Assembléias zooplanctônicas (Cladocera, Copepoda e Rotifera) e condiçoes limnolócas no gradiente longitudinal barragem-jusante do reservatório de Itaipu, rio Paraná (Brasil, Paraguai e Argentina)

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Efeitos dos pulsos de vazão dos reservatórios do baixo rio Paranapanema (SP/PR) sobre os sistemas de jusante - variáveis físicas, químicas e assembléias zooplanctônicas (Cladocera e Copepoda)

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Análise temporal da composição, abundância, diversidade dos Cladocera e crescimento alométrico da Daphnia spp. O. F. Müeller, 1785 na Lagoa do Camargo, lateral ao Rio Paranapanena em sua zona de desembocadura na Represa do Jurumirim

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Distribuição espaço-temporal de Cladocera(Crustácea, Branchiopoda) em uma lagoa subtropical lateral ao Rio Paranapanema(zona de desmbocadura na Represa de Jurumirim/SP)

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Diversidade da Cladocera (Crustacea, Anomopoda e Ctenopoda) em reservatórios e trechos lóticos da bacia do Rio Prata (Brasil, Paraguai, Argentina e Uruguai)

Pós-graduação em Ciências Biológicas (Zoologia) - IBB

ECOTOXICITY AND ENVIRONMENTAL RISK ASSESSMENT OF LARVICIDES USED IN THE CONTROL OF Aedes aegypti TO Daphnia magna ( CRUSTACEA, CLADOCERA)

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Efeitos do deplecionamento induzido do reservatório de Salto Grande, Rio Paranapanema(SP/PR) sobre as assembléias de microcrustáceos (Cladocera e Copepoda) de duas lagoas marginais

No reservatório de Salto Grande (22º53’53’’S / 49º59’33’’W), Rio Paranapanema (SP/PR), é realizado um tipo de manejo (redução do nível de água) para redução da biomassa da macrófita submersa Egeria densa desde 2004. Estas plantas causam perdas econômicas para o programa de geração elétrica e infortúnio para a população local. O reservatório de Salto Grande possui lagoas marginais que apresentam elevada densidade dessas macrófitas e são tidas como ambientes de alta importância para o desenvolvimento, alimentação e reprodução de muitas assembléias, principalmente as de microcrustáceos zooplanctônicos. O objetivo deste trabalho foi analisar as mudanças na estrutura (composição, riqueza, abundância e diversidade) das assembléias de microcrustáceos zooplanctônicos (Cladocera e Copepoda) e suas relações com as alterações nas condições limnológicas decorrentes da variação de nível em duas lagoas marginais (Pedra Branca e Guaritá) em função do deplecionamento. Foram realizadas amostragens mensais de abril/2005 a julho/2006, além de coletas nictemerais durante o processo de deplecionamento (agosto/05) e um mês após o mesmo. Para a análise do zooplâncton foram amostrados 150 litros de água superficial em cada lagoa (região limnética). Simultaneamente, foram medidas as variáveis físicas e químicas da água: temperatura, pH, oxigênio dissolvido, condutividade elétrica, transparência, turbidez, material em suspensão (total, frações orgânica e inorgânica) e concentração de clorofila a. As variáveis limnológicas demonstraram um padrão de variação sazonal, além da influência do deplecionamento, principalmente sobre a temperatura e oxigênio dissolvido. O valor de riqueza encontrado para Cladocera foi elevado, totalizando 49 táxons. Os Copepoda foram analisados apenas até o nível de Ordem... (Resumo completo, clicar acesso eletrônico abaixo)

Life history and DNA barcode of Oxyurella longicaudis (Birgei, 1910) (Cladocera, Anomopoda, Chydoridae)

Background: Cladocera is an important group of freshwater zooplankton, and the species plays an important role in energy transfer and in aquatic food webs. Oxyurella longicaudis is a Chydoridae species that has been recorded in North and South America. The aim of this study is to investigate the life cycle aspects of parthenogenetic females of O. longicaudis cultured in laboratory under controlled conditions: temperature (23 degrees C +/- 05 degrees C), photoperiod (12 h light/12 h dark), food supply, and reconstituted water.Results: Embryonic development duration (2.3 +/- 0.5 days), post-embryonic development (5.2 +/- 0.69 days), mean fecundity (two eggs female(-1) brood(-1)), total egg production (22.55 +/- 3.98 eggs), average longevity (58 days), and body growth of the species were recorded. We also report the first DNA barcode for O. longicaudis isolated in Brazil, which will allow for easy identification in future zooplankton community studies. The analysis shows a genetic divergence of around 7% between our Brazilian isolate and O. longicaudis isolates from Mexico.Conclusions: The time of embryonic and post-embryonic development of O. longicaudis was higher than that of the other species of the same family, which contributed to lower total egg production throughout its life cycle. The genetic divergence appears to be sufficient to classify the two isolates as different species.

