103 Documenta Praehistorica XLIII (2016) Becoming sedentary| The seasonality of food resource exploitation in the Mesolithic-Neolithic Danube Gorges Vesna Dimitrijević 1, Ivana ?ivaljević 2 and Sofija Stefanović 2 1 Laboratory for Bioarchaeology, Department of Archaeology, Faculty of Philosophy, University of Belgrade, RS vdimitri@f.bg.ac.rs 2 BioSense Institute, University of Novi Sad, RS sofija.stefanovic@biosense.rs Introduction With their long temporal sequence, spanning be- tween c. 9500 to 5500 cal BC (corresponding to the regional Mesolithic, Mesolithic-Neolithic Transforma- tion phase and the Early/Middle Neolithic) (Bori≤, Dimitrijevi≤ 2009; Bori≤ 2011), open-air sites in the Danube Gorges (North-Central Balkans) provide great opportunities for studying and understanding vari- ous aspects of Mesolithic-Neolithic transition. In par- ticular, intensified building activities in the Late Me- solithic and Transformational Mesolithic-Neolithic phases (cf. Bori≤, Dimitrijevi≤ 2009; Bori≤ 2011) have been interpreted as archaeological indicators of increased sedentism resulting from developing social complexity of local hunter-gatherer-fisher communi- ties (cf. Voytek, Tringham 1989; Chapman 1993; Radovanovi≤ 1996; Radovanovi≤, Voytek 1997) and from merging local traditions with new economic and social practices accompanying ‘Neolithic’ life- ways (cf. Bori≤ 2007; 2011; Jovanovi≤ 2008). Ob- viously, there is no universal mode of hunter-fisher- gatherer existence, as opposed to a presumed seden- tary lifestyle of food-producing communities, nor can a clear-cut change from mobility to sedentism be assumed. Moreover, degrees of sedentism are often difficult to assess and divide into neat categories due to the complexity of human lifestyles and residen- tial practices (cf. Whittle 2001). One of the starting points, however, most commonly involves determin- ing whether the sites in question were occupied sea- sonally or year-round. This feature can be addressed by looking at subsistence patterns, i.e. the seasons of exploitation of most important animal species, as has been demonstrated by a number of studies, which range from simple observations of the pres- ABSTRACT – In this paper, we investigate whether the Mesolithic-Neolithic sites in the Danube Gorges were occupied seasonally or all year round by looking at animal skeletal remains. The hunting sea- sons of most important game animals have been determined on the basis of antler and teeth growth, supplemented by looking into the presence of migratory fish and birds. The patterns of food resource exploitation seem to indicate year-round occupation of the settlements, and suggest that a significant degree of sedentism existed in the Danube Gorges prior to, and independently of, the adoption of animal and plant husbandry. IZVLE∞EK – V ≠lanku na podlagi analize ∫ivalskih ostankov raziskujemo, ali so bila mezolitsko-neo- litska najdi∏≠a na obmo≠ju soteske D∫erdap poseljena sezonsko ali ≠ez celo leto. Na podlagi rasti ro- govja in zob smo dolo≠ili lovno sezono za najpomembnej∏o divjad, podatke pa smo dopolnili z anali- zo selitve rib in ptic. Vzorci rabe raznih virov prehrane ka∫ejo na celoletno poselitev na naselbinah; sklepamo tudi, da se je na obmo≠ju D∫erdapa delno sedentaren na≠in ∫ivljenja pojavil lo≠eno od in pred pojavom prvih doma≠ih ∫ivali in kultiviranih rastlin. KEY WORDS – seasonality; archaeozoology; sedentism; Danube Gorges; Mesolithic-Neolithic DOI> 10.4312\dp.43.4 Vesna Dimitrijević, Ivana ?ivaljević and Sofija Stefanović 104 ence/absence of seasonally available fauna, to more sophisticated analytical procedures, including the determination of the individual ages and the season of death of exploited animals, skeletochronology, or growth-increment studies (cf. Pike-Tay et al. 2004), or stable isotope balances in teeth and bones (Blaise, Balasse 2011). In this study, we present estimated seasons of cap- ture on the basis of the results of ageing of faunal skeletal elements (teeth and antler) of economical- ly important wild game species, supplemented by quantifications of fish and bird remains (some of them available seasonally and others more or less all year round) from sites at Vlasac, Lepenski Vir, and Padina. By no means exhaustive, this study aims to offer additional data relevant to understanding subsistence and settlement patterns, and to shed more light on the relationship between hunting, fish- ing and increased sedentism in the Danube Gorges. Archaeological background The Padina, Lepenski Vir, and Vlasac sites are situ- ated in the Upper Gorge (Gospo∂in Vir, or Lady’s Whirlpool) of the Danube Gorges (Fig. 1), on river- ine terraces sloping towards the Danube. The initial rescue excavations of the sites were undertaken in the 1960s and 1970s (Srejovi≤ 1969; 1972; Srejo- vi≤, Letica 1978; Radovanovi≤ 1996; Jovanovi≤ 2008), prior to the raising of the water level due to dam construction, and new revisory excavations of the preserved portion of the Vlasac terrace were car- ried out in 2006–2009 (Bori≤ 2006; Bori≤ et al. 2008; 2014). The earliest traces of human presence in these locations date to the period of c. 9500– 7400 cal BC (the Early Mesolithic) (Bori≤, Dimitrije- vi≤ 2009; Bori≤ 2011), and are manifested by occa- sional burials (some in a seated position), several stone constructions (Bori≤, Miracle 2004; Jovanovi≤ 2008), as well as caches of animal bones originating predominantly from wild game and fish (Bori≤, Di- mitrijevi≤ 2006), but also from canids displaying mixed wolf and dog features, suggesting that the ini- tial stages of dog domestication took place during this time (Dimitrijevi≤, Vukovi≤ 2015). The few and fragmentary traces of Early Mesolithic occupation are mostly due to their disturbance and devastation by later (Late Mesolithic and Transfor- mation phase) building and occupational activities (Bori≤ 2011). The Late Mesolithic phase (c. 7400– 6300/6200 cal BC) is particularly well documented at Vlasac (Bori≤ 2011), where numerous burials, se- veral dug-out dwelling structures, stone-lined rectan- gular hearths and a large number of chipped stone, bone and antler artefacts have been discovered (Sre- jovi≤, Letica 1978; Nemeskéri 1978; Kozłowski, Kozłowski 1982; Roksandi≤ 1999; 2000; Bori≤ et al. 2008; 2014), as well as an enormous assemblage of animal bones (Bökönyi 1978). This phase also produced evidence of large-scale exchange networks, witnessed by occasional finds of good-quality flint of non-local origin, and the occurrence of marine gas- tropods Cyclope neritea and Columbella rustica in some of the burials (Cristiani, Bori≤ 2012; Bori≤ et al. 2014; Srejovi≤, Letica 1978). The Transformation/Early Neolithic phase (c. 6300/ 6200–5900 cal BC) (Bori≤, Dimitrijevi≤ 2007; Bori≤ 2011), coinciding with the emergence of the first farming communities in the Balkans, saw the estab- lishment of the first settlements with elaborate tra- pezoidal-base dwellings, distinctive sandstone sculpt- ed boulders and the introduction of pottery at Le- penski Vir and Padina (Srejovi≤ 1969; 1972; Rado- vanovi≤ 1996; Gara∏anin, Radovanovi≤ 2001; Jo- vanovi≤ 2008), but with unchanged subsistence stra- tegies dependent on hunting and fishing (Bori≤, Di- mitrijevi≤ 2006). The first domesticates (apart from Fig. 1. The Danube Gor- ges area with relevant sites mentioned in the text. The position of the Danube Gorges within a wider area – the Bal- kan peninsula shown in the lower left corner. Images from Google Earth. Becoming sedentary| The seasonality of food resource exploitation in the Mesolithic-Neolithic Danube Gorges 105 dogs) make an appearance only after c. 6000/5900 cal BC (Bori≤, Dimitrijevi≤ 2007), after most of the dwellings had been abandoned and new elements of material culture (domed ovens, ground stone tools, bone spoons), along with certain individuals of non- local origin