SciELO - Scientific Electronic Library Online

 
vol.74 número2Distribución histórica y actual de la lagartija Liolaemus pictus (Dumeril & Bibron 1837) (Liolaemidae) y nuevo límite continental sur de distribución índice de autoresíndice de materiabúsqueda de artículos
Home Pagelista alfabética de revistas  

Servicios Personalizados

Articulo

Indicadores

  • No hay articulos citadosCitado por SciELO

Links relacionados

  • No hay articulos similaresSimilares en SciELO

Gayana (Concepción)

versión On-line ISSN 0717-6538

Gayana (Concepc.) v.74 n.2 Concepción  2010

http://dx.doi.org/10.4067/S0717-65382010000200009 

Gayana 74(2): 147 -151, 2010. ISSN 0717-652X

 

Comunicación breve

 

Changes to the benthic assemblage associated with mollusc and seaweed cultivation in the Quempillén estuary, north patagonia, Chile.

 

Cambios bentónicos asociados a los cultivos de moluscos y de algas del estuario Quempillén en la patagonia norte de Chile.

 

Elizabeth Encalada1, Carlos Bertrán1 & Luis Vargas-Chacoff1,2

1 Instituto de Zoología, Facultad de Ciencias, Universidad Austral de Chile, Valdivia, Chile. *E-mail: luis.vargas@uach.cl

2 Departamento de Biología, Facultad de Ciencias del Mar y Ambientales, Universidad de Cádiz, Cádiz, España.


RESUMEN

Las principales actividades acuícolas en el estuario de Quempillen son la acuicultura de ostras, Ostrea chilensis, y del alga Gracilaria chilensis. La intervención antropogénica al interior del estuario genera cambios significativos a nivel del sedimento y de los contenidos de materia orgánica.


ABSTRACT

The main aquaculture activities in the Quempillen estuary involve cultures of oysters, Ostrea chilensis and algae Gracilaria chilensis. Anthropogenic intervention inside the estuary generates significant changes in sediments and organic matter content.


Estuaries are coastal habitats that show a great deal of heterogeneity in both the physical and chemical characteristics of the water column (e.g. current velocity and salinity gradient), which are generated mainly by the action of the tides (Bertrán et al. 2001, Jaramillo et al. 1984). The fauna inhabiting these estuaries are subjected to considerable variation in environmental factors that determine their distribution, these physical-chemical factors include temperarme and salinity (Beukema 1990, Holland et al. 1987), gradients in the interstitial water (Meadows & Tait 1989) and the characteristics of the sediment, including texture and organic matter content (Nichols et al. 1986, Richter 1985). The aim of this study was to determine the composition and distribution patterns of subtidal macrobenthic communities inhabiting the sediment in the Quempillen estuary, and the effects of two anthropogenic sources of perturbation, mollusc and seaweed cultivation.

The Quempillen estuary is located on the Island of Chiloé (41°52' S; 73°46' W). It was divided into seven stations from the mouth, to the head of the estuary (Fig. 1). The estuary supports aquacultural activity, including the cultivation of oysters (Ostrea chilensis) (stations 3, 4 and 5) and further up the estuary (stations 6 and 7) the cultivation of the algae (Gracilaria chilensis). Sediment and macrofauna samples (n=5) were collected using a PVC corer, 0.0019 m2 for sediments and 0.0095 m2 for macrofauna, at all sampling stations. The sediment samples were frozen and the macrofaunal samples fixed with 10% formalin, the fauna was then extracted with a 0.5 mm sieve, and then preserved in 70% alcohol for later laboratory analysis. Sediment fractions and organic matter content were determined using the methodology of Folk (1980) and Milis (1978) respectively. The samples were sieved using mesh sizes of -1.0 § to separate the gravel and 4 § to separate the sand from the mud fraction. The fauna was removed from the sediment using a stereomicroscope, identified and then counted. Community parameters: Species Richness, Diversity (H'), Dominance (D) and Uniformity (J') (Klemn et al. 1990) were calculated from the obtained data. Analyses of the community structure and sediments were made using nonmetric-Multidimensional Scaling(MDS)withaBray-Curtissimilaritymatrix calculated using data averaged for each station. A one-way ANOVA was made for sediments and the macrofauna. The sediment data were transformed using arcos Vp. For those data that presented significant differences a posteriori Tuckey HSD (PO.05) analysis was conducted.

