Department of Marine Biology, Texas A&M University, 5007 Avenue U, Galveston, TX 77551, USA.
J Fish Biol. 2009 Nov;75(7):1719-32. doi: 10.1111/j.1095-8649.2009.02424.x.
Stable isotope ratios of carbon (delta13C) and nitrogen (delta15N) were used to investigate feeding patterns of larval and early juvenile pelagic fishes in slope waters of the Gulf of Mexico. Contribution of organic matter supplied to fishes and trophic position within this pelagic food web was estimated in 2007 and 2008 by comparing dietary signatures of the two main producers in this ecosystem: phytoplankton [based on particulate organic matter (POM)] and Sargassum spp. Stable isotope ratios of POM and pelagic Sargassum spp. were significantly different from one another with delta13C values of POM depleted by 3-6 per thousand and delta15N values enriched by 2 relative to Sargassum spp. Stable isotope ratios were significantly different among the five pelagic fishes examined: blue marlin Makaira nigricans, dolphinfish Coryphaena hippurus, pompano dolphinfish Coryphaena equiselis, sailfish Istiophorus platypterus and swordfish Xiphias gladius. Mean delta13C values ranged almost 2 among fishes and were most depleted in I. platypterus. In addition, mean delta15N values ranged 4-5 with highest mean values found for both C. hippurus and C. equiselis and the lowest mean value for M. nigricans during both years. Increasing delta13C or delta15N with standard length suggested that shifts in trophic position and diet occurred during early life for several species examined. Results of a two-source mixing model suggest approximately an equal contribution of organic matter by both sources (POM=55%; pelagic Sargassum spp.=45%) to the early life stages of pelagic fishes examined. Contribution of organic matter, however, varied among species, and sensitivity analyses indicated that organic source estimates changed from 2 to 13% for a delta(13)C fractionation change of +/-0.25 per thousand or a delta15N fractionation change of +/-1.0 per thousand relative to original fractionation values.
稳定同位素碳(δ13C)和氮(δ15N)比值被用于研究墨西哥湾斜坡水域中浮游幼鱼和早期幼鱼的摄食模式。通过比较生态系统中两种主要生产者(基于颗粒有机物质(POM)的浮游植物和马尾藻属)的饮食特征,估计了 2007 年和 2008 年向鱼类提供的有机物的贡献及其在该浮游食物网中的营养位置。POM 和浮游马尾藻属的稳定同位素比值彼此之间有显著差异,POM 的 δ13C 值比马尾藻属低 3-6‰,而 δ15N 值则比马尾藻属高 2‰。在所研究的五种浮游鱼类中,稳定同位素比值存在显著差异:黑马林鱼、鲯鳅、黄鳍金枪鱼、旗鱼和剑鱼。鱼类的平均 δ13C 值相差近 2,其中 I. platypterus 的值最低。此外,平均 δ15N 值相差 4-5,C. hippurus 和 C. equiselis 的平均 δ15N 值最高,M. nigricans 的平均 δ15N 值最低,这两年均如此。随着标准长度的增加,δ13C 或 δ15N 的增加表明,在几种研究物种的早期生活中,营养位置和饮食发生了变化。双源混合模型的结果表明,两种来源(POM=55%;浮游马尾藻属=45%)对所研究的浮游鱼类早期生活阶段的有机物贡献大致相等。然而,有机物的贡献因物种而异,敏感性分析表明,对于 ±0.25‰的 δ13C 分馏变化或相对于原始分馏值的 ±1.0‰的 δ15N 分馏变化,有机源估计值从 2%变化到 13%。