appear in the area (Bori≤ 2011; Bori≤, Price 2013). Large-scale animal husbandry, however, was never fully introduced into the Upper Gorge; the sites continued to be in use until c. 5500 cal BC, but probably for specialised activities, most notably fishing (Bonsall 2008; Bori≤ 2011). The faunal assemblages The assessment of the nature of animal exploitation and quantification of faunal remains from the Danube Gorges are hindered by several factors, namely the inadequate recovery techniques and selective collec- tion imposed by time constraints during the course of the excavations, and the fragmentary state of fau- nal assemblages from some of the sites (Bori≤ 2001; 2002; Bori≤, Dimitrijevi≤ 2006; Dimitrijevi≤ 2000; 2008). The faunal assemblages from the old excava- tions of Lepenski Vir (1965–1970), Vlasac (1970– 1971), and Padina (1968–1970) were collected en- tirely by hand, using collection grids consisting of 4x4m quadrants. Furthermore, the enormous assem- blage from the original excavations of Vlasac, com- prising nearly 30 000 identified specimens was dis- carded after the initial analysis by Sándor Bökönyi (1978), with only a small sample of bird (Tab. 5) and fish remains preserved (Bori≤ 2002.App. 5; Di- mitrijevi≤ et al. submitted). Part of the faunal assem- blage from Lepenski Vir, mainly from first excavation seasons (up to 1969, cf. Bori≤, Dimitrijevi≤ 2006) was also discarded after the preliminary analysis by Bökönyi (1969; 1970; 1972). The preserved part of the assemblage originated from later campaigns (1968–1970), and consisted of animal bones pri- marily related to the floors of trapezoidal-base dwel- lings, and areas between and underneath them (Di- mitrijevi≤ 2000; 2008). Only the faunal assemblage from the new (2006–2009) excavations of Vlasac, as well as the one collected in 1992–1996 at the down- stream site of Schela Cladovei (Fig. 1) (Bartosiewicz et al. 1995; 2001; 2008), were collected by water sieving and flotation, in addition to hand collection (Bori≤ et al. 2014; Dimitrijevi≤ et al. submitted). The environment of Padina, Lepenski Vir and Vla- sac, which were situated on riverine terraces in a narrow belt between the river and the forest, pro- vided both good hunting and fishing conditions. The dense forests surrounding the sites were the natur- al habitat of various wild game species which were hunted for meat, as well fur-bearing animals which were probably hunted for fur or as vermin. The vi- cinity of the river and its large whirlpools enabled fishing for both freshwater species (available most of the year) and seasonally available anadromous species, as well as the exploitation of waterfowl. In terms of wild game at all three sites, the most nu- merous remains are of red deer (Cervus elaphus) which was most commonly hunted, followed by wild boar (Sus scrofa), roe deer (Capreolus capreolus), and aurochs (Bos primigenius) (cf. Bökönyi 1969; 1970; 1972; 1978; Clason 1980; Dimitrijevi≤ 2008). In terms of fishes, the remains of various cyprinids (Cyprinidae), Wels catfish (Silurus glanis), migrato- ry sturgeons (Acipenseridae), and huchen (Hucho hucho) have been discovered at all three sites, but in varying quantities (Ωivaljevi≤ in prep.). As expect- ed, the hand-collected, water-sieved and flotated sample from new excavations of Vlasac contained many more remains of smaller cyprinids and exhib- ited the greatest species diversity in comparison to hand-collected assemblages from Lepenski Vir and Padina (Tab. 4). However, in spite of the same col- lection methods employed at the latter two sites, their faunal assemblages also exhibited significant differences, namely in the absolute predominance of catfish observed at Padina. The Lepenski Vir assem- blage contained a significant number of cyprinid, cat- fish and huchen remains, but also a much greater number of sturgeon remains in comparison to Pa- dina and Vlasac (Tab. 4). The role of hunting vs. fishing in subsistence strate- gies is difficult to assess on the basis of a straight- forward comparison of quantified mammal and fish remains, given the differences in their anatomy and size, and biases affecting their survival and recovery (cf. Wheeler, Jones 1989; Takács, Bartosiewicz 1998; Bartosiewicz, Bonsall 2004; Bori≤ 2001). The analyses of carbon (δ13C) and nitrogen (δ15N) iso- tope ratios in human bone collagen have suggested that the Mesolithic inhabitants of the Danube Gorges consumed considerable amounts of fish, with a gra- dual broadening of the dietary spectrum to include more terrestrial resources at the onset of the Neoli- thic (Bonsall et al. 1997; 2004; Grupe et al. 2003; Bori≤ et al. 2004), whereas the analysis of the sul- phur (δ34S) isotope ratio has suggested that there have been significant inter- and intra-site variabili- ties in dietary practices (Nehlich et al. 2010). On the basis of faunal data, it can be hypothesised that both hunting and fishing made significant contribu- Vesna Dimitrijević, Ivana ?ivaljević and Sofija Stefanović 106 tions to the diet; the former mainly oriented to- wards red deer and the latter exhibiting more intra- site (and possibly diachronic) variety. Apart from a general emphasis on the importance of annual cycles in shaping human lives in the Danube Gorges (cf. Srejovi≤ 1969; 1972), the subject of sea- sonality was first addressed by Anneke T. Clason (1980) in her study of Star≠evo and Padina animal remains. In the description of mammal remains, she specified some specimens as seasonal markers, made some remarks on the seasonal availability of bird and fish, and hypothesised that “Padina was perma- nently inhabited during all seasons of the year”, and furthermore, that this was probably also true for Vlasac and Lepenski Vir. A discussion on the in- fluences of seasonal cycles on life in the Mesolithic Danube Gorges is given by Bori≤ in his thesis (Bo- ri≤ 2002). Here, and in several later references, sea- sonal estimates determined on the basis of particu- lar specimens of mammal remains were also noted (Dimitrijevi≤ 2000; 2008; Bori≤, Dimitrijevi≤ 2006; 2009). Materials and methods The seasonal schedule of food resource acquisition in the Danube Gorges has been determined on the basis of skeletal elements which are sensitive to the question of seasonality. This included determining the kill season of red deer and roe deer on the basis of antler growth (cf. Schmid 1972), and ageing of red deer, roe deer, fox and wild boar on the basis of tooth eruption and wear (cf. Habermehl 1985; Brown, Chapman 1991; Carter 2006; Carter, Mag- nell 2007) (Tabs. 1–3). Although radiographs were not made, the fragmentary state of some of the man- dibles and loose teeth enabled ageing on the basis of root formation stages (after Brown, Chapman 1991; Carter 2006; Carter, Magnell 2007). Other mammal species were not taken into account, either because they were not represented by juvenile ani- mals, are not seasonal breeders, or they give birth several times a year. The breeding and reproduction patterns of dogs in particular could have changed significantly as a result of domestication, and could have extended throughout several seasons. In this respect, the most reliable season indicators are milk and erupting permanent teeth of juvenile animals, given that they follow a fairly standardised schedule, whereas tooth wear does not occur at an even pace (Bartosiewicz 1989; Pike-Tay et al. 2004). Less reliable season indicators are shed antlers; even if they are dropped during limited periods of the year (February-March in the case of red deer and Oc- tober-November for roe deer, cf. Schmid 1972), they could have been collected at any time and/or curat- ed, especially since they were extremely valued as raw material and often structurally deposited. We assumed that red deer give birth at the begin- ning of June (cf. Carter 2006); similarly, the birth- ing