Background
14
Notothenioids are a well characterised species flock endemic to the Antarctic and an important model 15
group for the study of genome adaptation to extreme cold. We used a new reference assembly and clade-16
wide comparative genomic analysis to investigate cryonotothenioid evolution and the appearance of 17
novel functionalities linked to cold adaptation. 18
Results
19
A new phased assembly of a model notothenioid, Harpagifer antarcticus, demonstrated low levels of 20
haplotypic variability across the genome . Nevertheless, numerous insertions from multiple LINE -L2 21
clades were found, suggesting ongoing transposition with potential contribution to speciation. Contrary 22
to expectations the afgp locus was highly similar between haplotypes, except for large length allelic 23
variants of afgp genes. Analysis suggests a model for the afgp locus expansion in H. antarcticus through 24
segmental tandem duplications involving two pairs of afgp genes at time. Syntenic reconstruction of 25
genomes from across the clade demonstrates conserved macrosyntenic relationships and group specific 26
chromosomal fusions of notothenioids. Quantification of genome gain and transposition rates during 27
cryonotothenioid diversification showed a first ancestral slow genome expansion concurrent with 28
historic temperature drops. This was followed by lineage-specific massive peaks of genomic gain and 29
transposition activity . Finally, w e identified a set of genes that underwent ancestral diversifying 30
selection and acquired novel conserved non -coding elements during the cryonotothenioid emergence. 31
These were related to antioxidants and proteostasis , which may have facilitated the notothenioid 32
Antarctic radiation. 33
Conclusion
34
Diversifying selection and genomic gain linked to transposon activity are primary contributors to 35
lineage-specific evolutionary dynamics through the clade which facilitated adaptation to life in the cold. 36
Keywords
37
cold adaptation, transposons, LINE-L2, afgp, haplotype diversity, genome expansion, proteostasis, 38
diversifying selection, antioxidant activity 39
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Background
40
The notothenioids are one of the most diverse and dominant fish groups in the Southern Ocean and a 41
rare example of a well characterised marine flock species [1]. The clade is formed by approximately 42
140 species grouped in eight families, including three non-Antarctic (basal groups) and five mostly high 43
specialised Antarctic families which are also known as cryonotothenioids [2]. They are characterised 44
by genomic adaptations to extreme cold and they are considered to be an important model group for the 45
study of cold adaptation [3]. 46
The appearance of the antifreeze glycoproteins (AFGPs) is one of the most characteristic innovations 47
enabling freeze avoidance in this group, and are present in members of the cryonotothenioid clade [4]. 48
However, multiple other adaptations on the molecular and cellular level have also been considered to 49
play important roles in the survival and establishment of notothenioids (e.g., cold stable enzyme 50
production, lipid composition of cell ular membranes, modified mechanisms of protein homeostasis) 51
(summarised in [5]). The mechanisms through which such adaptations may have arisen, or the timing 52
of their appearance along the ancestral cryonotothenioid clade remain poorly understood. 53
Assembly of notothenioid genomes has been confounded by the high number of repeat elements present 54
in these genomes [6]. This is exemplified by t he structure of the antifreeze gene locus , which is 55
characterised by tandemly arranged genes [4,7], and high levels of repeat content making it very 56
challenging to assemble and analyse accurately [6]. For the afgp gene locus in particular it has been 57
suggested that high levels of structural variation on the haplotype level may be present. These estimates 58
were based on BAC library sequencing reconstruction of the afgp locus of the Antarctic toothfish 59
species Dissostichus mawsoni [8]. In that case it was shown that the two haplotypes of the afgp locus 60
were characterised by extensive structural variation, with a distinct number of afgp gene copies, with a 61
difference in overall size and mapping within each haplotype of the locus. Other reconstructions of the 62
afgp locus based on whole genome sequencing data were only able to map the consensus structure of 63
one assembled haplotype [6,9,10] though haplotig data have also been analysed [6]. To be able to test 64
this hypothesis on other species, haplotype resolved (phased) genome assemblies are required. 65
Using Oxford Nanopore Technologies (ONT) and Hi-C data we assembled a new haplotype resolved 66
chromosomal reference genome assembly for Harpagifer antarcticus (Antarctic spiny plunderfish). 67
This is the first phased assembly for any notothenioid species . In addition, H. antarcticus, as a small, 68
shallow-water and experimentally tractable member of the cryonotothenioids, is also an important 69
model species for the study of cold adaptation [11–13]. 70
Previous work on notothenioid genomes revealed the significant contributions of transposable elements 71
(TEs) in the evolution of the clade. For the cryonotothenioid clade in particular it has been shown that 72
a recent massive burst of transposons was linked to a significant genome expansion compared to the 73
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3
sub-Antarctic group [6,14,15], while the evolution of various other genomic features has also been 74
linked to transposon activity such as expansion of the antifreeze locus, and the loss of haemoglobins in 75
the Channichthyidae family [6]. Furthermore, it has been suggested that TE accumulation in some 76
notothenioid groups, may have promoted karyotypic reorganisations likely leading to species 77
diversification [16]. 78
In general, TEs are known to be a major source of genomic variation across eukaryotes by disrupting 79
gene structures , reshaping regulatory networks, and co-opting novel regulatory elements [17]. The 80
extensive presence of TEs throughout the genome might amplify the occurrence of recombination 81
events thus promoting deletions, inversions, and translocations [18], while the presence of 82
environmental stressors may also promote TE activity [19]. Using whole genome comparisons can be 83
a powerful method for understanding the mechanisms and patterns of transposon activity at a large scale, 84
while it could also enable highly accurate quantification of genomic losses and gains occurring during 85
diversification events [20–22]. 86
In the present study we employed large scale genome wide analyses of chromosomal references across 87
the notothenioid radiation along with novel genomic resources, to understand the 1) overall contribution 88
of transposable elements in the cryonotothenioid diversification, through timed and quantified analysis 89
of genomic gains and losses, 2) the evolutionary dynamics of the antifreeze gene locus across the 90
cryonotothenioids, and models of expansion of afgps and haplotypic diversity in the H. antarcticus 91
phased assembly, 3) impact of other genomic features that may have enabled genomic adaptation to 92
extreme conditions. 93
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Results
94
Genome assembly and gene annotation 95
The assembled genome for H. antarcticus using ONT long reads and Hi-C data resulted in a fully phased 96
assembly with two high-quality haplotypes (Fig. 1, Fig. S1). The genome was assembled at a total length 97
of 1,069 Mb (Hap1) and 1,222 Mb (Hap2), and contig N50 of 17 Mb (Hap1) and 12,8 Mb (Hap 2). Each 98
haplotype was assigned to 24 chromosomes (Fig. 1A, C) with a scaffold N50 of 44.8 Mb (Hap1) and 41 99
Mb (Hap2) (Table S1). Both haplotypes were highly complete, with 99% BUSCO completeness for both 100
haplotypes, and QV scores of QV 40 (Hap 1) and QV 40.4 (Hap2) ( Table S1). Chromosomes were 101
named based on syntenic relationships with Cottoperca gobio genome assembly (fCotGob3.1) [23] (Fig. 102
1C; Table S2). Completeness of the assembly was confirmed by a clear enrichment of telomeric repeats 103
on at least one end of all chromosomes on both haplotypes (Fig. 1A, Fig. S2), confirming previous higher 104
level localisation data using in situ hybridization data of the (TTAGGG)n repeat motif [24]. Based on k-105
mer analysis, the heterozygosity rate of the H. antarcticus genome was estimated at 0.37%. 106
107
Fig. 1: Genome assembly and genomic features. A. Circos plot showing the 24 chromosomes of the 108
fHarAnt1.2 genome assembly (Hap1) and the distribution of protein coding genes (Genes), transposable 109
elements (TEs), tandem repeats (TR), and canonical telomeric repeats (TeloRep) . Chromosomes are 110
ordered by length and named based on syntenic positions with Cottoperca gobio reference genome [23]. 111
B. Photograph of a H. antarcticus specimen from Ryder Bay, Antarctic Peninsula (Photo credit: BAS 112
Photo Library. Photographer: Simon Brockington) . C. Hi-C-contact map of fHarAnt1. 2 Hap1. D) 113
Syntenic relationships between H. antarcticus Hap1 and C. gobio genomes. 114
De-novo gene annotation (BREAKER) for Hap1 identified 23,057 protein-coding genes, with an average 115
length of 14,904 bp, an average of 8.3 introns per gene, and mean intron and exon lengths of 1,555 bp 116
and 174 bp, respectively (Table S3). By lifting Hap1 annotation onto Hap2 we identified 22,463 (Table 117
S3) protein coding genes with 696 flagged as pseudogenes (i.e., containing premature stop codons). 118
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BUSCO completeness of the gene annotation was high for both haplotypes with 97 .7% for Hap1 and 119
95.6% for Hap2 (Table S3). 120
Genomic landscape of repetitive elements 121
122
Fig. 2: LINE -L2 elements in the H. antarcticus genome. A. Repeat landscape profile showing the 123
activity of the three main TE groups through absolute time. Each bin represents one million years (MYA 124
= million years ago). B. Maximum likelihood phylogenetic tree of clustered LINE -L2 rever se-125
