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Latin american journal of aquatic research

versión On-line ISSN 0718-560X

Lat. Am. J. Aquat. Res. vol.46 no.5 Valparaíso dic. 2018 

Research Article

Abundance and distribution of the deep-sea crab Chaceon ramosae (Decapoda: Geryonidae) in southern Brazil: contribution to the fishing regulation

Harry Boos¹  ² 

Paula Beatriz Araujo² 

¹Centro Nacional de Pesquisa e Conservação da Biodiversidade Marinha do Sudeste e Sul-CEPSUL. Instituto Chico Mendes de Conservação da Biodiversidade-ICMBio, Itajaí, Santa Catarina, Brazil.

2Programa de Pós-Graduação em Biologia Animal, Instituto de Biociências. Universidade Federal do Rio Grande do Sul-UFRGS, Porto Alegre, Rio Grande do Sul, Brazil.


The deep-sea crab Chaceon ramosae occurs at 350-1200 m depth in the southeast and south of Brazil. Here we evaluated the latitudinal, bathymetric, and seasonal abundance of C. ramosae in southern Brazil obtained during several research cruises. We also obtained populational data to evaluate the effectiveness of the fishing regulations for C. ramosae. Five sampling cruises were carried out in 2009-2010 and the sampling effort comprised 32 fishing hauls with four pots per mainline. In total, 195 individuals were caught, 128 males and 67 females, of which 17 were ovigerous. The highest catch per unit effort occurred between 29°03’ and 29°05’S at 800-1000 m in depth. The highest abundance occurred in winter, and almost all ovigerous females were captured in this season. The size at the onset of sexual maturity was estimated at 120 mm carapace width. Depth was the most critical environmental factor explaining C. ramosae distribution. The largest individuals, as well as the mature ones, were mainly captured in shallower regions (400-600 m). Our results confirm the need for prohibiting the fishing for C. ramosae at depths lesser than 500 m.

Keywords: Chaceon ramosae; sexual maturity; deep-water resources; continental slope; southern Atlantic


Deep-sea crabs of the family Geryonidae Colossi, 1923 (Decapoda: Brachyura) inhabit muddy and sandy-mud substrates from 50 to 2800 m depth, where tempe-ratures range from 12 to 4°C (Wigley et al., 1975; Haefner, 1978; Manning & Holthuis, 1989). Studies about their growth and longevity are scarce, but they probably exhibit the common traits of most deep-sea species: high longevity, late maturation, slow growth, and non-annual reproduction (Melville-Smith, 1989). These traits often result in populations with low biomass production, and therefore, with slow recovery when intensely exploited (Rogers et al., 2008; Groeneveld et al., 2013).

Four Geryonidae species occur along the Atlantic coast of South America, and all belong to the genus ChaceonManning & Holthuis, 1989: C. eldorado Manning & Holthuis, 1989 (Colombia, Venezuela, Trinidad Tobago, French Guyana); C. linsiTavares & Pinheiro, 2011 (northeastern Brazil); C. ramosae Manning, Tavares & Albuquerque, 1989 (southeastern and southern Brazil); and C. notialis Manning & Holthuis, 1989 (southern Brazil, Uruguay and Argentina) (Tavares & Pinheiro, 2011). Molecular analyses suggested that C. notialis might be a species complex, whereas the taxonomic status of the other three species was confirmed (Mantelatto et al., 2014). Recently, C. gordonae (Ingle, 1985) was reported in Brazil at the St. Peter and St. Paul Archipelago (Ferreira et al., 2016).

The first fishing cruises targeting deep-sea crabs in southern Brazil at more than 400 m depth, occurred in 1984-1985 between latitudes 25° and 34°S (Lima & Lima-Branco, 1991; Haimovici et al., 2007). After the launch of a governmental program to develop deep-sea fisheries in 1998, the continental slope of southern Brazil and Uruguay became a profitable fishing region (Perez & Wahrlich, 2005; Pezzuto et al., 2006a, 2006b). However, the deep-sea fauna remains sparsely studied in Brazil, and new species are still being discovered, mainly as bycatch of the industrial fishing (Mincarone & Anderson, 2008).