season of recent red deer populations in the re- gion is described as taking place “at the end of May – beginning of June” (Grupa autora 1991). Roe deer give birth in May (Grupa autora 1991; Haber- mehl 1985; Carter 2006). The farrowing season of wild swine is seasonally less restricted, occuring in March-April in recent wild pig populations in the Balkans (Grupa autora 1991), whereas in Sweden and Germany (Carter, Magnell 2007), as well as in Turkey (Bull, Payne 1982) it occurs between March and May. Wild sows may breed twice a year, thus substantially widening the farrowing season; how- ever, 65–90% of births occur between March and May, mostly March and April in Sweden and Ger- many (Carter, Magnell 2007 and references there- in). Similarly, in the Balkans, 85% of births take place in March and April (Grupa autora 1991). Fox cubs are born in March (Habermehl 1985). The observations on the hunting seasons of most important game animals were supplemented by looking into the seasonal availability of migratory fish and birds and quantifying their remains (Tabs. 4–5). As noted by László Bartosiewicz and Clive Bonsall (2004) and Bartosiewicz et alii (2008), the presence/absence criteria is highly probabilistic, given that the presence of a certain species might signal occupation during a particular season, but its absence does not imply the lack of occupation at other times. For example, prior to the Iron Gates’ dams construction, anadromous sturgeons – beluga (Huso huso), Russian sturgeon (Acipenser guelden- staedtii), ship sturgeon (Acipenser nudiventris), and stellate sturgeon (Acipenser stellatus), undertook their bi-annual spawning migrations from the Black Sea at particular times of the year (in early spring and autumn), but with inter-specific and individual differences in the start and peak dates depending on water temperature. Also, the populations migrating in autumn were known to overwinter in the river (Risti≤ 1977). It should be noted, however, that the main sturgeon fishing seasons in the Danube Gorges in more recent times corresponded with their migra- tion patterns, with most catches occurring in spring, followed by autumn (cf. Petrovi≤ 1998. [1941]; for Becoming sedentary| The seasonality of food resource exploitation in the Mesolithic-Neolithic Danube Gorges 107 different data from Hungary, see Bartosiewicz et al. 2008). The investigation of the presence of migratory birds as seasonal indicators is also based on the assump- tion that their behaviour in the past roughly mir- rored their present migration patterns. In addition, it should be noted that bird remains at sites could have been accumulated not only by humans and dogs, but wild predators as well, having in mind that no bird bones bore butchering marks. This hypoth- esis does not seem likely for certain species – parti- cularly birds of prey, which nested in the high cliffs of the Gorges – but cannot be completely ruled out. Therefore, the data we present here includes the sug- gested seasons of kill of the most important game animals, which could vary to some extent due to slight or greater variations in the birthing seasons of the species and their ontogeny, as well as the most probable seasons of exploitation of migratory spe- cies, assuming their past migration patterns broadly correspond to those observable in more recent times. Results Vlasac As opposed to the 640m2 area excavated in 1970– 1971 (Srejovi≤, Letica 1978), the preserved portion of the Vlasac terrace encompassed by the 2006– 2009 excavations (326m2) covered the southern- most peripheral area of the original settlement (Bo- ri≤ et al. 2014), with much less evidence of domes- tic activities or food preparation and consumption (Dimitrijevi≤ et al. submitted). This feature is cer- tainly manifested in the quantity and preservation of animal remains from the two areas of the site, in particular concerning mammal remains, which are least likely to suffer from bias in recovery techni- ques. The total number of mammal bone specimens identified to the species/genus/family level from the 1970–1971 excavations equaled 11188 (Bökönyi 1978), as opposed to 801 specimen identified to the species/genus/family level and 10955 unidentified mammal remains from the 2006–2009 excavations (Dimitrijevi≤ et al. submitted). In terms of the most important game animals, the NISP (number of iden- tified specimens) of red deer, wild boar and roe deer in the 1970–1971 assemblage equaled 6732, 1185 and 510, respectively (Bökönyi 1978), as opposed to their NISP in the 2006–2009 assemblage (209, 86 and 47, respectively) (Dimitrijevi≤ et al. submitted). However, due to more sophisticated collection tech- niques, the new excavations of Vlasac enabled the recovery of even the most fragile skeletal elements, including the deciduous teeth which were used in this study (Tab. 1), as well as a plentitude of fish re- mains (Tab. 4). Most of the mammal remains used in this study origi- nated from the 2006–2009 excavations of Vlasac, and included a fragmented red deer skull, a fragment of a roe deer skull with an antler, as well as decidu- ous and permanent teeth of red deer, roe deer, wild boar and fox. Given that the largest part of the fau- nal assemblage from 1970–1971 was discarded, in this study we were able to include only 9 unshed and 31 shed antlers of red deer, and 3 unshed ant- lers of roe deer, which were originally packed with bone and antler artefacts and thus saved (Tab. 1). The fragmented red deer skull VL 29/1 (Fig. 2) ori- ginated from a young male, and on the basis of par- tially preserved antlers still on pedicles, it was deter- mined that it was captured between September and February. The skull had been used (possibly, for a significant amount of time), most likely in a series of ritualistic activities, given that it exhibited a num- ber of modifications (numerous cuts and damage to the cranial roof and flattened occipital condyles) which could not be explained by standard butcher- ing practices (Dimitrijevi≤ et al. submitted), and that it had been deposited at the top of a sequence of several inhumations and cremations (Bori≤ 2010; Bori≤ et al. 2014.Tab. 1: the skull is described as ori- ginating from context 19). Unshed antlers collected over the course of previous excavations indicate the same broad (autumn-winter) time span, whereas, as Fig. 2. Fragmented male red deer skull (VL 29/1) from Vlasac, with fragmented antlers attached to pedicles, captured between September and Febru- ary. already noted, the use of shed antlers (even though shedding occures within a short time span) as sea- sonal indicators should be taken with caution, as it is possible they were collected later. The stages of teeth eruption and wear indicate sev- eral seasons of capture of red deer, some with more precision than others. In particular, a 3rd and 4th decidious premolar from a fragmented left maxilla (VL 216/15) (Fig. 3) pointed to an age of 7–8 months, indicative of a December-January capture; whereas a left 3rd permanent incisor with an open root and milk incisors (left and right 2nd and 3rd) and right canine (VL 237/4) (Fig. 4) from a mandible that had not been preserved pointed to an approximat eage of 15–18 months or a kill that occurred between Au- gust and November. A fragment of a roe deer skull with an antler frag- ment on a pedicle (VL 314 x. 23), as well as three unshed antlers collected in previous excavations in- dicated that the capture seasons occurred between May and October (cf. Schmidt 1972). Assuming the end of May as the season when roe deer give birth (cf. Habermehl 1985), one decidious premolar (3/4) (VL 51/1) indicated an age of one month, i.e. a June capture. As already noted, the farrowing season for wild swine is generally from March to April (cf. Grupa autora 1991; Carter, Magnell 2007); in our study, the ageing and the estimation