Abundância natural do isótopo estável de carbono (13C) de alguns itens alimentares e sua contribuição no crescimento de juvenis de pintado, Pseudoplatystoma corruscans (Agassiz, 1829) (Osteichthyes, Pimelodidae)

• Autor(a) principal: Barriviera Furuya, Valéria Rossetto
• Data de Publicação: 2002
• Outros Autores: Hayashi, Carmino, Massamitu Furuya, Wilson, Ducatti, Carlos [UNESP]
• Tipo de documento: Artigo
• Idioma: por
• Título da fonte: Repositório Institucional da UNESP
• Texto Completo: http://dx.doi.org/10.4025/actascibiolsci.v24i0.2384; http://hdl.handle.net/11449/67098
• topic: 13C; Feeding; Pintado; Pseudoplatystoma corruscans; Stable isotope; carbon; stable isotope; analysis; copepod; experimentation; feeding; fish; food chain; food composition; morphometrics; nonhuman; phytoplankton; pond; pseudoplatystoma corruscans; stomach content; water sampling; zooplankton; Chironomidae; Cladocera; Copepoda; Osteichthyes; Pimelodidae; Pisces; Pseudoplatystoma; Vertebrata

The aim of this study is to determine the natural abundance of carbon stable isotope (13C) of some food components and determine its contribution to the pintado juvenile growth, in laboratory conditions. 150 fishes were used with average weight of 1.39 g, and stocked in two net ponds with 125L each, during 60 days. Every 10 days a water sample was collected to analyse phytoplakton and zooplankton. Clacocera was dominant in the analysis of the stomach contents, following Chironomidae and Copepoda. A fish sample was collected in the beginning, and at the end of the experiment to analyses the isotopic signal. An average value of -20.94; -15.36 and -18.81 δ13C%o was obtained for phytoplankton, Cladocera and Chironomidae, respectively. Cladocera was the main carbon source and contribution with carbon average 89.24% in feeding this species, while the Chironomid contribution was 10.76%. The δ13C was effective as carbon tracer in food chain, because the consumer reflects its diet isotopicly.