transcriptase sequences (fHarAnt1.2 genome). Tips represent the longest element for each cluster. The 126
size and colour of bubbles is proportional to the number of elements contained in each cluster. Arrows 127
highlight the eight identified high -copy number families. Tips without bubbles represent reference 128
sequences extracted from [25]. C. Genome coverage per LINE -L2 family, and D. activity through 129
absolute time of the eight LINE-L2 families highlighted in panel B. Each bin represents 500 thousand 130
years. E. Number of insertions across notothenioid genomes for each LINE-L2 family identified in H. 131
antarcticus. 132
Annotation of transposable elements on the fHarAnt 1.2 genome revealed 41% coverage (Total repeats 133
43%) (Table S4) with a clear enrichment towards chromosome ends (Fig. 1A). Each of the three major 134
TE classes (LINEs, LTRs, DNA), were almost equally represented in Hap1, covering approximately 13% 135
of the genome respectively , whereas LTRs are more prevalent on Hap2 (17.84% of the genome) . 136
Classification at the RepeatMasker superfamily level was achieved for just 32% of LTR and 41% of 137
DNA elements, in contrast to 97% of LINE elements. These predominantly consisted of LINE-L2 which 138
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accounted for 9.6% (Hap1) and 8.44% (Hap2) of the genome ( Table S4). Tandem repeats and simple 139
repeats accounted for about 4.5% and 2% of the genome on the haplotypes, respectively. Repeat 140
landscape profiles describing activity of TEs through absolute time revealed that the TE content of the 141
Antarctic spiny plunderfish genome mainly derived from a recent burst of activity of all three major TE 142
groups that occurred after the diversification of cryonotothenioids, between 4 and 7 Million Years Ago 143
(MYA) (Fig. 2A). 144
To further characterize the evolutionary history of the highly abundant LINE -L2 elements we first 145
employed a phylogenetic approach to identify evolutionarily distinct LINE-L2 families ( Fig. 2B). 146
Among the 33,670 insertions harbouring a reverse transcriptase segment, 86% clustered with reference 147
L2 elements, whereases others are part of other L2-related clades (Crack, Daphne L2A and L2B) [25]. 148
Eight different high copy-number LINE-L2 families were identified, which were named HarAnt_LINE-149
L2_I – VIII. These families accounted for 60% of the total LINE -L2 content, and 57% of the genome 150
(both haplotypes). The two most abundant of these were L2_IV (27.4% LINE-L2, 1.5% of the genome), 151
and L2_II (22.9% LINE-L2,1.3% of the genome) (Fig. 2C). Dated repeat landscape plots suggest that all 152
families were already active before the extant cryonotothenioid radiation, with a first peak concurrent 153
with their emergence time ~10 MYA and a second more recent activity peak between 4 MYA and 500 154
thousand years ago (Fig. 2D). The two most abundant appear to have decreased their transposition rate 155
over the last 1 MYA, whereas the less abundant ones LINE-L2_VI, LINE-L2_VII, and LINE L2_VIII, 156
have become predominant. 157
Subsequent analysis of LINE -L2 families across 12 notothenioid genomes (Table S5), identified all 158
LINE-L2 families across all cryonotothenioid species. The three most abundant LINE-L2 families in the 159
H. antarcticus genome were also the most abundant ones in the other species ( Fig. 2E). In the sub -160
Antarctic species E. maclovinus and C. gobio, some low-abundance families, 2 and 3 respectively, were 161
missing and therefore likely have originated along the cryonotothenioid stem branch (Fig. 2E). 162
A total of 170 (18S), 534 (5S), 166 (5.8S), and 181 (28S) ribosomal RNA (rDNA) genes were annotated 163
in the H. antarcticus genome. Among the 18S, 5.8S, and 28S genes, multiple copies were found to be 164
dispersed throughout the genome, however, the majority, 97.1% of 18S, 97.6% of 5.8S, and 97.2% of 165
28S, were located in a single main 45S rDNA locus at the end of chromosome 18 (Fig. S3 A, B). The 5S 166
genes occur in three distinct contexts: (i) within the 45S locus forming 18S –5.8S–28S–5S arrays (155 167
copies), (ii) as 20 interspersed single copies scattered across the genome, and (iii) in two large tandem 168
arrays on chromosomes 13 and 21 (Fig. S3 A, C), which contain 151 and 208 paralogues, respectively. 169
These data expand our knowledge of 45S and 5S rDNAs in H. antarcticus , which were previously 170
thought to be co -localised to a single locus [26]. However, the dispersed nature of the 5S locus is 171
consistent with reports for other notothenioids and fish in general [26]. 172
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Haplotypic variation in the H. antarcticus genome 173
Alignment of the two haplotypes of the fHarAnt.1. 2 assembly showed heterozygosity rate of 0.15%, 174
consistent with the low heterozygosity estimated based on k-mers, and a generally low number of 175
structural variants ( Table S 6; Fig. S4). More specifically 1.68% of the genome was present in a 176
hemizygous state (i.e., composed of heterozygous insertions and deletions), and 8.9 Mb and 9.1 Mb 177
was affected by heterozygous inversions on Hap1 and Hap2, respectively. Hemizygous deletions 178
relative to Hap1 affect a total of 849 exons, and 136 genes are completely deleted on Hap2 and thus 179
might be subjected to presence-absence variation at the population level. Importantly, 66.6% of all SVs 180
were also detected in a heterozygous state when performing a read-based SV call, while only 1.7% were 181
genotyped as homozygous for the alternate allele, indicating low levels of false positives due to 182
assembly errors. The remaining 31.7% were not detected using ONT reads. Using generalized linear 183
mixed models and chromosome identity as random effect, a significant positive association was 184
observed between SV occurrence (considering inversions, duplications, and translocations) and 185
repetitive content within 50 kb flanking regions of the breakpoints. The strongest predictor of SV 186
occurrence was the density of tandem repeats, with an odd ration of 2.7. Additionally, we found a 187
negative association of SV occurrence with gene content, distance from both chromosome ends , and 188
assembly gaps as well as LINE-L2 content (Fig. 3A, B). 189
The phased assembly allowed the inspection of the genome for the detection of potentially recently 190
active TEs , as recent insertions are expected to be found mostly in a heterozygous state and thus 191
correspond to insertion/deletion events between the two haplotypes ( Fig. 3C). Overall, 20% of the 192
insertions/deletions have a reciprocal overlap of at least 75% with annotat ed TEs and might therefore 193
correspond to heterozygous TE insertions. Accordingly, these TEs have a significantly lower 194
divergence from their consensus sequences than other TEs, which is used as a proxy for insertion time 195
(One-tail Wilcoxon rank sum test, p-value <0.001) (Fig. 3D). A 39.1% of all heterozygous TE insertions 196
correspond to LINE -L2 elements followed by unknown LTRs with 17.2%, and unknown DNA 197
transposons with 12.4% (Fig. 3E; Fig. S5). Among all heterozygous TE insertions, most are located in 198
intergenic regions (9,578), followed by 2,500 bp gene flanking regions (3,800) and introns (1,958). 199
Only 23 insertions affect coding exons, leading to allelic pseudogenization of the impacted genes. 200
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201
Fig. 3: Haplotypic variation in the H. antarcticus genome. A. Detail of the right end of chromosome 202
15 harbouring multiple structural variants (SVs). B. Association between different genomic features 203
and SV distribution, using a randomized control expressed as log -odds ratios. Points represent the 204
estimated coefficients from the mixed -effects logistic regression. Horizontal lines indicate 95% 205
confidence intervals (“Dist. Chr . end”: distance from closest chromosome end “Dist. Gaps ” distance 206
from closest genomic gap percentage (%) of TEs, LINEs, genes, and tandem repeats shown along 50 207
kb genomic regions flanking the SV breakpoints, SV: length of SVs). C. Schematic representation of a 208
heterozygous LINE insertion between haplotypes. The blue rectangle marks the reverse transcriptase 209
domain. D. Percentage of divergence of TEs from their source consensus sequences as a proxy of the 210
time of the insertion of heterozygous, and all other TEs. E. Contribution of TE groups to heterozygous 211
insertions (see detailed figure in Fig. S5) (*** = p-value <0.001). 212
Genome evolution during notothenioid diversification 213
Synteny analyses of 12 notothenioid chromosome-scale genomes (Fig. 4A; Table S5) revealed strong 214
conservation of macrosyntenic relationships during their diversification, together with lineage-specific 215
Robertsonian chromosomal fusions ( Fig. 4B ), in line with previous karyotype analyses [27]. Most 216
assemblies, including H. antarcticus, show the predominant notothenioid karyotype of n=24, which 217
largely comprises acrocentric chromosomes with the exception of Notothenia rossii (Nototheniinae) 218
(n=12), and Pagothenia borchgrevinki (Trematominae) and Pogonophryne albipinna 219
(Artedidraconidae) (n=23). In N. rossi 10 of the chromosomes appear to have originated from the 220
Robertsonian fusion of 10 ancestral acrocentric pairs, one from the fusion of three chromosomes, and 221
one remained unfused leading to a karyotype of n=12. In P. borchgrevinki and P. albipinna, only two 222
different chromosomes have been fused, resulting in n=23 karyotype in both species. Across all 223
notothenioid genomes , detailed molecular mapping detected only a few large inversions and 224
intrachromosomal translocations were detected, mostly at chromosome ends (Fig. 4B; Fig. S4). 225
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We used a whole genome alignment of 12 chromosomal assemblies to understand patterns of DNA gain 226
and loss during notothenioid diversification, and quantified the amount of bp involved in insertion and 227