of season is given counting from April (Tab. 1). Two teeth – an upper 3rd deciduous premolar (VL 237/5) and an upper 2nd deciduous premolar (VL 282/3) – produced fairly re- liable season estimates, an April-May and September- October kill respectively. Fox teeth (an upper deciduous canine and a germ of the first molar, VL 222/22–23) were included in this study, as they provided a fairly reliable kill season (May), given that this stage of teeth eruption is in- dicative of a three-month-old individual (cf. Haber- mehl 1985). Although most of the elements utilised in ageing offered very broad season estimates spanning over several months (Tab. 1), the aforementioned spec- imens provided fairly accurate and short seasons of death. They signal particular events which took place in December-January, April-May, May, June and Sep- tember-October, i.e. are indicative that hunting did not take place during a limited period of the year. Both the fragment of a roe deer skull with an antler (VL 314 x. 23) and the red deer skull (VL 29/1) have been directly dated, producing a date of 7131–6823 cal BC at 95% probability (OxA-21962) and 6006– 5838 cal BC at 95% probability (OxA-16544) respec- tively (Bori≤ et al. 2014). At the same time, these two dates are currently the oldest and the youngest obtained from the new excavations of Vlasac, thus dating the span of activities in the peripheral zone of the settlement, with Transformation phase activ- ity (post c. 6200 cal BC) mainly related to the inter- ment of the latest burials in the successive burial zone closed by the red deer skull (Bori≤ et al. 2008; 2014). A wild boar tooth (VL 282/3) was found in a context (a concentration of artefacts beneath the floor of a dug-out dwelling) dated with two absolute dates: 7034–6692 cal BC at 95% probability (OxA- 24809) and 7035–6698 cal BC at 95% probability (OxA-24810) (Bori≤ et al. 2014). From the previous 1970–1971 excavations, encompassing the central area of the settlement, a roe deer skull with antlers found on the floor of Building 2 (Srejovi≤, Letica 1978) produced a date of 7047–6699 cal BC at 95% probability (OxA-16216) (Bori≤ et al. 2008). There- fore, it can be concluded that the majority of these events occurred during the last century of the 8th millennium and the first half of 7th millennium BC, and could be taken as representative of Late Mesoli- thic resource exploitation patterns at the site. Vesna Dimitrijević, Ivana ?ivaljević and Sofija Stefanović 108 Fig. 3. 3rd and 4th decidious premolar from a fragmented red deer left maxilla (VL 216/15) from Vlasac, indicating an age of 7–8 months or a December-January capture: a lingual view; b buccal view; c roots, apical view. Becoming sedentary| The seasonality of food resource exploitation in the Mesolithic-Neolithic Danube Gorges 109 Similarly to mammal remains, the fish faunal assem- blage from 2006–2009 displayed significant differ- ences in comparison to the one collected in 1970– 1971. Only common carp (Cyprinus carpio), catfish, pike (Esox lucius), unidentified cyprinids and a great number of unidentified fish bones were reported by Bökönyi (1978). The absence of sturgeon was clear- ly a result of author-related bias, given that sturgeon remains were in fact identified in the preserved fau- nal sample from 1970–1971 (Bori≤ 2002.App. 5), as well as in the sample from new excavations of Vla- sac (Ωivaljevi≤ in prep.) (Tab. 4). Albeit few, the re- mains of migratory beluga, Russian sturgeon and stellate sturgeon are indicative of spring and autumn fishing at the site, given that sturgeon remains as a rule tend to be underrepresented due to their large- ly cartilaginous skeleton (Brinkhuizen 1986; Barto- siewicz et al. 2008). The exploitation of anadro- mous Black Sea shad (Alosa immaculata) would have been even more seasonally restricted, as the species is present in the Danube only between the end of March and the beginning of June (Tab. 4). However, the vast majority of fish remains from the new excavations of Vlasac originated from yet anoth- er anadromous species – the vyrezub (Rutilus frisii) of the cyprinid family, mainly due to the large number of its pharyngeal teeth found in burials, but also in ‘loose’ contexts. Burials with pharyngeal teeth ornaments, from both the old and new excava- tions of Vlasac have mainly been related to the Late Mesolithic phase, but have also been found in a Transformation phase burial at Vlasac and settle- ment deposits at Lepenski Vir (Cristiani, Bori≤ 2012; Cristiani et al. 2014; Bori≤ et al. 2014; Ωivaljevi≤ in prep.), whereas unmodified vyrezub teeth and bones occur as early as mid-10th millenium BC (Early Me- solithic) at Lepenski Vir (Ωivaljevi≤ in prep.). The species has not been reported in the Middle/Lower Danube previously, but it was probably migrating into the river from the Black Sea at least up to the Middle Holocene (Ωivaljevi≤ et al. submitted). Mo- dern Black Sea populations enter the rivers in Octo- ber, overwinter in freshwater, and return to estuar- ies after spawning, which takes place in April and May (Kottelat, Freyhof 2007). Therefore, it can be hypothesised that the main fishing seasons at Vla- sac corresponded with their autumn migration and spring spawning season, although the possibilities of winter catches should not be excluded. The possi- bility of opportunistic winter exploitation of fresh- water fish should also be allowed, although fishing during this time would have been difficult, as most species take refuge on the river bottom and hiber- nate until spring. The remains of pike, one of the few species most succesfully caught from January to April (Tab. 4), could be indicative of winter fishing at Vlasac. The bird faunal assemblage from both new and old excavations of Vlasac contained the remains of aqua- tic birds and waterfowl, as well as birds of prey and songbirds. Given that bird remains were few even in the hand-collected, water-sieved and flotated sam- ple from the new excavations (Tab. 5), it may be hy- pothesised that their exploitation was opportunistic. A somewhat greater frequency of imperial eagle (Aquila heliaca) and white-tailed eagle (Haliaeëtus albicilla) remains (Bökönyi 1978; Dimitrijevi≤ et al. submitted), and the spatial clustering of some of their remains around the area of Late Mesolithic Building 2 (Bori≤ 2002.190) could suggest that these birds of prey were possibly held in special regard. Most of the species represented in the 1970–1971 and 2006–2009 assemblage are still resident in the Danube Gorges, and therefore their presence cannot be used as a seasonal indicator. The only exceptions Fig. 4. Red deer permanent and milk front teeth (VL 237/4) from a mandible that had not been preserv- ed from Vlasac, indicating an age of 15–18 months or an August-November kill: a right milk 2nd incisor; b right milk 3rd incisor; c right milk canine; d a germ of the left 3rd permanent incisor; e left 2nd milk in- cisor; f left 3rd milk incisor. Vesna Dimitrijević, Ivana ?ivaljević and Sofija Stefanović 110 stuck to the crushed skull bones. The age of the ani- mal has been determined fairly accurately on the basis of its upper teeth, which were in the last stages of decidious/ permanent dentition replacement. In both right and left maxilla (LV 273/4), 3rd decidious molars were still holding above the crowns of per- manent fourth premolars, and it would have been a matter of days before they fell out. The 2nd and 3rd premolars, and the left 3rd molar were erupting. This stage of dental development is related to an age of 27 months, which would signal that this individual was caught in October (Dimitrijevi≤ 2000; 2008; cf. Brown, Chapman 1991). Another example is a red deer skull (LV 261/1–2) deposited on the floor of House 22 (Dimitrijevi≤ 2008.Fig. 3). At present, only antlers have been pre- served, one of which produced a date of 