Peces linterna (Myctophidae) de la costa oriental de Brasil, Atlantico suroeste.
Myctophids are typically pelagic fish of the open ocean (Hartel & Craddock, 2002) and, together with members of Sternoptychidae, Gonostomatidae, Chauliodontidae and the suborder Stomiatoidei, represent the characteristic families in mesopelagic depths (Haedrich, 1997). Among these, Myctophidae is the dominant family (Nafpaktitis et al., 1977) and the most speciose, including almost 250 species referred to as lanternfish due to a variety of luminous organs, among which photophores are the most characteristic (Nelson, 2006). Lanternfish range from arctic to antarctic waters, and from the surface at night to depths exceeding 2000 m (Nafpaktitis et al., 1977). The family also includes species known as pseudoceanic, associated with continental shelf and slope regions and in the neighbourhood of oceanic islands (Hulley, 1981). Continental slopes are particularly important due to the topographic and hydrographic gradients, and are considered areas of dynamic tension (Merrett & Haedrich, 1997). Continental slopes also encompass a wider set of physical niches, and provide an environment for the development of a recognizable and trophically-dependent community of benthic and benthopelagic fish (Haedrich et al., 1980). Down-slope zonation of lanternfish may result from the combined effects of depth and water column structure (Hulley, 1992).
Much of the current knowledge on Atlantic myctophids resulted from the study of the collections of the Woods Hole Oceanographic Institution (WHOI) (Nafpaktitis et al., 1977) and Institut fur Seefischerei (Hulley, 1981). In the southwestern Atlantic (0[degrees]-60[degrees]S), 79 species (22 genera) were collected during the 11th cruise of the R/V Akademik Kurchatov (Parin & Andriyashev, 1972; Parin et al., 1974). The distribution of 40 of these species, with respect to the water masses between 40[degrees]30'-47[degrees]00'S, was further examined (Konstantinova et al., 1994; Figueroa et al., 1998). Off the coasts of Suriname and French Guiana, 15 species from 7 genera were reported (Uyeno et al., 1983). In the Eastern Central Atlantic, Wienerroither et al. (2009) reported 52 species for the Canarian archipelago.
Although relatively few documents have been published on myctophids from low latitude oligotrophic waters (Nafpaktitis & Nafpaktitis, 1969; Hulley, 1972, 1981; Clarke, 1973; Gartner et al., 1987), high diversity is apparent (Backus et al., 1977). Figueiredo et al. (2002) and Santos (2003) reported 37 species captured in 133 midwater trawl hauls off southeastern and southern Brazil (22[degrees]-34[degrees]S), with sampling effort concentrated from 100 to 500 m. From Rio Real, BA to Cabo Sao Tome, RJ (12-22oS), 27 larval lanternfish species were identified in 658 samples collected in depths <200 m (Castro et al., 2010), and Myctophidae was the most diverse family at epi- and mesopelagic depths (Braga et al., 2007).
The present study provides knowledge about southwestern Atlantic lanternfish, including samples from Vitoria-Trindade chain, an area understudied (Clark et al., 2010), adjacent to a transition zone between tropical Atlantic and temperate South America biota. We report the occurrence and distribution of lanternfish in relation to oceanographic conditions and attempt to examine whether species associations are spatially different.
MATERIALS AND METHODS
The eastern coast of Brazil is a typical oligotrophic system (Gaeta et al., 1999), and the most important oceanic surface feature is the southward flowing Brazil Current (BC: 22-27[degrees]C, 36.5-37.0 psu), the warm western boundary current of the subtropical gyre (Silveira et al., 2001). The continental shelf of the study area (11-22[degrees]S) extends for only 8 km off Salvador (Franca, 1979) and widens to the south to form the Royal Charlotte Bank (RCB, 16[degrees]S) and the Abrolhos Bank (AB, 18oS). The Vitoria-Trindade chain that extends along 20.5[degrees]S comprises seamounts that have shallow summits at depths of 34-76 m (Miloslavich et al., 2011). These topographic barriers produce a complex hydrographic structure including vortices, upwellings and vertical mixing processes, which alter the oligotrophic condition mainly south of AB (Ciotti et al., 2007; Valentin et al., 2007). The subsurface layer beneath the BC is occupied by the cold and nutrient-rich South Atlantic Central Water (SACW: 6.0-18.5[degrees]C, 34.5-36.0 psu) flowing north, between 400-700 m (Schmid et al., 1995). Periodic upwelling of SACW beyond the deep thermocline (80-120 m) enhances primary production (Nonaka et al., 2000). In the subthermocline region there are three major water masses, Antarctic Intermediate Water (AAIW) near 800-900 m, North Atlantic Deep Water (NADW) centered at about 2500 m, and Antarctic Bottom Water (AABW) below about 3500 m (Hogg & Owens, 1999).