deletion events across all internal and terminal branches. Overall, genomic gain greatly outweighs 228
genomic loss which accelerates towards recent times, reaching a maximum net rate of 76 Mb per MY 229
along the ancestor of the Channichthyidae family (Fig. 4A; Table S7). Along the cryonotothenioid stem 230
branch we observed a net genome expansion of 256 Mb. Although this represents the fourth largest 231
absolute gain across all branches, surpassed only by the terminal expansions in N. rossii, H. antarcticus, 232
and P. borchgrevinki, the long branching time resulted in a relatively modest rate of genome gain of 233
16.46 Mb per MY (Fig. 4A; Table S7). 234
Between 3,107 and 51,757 of the insertions inferred along H. antarcticus ancestors, map to an annotated 235
TE element of its genome, requiring a reciprocal overlap of 75% between the two annotations and thus 236
likely correspond to genuine TE insertions (Table S8). The number of TE insertions per MY greatly 237
increased during early evolution of cryonotothenioids, between 10.7 - 6.86 MYA, slightly decreased 238
along the lineage leading to the Harpagiferidae and Artedidraconidae sister species, and reached a main 239
spike of activity along H. antarcticus terminal branch (10,456 insertions per MY; Fig. 4C). DNA 240
transposons were the most active along all branches, but LINEs were predominant along the 241
cryonotothenioid stem branch (41% DNA vs 42% LINEs) and, particularly (Table S8), H. antarcticus 242
terminal branches (33% DNA vs 46% LINEs). Patterns of TE activity, especially for LINE elements, 243
mirror variations in temperature data, based on δ 18O variability [28] (Fig. 4C ), with higher values 244
related to lower temperatures. 245
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246
Fig. 4: Genome evolutionary dynamics during notothenioid diversification. A. Dated phylogeny of 247
notothenioid species included in all comparative genomic analyses. Branch colours show the rate of net 248
genomic gain per million years as megabases per million years (Mb x MY). B. Syntenic relationships 249
among notothenioid chromosomes. Chromosomes were named based on synteny with C. gobio 250
assembly. C. Number of TE -related insertions along H. antarcticus ancestral and terminal branches 251
(highlighted in red in the phylogenetic tree above), shown as a smoothed curve. Scatterplot and black 252
curve show temperature variation over time based on deep-sea δ18O records (data from [28]). 253
Conserved elements and selection analyses on protein-coding genes 254
We identified genes and non -coding regulatory elements that may have facilitated the successful 255
colonization and diversification of cryonotothenioids in the cold waters of the Southern Ocean. First, 256
we analysed intergenic conserved elements (CEs) which are arising along their stem branch and are 257
conserved among all analysed species based on the notothenioid whole genome alignments, and second, 258
we investigated signs of diversifying selection on protein coding genes along the same ancestral branch 259
using a gene-wise branch-site model. We expect that genomic innovations underlying cold adaptation 260
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arose along the notothenioid ancestral lineage. Although some cryonotothenioids such as D. eleginoides 261
and C. esox, inhabit more temperate regions, by colonizing Patagonia and several sub-Antarctic islands 262
[29,30], these are nevertheless considered secondary adaptations [31]. Prediction of CEs yielded a total 263
of 675,818 conserved genomic regions accounting for a total of 78,685,553 bp (Fig. S6A). Most CEs 264
(78%) are shared by all notothenioids, whereases only 10,182 emerged in the cryonotothenioid ancestor 265
and are shared by all members of the Antarctic clade (cryonotothenioid-specific CEs) (Fig. S6). Among 266
the cryonotothenioid-specific CEs, most correspond to intergenic (42.9%) and exonic (29.3%) genomic 267
regions. Intergenic, non-coding CEs (CNEs) might play a regulatory role in gene expression. We found 268
that the 1,261 genes associated with at least one cryonotothenioid -specific CNE were enriched for a 269
total of 236 Gene Ontology (GO) terms, most of which are related to signalling, cell differentiation and 270
developmental processes ( Table S9). However, we also identified 120 genes involved in biological 271
functions known to be important for cold adaptation, in processes such as antioxidant activity, lipid 272
metabolism, protein folding, and cytoskeleton organization ( Table S 10). Some genes of particular 273
interest including prdx5 associated with antioxidant activity (Fig. S6B), ube2e1 and ube2h, involved in 274
protein ubiquitination; ahsa1 which has chaperone -binding activity, and tubb4a, with Antarctic fish 275
tubulins previously having been identified as cold adapted at the amino acid level [32]. 276
For selection analyses we used an extended dataset which includes an additional seven temperate or 277
tropical fishes tagging on the cryonotothenioid stem branch ( Fig. S7). To avoid conflating the signal 278
with lineage -specific evolutionary dynamics, we did not test for diversifying selection in any 279
cryonotothenioid child branch. Furthermore, to establish a stronger link between the identified genes 280
and cold adaptation, we also excluded genes that were found to be under diversifying selection in any 281
other non-cryonotothenioid temperate or tropical fish, based on a control analysis (Fig. S7). While we 282
acknowledge that this latest approach might increase the false negative rates, excluding genes that might 283
be related to both cold -adaptation and other phenotypic traits due to for example substitution on 284
different codons [33] we prefer to automatically exclude genes that might be subjected to pervasive 285
diversifying selection along multiple branches of the phylogeny. We identified a total of 334 genes 286
under selection on the cryonotothenioid ancestor but not in temperate -adapted species, of which 256 287
were functionally annotated (Table S11). A total of 54 GO terms were enriched among the se genes 288
(Table S12). Of these, several are potentially linked to cold adaptation, particularly to oxidative stress 289
(GO:0070301, GO:0010039 ), lipid metabolism ( GO:0006084, GO:1903727, GO:0006690 ) and 290
proteostasis (GO:0051260, GO:0051603, GO:0006509, GO:1901984 ). Example gene include the 291
sirtuin 1 ( sirt1), peroxiredoxin 3 ( prdx3), mitochondrial superoxide dismutase 2 ( sod2), and 292
dihydrolipoamide dehydrogenase (dld) genes. 293
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Characterization and evolution of the antifreeze gene locus 294
The antifreeze gene locus was located on chromosome 16, spanning approximately 699 kb on each 295
haplotype, in a region flanked by the hsl and tomm40 genes. Using a combination of automated and 296
manual approaches, we identified 17 and 16 afgp gene copies on Hap1 and Hap2, respectively, as well 297
as two chimeric afgp/tlp genes on each haplotype (Fig. 5A). The gene annotation completely matched 298
the afgp-specific k-mer signature identified by Klumpy suggesting a complete representation of the 299
locus (Fig. S8). Repeat coverage of the afgp locus was 58.7% (Hap1) and 59.1% (Hap2), approximately 300
1.43 times higher than the genome-wide estimation (Fig. 5A). 301
The typical structure of a functional afgp gene encodes for an exon -1 signal peptide and an exon -2 302
AFGP polyprotein with XLF spacer and AARG terminal motif [4] (Fig. 5B). On Hap1, 14 of the afgp 303
genes identified contained the correct structure and were thus considered to be functional. All complete 304
afgp copies except one were automatically predicted by GeMoMa, highlighting its strong ability to 305
detect intact afgp genes (Fig. S8). Three more identified copies were putative pseudogenes (Table S13), 306
two of which miss the exon -l signal peptide ( afgp1 and afgp17) (Fig. 5A). The third copy ( afgp4) 307
encodes a partial AFGP polyprotein with an unrelated amino acid tail sequence that lacks the canonical 308
AARG terminal motif. The two chimeric afgp/tlp genes contain a signal peptide, but while afgp/tlp1 309
encodes the XLF spacer and a short TLP segment, afgp/tlp2 encodes an unrelated amino acid tail 310
sequence and lacks the XLF spacer, making it a putative pseudogene (Fig. S9). 311
The structure of the afgp locus of fHarAnt1.2 is almost identical in both haplotypes, without evidence 312
of major rearrangements. One afgp gene copy is missing in Hap2 (afgp6) compared to Hap1, but this 313
may be likely due to a mis -assembly resulting in a gap ( Fig. 5A). Only insertions and deletions were 314
identified between the two haplotypes, with 48 short variants (<50bp), involving a total of 428 bp and 315
other 16 with a length from 51 bp to 7,477 bp affecting a total of 32,109 bp. The previously mentioned 316
pseudogenization of afgp4 on Hap1 resulted from a single -base deletion that shifts the reading frame 317
relative to Hap2, which retains a functional copy. Here, 22 insertions/deletions occur on exon2 of afgp 318
or afgp/tlp genes affecting a total of 3,27 k b. These variants do not disrupt the reading frame but 319
generate length allelic variants of the AFGP polyprotein. Specifically, we identified five large indels 320
with a length between 51 bp and 1,224 bp affecting a large portion of exon-2 of afpg7, afgp9 and afgp11 321
genes, respectively (Fig. 5B). Finally, the chimeric afgp/tlp2 gene on Hap1 is affected by the largest 322
identified SV within the locus: a large deletion of 7,334 bp that involves all tlp-derived exons encoding 323
the TLP mature protein (Fig. 5B). 324
The locus is characterized by a clear and repetitive organization with 14 afgp gene copies found in an 325
area spanning 287 ,044 bp. The genes and TEs in this region are arranged in a characteristic motif 326
consisting of two pairs of afgp genes with alternating orientation, and a specific set of TE insertions 327
(Fig. 5Aii). The motif is consistently repeated along the region suggesting that it mainly consists of 328
