Abstract
20
21
On 26 November 2021, the World Health Organization designated the SARS-CoV-2 22
variant B.1.1.529, Omicron, a variant of concern. However, the phylogenetic and 23
evolutionary dynamics of this variant remain unclear. An analysis of the 131 24
Omicron variant sequences from November 9 to November 28, 2021 reveals that 25
variants have diverged into at least 6 major subgroups. 86.3% of the cases have an 26
insertion at amino acid 214 (INS214EPE) of the spike protein. Neutrality analysis of 27
DH (-2.814, p<0.001) and Zeng’s E (0.0583, p=1.0) tests suggested that directional 28
selection was the major driving force of Omicron variant evolution. The 29
synonymous (Dsyn) and nonsynonymous (Dnonsyn) polymorphisms of the Omicron 30
variant spike gene were estimated with Tajima’s D statistic to eliminate 31
homogenous effects. Both D ratio (Dnonsyn/Dsyn, 1.57) and DD (Dsyn-Dnonsyn, 0.63) 32
indicate that purifying selection operates at present. The low nucleotide diversity 33
(0.00008) and Tajima D value (-2.709, p<0.001) also confirms that Omicron variants 34
had already spread in human population for more than the 6 weeks than has been 35
reported. These results, along with our previous analysis of Delta and Lambda 36
variants, also supports the validity of the Tajima’s D test score, with a threshold 37
value as -2.50, as an accurate predictor of new COVID-19 outbreaks. 38
39
40
41
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3
Introduction
42
43
On 26 November 2021, World Health Organization designated the SARS-CoV-2 44
variant B.1.1.529, Omicron, a variant of concern based on its unique mutations, and 45
unusual features suggesting that therapeutic monoclonal antibodies, such as 46
Regeneron, may be less effective against Omicron. Evidences that new mutations in 47
Omicron could have an impact on viral transmission or the severity of illness are 48
still under investigation (World Health Organization, 2021). Omicron variants were 49
first reported in the Gauteng province, South Africa on November 9, 2021, and 50
shortly it was detected in recent travelers to Belgium, Botswana, Canada, Hong 51
Kong, Austria, Australia, Portugal, Israel, United Kingdom, Netherland, and the 52
United States. One of the major concerns is that Omicron variants contain more than 53
30 mutations to the spike protein (A67V, Δ69-70, T95I, G142D/Δ143-145, 54
Δ211/L212I, ins214EPE, G339D, S371L, S373P, S375F, K417N, N440K, G446S, 55
S477N, T478K, E484A, Q493R, G496S, Q498R, N501Y, Y505H, T547K, D614G, 56
H655Y, N679K, P681H, N764K, D796Y, N856K, Q954H, N969K, L981F). Some of 57
these changes have been previously identified in Delta or Alpha variants and are 58
linked to heightened infectivity and the ability to evade infection-blocking 59
antibodies (Callaway, 2021). The likelihood of higher transmission rates has led 60
multiple countries to respond quickly to the Omicron variant. 61
62
The rapid increase in Omicron variant cases was found in the Gauteng province in 63
November, particularly in schools and among young people. Preliminary evidence 64
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4
from genotyping tests suggests that Omicron may have been in circulation for quite 65
some time in South Africa (Callaway, 2021). To date, phylogenetic and evolutionary 66
status of Omicron variants are still not clear. Here we analyze the phylogenetic 67
relationship and selection pressure among the 131 available sequences of Omicron 68
variants. 69
70
Materials and methods
71
72
131 complete SARS-CoV-2 genome sequences excluding low coverage from 73
November 9 to November 28, 2021 in 9 countries: Austria (N=1), Australia (N=1), 74
Belgium (N=1), Canada (N=1), Botswana (N=17), Hong Kong, China (N=2), Italy 75
(N=1), South Africa (N=105), and United Kingdom (UK, N=2) were collected from 76
the Global Initiative on Sharing All Influenza Data (GISAID) 77
(https://www.gisaid.org/). Sequence data in this study is available and deposited at 78
Figshare website (10.6084/m9.figshare.17105090). 79
80
FASTA files of viral sequences were downloaded and first aligned using MAFFT 7 81
software (Katoh and Standley, 2013, Kuraku et al, 2013). Phylogenetic relationships 82
between Omicron variants were analyzed using the neighbour-joining method and 83