Along the Brazilian coast, C. ramosae occurs from Espírito Santo to Rio Grande do Sul, at depths of 350-1200 m (Manning et al., 1989; Melo, 1996). Nowadays, according to the National Program of Fishing Vessel Monitoring by Satellite (PREPS), there is no fishing activity targeting the deep-sea crab (C. ramosae). However, between 1999 and 2009, it was captured almost 585 t y-1 of this species. Only in 2004, the total of capture reached 1742 t (Univali/CTTMar, 2010). Due to inefficient management and biological attributes such great longevity and slow-growth, fisheries targeting deep-sea species usually follows a pattern of a fast increase in catches, followed by an abrupt decline, driving species to overfishing (Rogers et al., 2008; Clark et al., 2016). In recent assessments of extinction risk, it was estimated that in the last 45 years the population of C. ramosae decreased by nearly 50%. However, this species was categorized as "Near Threatened," as its bathymetric and latitudinal distri-bution is wider than the range exploited by the industrial fishing fleet (Instituto Chico Mendes, 2016; Pezzuto et al., 2016).

The small number of research vessels in operation limits the knowledge of the Brazilian marine fauna, especially in regions deeper than 200 m. The existing information about these regions comes mainly from the industrial fishing. In these cases, however, the estima-tion of distribution and abundance might be biased because the industrial fishing has a typical non-random search mode towards their target species (Walters, 2003). Although marine fauna inventories have been done previously in Brazil, mainly focusing the southeast and extreme south, some of them occurred more than three decades ago and were sporadic and irregular (Haimovici et al., 2007). However, despite being provided by industrial fishing vessels, Pezzuto et al. (2002) did analyze unbiased data, once deep-sea crabs were caught during an exploratory phase of the fishery when almost none were known about occurrence and abundance of their stocks. Conversely, the evaluation of the effectiveness of deep-sea fisheries management measures are recommended by FAO (2009), which establishes that countries should monitor the implementation of their fisheries management plans, and periodically review the plans using the best data available.

In this sense, the aim of the study was to verify the validity of two restriction measures present in the normative which regulates the fishing of C. ramosae in Brazilian waters: i) the minimum fishing depth of 500 m, and ii) prohibition of fishing, during summer and autumn, at depths lesser than 700 m. In order to achieve this, we sought to identify the patterns of the bathymetric, latitudinal and seasonal distribution of C. ramosae in southern Brazil and, also, to analyze the reproductive period, proportion and sexual maturity from samples obtained in five research cruises.


Study area

Low nutrient concentrations and low productivity characterize the Brazilian Economic Exclusive Zone (EEZ). However, the Subtropical Convergence (SC) contributes to increasing its productivity (Rossi-Wongtschowsky et al., 2006; Castello et al., 2012). The SC (38 ± 2ºS) is formed by the encounter of the Brazilian and Falklands currents in the southeastern and southern regions (Olson et al., 1988). The continental shelf between Cape of São Tomé (22°S) and Chuí (34°34’S) is more extensive in the central part and narrower next to Cabo Frio (23°S) and Cape Santa Marta Grande (28°40’S), furthermore it is also characterized by a very gentle slope less than 2 m km-1. In the upper continental slope, the slope is about 20 m km-1, except between Rio Grande and Chuí, where it is 80-130 m km-1, and north of Cabo Frio, where it is 100 m km-1. The shelf break, where the continental slope begins, occurs at depths between 160 and 190 m (Zembruscki et al., 1972; Haimovici et al., 2007).


Five research cruises were conducted in 2009 (winter and spring) and 2010 (summer, autumn, and winter), aboard the R/V Soloncy Moura. This vessel belongs to the "Centro Nacional de Pesquisa e Conservação da Biodiversidade Marinha do Sudeste e Sul do Brasil" (CEPSUL), of the Brazilian Ministry of Environment. The sampling stations were distributed off the southwestern Brazilian coast between 400 and 1000 m depth, along with the upper continental slope from 26° to 29°S. This area was divided into five latitudinal sectors: north (26°14’-26°18’S), central-north (26°50’-26°51’S), central (27°15’-27°46’S), central-south (28°31’-28°45’S), and south (29°03’-29°05’S) (Fig. 1).

