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Post by Admin on Aug 30, 2021 23:25:45 GMT
Bell Beaker The earliest BB individuals occupy a similar position in PCA as CW individuals (Fig. 4B and fig. S7), suggesting a degree of genetic continuity. To explore the genetic origin of early BB individuals (Bohemia_BB_Early; mean date, >2400 BCE; n = 3), we modeled them as a two-way mixture between preceding and contemporaneous cultural groups. We found support for a local origin, although nonlocal alternatives cannot be ruled out (table S28). However, our Bohemia_BB_Early group consists of only three (female) individuals and is therefore likely limited in representativeness and resolution to discern source populations.
We find that late BB individuals (Bohemia_BB_Late; mean date, ≤2400 BCE; n = 56) carry significantly more Middle Eneolithic–like ancestry compared to Bohemia_BB_Early (table S29). To explore this genetic shift, we modeled the ancestry of Bohemia_BB_Late as a two-way mixture of Bohemia_BB_Early and local Middle Eneolithic sources (table S30), finding support for an additional ~20% local Middle Eneolithic–like ancestry in late compared to early BB.
We observe a closer phylogenetic relationship between the Y chromosome lineages found in early CW and BB than in either late CW or Yamnaya and BB. R1b-L151 is the most common Y-lineage among early CW males (6 of 11, 55%) and one branch ancestral to R1b-P312 (Fig. 4A), the dominant Y-lineage in BB (5). Although it is not possible to determine whether the P312 mutation(s) occurred in one of the early CW R1b-L151 males from Bohemia, we note that most Bohemian BB males are further derived at R1b-L2/S116 (R1b1a1a2b1), in contrast to BB males from England, several of whom are derived at R1b-L21(R1b1a1a2c1), showing that English and Bohemian BB males cannot be descendants of one another, but rather diversified in parallel. A scenario of R1b-P312 originating somewhere between Bohemia and England, possibly in the vicinity of the Rhine (66, 67), followed by an expansion northwest and east is compatible with our current understanding of the phylogeography of ancient R1b-L151–derived lineages.
EBA—Únětice culture The transition to the EBA in Bohemia is associated with a positive shift in the coordinates of PC2, relative to preceding late BBs (Fig. 4B, fig. S7, and table S31). Admixture f3 statistics are most negative when EHG (Eastern HG) or WSHG (West Siberian HG) are used as a second source in addition to the geographically and temporally proximal Bohemia_BB_Late (table S32), suggesting a northeastern contribution to Bohemia_Únětice_preClassical. To find a suitable proxy for a potential additional source population, we modeled Bohemia_Únětice_preClassical as a two-way mixture of local Bohemia_BB_Late and various sources more positive on PC2 (table S33). We reject mixture models involving Bohemia_BB_Late and Yamnaya (Samara, P = 5.3 × 10−10; Kalmykia, P = 5.8 × 10−10; Ukraine, P = 7.3 × 10−12; and Caucasus, P = 3.2 × 10−15) or Bohemia_BB_Late and CW (early, P = 1.1 × 10−4; late, P = 5.4 × 10−6). We fail to reject a two-way mixture model of 63.5% Bohemia_BB_Early and 36.5% Bohemia_BB_Late (P = 0.29), suggesting a large (63.5%) contribution from an early BB lineage, which was largely unsampled during the late BB phase (2400 to 2200 BCE), but represents a potential new lineage at the dawn of the Bronze Age. The Y-chromosomal data suggest an even larger turnover. A decrease of Y-lineage R1b-P312 from 100% (in late BB) to 20% (in preclassical Únětice) implies a minimum 80% influx of new Y-lineages at the onset of the EBA.
However, aware of the limited resolution of Bohemia_BB_Early (small sample size, low resolution, and large SEs), we explored alternative models for preclassical Únětice individuals. All model fits improve when Latvia_BA is included in the sources, resulting in two additional supported models (table S33). A three-way mixture of Bohemia_BB_Late, Bohemia_CW_Early, and Latvia_BA (P value of 0.086) not only supports a more conservative estimate of 47.7% population replacement but also accounts for the Y-chromosomal diversity found in preclassical Únětice, with R1b-P312 from Bohemia_BB_Late, R1b-U106 and I2 from Bohemia_CW_Early, and R1a-Z645 from Latvia_BA (Fig. 4A).