Growth and development time of subtropical Cladocera Diaphanosoma birgei Korinek, 1981 fed with different microalgal diets

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Contribuição dos ovos de resistência de Cladocera (Crustacea: Branchiopoda) para a recolonização de ambientes lacustres temporários

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Seasonal contrasts in abundance and reproductive parameters of Penilia avirostris (Cladocera, Ctenopoda) in a coastal subtropical area

We studied the population dynamics and the reproductive biology of Penilia avirostris during three consecutive years on the inner shelf off Ubatuba, Brazil. Penilia avirostris individuals and its eggs and embryos were counted, measured, and classified into stages. The species occurred throughout the studied period, in a wide temperature range (14.8-28.2A degrees C). Cladoceran densities were usually higher (> 2,000 ind m(-3)) in warm seasons, when the water column was stratified as a consequence of bottom intrusions of the cold- and nutrient-rich South Atlantic Central Water. Juveniles, non-reproducing females, and parthenogenic females were the dominant developmental stages. Males and gamogenic females were rare and only occurred when females reached peak abundances. This suggests that in tropical and subtropical coastal seas gamogenesis in P. avirostris is not as common as in temperate seas, but may play a significant role in the density-dependent control of the population preceding unfavourable periods.

Life cycle and reproductive traits of marine podonids (Cladocera, Onychopoda) in a coastal subtropical area

We studied the temporal distribution and reproductive biology of marine podonids during two consecutive years off Ubatuba, southeast coast of Brazil. Podonid specimens and their eggs and embryos were counted, measured and classified into categories. Pseudevadne tergestina was the most abundant species, and was more abundant in surface layers, in warm seasons, when the water column was stratified because of bottom intrusions of the cold and nutrient-rich South Atlantic Central Water (SACW) onto the inner shelf. Evadne spinifera had a similar temporal and vertical distribution, but with lower abundance and frequency. Pleopis schmackeri did not show a clear seasonal distribution, but preferred bottom layers. Pleopis polyphemoides and Podon intermedius occurred in low abundances, and only under SACW influence. Parthenogenetic females were dominant among all podonid species. Gamogenetic females of P. polyphemoides and P. intermedius were observed, but males of neither species occurred. This suggests that in tropical and subtropical regions, P. tergestina, E. spinifera and P. schmackeri reproduce through parthenogenesis during most of the year.

Response of subfossil Cladocera in Gerzensee (Swiss Plateau) to early Late Glacial environmental change

Sub-fossil Cladocera were studied in a core from Gerzensee (Swiss Plateau) for the late-glacial periods of Oldest Dryas, Bølling, and Allerød. Cladocera assemblages were dominated by cold-tolerant littoral taxa Chydorus sphaericus, Acroperus harpae, Alonella nana, Alona affinis, and Alonella excisa. The rapid warming at the beginning of the Bølling (GI-1e) ca. 14,650 yr before present (BP: before AD 1950) was indicated by an abrupt 2‰ shift in carbonate δ18O and a clear change in pollen assemblages. Cladocera assemblages, in contrast, changed more gradually. C. sphaericus and A. harpae are the most cold-tolerant, and their abundance was highest in the earliest part of the record. Only 150–200 years after the beginning of the Bølling warming we observed an increase in less cold-tolerant A. excisa and A. affinis. The establishment of Alona guttata, A. guttata var. tuberculata, and Pleuroxus unicatus was delayed by ca. 350, 770, and 800 years respectively after the onset of the Bølling. The development of the Cladocera assemblages suggests increasing water temperatures during the Bølling/Allerød, which agrees with the interpretation by von Grafenstein et al. (2013-this issue) that decreasing δ18O values in carbonates in this period reflect increasing summer water temperatures at the sediment–water interface. Other processes also affected the Cladocera community, including the development and diversification of aquatic vegetation favourable for Cladocera. The record is clearly dominated by Chydoridae, as expected for a littoral core. Yet, the planktonic Eubosmina-group occurred throughout the core, with the exception of a period at ca. 13,760–13,420 yr BP. Lake levels reconstructed for this period are relatively low, indicating that the littoral location might have become too shallow for Eubosmina in that period.

Modern diatom, cladocera, chironomid, and chrysophyte cyst assemblages as quantitative indicators for the reconstruction of past environmental conditions in the Alps. II. Nutrients

Surface sediments from 68 small lakes in the Alps and 9 well-dated sediment core samples that cover a gradient of total phosphorus (TP) concentrations of 6 to 520 μg TP l-1 were studied for diatom, chrysophyte cyst, cladocera, and chironomid assemblages. Inference models for mean circulation log10 TP were developed for diatoms, chironomids, and benthic cladocera using weighted-averaging partial least squares. After screening for outliers, the final transfer functions have coefficients of determination (r2, as assessed by cross-validation, of 0.79 (diatoms), 0.68 (chironomids), and 0.49 (benthic cladocera). Planktonic cladocera and chrysophytes show very weak relationships to TP and no TP inference models were developed for these biota. Diatoms showed the best relationship with TP, whereas the other biota all have large secondary gradients, suggesting that variables other than TP have a strong influence on their composition and abundance. Comparison with other diatom – TP inference models shows that our model has high predictive power and a low root mean squared error of prediction, as assessed by cross-validation.