The bathymetry was grouped using intervals of 200 m depths, and the samples of each cruise were grouped seasonally: winter and spring’2009 and summer, autumn and winter’2010. The total sampling effort was approximately 265 hours (Table 1).

To capture the crabs, we carried out 32 fishing operations with four pots per the main line, baited with skipjack tuna, Katsuwonus pelamis (Linnaeus, 1758). The pots were of a beehive pot type with a conical iron frame (Japanese model for deep-sea crab fishing) (Slack-Smith, 2001). On the upper face of the frame, there was a plastic entrance with 30 cm of diameter, and the covering surface was nylon netting with a mesh size of 20 mm. Each pot was fixed to a secondary line of 2 m long, which was attached to the main line. The distance between pots was 30 m (Fig. 2).

Figure 1 Sampling area conducted in 2009 (winter and spring) and 2010 (summer, autumn, and winter), aboard the R/V Soloncy Moura/CEPSUL. Circles indicate the sampling stations and rectangles indicate the latitudinal sectors: A: north (26°14’-26°18’S), B: north-central (26°50’-26°51’S), C: central (27°15’-27°46’S), D: south-central (28°31’-28°45’S), and E: south (29°03’-29°05’S). 

These pots have been the main fishing device used to capture deep-sea crabs in Brazil (Chaceon spp.) (Athiê & Rossi-Wongtschowski, 2004).


The carapace width (CW) of all crabs was measured to the nearest 0.1 mm using vernier caliper, as the maximum transversal distance at the midline of the carapace, including the dorsolateral spines. The sex was determined upon the presence of secondary sexual characters: the shape of the abdomen and absence of gonopods. As from the identification of copula evidence in males and females, the animals were grouped in five categories: i) males without mating marks; ii) males with mating marks (dark spots on the ventral side of the coxae, ischia, and meri); iii) females with closed vulvae (gonopores near thoracic sternal suture 5/6); iv) females with opened vulvae and v) ovigerous females (with eggs attached to pleopods) (Elner et al., 1987; Melville-Smith, 1987; Biscoito et al., 2015) (Fig. 3).

Identification and vouchers

The animals were identified according to Manning et al. (1989) and Melo (1996). Some of the sampled animals were cryo-anesthetized and subsequently fixed and preserved in 95% ethanol. Vouchers were deposited in the Biological Collection of CEPSUL (Nº168-175, 177, 178, 183, 186) and the samplings were authorized by the Brazilian authority (SISBIO/ ICMBio License N°16886-2).

Data analysis

The analysis of variation in the distribution and abundance of collected C. ramosae (sex and age groups categories) was undertaken from the calculation of Catch per Unit Effort (CPUE, in a number of individuals per 6 h captured in fishing operations with four pots per main line). Since CPUE variances of the depth intervals were not homogeneous, they were compared with the non-parametric Kruskal-Wallis test. However, CPUEs among the latitudinal sectors were compared by analysis of variance (ANOVA) (Ayres et al., 2007; Borcard et al., 2011). A cluster analysis (Unweighted Pair-Group Method using arithmetic Averages-UPGMA) was used to verify how the categories are related (males without marks, males with marks, females with closed vulvae, female with opened vulvae and ovigerous females) according to the variation of latitude, bathymetry and seasons (Legendre & Legendre, 1998; Borcard et al., 2011). A Principal Component Analysis (PCA) was used to verify how the males and females categories were distributed along the latitudinal, bathymetric, and seasonal gradients. The importance of each variable and their contribution to the pair of axes was analyzed from the circle of equilibrium contribution (Borcard et al., 2011). The relationship between female carapace width (mm) and depth (m) was analyzed by linear regression.

