Have historical climate changes affected Gentoo penguin (Pygoscelis papua) populations in Antarctica?

• Published in: PLoS ONE
• Main Authors: Fabiola Peña M, Elie Poulin, Gisele P M Dantas, Daniel González-Acuña, Maria Virginia Petry, Juliana A Vianna
• Format: Article in Journal/Newspaper
• Language: English
• Published: Public Library of Science (PLoS) 2014
• Subjects: Medicine; R; Science; Q; Antarctic; Antarctic Peninsula; Sandwich Islands; South Shetland Islands; The Antarctic; Adelie penguin; Antarc*; Antarctica; Gentoo penguin; Ice Sheet; Pygoscelis papua; Sea ice
• Online Access: https://doi.org/10.1371/journal.pone.0095375; https://doaj.org/article/479ba51509fd43e793e129c89eaa8486

The West Antarctic Peninsula (WAP) has been suffering an increase in its atmospheric temperature during the last 50 years, mainly associated with global warming. This increment of temperature trend associated with changes in sea-ice dynamics has an impact on organisms, affecting their phenology, physiology and distribution range. For instance, rapid demographic changes in Pygoscelis penguins have been reported over the last 50 years in WAP, resulting in population expansion of sub-Antarctic Gentoo penguin (P. papua) and retreat of Antarctic Adelie penguin (P. adeliae). Current global warming has been mainly associated with human activities; however these climate trends are framed in a historical context of climate changes, particularly during the Pleistocene, characterized by an alternation between glacial and interglacial periods. During the last maximal glacial (LGM∼21,000 BP) the ice sheet cover reached its maximum extension on the West Antarctic Peninsula (WAP), causing local extinction of Antarctic taxa, migration to lower latitudes and/or survival in glacial refugia. We studied the HRVI of mtDNA and the nuclear intron βfibint7 of 150 individuals of the WAP to understand the demographic history and population structure of P. papua. We found high genetic diversity, reduced population genetic structure and a signature of population expansion estimated around 13,000 BP, much before the first paleocolony fossil records (∼1,100 BP). Our results suggest that the species may have survived in peri-Antarctic refugia such as South Georgia and North Sandwich islands and recolonized the Antarctic Peninsula and South Shetland Islands after the ice sheet retreat.