Abstract

The occurrence of ichthyoplankton is associated to the hydrodynamics and spawning behavior of adults. In this study we aimed to detect regions of concentration of ichthyoplankton in São Marcos Bay, which has macro tidal amplitudes in Amazon Coast, Brazil. Ichthyoplankton was acquired by way of drag technique, using with 300 μm mesh. The density was obtained considering the number of eggs and larvae in filtered water. The sources of Ichthyoplankton were defined continuous and organized to denote the asynchronously the distribution conditions. To this was done using Voronoi polygon to determine the spatial shape of the region of operation of all sampling points. The use of CESM, as a spawning site and breeding fish larvae, was verified at all times of the year, with a higher density of eggs in the wet period and a higher density of larvae during the dry period. The position of the higher ichthyoplankton densities varied, considering concentrations in the area at south-east channel of the CESM in the rainless period, going to the central area in the wet period. The southeast of CESM is, therefore, a nursery for fish, requiring environmental management actions.

Highlights

  • São Marcos Bay (Complexo Estuarino de São Marcos - CESM, Maranhão) has greater tides in Brazil (Filho & Martins, 2005) and his dynamics is in focus to converrsion of energy (González-Gorbeña, Rosman, & Qassim, 2015)

  • CESM is a representative estuaries of northeastern Brazil (Pereira & Harari, 1995), operates onde mais um porto carrying loads potential impact com os Aquatic organisms

  • Environments with hydrodynamics similar to CESM are found in the Amazonas estuary in Pará. (Geyer, 1995; Le Bars, Lyard, Jeandel, & Dardengo, 2010; Rockwell Geyer et al, 1996) and in Amapá, Brazil (Santos et al, 2005), and in other locations like Bristol Channel and Severn River, England (Allen, 1991, 1992; Allen & Rae, 1987; Kirby & Parker, 1983), Mont Saint-Michel Bay, France (Larsonneur, 1994) and Cook Inlet, Alaska (Bartsch-Winkler & Ovenshine, 1984; Bartsch-Winkler & Schmoll, 1984)

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Summary

Introduction

São Marcos Bay (Complexo Estuarino de São Marcos - CESM, Maranhão) has greater tides in Brazil (Filho & Martins, 2005) and his dynamics is in focus to converrsion of energy (González-Gorbeña, Rosman, & Qassim, 2015). CESM is a representative estuaries of northeastern Brazil (Pereira & Harari, 1995), operates onde mais um porto carrying loads potential impact com os Aquatic organisms Environments with hydrodynamics similar to CESM are found in the Amazonas estuary in Pará. (Geyer, 1995; Le Bars, Lyard, Jeandel, & Dardengo, 2010; Rockwell Geyer et al, 1996) and in Amapá, Brazil (Santos et al, 2005), and in other locations like Bristol Channel and Severn River, England (Allen, 1991, 1992; Allen & Rae, 1987; Kirby & Parker, 1983), Mont Saint-Michel Bay, France (Larsonneur, 1994) and Cook Inlet, Alaska (Bartsch-Winkler & Ovenshine, 1984; Bartsch-Winkler & Schmoll, 1984) Environments with hydrodynamics similar to CESM are found in the Amazonas estuary in Pará. (Geyer, 1995; Le Bars, Lyard, Jeandel, & Dardengo, 2010; Rockwell Geyer et al, 1996) and in Amapá, Brazil (Santos et al, 2005), and in other locations like Bristol Channel and Severn River, England (Allen, 1991, 1992; Allen & Rae, 1987; Kirby & Parker, 1983), Mont Saint-Michel Bay, France (Larsonneur, 1994) and Cook Inlet, Alaska (Bartsch-Winkler & Ovenshine, 1984; Bartsch-Winkler & Schmoll, 1984)

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