scholarly journals Stable isotopes of amino acids from reef fishes uncover Suess and nitrogen enrichment effects on local ecosystems

2020 ◽  
Vol 647 ◽  
pp. 149-160
Author(s):  
AJM Sabadel ◽  
LM Durante ◽  
SR Wing

In 1979, the Suess effect was described as decreasing δ13C in the oceans linked to anthropogenic CO2 emissions. After years of over-fertilization of farming soils and runoff, we hypothesized that δ15N in coastal environments would also decline, whereby synthetic fertilizers lead to depletion of the heavy isotope 15N. We used museum-preserved and modern samples of 3 fishes from Otago, New Zealand, to reconstruct the isotopic baselines of C and N and assess specific trophic positions through time (1955-present) based on bulk and amino acid stable isotope values. Our sample set included Odax pullus, a strictly herbivorous species, and 2 commercially important species: Nemadactylus macropterus and Parapercis colias. Muscle tissue of the fishes recorded the change in δ13CBulk through time, which matched estimated Suess effect values for New Zealand. We also resolved the effects on the C isotopic baseline from natural changes in the food web using analysis of the δ13C of essential amino acids and found that while P. colias maintained a steady diet, the food web position of N. macropterus likely changed. Analysis of δ15N of phenylalanine in O. pullus indicated a decrease of 0.023‰ yr-1 since 1955, which corroborates our coastal N-enrichment hypothesis. Furthermore, we found that isotopic changes for N. macropterus were consistent with overfishing and habitat degradation in the region. These data provide vital information for our resolution and understanding of how past environments have changed in terms of both anthropogenic influences on coastal food web structure and biogeochemical cycles of C and N in marine ecosystems.

Oecologia ◽  
2014 ◽  
Vol 175 (3) ◽  
pp. 911-922 ◽  
Author(s):  
Naoto F. Ishikawa ◽  
Yoshikazu Kato ◽  
Hiroyuki Togashi ◽  
Mayumi Yoshimura ◽  
Chikage Yoshimizu ◽  
...  

Radiocarbon ◽  
1997 ◽  
Vol 40 (2) ◽  
pp. 601-613 ◽  
Author(s):  
Nancy Ragano Beavan ◽  
Rodger J. Sparks

An isotopic database for the Pacific/Polynesian rat (Rattus exulans) and foods that it scavenges is used to examine diet-induced 14C age variation in omnivores. We discuss a suite of 26 δ14C determinations and 13C and 15N analysis for modern Pacific/Polynesian rat bone gelatin and available food items from Kapiti Island, New Zealand (40°51'S, 174°75'E). These analyses provide the first isotopic data for modern specimens of the species, collected as part of a larger project to determine potential sources of bias in unexpectedly old 14C age measurements on subfossil specimens of R. exulans from New Zealand. Stable C, N and 14C isotopic and trapping data are used to trace carbon intake via the diet of the rats in each habitat. Data from specimens linked to five specific habitats on the island indicate that modern populations of R. exulans are not in equilibrium with atmospheric values of δ14C, being either enriched or depleted relative to the atmospheric curve in 1996/97, the period of collection. The δ14C values recorded for R. exulans are associated with diet, and result from variation in δ14C values found in animal-protein food items available to a scavenging omnivore. The titer of carbon deviating from atmospheric values is believed to be derived from the essential amino acids in the protein-rich foods of the rat diet.Present evidence suggests that the depletion required to affect 14C ages limits the possibility that diet introduces dramatic offsets from true ages. Marine diets, for example, would have a variable effect on ages for terrestrial omnivores, contraindicating the application of a standard marine correction for such specimens. We suggest that to identify the extent to which diet may influence the 14C age in a given specimen of terrestrial omnivore, the separation and dating of essential amino acids vs. a nonessential amino, such as glycine, be applied.


2016 ◽  
Vol 62 (2) ◽  
pp. 541-560 ◽  
Author(s):  
Elizabeth D. Hetherington ◽  
Robert J. Olson ◽  
Jeffrey C. Drazen ◽  
Cleridy E. Lennert-Cody ◽  
Lisa T. Ballance ◽  
...  

Polar Biology ◽  
2018 ◽  
Vol 41 (5) ◽  
pp. 1013-1018 ◽  
Author(s):  
E. Ashley Shaw ◽  
Byron J. Adams ◽  
John E. Barrett ◽  
W. Berry Lyons ◽  
Ross A. Virginia ◽  
...  

2008 ◽  
Vol 153 (6) ◽  
pp. 1181-1198 ◽  
Author(s):  
Chang-Keun Kang ◽  
Eun Jung Choy ◽  
Yongsoo Son ◽  
Jae-Young Lee ◽  
Jong Kyu Kim ◽  
...  

2009 ◽  
Vol 7 (11) ◽  
pp. 740-750 ◽  
Author(s):  
Yoshito Chikaraishi ◽  
Nanako O. Ogawa ◽  
Yuichiro Kashiyama ◽  
Yoshinori Takano ◽  
Hisami Suga ◽  
...  

2006 ◽  
Vol 63 (10) ◽  
pp. 2167-2172 ◽  
Author(s):  
Brent A Murry ◽  
John M Farrell ◽  
Mark A Teece ◽  
Peter M Smyntek

Stable isotopes of carbon (C) and nitrogen (N) are commonly used to evaluate trophic relationships and food web structure; however, the decision to extract lipids or not may influence the interpretation of results. Lipid extraction is not a universal practice, thus pooling or comparing results across studies may not always be appropriate. Additionally, common lipid extraction techniques remove not only lipids, but also N-containing compounds that may alter the δ15N value of a sample. We examined differences in the interpretation of fish community trophic structure derived from δ13C and δ15N stable isotope data based on lipid-extracted and nonextracted samples from nine freshwater fish species. Lipid extraction significantly increased δ13C and δ15N, causing a positive shift in overall food web placement. The magnitude of isotopic change did not, however, differ among species, such that the overall interpretation of the fish community structure was not altered. The consistent increase in both C and N isotopes did, however, significantly alter the placement of the food web in coordinate space relative to nonextracted webs. Cross-study comparisons need to consider these procedural inconsistencies when drawing conclusions from multiple studies.


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