Abstract

AbstractThe lack of any abundant recruiting year class of Norwegian spring-spawning (NSS) herring between 2005 and 2015 contributed to an approximate reduction of 40% in the spawning-stock biomass since 2009, i.e. from 7 to 4 million tonnes. Warming of the North Atlantic is suggested to contribute to this reduction in recruitment. In the past, a warm phase induced by a positive Atlantic Multidecadal Oscillation (AMO) in the North Atlantic was positively correlated to the NSS herring stock size. Recent unprecedented ocean warming in the Norwegian Sea ecosystem, besides elevated temperatures due to a positive AMO, seems to be outside optimal environmental conditions for early life history stages of NSS herring. We analysed 28 years of survey data using generalized additive models to reconstruct environmental conditions for drifting yolksac and preflexion stage larvae. Our results indicate that strong recruitment years were more likely when the larvae occurred simultaneously with a negative AMO during positive temperature anomalies. The transition from yolksac stages towards preflexion stages occurred while there was a slow increase in water temperature during the larval drift. Weak recruitment years generally occurred when larvae experienced elevated temperatures during the life stage transition under a positive AMO. These results augment evidence that the historical positive relationship between AMO and stock dynamics is reversed between 1988 and 2015. Albeit not implying any specific mechanistic biological interactions, we can assume that the unprecedented warming has modified the ecosystem drivers that negatively affect drifting larvae. Since 2016, the North Atlantic is shifting into a negative AMO phase, possibly resulting in the 10-year recruitment suppression of NSS herring ending soon.

Highlights

  • The survival of early life history stages was suggested by Hjort (1914) to be the main determiner of the year-class strength in fish populations

  • As one of the main bottlenecks for successful recruitment is based on the survival of early life history stages of fishes, our aim was to model environmental conditions during the drift of yolksac and preflexion larvae to understanding what environments may lead to variation in recruitment success between 1988 and 2015

  • In years with strong recruitment, larvae experienced a slight temperature difference during a negative Atlantic Multidecadal Oscillation (AMO) when shifting from yolksac to preflexion stages

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Summary

Introduction

The survival of early life history stages was suggested by Hjort (1914) to be the main determiner of the year-class strength in fish populations. A slight shift in survival rates of these stages has considerable effects on recruitment success (Houde, 1987). Every life stage has specific requirements on the environment, and changes will modify the chances of survival. Fish species exhibit a dome-shaped relationship to many. We shed light on the historic and current climate effects affecting Norwegian spring-spawning (NSS) herring (Clupea harengus) population dynamics, by investigating environmental regimes during the very early larval stages between 1988 and 2015

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