Made available in DSpace on 2017-07-21T18:13:50Z (GMT). No. of bitstreams: 1 LucineiJoseMysznskijunior.pdf: 4515058 bytes, checksum: 797466883c2d16669cdd6591abd1131c (MD5) Previous issue date: 2012-03-09 / In this study we investigated the taphonomic and stratigraphic analyses of the basal layers of Sequence B (Neopraghiano / Eoemsiano), Ponta Grossa Formation, with a focus on Curva II outcrop, Ponta Grossa, Paraná, which until then had not been studied under these aspects. The objective is to provide a description and interpretation of the above mentioned outcrop, as well as the inclusion of its layers in stratigraphic framework of the sequence. In order to obtain more accurate data, the methodology used to collect data was of taphonomic high-resolution. The fauna here considered is a typical representative of the Malvinokaffric Realm and occurs distinctly along the Curva II outcrop. Three different taphocenosis representing different sedimentary environments have been identified. The data obtained in this study were integrated into the areas of occurrence of fossiliferous outcrops adjacent to Curva II. A combined analysis of the taphonomic, paleontological and stratigraphic aspects, followed by a reinterpretation of the outcrops in northeastern urban area of Ponta Grossa, inserts the Curva II outcrop above sections of the UEPG Campus, as well as Francelina I, II and III and below sections of Curva I and Franco da Rocha, which are representatives of a transgressive process, in a situation of sedimentary retrogradation which occurred in the passage Neopraghiano/Eoemsiano in the Ponta Grossa Formation, filling, thus, a gap in the stratigraphic sequence of the base of sequence B. / Na presente pesquisa buscou-se a análise estratigráfica e tafonômica das camadas basais da Sequência B (Neopraguiano/Eoemsiano), Formação Ponta Grossa, com enfoque no afloramento Curva II, Ponta Grossa, Paraná, que até então não havia sido estudado sob estes aspectos. Objetivou-se a descrição e interpretação do afloramento citado bem como a inserção de suas camadas no arcabouço estratigráfico de sequências. Com o intuito de se obter dados mais precisos, utilizou-se metodologia de coleta de alta resolução tafonômica. A fauna aqui analisada é representante típica do Domínio Malvinocáfrico e ocorre distintamente ao longo do afloramento Curva II tendo sido identificadas três diferentes tafocenoses que representam distintos ambientes de sedimentação. Os dados obtidos nesta pesquisa foram integrados aos de áreas de ocorrência fossilífera adjacentes ao afloramento Curva II. Com uma análise conjunta entre os aspectos tafonômicos, paleontológicos e estratigráficos e após uma reinterpretação dos afloramentos da região nordeste do perímetro urbano de Ponta Grossa, insere-se o afloramento Curva II acima das seções Campus UEPG e Francelina I, II e III e abaixo das seções Curva I e Franco da Rocha, sendo representantes de um processo transgressivo, em situação de retrogradação sedimentar ocorrida na passagem Neo-praguiano/Eo-emsiano da Formação Ponta Grossa, preenchendo, desta maneira, uma lacuna na coluna estratigráfica de sequências local da base da Sequência B.