Jukes-Cantor substitution model with bootstrap resampling number set as five. The 84
radial phylogenetic tree was generated by exporting the tree file in Newick format 85
by MAFFT. The FigTree software (version 1.4.2) was used to display the cladogram 86
(Rambaut, 2021). 87
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5
88
The polymorphisms of the SARS-CoV-2 Omicron variants was analyzed based on the 89
site-frequency spectrum: (1) Tajima's D test, (2) normalized Wu and Fay’s DH test, 90
and (3) Zeng’s E test, using DNASP6 software with the bat SARS-CoV-2 WIV04 91
(GenBank MN996528.1) as the outgroup sequence (Rozas, et al., 2017). Statistical 92
significance of observed values of different tests was obtained by coalescent 93
simulation with intermediate recombination after 10,000 replicates. The probability 94
for each statistic was calculated as the frequency of replicates with a value lower 95
than the observed statistic (two-tailed test) by DNASP6 (Rozas, et al., 2017). 96
97
A modified Tajima’s D statistic was used to examine purifying selection based on 98
non-synonymous (Dnonsyn) versus synonymous sites (Dsyn) of SARS-CoV-2 genes was 99
calculated as previously described (Hahn et al, 2002, Hughes, et al., 2005, Yeh and 100
Contreras, 2021). The average number of pairwise synonymous differences (kS) 101
and the average number of nonsynonymous pairwise differences (kN), the number 102
of synonymous segregating sites (SS), and the number of nonsynonymous 103
segregating sites (SN) were computed with equation: (1) S*S=SS/a1, (2) S*N=SN/a1, 104
where a1 is defined as (Tajima, 1989, Hughes, et al., 2005). Dsyn was 105
defined as kS − S*S, divided by the standard error of that difference, and Dnonsyn was 106
defined as kN − S*N, divided by the standard error of that difference (Tajima, 1989, 107
Hughes, et al., 2005). 108
109
Results
and Discussion 110
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111
The insertion mutation Ins214EPE at the spike protein is present in some 112
Omicron variants 113
The phylogenetic tree identifies at least 6 major subgroups of 131 Omicron variant 114
sequences after rooting with an outgroup virus sequence of SARS-CoV-2 WIV04 115
from Wuhan, China (Figure 1). 113 Omicron cases (86.3%) contain an insertion of 116
nine nucleotides (GAGCCAGAA) between nucleotide 22204 and 22205 according to 117
WIV04 sequence (Figure 2). This generates an insertion of three amino acids 118
(Glutamic acid-Proline-Glutamic acid) (INS214EPE) in the N-terminal domain (NTD) 119
of the spike protein. 120
121
Resende et al. has reported that most ins214 motifs were rare in sequences of 122
different lineages of SARS-CoV-2 (A.2.4, B.1, B.1.1.7, B.1.177, B.1.2, B.1.214, and 123
B.1.429) with an insertion motif of 3 or 4 amino acids (AKKN, KLGB, AQER, AAG, 124
KFH, KRI, and TDR) (Resende, et al, 2021). Interestingly, the ins214 with four amino 125
acids (ins214GATP, ins214GATP, ins214GATS) were also present in bat SC2r-CoV 126
isolated in China (RmYN02), Thailand (RacCS203), and Japan (Rc-o319), 127
respectively. Although amino acid identity at ins214 vary among SARS-CoV-2 or 128
SC2r-CoV lineages, the insertion size (3 or 4 amino acids) is also conserved in 129
Omicron. It suggested that this region of NTD is susceptible to a mutation or 130
insertion. Whether or not INS214EPE affects spike protein function or immune 131
response requires further investigation. 132
133
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Tajima’s D test is able to forecast new Omicron outbreaks 134
We have previously used neutrality tests to analyze the selection pressure of SARS-135
CoV-2 in the shipboard quarantine on the Diamond Princess (Yeh and Contreras, 136
2021a) and the influence of full vaccination coverage on Delta variants among 137
different countries (Yeh and Contreras, 2021b). We also proposed that Tajima’s D 138
test, a popular statistic in population and evolution genetics, can provide a 139
promising tool to forecast new COVID-19 outbreaks (Yeh and Contreras, 2021b). 140
141
Here the selection pressure of Omicron variants was first analyzed by multiple 142
neutrality tests. Within 131 Omicron variant sequences, 75 mutation sites were 143
identified with the nucleotide diversity (π, the average number of nucleotide 144
