Tests of larval retention in a tidally energetic environment reveal the complexity of the spatial structure in herring populations

Dispersion during the larval phase is of central importance in the dynamics of marine fish and invertebrate populations. Rapid transport or dispersion of larvae may contribute to connectivity and mixing, whereas spatial persistence (retention) is hypothesized to favour stock complexity and local sub...

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Published in:Fisheries oceanography Vol. 24; no. 6; pp. 553 - 570
Main Authors: Stephenson, Robert L, Power, Michael J, Laffan, Shawn W, Suthers, Iain M
Format: Journal Article
Language:English
Published: Oxford Blackwell Science 01-11-2015
Blackwell Publishing Ltd
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Summary:Dispersion during the larval phase is of central importance in the dynamics of marine fish and invertebrate populations. Rapid transport or dispersion of larvae may contribute to connectivity and mixing, whereas spatial persistence (retention) is hypothesized to favour stock complexity and local subpopulations. Larval retention, while rarely quantified, may be defined in species with protracted spawning by the spatial co‐occurrence of larvae of different sizes or ages. The spatial distributions of larval Atlantic herring (Clupea harengus) were examined from 22 annual autumn surveys (1975–1998) and 9 spring surveys (1975–1984) from the Bay of Fundy, a region with large tides and residual flow. Larvae of all sizes (3–27 mm in length, from hatch to nearly 4 months post‐hatch) were observed each year in two major aggregations; one off southwestern Nova Scotia, and the other in the mid‐inner Bay of Fundy off the northwestern shore of Nova Scotia. Two similar aggregations were evident over 5 months later from 9 spring surveys (1975–1984), despite the residual flow that would have swept the larvae from the region within 1 month. Larval retention was apparent from overlapping centres of mass of different size (=age) classes of larvae, and tested using a size diversity index, based on the co‐occurrence of 1‐mm‐size categories, derived from protracted spawning of several weeks. Geospatial ‘hot spots’ (Gᵢ* statistic) of four size (age) classes were evident at specific stations in the 50–100 m bathymetric zone and not elsewhere. These metrics provide quantitative measures of retention that may be applied to many ichthyoplankton data sets. One of the three main spawning areas collapsed during the study period after a period of intense fishing and failed to rebuild, but there was no substantial change in the location of larval hotspots in subsequent years. While larval retention does not directly relate to each spawning location, larval retention in the Bay of Fundy contributes to the complex ‘metapopulation’ structure of herring stocks in the western Atlantic.
Bibliography:http://dx.doi.org/10.1111/fog.12129
Canadian Department of Fisheries and Oceans
ArticleID:FOG12129
Canadian Department of Fisheries and Oceans, St. Andrews Biological Station
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istex:F963F0DDFAB84EAB87FED1E3532C86264D20AC3D
Figure S1. The initial abundance of fall spawned herring (3-27 mm TL m−2, 4th root transformed), plotted on the abundance of herring larvae (8-27 mm TL m−2, 4th root transformed), sampled at identical stations 1 week (●), 2 weeks (x) and 3 weeks(+) later, selected from all repeated stations in 1985, 1986 and 1987. Figure S2. Figures of annual distribution. Contours (number m−2 to bottom) of the annual distribution of Bay of Fundy autumn larval herring abundance for standard stations for the years 1975-1998. Figure S3. Instructions for replicating the analyses of larval retention with the Getis-Ord Gi* statistic using the Biodiverse software (Laffan et al., ; http://purl.org/biodiverse). Figure S4. Overall average weighted latitude and longitude for each of the four size classes of autumn spawned herring (1975-1998), and the abundance of herring from the spring surveys (1975-1984), for the inner and outer Bay of Fundy. Error bars are 95% confidence intervals.
Australian Association for Advancement of Science
Australian Research Council
ObjectType-Article-1
SourceType-Scholarly Journals-1
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ISSN:1054-6006
1365-2419
DOI:10.1111/fog.12129