No presente estudo foi realizada uma caracterização limnológica comparativa de dezoito lagoas pertencentes ao sistema lacustre do vale do médio Rio Doce e da comunidade de macroinvertebrados bentônicos, analisando-se a composição e a riqueza de espécies. A espécie exótica Melanoides tuberculata invadiu várias regiões do Brasil, e representa uma ameaça para a fauna de moluscos e outros invertebrados nativos das comunidades bentônicas onde se estabelecem. Para isto foram realizadas coletas nos períodos climáticos, chuvoso e seco, amostrando-se em cinco pontos em cada lagoa incluindo a região litorânea e limnética. Foram realizadas medidas físicas e químicas da água e a análise granulométrica, teor de matéria orgânica e classificação textural do sedimento das lagoas. A comunidade bentônica foi amostrada com draga de Van Veen nos diferentes pontos e o material foi lavado em peneiras de 210 \'mü\'m de abertura de malha, preservado em formol 8% e posteriormente triado e identificado. Os resultados obtidos evidenciaram que a maioria das lagoas estudadas são ambientes de águas levemente ácidas, bem oxigenadas, com baixa concentração de nutrientes na coluna da água, sendo sistemas de baixa trofia (oligotróficos ou mesotróficos). As lagoas diferem quanto à profundidade e transparência da água e aquelas com profundidade superior a 10 metros observou-se estratificação térmica no período chuvoso e isotermia no período seco. A comunidade de macroinvertebrados bentônicos foi bastante diversificada, com um total de 52 e 75 táxons registrados durante o período chuvoso e seco respectivamente. Os Chironomidae foram os mais abundantes e com maior diversidade taxonômica entre os grupos de artrópodes com representantes aquáticos. Houve variação na densidade dos macroinvertebrados bentônicos, com maiores densidades no período de seca. A ocorrência do molusco exótico Melanoides tuberculata foi registrada na maioria das lagoas (15 entre as 18 lagoas estudadas), sendo que em algumas delas as populações já se encontravam dominantes numericamente, como nas lagoas Águas Claras, Aníbal, Baixa Verde, Barra, Dom Helvécio, Jacaré, Ferrugem e Lagoinha. Recomenda-se que, pelo fato das lagoas do Vale do Médio Rio Doce representarem o maior sistema lacustre natural brasileiro, será necessário a curto prazo um grande esforço para impedir a dispersão deste molusco nas demais lagoas do sistema, e a longo prazo sua erradicação, visando restaurar e preservar as comunidades bênticas nativas. / In the present study a comparative limnological characterization of eighteen lakes belonging to the lacustrine system of middle Rio Doce was performed, as well as the analysis of the benthic macroinvertebrate community in relation to the taxonomic composition and population densities. Among the benthic organisms a greater emphasis was devoted to the exotic gastropod Melanoides tuberculata, an exotic species that has invaded many regions in Brazil, and represents a risk to native mollusks and also to other invertebrates in the communities when it becomes established. Samplings were performed in two periods, rainy and dry, and at five localities in each lake, including the littoral and the limnetic region. Physical and chemical variables were measured in lake waters and the granulometric fractions, organic matter content and textural classification were performed for lake sediments. At each site benthic community was sampled with the van Veen grab, and the material was pooled in an integrated sample that was then washed and sieved through a 210 \'mü\'m sieve and the material was preserved in 8% formol solution. The results showed that most lakes are environments with slightly acid and well oxygenated waters, with low concentration of nutrients in the water column, being oligotrophic or mesotrophic systems. The lakes differ regarding depth, and water transparency, and in those with depth greater than 10m a thermal stratification was observed at the time of the sampling performed in the rainy season and isothermy in that on the dry period. The benthic macroinvertebrates community was diversified and totals of 52 and 75 taxa were recorded during rainy and dry period samplings, respectively. Chironomidae members were the most abundant and the taxonomically richest group of aquatic Arthropoda. Changes in the density of benthic macroinvertebrates were observed between the samplings, with highest densities in the dry season. The exotic mollusk Melanoides tuberculata was found in the majority of the lakes (15 among 18 lakes studied) and in some lakes it was numerically dominant, such as in lakes Águas Claras, Aníbal, Baixa Verde, Barra, Dom Helvécio, Jacaré, Ferrugem and Lagoinha. Considering the fact the lakes of middle Rio Doce constitute the larges natural lacustrine system in Brazil, it is recommended that, in short term, a great effort must be done to prevent this mollusk dispersion to other lakes of the system and that at the long run its erradication is required aiming to restore and preserve native benthic communities.