Although the geographic origin of this new ancestry cannot be precisely located, three observations offer clues. First, the Latvia_BA ancestry that improves all model fits (table S33) suggests an ultimate northeastern origin. Second, Y-haplogroup R1a-Z645 appears in Bohemia (and wider central Europe) for the first time at the beginning of the EBA, a lineage previously fixed in Baltic and common in Scandinavian CW males (23, 24), supporting a north/northeastern genetic contribution. Third, an Únětice genetic outlier (VLI051, male, Y-haplogroup R1a-Z645; table S34) resembles individuals from Bronze Age Latvia (Fig. 2D) (68), providing direct evidence for migrants from the northeast.
We also detect a genetic shift in the transition from preclassical to classical Únětice, reflected in the decrease in PC2 coordinates for Únětice individuals dated after ~2000 BCE (Fig. 4B and fig. S7) and confirmed using qpWave (table S35) and f4 statistics (table S36). Bohemia_Únětice_Classical can be modeled as a mixture of Bohemia_Únětice_preClassical and a local Eneolithic source (table S37). In contrast to the genetic shift between late BB and preclassical Únětice, the Y-lineage diversity remains similar throughout both Únětice phases, suggesting assimilation and subtler social changes.
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Post by Admin on Aug 31, 2021 21:23:10 GMT
DISCUSSION The high-resolution genetic time transect in Bohemia, allowing early and late phases of cultural groups to be divided and studied separately (e.g., CW, BB, and Únětice), elucidates several major processes before and after the arrival of steppe ancestry (Fig. 6). Our dense sampling allows detection of novel, important, and perhaps “unexpected” changes within cultural groups (e.g., CW and BB), if they are seen through a strict cultural-historical lens. Previous studies have largely been interpreted as revealing major migrations at the beginning and end of the Neolithic (i.e., periods where the incoming groups were genetically very distinct); however, our results reveal additional large genetic turnovers. By sampling consecutive and partially contemporaneous cultural groups, we show that the spread of Funnelbeaker and GAC (69, 70), as well as the origin of Únětice, involved large genetic shifts over short time periods, likely explained by migrations. Fig. 6 Schematic summary of the major processes that shaped the genetic and cultural diversity of Bohemia (red outline) over time. Arrows on maps indicate a general direction of influences rather than discrete routes of migration. We show that early CW were genetically exceptionally diverse, some resembling GAC and Yamnaya, with a few also falling outside of previously sampled central European Neolithic genetic diversity. Such a notably diverse signal is likely the result of the agglomeration of people from diverse cultural and linguistic backgrounds into an archaeologically similar but polyethnic or plural society. Important factors in ethnic identity include ancestry, history, ideology, and language (71, 72). The level of genetic differentiation (i.e., time since common ancestor) between early CW individuals with high and no steppe ancestry implies long biological isolation and hence different histories. The finding of GAC-like and Yamnaya-like genetic profiles in early CW suggests integration of people who came from ideologically diverse societies (i.e., neither GAC nor Yamnaya practiced strong gender differentiation in mortuary practices, unlike CW). It is likely that GAC and CW/Yamnaya individuals spoke different languages (3, 4, 43), meaning that early CW society in Bohemia encompassed people who had demonstrably different histories, likely originating from ideologically diverse cultures, who spoke different mother tongues. The assimilation process of individuals without steppe ancestry into early CW society was female-biased (43). However, finding females also among individuals with the highest amounts of steppe ancestry (3 of 5; Fig. 2B) suggests that they were also well represented among migrating CW individuals [in contrast to (43)] or perhaps assimilated from nearby Yamnaya groups (e.g., Hungary). Finding individuals without steppe ancestry in early CW contexts (n = 4) is more common than individuals with steppe ancestry in pre-CW contexts (e.g., GAC, n = 0). This pattern of asymmetric gene flow between the contemporaneous GAC and CW may reflect newcomers (CW groups) having more benefit from incorporating people with important local knowledge (i.e., from pre-CW cultural contexts) into their communities. The archaeological record shows continuity of such knowledge (e.g., pottery production and lithic raw materials) in several regions (22, 67, 73). Vliněves is crucial for elucidating interactions between individuals with high and no steppe ancestry. This site yields the earliest dated CW (VLI076, 3018 to 2901 BCE) who is also genetically most differentiated from pre-CW individuals, while 20% (3 of 15) of the sampled early CW from Vliněves had no steppe ancestry. Intriguingly, we observe no archaeological differences between CW graves of individuals with and without steppe ancestry from two sites (Vliněves and Stadice; see the Supplementary Materials), suggesting full integration of genetically, and likely ethnically, diverse individuals within the same archaeological culture. Finding Latvia_MN-like ancestry in early CW, in conjunction with the absence of Y-chromosomal sharing between early CW and Yamnaya males, suggests a limited or indirect role of known Yamnaya in the origin and spread of CW to central Europe. Our results allude to either a northeast European Eneolithic forest steppe contribution to early CW or a hitherto unsampled steppe population who carried excess Latvia_MN-like ancestry, a scenario that is less likely given the high degree of genetic homogeneity among 3000-BCE steppe groups [e.g., Yamnaya and Afanasievo separated by ~2500 km but genetically almost indistinguishable (4, 61)]. As much of 4000- to 2500-BCE (north)eastern Europe remains unsampled, inferring the precise geographic origin of early CW individuals remains elusive. Since social kinship systems influence patterns of genetic diversity (13, 42, 48, 74), it is likely that several different kin systems existed in third millennium BCE central Europe. The highly diverse genetic profiles (both nuclear and Y-chromosomal) of early CW suggest a different social organization to late CW and BB, whose Y chromosome pattern is indicative of strict patrilineality. This suggests that different cultural groups, in addition to using various forms of material culture and mortuary practices, likely also conformed to different ideologies as expressed in their mating pattern and/or social organization. This is supported by the finding of completely nonoverlapping Y chromosome variation between the partially contemporaneous late CW and BB, indicating a large degree of paternal mating isolation between these two groups, even when found at the same site (e.g., Vliněves). The onset of the preclassical Únětice was accompanied by a ≥40% nuclear and ≥80% Y-chromosomal contribution ultimately originating from the northeast and breaking down the gender-differentiated mortuary practices and strict patrilineality of late CW and BB. This was neither evident in the burial customs nor in the material culture but could represent the underlying connection to the Baltics, the ultimate source of EBA amber in Bohemia associated with the later emerging Amber Road (75–77). Therefore, our results suggest two main periods (early CW and early Únětice) of genetic influence from the northeast, much of which remains unsampled in the European archaeogenetic record (e.g., Belarus). Our results reveal a complex and highly dynamic history of Neolithic to EBA central Europe, during which migration and the movement of people facilitated abrupt genetic and social changes. Large-scale demic expansions occurred multiple times before and after the appearance of steppe ancestry in Europe. Early CW society was diverse and emerged amid a strong cultural and genetic transition, involving males and females of diverse origins and likely ethnicities. Genetic shifts occurred within CW, BB, and EBA societies despite continuity in material culture. Cultural affiliations played a major role in third millennium BCE social behaviors, which ultimately changed with the influx of new people over time. Although the impact of social processes is observable in patterns of genetic diversity, further interdisciplinary research is required to characterize the drivers of these changes, both at a micro- and macro-regional level.