The studied material was obtained with midwater and demersal trawls, both performed only during the day, on the continental shelf, continental slope and near oceanic banks and seamounts off eastern Brazil (Fig. 1). Table 1 summarizes the characteristics of midwater and demersal sampling, effort and catch of myctophids. Samples were taken aboard the French R/V Thalassa in May-July 1999 (midwater) and May-June 2000 (demersal). Both cruises were developed in the context of the Brazilian fishery research program REVIZEE, in scientific cooperation with IFREMER (Institut Francais de Recherche pour l'Exploitation de la Mer).
During the midwater cruise, the collections were obtained using a large midwater net (292 m circumference and 191 m long). During operations, maximum horizontal and vertical opening was 56 and 25 m, respectively. Mesh sizes were 8000 mm in the wings and 20 mm in the cod-end. A total of 62 pelagic midwater trawls were towed at depths from 19 to 910 m, among which 50 had myctophid catches (n = 28,645). Hauls were undertaken on acoustically detected fish aggregations.
During the demersal cruise, the individuals were obtained using a bottom-trawl net with a 26.8 m head rope and 47.2-m foot rope, equipped with 40 rubber bobbins (rockhoppers) attached to the foot-rope. Mesh sizes were 110 mm for the wings and 20 mm for the cod-end. During the fishing operations, the horizontal and vertical mouth openings ranged between 28.0 and 45.5 m and from 3.0 to 10.6 m, respectively.
Demersal trawls were decided based on the availability of trawlable bottoms. A total of 58 stations yielded more than 45,000 specimens, from which 2,720 specimens of myctophids were recorded in 47 stations, ranging in depth from 100 to 2,271 m. On both cruises, trawl depth was acoustically controled using SCANMAR system, which was also used to access trawl geometry, including the horizontal opening and distance from net to bottom. The vertical opening and its distance in relation to the bottom was controled by the Ossian Trawl-Eye 49 KHz transducer fixed in the headrope. These systems allowed maintaining the net operating at specific depths during fishing and further classify the stations into different depth strata.
Water mass distribution in the study area
Temperature and salinity profiles (n = 116) recorded during the midwater cruise were used to analyse the horizontal distribution of temperature contours at the 200 m isobath (e.g., beginning of the mesopelagic zone), throughout the studied area (11-22[degrees]S). Water masses distribution was inferred from a T-S diagram using data compiled from the National Oceanographic Data Centre (Brazilian Navy), including CTD profiles down to 5,000 m. These data was sorted from the same geographic area and period (May-July) and processed using Ocean Data View (ODV) software.
Identification of species and abundance
The ichthyological material analysed was identified using identification keys provided by Nafpaktitis et al. (1977), Hulley (1986), McEachran & Fechhelm (1998), and Wang & Tsung-Chen (2001). Measurements and counts were made according to Nafpaktitis & Nafpaktitis (1969). Photophore terminology followed Parr (1929) and Nafpaktitis & Nafpaktitis (1969). A representative number of specimens were deposited in the collections of Museu Nacional do Rio de Janeiro (MNRJ) and Museu Oceanografico do Vale do Itajai (MOVI).
Species abundance followed primarily the classification proposed by Gartner et al. (1987) based on total number of specimens captured [abundant (>500 individuals), common (100-500 individuals), uncommon (10-100 individuals), rare (<10 individuals)], with an additional category, extremely abundant (>2,000 individuals).
The distribution of myctophid assemblages was analysed with non-metric multidimensional scaling (Clarke & Warwick, 2001) using the Sorensen similarity index calculated with species presence-absence in the samples. The final matrix used in the ordination was composed by 29 species and 53 samples (9 midwater and 44 demersal trawls). Stations with only one species (n = 11) were excluded from the matrix. A non-quantitative index was chosen due to differences in net sizes and sampling strategies between midwater and demersal fishing.