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13
segmental duplications (Fig. 5A). Mapping of ONT, and 10X reads (minimum mapping quality >0, and 329
excluding secondary alignments) from [6] which come from the same individual, revealed sharply 330
reduced coverage within the previously mentioned central region of the locus ( Fig. S10 A, B, C). On 331
average, coverage decreased by 16.8% for ONT reads and by 55.5% for 10X reads. These values reach 332
the 85.4% and 32.8% when only reads with a minimum mapping quality of 20 are considered. Under 333
this threshold 32.9% of the locus show no coverage of 10X reads. 334
To better understand the evolutionary dynamics and duplication history of afgp and afgp/tlp genes we 335
inferred a maximum likelihood tree based on the conserved exon -1 and the starting region of intron -1 336
which is shared between afgp and chimeric genes ( Fig. S11; Fig. S12 ). Due to the difficulties in 337
resolving relationships among highly similar afgp gene copies, based on few alignment positions (391, 338
of which 56 are parsimony informative) ( Fig. S12A), we additionally performed a ML tree inference 339
excluding chimeric genes (Fig. S12B). This allowed us to include the full intron -1 and analyse a total 340
of 1,964 positions with 3.2 times more parsimony -informative sites. Because both trees recovered the 341
same two main afgp clades, we combined the two topologies by placing the chimeric genes onto the 342
afgp-only tree, preserving their phylogenetic positions ( Fig. 5C). The chimeric afgp/tlp2 genes from 343
both haplotypes form a clade separated by a long branch from all other genes (Fig. S12A). Considering 344
that afgps likely originated from a chimeric gene (Chen et al., 1997), afgp/tlp2 probably represents the 345
most ancestral gene and was therefore used to root the tree. All other analysed genes form two clades 346
that perfectly separate genes on the plus strand from those on the minus strand, including the chimeric 347
afgp/tlp1, which is also the first to diverge within its clade. 348
To have a broader overview of the locus across cryonotothenioids we also annotated the locus in 349
additional species. We used an automated re -annotation process of the afgp locus by employing 350
GeMoMa and Klumpy, followed by visual inspection of candidate genes. To benchmark this approach 351
we used the afgp locus of species P. georgianus which had previously been manually annotated, which 352
we then re -annotated through the automated process. The automated approach identified the same 353
number of chimeric afgp/tlp (1) and afgp (15) genes in P. georgianus, organized in the same structure 354
as described by [6]. We then auto-annotated two additional species: P. albipinna and N. rossii (Fig. 5D; 355
Fig. S8). In P. albipinna the locus was distributed across different unlocalized scaffolds despite the use 356
of long-read sequencing technologies and Hi -C data (Fig. S8). In N. rossii we detected two chimeric 357
genes and 10 afgp genes. We performed comparison of the structure of the locus along a number of 358
species including our new and published annotations for other included species (Fig. 5D). Overall we 359
detected some notable similarities between species C. esox, C. gunnari, H. antarcticus , and N. rossii. 360
Specifically, in all these species the majority of afgp genes are arranged in arrays with alternating 361
orientation. However, each pair of afgp genes lack s the previously described TE motif that was 362
identified in the H. antarcticus afgp locus. 363
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14
364
Figure 5: Structure and evolution of the antifreeze locus. A . Structure of the antifreeze gene locus 365
on both H. antarcticus haplotypes. Triangles represent different genes , and rectangles represent 366
transposable elements. Afgp genes are named from 1 to 16 based on their position on the locus. Asterisks 367
highlight pseudogenes and double-slash lines indicate assembly gaps. The grey panel (ii) on the right 368
corner shows a zoomed in version of the tandemly repeated genomic unit marked by the characteristic 369
TE motif. B. Top: simplified representation of afgp and chimeric afgp/tlp genes (exon and intron lengths 370
are not proportional to their actual size). Bottom: representative afgp and afgp/tlp chimeric genes 371
subjected to insertion/deletion events between the two haplotypes. Coverage refers to ONT reads 372
mapped back to assembly. C. Phylogenetic tree of afgp and chimeric afgp/tlp gene copies. Different 373
colours correspond to strand (+/ -). D. Structure of the afgp locus across notothenioids. All genes, 374
including pseudogeni sed copies are reported. Locus for P. borchgrevinki , C. esox , C. gunnari, C. 375
aceratus, P. georgianus and D. mawsoni is based on published work [6,8,9,34]. P. albipinna could not 376
be included in this analysis due to the locus being highly fragmented in the corresponding assembly 377
(Fig. S8). 378
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Discussion
379
Haplotype-resolved assembly of the Antarctic spiny plunderfish genome reveals low 380
haplotypic structural variation 381
Here, we present the first haplotype -resolved genome assembly of a notothenioid species and one of 382
the most contiguous notothenioid genome assemblies to date. The assembly was generated with ONT 383
reads which supported assembly more successfully compared to sequencing attempts with HiFi data. 384
The two haplotypes exhibit low levels of divergence and a relatively small number of structural 385
variations, which is consistent with the low k-mer based and SNP based heterozygosity (0.37% and 386
0.15%, respectively) of the H. antarcticus genome (Table S6; Fig. S4). Few exons and genes were 387
found to be absent from one of the two haplotypes, in contrast to findings in other metazoans, where 388
highly divergent and hemizygous genomic regions can represent more than 50% of a diploid genome 389
[35,36]. 390
Complex SVs, such as translocations, duplications, and inversions were found to colocalize towards the 391
repeat-rich and gene -poor chromosome ends ( Fig. 2A, Fig. S4). This was even more so in terms of 392
tandem repeat content, consistent with a model of elevated mutation rates in sub -telomeric genomic 393
regions [37]. Accumulation of repeats towards chromosome ends was also observed in another 394
cryonotothenioid species, T. borchgrevinki [34], so we suggest that this might be a plesiomorphic 395
feature of the clade. Furthermore, recent TE insertions were found to significantly contribute to the 396
emergence of insertions and deletions between haplotypes. Even though heterozygous TE insertions are 397
usually found in intergenic genomic regions likely due to strong negative selection against TE insertion 398
within genes, as observed in zebrafish [38], here a high number of TE insertions were detected in gene-399
flanking regions. In few cases, insertions within the exons of protein-coding genes were detected, which 400
have led to the truncation and putative pseudogenization of the affected genes on one of the haplotypes. 401
Overall, our results suggest that despite the low levels of overall haplotypic structural varia bility, 402
recently active TEs likely represent important contributors in driving population-level differentiation in 403
H. antarcticus, promoting gene-loss and reshaping cis- and trans- regulatory elements. 404
Furthermore, haplotype resolved assemblies would also have the potential to shed new light on overall 405
genome evolutionary dynamics, facilitating assembly -based variant calling [39], pangenome 406
reconstruction [40], allele-specific expression analyses [41], and TE identification [42]. 407
Recent accumulation of ancient LINE-L2 elements in H. antarcticus 408
Different TE clades can have varying evolutionary trajectories across species, reflecting host–element 409
co-evolution, lineage-specific regulatory constraints, and variation in genomic defence mechanisms 410
[43,44]. LINE-L2 transposons were previously shown to be particularly abundant in H. antarcticus 411
compared to other notothenioids, covering about 8% of the genome [6]. Analysis of the new genome 412
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assembly similarly showed high LINE -L2 levels deriving mainly from the activity of eight different 413
LINE-L2 families. Both the high number of heterozygous LINE -L2 insertions and the repeat -414
divergence landscape analyses suggest a recent, lineage-specific accumulation of these elements (Fig. 415
2). Eight evolutionary distinct families of LINE-L2 elements were identified, with concurrent activity 416
within the last four million years (MY) (Fig. 2D). Moreover, most of these LINE-L2 families, including 417
the most abundant ones, are also shared with sister species of the cryonotothenioid clade, suggesting 418
their ancient emergence. Despite the recent activity of LINE-L2 elements, we observe a negative effect 419
of their genomic content around breakpoint regions and occurrence of inversions, duplications and 420
translocations between haplotypes suggesting that their accumulation has not resulted in the emergence 421
of other more complex structural variants. 422
In another LINE transposon family, the LINE-L1 retrotransposons, it has been shown that either a single 423
lineage was usually active at high replication rate at any given time in mammals, or multiple, ancient 424
LINE-L1 lineages were concurrently active in fishes, reptiles, and bivalves [44,45]. The evolutionary 425
path of LINE-L2s in notothenioids appear therefore to follow the generally observed evolution of LINE-426
L1 of fishes. 427
Rampant genomic gain and low levels of genomic deletion during cryonotothenioid 428
diversification 429
TE-mediated genome expansion has been shown to predate the diversification of extant 430
cryonotothenioids and that enhanced TE activity continued in more derived clades such as icefishes 431
[6,34]. To further test this hypothesis, we have quantified genomic gains through TEs along the 432
notothenioid ancestral branches ( Fig. 4A ). Mapped TE insertions along H. antarcticus ancestral 433
