Stable oxygen isotope reconstruction of temperature exposure of the Icelandic cod (Gadus morhua) stock over the last 100 years

Publisher's version (útgefin grein) Increasing water temperatures are predicted around the globe, with high amplitudes of warming in Subarctic and Arctic regions where Atlantic cod (Gadus morhua) populations currently flourish. We reconstructed oxygen isotope and temperature chronologies from I...

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Bibliographic Details
Published in:ICES Journal of Marine Science
Main Authors: von Leesen, Gotje, Ninnemann, Ulysses S., Campana, Steven
Other Authors: Líf- og umhverfisvísindadeild (HÍ), Faculty of Life and Environmental Sciences (UI), Verkfræði- og náttúruvísindasvið (HÍ), School of Engineering and Natural Sciences (UI), Háskóli Íslands, University of Iceland
Format: Article in Journal/Newspaper
Language:English
Published: Oxford University Press (OUP) 2020
Subjects:
Ecology
Aquatic Science
Oceanography
Þorskur
Haffræði
Loftslagsbreytingar
Norður-heimskautið
Sjávarhiti
Arctic
Norway
atlantic cod
Gadus morhua
Iceland
Subarctic
Online Access:https://hdl.handle.net/20.500.11815/1923
https://doi.org/10.1093/icesjms/fsaa011
Description
Summary:Publisher's version (útgefin grein) Increasing water temperatures are predicted around the globe, with high amplitudes of warming in Subarctic and Arctic regions where Atlantic cod (Gadus morhua) populations currently flourish. We reconstructed oxygen isotope and temperature chronologies from Icelandic cod otoliths, one of the largest cod stocks in the world, to determine if cod moved or migrated over the last 100 years to avoid increasing water temperatures. For δ18Ootolith analysis, individual annual growth increments from immature and mature life history stages were micromilled from adult otoliths, which were collected in southern Iceland. Linear mixed-effect models confirmed that stable oxygen isotope time series of immature and mature cod differ significantly between both life stages (p < 0.001). Overall, cod otolith δ18O was significantly correlated with water temperature (sea surface temperature: p < 0.001, temperature at 200 m depth: p < 0.01), indicating that Atlantic cod were exposed to fluctuating water temperatures during the past 100 years and did not move as a response to increasing ocean temperatures. All of the alternate physical factors that were considered for the isotope-based variation in the temperature exposure of Icelandic cod were rejected. Funding for this study was provided by Icelandic Research Fund Grant 173906-051. Establishment funding for FARLAB (Facility for advanced isotopic research and monitoring of weather, climate, and biogeochemical cycling) by Research Council Norway Grant 245907 is also acknowledged. Peer reviewed

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