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Post by Admin on Sept 1, 2021 2:27:22 GMT
MATERIALS AND METHODS Processing sites for the newly reported individuals Most (186 of 206, 90.2%) of the newly reported individuals were entirely processed at the Max Planck Institute for the Science of Human History in Jena, Germany, and the full details of sampling and ancient DNA wet laboratory work and bioinformatic processing are summarized in what follows. The individuals from the site Makotřasy were initially sampled and processed into powder at the University of Vienna, followed by subsequent laboratory work and bioinformatic and ancient DNA analysis at Harvard Medical School following previously described protocols (61). Sampling In total, 389 pars petrosa, teeth, and bones from 261 individuals were processed as part of this study. Upon introduction into the clean room facilities at the Max Planck Institute for the Science of Human History in Jena, Germany, all samples were wiped with 5% bleach and ultraviolet (UV) irradiated for 20 min on each side. Teeth were sampled by removing the crown followed by drilling into the pulp chamber to create bone powder. Pars petrosa were sampled by drilling into their dense region (78) to create bone powder. Between 50 and 100 mg of resulting bone powder from each sample were collected in different 2-ml Biopure tubes (one tube per sample) and used in subsequent DNA extraction. DNA extraction One milliliter of extraction buffer [containing 0.9 ml of 0.5 M EDTA, 0.025 ml of proteinase K (0.25 mg/ml), and 0.075 ml of UV high-performance liquid chromatography (HPLC) water] was added to Biopure tubes containing bone powder. Biopure tubes were then sealed with Parafilm and incubated overnight on a rotating wheel at 37°C. After incubation, Biopure tubes were spun for 2 min at 18,500 relative centrifugal force (rcf), separating the soluble from insoluble parts of the resulting solution. The soluble part was transferred to a 50-ml falcon tube containing 10 ml of binding buffer and 400 μl of sodium acetate (3 M, pH 5.2). Resulting mixture was transferred to a high pure extender assembly (HPEA) falcon tube, which was centrifuged at 1500 rpm in a 50-ml Thermo Fisher Scientific TX-400 Swinging Bucket Rotor for 8 min. The column from each HPEA tube was removed and inserted into a fresh collection tube and centrifuged at 18,500 rcf for 2 min. A total of 450 μl of wash buffer from the high pure viral nucleic acid kit (HPVNAK) was added to each column, which was then centrifuged at 8000 rcf for 1 min. Columns were then removed and placed into new collection tubes. Another round of washing was performed whereby 450 μl of wash buffer from the HPVNAK was added to each column and centrifuged at 8000 rcf for 1 min. Columns containing washed DNA were then transferred to 1.5-ml siliconized tubes. Fifty microliters of TET (tris-EDTA + Tween 20) buffer were added to the center of columns, and the columns were then incubated at room temperature for 3 min and centrifuged at 18,500 rcf for 1 min. Another 50 μl of TET buffer was added to the center of columns, after which they were centrifuged once more at 18,500 rcf for 1 min. The resulting 100 μl of DNA extracts was stored at −20°C until further processing. DNA libraries and in-solution capture Twenty-five microliters of DNA extract was used for the construction of (in most cases) double-stranded uracil DNA glycosylase (UDG) half-treated DNA libraries. UDG repair was performed by adding DNA extract to a 25-μl mastermix containing 6 μl of 10× Buffer Tango, 6 μl of 10 mM adenosine 5′-triphosphate, 0.5 μl of bovine serum albumin (BSA; 20 mg/ml), 0.2 μl of 25 mM each deoxynucleoside triphosphate (dNTP), 3.6 μl of 1-U USER enzyme, and 8.7 μl of UV HPLC water. Resulting mixture was incubated at 37°C for 30 min followed by 12°C for 1 min. Inhibition of UDG treatment was achieved through the addition of 3.6 μl of 2-U uracil glycosylase inhibitor (UGI) to each tube followed by incubation at 37°C for 30 min and again at 12°C for 1 min. Blunt-end repair was performed by adding 3 μl of 10-U T4 polynucleotide kinase and 1.65 μl of 3-U T4 DNA polymerase and incubating the resulting mixture at 25°C for 20 min and then at 12°C for 10 min. Blunt-end repaired mixture was purified using a MinElute kit and eluted in 20 μl of elution buffer (EB) containing 0.05% Tween. Illumina adapters were ligated onto DNA molecules through the mixture of 18 μl of eluate from the previous step with 20 μl of 2× Quick Ligase Buffer, 1 μl of 10 μM Adapter Mix, and 1 μl of 5-U Quick Ligase. Resulting mixture was incubated at 22°C for 20 min followed by purification with a MinElute kit and elution in 22 μl of EB containing 