branches as well as a dated repeat landscape plot, indicate that most TE activity occurred recently, 434
concurrently with the recent cryonotothenioid diversification. A single massive burst of TE activity was 435
also detected in repeat profiles of other cryonotothenioids [6,15,34]. Low levels of ancient TE activity 436
followed by recent peaks could reflect either genuinely increased transposition rates or extensive 437
genomic deletions that removed older insertions, thereby erasing evidence of ancient bursts. However, 438
net genome -gain estimates reveal low deletion rates during notothenioid evolution, supporting the 439
former scenario: a slow accumulation of TEs before the emergence of extant cryonotothenioids, 440
followed by a more recent increased rate of TE accumulation . Our reconstruction also revealed an 441
ancient burst of genome expansion in the ancestor of icefishes explaining their exceptionally large 442
genomes, which may be explained by sea temperature history in the region [6]. 443
Paleoclimatic based temperature calculations ( Fig. 4C ) indicate an initial temperature drop at 444
approximately 16 MYA which predates the emergence time of the extant cryonotothenioid clade, and 445
a second, stronger reduction around 3 MYA which could have contributed to their recent diversification 446
[6], similarly to other marine clades [46]. Here we show that the timing of these temperature variations 447
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appear to coincide with our reconstructions of TE levels of activity (Fig. 4C). LINE elements were 448
found to be particularly expanded not only in H. antarcticus but also in other cryonotothenioids (Fig. 449
2E). The presence of environment induced stressors , such as fluctuations of temperature , have been 450
linked to increased TE activity due to likely disrupting mechanisms of epigenetic regulation [47]. In the 451
cryonotothenioid species D. mawsoni, it has been shown that the levels of LINE element transposition 452
are increased through cold induced cell transfection [48]. We provide evidence that compared to other 453
TEs, LINEs have been particularly active along the cryonotothenioid ancestor and starting from 4 MYA, 454
concurrently with the two main temperature drops documented in the region (Fig. 4C). Overall, our 455
comparative genomics analysis suggests that the increased genome size of cryonotothenioids may have 456
occurred through a two -step process: one ancient, slow TE activity in the absence of major genomic 457
deletions that predate the emergence of extant species and one more recent, lineage -specific massive 458
bursts of transposition due to loss of epigenetic control. 459
Macrosyntenic relationships and chromosomal fusions in notothenioid genomes 460
Our synteny analyses of 12 chromosome -scale notothenioid genomes demonstrated conserved 461
marcosyntenic relationships between notothenioid chromosomes in accordance with the presence of a 462
stable karyotype with low structural divergence during notothenioid radiation [49]. In the Nototheniidae, 463
the most common chromosome number is 2n=48, mainly comprising acrocentric chromosomes. Indeed 464
H. antarcticus has a karyotype of 2n=48 comprising 42 acrocentric, 2 metacentric and 4 submetacentric 465
chromosomes [49]. Lineage-specific Robertsonian chromosomal fusions have occurred in some 466
notothenioids [50], with the most notable case being N. rossii where only 12 chromosomes (2n=24) are 467
observed (Fig. 4B). The few other identified smaller scale rearrangements tended to colocalize towards 468
repeat-rich chromosome ends, similar to haplotypic structural variants identified in the H. antarcticus 469
genome. These genomic regions are therefore thought to be subjected to higher rates of structural 470
variation compared to the rest of the chromosomes, with repetitive elements that may drive this 471
variability. Furthermore, the existence of LTR retrotransposon –insertion hotspots near chromosome 472
ends and at chromosome fusion points, suggests that such repetitive sequences may have facilitated 473
Robertsonian fusions, as has occurred in other more distant species [16,51]. In cryonotothenioids, 474
reduction in chromosome number from the ancestral karyotype of n=24, caused by multiple independent 475
chromosomal fusions, appears to be common within specific subfamilies, with such cases observed in 476
the genera Trematomus, Notothenia, and Pogonophryne [24]. 477
Tandem segmental duplications and haplotype length variants shape the structure of the 478
antifreeze locus 479
The antifreeze locus is a very challenging genomic region to assemble both because of its repetitive 480
structure due to the presence of tandemly duplicated gene families such as the afgps, and trypsinogens, 481
as well as due to its high TE content [6]. Using ONT reads we were able to assemble and annotate the 482
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complete afgp locus for H. antarcticus for both distinct haplotypes. The locus comprises 17 afgp copies 483
(Hap1) and a higher repeat content compared to the genome average (59% vs 43%). One copy of the 484
chimeric afgp/tlp gene was identified on each haplotype (Fig. 5A), both of which are characterized by 485
canonical structure in accordance to previously described genes (Chen et al., 1997; Cheng and Chen, 486
1999; Nicodemus-Johnson et al., 2011) and are considered to be functional copies. These chimeric 487
genes were previously considered to be putative evolutionary intermediates of the afgp genes [7]. 488
Annotation of the locus on members of the icefish family showed either lack ( C. gunnari and C. 489
aceratus) or pseudogenisation ( P. georgianus ) of chimeric gene copies, suggesting that chimeric 490
afgp/tlp genes might have been lost in low latitudes of the Southern Ocean by relaxed selection due to 491
redundancy function with afgp genes [6,9]. However, chimeric genes have been retained in H. 492
antarcticus which has a partially overlapping distribution range with these species, leading us to 493
question the drivers of retaining these genes for this species. 494
BAC library -based analyses of the afgp locus of D. mawsoni suggested the presence of massive 495
variation between haplotypes in both the overall size of the locus, and in the number of afgp gene copies 496
[8]. Tandem arrays are generally expected to be frequently subjected to copy number variation due to 497
recombination between homologue chromosomal regions which could also promote high levels of 498
haplotypic variation [52]. Through this haplotype resolved assembly for H. antarcticus we were able to 499
directly investigate the potential presence of haplotypic divergence in the locus. Nevertheless, we found 500
that in H. antarcticus, both haplotypes exhibit almost identical structure and gene copy number. The 501
main structural variations identified where pseudogenizations of one afgp gene due to a single base-pair 502
deletion and of the only putatively functional afgp/tlp gene due to large deletion of all tlp derived exons 503
on Hap1. 504
Despite low levels of variation at gene copy and functionality levels, we also identified allelic variation 505
of the afgp gene copies, with regards to the actual length o f the AFGP polyprotein coding exons. 506
Potential variation on the length of the AFGP polyprotein could have important biological implications. 507
The notothenioid AFGP proteins function th rough an “adsorption –inhibition” mechanism [53], 508
adsorbing to the surface of ice and preventing the growth of the crystals as a function of glycoprotein 509
concentration, size, and shape [54,55]. It has been observed that smaller protein molecules are less 510
effective than large ones to interfere with ice crystal growth [54]. We could hypothesise that allelic 511
variation linked to the size of AFGP polyproteins in H. antarcticus populations could represent an 512
important source of genomic variation that allows local adaptation to more extreme conditions. 513
Length allelic variants have also been observed in other highly repetitive gene families, such as silk 514
genes in caddisflies, butterflies, and spiders [56], where sequence length was linked to the properties of 515
the silk fibres [57]. Such types of allelic variants may represent a convergence source of variation in 516
proteins composed of repeated motifs across all metazoans. In these cases we could consider that 517
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because the gene itself provides a substrate for recombination, and the repetitive structure can weaken 518
purifying selection against insertions and deletions, these could create a standing pool of genetic 519
variation on which positive selection can eventually act. 520
In the case of the afgp locus, t he characteristic TE plus afgp gene motif that was detected in H. 521
antarcticus likely supports a specific mode of expansion of the locus. The afgp copies are arranged in 522
opposite orientation separated into two strand -specific clusters ( Fig. 5A, C), suggesting that the 523
expansion of the genes occurred through tandem segmental duplications, which duplicated as two pairs 524
of genes at a time. Furthermore, the high sequence homology identity across duplicated regions and the 525
short branch lengths separating gene copies in phylogenetic analyses (Fig. 5, Fig. S12) suggest that 526
these duplications are either evolutionarily recent or have been strongly homogenized by concerted 527
evolution. 528
After their emergence in the cryonotothenioid ancestor, reduction and loss of afpg genes has occurred 529
multiple independent times during their radiation [58]. However, the exact time at which afgp genes 530
begun duplicating and expanding remains an open question. Comparison of the afgp locus structure 531
across multiple notothenioid genomes (Fig. 5D ) showed a similar genomic configuration of some 532
genomic features in P. borchgrevinki, H. antarcticus, C. esox, C. gunnari, and N. rossii. Nevertheless, 533
