Post by Admin on Mar 7, 2021 22:24:46 GMT
A potential limitation of our approach, which is
inherent to most aDNA studies, is genetic discontinuity
due to large population replacements or to sampling bias
for geographical locations.35 For example, different sampling
proportions from northern and southern Europeans
across epochs may result in genetic discontinuity in our
dataset, given that the former present higher Eastern
steppe ancestry than the latter after the Bronze Age.36 We
thus repeated our ABC setup for northern and southern Europeans
using a geographical division,37 designed to distinguish
high and low levels of Steppe ancestry (Figure S8).
Despite much lower sample sizes, we found evidence for
negative selection in both northern (s ¼ 0.24; 95% CI:
[0.02–0.87]) and southern (s ¼ 0.13; 95% CI: [1.6 3 10
4–0.81]) European homozygotes, with a slightly left-shifted
posterior distribution in southern Europe, where the sample
size is more limited (Figure S9). We also found, using
factor analysis,38 that P1104A carriers scattered
throughout European sub-structured populations, across
all epochs after its introduction to Europe (Figure 4).
inherent to most aDNA studies, is genetic discontinuity
due to large population replacements or to sampling bias
for geographical locations.35 For example, different sampling
proportions from northern and southern Europeans
across epochs may result in genetic discontinuity in our
dataset, given that the former present higher Eastern
steppe ancestry than the latter after the Bronze Age.36 We
thus repeated our ABC setup for northern and southern Europeans
using a geographical division,37 designed to distinguish
high and low levels of Steppe ancestry (Figure S8).
Despite much lower sample sizes, we found evidence for
negative selection in both northern (s ¼ 0.24; 95% CI:
[0.02–0.87]) and southern (s ¼ 0.13; 95% CI: [1.6 3 10
4–0.81]) European homozygotes, with a slightly left-shifted
posterior distribution in southern Europe, where the sample
size is more limited (Figure S9). We also found, using
factor analysis,38 that P1104A carriers scattered
throughout European sub-structured populations, across
all epochs after its introduction to Europe (Figure 4).
In addition, ancestry proportions were similar between
P1104A carriers and the rest of the dataset at each epoch (Table
S1). Notably, the observed ancestry shift between Bronze
Age and present-day samples (from 0.29 to 0.36 for the whole
dataset [Table S3], representing a 24% relative increase, and
from 0.23 to 0.39 for P1104A carriers [Table S1]) does not,
on its own, explain the frequency decline of the allele after
the Bronze Age (from 0.074 to 0.029, representing a 61% relative
decrease). Yet, we performed an ABC estimation accounting
for ancestry variation across epochs (supplemental
material and methods). Using the estimated Anatolian
ancestry of our dataset at each epoch fromthe Late Neolithic
onward, we estimated very similar values for the strength
and onset of negative selection for TYK2 P1104A at the
pan-European level (s ¼ 0.27; 95% CI: [0.08–0.93]; Tonset ¼
2,045 ya; 95%CI [500–8,690]; Figures S10A and S10B). Similarly,
we found comparable estimations for northern and
southern Europeans (s ¼ 0.26; 95% CI [0.06–0.83]; Tonset ¼
1,046 ya; 95% CI [500–6,934]; Figures S10C and S10D; and
s ¼ 0.24; 95% CI [0.02–0.85]; Tonset ¼ 3,229 ya; 95% CI
[500–8,963]; Figures S10E and S10F, respectively).
Conversely, we found no evidence of selection for TYK2
I684S (s ¼ 0.02; 95%CI: [0–0.69]), as expected, and a weaker
signal of negative selection for HFE C282Y (s¼0.12; 95%CI:
[0–0.76]). Collectively, these findings suggest that the
observed frequency drop of P1104A after the Bronze Age is
not due to major geographical and/or temporal differences
in ancestry components in our aDNA dataset, but instead
to the action of natural selection. Moreover, when re-estimating
the age of P1104A without modern data from Middle
Easterners and Central Asians, as they are not entirely representative
of ancestral Anatolian farmers and steppe herders,
respectively,39,40 we obtained almost identical results (mode
¼ 30,303 ya; 95% CI [23,113–60,273]).