Le changement climatique devrait induire une augmentation des précipitations pendant l'hiver et le printemps dans les régions tempérées et la côte nord de l'Europe. Dans les écosystèmes fluviaux, les précipitations affectent directement le débit des eaux courantes et les rivières subiront des crues plus sévères. En outre, la température de l'air et de l'eau augmenteront à travers le monde. Ces nouvelles conditions environnementales vont avoir des conséquences sur la phénologie des espèces et les interactions prédateurs/proies. Les jeunes truites fario (Salmo trutta L.) commencent leur alimentation exogène en mars/avril. Cette étape critique de leur cycle de vie induit d’importants changements aussi bien physiologiques que comportementaux. Pour permettre un bon développement des individus et un taux de survie élevé, les proies doivent être disponibles et abondantes, en particulier à ce moment de l’ontogénèse où les juvéniles sont vulnérables au manque de nourriture et à la prédation. Des expériences en milieux contrôlés ont été menées pour quantifier la sensibilité à différentes modalités de vitesses de courant de trois espèces d’invertébrés couramment consommées par les salmonidés et pour évaluer l’effet de la température sur le métabolisme d’alevins en situation de jeûne. Des expériences en milieu semi-naturel ont été mises en place pour mieux comprendre les effets d’une crue sur la communauté d’invertébrés et sur la survie, le comportement et la croissance des alevins en première alimentation. Il apparaît que la crue impacte différemment les truites en fonction du moment de la saison auquel elles commencent à s’alimenter (au début ou à la fin du printemps) et de la productivité du système. / Global Climate Change will increase precipitations in the temperate and Northern coast of Europe during winter and spring. In riverine ecosystems, precipitation affects directly the discharge of running waters and, thus, it is predicted that streams will face more severe floods. Additionally, air and water temperature will increase all over the world. These new environmental conditions can alter the phenology of species and predator/prey interactions. Newborns of brown trout (Salmo trutta L.) start their exogenous feeding in March/April. This stage is a critical step as individuals undergo huge physiological and behavioral changes. To allow a good development and a high survival rate, prey has to be abundant, particularly during early ontogenesis when they are most vulnerable to food scarcity and predation. In this thesis, experiments in controlled-environment were conducted to estimate the effect of water velocity on the preferred prey taxa for salmonids and to understand the effect of temperature on the metabolism of alevins facing starvation. Experiments in semi-natural conditions were set up to better understand the effects of floods on invertebrate communities and on survival, behavior and growth of first-feeding alevins. Our data support that floods affect trout differently depending on when they start feeding (early or late spring) and the availability of prey in their environment.

Les cours d’eau de tête de bassin versant, malgré leurs tailles réduites, jouent des rôles importants pour le fonctionnement des milieux situés en aval, et rendent de nombreux services écologiques. Depuis l’émergence du River Continuum Concept, le fonctionnement de ces cours d’eau est considéré comme reposant principalement sur les apports allochtones de matière organique détritique par opposition aux écosystèmes aval de plus grande taille dans lesquels la production primaire autochtone est considérée comme prépondérante. Bien que les détritus soient, par définition, des ressources de moindre qualité pour leurs consommateurs que les végétaux vivants, le rôle des facteurs qui limitent la production biologique et les processus fonctionnels dans ces écosystèmes détritiques reste encore peu exploré. Par exemple la carence en éléments minéraux essentiels (notamment en azote et en phosphore) dans les détritus peut limiter le développement des organismes vivants dans les cours d’eau. De ce fait, la disponibilité en éléments minéraux dans la colonne d’eau, en stimulant la croissance, l’activité des décomposeurs et la qualité élémentaire des ressources par le processus d’immobilisation microbienne, pourrait contrôler pour partie les processus écologiques en jeu dans ces écosystèmes. En étudiant in situ la réponse des communautés microbiennes aux nutriments le long d’un gradient d’occupation des sols, nos travaux ont mis en évidence un effet positif des éléments dissous (N et P) sur la décomposition des litières et les activités enzymatiques des décomposeurs, et ce même pour les niveaux en nutriments les plus élevés du gradient, pour lesquels des effets inverses étaient attendus. Indépendamment, dans des cours