Conservative N cycling despite high atmospheric deposition in early successional African tropical lowland forests

• Published in: Plant and soil Vol. 477; no. 1-2; pp. 743 - 758
• Main Authors: Makelele, Isaac Ahanamungu, Bauters, Marijn, Verheyen, Kris, Barthel, Matti, Six, Johan, Rütting, Tobias, Bodé, Samuel, Cizungu Ntaboba, Landry, Mujinya Bazirake, Basile, Boyemba Bosela, Faustin, Kimbesa, Fabrice, Ewango, Corneille, Boeckx, Pascal
• Format: Journal Article
• Language: English
• Published: Cham Springer International Publishing 01.08.2022; Springer; Springer Nature B.V
• Subjects: Agricultural Science; Agriculture; Analysis; Atmospheric deposition; basin; basins; Belgium; biogeochemistry; biomass production; Biomedical and Life Sciences; Botanik; Botany; Canopies; canopy; carbon; Congo (Kinshasa); Congo basin; Cycles; Deposition; Ecological succession; Ecology; Emission; Emissions; Essential nutrients; fine roots; fixation; forest succession; Forests; interception; isotopic composition; Jordbruksvetenskap; Leaching; Leaf litter; Leaves; Life Sciences; Litter; Litter fall; Nitrogen; nitrogen content; Nitrogen cycle; nitrogen deposition; Nitrous oxide; Nutrient availability; Nutrients; Old growth forests; plant litter; Plant Physiology; Plant Sciences; rain-forest; Research Article; secondary forests; Secondary succession; soil; Soil Science & Conservation; Stoichiometry; throughfall; Tropical environments; Tropical forests; Belgium; Congo (Kinshasa); Tropical forests biogeochemistry; Secondary succession; Nitrogen cycle; Congo basin
• ISSN: 0032-079X; 1573-5036
• DOI: 10.1007/s11104-022-05473-7

Background Across the tropics, the share of secondary versus primary forests is strongly increasing. The high rate of biomass accumulation during this secondary succession relies on the availability of essential nutrients, such as nitrogen (N). Nitrogen primarily limits many young secondary forests in the tropics. However, recent studies have shown that forests of the Congo basin are subject to high inputs of atmospheric N deposition, potentially alleviating this N limitation in early succession. Methods To address this hypothesis, we assessed the N status along a successional gradient of secondary forests in the Congo basin. In a set-up of 18 plots implemented along six successional stages, we quantified year-round N deposition, N leaching, N 2 O emission and the N flux of litterfall and fine root assimilation. Additionally, we determined the N content and C:N stoichiometry for canopy leaves, fine roots, and litter, as well as δ 15 N of canopy leaves. Results We confirmed that these forests receive high amounts of atmospheric N deposition, with an increasing deposition as forest succession proceeds. Additionally, we noted lower C:N ratios, and higher N leaching losses, N 2 O emission, and foliar δ 15 N in older secondary forest (60 years). In contrast, higher foliar, litter and root C:N ratios, and lower foliar δ 15 N, N leaching, and N 2 O emission in young (< 20 years) secondary forest were observed. Conclusions Altogether, we show that despite high N deposition, this early forest succession still shows conservative N cycling characteristics, which are likely indicating N limitation early on in secondary forest succession. As secondary succession advances, the N cycle gradually becomes more open.