6084–5926 cal BC at 95% probability (OxA-16075) (Bori≤, Di- mitrijevi≤ 2009), but both the skull (placed upside down) and antlers can be seen in a photograph taken during excavation (Fig. 5). The animal was just about to shed its antlers at the moment of cap- ture; as a result, they parted from the skull when ex- cavated. This occurrence is a fairly reliable indica- tor that the kill took place in February-March, and the deposition of the skull shortly after. Given that the abandonment of aforementioned House 28 was marked by a red deer skull from an individual caught in October, these two instances indicate that the ‘life cycles’ of each building were probably unique, end- ing with similar preparations but at different times throughout the year. It would seem that certain buil- dings were in use after others fell into disuse; this practice is also suggested by the deposition of sculpt- ed boulders. Most boulders were initially placed in the rear area of rectangular hearths; however, cer- tain dwellings had empty sockets in the floor behind the hearth area, or merely a fragment of an origi- nally larger boulder inserted in the socket, which suggests that some of the boulders were moved from abandoned buildings and inserted at new locations (Srejovi≤ 1969; Bori≤ 2005). Consequently, the data on seasons of abandonment enables a better under- standing of the individual histories of the houses and the occupation of the settlement as a whole. Another fairly accurate season indicator comes from a context underneath of the floor of House 31, where a cache of animal bones, including a large part of a red deer and a brown bear skeleton, as well as re- mains of chamois, wild boar, beluga, Russian stur- geon, common carp, vyrezub, catfish, huchen and an unidentified bird bone have been found (Dimitrije- include the remains of white pelican (Pelecanus cf. onocrotalus) which migrates to the area in October- November, black kite (Milvus migrans) and imperi- al eagle which are passage visitors, present from spring to autumn, and fieldfare (Turdus pilaris) which overwinters in the area (from November to March) (Tab. 5). In the case of the resident cormo- rant (Phalacrocorax carbo), teal (Anas crecca), and mallard (Anas platyrhynchos), it should be noted that their populations increase in winter, joined by visitors from Northwestern Europe (cf. Ra- ∏ajski, Kiss 2004; Clason 1980.164). According to Anne Pike-Tay et alii (2004), teal and mallard are migratory, and are present in neighbouring Hungary in early spring and in autumn (the former used to breed in Hungary), whereas the great white egret (Egretta alba) and ferruginous duck (Aythya nyro- ca) leave the area in winter. The data on present po- pulations in Serbia and the Danube Gorges (Ra∏aj- ski, Kiss 2004; Gruba≠ et al. 2013) suggest that these are resident species, so their past migratory status is less clear. Lepenski Vir The hand-collected and partially preserved faunal assemblage from Lepenski Vir contained fewer ele- ments sensitive to seasonality (Tab. 2), but their con- textual provenance enables a better understanding of the use of trapezoidal-base dwellings and the site as a whole. At least 13 buildings contained red deer skulls with antlers (Bökönyi 1969; 1970; 1972), which were probably deposited on the floors, mark- ing the event of house abandonment (Dimitrijevi≤ 2000; 2008). Similarly to the structurally deposited red deer skull from Vlasac, these could have been curated over longer periods of time, but in a couple of cases provided a fairly reliable indication of the kill season. One such example comes from House 28 in the west- ernmost (upstream) periphery of the settlement, where a red deer skull with unshed antlers (very thin and quite unusual in their asymmetry) had been deposited on the floor (Dimitrijevi≤ 2000.Fig. 16; 2008.Fig. 7). The skull has been directly dated to a range 6206–5989 cal BC at 95% probability (OxA-16078), which corresponds with the construc- tion and use of the trapezoidal buildings, i.e. the phase identified as the Mesolithic-Neolithic Transfor- mation (Bori≤, Dimitrijevi≤ 2009). The skull was damaged during excavation, with only the antlers and frontal, temporal and occipital parts of the skull and the upper jaws remaining (Dimitrijevi≤ 2000. Fig. 17), while fish and gastropod remains were Becoming sedentary| The seasonality of food resource exploitation in the Mesolithic-Neolithic Danube Gorges 111 vi≤ 2000; Bori≤, Dimitrijevi≤ 2006; Ωivaljevi≤ in prep.). The context has not been AMS dated, but given that the deposition of faunal remains predat- ed the house construction, it can be concluded that the event(s) took place during an early settlement phase. The unity of the assemblage is seen in the large portions of the red deer and brown bear car- casses, which were probably butchered in situ. The red deer remains originated from a young individ- ual, given its milk dentition, unfused proximal and distal epiphyses of long bones and porous structure of the short bones. Its age has been determined on the basis of a left mandible (LV bb-30/2) with a 2nd and 3rd decidious molar, alveole for the 4th decidi- ous molar and an erupting 1st permanent molar (Di- mitrijevi≤ 2000.Fig. 12). This stage of dental devel- opment and wear indicate a four-month-old indivi- dual, suggesting that the kill season was in Septem- ber (Dimitrijevi≤ 2000; cf. Brown, Chap- man 1991; Carter 2006). If we assume that the whole faunal assemblage underneath House 31 accumulated over a short period, September would correspond with the start of the autumn migration of beluga and Rus- sian sturgeon (Tab. 4), slightly preceding the start of vyrezub migration, if migratory patterns of modern populations are taken into account. Another red deer mandible (LV bb-14/3) (Fig. 6) from an unspecified context origi- nated from a 13- to 15-month-old individ- ual, judging from the presence of 2nd, 3rd and 4th decidious molars with formed but unresorbed roots (cf. Brown, Chapman 1991). This specimen is indicative of a sum- mer kill event that took place between July and September. An autumn/winter kill is suggested in the case of a red deer left maxilla (LV 1074/5) found in the eastern part of the settlement (sq. a/11-14). The presence of both decidious 4th molar and the 1st permanent molar indicates a 12- to 16-month-old individual (cf. Habermehl 1985), captured between October and February. The same season has been determined in the case of red deer maxillae (LV 1296/1) found beneath the floor of House 19. Both left and right maxilla had mixed de- cidious/permanent dentition (D4, M1; and D3-D4, M1, respectively) (Fig. 7), suggesting they also orig- inated from a 12- to 16-month-old individual (cf. Habermehl 1985). In addition, vyrezub pharyngeal teeth were stuck to the right maxilla. The October- February time span corresponds well with the sea- son during which vyrezub migrate to rivers and over- winters, but precedes its spawning season (Tab. 4). The red deer maxilla with vyrezub teeth, as well as the aforementioned red deer skull from House 28 Fig. 5. Red deer skull with antlers (LV 261/1–2) deposited facing the floor of House 22 at Lepenski Vir; the kill took place in February-March. Photo from the archive of the Com- puter Documentation Centre, Faculty of Philosophy, Belgrade. Fig. 6. Red deer right mandible with milk molars (LV bb-14/3) from Lepenski Vir, originating from a 13– 15 month old individual, killed between July and September: a buccal; b lingual. with small fish bones stuck to it seem to embody quite literally the merging role of wild game and fish. The fish faunal assemblage from Lepenski Vir consisted mainly of cyprinid remains (of freshwater species and anadromous vyrezub), as well as catfish, huchen and a small number of Black Sea shad, pike and pikeperch (Sander lucioperca) bones, but also a significant