d’eau anciennement soumis à de forts dépôts acidifiants, nous avons pu observer une récupération du processus de décomposition des litières. Néanmoins, cette restauration s’accompagnant d’un appauvrissement marqué en N, des perturbations du fonctionnement de ces cours d’eau pourrait se manifester à terme. Le rôle de la production primaire dans les cours d’eau de tête de bassin versant a ensuite été questionné. En effet, bien qu’étant mineur quantitativement, l’apport de carbone de forte qualité pourrait jouer un rôle non négligeable sur le fonctionnement des cours d’eau de tête de bassin versant. En particulier, l’importance et le rôle des apports en acides gras polyinsaturés (AGPI) via les biofilms phototrophes ont été questionnés. En se basant sur un suivi de terrain sur 15 cours d’eau des Vosges le long d’un gradient d’acidification, nos recherches ont tout d’abord pu mettre en évidence la présence de biofilms diatomiques riches en AGPI, malgré le caractère très forestier de ces cours d’eau. Dans un second temps, une expérience en conditions contrôlées a permis d’observer le rôle positif des apports, mêmes faibles, de ressources diatomiques sur la croissance et la survie du crustacé amphipode Gammarus fossarum. Sans cet apport, ces organismes se sont avérés incapables de maintenir leurs niveaux internes d’AGPI, suggérant qu’une consommation de producteurs primaires autochtones était indispensable à ces organismes détritivores. Nos résultats ont ainsi pu mettre en évidence les rôles fondamentaux que peuvent jouer la disponibilité en éléments dissous (N et P) et la qualité du carbone dans les ressources sur la production biologique et sur le processus de décomposition des litières dans les cours d’eau de tête de bassin versant. Ces résultats appellent désormais à investiguer plus profondément les interactions entre ces deux facteurs limitants, et à comprendre dans quels contextes l’un des facteurs pourrait suppléer l’autre. En particulier, il sera intéressant de rechercher comment diverses perturbations anthropiques (xénobiotiques, réchauffement climatique etc…) pourraient affecter l’intensité ou la nature de ces limitations / Despite their reduced sizes, headwater streams play important roles in the functioning of downstream ecosystems and provide numerous ecological services. Since the River Continuum Concept, the functioning of these streams has been considered as mainly relying on allochthonous supplies of detrital organic matter for their functioning, in contrast with downstream ecosystems of larger size where primary production is considered to be predominant. Despite that detritus represent, by definition, a resource of lower quality for its consumers than living plants, the nature of the factors limiting the biological production and functional processes in these detrital ecosystems remains sparsely explored. First, the lack of essential elements (in particular nitrogen and phosphorus) in detritus could be a major constraint for the development of living organisms in streams. As a result, the availability of mineral elements in the water column, by stimulating the growth and activity of decomposers, but also by increasing the elemental quality of resources through microbial immobilization, could control ecological processes in a higher extent than previously believed in these ecosystems. By studying in situ, the response of microorganisms to nutrients availability along a land-use gradient, our results have shown a positive effect of the dissolved elements (N and P) on the decomposition of leaf litters and the enzymatic activities of the decomposers, even for the highest nutrient levels of the gradient, for which adverse effects were expected. Independently, in streams formerly subjected to acidification, we observed a recovery of the process of leaf litter decomposition. Nevertheless, this recovery was accompanied by a marked N reduction in the ecosystem, huge changes in stream functioning might be expected in the medium to long term. The role of autochthonous primary production was then questioned. Indeed, while being quantitatively minor, this contribution of high quality carbon may play a significant role in the functioning of headwater streams. In particular, the importance and role of polyunsaturated fatty acid (PUFA) intakes via phototrophic biofilms was questioned. Based on a field survey of 15 rivers in the Vosges Mountains along an acidification gradient, our results first showed the presence of diatomic biofilms rich in PUFA, despite these streams are clearly in a forested context. In a second step, an experimentation carried out under controlled conditions permitted to observe the positive role of diatomic resources, even in low concentrations, on the growth and survival of the crustacean amphipod Gammarus fossarum. Without this input, these organisms were