It’s elemental, my dear Watson: validating seasonal patterns in otolith chemical chronologies

Author:

Hüssy Karin1,Krüger-Johnsen Maria1,Thomsen Tonny Bernt2,Heredia Benjamin Dominguez2,Næraa Tomas3,Limburg Karin E.45,Heimbrand Yvette5,McQueen Kate6,Haase Stefanie6,Krumme Uwe6,Casini Michele57,Mion Monica5,Radtke Krzysztof8

Affiliation:

1. National Institute of Aquatic Resources, Technical University of Denmark, Kemitorvet, DK-2800 Kgs. Lyngby, Denmark.

2. Geological Survey of Denmark and Greenland, Øster Voldgade 10, DK-1350 Copenhagen K., Denmark.

3. Lund University, Department of Geology, Sølvegatan 12, SE-22362 Lund, Sweden.

4. State University of New York College of Environmental Science and Forestry, Syracuse, NY 13210, USA.

5. Department of Aquatic Resources, Institute of Marine Research, Swedish University of Agricultural Sciences, Turistgatan 5, SE-453 30 Lysekil, Sweden.

6. Thünen Institute of Baltic Sea Fisheries, Alter Hafen Süd 2, D-18069 Rostock, Germany.

7. Department of Biological, Geological and Environmental Sciences, University of Bologna, Via Selmi 3, IT-40126 Bologna, Italy.

8. National Marine Fisheries Research Institute, Ul. Kołłątaja 1, 81-332 Gdynia, Poland.

Abstract

Accurate age data are essential for reliable fish stock assessment. Yet many stocks suffer from inconsistencies in age interpretation. A new approach to obtain age makes use of the chemical composition of otoliths. This study validates the periodicity of recurrent patterns in 25Mg, 31P, 34K, 55Mn, 63Cu, 64Zn, 66Zn, 85Rb, 88Sr, 138Ba, and 208Pb in Baltic cod (Gadus morhua) otoliths from tag–recapture and known-age samples. Otolith P concentrations showed the highest consistency in seasonality over the years, with minima co-occurring with otolith winter zones in the known-age otoliths and in late winter – early spring when water temperatures are coldest in tagged cod . The timing of minima differs between stocks, occurring around February in western Baltic cod and 1 month later in eastern Baltic cod; seasonal maxima are also stock-specific, occurring in August and October, respectively. The amplitude in P is larger in faster-growing western compared with eastern Baltic cod. Seasonal patterns with minima in winter – late spring were also evident in Mg and Mn, but less consistent over time and fish size than P. Chronological patterns in P, and to a lesser extent Mg and Mn, may have the potential to supplement traditional age estimation or to guide the visual identification of translucent and opaque otolith patterns used in traditional age estimation.

Publisher

Canadian Science Publishing

Subject

Aquatic Science,Ecology, Evolution, Behavior and Systematics

Reference79 articles.

1. The Legacy of Hypoxia: Tracking Carryover Effects of Low Oxygen Exposure in a Demersal Fish Using Geochemical Tracers

2. Proportions of demersal fish exposed to sublethal hypoxia revealed by otolith chemistry

3. Beckman, D., and Wilson, C.A. 1995. Seasonal timing of opaque zone formation in fish otoliths. In Recent developments in fish otolith research. Edited by D.H. Secor, J.M. Dean, and S.E. Campana. University of South Carolina Press, Columbia, S.C. pp. 27–44.

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