Return of large fin whale feeding aggregations to historical whaling grounds in the Southern Ocean

Fin whales (Balaenoptera physalus quoyi) of the Southern Hemisphere were brought to near extinction by twentieth century industrial whaling. For decades, they had all but disappeared from previously highly frequented feeding grounds in Antarctic waters. Our dedicated surveys now confirm their return...

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Bibliographic Details
Published in:Scientific Reports
Main Authors: Herr, Helena, Viquerat, Sacha, Devas, Fredi, Lees, Abigail, Wells, Lucy, Gregory, Bertie, Giffords, Ted, Beecham, Dan, Meyer, Bettina
Format: Article in Journal/Newspaper
Language:unknown
Published: Nature 2022
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Online Access:https://epic.awi.de/id/eprint/56676/
https://epic.awi.de/id/eprint/56676/1/Herr_etal_2022.pdf
https://hdl.handle.net/10013/epic.f264677f-d20e-4ab0-87b4-8fe5818d4fa8
https://hdl.handle.net/
Description
Summary:Fin whales (Balaenoptera physalus quoyi) of the Southern Hemisphere were brought to near extinction by twentieth century industrial whaling. For decades, they had all but disappeared from previously highly frequented feeding grounds in Antarctic waters. Our dedicated surveys now confirm their return to ancestral feeding grounds, gathering at the Antarctic Peninsula in large aggregations to feed. We report on the results of an abundance survey and present the first scientific documentation of large fin whale feeding aggregations at Elephant Island, Antarctica, including the first ever video documentation. We interpret high densities, re-establishment of historical behaviours and the return to ancestral feeding grounds as signs for a recovering population. Recovery of a large whale population has the potential to augment primary productivity at their feeding grounds through the effects of nutrient recycling, known as 'the whale pump'. The recovery of fin whales in that area could thus restore ecosystem functions crucial for atmospheric carbon regulation in the world's most important ocean region for the uptake of anthropogenic CO2.