Gravel, sand and mud fractions are all present inthe sediments of the Quempillen estuary with varying percentages at each of the stations. The biggest percentage of gravel occurred at station 1 (64.71%), the highest percentage of sand at station 3 (93.54%) and the mud fraction was highest at station 7 (48.75%). Across the whole estuary, the sand fraction was the most common type of sediment, whilst gravel was the least common (Table 1, P<0.05). The total organic matter content was highest at station 7 (19.88 %) (Table 2, PO.05). Based onthe results of the MDS and Cluster analyses the separation of several stations is determined by grain size. Throughout cluster and the MDS analyses on the x-axis, it is possible to observe the gradient of grain size, with coarser grains toward the left (1-2) and finer toward the right (Fig. 2 a and b).

Figure 1: The Quempillén Estuary: Location of the study area and of the sampled subtidal stations. The numbers show the exactly position of the stations.

Figura 1: Estuario Quempillén: Ubicación del área de estudio y de las estaciones submareales muestreadas. Los números indican la ubicación exacta de las estaciones.

Figure 2: Cluster (a) and nonmetric MDS (b) analyses of sediments, per stations, in the Quempillén estuary. E = station.

Figura 2: Análisis de Cluster (a) y MDS (b) de sedimentos, de las estaciones, en el estuario Quempillén. E = estación.

Overall 36 species were identified, Corophium insidiosum (Arthropoda, Corophiidae) being the most abundant species (Table 3). Community parameters showed that Diversity values were highest at station 2 (value of 1.88). The values of Uniformity (J) were also high, which relates to the low Dominance of Simpson (D = 1-J') values and this was reflectedby the high values of Diversity (see Table 4). The Diversity and Species Richness values exhibited significant differences (PO.05), while Uniformity and Abundance did not exhibit significant differences (P>0.05) between stations. Both cluster and MDS analyses supported this finding, forming two large groups : a) stations 1, 2 and 4 and b) stations 3, 5, 6 and 7, separating the stations of both ends, and placing together the stations at the centre of the estuary (Figs. 3 a and b).

Figure 3: Cluster (a) and nonmetric MDS (b) analyses of macrofauna, per stations, in the Quempillén estuary. E = station.

Figura 3: Análisis de Cluster (a) y MDS (b) de fauna, de las estaciones, en el estuario Quempillén. E = estación.

Anthropogenic activities at the inside the Quempillén estuary (mollusc and algae cultivation) would depend upon the type andtextural charactenstics of the sediment andthe composition and diversity of macrofauna associated. Summarizing our results, the sediment in the estuary (after analysis of ANOVA, Pos Hoc, MDS and Cluster Analyses) can be divided into 3 groups. The first group formed by the stations nearest to the mouth (1 and 2) was dominated by coarse sediments (< -1 <1>) (Folk 1980) with low organic content, the second group (stations 4 and 5) covered the middle reaches of the estuary and was dominated by sand (between -1 and 4 <1>), finally the third group (3, 6 and 7 stations) at the head of the estuary dominated by sand-muddy sediments (> 4 <1>).

The distribution of sediment type and organic matter withinthe estuary concur with that reported by Bertrán (1984,1989),  and Peterson et al. (1984) in Washington and Oregon (USA).  Jaramillo et al. (1985) and Richter (1985) for the Queule and  Lingüe estuaries (Southern Chile). In those estuaries the sand fraction decreased while the mud fraction increases across the transition from marine waters to the limnetic waters. These results are also similar to those obtained for estuarine areas at other latitudes: Chester et al. (1983) in North Carolina (USA)

 However, the values of total organic matter at all stations were very high supporting the observations of authors such as Alveal 1988, Berrios et al. 1991-1992; who indicated that cultivated algae such as Gracilaria chilensis serves as a trap for fine sediment.

