Mousterian of Acheulian Tradition (MTA) (Koehler 2009; Ruebens 2012, 2013). To date, no definite attribution of the different assemblages can to be made. But rather than defining a discrete technocomplex, we propose to see the southern Burgundy site cluster in terms of a regional \u201cstyle zone\u201d (Binford 1965: 208), embedded in and reflecting the technological traditions of the surrounding space-time units and thus demonstrating the \u201c[&#8230;] typo-technological and spatio-temporal variability\u201d (Ruebens 2013: 349) of late Middle Paleolithic behavior.<\/p>\n<h2>Conclusion<\/h2>\n<p>We provide a comparative overview of a number of Middle Paleolithic assemblages from the C\u00f4te Chalonnaise that reveals quite homogeneous characteristics. The presence of bifacial objects, and, therein, particularly the presence of <span class=\"fachbegriff\">Keilmesser<\/span> (with tranchet blow), embedded in a nearly exclusively Levallois-based blank production with a laminar component, strongly suggest a litho-technological linked site cluster. In total, five sites out of ten feature <span class=\"fachbegriff\">Keilmesser<\/span> within their assemblages and four more contain bifacial elements (Table 7). The Levallois production shows a clear predilection for preferential and centripetal reduction (Fig. 4). On a regional scale, initial indications emerge regarding inter-site functionality within the ranged habitat. High resolution data from stratified deposits show further evidence for spatial intra-site organization within the region. There, the example of Verpilli\u00e8re I demonstrates spatial patterning for lithic production purposes (Fig. 11). At Verpilli\u00e8re II, a distinct deposition of faunal remains and lithic artifacts indicates intended zoning within the occupation area (Fig. 12). Located on the margins of surrounding traditional late Middle Paleolithic techno-complexes, the research area is judged crucial to further our understanding of the relationship and possible interplay between these lithological facies at the end of MIS4 and the beginning of MIS3.<\/p>\n<h2>Acknowledgments<\/h2>\n<p>We would like to thank H. Koehler for initiating and organizing the conference \u201cThe Rhine during the Middle Paleolithic: Boundary or Corridor?,\u201d from which this article originates. Further thanks go to those who support and contribute to our research in Burgundy.<\/p>\n<p>Research presented in this paper was financed in the course of the DFG CRC 1070 \u201c<span class=\"eigenname\">RessourcenKulturen<\/span>\u201d at the University of T\u00fcbingen, the DFG project FL 244\/5-2 and the PCR \u201c<span class=\"eigenname\">Le Pal\u00e9olithique sup\u00e9rieur ancien en Bourgogne m\u00e9ridionale<\/span>,\u201d UMR 6298 ARTeHIS, affiliated with the Universit\u00e9 de Bourgogne, Dijon.<\/p>\n<p>Cordial thanks also go to Dominique Rose for her patient English revision. Furthermore, we would like to thank the editors and anonymous reviewers, whose excellent remarks greatly helped transform the initial manuscript into a paper worthy of publication.<\/p>\n<h2>Literature<\/h2>\n<p>Banks, W. E. 2004. Toolkit Structure and Site Use: Results of a High-Power Use-Wear Analysis of Lithic Assemblages from Solutr\u00e9 (Sa\u00f4ne-et-Loire), France. 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T\u00fcbingen.<\/p>\n","protected":false},"excerpt":{"rendered":"<div class=\"entry-summary\">\nDieser Beitrag untersucht das technologische und allgemeine Erscheinungsbild der mittelpal\u00e4olithischen Inventare aus mehreren Fundstellen im Gebiet der C\u00f4te Chalonnaise, Burgund, Frankreich. Ausgehend von mehreren charakteristischen Merkmalen innerhalb des stratifizierten Materials der Grotte de la Verpilli\u00e8re II (Germolles), konnten die aktuellen Forschungen kongruente technologische Muster f\u00fcr eine Reihe der umliegenden Fundstellen nachweisen.\n<\/div>\n<div class=\"link-more\"><a href=\"https:\/\/kernsverlag.com\/de\/the-middle-paleolithic-of-the-cote-chalonnaise-chronology-technology-and-palethnological-elements\/\" class=\"more-link\">Weiterlesen\u2026<\/a><\/div>\n","protected":false},"author":1,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[303,305,398],"tags":[],"class_list":["post-2724","post","type-post","status-publish","format-standard","hentry","category-englisch","category-open-access-artikel","category-rhine-during-middle-paleolithic-de","entry"],"acf":[],"_links":{"self":[{"href":"https:\/\/kernsverlag.com\/de\/wp-json\/wp\/v2\/posts\/2724","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/kernsverlag.com\/de\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/kernsverlag.com\/de\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/kernsverlag.com\/de\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/kernsverlag.com\/de\/wp-json\/wp\/v2\/comments?post=2724"}],"version-history":[{"count":2,"href":"https:\/\/kernsverlag.com\/de\/wp-json\/wp\/v2\/posts\/2724\/revisions"}],"predecessor-version":[{"id":3365,"href":"https:\/\/kernsverlag.com\/de\/wp-json\/wp\/v2\/posts\/2724\/revisions\/3365"}],"wp:attachment":[{"href":"https:\/\/kernsverlag.com\/de\/wp-json\/wp\/v2\/media?parent=2724"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/kernsverlag.com\/de\/wp-json\/wp\/v2\/categories?post=2724"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/kernsverlag.com\/de\/wp-json\/wp\/v2\/tags?post=2724"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}