0.05% Tween. Adapter fill in reaction was performed by adding 20 μl of eluate from the previous step to 4 μl of 10× isothermal buffer, 0.2 μl of 25 mM each dNTP, 2 μl of 8-U Bst 2.0 polymerase, and 13.8 μl of UV HPLC water, followed by incubation at 37°C for 30 min and 80°C for 10 min. Resulting libraries were stored at −20°C until further processing. Unique library-specific indexes were added to the 5′ and 3′ ends of molecules in each library through an indexing polymerase chain reaction (PCR). Each library was split into four separate indexing PCR reactions, which were carried out using 10 μl of 10× Pfu Turbo buffer, 1.5 μl of BSA (20 mg/ml), 1 μl of 25 mM each dNTP, 1 μl of 2.5-U Pfu Turbo polymerase, 73.5 μl of UV HPLC water, 2 μl of 10 μM P5 index, 2 μl of 10 μM P7 index, and 9 μl of DNA library. Amplification was achieved through an initial denaturation at 95°C for 2 min, followed by 10 cycles of 95°C for 30 s, 58°C for 30 s, and 72°C for 1 min, followed by 72°C for 10 min. Resulting indexed libraries of the same sample were pooled and purified using a MinElute purification kit. Purified libraries were quantified using quantitative PCR and amplified to 1013 copies. Amplified libraries were shallow shotgun sequenced (~5 million reads) on an Illumina HiSeq or NextSeq platform to estimate the general human DNA content, presence of ancient DNA damage, and mitochondrial:nuclear coverage ratio. Libraries with >0.1% endogenous human DNA and >5% C-to-T misincorporations at the 5′ end were chosen for 1240k capture (8) and mitochondrial DNA (mtDNA) capture. In cases where more than one library from the same individual satisfied the criteria for capture, the better quality (higher endogenous DNA content) library was used for 1240k and mtDNA capture. Sequencing Postcapture libraries were single-end (75 cycles) or paired-end sequenced (2 × 50 or 2 × 75) on HiSeq or NextSeq Illumina platforms to a depth of 20 to 50 million reads per library. Resulting sequence data were processed through EAGER (v1.92.38) (79). Illumina adapters were removed using AdapterRemoval (v2.2.0) (80), and in case of paired-end sequencing, corresponding reads from the same template molecule with a minimum of 11 base pairs (bp) of overlap were merged. Fastq files of merged and unmerged reads were concatenated, and reads shorter than 30 bp were discarded. Processed reads were mapped to the human reference genome (hg19) using BWA-aln and BWA-samse (v0.7.12) (81) applying maxdiff (-n) 0.01 and seeding turned off (-l 10000). Resulting bam files were sorted, and duplicate reads were removed using DeDup (v0.12.1) (https://github.com/apeltzer/DeDup). Damageprofiler (v0.3.10) (https://github.com/Integrative-Transcriptomics/DamageProfiler) was used to calculate rates of misincorporation in read termini of DNA fragments in our captured libraries. BAM files had the last three bases from both 5′ and 3′ ends of reads and corresponding base quality scores masked for downstream analyses (82). Sex determination and authentication The genetic sex of each sample (bam file) was determined by calculating the normalized mean coverage on the X (mean X coverage/mean autosome coverage) and Y (mean Y coverage/mean autosomal coverage) chromosomes (83). Samples with normalized mean Y coverage values greater than 0.2 were assigned male. Contamination was estimated in males by calculating the rate of heterozygosity on their X chromosome (84). In addition, we used Schmutzi to estimate the mitochondrial contamination in all libraries (85). Schmutzi was run on BAM files resulting from mapping 1240K capture sequencing data to the human mitochondrial reference genome. In cases where 1240k data were not enough to give an mtDNA contamination, we ran Schmutzi on the mtDNA capture data mapped to the human mitochondrial reference genome. Genotyping We used SAMtools (v1.3) (86) mpileup and pileupCaller from the sequenceTools (v1.4.0.2) package (https://github.com/stschiff/sequenceTools) to call pseudo diploid genotypes by sampling a random high-quality allele (base quality, ≥30; mapping quality, ≥30) from each of the 1240k sites (8). Newly generated genotype data for this study were then merged to a compiled dataset of previously published ancient and modern worldwide populations (https://reich.hms.harvard.edu/allen-ancient-dna-resource-aadr-downloadable-genotypes-present-day-and-ancient-dna-data) (v42.2) using mergeit (v2450) from the EIGENSOFT package (https://github.com/DReichLab/EIG). Mitochondrial and Y chromosome haplogroups Mitochondrial haplogroups were called by mapping 1240k or mtDNA capture data to the human mitochondrial reference genome followed by creating pileups at each position (map quality and base