Post by Admin on Jul 18, 2024 3:59:31 GMT
Insights into Artificial Cranial Deformations (ACD) from aDNA
Within our dataset, 17 individuals from Samtavro, Samshvilde, Nedzikhi, and Tserovani had artificially elongated skulls. Artificial Cranial Deformations (ACD), a form of skull modification, has occurred independently throughout the world and as early as the Early Neolithic in Southwest Asia, where it is thought to have been widespread 37,38. In Georgia, the earliest documented ACD cases date to the Late Bronze Age - Early Iron Age transition 39, but the frequency substantially increased in the Mtskheta area during the Migration Period of Europe (4th - 7th century AD) 40. In particular, craniological material from early medieval Georgia suggests a frequency of c. 20% (126/579 preserved skulls), and even higher in the Samtavro cemetery (c. 30%; 43/132) 39 Furthermore, within one type of ACD, Georgian skulls show higher diversity than those associated with the Huns, challenging the widespread idea that the practice spread due to Hunnic influence 40.
Here, we associate information about genetic ancestry and ACD typology on 16 adult individuals from the end of the Late Antique period (late 3rd century AD) to the Early Middle Ages. According to our PCA and IBD network analyses (Figures 2B and 5A), the ACD cases from Nedzikhi, which comprise a third of our dataset, occurred among individuals from a close mating network within the local population. Distantly linked to this network, an individual from Samtavro with ACD (SMT009) is the mother or daughter of another individual with ACD (SMT010). Both have ancestry profiles from the South Caucasus (called ‘local’ hereafter). Although they were subjected to different elongation techniques, the evidence of lineal kinship suggests that the practice was common among the local population and passed on through genealogical transmission.
Despite the majority of individuals with ACD (12 out of 17 individuals) carrying ‘local’ genetic ancestry, four ACD cases of tabular (n=3) and circular (n=1) “Hunnic” type are clear ancestry outliers in our dataset. The genetic backgrounds of these individuals are very diverse, ranging from Central/Eastern Europe (SMT025), Central/Inner Asia (SMT013 and SVL005), and East Europe/Central Asia (SVL015). Their 14C date span is 220-525 cal AD (Table S1), which partially predates the widespread presence of Huns in Eastern Europe (c. 370-460 AD). More specifically, the tool mobest, using PCA and spatiotemporal coordinates as input (see Methods), estimates higher similarity probabilities for the Carpathian Basin for SMT025, the Caucasus - including part of the Pontic-Caspian steppe - for SVL005, present-day Kazakhstan, Mongolia, and southeast China for SVL015 and SMT013 (Supplementary Figure 1C, 1D and 1E). For ACD individual SMT027 mobest outputs the highest probabilities for a genetic origin within the Caucasus. In addition, SMT027 -along with SMT032 and SMT003- occupy the extreme end of the qpWave first cluster, plotted closer to individuals from the Alan and Sarmatian groups of Russia but also Eastern Europe (late Sarmatian to Hunnic period).
Informed by these analyses, we then formally modeled the ancestry of each genetically non-local ACD individual using qpAdm. Low-coverage SMT027 clusters with SMT032 (no ACD), which shows the same placement on the PCA. Together, they could be modeled as a one-source model from the pastoralist group of Alans in the North Caucasus (7th cent. AD) with p-value=0.02 (Figure 3D, Table S8). An alternative model of a two-way mixture from LA-EMA Georgia and individuals from the Carpathian Basin from the Late Sarmatian or Langobard period is also accepted; however, no decay of local ancestry due to recent admixture could be fitted with the DATES software. For individual SMT025, adequate models (p-value≥0.05) include c. 70% ancestry related to the Carpathian Basin (i.e., Langobards) admixed with a source from the Kazakh-Pontic Steppe (e.g., Sarmatians), although adding local ancestry from Georgia (LA-EMA; c. 20%) further improved the fit of the model. Consistently, a simple one-source model - although marginally rejected with p-value=0.035 - was achieved with the group from the Late Sarmatian period in Hungary (Danube-Tisza interfluve region, 4th-5th centuries), which was shown to be distinct from others in the area due to its higher affinity with populations from the Pontic Steppe 31. Individuals SVL015 (262-525 cal AD) and SMT013 (218-328 cal AD) exhibit a genetic profile common in the central and eastern steppe that has spread as far as the Carpathian Basin in the Avar period 30. Coeval groups from the central steppe such as ‘Kazakhstan_Berel_IA’ and ‘Kyrgyzstan_TianShan_Hun.SG’ fit neither as one-source models nor in combination with a local source (Georgia LA-EMA). The exception is the medieval group from east Kazakhstan, which serves as a majority source (c. 85%) in a two-way model with LA-EMA Georgia. The mitochondrial haplogroup H of SVL015 also supports West Eurasian ancestry. For the earliest individual, SMT013, who carries the East Asian mitochondrial haplogroup D4e1, this model can be attributed to a recent admixture event of 10±4 generations before her time (estimated with DATES). Furthermore, IBD analysis distantly connects SMT013 with one individual from Hungary from the Early Avar Period (SZOD1-187; 25cM in total) and two more from the Hun Period (KMT-2785, VZ-12673; 14 and 13cM, respectively), all of which are genetically associated with the Eastern Steppe 30 (Supplementary Figure 1A and 1B). These IBD connections suggest that SMT013 originates from the transcontinental mating network that reached Eastern Europe shortly after.
