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GREECE - Neolithic/Chalcolithic Minoan/Mycenaean

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  • GREECE - Neolithic/Chalcolithic Minoan/Mycenaean

    In the overview of Greece (Fig. S41),Neolithic Greece, on the basis of available samples,
    is composed of primarily Anatolian Neolithic-related ancestry as previously inferred.(9, 421)We
    confirm the presence of some “eastern” CHG-related ancestry in the Peloponnese Neolithic,

    234
    although we infer that it was also present in the Neolithic of northern Greece(421), and also in
    the Neolithic-to-Chalcolithic samples from Albania previously discussed. In the Peloponnese it
    was accompanied by a small but significant (6±2%) amount of Levantine ancestry. The joint
    presence of CHG/Levantine ancestry suggests that this non-Anatolian related ancestry may be
    derived from a CHG/Levantine cline of which we have already seen the Mesopotamian Neolithic
    was a part.

    In the Bronze Age we group individuals into broad Minoan and Mycenaean groups which

    are used as convenient labels to indicate Cretan and mainland Greece samples; we will look at
    individual variation within these broad groups below. Anatolian Neolithic ancestry continues to
    make up the greater part of the ancestry of the Bronze Age samples of both groups, but there is a
    stronger presence of the “eastern” CHG and to lesser extent Levantine ancestry. This may reflect
    a fresh pulse of “eastern” ancestry into the Aegean prior to the Bronze Age samples, as it in
    Anatolia and the rest of West Asia that CHG ancestry exceeds the low levels that occurred in
    southeastern Europe in the Neolithic. The proportion of eastern hunter-gatherer ancestry is very
    small but is nevertheless different(16)in the combined Mycenaean sample at a significant 4±1%
    with the Minoans at a non-significant 1±1%. The EHG ancestry is ~3-fold lower in the
    Mycenaean samples than in Bronze Age samples from North Macedonia and Albania
    immediately to the north of Greece and ~10-fold lower than in Moldova on the edge of the
    steppe. Thus, our results suggest that although steppe-derived ancestry was present in Bronze
    Age Greece it was quantitatively the weakest discernible component, only a little above the
    practically non-existent Balkan hunter-gatherer ancestry.

    The highest EHG ancestry is found in a previously published(16)low-coverage individual
    from Armenoi in Crete at 24±6% but this is accompanied by a much smaller 3±7% of CHG
    ancestry so it is difficult to interpret as being derived from steppe migrations where EHG/CHG
    components are balanced. We do not overinterpret this Cretan outlier except to note it puts an
    upper bound on the amount of EHG ancestry observed in the Bronze Age Aegean in a collective
    sample of43 individuals. On the basis of this sample, it is justified to claim that while there was
    variation in EHG ancestry in the Aegean, individuals of very high steppe ancestry such as the
    ones found north of Greece were not common there during the Middle/LateBronze Age
    time frame of ours samples.

    Two individuals from Kastrouli near Delphi were from the Archaic age (I17962; 775
    -542
    calBCE, and I17959 800-500 BCE). They were genetically similar to Mycenaean-era samples
    from Kastrouli but their combined EHG ancestry was not significant (2±1%). They differed from
    the Mycenaean sample set in having more Anatolian Neolithic and less Levantine-related
    ancestry; their ancestral composition does not suggest any external influence between the Late
    Bronze Age and Archaic periods as influence from the north would have introduced more
    EHG/Balkan hunter-gatherer ancestry, and from the east more CHG/Levantine ancestry none of
    which are observed for the Archaic individuals. Another individual from the vicinity of the
    Palace of Nestor of Proto-Geometric/Early Iron Age time (I19368) has 14±5% which is similar
    to the proportion seen north of Greece, albeit with a high standard error and a proportion that is
    not significantly higher than the Mycenaean group as a whole. On the basis of these 3 post
    Mycenaean individuals from Pylos and Kastrouli, it appears that some of the variation that
    existed in the Mycenaean period persisted into the Iron Age without a sign of external influence.
    Finally, we note that a Roman-era individual from Marathon (I7833; 252-392 calCE) is
    within the range of ancestry for the population of the Bronze Age, although with somewhat more
    eastern (CHG) ancestry; there would definitely have been an opportunity for such ancestry to

    reach Greece in Hellenistic and Ro
    man times, as evidenced also by the study of the population of
    Rome in Republic and Imperial times.(436)On the basis of a single individual we cannot
    conclude that there was a systematic Roman-era shift of the population in an eastward direction
    as was proposed for Rome for Imperial times. Nonetheless, such “eastern”-shifted individuals
    were described also in North Macedonia (above) and Croatia (below), and so may cumulatively
    suggest that southeastern Europe also participated to some degree in the eastward shift of
    ancestry that was also observed in Central Italy.
    To better understand patterns of ancestry in the main Minoan and Mycenaean clusters, we
    also plot finer-scale variation diagrams for these two groups(Fig. S42).

