Survey
* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project
* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project
VERTIMAR-2005 Symposium on Marine Accidental Oil Spills Temporal evolution of infaunal and suprabenthic communities on the Galician continental shelf (NW, Iberian Peninsula), after the Prestige oil spill Santiago PARRA and Inmaculada FRUTOS Instituto Español de Oceanografía, C.O. de A Coruña, Apdo. 240, 15001 A Coruña, Spain 1. INTRODUCTION In November, 2002 the single-hulled tanker Prestige sank 130 miles off the coast of Muxía (A Coruña, Galicia). Roughly 20,000 tons of fuel oil spilled into the sea, causing a vast black tide which mainly affected the entire Galician coast. During the 2002-2004 period a series of oceanographic surveys were conducted using different, complementary sampling systems to be able to quantify the different compartments of the bottom ecosystem (infauna, suprabenthos, epifauna and megafauna) and to acquire knowledge on the state of the communities and resources (Sánchez, 2003; Serrano et al., in press). A sampling strategy was designed to include bottom stations located in two geographic sectors organized in a radial arrangement at three depth strata. This paper presents new data on the temporal evolution of the sediment characteristics in all the sectors and depth strata during the 2002-2004 period and temporal changes in the infaunal communities (zones 1 and 2, depth strata A and B) and suprabenthic communities (zone 3, depth strata A, B and C) during the first year of study (2002-2003). 2. RESULTS AND DISCUSSION No important changes were seen in the temporal evolution of the sedimentological characteristics (granulometry and organic content) of the stations under study during the entire study period (2002-2004). As regards the infaunal communities zone 1, in stratum A (71-120 m), the stations presented mud bottoms or fine sands with a moderate amount of organic content. The dominant zoological group in terms of abundance in this stratum were the polychaetes (accounting for over 77 %), with the spionid Prionospio fallax being the characteristic species. One of the outstanding traits of the temporal evolution in this depth stratum was the increase in spring in the abundance of the polychaetes and molluscs and the decreasing presence of the group “others”. In stratum B (121-200 m) the stations had a sediment made up of fine sands with a low organic content. In this stratum, the polychaetes were also the prevailing zoological group with the dominant species being Prionospio fallax, Monticellina dorsobranchialis and Aricidea sp. As regards the temporal evolution in this depth stratum, we may point to a slight decline in the abundance of polychaetes in spring and a significant increase in molluscs and crustaceans, and to a lesser extent, the group “others”. The stations located in the most shallow stratum (A; 71-120 m) of zone 2, presented mud bottoms or fine sands with a moderate to low organic content. In this stratum the dominant zoological group in abundance were the polychaetes (which did not exceed 70% of the abundance), followed by the echinoderm, molluscs and “others”, accounting for over 10%. The most common species were the polychaetes Prionospio fallax and Tharyx sp., the echinoderm Amphiura filiformis and the bivalve Mysella bidentata. In the temporal evolution of these depth strata we may highlight a decrease in the abundance of the polychaete group in spring and a significant rise in the echinoderms and, to a lesser extent, in the groups molluscs, crustaceans and “others”. The stations in stratum B (121-200 m) had a characteristic sediment comprised of very fine sands with a moderately selected low organic content. The dominant zoological group in this stratum was made up of the polychaetes (more than 73 %), followed by the crustaceans which accounted for up to 12.73 %. The characteristic species in this stratum were the peracarida crustacean Ampelisca sp. and the polychaetes Prionospio fallax, P. steentrupii and Monticellina dorsobranchialis. The temporal evolution of this depth strata in spring exhibited a slight increase in the abundance of the group molluscs and crustaceans and a decrease in the group “others”. The dominant species, the polychaetes, did not undergo any significant changes. Overall, slight variations in the population parameters were seen in the winter and spring in zone 1. The most significant changes in spring were a slight decrease in total abundance and in VERTIMAR-2005 Symposium on Marine Accidental Oil Spills the abundance of some of the less important groups while the crustaceans underwent a modest increase, particularly in the deepest stratum (figure 1). Species richness, diversity and equitableness rose slightly. The most notable decrease was found in total abundance and in the group “others”, while increased values were recorded for molluscs, echinoderms and crustaceans in spring. At present, no important changes were seen in the temporal evolution of the bioindicator infaunal species (opportunistic or sensible oil spill species) during the first study period (2002-2003), like was observed in 1993, in A Coruña coast, after Aegean Sea oil spill (Gómez Gesteira and Dauvin, 2000; Parra and López-Jamar, 1997). ZONE 1 WINTER ZONE 2 SPRING Total WINTER SPRING Total Stratum A Stratum A Stratum B Stratum B Polychaetes Echinoderms Others Molluscs Crustaceans Figure 1: Percentage of total infaunal abundance shown by taxonomic group in zones 1 and 2, by depth strata. The suprabenthic communities under study from the shallowest stratum (71-120 m) of zone 3 were dominated by the amphipod Amphilochoides boecki, the mysids Leptomysis gracilis and Anchialina agilis and the euphausiid Nyctiphanes couchi. As regards the temporal evolution, we may point to an increase in spring in the abundance of the group euphausiids along with a substantial decrease in the amphipods and mysids. In the middle stratum (121-200 m) of zone 3, the community was characterised by the mysids Anchialina agilis and Erythrops neapolitana and the euphausiid Nyctiphanes couchi. On a temporal level, we observed a considerable increase in the amphipods in addition to a less important decrease in the cumaceans and euphausiids in spring. In contrast, in the deepest stratum (201-500 m) of zone 3, where the winter community was dominated by the decapods, this group underwent a substantial decline accompanied by a great rise in the euphausiids group. The dominant species in this community were the decapod Pasiphaea sivado, the amphipods Scopelocheirus hopei and Orchomenella nana. REFERENCES Gómez Gesteira, J.L., Dauvin, J.-C., 2000. Amphipods are good bioindicators of the impact of oil spills on soft-bottom macrobenthic communities. Mar. Poll. Bull. 40, 1017-1027. Parra, S. y López-Jamar, E., 1997. Cambios en el ciclo temporal de algunas especies endofaunales como consecuencia del vertido del petrolero Aegean Sea. Publ. Esp. Ins. Esp. Oceanogr. 23, 71-82. Sánchez, F., 2003. Presencia y cuantificación del fuel sedimentado en las plataformas de Galicia y mar Cantábrico. IEO Prestige web report nº 14: www.ieo.es/prestige/informe14.htm, 7 pp. Serrano, A., Sánchez, F., Preciado, I., Parra, S. and Frutos, I. In press. Spatial and temporal changes in benthic and demersal communities of the Galician continental shelf after the Prestige oil spill. Mar. Poll. Bull.