THE MESOLITHIC of the CHANNEL ISLANDS: ECONOMY and SETTLEMENT IN A CHANGING LANDSCAPE

Summary: Results of recent surveys, combined with a re-evaluation of lithic assemblages from earlier surface collections, suggest the existence of several Mesolithic sites in the Channel Islands. the lithic assemblages from these sites find parallels on the mainland of North-Western France, suggesting that most of the Channel Island sites date to the 'Middle Stage'Mesolithic (c 8500-10,000 BP). the evidence for Mesolithic activity in the island is discussed in the context of the evidence for changing sea-levels and environmental conditions. It is argued that sites were preferentially located at the junction of several ecozones and that, for a short period of time during the 8th & 9th Millennia BP, sea-levels and environmental conditions in the area were particularly favourable for the exploitation of a broad range of resources.     

Radiocarbon chronology and the correlation of hunter–gatherer sociocultural change with abrupt palaeoclimate change: the Middle Mesolithic in the Rhine–Meuse–Scheldt area of northwest Europe

Recent refinements in radiocarbon sampling procedures have enabled a more robust absolute chronology for the Mesolithic in the Rhine–Meuse–Scheldt area of northwest Europe. These refinements have allowed for a new chronological sub-division of the Early and Middle Mesolithic periods. Results of this research have indicated that the Middle Mesolithic period was bound by two Early Holocene cooling events, one at 9300 cal. BP and the other at 8200 cal. BP. These results enable a critical evaluation of the role of chronological precision in the investigation of contemporaneity between abrupt climate change and hunter–gatherer sociocultural change. In this paper we focus on the variable chronological resolution of the Early to Middle and Middle to Late Mesolithic transitions in the RMS area, and the role of this variable resolution in our ability to investigate the contemporaneity of these two transitions with different Early Holocene abrupt cooling events. This paper highlights two central challenges facing archaeological investigations of the relationships between climate and culture change: first, the requirement of tight chronological overlap between climate and culture change events and consideration of leads and lags in ecosystem and subsequent human responses to climate change; second, the equifinality problem and the separation of the impact of gradual from punctuated environmental change on human societies.     

Contexts of Monumentalism: regional diversity at the Neolithic transition in north-west France

The origins of funerary monumentalism in north-west France remain inextricably linked to questions surrounding the Neolithic transition in that region. Debate continues over the relative importance of influences from earlier Neolithic communities in north-east or southern France on the Mesolithic communities of western France. An alternative interpretation places these influences within the context of broad processes of change affecting indigenous communities throughout northern and western France during the fifth millennium BC. The evidence from several regions of northern and western France is reviewed in this perspective, with emphasis on the regional character of monument traditions. Though at one level these regional narratives must have been interrelated, the regional diversity of the process must also be underlined. The argument moves us away from simplistic notions of extraneous influences to a more nuanced understanding of change within the context of individual communities at the Mesolithic/Neolithic transition.     

The existence of open areas during the Mesolithic: evidence from aeolian sediments in the Elbe–Jeetzel area,northern Germany

Traditionally Mesolithic hunter–gatherer cultures are supposed to have lived in a primeval forest environment with a closed vegetation cover during the Early and Mid-Holocene. It is not until the onset of subsequent Neolithic agricultural societies that the development of more expansive open areas is assumed. Therefore our perception of the Mesolithic economy in the European lowlands is highly affected by the idaea of adaptation to dense forest environments and a very stable system of resource exploitation. However, recent palaeoenvironmental studies provide evidence that areas of open landscapes must have existed at least temporarily during the Mesolithic and evoke the question whether human impact may be accountable for this.     