Water mass distribution in the study area
The thermal structure of the water column during the two cruises, both during winter, was similar. The water temperature ranged from 24-28[degrees]C at surface, 2024[degrees]C at 100 m depth, 15.7-16.1[degrees]C at 200 m, 8-9.5[degrees]C at 500 m, and was always <3[degrees]C beyond 1,000 m depth. Tropical Water (TW) from BC (T > 20[degrees]C; S > 36.2 psu) was present at surface (29-68 m), and the subtropical SACW with lower temperatures (618.5[degrees]C) and salinities (34.6-36.0 psu) occuppied the subsurface layer (118-624 m) (Fig. 2).
AAIW was present mainly from 700 m (2.0-4.0[degrees]C and 34.2-34.6 psu) to eventually 1,500 m, while NADW was found at depths between 1,500-2,000 m (3.0-4.0[degrees]C; 34.6-35.0 psu). At depths greater than 2,000 m, the top layer of the AABW (3.0-3.5[degrees]C; 34.6-35.0 psu) was found.
The horizontal distribution of the water temperature at 200 m (Fig. 3) showed that this depth was occuppied by SACW throughout the studied area, with an east-west gradient of decreasing temperatures. The lowest temperatures (14-15[degrees]C) were identified between 13-15[degrees]S off Salvador, and near RCB, AB and the Vitoria Channel, reflecting the upwelling of SACW as a result of BC meandering along the shelf edge and seamounts.
Distribution of catches
Myctophids were more frequent in demersal (78%) than in midwater (24%) trawls, although higher abundances in midwater catches resulted from acoustically detected schools (Fig. 4). The total number of myctophids per trawl ranged from 1 to 12,415, although almost always <50 ind [trawl.sup.-1] occurred in demersal trawls (85%). Midwater trawl catches were mostly >200 ind [trawl.sup.-1], including massive catches (>1,000 ind [trawl.sup.-1]) near the Royal Charlotte Bank and seamounts (Minerva, Hotspur).
The number of species/trawl ranged from 1-13 (Fig. 5), but captures of more than 5 species/trawl were more frequent in demersal trawls (21%) than in midwater trawls (17%). The maximum number of species per trawl (13) was similar in demersal and midwater trawls. Midwater trawls near seamounts south of Abrolhos Bank yielded the highest number of species (Vitoria: 13 spp.; Davis: 7 spp.). Demersal trawls that yielded the highest number of species occurred at the southernmost part of the area at 624.5 m (13 spp.) and at 2,126 m off Salvador (10 spp.). Nine trawls yielded 6-9 species trawl-1. Among these, six were performed between 13-14[degrees]S at depths from 522 to 1,929 m, and three were performed between 19-20[degrees]S at depths from 895 to 1,649 m.
From a total of 31,365 myctophids examined, all but 278 (0.9%) were identifiable to species. Table 2 lists the species grouped according to abundance, along with their totals and frequency of occurrence in midwater and demersal trawls, depth of occurrence and size range. The identified material comprised 11 genera and 29 species. The top five most abundant species comprised approximately 95% of the total number of individuals. Only one species was extremely abundant, 4 were abundant, 5 were common, 8 were uncommon and 11 were rare. Diaphus dumerilii was the most frequent species, both in demersal (62%) and midwater (66%) trawls. The majority of species (79%) had broadly tropical and tropical affinities (as indicated by Hulley, 1981), while species with subtropical and temperate affinities were poorly represented and occurred in very low numbers (1-17 ind).
Three groups of trawl stations were identified in MDS ordination (Fig. 6): North of Abrolhos Bank (NAB), South of Abrolhos Bank (SAB) and Seamounts (SEAM). Assemblages were significantly different (P = 0.02) when similarities between SEAM x NAB (P = 0.014) and SEAM x SAB (P = 0.030) were compared (ANOSIM Global R: 0.181).
Although NAB and SAB did not significantly differ (P = 0.255), a change in dominance was evident when mean densities (ind [h.sup.-1]) of the nine most abundant and frequent species in midwater trawls were compared (Fig. 7). Diaphus garmani and D. dumerilii were caught throughout the area, though mostly abundant at RCB and Minerva seamount. M obtusirostre occurred associated to the four seamounts sampled (Minerva, Hotspur, Vitoria, and Davis). At Vitoria seamount, except for D. garmani, the eight remaining species occurred together in catches, with yields that ranged from 4.2 to 110.2 ind [h.sup.-1]. A monospecific school of D. brachycephalus caught at 15[degrees]S yielded 1,115 ind [h.sup.-1].
