Hostname: page-component-78c5997874-mlc7c Total loading time: 0 Render date: 2024-11-20T00:34:42.805Z Has data issue: false hasContentIssue false

Vertical migration and dispersion of sprat (Sprattus sprattus) and herring (Clupea harengus) schools at dusk in the Baltic Sea

Published online by Cambridge University Press:  15 July 2003

L. A. Fredrik Nilsson*
Affiliation:
Informatics and Mathematical Modelling, Technical University of Denmark, Building 321, 2800 Kgs., Lyngby, Denmark
Uffe Høgsbro Thygesen
Affiliation:
Department for Marine Fisheries Research, Danish Institute for Fisheries Research, Charlottenlund Slot, 2920, Charlottenlund, Denmark
Bo Lundgren
Affiliation:
Department for Marine Fisheries Research, Danish Institute for Fisheries Research, North Sea Centre, 9850, Hirtshals, Denmark
Bo Friis Nielsen
Affiliation:
Informatics and Mathematical Modelling, Technical University of Denmark, Building 321, 2800 Kgs., Lyngby, Denmark
J. Rasmus Nielsen
Affiliation:
Department for Marine Fisheries Research, Danish Institute for Fisheries Research, Charlottenlund Slot, 2920, Charlottenlund, Denmark
Jan E. Beyer
Affiliation:
Department for Marine Fisheries Research, Danish Institute for Fisheries Research, Charlottenlund Slot, 2920, Charlottenlund, Denmark
Get access

Abstract

In populations of herring (Clupea harengus) or sprat (Sprattus sprattus), one typically observes a pattern of schools forming at dawn and dispersing at dusk, usually combined with vertical migration. This behaviour influences interactions with other species; hence a better understanding of the processes could contribute to deeper insight into ecosystem dynamics. This paper reports field measurements of the dispersal at dusk and examines two hypotheses through statistical modelling: that the vertical migration and the dissolution of schools is determined by decrease in light intensity, and that the dissolution of schools can be modelled by diffusion, i.e. active repulsion is not required. The field measurements were obtained during 3 days in March at one location in the Baltic Sea and included continuous hydroacoustical monitoring, trawl samples, and hydrographical CTD data. Echogram patterns were analysed using the school detection module in Echoview® and local light intensities were calculated using a model for surface illuminance. The data and the analysis support that schools migrate upwards during dusk, possibly trying to remain aggregated by keeping the local light intensities above a critical threshold, that schools initiate their dissolution when ambient light intensity drops below this critical threshold, and that fish subsequently swim in an uncorrelated random walk pattern.

Type
Research Article
Copyright
© Elsevier, IRD, Inra, Ifremer, Cemagref, 2003

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)