differences per site between two sequences) equal to 0.00008, which is significantly 145
lower than earlier outbreak of Delta variants in UK (0.0004-0.0006, N=376, March 146
26 to April 22, 2021), India (0.0004-0.0006, N=67, January 1 to March 11, 2021), or 147
Australia (0.0006, N=75, April 9 to May 6, 2021) (Yeh and Contreras, 2021b). Tajima 148
D test was calculated to compare π and total polymorphism (Tajima, 1989). Tajima’s 149
D values were negative and significantly deviated from zero (-2.709, P < 0.001) 150
among the whole genome sequences of Omicron variants. The negative values of 151
Tajima D were also detected in the ORF1ab (-2.617, P < 0.001) and the spike gene (-152
1.948, P < 0.005). This result indicates an excess of nucleotide variants of low 153
frequency (Table 1), and strong selection and/or demographic expansion was 154
operating in Omicron. 155
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We have previously shown that Tajima D values decreased as SARS-CoV-2 Delta and 156
lambda variants spread in human populations. One to three weeks after Tajima D 157
fell below -2.50, Delta variant outbreaks emerged in India and the UK (Yeh and 158
Contreras, 2021b). Taken together, the low π and Tajima D values suggested that 159
Omicron variants have most likely spread within a population weeks before the 160
samples were collected. This data also agreed with our previous proposal that 161
Tajima’s D test is useful to forecast new COVID-19 outbreaks regardless of the 162
sample sizes of different variants (Yeh and Contreras, 2021b). 163
164
Purifying selection was operating in Omicron variants 165
Application of Tajima D is limited by the difficulty in distinguishing the influence of 166
both selection pressure and demographic expansion. To overcome this problem, we 167
included normalized DH test and Zeng’s E test in our analysis (Zeng et al., 2006, Yeh 168
and Contreras, 2021b). The normalized DH test is affected by directional selection 169
but insensitive to demographic expansion. Zeng’s E test is very sensitive to 170
population growth immediately after a sweep (Zeng et al., 2006). Genomic 171
polymorphisms of Omicron variants showed significantly negative DH values (-172
2.814, P0.1) (Table 1). The results were similar after confining our analysis to the spike 174
gene (DH, -9.014, p<0.001; Zeng’s E, 5.504, p<0.001) (Table 1), suggesting that 175
directional selection was the major driving force, without significant influence by 176
the demographic expansion. 177
178
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We and others have shown the limitations to application of the inter-species 179
divergence, the dN/dS (w) test, for analyzing selection pressure of SARS-CoV-2 180
previously (Mugal, et al., 2014, Kang et al., 2021, Yeh and Contreras, 2021a, Yeh and 181
Contreras 2021b). Therefore, here we determined the purifying selection using a 182
modified Tajima’s D statistics instead of dN/dS (w) test. Under purifying selection, 183
the frequency distribution of non-synonymous polymorphisms is negatively skewed 184
relative to the distribution of synonymous polymorphisms. Therefore, it takes more 185
negative values for non-synonymous (Dnonsyn) than for synonymous sites (Dsyn) of a 186
given gene (Hahn et al, 2002, Hughes, et al., 2005, Yeh and Contreras, 2021b). One 187
of the major advantages of Dnonsyn and Dsyn analysis is that it is independent of 188
sample size, which allows us to compare Dnonsyn and Dsyn values among different data 189
sets (Hughes et al., 2008). The same excess of low-frequency alleles in non-190
synonymous polymorphism was also shown by the Dnonsyn values of the spike (-191
1.771, p<0.001) and N gene (-1.943, , p<0.005) (Table 1). We conclude that 192
purifying selection led to constraints on the neutral mutations at non-193
synonymous sites of the spike gene of Omicron variants. 194
Negative values of Tajima D could be caused by a bottleneck event rather than 195
selection, but the bottleneck effect should affect all types of polymorphism equally 196
(Tajima, 1989). Hahn et al. have reported that Dnonsyn is disproportionally lower than 197
Dsyn, because non-synonymous and synonymous mutations are affected unequally 198