In this study, myctophids were more frequent in demersal than in midwater trawls, possibly as a result of our exclusive daytime sampling, since under the normal diel vertical migration pattern these fishes hide from visual predators at depth during the day and forage on abundant plankton in upper waters at night (Pearre, 2003). Also, a number of specimens could have been caught during retrieval and/or deployment of the bottom trawl (the nets used were devoid of open/close mechanisms) and, for this reason, fish density estimates were not compared between midwater and demersal trawls. Moreover, the presence of myctophids in demersal trawls could represent the adoption of an adult benthopelagic life strategy, as indicated by Vinnichenko (1997). Gartner et al. (2008) suggested that persistent high-density near-bottom aggregations (NBAs) are a normal part of the life history of several species traditionally considered to be mesopelagic. These NBAs would enhance the probability of feeding success, as fishes could explore food supplies in a two dimensional search area (i.e near bottom).
Among the 29 myctophid species captured in this study, tropical and broad tropical distribution patterns dominated. Species with temperate and subtropical affinities were restricted to hauls that sampled depths below 700 m, which is the upper limit of AAIW in the area (Hogg & Owens, 1999). Although this number is lower than that recorded off southeastern and southern Brazil between 22-34[degrees]S (41 species: Figueiredo et al., 2002; Bernardes et al., 2005), if larval occurrence is considered (Bonecker & Castro, 2006), ten more species could be added (Benthosema suborbitale, Centrobranchus nigroocelattus, Diaphus anderseni, Diogenichthys atlanticus, Hygophum macrochir, Hygophum taaningi, Lampanyctus nobilis, Lepidophanes gaussi, Nannobrachium cuprarium, Notolychnus valdiviae) and the numbers be similar. All myctophids spend their larval stages in the productive epipelagic zone (Sassa et al., 2004), moving to the mesopelagic zone after reaching the juvenile stage (Clarke, 1973).
Eastern and south-southeastern Brazilian waters share 12 of 16 myctophid genera. Regarding the four genera exclusive within each area, broad or tropical genera (Centrobranchus, Diogenichthys, Lampadena, Notolychnus) occur between 11-22[degrees]S, while coldwater genera associated with the STC (Electrona, Gymnoscopelus, Lampichthys, Scopelopsis) occur between 22-34[degrees]S. The diversity within each area (11-22[degrees]S: 39 species, 16 genera; 22-34[degrees]S: 41 species, 16 genera) is comparable to that reported for Hawaii (47 species, 18 genera; Clarke, 1973), eastern Gulf of Mexico, GOM (49 species, 17 genera; Gartner et al., 1987) and north-central GOM (38 species, 17 genera; Ross et al., 2010). Collectively, Brazilian waters have a high diversity of myctophids (79 species, 23 genera: Menezes et al., 2003) comparable to that registered in the North Atlantic (82 species, 20 genera: Nafpaktitis et al., 1977). These numbers include the 30 species reported by Hulley (1981) for waters beyond 3,000 m during the research cruises of FRV "Walther Herwig" to South America (1966-1976). Among these, many are typically associated with the STC, the frontal zone where subantarctic and subtropical waters meet, which is a circumglobal feature of the Southern Ocean (Williams et al., 2001). The STC is a major biogeographic boundary, as well as a region of enhanced productivity (Pakhomov et al., 2000), and much of the plankton and fish fauna in this region have a circumglobal distribution (McGinnis, 1982; Pakhomov et al., 2000).
Excluding two hauls that sampled massive aggregations of D. garmani and captured 23,502 individuals, the top four species off eastern Brazil between 11-22[degrees]S (D. garmani, D. dumerilii, D. brachycephalus, D. perspicillatus) comprised 76.4% of the specimens caught. Off southeastern and southern Brazil between 22-34[degrees]S, the three dominant species (D. dumerilii, L. guentheri, Symbolophorus barnardi) comprised 74.9% (Figueiredo et al., 2002; Bernardes et al., 2005). Both values were similar to those reported for the contribution of the top seven species off Hawaii (75.5%; Clarke, 1973) and eastern GOM (74.7%; Gartner et al., 1987), and of the top six species off north-central GOM (75.1%; Ross et al., 2010). Diaphus is the most species among myctophid genera (60 species; Nafpaktitis et al., 1977) and 19 species are reported for Brazil (Santos & Figueiredo, 2008). In ichthyoplankton surveys off eastern Brazil, Diaphus spp. larvae integrated the transitional and oceanic assemblages (Nonaka et al., 2000; Castro et al., 2010), and the numeric dominance of adults between 11-22[degrees]S probably reflects the higher sampling effort in deeper waters when compared to 22-34[degrees]S, where sampling was shallower (<500 m: Figueiredo et al., 2002).