Table 1: Variation in the sediment fractions and organic matter content, at each station of the Quempillén estuary. Data points represents mean ± S.D. (n=5 per group at each sampling station). Different letters indicate significant differences among stations (P<0.05, one-way ANOVA, Tukey test).

Tabla 1: Variación de las fracciones del sedimento y contenido de materia orgánica, en cada estación del estuario Quempillén. Los datos representados son la media ± S.D. (n=5 por grupo de cada estación muestreada). Letras diferentes indican diferencias significativas entre estaciones (P<0.05, una-va ANOVA, prueba de Tukey).

Table 2: Average percentage of the Total Organic Matter in the sediments, of the Quempillén estuary. Further details as in legend of table 1.

Tabla 2: Promedio en el porcentaje del Total de Materia Orgánica de los sedimentos en el estuario Quempillén. Más detalles como en la leyenda de la tabla 1.

Table 3: Average Abundance (N° ind.nv2) of macroinfauna collected at each station, in the Quempillén estuary.

Tabla 3: Abundancia promedio (N° ind.nv2) de la macroinfauna colectada en cada estación en el estuario Quempillén.

Table 4: Community parameters: Species Richness, Diversity (H') and Uniformity (T) at all stations.

Tabla 4: Parámetros comunitarios: Riqueza de Especies, Diversidad (H') y Uniformidad (T) en todas las estaciones.

The subtidal macrobenthic communities in the Quempillén estuary comprised of 36 species, which is similar to other estuaries studied in southern Chile, suchas the Queule estuary where Bravo (1984) reported 35 species, the Lingüe where Richter (1985) reported 20 species, and the Bio Bío estuary where, depending on the seasons of the year, between 16 and 42 species were recorded (Bertrán et al. 2001). Diverse studies made in estuarine areas (Bertrán et al. 2001, Hughes & Gerdol 1997, Jaramillo et al. 1985, Richter 1985, Bravo 1984) have concluded that a decrease species diversity moving upstream correlates with an increase in the density of those species present. The results obtained in the present study concur with this hypotheses, there was a gradual decrease in the number of species moving from the most marine station upstream (from 20 to 12 different species). The Cluster and the MDS analyses indicate 2 groups, with stations 1,2 and 4 in the first group and the remaining stations in the second group (3,5,6 and 7 stations), representing the change inthe diversity inthe middle zone of the estuary. The higher Diversities and Species Richness values were found in the first group (stations 1, 2 and 4), towards the mouth of the estuary, as has been found previously by Bertrán et al. 2001, Hughes & Gerdol 1997, Richter 1985, Jaramillo et al. 1985, Bravo 1984. The conclusion of this study is that different anthropogenic activities change the characteristics of the macrofaunal benthos, and particularly the sediment structure and organic matter content.

ACKNOWLEDGEMENTS

We thank Dr. Sandor Mulsow and Dr Matthew Lee (Instituto de Geociencias e Instituto de Biología Marina, Universidad Austral de Chile, Valdivia, Chile) for their help in correcting the English of this manuscript. This study was carried out with financial assistance provided by the benthic Sub-program 45703926, Facultad de Ciencias and financial assistance provided by DID 1301-32-28 of the Universidad Austral de Chile.