amount of remains of migratory stur- geon. Having in mind their largely cartilaginous ske- leton and preservation bias affecting their remains (Brinkhuizen 1986; Bartosiewicz et al. 2008), it is remarkable that sturgeon constitute nearly 20% (in terms of NISP) of identified fish remains at Lepen- ski Vir (Ωivaljevi≤ in prep.); it is also highly signifi- cant that some of the sculpted boulders from this site bore a resemblance to sturgeon features (Rado- vanovi≤ 1997; Bori≤ 2005). At the same time, the Lepenski Vir assemblage exhibited the greatest di- versity of sturgeon species, including the remains of migratory beluga, Russian sturgeon, ship sturgeon, and stellate sturgeon, as well as those of freshwater sterlet (Acipenser ruthenus). The first species to enter the Danube is the large beluga, whose spring migration commences in late winter/early spring, reaching a peak in April and ending in late May/ June. Its autumn migration starts by late August, peaking in October/November. The Russian sturgeon starts its spring migration somewhat later than bel- uga (end of February/March), which peaks in April, and ends mid-May. The second migration starts in August/September, peaks in late September/mid-Oc- tober and ends by mid-November. The ship sturgeon migrates in spring and autumn, with autumn popu- lations remaining in the river until spawning, which takes place from March/April until June. The stellate sturgeon, the last species to enter the Danube, starts its spring migration in late April/ March, reaching a peak in May. Its autumn run begins by August and ends by September/mid-October (Tab. 4) (cf. Dinu 2010; Petrovi≤ 1998[1941]; Risti≤ 1977; Simonovi≤ 2001; Kottelat, Freyhof 2007; Bartosiewicz et al. 2008). Judging from interspecific variations in the migration start and peak dates of sturgeon species, migration pattern of vyrezub, as well as availabili- ty of freshwater fish, it might be hypothesised that fishing could have successfully taken place between late winter and late autumn, with particular inten- sity in spring and autumn. The remains of species active in winter (namely pike) are few, but the pos- sibility of smoking and drying fish (the hearths in particular could have been used for this purpose) and storing it for winter months should not be ex- cluded (cf. Bonsall 2008; Bori≤ 2002; 2007). On the basis of fish remains from AMS dated contexts from Lepenski Vir (cf. Whittle et al. 2002; Bonsall et al. 1997; 2008; Bori≤, Dimitrijevi≤ 2009; Bori≤ 2011), it was determined that fishing patterns remained relatively unchanged throughout the temporal se- quence, i.e. that the distribution and proportion of species is more or less the same in both Mesolithic and Transformation phase contexts at the site (Ωi- valjevi≤ in prep.). Although bird remains have been uncovered at Le- penski Vir (Bökönyi 1969; 1970; 1972; Dimitrijevi≤ 2008), only a single bird bone found between the superimposed floors of Houses 20 and 33 (context dated to 6231–6056 cal BC at 95% probability (OxA- 15998) (Bori≤, Dimitrijevi≤ 2009) has been iden- tified to the species level, originating from mallard (Bori≤, Dimitrijevi≤ 2006). As already noted, Anne Pike-Tay et alii (2004) state that the species is mi- gratory, but used to breed in Hungary; whereas Ja- vor Ra∏ajski and Andrei Kiss (2004) note that it is Vesna Dimitrijević, Ivana ?ivaljević and Sofija Stefanović 112 Fig. 7. Red deer left and right fragmented maxil- lae (LV 1296/1) found be- neath the floor of House 19 at Lepenski Vir, origi- nating from a 12–16 month old individual, captured between Octo- ber and February. A frag- ment of vyrezub left pha- ryngeal bone with a row of 4 preserved teeth is attached to the right max- illa. a a fragment of the right maxilla with the two milk molars (D3 and D4) and the first molar (M1) in eruption, lingual, attached vyrezub pharyngeal bone at the left; b same, buccal view, vyrezub teeth seen at the right side; c a fragment of the left maxilla with the last milk (D4) and the first permanent molar (M1), lingual; d same, buccal view. Becoming sedentary| The seasonality of food resource exploitation in the Mesolithic-Neolithic Danube Gorges 113 resident in Serbia, with a winter population increase due to migrant populations from the North of Europe. Padina The faunal assemblage from Padina, albeit entirely preserved, contained the fewest elements for a reli- able estimate of occupational seasons (Tab. 3). Si- milarly to Lepenski Vir, this was mainly due to the hand-collection of animal bone, particularly biased towards fragile deciduous teeth and fish and bird remains. The majority of elements indicative of sea- sonality included shed and unshed red deer and roe deer antlers from both Mesolithic and Transforma- tion phase contexts. These indicate kill seasons which occurred between September and February, deter- mined on the basis of unshed red deer antlers, and May and October, on the basis of unshed roe deer antlers. The occurrence of shed antlers of red and roe deer indicate occupation in February-March and October-November, respectively, assuming they were collected shortly after shedding. The only mandible from a juvenile animal (PAD 28.8.69/1) originated from a roe deer, and was found in a Mesolithic occu- pational context (cf. Bori≤ 2002.App. 3). Based on the presence of alveoli for D2-D3, D4 and a fragment of M1 (Fig. 8), it was determined that the animal was between four and eight months old (cf. Carter 2006), which suggested that it was captured between September and January. In terms of fish remains, a specific feature of the faunal assemblage from Padina (even in comparison with other assemblages collected by hand) is the absolute predominance of catfish (69.9% of all iden- tified fish remains, and 77.1% of all fish remains identified to species) and least species diversity (Tab. 4) (Ωivaljevi≤ in prep.). Moreover, judging from the species distribution in AMS dated contexts (cf. Whittle et al. 2002; Bori≤, Miracle 2004; Bori≤ 2011) and in contexts attributed to particular phas- es on the basis of stratigraphy (cf. Bori≤ 2002.App. 3), it was determined that catfish remains become exceptionally abundant in the Transformation phase of the settlement. This could suggest that Padina established itself as a specialised centre oriented to- wards catching catfish during this time (Ωivaljevi≤ in prep.). Catfish is most successfully caught during its spawning season (from May to July) and during summer months, when it feeds most intensely (Ri- sti≤ 1977; Simonovi≤ 2001; Kottelat, Freyhof 2007; Dinu 2010); however, given that the species is sta- tionary, and hardly moves from its respective habi- tat (Risti≤ 1977), it can be hypothesised that it was available for most of the year. During cold seasons, however, catfish populations would decrease in number, as the species requires a water temperature of at least 18°C to reproduce (cf. Bartosiewicz, Bon- sall 2004.Tab. 7). As already suggested, the harsh winter seasons and periods when the river was co- vered in ice could be overcome by storing fish by smoking and drying (cf. Bonsall 2008; Bori≤ 2002; 2007). In addition, the presence of anadromous sturgeons and vyrezub in the faunal assemblage sug- gests that freshwater fish exploitation at Padina was supplemented with fishing of seasonally available species, most notably in spring and autumn. Bird remains are few in the faunal assemblage from Padina, which is suggestive of opportunistic exploi- tation; however, it is probably also a consequence of the sampling bias. The faunal assemblage consisted of the remains of six resident and three migratory species, some of them available in the Danube Gor- ges area for fairly short and seasonally limited pe- riods of time (Tab. 5). Such is the case with the shell- duck (Tadorna tadorna), which is present only in March and September-October, and white pelican, present in October-November. The black-throated diver (Gavia arctica) is present in the area from No- vember to March (Ra∏ajski, Kiss 2004), whereas in Central Europe it migrates in spring and autumn (Cla- son 1980). As already noted, the numbers of some of the resident populations (such as cormorant) in- crease in winter (cf. Clason 1980; Ra∏ajski, Kiss 2004), which tentatively suggests they could have been exploited more frequently during this time. Discussion An important issue to be addressed here is whether permanent, year-round occupation can be distingui- shed from a series of repeated visits, of varying du- Fig. 8. Roe deer mandible with alveoli for milk mo- lars (D2-D3), last milk molar (D4) and a fragment of the first permanent molar (PAD 28.8. 