unable to maintain their internal levels of PUFAs, suggesting that the consumption of autochthonous primary producers might be essential for these detritivore organisms. All our results permit to highlight the fundamental roles that can be played by the availability of dissolved elements (N and P) and the carbon quality of the resources on the biological production and on leaf litter decomposition in headwater streams. These results stress the need for more profound investigation of the interactions between these two limiting factors, and for understanding in which contexts one factor could supplement the other. In particular, it will be interesting to investigate to what extent various anthropogenic disturbances (xenobiotics, global warming, etc...) could affect the intensity or the nature of these limitations

Man-made wetlands are often created to compensate for the loss or degradation of natural wetlands, but little is known about the processes taking place in these artificial environments, especially at the community level. Throughout this thesis, we have assessed the phenomena of primary succession over different time (short-, mid- and long-term) and spatial scales (local, regional, interregional levels), applying different approaches (taxonomic and functional) and subject groups (invertebrates and amphibians). Our main findings regarding time scales show a 3-phase successional pattern in Mediterranean man-made wetlands’ communities, where at the short term (1 year) colonization processes dominate; at mid term perspectives (2 to 7 years) succession signs begin to be conspicuous, and later on (≥ 10 years) parameters such as species richness reach an asymptote. At that moment, some biological strategies dominate, and biodiversity surrogates indicate that communities are indistinct between man-made and natural wetlands. Regarding spatial effects, we corroborated that both local and regional factors affect the establishing communities. Particularly, the low hydrological stability of the Mediterranean region has enhanced biological traits favoring resilience and resistance to disturbances when comparing Mediterranean and cold temperate aquatic communities. Even within the Mediterranean region, low levels of hydrological stability have significant effects on the successional dynamics. In these cases, local communities are highly nested within regional natural ones, and so are not able to make net contributions to regional richness. We also showed the influence of the regional pool of recruiters over local communities, both in the case of invertebrates and amphibians. Especially for the latter group, man-made Mediterranean temporary ponds (MTPs) can play an important role in their conservation. / Les zones humides de nova creació són sovint concebudes per compensar la pèrdua i degradació de les naturals, però el coneixement dels processos que tenen lloc en aquests ambients artificials encara és superficial, especialment a nivell de comunitat. Al llarg d’aquesta tesi, hem analitzat el fenomen de la successió primària a diferents escales temporals (a curt, mitjà i llarg termini) i a diferents escales espacials (a nivell local, regional i interregional), mitjançant diverses aproximacions (taxonòmiques i funcionals) i subjectes (invertebrats i amfibis). Les nostres aportacions pel que fa a les escales temporals mostren un patró de successió basat en 3 fases, on a curt termini (1 any) dominen els processos de colonització; en perspectives de mitjà termini (2 a 7 anys) els signes de successió comencen a ser conspicus, i més tard (≥ 10 anys) paràmetres com la riquesa d’espècies arriben a una asímptota. En aquesta fase avançada, algunes estratègies biològiques dominen, i els índexs de biodiversitat indiquen que les comunitats poden ser indistintes entre les llacunes naturals i les de nova creació. Pel que fa als efectes espacials, hem corroborat que tant factors locals com regionals afecten les comunitats que s’hi estableixen. En particular, la baixa estabilitat hidrològica de la regió Mediterrània ha afavorit trets biològics que proveeixen resiliència i resistència enfront de pertorbacions, sobretot quan es comparen amb les comunitats pròpies del clima temperat fred. Fins i tot dins la mateixa regió Mediterrània, nivells baixos d’estabilitat hidrològica poden tenir efectes importants en la dinàmica de la successió. En aquests casos, les comunitats locals estan altament aniuades en les naturals a nivell regional, i per tant difícilment poden fer contribucions netes a la riquesa regional. També hem mostrat la influència del pool regional de colonitzadors sobre les comunitats locals, tant en el cas dels invertebrats com en el dels amfibis. Especialment per aquest darrer grup, les Basses Temporànies Mediterrànies (BTMs) de nova creació poden jugar un paper important per a la seva conservació.

