Marine nitrogen in central Idaho riparian forests: evidence from stable isotopes

2005 ◽  
Vol 62 (3) ◽  
pp. 518-526 ◽  
Author(s):  
Akihiro Koyama ◽  
Kathleen Kavanagh ◽  
Andrew Robinson

Terrestrial and marine ecosystems are linked by the annual migration of salmonids. We examined the contribution of anadromous fish to foliar nitrogen (N) in central Idaho riparian forests where anadromous fish have been in sharp decline for approximately 30 years. To determine if the amount of N from anadromous fish carcasses can be assessed from conifer foliage, we fertilized seedlings with varying proportions of N from marine sources and analyzed their foliar 15N/14N ratio (δ15N). Also, to evaluate whether N obtained from marine sources was evident in riparian forests, we analyzed the δ15N of conifer foliage, above and below waterfalls, along historically salmon-bearing and non-salmon-bearing streams and rivers in central Idaho. In the seedling study, the amount of marine N was positively correlated with foliar δ15N. Furthermore, we determined that foliar δ15N values in riparian forests were explained by the historical occurrence of salmon. Foliar δ15N declined significantly from bankside to upslope trees in transects along salmon-bearing streams and rivers, whereas there was no significant gradient along transects perpendicular to non-salmon-bearing reaches. We therefore conclude that marine nutrient sources have historically contributed to the N pool in riparian conifer forests and marine N persisted following 30 years of severe populations declines.

2017 ◽  
Vol 47 (11) ◽  
pp. 1506-1516 ◽  
Author(s):  
Tadd A. Wheeler ◽  
Kathleen L. Kavanagh

The historic abundance of salmonids returning to natal streams of the inland Pacific Northwest, USA, may have constituted a major nutrient influx into these commonly oligotrophic ecosystems. Inland ecosystems tend to be warmer and dryer and more nutrient limited than coastal ecosystems; therefore, understanding how these inland conditions influence the soil biogeochemical responses to salmon carcass deposition in riparian forests is a vital step in appropriately mitigating for the loss of this nutrient subsidy. Deposition of salmon carcasses in central Idaho riparian forests resulted in a 480-fold increase in soil nitrogen (N), a sevenfold increase in dissolved organic carbon (C), and a fourfold increase in soil respired CO2, with significant biogeochemical responses persisting at one year after amendment. Despite these large increases in soil N and C, estimates of soil N and C loading only accounted for 31% and 16% of the fish carcass N and C, respectively. However, the magnitude and persistence of soil biogeochemical responses to the deposition of anadromous fish carcasses in central Idaho attests to the importance of this nutrient subsidy to inland riparian ecosystems of the Pacific Northwest.


2020 ◽  
Vol 39 ◽  
pp. 101413
Author(s):  
Roberto González-De Zayas ◽  
Sergio Rossi ◽  
Leslie Hernández-Fernández ◽  
Roberto Velázquez-Ochoa ◽  
Marcelo Soares ◽  
...  

2015 ◽  
Vol 162 (5) ◽  
pp. 1099-1110 ◽  
Author(s):  
John E. Richert ◽  
Felipe Galván-Magaña ◽  
A. Peter Klimley

Forests ◽  
2019 ◽  
Vol 10 (3) ◽  
pp. 251 ◽  
Author(s):  
Emmanuel Boakye ◽  
Aster Gebrekirstos ◽  
Dibi Hyppolite ◽  
Victor Barnes ◽  
Stefan Porembski ◽  
...  

Stable isotopes of tree rings are frequently used as proxies in climate change studies. However, species-specific relationships between climate and tree-ring stable isotopes have not yet been studied in riparian forests in the savannas of West Africa. Four cross-dated discs, each of Afzelia africana Sm. (evergreen) and Anogeissus leiocarpus (DC.) Guill. & Perr. (deciduous) in the humid (HSZ) and dry (DSZ) savanna zones of the Volta basin in Ghana were selected from a larger tree-ring dataset to assess the relationships between the tree-ring carbon isotope composition (δ13C values) and climatic parameters. The atmospherically corrected δ13C values of both studied species showed that A. africana was enriched in 13C compared to A. leiocarpus. Strong correlations were found between δ13C values of A. africana and A. leiocarpus with temperature, but weak correlations with precipitation. Spatial correlation analysis revealed significant relationships between δ13C values of both tree species and Sea Surface Temperatures in the Gulf of Guinea in the southern Atlantic Ocean. The results suggest that the carbon isotope composition of riparian trees in the Volta river basin has a potential to reconstruct climate variability and to assess tree ecological responses to climate change.


2006 ◽  
Vol 84 (10) ◽  
pp. 1453-1460 ◽  
Author(s):  
Rania A. Tarboush ◽  
Stephen E. MacAvoy ◽  
Stephen A. Macko ◽  
Victoria Connaughton

Stable isotopes of carbon, nitrogen, and sulfur in organisms can trace nutrient sources and determine trophic interactions. However, time is required for an organism to reflect the isotopic composition of its diet. The rate at which an organism incorporates the isotopic signature of its food has a growth (k) component and a metabolic tissue replacement (m) component. This study shows that metabolic tissue replacement accounts for between 68% and 80% of the observed changes in isotopic signature in zebra danio ( Danio rerio (Hamilton, 1822)) muscle following a dietary shift, with the remainder owing to growth of new tissue. The half-lives of carbon, nitrogen, and sulfur were ~53, ~147 and ~58 days, respectively. This indicates that a significant period of isotopic disequilibria exists before zebra danio resemble dietary isotopic composition. These results show that catabolic replacement of tissue, as well as growth, must be taken into account when predicting the rate of isotope incorporation in warm-water fish. When using isotopic ratios to decipher food webs and trophic interactions, researchers should be aware that the often held assumption of isotopic equilibrium between diet and consumer may be violated.


Author(s):  
Tasman P. Crowe ◽  
Christopher L. J. Frid
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