69/1) from a Mesolithic occupational context at Padina. The animal was between 4–8 months old, suggesting the capture occurred between September and Janu- ary. Vesna Dimitrijević, Ivana ?ivaljević and Sofija Stefanović 114 ration, occurring at different seasons throughout the year? (cf. Whittle 2001; Conneller et al. 2012). This question, of course, remains very difficult to answer archaeologically. The patterns of food re- source exploitation at Vlasac, corroborated with archaeological evidence, could be indications of the first scenario. The intensity of occupation in the Late Mesolithic phase (c. 7400–6300/6200 cal BC) is evi- denced by several dug-out dwellings vaguely resem- bling the trapezoidal shape in plan, numerous stone- lined hearths which were constructed in the open or were originally incorporated into dwellings that left no trace in the archaeological record, over hundred buried individuals and an enormous assemblage of tools and animal bones (cf. Srejovi≤, Letica 1978; Nemeskéri 1978; Bökönyi 1978; Kozłowski, Koz- łowski 1982; Roksandi≤ 1999; 2000; Bori≤ et al. 2008; 2014). The faunal assemblage from the new 2006–2009 excavations of the site, which contained most elements suggestive of kill seasons (namely, erupting teeth of young animals), seems to indicate year-round occupation of the settlement. The exploi- tation patterns of red deer, the most important game animal, do not suggest any significant seasonal hia- tus. Similarly, wild boar and roe deer hunting does not seem restricted to a particular season. Although most elements utilised in this study indicated a rel- atively broad time span, those that provided most precise and temporally restricted seasonal estimates point to hunting events which took place in all sea- sons. The fishing activity is indicative of spring and autumn months, judging from the presence of ana- dromous vyrezub and various sturgeon species, but fishing at other times was certainly possible, given that freshwater species represented in the sample would have been available for longer periods of time. Moreover, the fish could have been stored for winter by smoking and drying. The hand-collected faunal assemblages from Lepen- ski Vir and Padina offered much less information for precise season determination, but tentative estimates do not point to a particular season of hunting. Fur- thermore, it can be suggested that resource exploita- tion patterns observed in the Late Mesolithic would have continued in the Transformation phase settle- ments (c. 6200–5900 cal BC). Several fairly precise season estimates obtained from specimens related to the construction and use of elaborate trapezoidal- base buildings at Lepenski Vir offer important in- sights into the life-cycles of particular buildings and, consequently, of the settlement as a whole. It is evi- dent that some of dwellings were abandoned at dif- ferent times of the year, while others remained in use; this feature is also suggested by the secondary position of some of the sculpted boulders. The signi- ficance of both hunting and fishing activities, which took place simultaneously for most of the year, is particularly illustrated by caches of mammal and fish bones stuck together and formed over a short period of time. It remains unclear to what extent the observed differences in preferences for fish species at Lepenski Vir and Padina would influence the na- ture of occupation of these sites; the latter oriented mostly towards catfish available for most of the year, and the former exhibiting greater species diversity and a significant amount of seasonably available sturgeon. Whereas the environment of Lepenski Vir and other sites would have provided substantial means for occupation lasting throughout the year, the exploitation of seasonally available fish could have been vital in (re)creating memories, events and specific temporal perspectives (Bori≤ 2002). Conclusion This study offers additional data supporting the hy- pothesis that a significant degree of sedentism in the Danube Gorges existed already in the Late Me- solithic, prior to, and independently of, the adoption of animal and plant husbandry. Furthermore, recent studies of other Mesolithic contexts in Europe pro- vide evidence of practices involving prolonged stays of human groups in certain locations; for example, the construction (involving a significant amount of time and effort) of substantial timber structures at Starr Car in Britain (Conneller et al. 2012) and large- scale food storage and fish fermentation, implying a delayed-return subsistence strategy, at Norje-Sun- nansund in Southern Scandinavia (Boethius 2016). Moreover, ‘full-scale’ sedentism commonly associated with food-producing communities could have also taken many different forms, including shifting culti- vation crops or herds, and varying levels of mobili- ty of individuals involved in such practices (Whittle 2001). These studies further problematise the rela- tionship of sedentism and subsistence strategies, and add to our understanding of the complexity and diversity of forager and food-producing lifestyle and residential practices. In the Danube Gorges, evidence of Early Mesolithic occupation is relatively scarce, but the presence of several burials and stone con- structions indicate a prolonged stay at riverine ter- races. The higher resolution of dates, architectural features and artefacts related to the Late Mesolithic occupancy signal that by this time these locations were a home to fairly sedentary populations prac- ticing an exclusively hunter-gatherer-fisher lifestyle. Becoming sedentary| The seasonality of food resource exploitation in the Mesolithic-Neolithic Danube Gorges 115 Their environment enabled the successful exploita- tion of wild game and fish for most, if not the whole, of the year. Therefore, it can be argued that the construction of later, Mesolithic-Neolithic Transformation phase set- tlements at Lepenski Vir and Padina took place in a context where continuous human occupation and relationship with particular locales had been long established. It can also be hypothesised that these settlements, with more elaborate and permanent dwellings, would have followed similar patterns of occupation. Although the changes observed in the Transformation phase largely coincide with the emergence of the first food-producing communities in the region (and contacts with distant communi- ties are evident already in the Late Mesolithic), cer- tain (but not all) elements of Neolithic lifestyles were incorporated only after “they made sense in local terms” (Bori≤ 2007). Most notably, animal husban- dry had fairly little impact on the economy and life- style of Upper Gorge communities, with the remains of the first domesticates appearing only after most of the trapezoidal buildings had been abandoned. It can be assumed then, that local traditions, estab- lished in a particular environment and involving locally available resources, merged with new cultur- al elements in the later parts of the sequence, played substantial roles in settlement practices in the Da- nube Gorges context. This paper is a result of the Project “BIRTH: Births, mothers and babies: prehistoric fertility in the Balkans between 10 000–5000 BC”, funded by the European Research Council (ERC) under the European Union’s Horizon 2020 research and innovation programme (Grant Agreement No. 640 557). We thank Du∏an Bo- ri≤ for the opportunity to study the faunal remains from the 2006–2009 excavations of Vlasac, Igor Aske- yev for his help with determining some of the fish bones, and Mihael Budja for his kind invitation to participate in the 22nd Neolithic Seminar and for the superb organisation of the conference. We would also like to thank two anonymous reviewers for their in- sightful and constructive comments on earlier drafts of this paper. ACKNOWLEDGEMENTS References Bartosiewicz L. 1989. Variability of tooth eruption in cat- tle. Acta Veterinaria Hungarica 37(4): 303–317. Bartosiewicz L., Bonsall C. 2004. Prehistoric fishing along the Danube. Antaeus 27: 253–272. 