Contrasting nitrogen cycling between herbaceous wetland and terrestrial ecosystems inferred from plant and soil nitrogen isotopes across China. (10th March 2022)

• Record Type: Journal Article
• Authors: Hu, Yu‐Kun; Liu, Guo‐Fang; Pan, Xu; Song, Yao‐Bin; Dong, Ming; Cornelissen, Johannes H. C.
• Is Part Of: Journal of ecology. Volume 110:Number 6(2022)
• Page Start: 1259
• Page End: 1270
• Publication Date: 2022-03-10
• Subjects: large environmental gradients -- mycorrhizal types -- nitrogen availability -- nitrogen dynamics -- plant functional types -- plant–soil systems -- stable isotopes -- wetlands; Plant ecology -- Periodicals; 577.05
• DOI: 10.1111/1365-2745.13866
• Languages: English
• ISSNs: 0022-0477

Abstract

Abstract: Understanding nitrogen (N) cycling in different ecosystems is crucial to predicting and mitigating the global effects of altered N inputs. Although wetlands have always been assumed to differ largely from terrestrial ecosystems in N cycling, evidence from direct comparison from the field along wide environmental gradients is lacking. Here, we hypothesized strong coupling of plant and soil δ 15 N in terrestrial ecosystems due to lower N inputs and losses but weak coupling of plant and soil δ 15 N in wetlands because of higher N inputs and losses. We performed a large‐scale field investigation on 26 pairs of herbaceous wetland and terrestrial sites across China covering 21 degrees of latitude and determined natural abundance of nitrogen isotopes (δ 15 N) in soils and leaves of 346 dominant and subordinate plant species. We analysed the relationships between leaf and soil δ 15 N and their drivers including plant functional types in these two types of ecosystems. Plant functional types including mycorrhizal type and N2 ‐fixing status had consistently significant influences on leaf δ 15 N in herbaceous wetland and terrestrial ecosystems. Leaf δ 15 N increased significantly with soil δ 15 N within and across mycorrhizal types in both ecosystems, and, as hypothesized, the relationships were stronger and steeper in terrestrial than in wetland ecosystems. Moreover, leaf and soil δ 15 N were positively and significantly correlated within both N2 ‐fixers and non‐N2 ‐fixers in terrestrial ecosystems and within only non‐N2 ‐fixers in wetlands. At the community level, we also found more highly significant relationships between leaf and soil δ 15 N in terrestrial than in wetland ecosystems. Besides plant functional types, climatic and soil factors contributed to the variation in leaf δ 15 N in both ecosystems. Synthesis . Weaker relationships between plant and soil δ 15 N in wetlands at species and community levels support the hypothesis that larger N inputs and losses lead to weaker coupling in the plant–soil systems in wetlands than in terrestrial ecosystems. This provides strong evidence from a large spatial scale for contrasting N cycling in these two types of ecosystems regardless of plant functional type in terms of nutrient uptake strategy. Our findings add to our predictive power of ecosystem N dynamics under environmental changes, for example, land‐use changes and elevated N inputs. Abstract : Our results support the hypothesis that larger N inputs and losses lead to weaker coupling in the plant–soil systems in wetlands than in terrestrial ecosystems. Especially it is robust regardless of plant functional type in terms of nutrient uptake strategy. These findings add to our predictive power of ecosystem N dynamics under environmental changes, for example, land‐use changes and elevated N inputs.