2006
DOI: 10.1007/0-387-33745-8
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Stable Isotope Ecology

Abstract: except for brief excerpts in connection with reviews or scholarly analysis. Use in connection with any form of information storage and retrieval, electronic adaptation, computer software, or by similar or dissimilar methodology now known or hereafter developed is forbidden. The use in this publication of trade names, trademarks, service marks, and similar terms, even if they are not identified as such, is not to be taken as an expression of opinion as to whether springer.com

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Cited by 1,886 publications
(1,777 citation statements)
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“…Rstandard where R is the 15N/14N or 13C/ 12 e. The reference materials used were secondary standards (meal) of known relation to the international standards, PeeDee Belemnite for carbon and atmospheric nitrogen for nitrogen (Fry, 2006).…”
Section: Isotope and Elementary Analysismentioning
confidence: 99%
See 1 more Smart Citation
“…Rstandard where R is the 15N/14N or 13C/ 12 e. The reference materials used were secondary standards (meal) of known relation to the international standards, PeeDee Belemnite for carbon and atmospheric nitrogen for nitrogen (Fry, 2006).…”
Section: Isotope and Elementary Analysismentioning
confidence: 99%
“…Source 1 = terrestrial plants, source 2 = phytoplankton of Lake Constance. In this model, the fraction of allochthonous and authocthonous POMsed was calculated according to the formula (Fry, 2006 For this approach, it was assumed that differences observed between signatures of POMsed were exclusively due to supply of allochthonous organic carbon at the sampling sites.…”
Section: Mixing Modelmentioning
confidence: 99%
“…Pelagic phytoplankton are surrounded by excess CO2 and therefore can discriminate against the slightly heavier stable C isotope ( 13 C) unlike benthic algae that grow on the lake bottom where boundary layers induce more C limitation . Consequently, the pelagic (phytoplankton) and littoral (benthic algae) primary producers usually have distinct stable C isotope ratios ( 13 C: 12 C, denoted as Dž 13 C; see Fry 2006), which are further reflected to higher consumers, including the pelagic zooplankton and planktivorous fish and the littoral benthic macroinvertebrates and benthivorous fish ( Fig. 1 and 2).…”
Section: Food Webs In Lakesmentioning
confidence: 99%
“…We extended the study of by analysing stable carbon (d 13 C) and nitrogen (d 15 N) isotope ratios from fish muscle tissue to trace the long-term niche use of the three species. The stomach contents reveal the recently ingested prey items, whereas the carbon and nitrogen stable isotope ratios reflect the assimilated food sources and the trophic position of fish over several months (Fry 2006;. By combining these methods and data collected from one relatively deep (Z max = 52 m) and two shallower lakes (Z max = 12 and 17 m), we were able to explore the temporal and spatial stability of the possible resource partitioning between the three fish species.…”
mentioning
confidence: 99%
“…Isotopic data of a consumer and its potential prey are empirical measurements that track the flow of matter within a physical system. The relationship between isotopic data and trophic interactions has been well established in many ecosystems [85,128,60,84]. On the other hand, the relationship between prey availability and diet choice is still not well understood [1], need not be system-specific [77], and may di↵er across prey, even for the same predator [77].…”
Section: Incorporating Biological Informationmentioning
confidence: 99%