Abstract

Specific changes identified in the otolith macrostructure of Northeast Arctic cod as "spawning zones" are presumed to represent spawning events, but recent experimental studies have challenged this relationship. Because these zones are not routinely recorded outside of Norway, otoliths from multiple Atlantic cod populations with different life history and environmental traits were first examined to see if spawning zones could be identified as a general characteristic of cod. Then, a large archival collection of cod otoliths was used to investigate temporal changes in the occurrence of spawning zones and test for correlations between maturity at age derived from otolith spawning zones and gonad maturity stages. This study shows that spawning zones likely are a universal trait of Atlantic cod and not limited to certain environments or migratory behaviors as previously proposed. Maturity at age derived from spawning zone data showed trends consistent with those from gonad examinations. However, spawning zones appear to form with a one- or two-year lag with sexual maturity, which is suspected to reflect a stabilizing of energy partitioning after the first spawning events. Our results illustrate the potential for use of spawning zones, for example in species or populations with limited available maturity data, and highlights the need for addressing the physiological processes behind their formation.

Highlights

  • Otoliths have been widely used in fisheries research since the mid-20th century [1]

  • We aimed to investigate whether spawning zones could be reliably identified in multiple Atlantic cod populations from different environmental conditions and life histories

  • Definition and comparison of spawning zone occurrence across cod populations The visual criteria commonly used for determining spawning zones were checked on a random subsample of 56 previously read Northeast Arctic (NEA) cod otoliths

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Summary

Introduction

Otoliths have been widely used in fisheries research since the mid-20th century [1]. Otolith growth increments result from rhythmic variations in the accretion rates of both calcium carbonate crystals and an organic matrix [2], which is influenced by variability in temperature, food consumption and metabolism.

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