This doctoral dissertation was produced in a cooperation between Halmstad University (Wetland Research Centre, School of Business and Engineering) and Lund University (Limnology &amp; Marine Biology, Department of Ecology). Abstract . Wetland creation at large, regional scales is implemented as a measure to abate the biodiversity loss in agricultural landscapes and the eutrophication of watersheds and coastal areas by non-point source nutrient pollution (mainly nitrogen). The consequences of creating many new wetlands for biodiversity conservation and nutrient reten- tion (ecosystem functioning) in agricultural landscapes are still relatively unknown, both on local (per wetland) and regional (per landscape) scales. In Sweden, wetland creation has progressed already since the 1990s, and by now larger numbers of created wetlands are present, mainly in the intensively farmed landscapes of southwestern Sweden. This thesis aimed to investigate the following aspects in these systems: (i) their large-scale effects on biodiversity, (ii) their functional diversity of bacterial denitrifiers, (iii) the abiotic and biotic influences on wetland ecosystem functioning, (iv) the potential for biodiversity-function links, and (v) the potential for functional links and joint functioning.(i) Created wetlands hosted diverse assemblages of macroinvertebrates and plants. They maintained a similar com- position and diversity as natural ponds in agricultural landscapes. The environmental conditions per wetland did hardly affect macroinvertebrate and plant assemblages, and the prerequisites for nutrient retention did neither. In landscapes were wetland creation efforts had increased the total density of small water bodies by more than 30%, macroinver- tebrate diversity of created wetlands was facilitated on both local and regional scales. (ii) Diverse communities of denitrifying bacteria with the capacity for conducting different denitrification steps (functional types) were present in all investigated wetlands. The richness of denitrifying bacteria communities was affected by nitrate concentration and hydraulic loading rate, which may potentially be relevant for the nitrogen retention function of created wetlands. The diversity across different functional types of bacterial denitrifiers increased with nitrate concentration. (iii) Both abiotic and biotic factors influenced ecosystem functions of created wetlands. Variation in nitrogen retention was associated to nitrate load, but even to vegetation parameters. In wetlands with constant nitrate load, planted emergent vegetation facilitated nitrogen retention compared to other vegetation types. In wetlands with variable loads, nitrogen retention was facilitated if nitrate load was high and many different vegetation types were present; nitrogen load could explain the majority of the variation in nitrogen retention compared to vegetation parameters. Phosporus retention of created wetlands was best explained by vegetation parameters. Litter decomposition was inhibited at high nitrate to phosphorus ratios. Methane production increased with age and decreased with plant cover. (iv) Biodiversity may facilitate wetland ecosystem functions, particularly in dynamic wetland ecosystems. Nitrogen retention increased with vegetation type diversity, phosphorus retention capacity with plant richness, and litter decomposition with macroinvertebrate diversity. (v) Created wetlands have the capacity of sustaining several parallel ecosystem services. Some wetland functions were coupled; nitrogen retention increased with fast litter decomposition. On the other hand, methane emission and nitro- gen retention were independent of each other, as were nitrogen and phosphorus retention.In conclusion, created wetlands have the potential to at least partly abate the lost biodiversity and multifunctionality caused by the past extensive destruction of natural wetlands in agricultural landscapes. / <p>[Paper II] Milenkovski S., Thiere G., Weisner S.E.B., Berglund O. &amp; Lindgren P.-E. Variation of eubacterial and denitrifying bacterial biofilm communities among constructed wetlands. Submitted manuscript. [Paper V] Thiere G. &amp; Weisner S.E.B. Influence of biotic and abiotic parameters on ecosystem functioning of created wetlands. Manuscript.</p>

Thèse numérisée par la Division de la gestion de documents et des archives de l'Université de Montréal

