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Melendez-Vazquez, F.

Publications and source records attributed to Melendez-Vazquez, F..

3 recordsLinked to original sources

Independent origins of fish endothermy converge on a developmental regulatory signature

Why independent origins of the same complex physiological trait repeatedly produce similar body forms and physiological changes remains central in evolutionary biology. Endothermy, the internal production and retention of metabolic heat, evolved at least four times in ray-finned fishes, providing natural replicates for convergent genomic signatures. We present a chromosome-scale analysis of three transitions (opah, tunas, and swordfish), including a new chromosome-level genome of the rare, charismatic Pacific oarfish, analyzed with 31 other teleost genomes. The strongest signal is regulatory: of 253,680 conserved noncoding elements, 577 are rate-accelerated in endothermic lineages, with 67 accelerated in all three, exceeding matched ectothermic controls and enriched near developmental transcription factors and Wnt-signaling genes (e.g., irx1a, irx5a, her9, and lmo1). These elements overlap zebrafish developmental enhancers more than expected by chance but are not tied to genes emphasized by expression or coding-selection studies of endothermic lineages, marking a regulatory layer distinct from that metabolic layer. This convergence is part of a broader mosaic: endothermic lineages also share transition-biased substitution and convergent duplication signatures, including excess tandem duplications and lineage-specific gene-family expansion, whereas chromosome organization and protein-coding sequence change little. Endothermic convergence therefore leaves its clearest signal in regulatory remodeling, alongside shifts in substitution bias and gene-family evolution.

evolutionary biology↗

Competition among freshwater clades explains cave colonization in blind cavefishes

Flatfishes display the most dramatic asymmetric body plan in vertebrates, yet whether this rare innovation evolved once (flatfish monophyly, FM) or multiple times (flatfish polyphyly, FP) has remained contentious. A recent genome-wide study supported FP by placing Psettodes, the earliest-diverging flatfish lineage, among symmetric relatives within Carangaria, the clade that also includes billfishes, jacks, mahi-mahi, and barracudas. Subsequent work traced this to base-composition artifacts and inadequate substitution modeling. Here we revisit the question using whole-genome phylogenomic and synteny data from 17 carangarian species spanning flatfishes and carangarian relatives. We contribute three new chromosome-level assemblies, including the first for Psettodes. Nucleotide-based coalescent analyses (e.g., ROADIES, CASTER) yield strong support for FM, with Psettodes sister to all other flatfishes. Microsynteny analyses built from conserved gene-order blocks corroborate this result: topology tests, cluster-profile counts, and rearrangement-based trees favor FM over two competing FP topologies. Macrosynteny, based on chromosome-scale rearrangements, yields a more mixed signal, with support for FM depending on the metric and taxon-sampling scheme. We interpret this scale-dependent pattern in the context of the explosive post-Cretaceous radiation of Carangaria. The short intervals between speciation events that characterize rapid radiations appear to have left sufficient signal in fine-grained microsyntenic rearrangements, while chromosome-scale rearrangements were too rare to consistently resolve these closely spaced splits. When integrated with evidence from conserved developmental mechanisms active during metamorphosis, the stage at which flatfish asymmetry first emerges, and from the exceptionally complete fossil record, our multi-scale genomic evidence supports a single evolutionary origin of flatfish asymmetry.

evolutionary biology↗

Ancient climate changes and relaxed selection shape cave colonisation in North American cavefishes

Extreme environments serve as natural laboratories for studying evolutionary processes, with caves offering replicated instances of independent colonisations. The timing, mode, and genetic underpinnings underlying cave-obligate organismal evolution remains enigmatic. We integrate phylogenomics, fossils, paleoclimatic modeling, and newly sequenced genomes to elucidate the evolutionary history and adaptive processes of cave colonisation in the study group, the North American Amblyopsidae fishes. Amblyopsid fishes present a unique system for investigating cave evolution, encompassing surface, facultative cave-dwelling, and cave-obligate (troglomorphic) species. Using 1,105 exon markers and total-evidence dating, we reconstructed a robust phylogeny that supports the nested position of eyed, facultative cave-dwelling species within blind cavefishes. We identified three independent cave colonisations, dated to the Early Miocene (18.5 Mya), Late Miocene (10.0 Mya), and Pliocene (3.0 Mya). Evolutionary model testing supported a climate-relict hypothesis, suggesting that global cooling trends since the Early-Middle Eocene may have influenced cave colonisation. Comparative genomic analyses of 487 candidate genes revealed both relaxed and intensified selection on troglomorphy-related loci. We found more loci under relaxed selection, supporting neutral mutation as a significant mechanism in cave-obligate evolution. Our findings provide empirical support for climate-driven cave colonisation and offer insights into the complex interplay of selective pressures in extreme environments.

evolutionary biology↗