Date Nº of haul Start Lat. Start Log. Sector Initial depth Duration
14/08/2009 1 29°06.17’S 47°51.078’W South 570 11:12
16/08/2009 2 27°46.67’S 47°05.659’W Central 500 09:30
16/08/2009 3 27°46.24’S 47°00.993’W Central 530 11:00
25/10/2009 4 26°50.41’S 46°23.205’W North-central 430 02:52
25/10/2009 5 26°51.03’S 46°10.344’W North-central 750 06:45
26/10/2009 6 27°39.35’S 46°52.497’W Central 750 lost
26/10/2009 7 27°41.11’S 47°06.405’W Central 530 09:28
27/10/2009 8 28°42.09’S 47°19.403’W South-central 580 06:56
27/10/2009 9 29°05.96’S 47°45.597’W South 560 09:26
27/02/2010 10 26°14.95’S 46°02.026’W North 460 14:55
27/02/2010 11 26°18.23’S 45°41.09’W North 750 15:20
28/02/2010 12 26°50.93’S 46°10.483’W North-central 620 06:20
28/02/2010 13 26°50.73’S 46°24.138’W North-central 433 07:05
12/03/2010 14 29°04.78’S 47°49.979’W South 457 10:40
12/03/2010 15 29°03.95’S 47°45.365’W South 600 09:10
13/03/2010 16 28°30.58’S 46°48.669’W South-central 970 12:50
13/03/2010 17 28°33.83’S 47°04.522’W South-central 400 lost
14/03/2010 18 27°41.24’S 46°53.359’W Central 772 05:45
04/06/2010 19 27°41.1’S 47°06.007’W Central 536 12:10
09/06/2010 20 27°41.48’S 46°52.729’W Central 774 13:10
08/06/2010 21 26°14.63’S 46°04.712’W North 436 12:58
08/06/2010 22 26°18.15’S 45°41.98’W North 711 15:30
08/06/2010 23 26°50.65’S 46°10.483’W North-central 616 lost
09/06/2010 24 26°51.16’S 46°23.875’W North-central 433 08:40
30/06/2010 25 29°04.05’S 47°43.051’W South 600 07:30
01/07/2010 26 28°31.68’S 47°52.301’W South-central 749 lost
11/08/2010 27 26°15.42’S 46°02.826’W North 721 06:00
11/08/2010 28 26°18.09’S 45°41.665’W North 455 06:23
21/08/2010 29 26°51.04’S 46°23.3’W North-central 438 08:18
22/08/2010 30 27°39.25’S 46°57.358’W Central 703 06:37
23/08//2010 31 28°45.21’S 47°18.742’W South-central 816 06:11
24/08//2010 32 29°04.55’S 47°43.205’W South 650 06:27

Female size at the onset of sexual maturity was estimated from the size class containing 50% of mature females (ovigerous or with open vulvae) (Santos, 1978; Vazzoler, 1981). Male size at sexual maturity was estimated based on the presence of mating marks (Melville-Smith, 1987; Pezzuto & Sant’Ana, 2009). The dispersion of points was adjusted to the sigmoid model (y = 1/1+e(LC-LC50)), adapted from Fontelhes-Filho (1989) and Vazzoler (1996). The sex ratio was compared between the bathymetric, latitudinal, and seasonal gradients, using a chi-square test with Yates’ correction or G-test with Williams’ correction, with a 5% significance level. The presence of ovigerous females determined the reproductive period.

The R (R Development Core Team, 2014) was used for the estimation of size at the onset of sexual maturity.

The software Statistica 7.1 (StatSoft Inc., 2005) was used for the UPGMA and PCA.

Figure 2 a) Main line with a series of four pots ready to haul, b) pot with bait before to be hauling, c) hauling the pot to a surface, d) pot with prays after fishing. 


In total, 195 individuals were captured: 128 males and 67 females (17 ovigerous). The highest CPUE occurred in the Southern sector (CPUE = 9.9) and between 801 and 900 m depth (CPUE = 36.8). However, the CPUE was not significantly different among latitudinal sectors (ANOVA: P = 0.3474) or depths intervals (Kruskal-Wallis: P = 0.0814) (Fig. 4). Most individuals, and especially the ovigerous females, were captured during winter, and almost all ovigerous females (n = 16) were captured in the Central sector and between 501 and 600 m (Table 2).

Fifty percent of males and 67% of females were captured between 600 and 800 m depth. There was a clear bathymetric pattern in the distribution of females: females with a closed vulva occurred in the deepest areas, those with an open vulva occurred in intermediate depths, and ovigerous females were only captured in the shallowest areas, within 400-600 m of depth. A similar relationship was observed in males: immature (without marks) males were mainly captured in deeper regions, whereas mature ones were captured in shallower areas (Table 2).