    The Minoan individuals appear fairly homogeneous with few pairwise differences in

    ancestry being significant. Two possible exceptions are a published individual(16)from Odigitria
    (I9129) which is inferred to have more Anatolian Neolithic ancestry than average, and a newly
    published Middle Minoan individual from Zakros (I14196) which has less Anatolian Neolithic
    and more Levantine Neolithic ancestry than average.

    Examining subsets of the Mycenaean group
    (Fig. S43)and focusing on the diagonal we
    observe that most regional populations do not differ significantly from the population average in
    the five components. Some notable exceptions are the inferred absence of EHG ancestry in a
    low-coverage sample from ProskynasIV in Lokris (I6420_d; 1613-1509 calBCE), the less than
    average Levantine ancestry in Attica with corresponding more Anatolian Neolithic ancestry, and
    the corresponding 24±5% greater Anatolian Neolithic ancestry in Attica than in neighboring
    Salamis. So,while there may have been some variation in terms of ancestry in the Mycenaean
    world, this seems to be in terms of slightly different proportions of the major sources of ancestry.
    We also looked at per-individual diagrams for the two populations with large sample sizes:
    (Kastrouli, and the Palace of Nestor in Pylos)(Fig. S44)

    The individuals from these two sites in the southwestern Peloponnese and central Greece do

    not form site-specific clusters in terms of their ancestry. Some individuals differ in terms of their
    ancestral composition from the overall mean or from each other, suggesting some level of
    ancestral heterogeneity in Mycenaean Greece.
    We highlight the case of the “Griffin Warrior(437)”,from the Palace of Nestor in Pylos
    (I13519_d), a 30-35 year old male buried in a shaft grave with rich grave goods many of which
    were produced in the Minoan world. The ancestral composition of this individual is
    unremarkable suggesting that this elite individual did not belong to a genetically differentiated
    population relative to the population of the Bronze Age Aegean at large, similar to another high
    status individual from Peristeria(16)(I9033), thus showing no correlation between wealth and
    ancestry. However, he is estimated as not having EHG ancestry and this is significantly less than
    the Mycenaean population as a whole, thus lending some plausibility to potential Cretan
    connections, although he is by no means the only Mycenaean individual to lack evidence of this
    type of ancestry. In the PCA(6), the Griffin Warrior is near the center of the Bronze Aegean
    cluster, in-between the Minoan and Mycenaean subclusters and appears to be (a) unremarkable
    for a LBA individual from the Aegean, and (b) not clearly belonging to either of these two
    groupings that form the structure of the Aegean population.

    To test whether the Griffin Warrior was an outlier for the Palace of Nestor site in terms of
    his EHG ancestry we computed the difference between each individual of this site and the
    remaining individuals (Fig. S45). For the Griffin Warrior this difference is-5.9±1.1% which
    corresponds to a 4.08e-8 probability that the difference is negative (which remains significant
    even if we correct it for the 9 individuals considered). For most individuals the difference is not
    significantly negative, while for I13510 and I13516 it is. Individual I13516 was buried just
    outside the limits of the town surrounding the Palace of Nestor, while I13510 was buried in a
    chamber tomb 500m from the Palace of Nestor. Thus, the individuals identified as having less
    than average EHG ancestry in Pylos were buried in 3 different types of tombs associated with
    different levels of prestige, and 3 different localities within the area

    We also computed admixture proportions in ou
    r framework on 6 samples from Greece(31)
    that were published during the course of our analysis and present them in together with other
    comparative data(Fig. S46). Estimated admixture proportions for the Minoan sample from
    Kephala Petras is within 1% of those of the rest of the Minoans. EHG ancestry of the Elati-
    Logkas MBA samples from northern Greece is high (16±2%) and contrasts with that of the
    Mycenaean population and reaches levels seen in neighboring Albania at Çinamak. The Logkas
    samples are separated by a few hundred kilometers and a few centuries from the LBA
    Mycenaeans of Central-Southern Greece and are an important datapoint in the Southeastern
    European continuum between the low-EHG Mycenaean south and the higher-EHG north


    PG 233

    Supplementary
    Materials for
    The genetic history of the Southern Arc: A bridge between West Asia and Europe
    Iosif Lazaridis, Songül Alpaslan-Roodenberget al. 2022



    file:///C:/Users/18509/Downloads/science.abm4247_sm.pdf
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