scholarly journals Traceability of poultry offal meal in broiler feeding using isotopic analysis (δ13C and δ15N) of different tissues

2010 ◽  
Vol 12 (1) ◽  
pp. 13-20 ◽  
Author(s):  
RP Oliveira ◽  
C Ducatti ◽  
AC Pezzato ◽  
JC Denadai ◽  
VC Cruz ◽  
...  
2014 ◽  
Vol 2 (1) ◽  
Author(s):  
Matías G. Ammann ◽  
Osvaldo J. Mendonça ◽  
Noelia I. Merlo ◽  
María A. Bordach ◽  
Robert H. Tykot

Presented here are the first results of an ongoing research project on stable isotopic analysis of human bone samples from six sites located at Jujuy province, NW Argentina. The region was inhabited by hunter gatherers as early as 10,000 years ago (Archaic Period). Sometime between 500 BC-AD 1600, peoples from the region became agricultural-pastoralists. The prehistoric development of these societies was severed in 1596 by the Spanish Conquest. A diversity of environmental as well as chronological differences led the prehistoric societies of the region to adopt and display a series of adaptive responses. Active exchange of products was a common fact. The aforementioned circumstances raise expectations concerning the existence of possible variations in the actual consumption of available alimentary items in Puna (3000 to 4700 m asl), as well as in Quebrada de Humahuaca (2000 to 2800 m asl). The obtained δ13C and δ15N values on both apatite and collagen show elevated consumption of C4 resources in Quebrada de Humahuaca since the onset of the Formative Period (ca. 500 BC). Puna samples, on the other hand, show a sustained, long lasting chronological emphasis on camelid production and consumption as well as other C3 resources exploited. We conclude that, in spite of the considerable interactions and trading that took place between these two regions in prehistoric times, they were not strong enough to erase the environmental influences that determined the existence of distinctive stable isotope patterns related to diet (and composition of meals) between Quebrada de Humahuaca and Puna peoples.


2013 ◽  
Vol 308-309 ◽  
pp. 42-44 ◽  
Author(s):  
Yizhi Zhu ◽  
Peng Cheng ◽  
Yachang Yang

Animals ◽  
2020 ◽  
Vol 10 (12) ◽  
pp. 2301
Author(s):  
Miquel Planas ◽  
Alex Paltrinieri ◽  
Mario Davi Dias Carneiro ◽  
Jorge Hernández-Urcera

Isotopic stable analysis (SIA) is a powerful tool in the assessment of different types of ecological and physiological studies. For that, different preservation methods for sampled materials are commonly used prior to isotopic analysis. The effects of various preservation methods (freezing, ethanol and formaldehyde) were analyzed for C:N, and δ13C and δ15N signals on a variety of tissues including dorsal fins (three seahorse and two pipefish species), seahorse newborns (three seahorses species), and prey (copepods and different stages of Artemia) commonly used to feed the fishes under rearing conditions. The aims of the study were: (i) to evaluate isotopic effects of chemical preservation methods across different types of organisms and tissues, using frozen samples as controls, and (ii) to construct the first conversion models available in syngnathid fishes. The chemical preservation in ethanol and, to a lesser extent, in formaldehyde significantly affected δ13C values, whereas the effects on δ15N signatures were negligible. Due to their low lipid content, the isotopic signals in fish fins was almost unaffected, supporting the suitability of dorsal fins as the most convenient material in isotopic studies on vulnerable species such as syngnathids. The regression equations provided resulted convenient for the successful conversion of δ13C between preservation treatments. Our results indicate that the normalization of δ15N signatures in preserved samples is unnecessary. The conversion models should be applicable in isotopic field studies, laboratory experiments, and specimens of historical collections.


2012 ◽  
Vol 26 (5) ◽  
pp. 487-493 ◽  
Author(s):  
Christopher A. Vasil ◽  
Michael J. Polito ◽  
William P. Patterson ◽  
Steven D. Emslie

2007 ◽  
Vol 341 ◽  
pp. 205-215 ◽  
Author(s):  
J Guelinckx ◽  
J Maes ◽  
P Van Den Driessche ◽  
B Geysen ◽  
F Dehairs ◽  
...  

