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Concordance among zooplankton groups in a near-pristine floodplain system
Institution:1. Faculdade UnB Planaltina, Universidade de Brasília, Área Universitária n. 1 – Vila Nossa Senhora de Fátima, CEP 73340-710 Planaltina, Distrito Federal, Brazil;2. Departamento de Botânica, Universidade Federal do Paraná, Av. Cel. Francisco H. dos Santos, SCB, P.O. Box 19031, CEP 81531-990 Curitiba, Paraná, Brazil;3. Núcleo de Pesquisas em Limnologia, Ictiologia e Aqüicultura (NUPELIA), Universidade Estadual de Maringá, Av. Colombo, 5.790, CEP 87020-900 Maringá, Paraná, Brazil;4. Departamento de Ecologia, Universidade Federal de Goiás, Rod. Goiânia-Nerópolis, Km 5, P.O. Box 131, CEP 74001-970 Goiânia, Goiás, Brazil;1. Câmpus Henrique Santillo, Universidade Estadual de Goiás, 75.132-903 Anápolis, GO, Brazil;2. Universidade Paulista (UNIP), 74.845-090 Goiânia, GO, Brazil;3. Escola Superior Associada de Goiânia (ESUP), 74.840-090 Goiânia, GO, Brazil;4. Instituto de Física, Universidade Federal de Goiás, 74.690-900 Goiânia, GO, Brazil;5. Departamento de Física, Universidade Federal da Paraíba, 58.051-970 João Pessoa, PB, Brazil;1. Museu Paraense Emílio Goeldi, Campus de Pesquisa, Coordenação de Ciências da Terra e Ecologia, Av. Perimetral, Cx. postal 399, 1901, 66077-530 Belém, PA, Brazil;2. Departamento de Paleontologia e Estratigrafia, UFRGS, Cx. postal 15001, 91501-970 Porto Alegre, RS, Brazil;3. Micropalaeontology Unit, Department of Geology, University of Wales, Aberystwyth, SY23 3DB, United Kingdom;1. Laboratory of Marine Biology, Graduate School of Fisheries Science, Hokkaido University, 3-1-1 Minato-cho, Hakodate, Hokkaido, 041-8611, Japan;2. Shiretoko Foundation, 531 Iwaubetsu, Onnebetsu, Shari, Hokkaido, 099-4356, Japan;1. Graduate Faculty of Environment, University of Tehran, P.O. Box 14155-6135, Tehran, Iran;2. Environmental Research Laboratory, Department of Water and Environmental Engineering, School of Civil Engineering, Iran University of Science and Technology, P.O. Box 16765-163, Narmak, Tehran, Iran
Abstract:The search for biological surrogate groups has been an active and contentious area of research. A surrogate group is defined as one that allows researchers to detect a known spatial and temporal environmental gradient and to represent the responses of other biological groups to those gradients. Using spatiotemporal zooplankton data from a near-pristine floodplain (the Araguaia River floodplain in Central Brazil), we first assessed the capacity of four zooplankton assemblages (Cladocera, Copepoda, Rotifera and Protozoa) to depict the effects of flooding. Second, we evaluated whether, during each hydrological period, ordination patterns derived from an assemblage matched those patterns shown by a second assemblage and by the environmental dataset. All four assemblages satisfactorily detected the environmental differences caused by the flood event. Most pairs of assemblages were significantly concordant. Additionally, the ordination patterns generated by these assemblages matched those generated by the environmental data. These results suggest that the patterns of concordance were mediated by similar responses to environmental gradients. However, the strengths of concordance between the assemblages, albeit significant, were low. Our results suggest the potential for use of the surrogacy approach in monitoring hydrological changes. However, due to the low strengths of concordance, the biodiversity pattern revealed by a specific assemblage is unlikely to be a good predictor of another. We also highlighted that conducting a formal meta-analysis on strengths of concordance between assemblages would be a promising avenue for further research.
Keywords:Flooding  Biomonitoring  Biological surrogates  Concordance  Araguaia River
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