New Insights into Mesolithic Human Diet in the Mediterranean from Stable Isotope Analysis: The Sites of Campu Stefanu and Torre d'Aquila,Corsica

Mesolithic human remains are rare in the archaeological record of the French Mediterranean. Only the island of Corsica has so far produced relatively well‐preserved burials, and recent archaeological excavations have brought to light new Mesolithic human remains. The site of Campu Stefanu , located in Sollacaro in the southeast of the island, contained a collective burial of seven to eight individuals in a previously unobserved funerary context. A re‐evaluation of collections in regional museums yielded the remains from another Mesolithic individual from the site of Torre d 'Aquila , excavated at Pietracorbara, in the northern part of the island, at the beginning of the 1990s. These two discoveries presented the rare opportunity to obtain new radiocarbon dates and paleodietary insights from this crucial time period using stable isotope analysis (δ¹³C, δ¹⁵N) on collagen. From Campu Stefanu, one individual had sufficient collagen preserved for radiocarbon dating, revealing that it is the oldest Mesolithic human known on the island, dated to 10216–9920 cal. BP. At Torre d'Aquila, radiocarbon dates indicate that the individual belonged to a younger Mesolithic phase than Campu Stefanu, dated to 9903–9596 cal. BP. δ¹³C and δ¹⁵N isotope ratios are similar between the Campu Stefanu and Torre d'Aquila individuals and indicate a diet dominated by the consumption of terrestrial animal protein and a lack of marine resources. These findings are in contrast with the previous results from two other Mesolithic individuals from Corsica from the sites of Araguina Sennola and Monte Leone , for which about 25–30% of the consumed proteins came from a marine diet. The dietary variability recorded in Corsica is consistent with results obtained from Mesolithic human remains of Sicily and the Iberian Peninsula. We can hypothesise, that despite the nomadic lifestyle, the distance to the sea played a major role in Mesolithic food choices in Corsica. Copyright © 2016 John Wiley & Sons, Ltd.     

MESOLITHIC PLANT EXPLOITATION AT THE BALMA ABEURADOR (FRANCE)

Summary. Research conducted at the Balma Abeurador and a complex of related Epipalaeolithic and Mesolithic sites in the western Languedoc and eastern Pyrenees region of France (Abri de Dourgne, Grotte Gazel, Balma Margineda) reveals the complex processes of cultural and economic development during the early Holocene at a time of significant environmental change. Mesolithic groups expanded their subsistence base into a veritable "broad spectrum" economy including the hunting of large mammals, small game and birds; seasonal fishing for salmonids; collecting terrestrial and marine molluscs; and the gathering of wild legumes, fruits and nuts. The identification at Abeurador of lentils, peas and chick peas morphologically indistinguishable from the early cultigens of Southwest Asia raises the question of incipient cultivation practices in the west Mediterranean as early as 10,000 b.p.     

Radiocarbon Chronology of the Siberian Paleolithic

We have compiled 462 C-14 determinations for 120 Paleolithic and Mesolithic sites from Siberia and the Russian Far East. The Mousterian sites are dated to ca. 46,000–28,500 BP. The Middle–Upper Paleolithic transition dates to ca. 43,300–28,500 BP. Although there are a few earlier sites, most of the Upper Paleolithic sites are dated to the time interval between ca. 34,000 BP and 10,000 BP. The earlier Upper Paleolithic stage is characterized by macroblade technology and is radiocarbon-dated to ca. 34,000–20,000 BP. The earliest microblade technology occurs in the late stage of the Upper Paleolithic, dated to ca. 23,000–20,000 BP, but the majority of microblade sites is dated to ca. 20,000–11,000 BP. The Final Paleolithic (Mesolithic) sites date to ca. 12,000–6000 BP. At ca. 13,000–11,000 BP, the earliest Neolithic appeared in both the Russian Far East (Amur River basin) and the Transbaikal. The Paleolithic–Neolithic transition occurred ca. 13,000–6000 BP.     

