Distribuição geográfica da fauna e flora da Baía de Guanabara

The author studied, the horizontal and vertical distribution of most common part of the flora and fauna of the bay of Guanabara at Rio de Janeiro. In this paper the eulittoral, poly, meso and oligohaline regions were localised and studied; and the first chart of its distribution was presented (fig. 2). The salinity of superficial waters was established through determinations based on 30 trips inside the buy for collecting biological materials. Some often 409 determinations which were previous reported together with the present ones served for the eleboration of a salinity map of the bay of Guanabara (fig. 1). This map of fig. 2 shows the geographic locations of the water regions. EULITTORAL WATER REGIME — Fig. 3 shows the diagram scheme of fauna and flora of this regime. Sea water salinity 34/1.000, density mean 1.027, transparent greenish waters, sea coast with moderate bursting waves. Limpid sea shore with white sand, gneiss with the big barnacle Tetraclita squamosa var. stalactifera (Lam. Pilsbry. Vertical distributions: barna¬cles layers with a green region in which are present the oyster Ostrea pa-rasitica L., the barnacles Tetraclita, Chthamalus, Balanus tintinnabulum var. tintinnabulum (L.) e var. antillensis Pilsbry in connection with several mollusca and the sea beatle Isopoda Lygia sp. Covered by water and exposed to air by the tidal ritms, there is a stratum of brown animals that is the layer of mussels Mytilus perna L., with others brown and chestnut animals : the Crustacea Pachygrapsus, the little crab Porcellana sp., the stone crab Me-nippe nodifrons Stimpson, the sea stars Echinaster brasiliensis (Mull. & Tr.), Astropecten sp. and the sea anemones Actinia sp. Underneath and never visible there is a subtidal region with green tubular algae of genus Codium and amidst its bunches the sea urchin Lycthchinus variegatus (Agass.) walks and more deeply there are numerous sand-dollars Encope emarginata (Leske). The microplancton of this regime is Ceratiumplancton. POLYHALINE WATER REGIMB — Water almost sea water, but directly influenced by continental lands, with rock salts dissolved and in suspension. Salinity: 33 to 32/1.000. This waters endure the actions of the popular nicknamed «water of the hill» (as the waters of mesohaline and oligohaline regimes), becoming suddenly reddish during several hours. That pheno¬menon returns several times in the year and come with great mortality of fishes. In these waters, according to Dr. J. G. FARIA there are species of Protozoa : Peridinea, the Glenoidinium trochoideum St., followed by its satellites which he thinks that they are able to secret toxical substances which can slaughter some species of fishes. In these «waters of the hill» was found a species of Copepoda the Charlesia darwini. In August 1946 the west shore of the Guanabara was plenty of killed fishes occupying a area of 8 feet large by 3 nautical miles of lenght. The enclosure for catching fishes in the rivers mouthes presents in these periods mass dead fishes. The phenomenon of «waters of the hill» appears with the first rains after a period of long dryness. MESOHALINE WATER REGIME — Fig. 4 shows the the diagramm scheme. Salt or brackish water from 30 to 17/1.000 salinity, sometimes until 10/1.000. Turbid waters with mud in suspension, chestnut, claveyous waters; shore dirty black mud without waving bursting; the waters are warmer and shorner than those of the polihaline regime. Mangrove shore with the mangrove trees : Rhizophora mangle L., Avicennia sp., Laguncularia sp., and the »cotton tree of sea» Hibiscus sp. Fauna: the great land crab «guaimú» Cardisoma guanhumi Latr., ashore in dry firm land. There is the real land crab Ucides cordatus (L.) in wetting mud and in neigh¬ bourhood of the burrows of the fiddler-crabs of genus Uca. On stones and in the roots of the Rhizophora inhabits the brightly colored mangrove-tree-crab («aratu» Portuguese nickname) Goniopsis cruentata (Latreille) and the sparingly the big oyster Ostrea rhizophorae Guild. Lower is the region of barnacles Balanus amphitrite var. communis Darwin and var. niveus Darwin; Balanus tintinnabulum var. tintinnabulum (L.) doesn't grow in this brackish water; lower is the region of Pelecipoda with prepollency of Venus and Cytherea shell-fishes and the Panopeus mud crab; there are the sea lettuce Ulva and the Gastreropod Cerithium. The Paguridae Clibanarius which lives in the empty shells of Gasteropod molluscs, and the sessile ascidians Tethium plicatum (Lesuer) appears in some seasons. In the bottom there is a black argillous mud where the «one landed shrimps» Alpheus sp. is hidden. OLIGOHALINE WATER REGIME — The salinity is lower than 10/1.000. average 8/1.000. There are no barnacles and no sea-beetles Isopods of genus Lygia; on the hay of the shore there are several graminea. This brackish water pervades by mouthes of rivers and penetrates until about 3 kilometers river above. While there is some salt dissolved in water, there are some mud crabs of the genus Uca, Sesarma, Metasesarma and Chasmagnatus. The presence of floating green plants coming from the rivers in the waters of a region indicated the oligohaline waters, with low salt content because when the average of NaCl increases above 8/1.000 these plants die and become rusty colored.