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ELEM EN T W IN TER SPR IN G SU M M ER A U TU M N R eference w here the age JA N FEB M A R A PR M A Y JU N JU L A U G SEP O C T N O V D EC stage has been defined V L 29\1 skull fragm ent w ith antlers Schm idt 1972 \ unshed antler (9)* Schm idt 1972 \ shed antler (31)* Schm idt 1972 V L 216\15 m axilla sin. (D 3, 4) C arter 2006 V L 145 x.5 P4 inf. dext. C arter 2006 V L 20 4\5 D 3 sup.sin. C arter 2006 R ed deer V L 20 9 x.1 P4 inf. dext.sin. C arter 2006 C ervus elaphus V L 224\6 D 2 inf.dext. C arter 2006 V L 237\4 I3, D i2, D i3 sin. & D i2, D i3, D c dext. H aberm ehl 1985 V L 264 x.2 D 3 sup.dext. C arter 2006 V L 286\3 M 2, M 3 inf. dext. C arter 2006 V L 30 6\24 P2 inf.sin. C arter 2006 V L 35\2 P4 inf.sin. C arter 2006 V L 66 x.2 P4 inf. dext. C arter 2006 V L 314 x.23 skull fragm ent w ith left antler Schm idt 1972 R oe deer \ unshed antler (3)* Schm idt 1972 C apreolus capreolus V L 51\1 D 3\4 sup.sin. C arter 2006 V L 285\7 D 2 sup.sin. C arter 2006 Fox V ulpes vulpes V L 222\22-23 D c sup.dext. & M 1 sup.dext. (germ ) H aberm ehl 1985 V L 133 x.2 m ax. sin. (D 4) C arter, M agnell 2007** W ild boar V L 237\5 D 3 sup. dext. C arter, M agnell 2007** Sus scrofa V L 282\3 D 2 sup.dext. C arter, M agnell 2007** V L 30 8 x.9 D 4 inf.sin. C arter, M agnell 2007 V L 242\1 M 2 inf.dext. C arter, M agnell 2007 Tab. 1. Ten tative kill season of m am m als at V lasac. D ark shades represen t the m ost precise estim ation of the season of capture, restricted to 1–2 m on ths. A ll elem en ts used for estim ation s of season ality origin ate from the faun al assem blage collected in 2006–2009, apart from elem en ts m arked w ith an asterisk (*) w hich w ere collected in 1970–1971. **The agein g of w ild boar m axillary teeth assum in g they follow the sam e developm en t schedule as m an dibular teeth. Vesna Dimitrijević, Ivana ?ivaljević and Sofija Stefanović 120 TA X O N IN V . N O . ELEM EN T W IN TER SPR IN G SU M M ER A U TU M N Reference w here the age JA N FEB M A R A PR M A Y JU N JU L A U G SEP O C T N O V D EC stage has been defined \ unshed antler (8) Schm idt 1972 \ shed antler (8) Schm idt 1972 LV 261\1-2 skull w ith shed antlers Schm idt 1972 R ed deer LV 10 74\5 m axilla sin. (D 4, M 1) H aberm ehl 1985 C ervus elaphus LV 1296\1 m axilla dext. (D 3-D 4, M 1) & sin. (D 4, M 1) H aberm ehl 1985 LV 273\4 m axilla dext. (D 3, P2-M 3) & sin. (D 3, P2- M 2) B row n, C hapm an 1991 LV bb-30 \2 m andibula sin. (D 2-D 3, alv. D 4, M 1 bud) C arter 2006 LV bb-14\13 m andibula sin. (D 2-D 4) B row n, C hapm an 1991 R oe deer \ unshed antler Schm idt 1972 C apreolus capreolus \ shed antler Schm idt 1972 Tab. 2. Ten tative kill season of m am m als at Lepen ski V ir. D ark shades represen t the m ost precise estim ation of the season of capture, restricted to 1–2 m on ths. TA X O N IN V . N O . ELEM EN T W IN TER SPR IN G SU M M ER A U TU M N R eference w here the age JA N FEB M A R A PR M A Y JU N JU L A U G SEP O C T N O V D EC stage has been defined R ed deer PA D 8.70 \279\1 unshed antler Schm idt 1972 C ervus elaphus \ shed antler (5) Schm idt 1972 R oe deer PA D 7.70 \140 \1 unshed antler Schm idt 1972 C apreolus capreolus PA D 8.69\80 \1 shed antler Schm idt 1972 PA D 28.8\69\1 m andibula sin. (alv. D 2-D 3, D 4, M 1) C arter 2006 Tab. 3. Ten tative kill season of m am m als at Padin a. Becoming sedentary| The seasonality of food resource exploitation in the Mesolithic-Neolithic Danube Gorges 121 TA X O N V L 20 0 6–20 0 9 LV 1968–1970 PA 1968–1970 W IN TER SPR IN G SU M M ER A U TU M N N ISP % N ISP % N ISP % JA N FEB M A R A PR M A Y JU N JU L A U G SEP O C T N O V D EC R ussian sturgeon A cipenser gueldenstaedtii 9 0 ,1 54 6,4 13 0 ,6 Ship sturgeon A cipenser nudiventris \ \ 4 0 ,5 \ \ Sterlet A cipenser ruthenus \ \ 9 1,1 1 0 ,0 Stellate sturgeon A cipenser stellatus 5 0 ,1 7 0 ,8 16 0 ,7 B eluga H uso huso 27 0 ,3 83 9,9 72 3,1 B lack Sea shad A losa im m aculata 92 1,1 1 0 ,1 \ \ C om m on carp C yprinus carpio 80 3 9,5 92 10 ,9 20 8 8,9 B ream A bram is bram a 22 0 ,3 \ \ \ \ D anube bleak A lburnus chalcoides 2 0 ,0 \ \ \ \ A sp A spius aspius 8 0 ,1 2 0 ,2 \ \ B elica Leucaspius delineatus 1 0 ,0 \ \ \ \ C hub Leuciscus cephalus \ \ 3 0 ,4 \ \ Ide Leuciscus idus 4 0 ,0 2 0 ,2 \ \ R azor fish Pelecus cultratus 21 0 ,2 1 0 ,1 \ \ V yrezub R utilus frisii 7320 86,4 257 30 ,5 162 6,9 Pigo R utilus pigus 2 0 ,0 1 0 ,1 \ \ R oach R utilus rutilus 1 0 ,0 \ \ \ \ R udd Scardinius erythrophthalm us 7 0 ,1 \ \ \ \ V im ba bream V im ba vim ba 4 0 ,0 1 0 ,1 \ \ W els catfish Silurus glanis 61 0 ,7 168 20 ,0 180 6 77,1 Pike Esox lucius 44 0 ,5 1 0 ,1 \ \ H uchen H ucho hucho 29 0 ,3 154 18,3 65 2,8 B lack Sea trout Salm o trutta labrax \ \ 1 0 ,1 \ \ Pikepearch Sander lucioperca 8 0 ,1 1 0 ,1 \ \ TO TA L 8470 10 0 842 10 0 2343 10 0 Tab. 4. Fish taxa iden tified to the species level from V lasac, Lepen ski V ir, an d Padin a expressed in N ISP frequen cies (after Ωivaljevi≤ in prep.) an d their sea- son al availability on the basis of m igration /spaw n in g season s, feedin g season s an d optim al w ater tem perature. Light shades – availability; dark shades – peak availability (after D inu 2010.Tab. 2; Bartosiew icz, Bonsall 2004.Tab. 7; Bartosiew icz et al.2008.Tab. 6; Petrovi≤ 1998 [1941]; R isti≤ 1977; Sim onovi≤ 2001; K ot- telat, Freyhof 2007). Vesna Dimitrijević, Ivana ?ivaljević and Sofija Stefanović 122 N ISP W IN TER SPR IN G SU M M ER A U TU M N TA X O N V LA SA C PA D IN A L. V IR 1970 –1971 20 0 6–20 0 9 1968–1970 1968–1970 JA N FEB M A R A PR M A Y JU N JU L A U G SEP O C T N O V D EC B lack-throated diver G avia arctica \ \ 1 \ W hite pelican Pelecanus cf. onocrotalus 3 \ 1 \ C orm orant Phalacrocorax carbo 3 \ 1 \ M ute sw an C ygnus olor \ \ 1 \ G reat w hite egret Egretta alba 2 \ \ \ M allard A nas platyrhynchos 2 \ \ 1 Teal A nas crecca 2 \ \ \ G rey-lag goose A nser anser \ \ 2 \ Ferruginous (|) duck A ythya nyroca (|) 1 \ \ \ Shell-duck Tadorna tadorna \ \ 1 \ B lack kite M ilvus m igrans 5 (4) \ \ \ Im perial eagle A quila heliaca 6 (16) 2 \ \ W hite-tailed eagle H aliaeëtus albicilla 27 (0 ) \ 8 \ Taw ny ow l Strix aluco 2 (1) 1 \ \ Jay G arrulus glandarius 1 \ \ \ M agpie Pica pica 1 \ \ \ R aven C orvus corax 4 1 2 \ R ook C orvus frugilegus \ \ 1 \ Fieldfare Turdus pilaris \ 2 \ \ TO TA L 59 (21) 6 18 1 Tab. 5. B ird taxa iden tified to the species level from V lasac (n um bers in paren thesis represen t the revision of the preserved bird faun al assem blage an alyzed by Bökönyi 1978, after D im itrijevi≤ et al. subm itted), Padin a (after Clason 1980), an d Lepen ski Vir (after Bori≤, D im itrijevi≤ 2006) expressed in N ISP frequen - cies,an d their season al availability on the basis of residen cy an d m igration pattern s (after Puzovi≤ 2000; R a∏ajski, K iss 2004; G ruba≠ et al. 2013; Clem ents et al. 2014).