A multi-integrative approach was used to identify spatial and temporal relationships of natural and anthropogenic environmental variables affecting riverine ecosystem structure and function in the Athabasca Oil Sands Region (AOSR). A series of inter-related field studies were conducted to assess three key components of the freshwater food web (physico-chemical environment, basal productivity, benthic macroinvertebrates) utilizing an a priori environmental disturbance gradient experimental design. The gradient design was formulated to best discriminate the possible effects of natural and anthropogenic environmental variables on two river basins (Steepbank and Ells Rivers) each having different levels of oil sands (OS) land use disturbance. Findings from this study showed that natural variation explained most longitudinal and seasonal responses of physico-chemical environmental variables for both rivers, including possible mechanisms such as physical and chemical effects from the OS geological deposit and inputs from shallow groundwater upwelling. Basal productivity was likely controlled by natural variables within the Steepbank and Ells Rivers, such as potential OS deposit effects, nutrient availability and influences from turbidity and physical factors, with disturbance from OS development either negligible or not detected. Longitudinal and seasonal differences in benthic macroinvertebrate community composition were mostly related to natural variation, including possible mechanisms such as high discharge and sediment slump events on the Steepbank River, and community shifts from elevated metal concentrations from natural sources at upstream sites on the Ells River. This study demonstrated that developing baseline information on watersheds can be essential at discriminating sources of disturbance, with natural variation potentially confounding with anthropogenic factors. This study also highlights the need for further research to obtain an improved understanding of mechanistic pathways to better determine natural and anthropogenic non-point source disturbances and cumulative effects on the structure and function of tributary ecosystems in the AOSR at relevant spatial and temporal scales. / Graduate / 0329 / clsuzann@uvic.ca

Made available in DSpace on 2016-06-02T19:32:09Z (GMT). No. of bitstreams: 1 5884.pdf: 1894395 bytes, checksum: 2133839c319e8789b185c3b67f243db9 (MD5) Previous issue date: 2014-06-10 / Financiadora de Estudos e Projetos / The analyses of the relative condition factor in fish community and of the benthic macroinvertebrates communities structure were used as a tool for assessing the influence of disturbances and water quality in the tropical streams of the upper portion of Monjolinho River basin, São Carlos, SP, Brazil. The condition factor revealed different responses of the fish species regarding the organic pollution effect. Astyanax cf paranae was found to be a sensitive species, Phalloceros harpagos to be tolerant, and Poecilia reticulate to be resistant. The analysis of the benthic macroinvertebrate community structure showed that these populations are affected by the loss of environmental quality, resulting in great differences in species diversity, with the absence of groups considered sensitive to pollution and dominance of resistant groups. In this portion of the Monjolinho River basin it was possible to identify streams with high environmental integrity as the Espraiado stream, up to strongly polluted streams as the Belvedere stream. / O fator de condição relativo em peixes e a análise da estrutura da comunidade de macroinvertebrados bentônicos foram utilizados como ferramenta de avaliação de distúrbios nos córregos afluentes da porção superior da bacia do rio Monjolinho, São Carlos, SP, Brasil. O uso do fator condição relativo dos peixes evidenciou diferentes respostas desses organismos à poluição orgânica, tendo a espécie Astyanax cf paranae sido sensível; a espécie Phalloceros harpagos, tolerante e a espécie Poecilia reticulata, resistente. Já a análise da estrutura da comunidade de macroinvertebrados bentônicos evidenciou que essas populações são afetadas pela perda da qualidade ambiental, resultando, em geral, menor diversidade e ausência de grupos considerados sensíveis à poluição e dominância de grupos resistentes. Nessa porção da bacia do Rio Monjolinho foram identificados desde córregos com alta integridade ambiental, como o córrego do Espraiado, até córregos fortemente poluídos, como o Belvedere.

Os macroinvertebrados bentônicos são importantes componentes nos ecossistemas aquáticos devido à sua participação no fluxo de energia e na ciclagem de nutrientes, recebendo gradativamente maior atenção nos estudos ecológicos nas últimas décadas. O presente estudo visa uma caracterização limnológica comparativa de quatro lagoas do sistema de lagos do Vale do Rio Doce, MG (lagoas Águas Claras, Almécega, Verde e Carioca), e o estudo dos macroinvertebrados bentônicos, com ênfase na composição taxonômica, distribuição espaçotemporal e diversidade, além de uma avaliação de possíveis relações com a ocorrência de espécies exóticas neste sistema. As lagoas encontram-se na depressão interplanáltica do Vale do Rio Doce, formada por uma rica rede de drenagem, circundada por