the distinct TE motif appears to be specific to the H. antarcticus genome (Fig. 5Aii). We hypothesize 534
that the tandemly duplicated genomic region marked by the characteristic TE motif of H. antarcticus is 535
a plesiomorphic feature of the other species, with different rates of duplication and loss driving variation 536
of afgp gene copy number. We therefore suggest that from a hypothetical cryonotothenioid ancestral 537
locus with few afgp genes, independent tandem duplications increased gene-copy number in different 538
lineages. 539
Diversifying selection and origin of novel conserved elements in cold -adaptive pathways 540
during cryonotothenioid emergence 541
To detect additional genomic features underlying cold adaptation in notothenioids we searched for both 542
protein-coding genes that experienced diversifying selection and CNEs that first emerged along their 543
ancestral branch. Among the genes showing evidence of diversifying selection in the cryonotothenioid 544
ancestor, many were found to be associated with biological processes known to be important for 545
survival in extreme cold conditions (Table S12). We found that most CNEs were shared across all 546
notothenioid species, suggesting that a large portion of the genome expansion characterizing the 547
cryonotothenioid ancestral lineage may have evolved neutrally. Additionally, most cryonotothenioid-548
specific CNEs were found to be associated with genes involved in signalling, cell differentiation, and 549
developmental processes (Table S9). CNEs are known to have non -random distribution within the 550
genome, because they have the tendency to cluster near genes with regulatory functions in multicellular 551
development and differentiation (Polychronopoulos et al., 2017). A subset of the genes which we have 552
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found to contain newly acquired CNEs are related to two biological processes which are 553
overrepresented among genes under diversifying selection. These biological processes are antioxidant 554
activity and proteostasis and they have been linked to evolutionary cold adaptation [59,60]. We suggest 555
that because these genomic innovations arose in the cryonotothenioid ancestor, they are amongst the 556
key components of these pathways that enabled this clade to survive and become established in the 557
Southern Ocean. 558
Antioxidant activity and proteostasis 559
Life in freezing sea water poses particular biological problems for the organisms living there. The 560
amount of oxygen increases considerably with reduced sea water temperatures, producing naturally 561
high levels of cellular oxidative stress for Antarctic marine species [59,61]. In addition, cold 562
denaturation of proteins impacts proteostasis [60]. Therefore, in order to survive in this harsh 563
environment, organisms need to modify their biochemical processes. 564
Our analysis revealed four key genes related to oxidative stress that underwent diversifying selection in 565
the cryonotothenioid ancestral lineage, including the sirtuin 1 ( sirt1), peroxiredoxin 3 ( prdx3), 566
mitochondrial superoxide dismutase 2 (sod2), and dihydrolipoamide dehydrogenase ( dld) genes. 567
Moreover, we found that the peroxiredoxin 5 (prdx5) gene acquired novel CNEs concurrently with 568
extant cryonotothenioid emergence. Gene sirt1 is a class III histone deacetylase that is recruited in the 569
promoter region of multiple antioxidant genes, including sod2, prdx3 , and prdx5, promoting their 570
expression and their protein concentration [62]. These three genes encode mitochondrial enzymes that 571
act in concert to control reactive oxygen species (ROS) levels. Sod2 converts superoxide radicals into 572
hydrogen peroxide, which is then detoxified to water by prdx3 and prdx5 [63]. The interplay between 573
protein modifications and the emergence of novel, potentially regulatory CNEs within this pathway 574
may have strengthened the antioxidant capacity of the cryonotothenioid ancestor, enabling it to cope 575
with elevated oxidative stress in the mitochondria. 576
Signs of diversifying selection have been found [64] also in other cold-adapted notothenioids acting on 577
genes involved in antioxidant activity, such as in N. coriiceps [65] and D. mawsoni [15], and across 578
species. Moreover, genes such sod2 and prdx5 which are involved in ROS scavenging, have been found 579
to be overexpressed in cold-adapted notothenioids compared to their temperate-adapted relatives [66]. 580
Superoxide dismutase appears to be particularly important in combatting oxidative stress in Antarctic 581
species. Gene duplications used to enhance the cellular activity of this enzyme have been identified in 582
Antarctic invertebrates [67]. Furthermore, evolution to function efficiently in the cold have resulted in 583
at least some members of this gene family being particularly thermally sensitive in some Antarctic 584
marine invertebrates [68]. This would suggest that specific protein modifications might help to mitigate 585
cellular oxidative stress in Antarctic species. 586
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In terms of proteostasis, there is evidence that Antarctic species, including fish, face challenges in 587
producing, folding and maintaining proteins at such low temperatures [60]. Whole animal RNA to 588
protein ratios , ubiquitylation rates , and levels of chaperone proteins are much higher in Antarctic 589
compared to temperate species [69–71]. Some of this activity is due to a mutation in the promotor region 590
of the classical inducible form of hsp70 resulting in constitutive expression and cold-enhanced activity 591
of the proteosome in Antarctic notothenioids [72,73]. In our analyses on genes that were found to be 592
under diversifying selection, we identified genes involved in protein folding and degradation such as 593
members of heat shock protein family member (hspa4), ubiquilin/ubiquitin proteins (ubqln4 and ube2z) 594
and the chaperon psmc1. Similar to genes with acquired CNEs, such as the ubiquitin ube2h, ube2e1, 595
itch and the co -chaperon ahsa1. Furthermore, there was evidence of selection pressures on genes 596
involved in transcription, splicing, and the proteasome (e.g. eif3b, sf3a2 and psmb10) indicating wider 597
scale cold adaptation of the proteostasis pathway. 598
It should be noted that these examples are likely minimal identifications due to the stringency of 599
orthologue assignment, which may not accurately identify duplicated genes, the number of which are 600
considerable in the notothenioids [66]. Such analyses will also fail to identify those genes which are 601
poorly conservated between species, such as genes involved in the immune function, intrinsically 602
disordered proteins and those containing intrinsically disordered regions. 603
Conclusions
604
This haplotype-resolved genome assembly of H. antarcticus thus provides a valuable resource for future 605
functional investigations into cold adaptation and resilience to climate change. Overall haplotype 606
diversity was low and contrary to expectations haplotypic diversity in the afgp locus was also low 607
despite a high number of transposon insertions. However, we did identify sequence length variation in 608
the afgp genes between the two haplotypes, which could be biologically relevant. Furthermore, we show 609
that genomic gain was linked to transposon activity which correlates with drops in temperature in the 610
Southern Ocean, and this activity resulted in the generation of novel genomic elements . Finally, we 611
show that there has been significant selection pressure on notothenioid genomes, both in genes and 612
control regions, to enable these fish to thrive for much of their life below 0°C. 613
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22
Methods
614
Sequencing data generation 615
The specimen of Harpagifer antarcticus that was used for genome assembly was collected at Ryder 616
Bay in the Antarctic peninsula (coordinates: -67,59053 -68,28863), and was preserved by flash freezing. 617
This specimen was the same that was used for the generation of the fHarAnt1 .1 assembly (accession: 618
GCA_902827135.1; BioSample: SAMEA104132831) [6]. 619
High Molecular Weight (HMW) DNA was extracted using the Sanger Tree of Life Manual MagAttract 620
v1 protocol [74] in the Tree of Life Core Laboratory at the Wellcome Sanger Institute. To assess the 621
quantity of the extracted DNA the QubitTM 1X dsDNA High Sensitivity assay (ThermoFisher, Cat No. 622
Q33231) on the Qubit Flex Fluorometer (ThermoFisher, Cat No. Q33327) was used. The quality of the 623
DNA was then determined using the Femto Pulse (Agilent, PN: M5330AA) instrument with the gDNA 624
165 kb Analysis kit 275 samples (Agilent, Cat No. FP-1002-0275). Approximately 3µg of the extracted 625
DNA underwent library preparation for ONT sequencing using the Ligation Sequencing Kit V14 (SQK-626
LSK114). Sequencing was performed on one flow cell on the PromethION 24 in Sequencing Operations 627
at the Wellcome Sanger Institute. 628
Three H. antarcticus specimens were Schedule 1 killed and the gills rapidly dissected, added to tissue 629
culture media (L15 without phenol red, 10% foetal bovine serum and antibiotics) and placed on ice. 630
The gills were chopped up in culture media and the resultant cell suspensions of each sample added to 631
individual wells in 6-well Nunclon™ tissue culture plates. For each fish, one of each of the gill samples 632
was incubated at 0°C with the paired sample incubated at 6°C for 6 days. Cells were harvested and 633
RNA extracted using TRI Reagent according to manufacturer’s instructions. 1µg of rRNA depleted 634
RNA was used for RNAseq library preps with Kapa Hyperprep UDI kit. (Cat#KK8544). Paired end 635
sequencing was carried out by Novogene on the Novaseq PE150 platform. 636
Genome assembly 637
The ONT reads were sequenced at an estimated 23.4X coverage per haplotype and based called with 638
dorado 7.2.13 (https://github.com/nanoporetech/dorado) in super accurate mode. The reads were 639
assembled using Hifiasm version 0.24.0 -r702 [75] with --ont option in Hi -C phasing mode. This 640