Hunting,gathering, fishing and herding: Animal exploitation in Sandy Flanders (NW Belgium) during the second half of the fifth millennium BC

Abstract

At Doel, in the lower basin of the river Scheldt, excavations have revealed camp sites of the Swifterbant culture dating back to the second half of the fifth millennium BC. They document the transition period from the Late Mesolithic to the Early Neolithic in Sandy Flanders (NW Belgium). The sites were situated on the top of sandy ridges which were covered with an alluvial hardwood forest vegetation and surrounded by wetlands. Only burnt animal remains survived at the sites, illustrating (seasonal) fishing and hunting. In addition, botanical evidence indicates the herding of domestic mammals. The finds are of importance for the reconstruction of the chronological development of the food economy of the Swifterbant culture.     

Possible Wild Boar Management during the Ertebølle Period. A Carbon and Nitrogen Isotope Analysis of Mesolithic Wild Boar from Fannerup F,Denmark

This paper presents a stable isotope and radiocarbon study on a total of 85 samples of wild boar (Sus scrofa), humans (Homo sapiens), dogs (Canis familiaris), red deer (Cervus elaphus) and roe deer (Capreolus capreolus) from four Late Mesolithic sites in Jutland, Denmark. Four of the eight Sus scrofa samples from one site, the shell midden of Fannerup F, show markedly enriched carbon and nitrogen isotope values, indicating a dietary intake of a substantial amount of marine food. In contrast to standard interpretations of Late Mesolithic animal economy, we suggest that the enriched values of Sus scrofa may be an indication of management by Ertebølle groups in the area that facilitated access to substantial amounts of marine foods for these wild boars compared to contemporaneous conspecifics. The ¹⁴C dates of the Sus scrofa range from 5290 to 4335 cal BC, suggesting that the management of Sus scrofa developed independently of contact with Neolithic societies. Although the sample size remains small, the interpretation of Late Mesolithic animal management adds to the growing evidence for political and economic complexity in the Ertebølle culture.     

Coal used for Fuel at Two Prehistoric Sites in Southern France: Les Canalettes (Mousterian) and Les Usclades (Mesolithic)

Charcoal analysis—the study of charcoal from archaeological contexts—is designed to reconstruct palaeoenvironment and human use of wood. At two prehistoric sites in the Causse du Larzac (France)—Les Canalettes (Mousterian) and Les Usclades (Mesolithic)—charcoal analysis has revealed specimens whose anatomical structure was abnormally compressed in transverse section. The authors conducted experiments to determine how the compression could have occurred. The result was the first evidence for lignite in Palaeolithic settlements. Lignite fragments in a hearth suggest local Palaeolithic people used it for fuel. The lignite could have come from major coal outcrops within 7 to 15 km of the sites. Coal use is otherwise unknown for Palaeolithic cultures in France, and its use at Les Canalettes during the last glacial is the oldest recorded instance. Coal may have been used for fuel primarily because wood became scarce during the last glacial.     

The oldest agriculture in northern Atlantic Spain: new evidence from El Mirón Cave (Ramales de la Victoria,Cantabria)

Emmer wheat (Triticum diccocum) has been positively identified from the stratigraphically oldest ceramic- and domesticated livestock-bearing level of El Mirón Cave in the Cantabrian Cordillera. The grain is AMS ¹⁴C-dated to 5550±40 BP. This date is congruent with six others from the same layer, higher within which were found other grains of wheat, including einkorn as well as emmer. Although wild ungulates (mainly red deer) were still hunted, abundant ovicaprines, together with small numbers of cattle and pigs, appear in this level-for the first time in the 40,000-year record at El Mirón. Potsherds (undecorated, but of very good quality) also appear abruptly and abundantly. However, the associated lithic assemblage contains specific tool types also found in late Mesolithic contexts in Cantabrian Spain. In addition to the full suite of Neolithic indicators at El Mirón, as confirmed by less unambiguous early agro-pastoral evidence from other sites in the Vasco-Cantabrian region, there are megalithic monuments both in the vicinity of the cave and throughout the region that are similarly dated. All these data tend to suggest that Neolithic adaptations—already present about a millennium earlier not only along the Mediterranean coast, but also much closer, to the southeast of the Cordillera—were quickly adopted as “a package” by Cantabrian Mesolithic foragers, possibly as a consequence of social contacts with Neolithic groups in southern France and/or the upper Ebro basin of north-central Spain.     