Águas com predominância de Eutreptia lanowi steuer e Chlamydomonas reinhardi dangeard no plancton, na enseada de Inhauma, Baía de Guanabara

In brackish waters of a creek of Guanabara Bay, the author points by the first time the presence of Chlamydomonas reinhardi, Eutreptia lanowi, Oscillatoria putrida, O. limosa, O. chlorina that were unknown in our waters; such biologic indicators proved themselves pollutional conditions, so bad a stark-mesosaprobic regime. Other news are plankton analysis by the Standar methods, of two most expressive samples of water masses;also the mobility of the plankters are measured in micra by second.

Estudos aplicados à recuperação biológica da Baía de Guanabara

Continuamos observações sobre as biocenoses litorâneas, na parte oeste do Rio de Janeiro, na Enseada mais poluída, onde está a ilha do Pinheiro. Chegamos à conclusão que há graus de estragos acima dos verificados em publicações anteriores, os 7º, 8º, 9º e 10º graus de estragos, com desaparecimento de todas cinturas vegetais. Anotamos os assoreamentos; devido a aterros artificiais na vizinhança, a lama subiu muito, meio metro em 20 anos, ou seja 2,5 centímetros por ano. Apresentamos as alterações ecológicas resultantes do assoreamento, mostramos a mudança de vários nichos de alguns componentes do manguezal. Fizemos 4 mapas ecológicos, em local que constitui a média representativa do que se passou na Enseada de Inhaúma nesses últimos 5 anos. Chegamos a índices de recuperação de zonações do manguezal, como 60/1 para o Avicennietum; e nenhum para o Laguncularietum, comunidade de "mangues mansos" que está em regressão; Houve regeneração das populações de caranguejos Ucides e Cardisoma que voltaram a habitar a Ilha do Pinheiro. Mostramos uma correlação entre o guaiamu e a aroeira da praia, Schinus. Concluímos que: podem ser usadas as técnicas de recuperação de poluição para esses caranguejos e guaiamus, para a alimentação humana, assim como para peixes apanhados em alagados de manguezais poluídos. O material pescado no Rio de Janeiro, tendo algas do gênero Oscillatoria, apresenta um cheiro de urina pútrida, bem como outros cheiros, mas pode ser recuperado para a alimentação humana. Damos sugestões para se utilizar cercados de vegetação de manguezal contra a poluição em locais apropriados, alagados com camarões e peixes, como usam-se na Ásia. As plantas utilizadas baseiam-se no estudo ecológico que estabelece o nicho apropriado a cada uma delas, resistente á poluição, e que pode combater alguns estragos; entre elas as Iresine e as do gênero Avicennia, pois elas promoveram uma pequena recuperação na Ilha do Pinheiro, onde apareceram novamente os caranguejos e guaiamus.

Estudo do comportamento da população de Macaca mulatta Zimmermann, 1780 na Ilha do Pinheiro, RJ, Brasil: organização social, levantamento da população e condições de alimentação

Os AA. realizaram um trabalho com a finalidade de aumentar a população de Macaca mulatta na ilha do Pinheiro, RJ, através do conhecimento de dados comportamentais desta colônia. Neste estudo inicial são empregadas técnicas etológicas de observação direta visando a esclarecer aspectos da organização social, determinar a quantidade de animais discriminada por sexo e levantar as condições de alimentação. A população é constituída de 91 animais distribuídos em três grupos sociais, havendo 22 machos, 40 fêmeas e 29 filhotes.

Distribuição de coprostanol (5beta(H)-colestan-3beta-ol) em sedimentos superficiais da Baía de Guanabara: indicador da poluição recente por esgotos domésticos

A critical evaluation is presented on the use of faecal sterols for the identification of sewage contamination in Guanabara Bay. Sediments were collected from 8 stations in the bay selected as representative of different contamination levels. GC/MS determination of faecal sterols gave: coprostanol, 335 - 40000 ng g-1; coprostanone, 112-4136 ng g-1; cholesterol, 1407-7800 ng g-1; cholestanol, 2011 - 10900 ng g-1 and cholestanone, 655-7954 ng g-1. The observed concentration is in accordance with the presence of known pollution sources, however, concentration ratios of different sterols species produced unclear results evidently influenced by primary production and microbial processes.

Estimativa do fluxo de amônia na interface ar-mar na Baía de Guanabara: estudo preliminar

In the begining of April 2004, concentrations of NHx (NH3 + NH4+) were measured in surface waters of the Guanabara Bay. Concentrations varied from 2 to 143 mmol L-1. Ammonia exchange at the air-sea interface was quantified using a numerical model. No measurement of NH3 concentration in air (c air) was performed. Thus, calculations of NH3 flux were based on the assumptions of c air = 1 and 5 µg m-3. Fluxes were predominantly from the water to the atmosphere and varied from -20 to almost 3500 µg N m-2 h-1.

