RESUMOOs sistemas de ressurgência possuem uma grande diversidade de microrganismos pelágicos e sua composição e atividade são determinadas por fatores como a temperatura e a concentração de nutrientes. A técnica de Electroforese em Gel por Gradiente Desnaturante (EGGD) foi utilizada para verificar a variabilidade genética espacial e temporal de Bacteria e Archea em duas estações na costa da região de Arraial do Cabo; uma com maior pressão da ressurgência, e a outra sobre pressão antropogênica. Além disso, as variáveis bióticas e abióticas foram medidas nas águas superficiais e de fundo de outras três estações situadas entre essas estações. Seis amostragens foram realizadas durante um ano e representaram adequadamente os diferentes graus de ressurgência e de pressões antropogênicas no sistema. A Análise por Componente Principal (ACP) mostrou uma correlação negativa entre a concentrações de amônia e de fósforo e a produção secundária procariótica e o total de bactérias heterotróficas. A ACP também mostrou uma correlação negativa entre a temperatura e a abundância de células procarióticas. As composições de Bacteria e Archaea foram variáveis, assim como as condições oceanográficas, e a ressurgência teve uma pressão regional enquanto a pressão antropogênica foi pontual. Sugerimos que as medidas de produção secundária procariótica esteve associada à atividade de ambas Bacteria e Archaea, e que a disponibilidade de substrato e a temperatura determinam a ciclagem de nutrientes.

ABSTRACTUpwelling systems contain a high diversity of pelagic microorganisms and their composition and activity are defined by factors like temperature and nutrient concentration. Denaturing gradient gel electrophoresis (DGGE) technique was used to verify the spatial and temporal genetic variability of Bacteria and Archaea in two stations of the Arraial do Cabo coastal region, one under upwelling pressure and another under anthropogenic pressure. In addition, biotic and abiotic variables were measured in surface and deep waters from three other stations between these stations. Six samplings were done during a year and adequately represented the degrees of upwelling and anthropogenic pressures to the system. Principal Component Analysis (PCA) showed negative correlations between the concentrations of ammonia and phosphorous with prokaryotic secondary production and the total heterotrophic bacteria. PCA also showed negative correlation between temperature and the abundance of prokaryotic cells. Bacterial and archaeal compositions were changeable as were the oceanographic conditions, and upwelling had a regional pressure while anthropogenic pressure was punctual. We suggest that the measurement of prokaryotic secondary production was associated with both Bacteria and Archaea activities, and that substrate availability and temperature determine nutrients cycling.

Arraial do Cabo is where upwelling occurs more intensively on the Brazilian coast. Although it is a protection area it suffers anthropogenic pressure such as harbor activities and sporadic sewage emissions. Short-time studies showed a high variability of bacterial production (BP) in this region but none of them evaluated BP during long periods in a large spatial scale including stations under different natural (upwelling and cold fronts) and anthropogenic pressures. During 2006, we sampled surface waters 10 times (5 in upwelling and 5 in subsidence periods) in 8 stations and we measured BP, temperature as well as the concentrations of inorganic nutrients, pigments and particulate organic matter (POM). BP was up to 400 times higher when sewage emissions were observed visually and it had a positive correlation with ammonia concentrations. Therefore, in 2007, we did two samples (each during upwelling and subsidence periods) during sewage emissions in five stations under different anthropogenic pressure and we also measured particles abundance by flow cytometry. The 12 samples in the most impacted area confirmed that BP was highest when ammonia was higher than 2 μM, also reporting the highest concentrations of chlorophyll a and suspended particles. However, considering all measured variables, upwelling was the main disturbing factor but the pressure of fronts should not be neglected since it had consequences in the auto-heterotrophic coupling, increasing the concentrations of non fluorescent particles and POM. Stations clustered in function of natural and anthropogenic pressures degrees and both determined the temporal-spatial variability.