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

• Published in: Canadian journal of fisheries and aquatic sciences 2005-03, Vol.62 (3), p.518-526
• Main Authors: Koyama, Akihiro, Kavanagh, Kathleen, Robinson, Andrew
• Format: Article
• Language: English
• Subjects: Animal migration; Animal, plant and microbial ecology; Applied ecology; Biological and medical sciences; Coniferous forests; Coniferous trees; Environmental impact; Exploitation and management of natural biological resources (hunting, fishing and exploited populations survey, etc.); Fish populations; Foliage; Forest ecosystems; Forests; Freshwater; Fundamental and applied biological sciences. Psychology; Marine ecosystems; Nitrogen; Nutrient retention; Nutrient sources; Oncorhynchus mykiss; Retention; Riparian forests; Rivers; Salmon; Seedlings; Stable isotopes; Streams; Waterfalls
• ISSN: 0706-652X; 1205-7533
• DOI: 10.1139/f04-220

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 15 N/ 14 N ratio (δ 15 N). Also, to evaluate whether N obtained from marine sources was evident in riparian forests, we analyzed the δ 15 N 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 δ 15 N. Furthermore, we determined that foliar δ 15 N values in riparian forests were explained by the historical occurrence of salmon. Foliar δ 15 N 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.