Within our dataset, 17 individuals from Samtavro, Samshvilde, Nedzikhi, and Tserovani had artificially elongated skulls. Artificial Cranial Deformations (ACD), a form of skull modification, has occurred independently throughout the world and as early as the Early Neolithic in Southwest Asia, where it is thought to have been widespread 37,38. In Georgia, the earliest documented ACD cases date to the Late Bronze Age - Early Iron Age transition 39, but the frequency substantially increased in the Mtskheta area during the Migration Period of Europe (4th - 7th century AD) 40. In particular, craniological material from early medieval Georgia suggests a frequency of c. 20% (126/579 preserved skulls), and even higher in the Samtavro cemetery (c. 30%; 43/132) 39 Furthermore, within one type of ACD, Georgian skulls show higher diversity than those associated with the Huns, challenging the widespread idea that the practice spread due to Hunnic influence 40.
Here, we associate information about genetic ancestry and ACD typology on 16 adult individuals from the end of the Late Antique period (late 3rd century AD) to the Early Middle Ages. According to our PCA and IBD network analyses (Figures 2B and 5A), the ACD cases from Nedzikhi, which comprise a third of our dataset, occurred among individuals from a close mating network within the local population. Distantly linked to this network, an individual from Samtavro with ACD (SMT009) is the mother or daughter of another individual with ACD (SMT010). Both have ancestry profiles from the South Caucasus (called ‘local’ hereafter). Although they were subjected to different elongation techniques, the evidence of lineal kinship suggests that the practice was common among the local population and passed on through genealogical transmission.
Despite the majority of individuals with ACD (12 out of 17 individuals) carrying ‘local’ genetic ancestry, four ACD cases of tabular (n=3) and circular (n=1) “Hunnic” type are clear ancestry outliers in our dataset. The genetic backgrounds of these individuals are very diverse, ranging from Central/Eastern Europe (SMT025), Central/Inner Asia (SMT013 and SVL005), and East Europe/Central Asia (SVL015). Their 14C date span is 220-525 cal AD (Table S1), which partially predates the widespread presence of Huns in Eastern Europe (c. 370-460 AD). More specifically, the tool mobest, using PCA and spatiotemporal coordinates as input (see Methods), estimates higher similarity probabilities for the Carpathian Basin for SMT025, the Caucasus - including part of the Pontic-Caspian steppe - for SVL005, present-day Kazakhstan, Mongolia, and southeast China for SVL015 and SMT013 (Supplementary Figure 1C, 1D and 1E). For ACD individual SMT027 mobest outputs the highest probabilities for a genetic origin within the Caucasus. In addition, SMT027 -along with SMT032 and SMT003- occupy the extreme end of the qpWave first cluster, plotted closer to individuals from the Alan and Sarmatian groups of Russia but also Eastern Europe (late Sarmatian to Hunnic period).
Informed by these analyses, we then formally modeled the ancestry of each genetically non-local ACD individual using qpAdm. Low-coverage SMT027 clusters with SMT032 (no ACD), which shows the same placement on the PCA. Together, they could be modeled as a one-source model from the pastoralist group of Alans in the North Caucasus (7th cent. AD) with p-value=0.02 (Figure 3D, Table S8). An alternative model of a two-way mixture from LA-EMA Georgia and individuals from the Carpathian Basin from the Late Sarmatian or Langobard period is also accepted; however, no decay of local ancestry due to recent admixture could be fitted with the DATES software. For individual SMT025, adequate models (p-value≥0.05) include c. 70% ancestry related to the Carpathian Basin (i.e., Langobards) admixed with a source from the Kazakh-Pontic Steppe (e.g., Sarmatians), although adding local ancestry from Georgia (LA-EMA; c. 20%) further improved the fit of the model. Consistently, a simple one-source model - although marginally rejected with p-value=0.035 - was achieved with the group from the Late Sarmatian period in Hungary (Danube-Tisza interfluve region, 4th-5th centuries), which was shown to be distinct from others in the area due to its higher affinity with populations from the Pontic Steppe 31. Individuals SVL015 (262-525 cal AD) and SMT013 (218-328 cal AD) exhibit a genetic profile common in the central and eastern steppe that has spread as far as the Carpathian Basin in the Avar period 30. Coeval groups from the central steppe such as ‘Kazakhstan_Berel_IA’ and ‘Kyrgyzstan_TianShan_Hun.SG’ fit neither as one-source models nor in combination with a local source (Georgia LA-EMA). The exception is the medieval group from east Kazakhstan, which serves as a majority source (c. 85%) in a two-way model with LA-EMA Georgia. The mitochondrial haplogroup H of SVL015 also supports West Eurasian ancestry. For the earliest individual, SMT013, who carries the East Asian mitochondrial haplogroup D4e1, this model can be attributed to a recent admixture event of 10±4 generations before her time (estimated with DATES). Furthermore, IBD analysis distantly connects SMT013 with one individual from Hungary from the Early Avar Period (SZOD1-187; 25cM in total) and two more from the Hun Period (KMT-2785, VZ-12673; 14 and 13cM, respectively), all of which are genetically associated with the Eastern Steppe 30 (Supplementary Figure 1A and 1B). These IBD connections suggest that SMT013 originates from the transcontinental mating network that reached Eastern Europe shortly after.