Figure 3 Chaceon ramosae. a) Carapace width (CW) (scale = 10 cm), b) male showing mating marks (circles) (scale = 5 cm), c) ovigerous females, d) female with closed vulvae (scale = 1 cm), e) female with opened vulvae (scale = 1 cm). 

The UPGMA relating the abundances to the bathymetric, latitudinal, and seasonal gradients showed two main groups (distance = 98.6), one formed by males without mating marks, and another formed by the other four categories. The latter group, in turn, was formed by two subgroups (distance = 31.2), one consisting of males with mating marks and ovigerous females, and the other consisting of females with open and closed vulvae (Fig. 5). The PCA indicated that ovigerous females, females with an open vulvae and males with mating marks were similarly distributed along the gradients. The two first axes explained 78.6% of the total variation (Fig. 6). Latitudinal sectors (Axis 1) and depth (Axis 2) were the two variables which contributed more to this distribution.

The largest male and female measured reached 176.1 mm and 147.9 mm CW, respectively. In general, the largest individuals of both sexes (140.6 mm CW on average) were captured in shallow areas, between 400 and 600 m depth. The size was significantly different along the bathymetric gradient (Kruskal-Wallis, P = 0.0495), and an increase in size with the decrease in depth was evident in the females (Fig. 7).

The smallest and largest ovigerous females were 115 and 142 mm CW, respectively. The smallest male with mating marks was 123 mm and the largest, 166 mm CW. The size at the onset of sexual maturity of males and females was estimated at 140 mm and 120 mm CW, respectively (Fig. 8).

Figure 4 Catch per unit effort (ind 6 h-1) per season. a) winter 2009, b) spring, c) summer, d) autumn, e) winter 2010 in the sampling stations during the research cruises aboard the R/V Soloncy Moura/CEPSUL. 

The sex ratio favored males in almost all seasons and latitudinal sectors. Along the bathymetric gradient, however, the sex ratio was biased towards females in the shallowest region (401-700 m), and towards males in the deeper regions (701-900 m) (Table 3).


The high CPUE of C. ramosae recorded in the south of Cape Santa Marta Grande (29°19’S), and the presence of most ovigerous females between 27°15’ and 27°46’S (central sector), can be explained by some oceano-graphic processes in the region. One process is the Subtropical Convergence (SC), already mentioned, which increases productivity (Emilson, 1961; Carvalho et al., 1998; Amaral & Jablonski, 2005; Rossi-Wongtschowsky et al., 2006). A second one is the upwelling of the South Atlantic Central Water during the northeasterly winds. This upwelling occurs especially in spring and summer and increases the local primary production. Consequently, the primary produc-tivity favors the survival of plankton and the reproduction of the benthic fauna (Pires-Vanin & Matsuura, 1993; Matsuura, 1995). In addition, the distribution of fish larvae in the southern portion of the continental shelf of southern Brazil is influenced by the Plata Plume Water (Macedo-Soares et al., 2014), which is an important source of carbon of continental origin, particularly during periods of El Niño Southern Oscillation (ENSO) (Piola et al., 2005). Over the winter, the Plata Plume Water occupies a coastal band several tens of kilometers wide, nearly reaching our North-central latitudinal sector (26°14’-26°18’S) (Piola et al., 2008).

Another process that can influence the distribution of animals is the formation of frontal zones due to the encounter of water masses with different properties (temperature, salinity, etc.). These frontal zones, when associated with divergent water masses, generate upwelling events that bring nutrients up to the euphotic region. The inflow of nutrients favors the growth of phytoplankton, which favors the growth of other organisms. On the other hand, when the water masses converge, organisms with less swimming abilities are aggregated and passively dragged down to the bottom (Bakun, 2006). In the bottom, they can be preyed by opportunistic carnivores such as C. ramosae (Domingos et al., 2008). These phenomena have been identified as responsible for the fluctuation in the biomass of deep-water populations in south Brazil (Fischer, 2012). These two processes, upwelling and sinking, create feeding opportunities and influence many organisms in different life stages. These food sources may benefit fast-growing species with high mortality, as well as the slow-growing species with low mortality (Bakun, 2006; Fischer, 2012), such as C. ramosae.