produced a phased assembly with contig N50 of 19.3 Mb and 14.8 Mb in each haplotype. The sizes of 641
both haplotypes were 1.072 Gb and 1.222 Gb which were close to the kmer -based estimate from the 642
GenomeScope at 1,152 Gb. 643
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23
Furthermore Hi-C reads were mapped to each haplotype independently using bwa -mem2 [76]. Each 644
haplotype was then scaffolded with Hi -C data in YaHS [77], using the --break option for handling 645
potential mis-assemblies in contigs. The produced assembly was evaluated for kmer completeness using 646
MerquryFK (https://github.com/thegenemyers/MERQURY.FK) using kmers from the ONT reads. This 647
indicated 99.39% kmer completeness and QV value 42.6. 648
The individual haplotype assemblies were screened for contamination using the ASCC pipeline 649
(https://github.com/sanger-tol/ascc) removing 5.8Mb Hap1 and 1.8Mb Hap2 non -target and 650
mitochondrial sequences. The assemblies were then combined and prepared for curation using the 651
treeval pipeline ( https://github.com/sanger-tol/treeval) generating a Hi -C contact map with 652
supplementary analysis tracks (telomeres, gaps and long read coverage). Assembly errors were 653
corrected by manipulating the contact map in PretextView (https://github.com/sanger-tol/PretextView) 654
an AGP of the resolved chromosomal haplotypes were exported and a curated fasta for each haplotype 655
generated using pretext -to-asm (https://github.com/sanger-tol/agp-tpf-utils) with each super scaffold 656
named according to descending size. Contact maps for each resolved haplotype were generated by 657
curationpretext ( https://github.com/sanger-tol/curationpretext) and images generated with 658
PretextSnapshot (https://github.com/sanger-tol/PretextSnapshot). 659
Repeat annotation 660
Repetitive elements were de-novo mined with RepeatModeler v.2.0.5 [78] adding the -LTRStruct 661
extension to improve LTR detection. Potential multicopy host genes included in the repetitive library 662
were removed with ProtExcluder v.1.2 after blasting (Blastx, e -value 1e -10) the repetitive library 663
against a protein database consisting of all vertebrate proteins included in the Swiss-Prot database (The 664
UniProt Consortium, 2025) and the predicted proteomes of five published notothenioid genomes 665
available on NCBI RefSeq: C. gobio, P.georgianus, Gymnodraco acuticeps, Trematomus bernacchii, 666
Eleginops maclovinus . Furthermore, a TE library was made with MCHelper v.1.7.0 with default 667
parameters. Both haplotypes were annotated with RepeatMasker in sensitive mode (-s). RepeatMasker 668
derived annotation was post -processed with: (a) parseRM.pl script 669
(https://github.com/4ureliek/Parsing-RepeatMasker-Outputs/tree/master) to summarize the TE content 670
and obtain TE landscapes describing transposon activity through relative time, and (b) the RM2Bed.py 671
script from RepeatMasker to resolve overlaps in the TE annotation (--overlap resolution ‘higher score’) 672
and produce bed files describing the coordinates of TE insertions. 673
Tandem repeats were identified with the Centrominer function of quarTeT v.1.2.5 [79]. rDNA genes 674
were annotated with barrnap v.0.9 [80] https://github.com/tseemann/barrnap and telomeric repeats with 675
tidk v0.2.31 [81] screening the assembled chromosomes for the TTAGGG telomeric motif. 676
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24
Gene annotation 677
Gene annotation of Hap1 was performed with BRAKER3 [82]. Repetitive elements were soft masked 678
and both protein and transcriptomic data were used as external evidence to train AUGUSTUS [83] and 679
GeneMark-ETP [84] ab-initio gene predictors. Illumina RNAseq reads from muscle, skin, liver, kidney, 680
heart, and brain [5] (Table S14) and from gills (data generated herein) were mapped with HISAT2 [85]. 681
The sorted bam files were supplied to BRAKER3 together with the protein database previously used 682
for cleaning the repetitive libraries from host genes. The quality of the annotation was assessed with 683
BUSCO v.5 [86]. To obtain a gene annotation for Hap2, we mapped BRAKER -derived genes with 684
Liftoff [87] (-polish -copies) to obtain their lifted coordinates. Functional annotation was performed on 685
the Hap1 predicted proteome with eggNOG -mapper v2 [88] transferring only annotations with 686
experimental evidence and auto-adjusting the taxonomic scope based on the query sequence. 687
Annotation of the afgp locus 688
To annotate the afgp locus on each haplotype, a combination of automated and manual approaches was 689
used. The annotation of the D. mawsoni afgp locus (accession HQ447059.1, haplotype 1) [8] was used 690
as a reference for homology-based gene prediction with GeMoMa v.1.7.1 [89] under default parameters. 691
This initial annotation was supplemented by manually blasting D. mawsoni gene sequences with 692
BLASTN v.2.12.0 [90] and reconstructing the gene structure based on alignment coordinates. Each 693
identified afgp copy was then manually inspected for frameshifts and gaps to identify complete and 694
pseudogenised gene copies. Finally, we used Klumpy [91] with the find_klumps function to verify the 695
completeness of the annotation, using the exon -1 and exon-2 of one randomly chosen functional afgp 696
gene copy previously annotated as query. 697
To infer evolutionary relationships of afgp genes, we used the short exon-1 (signal peptide) and intron-698
1 nucleotide sequences, excluding the highly repetitive exon -2s encoding the AFGP polyprotein, 699
following the Nicodemus -Johnson et al. , (2011) approach. Analysis was performed both with and 700
without the chimeric afgp/tlp genes. Sequences were aligned with MAFFT v.7.525 [92] using the E-701
INS-i. Because afgp and afgp/tlp genes share only exon -1 and an initial part of intron -1, when these 702
latest genes were included in the analyses, we removed the non -homologue region based on visual 703
inspection of the alignme nt. Phylogenetic inference was performed with IQ -TREE 2 [93] with 1,000 704
ultrafast bootstrap replicates [94], to assess nodal support, selecting the best-fit evolutionary model with 705
ModelFinder [95]. 706
Characterization of LINE-L2 elements 707
LINE-L2 insertions annotated on Hap1 and longer than 1,000 bp were extracted with bedtools getfasta 708
and subjected to Blastx ( -evalue 1e -05 –max_target_seqs 1 –max_hsps 1) against all reverse 709
transcriptase (RT) amino acid (aa) sequences that compose the seed alignment of the Reverse 710
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25
transcriptase PFAM [96] profile PF00078. Based on the BLASTX v.2.12.0 [90] alignment coordinates, 711
the amino acid sequences of the RT segments were extracted, discarding those shorter than 100 amino 712
acids. To decrease the size of the dataset for the subsequent phylogenetic analyses all RT segments 713
were clustered at 80% sequence identity with CD -HIT [97] keeping the longest element as 714
representative of the cluster. All representative RT segments together with reference sequences of the 715
LINE-L2, L2A, L2b, Crack, Daphne and CR1 clades described in [25] were aligned with MAFFT in 716
G-INS-i mode and trimmed with Trimal v.1.4.1 [98] in gappyout mode. Phylogenetic inference was 717
performed with IQ-TREE v2.4.0 [93] with 1,000 UltraFast bootstrap replicates to assess nodal support 718
and selecting the best-fit evolutionary model with ModelFinder. 719
CD-HIT [97] clustering identified eight clusters, each comprising between 600 and 3,669 RTs, together 720
accounting for 73% of all extracted RTs longer than 100 aa. The complete insertion corresponding to 721
the representative element of each one of these clusters was used as query in a “Blast-Extend-Extract" 722
analyses [99–101] to reconstruct a consensus sequence representative of the family. The curated 723
consensi were used in an additional RepeatMasker analyses, as previously described. We finally looked 724
for the identified and reconstructed LINE -L2 family across genomes (Table S5) through BLASTN 725
searches requiring an alignment length of at least 500 nucleotides with at least 80% of identity to the 726
query consensus sequence. 727
Haplotype comparison 728
A whole genome alignment of the two haplotypes was performed with Minimap2 v.2.26 [102] and 729
inferred SNPs, SVs (insertions, deletions, and duplications), and rearranged genomic regions 730
(inversions and translocations) between the two haplotypes using Syri v.1.7.1 [103]. In each case Hap1 731
was used as the reference. We identified genes and exons subject to structural v ariation between the 732
two haplotypes by intersecting the gene annotation with Syri-derived SV and rearrangement coordinates 733
using bedtools v2.30 [104] intersect. We tested whether the genomic distribution of SVs, considering 734
only translocations, duplications and inversions, was associated with specific genomic features using a 735
generalized linear mixed model (GLMM) with a binomial error structure. SVs were compared to an 736
equal number of randomized genomic intervals generated with bedtools shuffle. For each interval we 737
quantified the following: distance to the nearest chromosome end, distance to the closest assembly gap, 738
length of the SV, and the proportion of bases within 50 kb flanking windows annotated as TEs, tandem 739
repeats, or LINE elements. All predictors were standardized prior to analysis. The model included 740
chromosome as a random intercept to account for non -independence of intervals on the same 741
chromosome. GLMMs were fitted in R using the lme4 package [105]. Odds ratios and 95% confidence 742
intervals were obtained by exponentiating model coefficients. 743
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26
To identify putative heterozygous TE insertions, we overlapped the RepeatMasker annotations of Hap1 744
and Hap2 with deletions and insertion events, respectively, requiring that both insertions/deletions and 745
the TE annotation overlap by at least 75% of their length. 746
To assess whether the SVs identified between haplotypes might result from assembly errors, we 747
