Synonymization of two, monotypic black-coral-commensal scale worm genera, Antipathipolyeunoa Pettibone, 1991 and Parahololepidella Pettibone, 1969 (Polynoidae, Aphroditiformia)

Parahololepidella Pettibone, 1969 is a polynoid genus commensal with the antipatharian genus Tanacetipathes Opresko, 2001. These scale worms are elongate with numerous segments and small elytra. To date, the only other known polynoid associated with Tanacetipathes is Antipathipolyeunoa Pettibone, 1991. By re-examining the holotype of Antipathipolyeunoa, we have identified several overlooked characters that no longer distinguish this genus from Parahololepidella. Based on the presence of chaetae on the tentacular segment and elytral irregularity on posterior segments, we propose synonymizing Antipathipolyeunoa with Parahololepidella.

Genomic analysis of a scale worm provides insights into its adaptation to deep-sea hydrothermal vents

Deep-sea polynoid scale worms endemic to hydrothermal vents have evolved an adaptive strategy to the chronic hypoxic environment, but its underlying molecular mechanisms remain elusive. Here, we assembled a chromosome-scale genome of a vent-endemic scale worm Branchipolynoe longqiensis (first annotated genome in the subclass Errantia) and annotated two shallow-water polynoid genomes aiming to elucidate the adaptive mechanisms. We present a genome-wide molecular phylogeny in Annelida and call for extensive taxonomy revision by including more genomes from key lineages. The B. longqiensis genome with a genome size of 1.86 Gb and 18 pseudo-chromosomes is larger than the genomes of two shallow-water polynoids, possibly due to the expansion of various transposable elements (TEs) and transposons. We revealed three inter-chromosomal rearrangements in B. longqiensis when compared to the other two polynoid genomes. The intron elongation and inter-chromosomal rearrangement can influence a number of biological processes, such as vesicle transport, microtubules, and transcription factors. Furthermore, the expansion of cytoskeleton-related gene families may favor the cell structure maintenance of B. longqiensis in the deep ocean. The expansion of synaptic vesicle exocytosis genes has possibly contributed to the unique complex structure of the nerve system in B. longqiensis. Finally, we uncovered an expansion of single-domain hemoglobin and an unique formation of tetra-domain hemoglobin via tandem duplications which may be related to the adaptation to a hypoxic environment.

Origin, diversity, and biogeography of Antarctic scale worms (Polychaeta: Polynoidae): a wide-scale barcoding approach

The Antarctic marine environment hosts diversified and highly endemic benthos owing to its unique geologic and climatic history. Current warming trends have increased the urgency of understanding Antarctic species history to predict how environmental changes will impact ecosystem functioning. Antarctic benthic lineages have traditionally been examined under three hypotheses: (1) high endemism and local radiation, (2) emergence of deep‐sea taxa through thermohaline circulation, and (3) species migrations across the Polar Front. In this study, we investigated which hypotheses best describe benthic invertebrate origins by examining Antarctic scale worms (Polynoidae). We amassed 691 polynoid sequences from the Southern Ocean and neighboring areas: the Kerguelen and Tierra del Fuego (South America) archipelagos, the Indian Ocean, and waters around New Zealand. We performed phylogenetic reconstructions to identify lineages across geographic regions, aided by mitochondrial markers cytochrome c oxidase subunit I (Cox1) and 16S ribosomal RNA (16S). Additionally, we produced haplotype networks at the species scale to examine genetic diversity, biogeographic separations, and past demography. The Cox1 dataset provided the most illuminating insights into the evolution of polynoids, with a total of 36 lineages identified. Eunoe sp. was present at Tierra del Fuego and Kerguelen, in favor of the latter acting as a migration crossroads. Harmothoe fuligineum, widespread around the Antarctic continent, was also present but isolated at Kerguelen, possibly resulting from historical freeze–thaw cycles. The genus Polyeunoa appears to have diversified prior to colonizing the continent, leading to the co‐occurrence of at least three cryptic species around the Southern and Indian Oceans. Analyses identified that nearly all populations are presently expanding following a bottleneck event, possibly caused by habitat reduction from the last glacial episodes. Findings support multiple origins for contemporary Antarctic polynoids, and some species investigated here provide information on ancestral scenarios of (re)colonization. First, it is apparent that species collected from the Antarctic continent are endemic, as the absence of closely related species in the Kerguelen and Tierra del Fuego datasets for most lineages argues in favor of Hypothesis 1 of local origin. Next, Eunoe sp. and H. fuligineum, however, support the possibility of Kerguelen and other sub‐Antarctic islands acting as a crossroads for larvae of some species, in support of Hypothesis 3. Finally, the genus Polyeunoa, conversely, is found at depths greater than 150 m and may have a deep origin, in line with Hypothesis 2. These “non endemic” groups, nevertheless, have a distribution that is either north or south of the Antarctic Polar Front, indicating that there is still a barrier to dispersal, even in the deep sea.