BIBLIOGRAPHY

Alveal, K. 1988. Gracilaria de Tabul. Historia y significado de un recurso marino. Gayana, Botánica 45: 119-140.        [ Links ]

Berrios, M., A. Pacheco, J. Olivares & E. Fonck. 1991-1992. Dinámica de sedimentos en una pradera de Gracilaria chilensis en Bahía la Herradura de guayacán. Ciencia y Tecnología del Mar. Comité Oceanógrafico Nacional 15: 31-41.        [ Links ]

Bertrán, C. 1984. Macroinfauna intermareal en un estuario del sur de Chile (Estuario del río Lingue, Valdivia). Studies on Neotropical Fauna and Environment 19: 33-46.         [ Links ]

Bertrán, C. 1989. Zonación y dinámica temporal de la macroinfauna intermareal en el estuario del río Lingue. Revista Chilena de Historia Natural 62: 19-32.         [ Links ]

Bertrán, C, J. Arenas & O. Parra. 2001. Macrofauna del curso inferior y estuario de río Biobío (Chile): cambios asociados a variabilidad estacional del caudal hídrico. Revista Chilena de Historia Natural 74: 331-340         [ Links ]

Beukema, J. 1990. Expected effects of changes in winter temperatures on benthic animals living in soft sediments in coastal North Sea areas, pp. 83-92 in J. J. Beukema et al (eds.), Expected Effects of Climatic Change on Marine Coastal Ecosystems. Kluwer Academic Publishers, The Netherlands.         [ Links ]

Bravo, A. 1984. Distribución de la Macroinfauna submareal en los fondos blandos de la bahía Queule y estuario del río Queule. Medio Ambiente 7: 37-46         [ Links ]

Chester, A., R. Ferguson & G. Thayer. 1983. Environment gradients and benthic macroinvertebrate distribution in a shallow north Carolina estuary. Bulletin of Marine Science 33: 282-295.         [ Links ]

Folk, R. 1980. Petrology of sedimentary rocks. Hemphill Publishing Co., Austin, Texas. 184 pp.         [ Links ]

Holland, A., A. Shaghnessy & M. Hiegel. 1987. Long-term variation in mesohaline Chesapeake Bay macrobenthos: Spatial and temporal patterns. Estuaries 10: 227-245         [ Links ]

Hughes, R.G. & V. Gerdol. 1997. FactorsAffecting the Distribution of the Amphipod Corophium volutator in two estuaries in South-East England. Estuarine, Coastal and Shelf Science 44: 621-627.         [ Links ]

Jaramillo, E., S. Mulsow, M. Pino & H. Figueroa. 1984. Subtidal Benthic Macroinfauna in an estuary of south of Chile: Distribution pattern in relation to sediment types. Marine Ecology-PS.Z.NI. 5: 119-133.         [ Links ]

Jaramillo, E., C. Bertrán, G. Aguilar, A. Turner & M. Pino. 1985. Annual fluctuations of the subtidal macroinfauna in an estuary of south of Chile. Studies on Neotropical Fauna and Environment 20: 33-44.         [ Links ]

Klemn, D.J., PA. Lewis, F Fulk & M. Lazorchak. 1990. Macroinvertebrates field and Laboratory Methods for evaluating the biological integrity of surface waters. EPA/600/4-90/030. United States Environmental Protection Agency 255 pp.         [ Links ]

Mills, A. 1978. A comparison of methods of determining organic carbon in marine sediments with suggestions for a standard method. Hydrobiologia 57:45-52.         [ Links ]

Meadows,P & J. Tait. 1989. Modificationof sediments permeability and shear strength by two borrowing invertebrates. Marine Biology 101:75-82.         [ Links ]

Nichols, F., J. Cloern, S. Luoma & D. Peterson. 1986. The modification of an estuary. Science 231: 525-648         [ Links ]

Peterson, C, K. Scheidegger & P Komar. 1984. Sediment composition and hydrography in six high-gradient estuaries of the Northwestern United States. Journal of Sedimentary Petrology 54: 86-97         [ Links ]

Richter, W. 1985. Distribution of the soft-bottom macroinfauna in an estuary of southern Chile. Marine Biology 86: 93-100.        [ Links ]

Recibido: 14.10.09

Aceptado: 20.06.10