scholarly journals Carbon and nitrogen isotope fractionation of amino acids in an avian marine predator, the gentoo penguin ( Pygoscelis papua )

2015 ◽  
Vol 5 (6) ◽  
pp. 1278-1290 ◽  
Author(s):  
Kelton W. McMahon ◽  
Michael J. Polito ◽  
Stephanie Abel ◽  
Matthew D. McCarthy ◽  
Simon R. Thorrold
2019 ◽  
Vol 21 (1) ◽  
pp. 51-62 ◽  
Author(s):  
Matthew J. Berens ◽  
Bridget A. Ulrich ◽  
Jennifer H. Strehlau ◽  
Thomas B. Hofstetter ◽  
William A. Arnold

The fractionation of nitrogen and carbon isotopes during the reduction of 2,4-dinitroanisole is substantially different than that observed for hydrolysis reactions.


1999 ◽  
Vol 56 (11) ◽  
pp. 2203-2210 ◽  
Author(s):  
Elena Gorokhova ◽  
Sture Hansson

The trophic isotope fractionation of mysids, in response to a change in the isotopic composition in their diet, was examined in the laboratory. Field-caught Mysis mixta and Neomysis integer had similar δ13C values, ranging between -23.1 and -21.5‰. They also had similar δ15N values, and for both species, this value increased with body size. Experimental starvation did not change the isotopic composition. To test for metabolic fractionation of isotopes, the mysids were fed different diets, newly hatched Artemia and detrital Enteromorpha. The isotopic composition was monitored in abdominal muscle tissue, exoskeleton, and feces over 12 weeks. The δ13C composition in muscle tissue had not reached an isotopic equilibrium with the diet at the end of the experiment, while the exoskeleton came into equilibrium with the food in 2-3 weeks. Muscle was enriched in 15N relatively to the food, +3.6‰ for Artemia and +2.7‰ for Enteromorpha. The isotopic composition in muscle, exuviae, and feces may form a basis for diet reconstruction of mysids. The feces δ13C and δ15N values mirror the diet over the last few hours, exuviae δ13C values represent nutrients metabolized 2-3 weeks ago, and muscle tissue integrates the isotopic signal over a relatively long period.


1983 ◽  
Vol 29 (2) ◽  
pp. 231-234 ◽  
Author(s):  
R. G. L. McCready ◽  
W. D. Gould ◽  
R. W. Barendregt

Desulfovibrio reduce NO3−to NH4+ via a dissimilatory pathway. In 21 days, four strains of Desulfovibrio reduced 36–48% of the available NO3− to ammonium. During this reductive process extensive nitrogen isotope fractionation occurred: the product NH4+ was enriched in 15N in the initial sample, then became enriched in 14N to a minimum value at approximately 20–25% reaction, and then became isotopically heavier as the reaction proceeded.


2008 ◽  
Vol 42 (6) ◽  
pp. 1997-2003 ◽  
Author(s):  
Thomas B. Hofstetter ◽  
Anke Neumann ◽  
William A. Arnold ◽  
Akané E. Hartenbach ◽  
Jakov Bolotin ◽  
...  

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