quality filter of 30) and calling the most frequent base at each position. Resulting genotype information was converted to fasta files, and haplogroups were called using haplofind (87). Y chromosome haplogroups were called by mapping 1240k capture data to the whole human reference genome (hg19) followed by visual inspection of ancestral/derived alleles (after map quality and base quality filter of 30) at ISOGG (v15.58 April 2020) sites. Principal components analysis PCA was conducted using smartpca (v1600) from the Eigensoft package (https://github.com/DReichLab/EIG). Principal components were calculated on the genotype data of modern West Eurasian individuals (table S7) (88–90). Ancient individuals were projected (lsqproject: YES) onto the axes calculated from modern individuals. “shrinkmode: YES” was used to account for artificial stretching of principal component axes between projected (ancient) individuals and modern individuals. Fst values were also calculated in smartpca using “fsthiprecision: YES” and “inbreed: YES” parameters. Ancestry decomposition and admixture modeling F statistics, qpWave, and qpAdm runs were conducted in admixr v0.7.1 (91), a wrapper program around ADMIXTOOLS (88). Selection of outgroups for each analysis is indicated in the corresponding Supplementary Table. Linear modeling of pre-CW HG ancestry (Fig. 3A) was performed using segmented linear regression as implemented in R using the segmented function for v.1.2-0 of the segmented library (92). To select the optimal number of breakpoints, we compared Akaike’s information criterion (AIC) for models with between zero and four breakpoints. The AIC is a score that considers how well a model fits the data while simultaneously penalizing models with additional parameters. In this way, model fit must be significantly improved for a more complicated model with additional parameters to be accepted over a simpler, nested model. A linear regression model with one breakpoint was found to have the minimum AIC and hence was selected (93). DATES v753 (61) was used to estimate length distributions of ancestry tracts and infer admixture dates between Anatolia_Neolithic and WHG (here, Loschbour+Körös_HG+Germany_BDB). Parameters binsize 0.001, maxdis 1, seed 77, jackknife YES, qbin 10, runfit YES, afffit YES, lovalfit 0.45, minparentcount 1, and checkmap YES were used. Y haplogroup frequency simulations To investigate the process of Y-haplogroup inheritance in early and late CW groups, we simulated 106 realizations, assuming a generational time of 25 years, and analyzed the results using approximate Bayesian computation (ABC). For the ith realization, we assumed a constant population size of Ni ~ U(102,104), with a starting a proportion of R1a-M417(xZ645) of pi ~ TN(0, 1)(0.27,0.134) from a truncated normal distribution based on the observed proportion of R1a-M417(xZ645) of 3 of 11 (0.27). For each simulation, we also included a selection coefficient denoted si ~ U(−1,1). Under random mating, for generation j + 1, let the number of a male offspring carrying R1a-M417(xZ645) be Xij+1 ~ B(Ni, wj), where wj = Xj−1/Nj−1. However, if one includes a selection coefficient, then wj = min(1,(1 + si)Xj−1/Nj−1). Hence, one may interpret sj as the average increase in the proportion of male offspring that R1a-M417(xZ645) individuals were having over this period. We then compared our observed number of per-generation R1a-M417(xZ645) to our simulated realizations using the rejection method and keeping the top closest 0.05% realizations (selected via cross-validation) to form samples from the joint posterior distributions for our simulation parameters. All ABC and cross-validation analyses were performed in R using the abc package (94). Supplementary Materials for Dynamic changes in genomic and social structures in third millennium BCE central Europe www.science.org/action/downloadSupplement?doi=10.1126%2Fsciadv.abi6941&file=sciadv.abi6941_SM.pdf
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Post by Admin on Sept 1, 2021 21:45:06 GMT
Archaeological background While this study is devoted primarily to archaeogenetic data it is important to briefly summarise the archaeological background and context of the presented datasets and research questions, namely in the „old fashioned“ and maybe „long-outdated“ (38) but still broadly accepted culture-historical way of “archaeological cultures“ (Table S38, Fig. 1; see the last handbooks to Bohemian prehistory (49, 50, 59)), by understanding them actually rather as “archaeological units of classification” (mainly of artefact styles, burial practices etc.) than in the sense of recently rightly criticised „distinct groups of people“ (21, 33, 37, 38, 40, 95, 96).
