| Literature DB >> 30963881 |
Lucy J E Cramp1, Jonathan Ethier2, Dushka Urem-Kotsou3, Clive Bonsall4, Dušan Borić5, Adina Boroneanţ6, Richard P Evershed7, Slaviša Perić8, Mélanie Roffet-Salque7, Helen L Whelton7, Maria Ivanova2.
Abstract
The spread of early farming across Europe from its origins in Southwest Asia was a culturally transformative process which took place over millennia. Within regions, the pace of the transition was probably related to the particular climatic and environmental conditions encountered, as well as the nature of localized hunter-gatherer and farmer interactions. The establishment of farming in the interior of the Balkans represents the first movement of Southwest Asian livestock beyond their natural climatic range, and widespread evidence now exists for early pottery being used extensively for dairying. However, pottery lipid residues from sites in the Iron Gates region of the Danube in the northern Balkans show that here, Neolithic pottery was being used predominantly for processing aquatic resources. This stands out not only within the surrounding region but also contrasts markedly with Neolithic pottery use across wider Europe. These findings provide evidence for the strategic diversity within the wider cultural and economic practices during the Neolithic, with this exceptional environmental and cultural setting offering alternative opportunities despite the dominance of farming in the wider region.Entities:
Keywords: aquatic; early farmer; lipid biomarkers; neolithic; organic residues; pottery
Mesh:
Year: 2019 PMID: 30963881 PMCID: PMC6367183 DOI: 10.1098/rspb.2018.2347
Source DB: PubMed Journal: Proc Biol Sci ISSN: 0962-8452 Impact factor: 5.349
Figure 1.(a) Map of the Iron Gates region showing the location of important Mesolithic and Neolithic sites, including those investigated here. (b,c) The modern landscape of the gorges and downstream area, respectively.
Figure 3.(a) Summary of archaeozoological assemblages from Vlasac [52,53], Lepenski Vir [34] and Schela Cladovei [33] based on NISP. Wild mammal data may include antler as this was not consistently quantified separately in the original reports. (b) Plot of δ13C16:0 against Δ13C (δ13C18:0–δ13C16:0) values, showing (red circles and stars) the data from the five sites investigated from the Iron Gates region (n = 45). By contrast, the grey circles show the stable isotope values from Neolithic pottery residues investigated from the northern and southern Balkans and Carpathian Basin, published in [6]; (n = 64). No aquatic biomarkers were detected in the lipid residues in pottery from the northern and southern Balkans. The ranges show the mean ± 1 s.d. from a database of reference values published in [49] (terrestrial fats); aquatic ranges as in figure 2.
Figure 2.Scatter plot of δ13C16:0 values against δ13C18:0 values from Neolithic pottery residues from the Iron Gates region (a–e; n = 45) and the Carpathian Basin/northern and southern Balkans (f; n = 64; *Data from [6]). Datapoints shown as red stars indicate where APAAs and DHFAs of carbon chain length ≧ C20 were also observed in the residue. Coloured ellipses are 1σ confidence ellipses derived from modern reference datasets. Reference fats are from [12,46,50], with additional new freshwater and migratory fish data from the Severn Estuary, UK and the Irish Sea (eels and salmon). Terrestrial and freshwater modern fats have been corrected for the contribution of post-industrial carbon (+1.3‰ [51]).
Figure 4.(a) Pie charts spanning distribution of sites from which organic residue analysis was undertaken, showing proportions of pottery lipids classified as ruminant (blue; Δ13C < −0.3‰) or non-ruminant (orange; Δ13C ≧ −0.3‰). Numbers in brackets denote the percentage of sherds containing aquatic biomarkers, where applicable. A—northwest Anatolia, Neolithic (seventh mill. BC), n = 65 [1]; B—Yenikapı, Neolithic (mid-seventh to late sixth mill. BC), n = 12 [4]; C—northern Greece, Early–Middle Neolithic (mid-seventh to mid-sixth mill. BC), n = 100 [5]; D—southern Balkans, Karanovo I (early sixth mill. BC), n = 24 [6]; E—northern Balkans, Starčevo (late seventh to early sixth mill. BC), n = 18 [6]; F—Iron Gates, Starčevo and Criş (early sixth mill. BC), n = 45 (this paper); G—Carpathian Basin, Starčevo (early sixth mill. BC), n = 22 [6,7]; H—Central Mediterranean, Impressa/Early Neolithic (sixth to fifth mill. BC), n = 29 [8]; I—Western Mediterranean, Impressa/Cardial (sixth mill. BC), n = 43 [8]; J—Poland, LBK (late sixth to early fifth mill. BC), n = 67 [9]; K—Germany, LBK (mid- to late sixth mill. BC), n = 25 [10]; L—Lithuania, Globular Amphora Culture and Rzucewo (late fourth to mid-third mill. BC), n = 18 [70]; M—southern Scandinavia, TRB (fourth mill. BC), n = 56 [15]; N—southern Finland, Corded Ware (third mill. BC), n = 7 [14]; O—Channel Isles, Cerny/Early Castellic, Le Pinacle/VSG (fifth mill. BC), n = 8 [13]; P—southern Britain, Early Neolithic (fourth mill. BC), n = 165 [12]; Q—northern Britain, Carinated Bowl/Unstan/Early Grooved Ware (late fifth to fourth mill. BC), n = 73 [13]; R—Northern and Western Isles of Scotland, Hebridean/Unstan/Early Grooved Ware (mid–late fourth mill. BC), n = 43 [13]; S—Isle of Man, Ronaldsway (late fifth to mid-fourth mill. BC), n = 10 [13]; T—Island of Ireland, Carinated Bowl (late fifth–fourth mill. BC), n = 106 [68]. Plot (b) Scatter plot of compound-specific isotope values of δ13C16:0 values plotted against Δ13C (δ13C18:0–δ13C16:0), showing data from this paper (red), the Balkans and Carpathian Basin [6] (grey) and Early–Middle Neolithic pottery from Europe (black; all other references above, except [4] not plotted). Ranges shown are as for figure 3. Total no. data points included = 904.