Contrasting processes drive ophiuroid phylodiversity across shallow and deep seafloors

• Published in: Nature (London) 2019-01, Vol.565 (7741), p.636-639
• Main Authors: O’Hara, Timothy D., Hugall, Andrew F., Woolley, Skipton N. C., Bribiesca-Contreras, Guadalupe, Bax, Nicholas J.
• Format: Article
• Language: English
• Subjects: 45/23; 704/158/851; 704/158/852; 704/158/857; 704/829/826; Analysis; Animal Migration; Animals; Biodiversity; Bioinformatics; Brittle stars; Cenozoic; Cluster analysis; Deep sea; Deep sea environments; Distribution; Ecosystems; Emigration and immigration; Endangered & extinct species; Equator; Evolution; Exchanging; Extinction; Fauna; Geologic Sediments; Humanities and Social Sciences; Immigration; Invertebrates; Latitude; Letter; Local extinction; multidisciplinary; Ocean floor; Oceans and Seas; Phylogenetics; Phylogeny; Polar waters; Science; Science (multidisciplinary); Shallow water; Southern Hemisphere
• ISSN: 0028-0836; 1476-4687
• DOI: 10.1038/s41586-019-0886-z

Our knowledge of the distribution and evolution of deep-sea life is limited, impeding our ability to identify priority areas for conservation 1 . Here we analyse large integrated phylogenomic and distributional datasets of seafloor fauna from the sea surface to the abyss and from equator to pole of the Southern Hemisphere for an entire class of invertebrates (Ophiuroidea). We find that latitudinal diversity gradients are assembled through contrasting evolutionary processes for shallow (0–200 m) and deep (>200 m) seas. The shallow-water tropical–temperate realm broadly reflects a tropical diversification-driven process that shows exchange of lineages in both directions. Diversification rates are reversed for the realm that contains the deep sea and Antarctica; the diversification rates are highest at polar and lowest at tropical latitudes, and net exchange occurs from high to low latitudes. The tropical upper bathyal (200–700 m deep), with its rich ancient phylodiversity, is characterized by relatively low diversification and moderate immigration rates. Conversely, the young, specialized Antarctic fauna is inferred to be rebounding from regional extinctions that are associated with the rapid cooling of polar waters during the mid-Cenozoic era. Our knowledge of the distribution and evolution of deep-sea life is limited, impeding our ability to identify priority areas for conservation.