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Marine Biology

, Volume 160, Issue 8, pp 1963–1972 | Cite as

The swimming kinematics of larval Atlantic cod, Gadus morhua L., are resilient to elevated seawater pCO2

  • R. H. Maneja
  • A. Y. Frommel
  • H. I. Browman
  • C. Clemmesen
  • A. J. Geffen
  • A. Folkvord
  • U. Piatkowski
  • C. M. F. Durif
  • R. Bjelland
  • A. B. Skiftesvik
Original Paper

Abstract

Kinematics of swimming behavior of larval Atlantic cod, aged 12 and 27 days post-hatch (dph) and cultured under three pCO2 conditions (control-370, medium-1800, and high-4200 μatm) from March to May 2010, were extracted from swim path recordings obtained using silhouette video photography. The swim paths were analyzed for swim duration, distance and speed, stop duration, and horizontal and vertical turn angles to determine whether elevated seawater pCO2—at beyond near-future ocean acidification levels—affects the swimming kinematics of Atlantic cod larvae. There were no significant differences in most of the variables tested: the swimming kinematics of Atlantic cod larvae at 12 and 27 dph were highly resilient to extremely elevated pCO2 levels. Nonetheless, cod larvae cultured at the highest pCO2 concentration displayed vertical turn angles that were more restricted (median turn angle, 15°) than larvae in the control (19°) and medium (19°) treatments at 12 dph (but not at 27 dph). Significant reduction in the stop duration of cod larvae from the high treatment (median stop duration, 0.28 s) was also observed compared to the larvae from the control group (0.32 s) at 27 dph (but not at 12 dph). The functional and ecological significance of these subtle differences are unclear and, therefore, require further investigation in order to determine whether they are ecologically relevant or spurious.

Keywords

Ocean Acidification Swimming Behavior Turn Angle Move Duration High pCO2 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

Notes

Acknowledgments

Funding support was provided through the European Marie Curie Initial Training Network “Calcification by Marine Organisms” (CalMarO) and the European Community’s Seventh Framework Programme (FP7/2007-2013) “European Project on Ocean Acidification” (EPOCA, grant agreement N211384). The study was also supported by the project “Biological Impacts of Ocean ACIDification” (BIOACID), funded by the German Ministry for Education and Research (BMBF), and by the Norwegian Institute of Marine Research (“Fine-scale behavioral interactions in the plankton” and “Biological effects of ocean acidification” projects to HIB). The experiments were conducted at the Norwegian National Mesocosm Centre, Espegrend, in cooperation with the Department of Biology, University of Bergen and at the Institute of Marine Research’s Austevoll Research Station.

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Copyright information

© Springer-Verlag 2012

Authors and Affiliations

  • R. H. Maneja
    • 1
  • A. Y. Frommel
    • 1
  • H. I. Browman
    • 2
  • C. Clemmesen
    • 1
  • A. J. Geffen
    • 3
  • A. Folkvord
    • 3
  • U. Piatkowski
    • 1
  • C. M. F. Durif
    • 2
  • R. Bjelland
    • 2
  • A. B. Skiftesvik
    • 2
  1. 1.Helmholtz-Zentrum für Ozeanforschung Kiel-GEOMARKielGermany
  2. 2.Institute of Marine ResearchAustevoll Research StationStorebøNorway
  3. 3.Department of BiologyUniversity of BergenBergenNorway

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