Figure 5 Cluster analysis (UPGMA) of males and females along the latitudinal (north 26°14’-26°18’S, north-central 26°50’-26°51’S, central 27°15’-27°46’S, south-central 28°31’-28°45’S, and south 29°03’-29°05’S), bathymetric (between 400 and 1000 m depth) and seasonal gradients (winter and spring’2009; summer, autumn and winter’2010). 

Table 2 Catch per unit effort (ind 6 h-1) of males and females per season (winter and spring’2009; summer, autumn and winter’2010), along the latitudinal (north 26°14’-26°18’S, north-central 26°50’-26°51’S, central 27°15’-27°46’S, south-central 28°31’-28°45’S, and south 29°03’-29°05’S) and bathymetric gradients. 

The presence of ovigerous females in shallow regions (500-600 m) of the continental slope may promote the survival of larvae released there. At these depths, the temperatures range from 4°C to 10°C, and the primary and secondary productivity is higher than in deeper regions, due to the SC (Gutiérrez et al., 2011). In Uruguay, most ovigerous females of C. notialis occurred at 300-400 m depth (Gutiérrez et al., 2011), whereas in the Madeira archipelago and the Canary Islands, ovigerous females were mainly found at 800-1000 m depth. In the latter case, the absence of females in shallow areas may be due to competition with other crab species (Biscoito et al., 2015). In addition to ovigerous females, larger and sexually mature individuals were also more abundant in shallower regions (500-700 m), indicating that depth is the main environmental factor influencing distribution. Males with mating marks, and females with open vulvae and ovigerous formed a distinct group in this region. A similar trend was observed in most geryonid crab populations, in C. affinis in the North Atlantic, where the size of both sexes decreased with depth (Biscoito et al., 2015). These results confirm precopulatory mate guard behavior (Elner et al., 1987) associated with mating-related migration to lower depths. The repro-duction of C. ramosae is not only dependent on satisfactory conditions to maturity individuals, with higher energy costs due to the reproductive behavior, but also favorable conditions to the larvae survival.

Figure 6 Ordination (PCA) of the abundance of males and females along the latitudinal, (north 26°14’-26°18’S, north-central 26°50’-26°51’S, central 27°15’-27°46’S, south-central 28°31’-28°45’S, and south 29°03’-29°05’S), bathymetric (between 400 and 1000 m depth) and seasonal gradients (winter and spring’2009; summer, autumn and winter’2010). Axes 1 and 2 explained 78.6% of total variation. 

Seasonal reproductive cycles are usually triggered by environmental changes, such as day length and temperature. In the deep sea, none of these stimuli can trigger reproduction (Melville-Smith, 1987). However, the absence of seasonal changes in these environments has been disproved recently (Morales-Nin & Panfili, 2005; Danovaro et al., 2014). The seasonal food supply that reaches the deeper regions, in the form of particulate organic carbon, is used by the benthic fauna for maintenance (respiration) and growth (Rowe, 2013), and sexual maturation is influenced by and synchro-nized with, food availability (Rosa & Nunes, 2003). Besides, the sinking of carcasses, by natural death or discards by industrial fishing, constitutes an important food source for animals of large size and high mobility, such as C. ramosae.

Figure 7 Relationship between female (n = 67) carapace width (mm) and depth (F = 31,3967; P < 0.0001). 

Nonetheless, oceanographic processes that provide water exchange between two currents (e.g., eddies) also contribute to the nutrients fluxes and have been identified as responsible for biomass fluctuations of deep-sea populations (Fischer, 2012). Unlike C. affinis in the Canary Islands, where ovigerous females were found throughout the year (Biscoito et al., 2015), ovigerous females of C. ramosae were only found in autumn and winter, suggesting a seasonal reproductive pattern in the studied area. Contrary to what occurs in most brachyuran species, evidence of seasonal reproduction in geryonid crabs is scarce (Wigley et al., 1975; Haefner, 1978; Lux et al., 1982; Melville-Smith, 1987). The reproductive cycle of C. ramosae is probably regulated by the seasonal availability of food, as already observed for other species (George & Menzies, 1968; Barradas-Ortiz et al., 2003; Rose & Nunes, 2003). However, the synergy among the oceanographic processes involved in the regulation of food availability, in the southeast and south of Brazil, and its influence on the life cycle of deep-sea populations, still needs to be better understood. However, the highest seasonal variation of CPUEs, between winter 2009 and 2010, it is probably explained by the different sampling depths and not by the different environment condition of the seasons. In 2009, the research cruiser sampled regions between 500 and 600 m depth, and in the winter of 2010 regions between 400 and 800 m.