remanescentes de Mata Atlântica (19 'GRAUS' 45’ 25,7” e 19 'GRAUS' 53’ 11,6” S; 42 'GRAUS' 37’ 35,6” e 42 'GRAUS' 35’ 11,3” W). Amostragens para análises físicas, químicas e biológicas foram realizadas em setembro e dezembro de 2002 e março e junho de 2003. As amostragens de sedimento para análises de composição granulométrica e da comunidade de macroinvertebrados bentônicos foram realizadas com draga do tipo Van Veen (337 'CM POT.2'), em um total de 77 estações de coleta e em quatro períodos de amostragem. Foram identificados 56 táxons, sendo 2 pertencentes ao Filo Mollusca, 13 à Classe Oligochaeta, 1 à Classe Hirudinae, 1 ao Filo Nematoda e 41 à Classe Insecta. Desses últimos, 27 pertencem à família Chironomidae. A maior riqueza de táxons foi registrada na lagoa Carioca (43 táxons) e a menor na lagoa Águas Claras (27 táxons). Melanoides tuberculata, um molusco invasor, foi o táxon numericamente dominante nas lagoas Águas Claras e Almécega. Na lagoa Verde esse molusco ocorreu em densidade média 5 vezes menor do que nas lagoas anteriormente citadas onde suas populações já se encontram bem estabelecidas. Na lagoa Carioca não há ocorrência desse molusco, e nesta lagoa foi registrada a maior riqueza de táxons entre as lagoas estudadas, sendo os Chironomidae os macroinvertebrados bentônicos mais representativos. Sazonalmente ocorreram diferenças na densidade das populações. Existem também diferenças quanto à composição taxonômica da comunidade bentônica entre as regiões litorânea e limnética, evidenciando a compartimentalização do sistema. Os sedimentos das lagoas Águas Claras, Almécega e Verde tem baixo conteúdo de matéria orgânica, sendo do tipo mineral e arenoso, enquanto o da lagoa Carioca é do tipo barrento e orgânico. Em relação às variáveis limnológicas, o pH é ligeiramente ácido e as águas bem oxigenadas. As concentrações de nutrientes na coluna d’água são relativamente baixas podendo as lagoas Águas Claras, Almécega e Verde serem consideradas oligotróficas e a lagoa Carioca meso-oligotrófica. / Benthic macroinvertebrates are important components of aquatic ecosystems due to their role in the energy flow and material cycling. They have gradually received more attention in ecological studies in the last decades. The present study aimed a comparative limnological characterization of four lakes belonging to the middle Rio Doce Valley lacustrine system, MG (Águas Claras, Almécega, Verde and Carioca lakes), and the study of its benthic macroinvertebrate communities with emphasis on the taxonomical composition, spatial and temporal distribution and diversity, besides an evaluation of possible relationships with the occurrence of exotic species in the system. The lakes are located in the interplanaltic depression of Rio Doce Valley, an extense drainage web surrounded by Atlantic Forest remnants (19 'DEGREES' 45’ 25,7” and 19 'DEGREES' 53’ 11,6” South; 42 'DEGREES' 37’ 35,6” and 42 'DEGREES' 35’ 11,3” West). Samplings for physical, chemical and biological analyses were carried out in September and December 2002 and in March and June 2003. Sediment sampling for granulometric determinations and for benthic community analyses were performed with a Van Veen (337 'CM POT.2') dredge. Considering the four lakes and the sampling seasons, 77 stations were sampled. A total of 56 taxa were identified, 2 belonging to the Mollusca, Gastropoda; 13 to Oligochaeta and 1 to the Hirudinae, Annelida; 1 to Nematoda and 41 Insecta, Arthropoda. Among the Insecta 27 taxa belonged to the family Chironomidae. The highest richness of taxa was recorded in lake Carioca (43 taxa) and the lowest in lake Águas Claras (27 taxa). Melanoides tuberculata, an invader molusc was the numerically dominant taxon in Águas Claras and Almécega lakes. In lake Verde this species ocurred in densities 5 times lower than in those lakes where its populations are already well established. This mollusc does not occur in lake Carioca. This was among the lakes studied, the one where the highjest richness of taxa was recorded and Chironomidae were the most representative benthic macroinvertebrates. There were seasonal changes in the population densities. There are also diferences regarding the taxonomic composition of the benthic community among the littoral and the limnetic regions evidencing the system compartimentalization. The sediments of lake Águas Claras, Almécega and Verde have low organic matter content in the littoral region, being classified as mineral and sandy, whereas the sediment of lake Carioca is loamy and organic. Regarding the general limnological conditions the results indicate that lake waters are slightly acidic and well oxygenated. Nutrient concentrations in the water column are relatively low. The lakes Águas Claras, Almécega and Verde can be classified as oligotrophic and lake Carioca as meso-oligotrophic.