کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4547927 1627273 2016 10 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Vertical distribution, composition and migratory patterns of acoustic scattering layers in the Canary Islands
ترجمه فارسی عنوان
توزیع عمودی، ترکیب و الگوهای مهاجرت لایه های پراکندگی صوتی در جزایر قناری
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات اقیانوس شناسی
چکیده انگلیسی


• Acoustic scattering and associated deep-sea fauna investigated in the Canary Islands.
• Four different scattering layers were observed from 400 to 1000 m depth.
• Migrant and non-migrant layers were ascribed to different fish a decapod species.
• Short (400 m) and long-range (700 m) migrations moved at 5 and 12 cm s− 1.

Diel vertical migration (DVM) facilitates biogeochemical exchanges between shallow waters and the deep ocean. An effective way of monitoring the migrant biota is by acoustic observations although the interpretation of the scattering layers poses challenges. Here we combine results from acoustic observations at 18 and 38 kHz with limited net sampling in order to unveil the origin of acoustic phenomena around the Canary Islands, subtropical northeast Atlantic Ocean. Trawling data revealed a high diversity of fishes, decapods and cephalopods (152 species), although few dominant species likely were responsible for most of the sound scattering in the region. We identified four different acoustic scattering layers in the mesopelagic realm: (1) at 400–500 m depth, a swimbladder resonance phenomenon at 18 kHz produced by gas-bearing migrant fish such as Vinciguerria spp. and Lobianchia dofleini, (2) at 500–600 m depth, a dense 38 kHz layer resulting primarily from the gas-bearing and non-migrant fish Cyclothone braueri, and to a lesser extent, from fluid-like migrant fauna also inhabiting these depths, (3) between 600 and 800 m depth, a weak signal at both 18 and 38 kHz ascribed either to migrant fish or decapods, and (4) below 800 m depth, a weak non-migrant layer at 18 kHz which was not sampled. All the dielly migrating layers reached the epipelagic zone at night, with the shorter-range migrations moving at 4.6 ± 2.6 cm s − 1 and the long-range ones at 11.5 ± 3.8 cm s − 1. This work reduces uncertainties interpreting standard frequencies in mesopelagic studies, while enhances the potential of acoustics for future research and monitoring of the deep pelagic fauna in the Canary Islands.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Journal of Marine Systems - Volume 157, May 2016, Pages 82–91
نویسندگان
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