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No barrier to emergence of bathyal king crabs on the Antarctic shelf

Journal article
Authors Richard Aronson
KE Smith
SC Vos
JB McClintock
MO Amsler
Per-Olav Moksnes
DS Ellis
JW Kaeli
H Singh
John W Bailey
Jessica C Schiferi
Robert Woesik van
Michael A Martin
Brittan V Steffel
Michelle E Deal
Steven M Lazarus
Jonathan N. Havenhand
Rasmus Swalethorp
Sanne Kjellerup
S Thatje
Published in Proceedings of the National Academy of Science of the United States of America
Volume 112
Issue 42
Pages 12997-13002
ISSN 0027-8424
Publication year 2015
Published at Department of marine sciences
Pages 12997-13002
Language en
Keywords biological invasion, polar emergence, climate change, predation, Southern Ocean
Subject categories Marine ecology


Cold-water conditions have excluded durophagous (skeleton-breaking) predators from the Antarctic seafloor for millions of years. Rapidly warming seas off the western Antarctic Peninsula could now facilitate their return to the continental shelf, with profound consequences for the endemic fauna. Among the likely first arrivals are king crabs (Lithodidae), which were discovered recently on the adjacent continental slope. During the austral summer of 2010‒2011, we used underwater imagery to survey a slope-dwelling population of the lithodid Paralomis birsteini off Marguerite Bay, western Antarctic Peninsula for environmental or trophic impediments to shoreward expansion. The population density averaged ∼4.5 individuals × 1,000 m−2 within a depth range of 1,100‒1,500 m (overall observed depth range 841–2,266 m). Images of juveniles, discarded molts, and precopulatory behavior, as well as gravid females in a trapping study, suggested a reproductively viable population on the slope. At the time of the survey, there was no thermal barrier to prevent the lithodids from expanding upward and emerging on the outer shelf (400- to 550-m depth); however, near-surface temperatures remained too cold for them to survive in inner-shelf and coastal environments (<200 m). Ambient salinity, composition of the substrate, and the depth distribution of potential predators likewise indicated no barriers to expansion of lithodids onto the outer shelf. Primary food resources for lithodids—echinoderms and mollusks—were abundant on the upper slope (550–800 m) and outer shelf. As sea temperatures continue to rise, lithodids will likely play an increasingly important role in the trophic structure of subtidal communities closer to shore.

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