The region of focus concerns the northern part of Bohemia, the basins of the Elbe, lower Vltava and Ohře rivers and the Bohemian part of the Ore Mountains. South and west Bohemia were not settled densely before the EBA. Before the Neolithic, these mainly forested regions at higher elevations were occupied by late Mesolithic hunter-gatherer groups, who may have persisted for some time during the Eneolithic (97). The Bohemian Stone Age prehistory is divided into two basic epochs: the Neolithic (ca. 5400–4400 BC) and Eneolithic (ca. 4400–2200 BC). The Neolithic is represented by the Linear Pottery (LBK, in Bohemia ca. 5400/5300–5000 BC) and Stroked Pottery cultures (STK, ca. 5000–4400 BC). There is broad consensus that the STK was derived from the LBK, without influence from outside (49).
The emergence of the Lengyel culture (ca. 4400–4200 BCE) (49) is regarded as a culture-historical turning point and marks the beginning of the Eneolithic in Bohemia (50) triggered by the arrival of a new population from the southeast (Moravia, Austria, Pannonia, southwest Slovakia). The Jordanów culture (ca. 4200– 3900 BC) is also included in the initial proto-Eneolithic period. Although culturally tied to the preceding Lengyel development, elements from the western Michelsberg culture are strongly manifested in the later phase. The status of the Michelsberg culture in prehistoric Bohemia is unclear, as Bohemia is on the boundary of two cultural traditions/phenomenons, the eastern Lengyel and western Michelsberg. Consequently, some scholars considered Michelsberg an autonomous entity, others a foreign influence into local Jordanów and older Funnel Beaker (Baalberge) culture (98, 99). From Jordanów/Michelsberg contexts exist first evidence of burials under barrows (Březno u Loun (100)), assumed also for the Funnel Beaker period and later on a mass scale for the CW and BB (50), alternatively for the EBA (101).
The Early Eneolithic (ca. 3800–3400 BC) is represented by the Funnel Beaker culture (Baalberge, incl. Siřem-stage). More than one hundred single inhumation burials in a crouched position and tens of burials in settlement features are recorded. The single graves with skeletons in a crouched position are characteristic since neolithic (LBK, STK) and as such for the entire Bohemian Eneolithic and EBA. Collective graves, which are typical for the Funnel Beaker in northern Europe, are absent in Bohemia completely.
The Middle Eneolithic (ca. 3400–2800 BC) was a period of cultures associated with the Baden cultural complex. The earliest stage of Baden in Bohemia (Boleráz) is thought to present a new population from the core of the Baden cultural complex in Carpathian Basin (102). In the following horizon, the late Funnel Beaker culture (Salzmünde (103)) is replaced by the classic Baden culture, from which the local post-Baden cultures develop: Řivnáč in central and northwest Bohemia, Bošáca in east Bohemia and Cham in west Bohemia (all ca. 3100–2800 BC). Inhumation graves during this period were quite rare (e.g. Holubice in this study) and the available anthropological material comes mainly from settlement features (sunken pits, semi-sunken huts etc.)
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Post by Admin on Sept 2, 2021 20:06:59 GMT
The Globular Amphora culture (GAC) extended into Bohemia as a new entity during the final Middle Eneolithic and its bearers are unanimously regarded as newcomers from the north. The GAC was partially contemporaneous with post-Baden Řivnáč and Cham cultures (GAC pottery was repeatedly found in settlements of both) (56) and is manifested by few burials of individuals in a crouched position. Regarding the possible coexistence of Řivnáč and GAC in Bohemia two possible scenarios were discussed. Firstly, the contemporaneous occupation by exploitation of different territories by more or less complete replacement of the Řivnáč settlement by the GAC in the late phase, secondly infiltration of GAC-people into the Řivnáč society (56, 104).
