Influence of balsam poplar tannin fractions on carbon and nitrogen dynamics in Alaskan taiga floodplain soils

• Published in: Soil biology & biochemistry Vol. 33; no. 12; pp. 1827 - 1839
• Main Authors: Fierer, Noah, Schimel, Joshua P., Cates, Rex G., Zou, Jiping
• Format: Journal Article
• Language: English
• Published: Oxford Elsevier Ltd 01.10.2001; New York, NY Elsevier Science
• Subjects: Agronomy. Soil science and plant productions; Balsam poplar; Biological and medical sciences; Chemical, physicochemical, biochemical and biological properties; Fundamental and applied biological sciences. Psychology; Mineralization; Nitrogen cycling; Organic matter; Physics, chemistry, biochemistry and biology of agricultural and forest soils; Populus balsamifera; Secondary chemicals; Soil science; Succession; Taiga; Tannin; tannins; Alaska; United States; North America; America; USA, Alaska; Succession; Tannin; Mineralization; Taiga; Nitrogen cycling; Secondary chemicals; Balsam poplar; Forest soil; Biogeochemical cycle; Vegetation dynamics; Microbial biomass; Salicaceae; Dose activity relation; Carbon cycle; Flood plain; Nitrogen cycle; Enzymatic activity; Dicotyledones; Angiospermae; Nitrification; Hardwood forest tree; Spermatophyta; Betulaceae; Populus balsamifera; Vegetal tannin
• ISSN: 0038-0717; 1879-3428
• DOI: 10.1016/S0038-0717(01)00111-0

The feedbacks between plant and soil processes play an important role in driving forest succession. One poorly understood feedback mechanism is the interaction between plant secondary chemicals and soil microbes. In the Alaskan taiga, changes in nutrient cycling caused by balsam poplar ( Populus balsamifera) secondary chemicals may affect the transition from alder ( Alnus tenuifolia) to balsam poplar on river floodplains. We examined the effects of four poplar condensed tannin fractions on N cycling in alder and poplar soils. Tannins were added to forest floor samples from both poplar and alder sites. Samples were incubated for 1 month in the laboratory with soil respiration rates measured over the course of the incubation. At the end of the incubation we measured both net and gross nitrogen mineralization and nitrification, microbial biomass C and N, and the activity of various exoenzymes. In all soils, tannin additions reduced N availability, however, the mechanisms differed depending on the molecular weight of the tannin and the native soil microbial community. Low molecular weight tannin fractions served as a labile C source in poplar Oi, poplar Oe, and alder Oe horizons but were toxic to microbes in alder Oi. High molecular weight tannin fractions appeared to act primarily by binding extracellular substrates and thus limiting C and N mineralization, with the strongest effects observed in the alder soils.