Author(s):  
D.E. Brownlee ◽  
A.L. Albee

Comets are primitive, kilometer-sized bodies that formed in the outer regions of the solar system. Composed of ice and dust, comets are generally believed to be relic building blocks of the outer solar system that have been preserved at cryogenic temperatures since the formation of the Sun and planets. The analysis of cometary material is particularly important because the properties of cometary material provide direct information on the processes and environments that formed and influenced solid matter both in the early solar system and in the interstellar environments that preceded it.The first direct analyses of proven comet dust were made during the Soviet and European spacecraft encounters with Comet Halley in 1986. These missions carried time-of-flight mass spectrometers that measured mass spectra of individual micron and smaller particles. The Halley measurements were semi-quantitative but they showed that comet dust is a complex fine-grained mixture of silicates and organic material. A full understanding of comet dust will require detailed morphological, mineralogical, elemental and isotopic analysis at the finest possible scale. Electron microscopy and related microbeam techniques will play key roles in the analysis. The present and future of electron microscopy of comet samples involves laboratory study of micrometeorites collected in the stratosphere, in-situ SEM analysis of particles collected at a comet and laboratory study of samples collected from a comet and returned to the Earth for detailed study.


1981 ◽  
Vol 45 (02) ◽  
pp. 110-115 ◽  
Author(s):  
György Csákó ◽  
Eva A Suba

SummaryPlatelet aggregations were studied by a turbidimetric method in citrated human platelet-rich plasmas (PRP) in vitro. Human Clq inhibited the aggregations caused by collagens derived from different tissues and species. Clq was needed by weight in comparable quantities to collagen for neutralizing the aggregating effect. The dependence of the inhibitory reaction on the preincubation of platelets with Clq and the differences in the occurrence of aggregating substances in supernatants of PRP triggered with collagen in the presence or absence of Clq, confirmed that Clq exerts its effect by preventing fixation of collagen to platelets. In addition, the high specificity of the inhibitory action of Clq for collagen-induced platelet aggregation was demonstrated by results obtained for testing a variety of aggregating agents in combination with Clq and/or collagen.Since normal concentrations of Clq in the blood are in the range of inhibitory doses of Clq for collagen-induced platelet aggregations in vitro and upon activation of complement Clq is known to dissociate from Cl, it is proposed that Clq may participate in a highly specific manner in regulating platelet reactivity to collagen in vivo.


2019 ◽  
Author(s):  
Marko J. Spasojevic ◽  
Sören Weber1

Stable carbon (C) and nitrogen (N) isotopes in plants are important indicators of plant water use efficiency and N acquisition strategies. While often regarded as being under environmental control, there is growing evidence that evolutionary history may also shape variation in stable isotope ratios (δ13C and δ15N) among plant species. Here we examined patterns of foliar δ13C and δ15N in alpine tundra for 59 species in 20 plant families. To assess the importance of environmental controls and evolutionary history, we examined if average δ13C and δ15N predictably differed among habitat types, if individual species exhibited intraspecific trait variation (ITV) in δ13C and δ15N, and if there were a significant phylogenetic signal in δ13C and δ15N. We found that variation among habitat types in both δ13C and δ15N mirrored well-known patterns of water and nitrogen limitation. Conversely, we also found that 40% of species exhibited no ITV in δ13C and 35% of species exhibited no ITV in δ15N, suggesting that some species are under stronger evolutionary control. However, we only found a modest signal of phylogenetic conservatism in δ13C and no phylogenetic signal in δ15N suggesting that shared ancestry is a weaker driver of tundra wide variation in stable isotopes. Together, our results suggest that both evolutionary history and local environmental conditions play a role in determining variation in δ13C and δ15N and that considering both factors can help with interpreting isotope patterns in nature and with predicting which species may be able to respond to rapidly changing environmental conditions.


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