1966
DOI: 10.1121/1.1910087
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Reverberation from Deep Scattering Layers in the Western North Atlantic

Abstract: Reverberation from deep scattering layers was measured at 37 sites in the western North Atlantic. Resonant scatterers, presumably the swimbladders of bathypelagic fish, were responsible for the bulk of the observed reverberation. Three scattering layers, each populated with a characteristic size of scatterer, were found to persist over distances of several hundred kilometers. During the day, these layers were at depths between 300 and 900 m. A migration towards the sea surface of scatterers from the shallowest… Show more

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Cited by 29 publications
(8 citation statements)
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“…The aggregation of the mesopelagic micronekton within the HBL in the CC suggests that this fauna descends as deeply as possible to avoid visually orienting predators, while avoiding the effects of hypoxia. Off southern California, we did not observe deeper DSLs, in marked contrast to well-oxygenated regions of the world ocean, such as the South Pacific and North Atlantic oceans, where DSLs of mesopelagic fishes and other micronekton are regularly found at depths of 500 to 1000 m (Chapman & Marshall 1966, Williams & Koslow 1997.…”
Section: Discussionmentioning
confidence: 83%
“…The aggregation of the mesopelagic micronekton within the HBL in the CC suggests that this fauna descends as deeply as possible to avoid visually orienting predators, while avoiding the effects of hypoxia. Off southern California, we did not observe deeper DSLs, in marked contrast to well-oxygenated regions of the world ocean, such as the South Pacific and North Atlantic oceans, where DSLs of mesopelagic fishes and other micronekton are regularly found at depths of 500 to 1000 m (Chapman & Marshall 1966, Williams & Koslow 1997.…”
Section: Discussionmentioning
confidence: 83%
“…The occurrence of a distinct lower DSL boundary in the southern California Current Ecosystem at depths shallower than in regions that lack an OMZ (Chapman & Marshall 1966, Williams & Koslow 1997, Bianchi et al 2013 suggests that most of the southern California mesopelagic community is bounded by an ecological threshold in the environment. Although a diverse group of metazoans has been found to reside within OMZ cores, this occurs primarily in regions with very shallow…”
Section: Bottom Boundarymentioning
confidence: 97%
“…Some of the data reported in Holliday (1977b) were collected with a seismic arcer as an acoustic source. Chapman and Marshall (1966) observed up to three resonance peaks in an aggregation of fish in the North Atlantic. Because the resonance frequency depends upon the volume of the swimbladder, which in turn is related to the size of the fish, the results suggested the presence of three size classes of fish.…”
Section: Introductionmentioning
confidence: 99%
“…Sizes of fish with swimbladders were originally studied and, in some cases, spectrally discriminated, through the use of broadband sound as early as the1940s by Hersey, Backus, and others, as briefly reviewed in Chapman and Marshall (1966). The work involved the use of broadband sound in the upper hundreds of hertz to low kilohertz frequencies to exploit the resonance of the swimbladder.…”
Section: Introductionmentioning
confidence: 99%