Growth versus metabolic tissue replacement in mouse tissues determined by stable carbon and nitrogen isotope analysis

2005 ◽  
Vol 83 (5) ◽  
pp. 631-641 ◽  
Author(s):  
Stephen E MacAvoy ◽  
Stephen A Macko ◽  
Lynne S Arneson

Stable-isotope signatures in animal tissues presumably reflect the local food web. However, that assumption may be complicated by differential nutrient routing, fractionation, and the possibility that large organisms are not in isotopic equilibrium with seasonally available food sources. Additionally, the rate at which organisms incorporate the isotopic signature of a food is largely unknown. In this study we assessed the rate of carbon- and nitrogen-isotope turnover in liver, muscle, and blood in mice (Mus musculus L., 1758) following a diet change. We report the proportion of tissue turnover caused by growth versus that caused by metabolic tissue replacement. Growth accounted for approximately 10% of observed tissue turnover in adult mice. Blood carbon had the shortest half-life (16.9 days), followed by muscle carbon (23.9 days). Liver carbon turnover, which was slower than blood and muscle carbon turnovers, was not as well described by the exponential decay equations. All tissues primarily reflect the protein carbon signature rather than the carbohydrate carbon signature. The nitrogen signature in all tissues was enriched by 3‰–5‰ over their diets' nitrogen signature, depending on tissue type, and the isotopic turnover rates of nitrogen in blood and muscle were comparable with those observed for carbon.

2012 ◽  
Vol 405 (9) ◽  
pp. 2857-2867 ◽  
Author(s):  
Kathrin Schreglmann ◽  
Martina Hoeche ◽  
Sibylle Steinbeiss ◽  
Sandra Reinnicke ◽  
Martin Elsner

2009 ◽  
Vol 44 (4) ◽  
pp. 313-322 ◽  
Author(s):  
Monalisa Elshayeb ◽  
Michael D. MacKinnon ◽  
D. George Dixon ◽  
Michael Power

Abstract One strategy for reclamation of oil sands leases in northern Alberta is the construction of lakes and wetlands by capping oil sands process-affected material (OSPM) with water. To assess this approach, experimental sites containing a range of OSPM have been constructed to monitor the evolution of the resulting aquatic habitats. Stable isotopes of carbon and nitrogen were used to assess the effects of OSPM on aquatic food webs. Carbon and nitrogen isotopic signatures of sediment, dissolved inorganic and organic carbon, particulate organic matter, periphyton, plants, plankton, aquatic invertebrates, and fish were used to assess differences related to the naphthenic acid (NA) concentration in OSPM and reference sites. NAs are a principal contaminant of concern in OSPM. Sites were grouped into low (0 to 4 mg/L), medium (4 to 15 mg/L), and high (>15 mg/L) NA concentrations. There were no significant differences in food web area or length among the three NA groupings. In most cases, carbon isotope analyses of samples from low, medium, and high NA concentration sites were not significantly different, suggesting that OSPM is not a significant contributor to food web carbon sources. Significant differences were found in nitrogen isotope signatures between low, medium, and high NA sites. Ammonia from OSPM is suggested as the main contributor to δ15N enrichment.


2019 ◽  
Vol 9 (1) ◽  
Author(s):  
Alexey G. Nikitin ◽  
Peter Stadler ◽  
Nadezhda Kotova ◽  
Maria Teschler-Nicola ◽  
T. Douglas Price ◽  
...  

AbstractArchaeogenetic research over the last decade has demonstrated that European Neolithic farmers (ENFs) were descended primarily from Anatolian Neolithic farmers (ANFs). ENFs, including early Neolithic central European Linearbandkeramik (LBK) farming communities, also harbored ancestry from European Mesolithic hunter gatherers (WHGs) to varying extents, reflecting admixture between ENFs and WHGs. However, the timing and other details of this process are still imperfectly understood. In this report, we provide a bioarchaeological analysis of three individuals interred at the Brunn 2 site of the Brunn am Gebirge-Wolfholz archeological complex, one of the oldest LBK sites in central Europe. Two of the individuals had a mixture of WHG-related and ANF-related ancestry, one of them with approximately 50% of each, while the third individual had approximately all ANF-related ancestry. Stable carbon and nitrogen isotope ratios for all three individuals were within the range of variation reflecting diets of other Neolithic agrarian populations. Strontium isotope analysis revealed that the ~50% WHG-ANF individual was non-local to the Brunn 2 area. Overall, our data indicate interbreeding between incoming farmers, whose ancestors ultimately came from western Anatolia, and local HGs, starting within the first few generations of the arrival of the former in central Europe, as well as highlighting the integrative nature and composition of the early LBK communities.


2020 ◽  
Vol 34 (18) ◽  
Author(s):  
Kerri J. Smith ◽  
Clive N. Trueman ◽  
Christine A.M. France ◽  
Markus J. Peterson

2015 ◽  
Vol 57 ◽  
pp. 69-79 ◽  
Author(s):  
Jessica A. Pearson ◽  
Amy Bogaard ◽  
Mike Charles ◽  
Simon W. Hillson ◽  
Clark Spencer Larsen ◽  
...  

2008 ◽  
Vol 22 (21) ◽  
pp. 3393-3400 ◽  
Author(s):  
Michael I. Bird ◽  
Elaine Tait ◽  
Christopher M. Wurster ◽  
Robert W. Furness

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