by purifying selection (Hahn et al., 2002). The value of DD (Dsyn-Dnonsyn) increased as 199
purifying selection became stronger, and DD can eliminate the homogenous effects 200
(demographic expansion, selective sweep etc.). DD values of the spike and N gene of 201
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SARS-CoV-2 Omicron variants are positive (0.643 and 0.377, p<0.005) (Table 1). 202
Austin Hughes showed that the standard error terms in both equations of Dnonsyn 203
and Dsyn cancel out the sample size effect when D ratio (Dnonsyn/Dsyn) was applied to 204
the data analysis (Hughes, 2008). D ratio values of the spike and N gene were 205
significantly more than 1 (1.57 and 1.24, Table 1), suggesting that purifying 206
selection pressure of Omicron spike and N gene was operating. The values of 207
DD and D ratio of ORF1ab (-0.05 and 0.980, p<0.001) were insignificant, consistent 208
with the idea that the spike and N gene have been under more selective constraint 209
than ORF1ab (Chaw et al., 2020). So far, no evidence has shown that vaccination or 210
other mitigation procedures causes positive selection of Omicron variants. 211
212
Perspectives 213
Previously we found that one to three weeks after the D value fell below -2.50, Delta 214
outbreaks emerged in India and UK, and the lambda variant outbreak in south 215
America (Yeh and Contreras, 2021b). This led to our proposal that Tajima D test 216
with a cut-off threshold value as -2.50, can predict new SARS-CoV-2 outbreak (Yeh 217
and Contreras, 2021b). Despites of the small sequence sample size (131 samples) in 218
this study, we detect a strong negative value of Tajima D in Omicron variants. This 219
finding also confirmed that the Omicron outbreak had emerged sometime before the 220
current breakout as the Tajima D test is sensitive to detect it and an efficient 221
predictor of future outbreaks. This study demonstrates that rapid genomic sequence 222
surveillance is essential, and Tajima D’ tests should be included to forecast future 223
outbreaks in different geographic populations. 224
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225
Disclosure statement 226
No potential conflict of interest was reported by the author(s). 227
228
Author contributions 229
All authors contributed to study concept, rationale, and initial manuscript drafts, 230
interpretation of data, and final manuscript preparation. All authors have read and 231
approved the final version of the manuscript. 232
233
Funding 234
No funding 235
236
Ethical approval 237
None declared. 238
239
References
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Figure Legend 288
Figure 1. Rooted phylogenetic tree of SARS-CoV-2 genomes of Omicron variants, 289
November 9 to November 28, 2021. Alignments of viral sequences were generated 290
using MAFFT, and the phylogenetic tree was visualized using FigTree. Rooting was 291
done by introducing SARS-CoV-2 WIV04 (red line, accession number MN996528) as 292
an outgroup virus. 293
Figure 2. Alignment of Omicron variant with and without insertion at the amino acid 294
214 of the spike protein. 295
296
297
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Figure 1. 298
299
300
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Figure 2. 301
302
303
304
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Table 1. Neutrality analysis of SARS-CoV-2 Omicron variants of the full genome and 305
the viral genes. The statistical significance was estimated using 10,000 coalescent 306
simulations in DNASP6. Not significant values (P>0.05) are indicated in italic. NS8 is 307
excluded in this table because no mutations were detected. (N.D., not determined; 308
N.A., not applicable). 309
310
Whole
genome ORF1ab Spike NS3 E M NS6 NS7a NS7b N
DH -2.814 -0.152 -9.014 -1.875 -5.264 -7.552 0.043 0.0588 0.204 -3.016
Zeng's E 0.053 -2.138 5.504 0.149 3.272 4.603 -0.725 -0.996 -0.598 0.716
Tajima's D -2.709 -2.617 -1.948 -1.706 -0.735 -1.281 -0.998 -1.342 -0.65 -2.237
DNonsyn N.D. -2.41 -1.771 -1.342 N.A. N.A. N.A. N.A. N.A. -1.947
Dsyn N.D. -2.46 -1.128 -1.34 N.A. N.A. -0.998 -1.342 -0.65 -1.57
D ratio
(Dnonsyn/Dsyn) N.D. 0.980 1.570 1.001 N.A. N.A. N.A. N.A. N.A. 1.240
DD (Dsyn-Dnonsyn) N.D. -0.05 0.643 0.002 N.A. N.A. N.A. N.A. N.A. 0.377
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