Stable carbon and nitrogen isotope analysis on human remains from the Early Mesolithic site of La Vergne (Charente-Maritime,France)

We report here the results of stable carbon and nitrogen isotope analysis of human and faunal remains from La Vergne (Charente-Maritime, western France), a rare Early Mesolithic burial site (ca. 8500–8000 cal BC). The results for nine humans (average δ¹³C = −19.3‰; δ¹⁵N = 9.4‰) indicate a strongly terrestrial diet, dominated by animal protein, with the possibility of, at best, a slight contribution of marine-derived protein. Given lower sea-levels in the early Holocene, the site would have been some 60–80 km from the sea at the time of its use; nevertheless, contacts with the coast are shown by the presence of numerous marine shell beads in the graves. In the light of the stable isotope results, it is suggested here that such contacts most likely took the form of exchange with coastal communities whose remains now lie underwater.     

Late Mesolithic hunting of a small female aurochs in the valley of the River Tjonger (the Netherlands) in the light of Mesolithic aurochs hunting in NW Europe

The valley of the River Tjonger, situated in the Province of Friesland (the Netherlands), is rich in prehistoric organic remains. The fill of the valley, consisting of waterlogged sediments (peat, gyttja and sands), presents favourable conditions for the preservation of bone, antler and botanical remains. Numerous bones with chop and cut marks, in majority of aurochs (Bos primigenius), are known from several locations in the valley. The Late Mesolithic (ca. 8000–5500 BP) is especially well represented. In this paper we present a recently discovered small hunting and butchering wetland site dating to the Late Mesolithic. The site, named Balkweg, represents a single hunting and primary butchering event pertaining to a small female aurochs with a height at the withers of 134 cm. The morphology of the vertebrae and the phalanges as well as the Late Mesolithic date confirm the identification as an aurochs cow. Single event sites are underrepresented in the archaeological record due to their small size and poor visibility. The importance of aurochs hunting during the Mesolithic is discussed in this paper as well.     

Trapeze shaped flint tips as proxy data for occupation during the Late Mesolithic and the Early to Middle Neolithic in the northern part of the Netherlands

In the northern part of the Netherlands (defined here as the area situated above the river Rhine), the Late Mesolithic is dated to the period between ca. 8100 and 6000 BP, and is characterised by the occurrence of trapeze shaped flint tips. Trapezes continue to be in use during the Swifterbant culture (ca. 6000–4800 BP), including the ceramic Mesolithic phase (Early Swifterbant) which is dated between 6000 and 5600 BP. During the Funnelbeaker culture or TRB (ca. 4800–4100 BP) transverse points dominate. With the onset of the Single Grave Culture (SGC) transverse points are no longer the ‘preferred weapon of choice’; they are replaced by surface-retouched (tanged) points. In this paper some of the basic premises of the typological development of trapezes (narrow to broad) and the chronological relevance of ‘subtypes’ (symmetric, asymmetric, right-angled and rhombic) are discussed based on analyses of trapezes from four excavated Mesolithic and Swifterbant sites. For comparison a random sample of TRB transverse points was included in several analyses as well. One of the main conclusions of this paper is that it is possible, based on analyses of metric and non-metric traits of trapeze shaped flint tips, to distinguish between true ‘Mesolithic’ trapezes, trapezes belonging to the (Neolithic) Swifterbant culture, and transverse points of the TRB. The outcomes of these analyses may help in obtaining a relative date for undated (surface) assemblages, and may furthermore lead to the positive identification of Swifterbant settlements in the higher (situated above the present-day sea level) Pleistocene areas in the northern and eastern part of the study area which are so far unknown. The results presented here will be put to the test in a forthcoming paper.     

