1986
DOI: 10.2307/1310304
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Stable Carbon Isotopes and Carbon Flow in Ecosystems

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Cited by 261 publications
(177 citation statements)
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References 33 publications
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“…This range was similar to that observed for C 3 plants that make up the base of the food web in inland environments (Smith and Epstein 1971;Rounick and Winterbourn 1986). Other studies have documented similar ranges in δ 13 C for wetland biota from inland environments of South Carolina and Georgia.…”
Section: Inland Isotopic Signaturessupporting
confidence: 84%
“…This range was similar to that observed for C 3 plants that make up the base of the food web in inland environments (Smith and Epstein 1971;Rounick and Winterbourn 1986). Other studies have documented similar ranges in δ 13 C for wetland biota from inland environments of South Carolina and Georgia.…”
Section: Inland Isotopic Signaturessupporting
confidence: 84%
“…Deciduous tree leaves were also relatively depleted in d 13 C, and increased use of this food source could have reduced d 13 C levels in consumers following the fire. However, this explanation would contradict the findings of other studies which report reduced use of allochthonous food sources following canopy removal (Hansmann and Phinney, 1973;Rounick and Winterbourn, 1986).…”
Section: Long-term Biotic Impacts Via Stable Isotope Analysiscontrasting
confidence: 66%
“…For example, several studies report a similar reduction in d 13 C in a variety of consumer organisms following experimental logging and burning of small catchments in New Zealand and attribute the isotopic shift to increased use of autochthonous energy sources following canopy removal (Rounick et al, 1982;Rounick and Hicks, 1985;Rounick and Winterbourn, 1986). Similarly, Winterbourn et al (1986) reported that macroinvertebrates from open-canopied stream sites in UK were more depleted in 13 C than consumers from closed-canopied forested sites.…”
Section: Long-term Biotic Impacts Via Stable Isotope Analysismentioning
confidence: 92%
“…Desde esta perspectiva, se han utilizado los isótopos estables con éxito en la descripción de un amplio abanico de tipos de ecosistemas acuáticos, tales como estuarios (Peterson et al, 1985;Cifuentes et al, 1988;Mulholland & Olsen, 1992;Caraco et al, 1998;Melville & Connolly, 2003), ríos (Rounick & Winterbourn, 1986;Rosenfeld & Roff, 1992;Junger & Planas, 1994;Hershey et al, 1997;Fisher et al, 2001), lagos (Keough et al, 1996;Bernasconi et al, 1997;Yoshii et al, 1999;, France, 1999;Grey et al, 2000;Herwig et al, 2004), marismas (Haines, 1976;Carman & Fry, 2002), mares y oceános (Minagawa & Wada 1984;VanDover et al, 1992;Hansson et al,1997).…”
Section: Características Generales De Los Sistemas Acuáticos Reveladaunclassified
“…Los isótopos de carbono han sido empleados para evaluar la contribución de las entradas de materia orgánica terrestre a los sistemas acuáticos continentales (Rounick & Winterbourn, 1986;Rosenfeld & Roff, 1992) y marinos (Fry & Sherr, 1984). La utilización de δ 13 C, facilita la posibilidad de detectar el origen de los recursos basales, y si además se combina con la medición de δ 15 N, se puede obtener un valor integrado de la dieta de los consumidores en el tiempo y facilitar la obtención de datos para estimar la producción secundaria de los ríos.…”
Section: Aplicacionesunclassified