Figure 8 a) Cumulative frequency of mature females (ovigerous or with open vulvae) per size class (carapace width in mm). The L50 is 120 mm, b) Cumulative frequency of mature males (with mating marks) per size class (carapace width in mm). The L50 is 140 mm. 

Table 3 Sex ratio (males/females) along the seasonal, latitudinal, (north 26°14’-26°18’S, north-central 26°50’-26°51’S, central 27°15’-27°46’S, south-central 28°31’-28°45’S, south 29°03’-29°05’S) and bathymetric gradients (m). achi-square test with Yates’ correction, bG-test with Williams’ correction, *Significant F. 

Variables Males Females Sex ratio (m/f) P
Winter’09 7 16 0.4 0.0953a
Spring 4 3 1.3 0.0542b
Summer 25 3 8.3 < 0.0001*
Autumn 24 5 4.8 0.0008*
Winter’10 71 37 1.9 0.0015*
North 19 0 - -
North-central 1 1 1 0.0261b*
Central 45 21 2.1 0.0046*
South-central 31 11 2.8 0.0034*
South 36 30 1.2 0.5383
401-500 m 0 2 - -
501-600 m 33 22 1.5 0.1775
601-700 m 13 26 0.5 0.0547
701-800 m 55 2 27.5 < 0.0001*
801-900 m 29 9 3.2 0.0021*
901-1000 m 2 2 1 0.0249b

The size at onset of sexual maturity estimated here for females and males, 120 mm and 140 mm CW, respectively, was very similar to those estimated by Pezzuto & Sant’Ana (2009): 122 mm and 136 mm. In their study, the crabs were captured by industrial fishing vessels and the sample size was larger than in our study (511 males and 579 females).

Regarding the validity of the current C. ramosae fishing regulation in Brazil (SEAP Normative Instruc-tion # 21, December 1, 2008), our results do confirm the need to prohibit the capture in areas less than 500 m depth, since ovigerous females were only recorded at depths of 600 m or less. The uncontrolled capture along this area, allowing ovigerous females to be captured, does put reproduction in risk, with immediate negative implications to population recruit-ment. Moreover, the prohibition of fishing during summer and autumn at depths lesser than 700 m can perhaps be reviewed, since ovigerous females were mainly collected during winter and always at depths lesser than 600 m. However, it should be considered that only a total of 17 ovigerous females were sampled on our cruises. Reductions in conservation measures to C. ramosae, elaborated from monitoring of catches made by industrial vessels leased in the early 2000s, can only be made when new research cruises, using a bigger sampling effort, capture more ovigerous females. In conclusion, the maintenance and recovery of the C. ramosae population are ensured by the current national fishing regulation.


The authors wish to express their gratitude to the Centro Nacional de Pesquisa e Conservação da Biodiversidade Marinha do Sudeste e Sul (CEPSUL) staff, Roberta Aguiar dos Santos, Felipe Farias Albanez, Elisabeth Michelleti and Luiz Fernando Rodrigues. To the undergraduate students of UFSC, UNIVALI and FURB that helped with sampling; to the crew of the R/V Soloncy Moura/CEPSUL; to Karin Schacht, Allan Scalco, Bernardo Cerantola, and Paula Salge, for suggestions and support in drafting the manuscript; and to CNPq for grants given to PBA. This research was supported by the Instituto Chico Mendes de Conservação da Biodiversidade (ICMBio), and Comissão Interministerial para os Recursos do Mar (CIRM) through Avaliação, Monitoramento e Conservação da Biodiversidade Marinha (REVIMAR). The authors also would like to thank the anonymous reviewers for their valuable contributions.


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Received: March 17, 2017; Accepted: August 29, 2018

*Corresponding author: Harry Boos (

Corresponding editor: Patricio Arana

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