Distribuição espacial de ferro, cobre e chumbo em sedimentos de manguezal em um gradiente de degradação na Baía de Guanabara (Estado do Rio de Janeiro)

Iron, copper and lead distribution was evaluated in sediment cores from a disturbed mangrove area in Guanabara Bay: a core from a seaward site where mangrove vegetation was removed ~20 yr before sampling (MD); a core from an intermediate site with dead vegetation, apparently due to insect attack (MP), and a core from a landward site with living vegetation (MV). Metal concentrations showed increasing values seaward while organic matter content showed an inverse trend, displaying a negative correlation with metals. This unusual correlation indicates opposite sources, since metals come from the bay and the main OM origin is probably degraded mangrove vegetation. Plant cover loss seems to be a critical factor affecting metal accumulation, particularly due to changes in OM input.

Marcadores orgânicos de contaminação por esgotos sanitários em sedimentos superficiais da baía de Santos, São Paulo

Organic markers, such as sterols and ketones, were used to assess sewage contamination in sediments from the Santos Bay, SP, and its continental shelf. These compounds were analyzed by GC/FID after soxhlet extraction, clean up and derivatization. The concentration of coprostanol and ratios between selected sterols were used to evaluate fecal contamination. The stations located in the mid-western part of the Santos Bay presented organic matter from sewage due to the input of fecal material from the city of Santos by submarine sewage outfall. Stations located at the continental shelf did not present fecal contamination. Coprostanol levels in sewage outfall stations were higher in comparison to other Brazilian coastal areas, except Guanabara Bay/RJ, and could be related to the fraction of the population without sewage treatment.

Fluxos de óxido nitroso na interface ar-mar na Baía de Guanabara

In Surface water concentrations of N2O were measured at 37 stations in Guanabara Bay and fluxes estimated across the air-sea interface. Concentrations averaged 8.2 ± 2.2 nmol L-1 and 90% of the stations showed supersaturation averaging 33%. N2O fluxes were estimated using a two-film model which is given by the product of the concentration difference across the film and the gas transfer coefficient (k w). Two parametrizations of k w were used which provided average fluxes of 0.3 and 3.0 µg N m-2 h-1. Flux measurements using floating chambers (not reported here) seem to agree with the upper limit of these estimates.

Bioconcentração e biomagnificação de metilmercúrio na baía de Guanabara, Rio de Janeiro

Methylmercury was determined in water and aquatic biota from Guanabara Bay. Trophic transfer of methylmercury was observed between trophic levels from prey (microplankton, mesoplankton and fish with different feeding habits) to top predator (pelagic demersal fish). Top predator fish presented the highest methylmercury concentrations (320.3 ± 150.7 mg kg-1 dry wt.), whereas microplankton presented the lowest (8.9 ± 3.3 mg kg-1 dry wt.). The successive amplification of methylmercury concentrations and its bioconcentration factor with increasing trophic levels from base to top indicate that biomagnification may be occurring along the food web. Results suggest the importance of feeding habits and trophic level in the bioaccumulation of methylmercury by aquatic biota.

Estrutura das comunidades fitobentônicas do infralitoral da Baía de Sepetiba, RJ, Brasil

Caracteriza-se neste estudo a estrutura das comunidades fitobentônicas em cinco locais da baía de Sepetiba, RJ. Foram realizadas amostragens do tipo destrutiva desde a região mais interna da baía, sujeita diretamente aos impactos antrópicos locais, até a região próxima ao mar aberto, onde a interferência humana é reduzida, em quatro épocas do ano de 1999 (janeiro, maio, agosto e novembro). Para comparação dos resultados foram utilizados: o número total de espécies, a biomassa total, a diversidade (H') e a equitabilidade (J). Foram identificados 96 táxons, sendo 61 rodofíceas, 18 clorofíceas, 15 feofíceas e duas cianofíceas. O maior número de táxons (65) e os mais elevados valores de biomassa (492,4 g.m-2) foram observados no ponto 5, situado na Ponta da Marambaia. Ficou evidenciado o aumento da diversidade da região mais interna da baía em relação ao local mais próximo ao oceano. Sargassum spp. apresentaram a maior biomassa, seguida por Padina gymnospora e outras algas de menor porte como Hypnea spp., Gelidium pusillum, Pterocladiella caerulescens e Gelidiopsis spp. A utilização do método destrutivo permitiu uma caracterização detalhada da composição e da estrutura das comunidades fitobentônicas da baía de Sepetiba, facilitando no futuro, a identificação das mudanças impostas às comunidades através de abordagens metodológicas mais simples.