Points in Time: The Mesolithic–Neolithic Transition and the Chronology of Late Rod Microliths in Britain

This paper presents the results of the Bayesian statistical modelling of radiocarbon dates associated with diagnostic late Mesolithic rod microliths from England and Wales. These date estimates are compared with results for the earliest evidence for Neolithic material culture and practices in Britain (Whittle et al. 2011; Griffiths 2011; 2014; forthcoming). The chronology of some rod microlith sites indicates a potential overlap between the earliest Neolithic and latest Mesolithic material culture and practices, in the first three centuries of the fourth millennium cal BC across England and Wales. The locations of late Mesolithic sites suggest regional processes of ‘neolithization’ may have occurred. In the region where we have the best chronological evidence for late Mesolithic sites – in Yorkshire – the location of the very latest Mesolithic sites suggests these lifeways may have persisted in landscapes which had been foci of hunter‐gatherer activity for hundreds of years, and which might have been understood as ‘ancestral’ or ‘persistent’ places.     

Smakkerup Huse: A Mesolithic Settlement in NW Zealand,Denmark

Abstract

Excavations at the site of Smakkerup Huse on the island of Zealand, Denmark, have revealed Late Mesolithic Ertebølle deposits, dating between 5000 and 3900 B.C. Preservation was excellent and a variety of bone, antler, wood, and other plant remains were recovered in the waterlogged deposits, along with stone and ceramic artifacts. The remains document a diverse subsistence base utilizing both marine and terrestrial foods, an elaborate wood technology, new artifact types, and some of the oldest domestic cows in Scandinavia. This report provides background information on the site, and discusses the artifacts and plant and animal remains. The question of domestic animals in the Late Mesolithic is addressed.     

Drowned and deserted: a submerged prehistoric landscape in the Solent, England

A submerged landscape containing worked flint tools has been found at—11m OD in the western Solent. This paper reviews coastal sites in northern Europe and suggests that many similar sites should exist around the coast of southern England; as a result of isostatic shifts and eustatic fluctuations many coastal sites of the Mesolithic will now be submerged. A need has been identified to locate, protect and record submerged sites before they are lost to erosion or development, for which outline proposals are suggested.     

Experimental studies of personal ornaments from the Iron Gates Mesolithic

Personal ornaments, especially those made from the shells of marine mollusks and animal teeth, have been recovered from many Mesolithic sites across Europe. This paper reviews the evidence of personal ornaments from the Mesolithic of the Iron Gates, where such finds were identified in five sites on the Romanian bank: the cave and rock shelter sites of Climente II and Cuina Turcului, and three open-air sites—Icoana, Ostrovul Banului, and Schela Cladovei. The ornaments from these sites were made from the shells of several gastropod taxa and at least one species of dentaliid scaphopod, as well as the pharyngeal teeth of cyprinids, the teeth of several species of terrestrial mammal, fish vertebrae, and pieces of antler and bone. Particular attention is given to taxonomic identification and questions of taphonomy, provenance, selection, manufacture, and use. Experiments were conducted in which several types of ornament were replicated. Archeological and experimental pieces (at various stages of production) were examined under a microscope, to establish the durability of the beads and estimate the length of time over which they were worn. Our results show that shells of Lithoglyphus and Theodoxus sp. were simply perforated and fixed in composed adornments, as were shells of Tritia neritea in the early part of the time range. In the later Mesolithic, T. neritea shells were processed in a different way and fixed to clothing in the manner of appliqués. No technological modification of the cyprinid teeth was observed; these were sewn individually onto clothing by means of a thread coated with an adhesive substance. The other categories of personal ornament were used mainly as pendants. Experimental use-wear analysis suggests that many ornaments were used over long periods, with broken or missing pieces replaced when necessary.     

The laziness of the short-distance hunter: The origins of agriculture in western Denmark

The Ertebølle Mesolithic culture of western Denmark resisted the advance of agriculture for over 1000 years. Marine resources were predominant in the Mesolithic diet. Oysters were a relatively minor resource but are argued to have played an important role by filling a gap in the resource cycle in late winter and spring. The appearance of agriculture coincides with a decrease in marine salinity, which caused a decline in oyster availability. Other marine resources may also have declined for the same reason.