A tendency of increasing species number with depth was observed, and since temperature correlates to lanternfish distribution (Brandt, 1983), this result could be associated with the marked thermal structure of the water column. During hauls that sampled depths higher than 1,500 m between 11[degrees]-22[degrees]S, the net was towed through four waters masses (BC, SACW, AAIW, NADW), possibly increasing the probability of catching a higher number of species. Hulley (1992) also observed an increase in lanternfish species richness and in the complexity of the distributions across the slope, possibly as the result of a higher structuring of the water column.
The presence of a variety of reliefs between 11-22[degrees]S adds topographic complexity, causing island-induced disturbance, in which upwelled nutrients promote primary and secondary production in the island wake (Bonecker et al., 1992, 1993) and probably act to affect the distribution of the mesopelagic fauna. Our hydrographic results showed the occurrence of SACW at 200 m between 13-15[degrees]S, and near RCB, AB and the Vitoria Channel; this possibly reflects the permanent cyclonic eddy that Schmid et al. (1995) detected to be formed south of the AB from the meandering movement of the BC after passing through the Vitoria Channel. The spatial distribution of the SACW in the area studied seems to explain the distribution of the more speciose trawls and, for some species, the highest densities associated with seamounts and banks.
While D. dumerilii was the most frequent and second most abundant species in our study, it was dominant between 22-34[degrees]S (47%; Figueiredo et al., 2002) and seemed to be important in the trophic relation on the slope, once it was found in the stomach contents of several demersal bony fish of STC ecosystem (Haimovici et al., 1994). Near RCB this species was most abundant in rather shallow depths (25-34 m), indicating a certain degree of land association, as it was observed by Wienerroither et al. (2009). Diaphus dumerilii dominated both the water column (deep scattering layer) and the bottom (NBAs) on deep coral banks off Cape Lookout middle slope, North Carolina (Gartner et al., 2008).
The occurrence of mesopelagic species in shallow waters is ascribed to the abrupt depth changeover around islands of volcanic origin (Uiblein & Bordes, 1999), and the direct interaction between pelagic and demersal organisms at the interfaces between submerged bottom features establishes and important link between epipelagic waters and the deep benthos (Marshall & Merrett, 1977). Lanternfish may be an important prey item for large pelagic species, abundant in longline catches from Vitoria-Trindade seamounts (Olavo et al., 2005). Future research in the area should address the study of oceanic food webs.
The authors wish to express their gratitude to the Captains (Herve Piton and Paul-Ives Guilcher) and crew of the R/V Thalassa for their collaboration. Special thanks are given to the Chief Scientists and coordinators of the Brazilian cruises aboard R/V Thalassa, for the facilitation of logistics and successful integration of the multidisciplinary teams during cruises Bahia-1 and Bahia-2. Two anonymous reviewers made numerous comments to improve the manuscript.
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Received: 10 June 2013; Accepted: 20 January 2014
Adriana da Costa Braga (1), Paulo A.S. Costa (1), Agnaldo S. Martins (2) George Olavo (3) & Gustavo W. Nunan (4)
(1) Laboratorio de Dinamica de Populates Marinhas, Departamento de Ecologia e Recursos Marinhos Universidade Federal do Estado do Rio de Janeiro, Av. Pasteur, 458, sala 410 Urca, Rio de Janeiro, 22290-240, RJ, Brazil
(2) Departamento de Oceanografia e Ecologia, Universidade Federal do Espirito Santo Av. Fernando Ferrari, 514, Vitoria, 29075-910, ES, Brazil
(3) Laboratorio de Biologia Pesqueira, Universidade Estadual de Feira de Santana Km-3, BR 116 Campus Universitario, s/n, Feira de Santana, 44031-460, BA, Brazil