A distinct turning point in cultural development was the emergence of Late Eneolithic Beaker phenomena: Corded Ware (CW; ca. 2900/2800–2400 BC) and Bell Beaker (BB; ca. 2500–2200 BC). Both had a large geographic distribution in Europe, with the CW in central and NE Europe and BB in central, north- and southwestern and southern Europe. The CW in Bohemia is almost exclusively limited to grave finds with skeletons in a crouched position in W-E orientation with females on their left side, and males on their right side. While the number of investigated graves is one of the highest in Bohemian prehistory (ca. 1,500 graves), human skeletal material has not been preserved in all of them. Views on the origin of the CW differed greatly, from migration models (57, 105) to a purely autochthonous emergence (106), as did opinions on the subsistence, which ranged from a culture of settled farmers (107), to a pastoral nomadic character (108). The CW in Bohemia was not uniform over time, and three phases can be distinguished archaeologically: early (A-horizon, Kalbsrieth-type graves), middle (“Fischgrätenbecherhorizont”) and late (local Bohemian Corded Ware) – material groups 1 – 3 after M. Buchvaldek (109).
The Bell Beaker phenomenon (BB) in Bohemia is represented by hundreds of documented inhumation and cremation burials (ca 10 %). The inhumation ritual stands in contrast to the Corded Ware with males mostly in a left-crouched position, and females mainly in a right-crouched position, in N-S orientation. Various interpretations exist about the origin of the BB in Bohemia, both allochthonous (Iberian Peninsula Northern Africa, Lower Rhine Region, etc.) and autochthonous, with advocates of both theories in Czech archaeology (58, 110, 111). A typo-chronology of BB should be compiled from graves containing decorated beakers (early stage) towards graves with so-called “associated pottery” – late stage. In Bohemia, this so-called “associated pottery” (“Begleitkeramik”) is very similar to the pottery of the early phase of the EBA Únětice culture, which has been interpreted as evidence of continuity in material culture between the two.
The central European EBA is characterised by the so-called Únětice culture, mostly known from thousands of inhumation graves in a N-S-oriented, right-crouched position facing east and with no apparent gender differentiation in orientation (unlike the CW and BB). Bohemia can be considered its core area. Traditionally it is separated into two main parts: early (proto-Únětice and pre-classic phases) and late (classic to post-classic) phases after ~2000 BCE (59, 112, 113). The late (classical) phase is characterised by large hoard finds, typical Únětice cups, eyelet pins (Ösenkopfnadeln) and large cemeteries with inhumation burials rich in bronze artefacts, amber and gold jewellery and other exotics (60, 75, 77, 114– 117). There is no continuity at many cemetery sites from the early to the late phase. Early Únětice grave groups are smaller (mostly less than 10–15 graves), graves contain almost exclusively vessels, and only rarely copper wire artefacts.
The only one Middle Bronze Age (MBA) individual which we have incorporated in our study is that from the only one burial of this age from the important site Vliněves, grave 504 (VLI053), containing female skeleton in age of 50+ years buried with two typical MBA bronze pins. In the qpAdm modelling we group this skeleton with Bohemia_Unetice_Classical samples.
Table S38. Chronological framework of the periods and archaeological cultures discussed in the text. Period Archaeological culture Phase cal. BC N e o l i t h i c Linear Pottery (LBK; Linearbandkeramik) 5400/5300-5000/4900 Stroked Pottery (STK; Stichbandkeramik) 5000/4900-4400/4300 E n e o l i t h i c Lengyel 4400/4300-4300/4200 Jordanów / early Michelsberg 4300/4200-3900/3800 late Michelsberg / Funnel Beaker 3900/3800-3500/3400 Baden 3500/3400-3200/3100 Řivnáč / Cham / Bošáca 3200/3100-2900/2800 Globular Amphora 3000/2900-2900/2800 Corded Ware 2900/2800-2500/2400 Bell Beaker 2500/2400-2200/2100 E B A Únětice (Aunjetitz) early 2300/2200-2000/1950 late 2000/1950-1750/1700
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