Highly structured populations of copepods at risk to deep‐sea mining: Integration of genomic data with demogenetic and biophysical modelling

Copepoda is the most abundant taxon in deep‐sea hydrothermal vents, where hard substrate is available. Despite the increasing interest in seafloor massive sulphides exploitation, there have been no population genomic studies conducted on vent meiofauna, which are known to contribute over 50% to meta...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Molecular ecology 2024-05, Vol.33 (9), p.e17340-n/a
Hauptverfasser: Diaz‐Recio Lorenzo, Coral, Tran Lu Y, Adrien, Brunner, Otis, Arbizu, Pedro Martínez, Jollivet, Didier, Laurent, Stefan, Gollner, Sabine
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Beschreibung
Zusammenfassung:Copepoda is the most abundant taxon in deep‐sea hydrothermal vents, where hard substrate is available. Despite the increasing interest in seafloor massive sulphides exploitation, there have been no population genomic studies conducted on vent meiofauna, which are known to contribute over 50% to metazoan biodiversity at vents. To bridge this knowledge gap, restriction‐site‐associated DNA sequencing, specifically 2b‐RADseq, was used to retrieve thousands of genome‐wide single‐nucleotide polymorphisms (SNPs) from abundant populations of the vent‐obligate copepod Stygiopontius lauensis from the Lau Basin. SNPs were used to investigate population structure, demographic histories and genotype–environment associations at a basin scale. Genetic analyses also helped to evaluate the suitability of tailored larval dispersal models and the parameterization of life‐history traits that better fit the population patterns observed in the genomic dataset for the target organism. Highly structured populations were observed on both spatial and temporal scales, with divergence of populations between the north, mid, and south of the basin estimated to have occurred after the creation of the major transform fault dividing the Australian and the Niuafo'ou tectonic plate (350 kya), with relatively recent secondary contact events (
ISSN:0962-1083
1365-294X
DOI:10.1111/mec.17340