(4) In memoriam
Corresponding author: Adriana C. Braga (firstname.lastname@example.org)
Table 1. Number of stations, depth range, effort and characteristics of nets used in midwater and demersal sampling off eastern Brazil and details of myctophids catch. Midwater Demersal net net Number of trawls 50 68 Number of stations (with myctophids) 12 53 Depth range (m) 19-910 100-2,271 Horizontal opening during operation (m) 24-56 28-45.5 Vertical opening during operation (m) 25-42 3-10.6 Net size (m) 191 80.5 Codend mesh size (mm) 20 20 Total sampling effort (hour) 40:59h 63:41h Total catch (number) 28,645 2,720 Number of species 17 26 Number of exclusive species 3 12 Table 2. Lanternfish catch in midwater and demersal trawls off eastern Brazil (frequency in parentheses). Tropical: distributed only in tropical waters, Subtropical: distributed between 20[degrees] and 35[degrees] in the western South Atlantic, Broadly Tropical: distributed in both tropical and subtropical waters, Amphi-Atlantic: restricted to warm subtropical waters. Biogeographical definitions according to Hulley (1981). Total Midwater Demersal catch trawls trawls (n) (n = 12) (n = 53) >2,000 individuals 26,199 24,953 (6) 1,246 (21) Diaphus garmani 500-2,000 individuals 1,703 1,192 (8) 511 (33) Diaphus dumerilii Diaphus brachycephalus 778 761 (4) 17 (6) Diaphus perspicillatus 614 436 (6) 178 (7) Myctophum obtusirostre 575 336 (6) 239 (28) 100-500 individuals 388 155 (3) 233 (5) Lepidophanes guentheri Ceratoscopelus 171 51 (3) 120 (10) warmingii Diaphus adenomus 139 -- 139 (8) Diaphus problematicus 107 11 (2) 96 (14) Diaphus fragilis 106 56 (1) 50 (3) 10-100 individuals Diaphus splendidus 81 16 (3) 65 (3) Myctophum affine 42 38 (1) 4 (3) Myctophum selenops 42 20 (2) 22 (10) Lampadena luminosa 31 -- 31 (14) Diaphus lucidus 28 10 (1) 18 (3) Bolinichthys distofax 17 -- 17 (10) Bolinichthys 17 -- 17 (5) photothorax Notoscopelus 15 2 (1) 13 (6) caudispinosus <10 individuals 6 6 (2) -- Symbolophorus rufinus Diaphus bertelseni 3 -- 3 (3) Diaphus meadi 3 -- 3 (3) Diaphus cf. ostenfeldi 3 -- 4 (2) Hygophum reinhardti 3 3 (1) - Lampanyctus alatus 3 -- 3 (1) Lobianchia gemellari 3 -- 3 (3) Myctophum nitidilum 3 -- 3 (3) Notoscopelus resplendens 3 -- 3 (1) Hygophum hygomii 2 -- 2 (2) Myctophum phengodes 1 1 (1) -- Standard Distribution length pattern (mm) >2,000 individuals 33-60 Tropical Diaphus garmani 500-2,000 individuals 46-105 Tropical Diaphus dumerilii Diaphus brachycephalus 25-52 Broadly Tropical Diaphus perspicillatus 40-86 Broadly Tropical Myctophum obtusirostre 34-98 Tropical 100-500 individuals 25-76 Tropical Lepidophanes guentheri Ceratoscopelus 43-76 Broadly Tropical warmingii Diaphus adenomus 83-203 Amphi-Atlantic Diaphus problematicus 68-95 Tropical Diaphus fragilis 69-95 Tropical 10-100 individuals Diaphus splendidus 38-92 Broadly Tropical Myctophum affine 28-44 Tropical Myctophum selenops 48-62 Broadly Tropical Lampadena luminosa 115-190 Tropical Diaphus lucidus 73-103 Broadly Tropical Bolinichthys distofax 71-85 Subtropical Bolinichthys 40-60 Tropical photothorax Notoscopelus 106-132 Broadly Tropical caudispinosus <10 individuals 50-72 Broadly Tropical Symbolophorus rufinus Diaphus bertelseni 44-60 Broadly Tropical Diaphus meadi 52-59 Temperate Diaphus cf. ostenfeldi 98-112 Temperate Hygophum reinhardti 39-41 Broadly Tropical Lampanyctus alatus 93-107 Broadly Tropical Lobianchia gemellari 44-69 Broadly Tropical Myctophum nitidilum 39-73 Broadly Tropical Notoscopelus resplendens 54-59 Broadly Tropical Hygophum hygomii 50-58 Subtropical Myctophum phengodes 49 Subtropical
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|Title Annotation:||articulo en ingles|
|Author:||da Costa Braga, Adriana; Costa, Paulo A.S.; Martins, Agnaldo S.; Olavo, George; Nunan, Gustavo W.|
|Publication:||Latin American Journal of Aquatic Research|
|Date:||Mar 1, 2014|
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