additionally mapped ONT reads back to the assembly with Minimap2 and called heterozygous SVs 748
with Sniffles2 [106]. We then quantified the overlap between the genome -based and read -based 749
heterozygous SVs larger than 50 bp using SURVIVOR [107]. Overlapping SVs genotyped as 750
homozygous for the alternate allele were considered as putative mis-assemblies. 751
Species tree reconstruction and divergence time estimation 752
Divergence times were estimated across a set of genomes of notothenioids, including our newly 753
generated H. antarcticus assembly (Hap1), and 11 publicly available chromosomal assemblies : 754
Cottoperca gobio (Cottoperca trigloides) [23], Notothenia rossii [108], Pseudochaenichthys 755
georgianus [6], Eleginops maclovinus [109], Dissostichus mawsoni [110], Dissostichus eleginoides, 756
Chaenocephalus aceratus [111], Pagothenia borchgrevinki (Trematomus borchgrevinki ) [112], 757
Champsocephalus gunnari, Champsocephalus esox [9], Pogonophryne albipinna [113] (Table S5). 758
Additionally another seven marine temperate and tropical fishes' representative of four, closely related 759
orders (Table S5). 760
First, we manually constructed a topology of the included species following the [6] and [9] inferred 761
phylogenetic relationships. Branch lengths were then estimated using the nucleotide sequences of 762
orthologous single -copy BUSCO genes extracted with BUSCO v.5.7.1 [86] and the 763
actinopterygii_odb10 reference dataset. Briefly, single-copy genes present in all analysed species, were 764
separately aligned using MAFFT [92] with the E -INS-i algorithm. Each alignment was cleaned of 765
ambiguous positions using TrimAl in automated mode, and sequences sharing only a reduced region 766
with the others in the alignment were removed using the parameters -resoverlap 0.8 and -seqoverlap 75. 767
Finally, only alignments with at least 500 positions and for which no sequences were excluded by 768
TrimAl were retained. To reduce computational time, 1,000 alignments were randomly selected, 769
concatenated, and subjected to constrained phylogenetic inference with IQ-TREE v2.4.0, selecting the 770
best-fit evolutionary model with ModelFinder. The resulting tree was dated with LSD2 [114] under a 771
fixed substitution rate using [6] estimates as priors of the following nodes:1) split between Takifugu 772
rubripes and Nelusetta ayraudi from all other species: 94 MYA, 2) notothenioid emergence: 47 MYA, 773
and 3) cryonotothenioid diversification: 10.7 MYA. A neutral substitution rate of notothenioids was 774
obtained by re-running the same analyses on the notothenioid-only subtree and using 4-fold degenerate 775
sites extracted from the BUSCO concatenated alignment. The resulting neutral rate of 3.2E -3 million 776
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27
year was used to translate % of CpG corrected Kimura Divergence of TE landscape profiles into 777
absolute time. 778
Selection analyses 779
Publicly available predicted proteomes of fish species included in divergence time estimation were 780
clustered into orthogroups (OG) with Ortho Finder v2.5.4 [115] in ultra-sensitive mode. We then 781
isolated OGs in which at least one gene for all species was present. Multi-copy OGs (i.e. more than one 782
gene was present for at least one species) were decomposed into single-copy OGs using DISCO [116]. 783
Decomposed and original single-copy OGs were then aligned with Prank v250331 [117] under a codon 784
model, cleaned of ambiguous positions with Gblocks taking into consideration the codon structure [118] 785
and from sequences with high percentage of gappy positions with TrimAl (-resoverlap 0.6 -seqoverlap 786
55) [98]. After filtering, only OGs for which all species were present were kept (i.e. not affected by 787
Trimal filtering) and with an alignment longer than 300 codon positions. IQ-TREE2 v2.4.0 was used to 788
infer gene trees under a GTR+I+G substitution model. Because our aim was to detect genes that might 789
be strictly related to cold adaptation in extant cryonotothenioids, we used aBSREL from the HyPhy 790
package v2.5.8 [119] testing for diversifying selection acting on their stem branch. Prior to this, to 791
ensure that we were testing the same evolutionary event we discarded any gene trees in which 792
cryonotothenioids were not monophyletic and not in a sister relationship with their true temperate 793
notothenioid sister species E. maclovinus using a custom R script. Finally, because aBSREL analyses 794
does not test that selection has not occurred outside tested branches we re-ran it for all genes previously 795
identified as under diversifying selection along the cryonotothenioid stem tagging all temperate-adapted 796
species (including non-cryonotothenioid notothenioids) and all their ancestral branches. OGs that were 797
found to be under positive selection in at least one temperate-adapted branch were then removed from 798
aBSREL significant results on the cryonotothenioid ancestor. GO term enrichment was performed using 799
all genes analysed by aBSREL as background based on EGG -NOG annotation with the TopGO R 800
package [120] with a Fisher exact test and an elim algorithm. 801
Synteny detection and multi-genome alignment of notothenioids 802
The same set of notothenioid genomes included in divergence time estimation was used to infer syntenic 803
relationships based on gene order conservation using GENESPACE v1.2.3 [121] with default 804
parameters and Progressive Cactus v2.9.7 [122] to perform a multi whole-genome alignment. Prior to 805
running Progressive Cactus, the genome assemblies were soft masked with RepeatMasker, using a 806
repeat library generated for each genome using RepeatModeler2 with default parameters. To guide the 807
whole-genome alignment we used the notothenioid -only subtree obtained with the constrained tree 808
search and the 1,000 randomly selected BUSCO genes. 809
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28
We inferred insertion and deletion events along all branches of the species tree with the 810
halBranchMutations function of the HAL package [123]. Net genome gain rates per MY were calculated 811
by subtracting the total number of base pairs involved in deletion events from those involved in insertion 812
events and dividing the result by the branch length in time. Insertions inferred along the H. antarcticus 813
ancestors were then lifted off to the H. antarcticus Hap1 assembly using halLiftover (--noDupes). Due 814
to the fragmentation of the lifted insertions, we merged intervals closer than 100 bp when they derive 815
from the same ancestral insertion events. To detect putative TE -derived insertion events, lifted 816
annotations were intersected with the MCHelper-derived TE annotation requiring a reciprocal overlap 817
of the TE annotation and lifted insertion of 75%. PhyloFit from the PHAST package v1.5 [124] was 818
used under a REV substitution model to train an initial non-conserved model of evolution on the same 819
set of 4 -fold degenerate sites extracted from BUSCO genes that was used to estimate the neutral 820
substitution rate. PhastCons was then applied to a MAF representation of the whole -genome multiple 821
alignment, generated with cactus-hal2maf using H. antarcticus as the reference genome (--noAncestors 822
--refGenome HarAnt1.hap1 --dupeMode single), to refine the non -conserved model and train a 823
conserved model for each chromosome. Parameters from the per -chromosome conserved and non -824
conserved models were then averaged using PhyloBoot, and PhastCons was re -run to predict discrete 825
Conserved Elements (CEs). CEs closer than 5 bp were then merged into single elements. To identify 826
CEs shared by all analysed notothenioids, and those that emerged along the cryonotothenioid stem 827
branch, we used halAlignmentDepth to calculate per -base alignment depth for the H. antarcticus 828
genome. Elements covered over at least 75% of their length by all other notothenioids were considered 829
ancestrally present, whereas elements covered over at least 75% of their length only by 830
cryonotothenioids were considered to have been acquired along their stem branch. We assigned each 831
CE to different genomic features (exons, introns, promoters, transcription terminating site , and 832
intergenic regions) with the HOMER annotatePeaks.pl script [125]. GO term enrichment analyses was 833
performed similarly to what was performed for selection analyses but using all H. antarcticus genes as 834
background. 835
Supplementary Material 836
Supplementary Figures 837
Supplementary Tables 838
Data availability 839
The datasets generated in the present study have been submitted on NCBI and will become public 840
upon acceptance for publication. Biosample: SAMEA104132831. 841
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29
Acknowledgments 842
We thank the Wellcome Sanger Institute DNA pipelines for support with sequencing data generation 843
of the H. antarcticus genome. We would like to thank the Rothera Marine Team for sample collection. 844
IB and JM were supported by the Centre for Translational Biodiversity Genomics (LOEWE -TBG) 845
funded through the program LOEWE –Landes-Offensive zur Entwicklung Wissenschaftlich -846
ökonomischer Exzellenz of Hesse's Ministry of Higher Education, Research, and the Arts. NF and DB 847
were supported by NIH grant R35 GM144336. 848
Competing Interests 849
The authors declare that they have no competing interests. 850
Author Contributions 851
I.B. conceptualised the study and supervised the work. I.B., J.M. designed analysis. A.D., M.S.C., N.F., 852
I.B., generated data. I.B., R.D., D.L.B., N.F. contributed resources, K.K. performed genome assembly, 853
T.M., J.M.D.W. performed genome curation, J.M. performed data analysis, with J.M.D.W input. J.M. 854
and I.B. wrote the original manuscript with contributions from M.S.C. All co -authors read, provided 855
feedback, and approved the manuscript. 856
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30
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