| Literature DB >> 29133903 |
Bettina Meyer1,2,3, Ulrich Freier4,5, Volker Grimm6, Jürgen Groeneveld7, Brian P V Hunt8,9,10, Sven Kerwath11,12,13, Rob King14, Christine Klaas4, Evgeny Pakhomov8,10, Klaus M Meiners14,15, Jessica Melbourne-Thomas14,15, Eugene J Murphy16, Sally E Thorpe16, Sharon Stammerjohn17, Dieter Wolf-Gladrow18, Lutz Auerswald11,13, Albrecht Götz19,20,21, Laura Halbach4, Simon Jarman14,22, So Kawaguchi14,15, Thomas Krumpen23, Gernot Nehrke18, Robert Ricker23, Michael Sumner14,15, Mathias Teschke4, Rowan Trebilco15, Noyan I Yilmaz24.
Abstract
A dominant Antarctic ecological paradigm suggests that winter sea ice is generally the main feeding ground for krill larvae. Observations from our winter cruise to the southwest Atlantic sector of the Southern Ocean contradict this view and present the first evidence that the pack-ice zone is a food-poor habitat for larval development. In contrast, the more open marginal ice zone provides a more favourable food environment for high larval krill growth rates. We found that complex under-ice habitats are, however, vital for larval krill when water column productivity is limited by light, by providing structures that offer protection from predators and to collect organic material released from the ice. The larvae feed on this sparse ice-associated food during the day. After sunset, they migrate into the water below the ice (upper 20 m) and drift away from the ice areas where they have previously fed. Model analyses indicate that this behaviour increases both food uptake in a patchy food environment and the likelihood of overwinter transport to areas where feeding conditions are more favourable in spring.Entities:
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Year: 2017 PMID: 29133903 DOI: 10.1038/s41559-017-0368-3
Source DB: PubMed Journal: Nat Ecol Evol ISSN: 2397-334X Impact factor: 15.460