Genome-wide analyses reveal drivers of penguin diversification

Author:

Vianna Juliana A.ORCID,Fernandes Flávia A. N.ORCID,Frugone María JoséORCID,Figueiró Henrique V.,Pertierra Luis R.ORCID,Noll Daly,Bi Ke,Wang-Claypool Cynthia Y.,Lowther Andrew,Parker Patricia,Le Bohec CelineORCID,Bonadonna Francesco,Wienecke Barbara,Pistorius PierreORCID,Steinfurth Antje,Burridge Christopher P.,Dantas Gisele P. M.,Poulin ElieORCID,Simison W. Brian,Henderson Jim,Eizirik EduardoORCID,Nery Mariana F.,Bowie Rauri C. K.ORCID

Abstract

Penguins are the only extant family of flightless diving birds. They currently comprise at least 18 species, distributed from polar to tropical environments in the Southern Hemisphere. The history of their diversification and adaptation to these diverse environments remains controversial. We used 22 new genomes from 18 penguin species to reconstruct the order, timing, and location of their diversification, to track changes in their thermal niches through time, and to test for associated adaptation across the genome. Our results indicate that the penguin crown-group originated during the Miocene in New Zealand and Australia, not in Antarctica as previously thought, and thatAptenodytesis the sister group to all other extant penguin species. We show that lineage diversification in penguins was largely driven by changing climatic conditions and by the opening of the Drake Passage and associated intensification of the Antarctic Circumpolar Current (ACC). Penguin species have introgressed throughout much of their evolutionary history, following the direction of the ACC, which might have promoted dispersal and admixture. Changes in thermal niches were accompanied by adaptations in genes that govern thermoregulation and oxygen metabolism. Estimates of ancestral effective population sizes (Ne) confirm that penguins are sensitive to climate shifts, as represented by three different demographic trajectories in deeper time, the most common (in 11 of 18 penguin species) being an increasedNebetween 40 and 70 kya, followed by a precipitous decline during the Last Glacial Maximum. The latter effect is most likely a consequence of the overall decline in marine productivity following the last glaciation.

Funder

MINEDUC | Comisión Nacional de Investigación Científica y Tecnológica

Instituto Antartico Chileno

NSF | National Science Board

French Polar Institute Paul-Emile Victor

California Academy os Science

Publisher

Proceedings of the National Academy of Sciences

Subject

Multidisciplinary

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