Litter decomposition and organic matter turnover in northern forest soils
By B. Berg. 2000
1,007 citations recorded by the source corpus.
Subfields: Ecology, Insect Science, Soil Science
View Paper: https://www.semanticscholar.org/paper/6fe528df09c1b31cc275a9e4bcd9eb50b01c1e24
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Ecology
- S. Hättenschwiler
- Petr Baldrian
- R. Brandl
- M. Schädler
- V. Meentemeyer
- J. Schimel
- K. Fujii
- M. Bradford
In Insect Science
- Petr Baldrian
- S. Hättenschwiler
- A. Austin
- Lucía Vivanco
- V. Meentemeyer
- R. Brandl
- M. Schädler
- M. Bradford
In Soil Science
- D. Forrester
- S. Hättenschwiler
- Petr Baldrian
- M. Bradford
- J. Schimel
- Lucía Vivanco
- A. Austin
- M. Schädler
Citations in the corpus
- Soil acidification and adaptations of plants and microorganisms in Bornean tropical forests (2014, background): “Lignin degradation is a rate-limiting step for litter decomposition by microorganisms (Berg 2000; Wieder et al. 2009).”
- Consequences of non‐random species loss for decomposition dynamics: experimental evidence for additive and non‐additive effects (2008, background): “prinus were only similar in their initial lignin concentrations, contradicting the hypothesis that lignin concentration is more important in later stages of decay (McClaugherty & Berg 1987; Taylor et al. 1989; Berg 2000).”
- Defining nutritional constraints on carbon cycling in boreal forests – towards a less `phytocentric' perspective (2002, background): “However, decomposition of litter with a high content of lignin during the late stages of decomposition seems to be retarded by high nutrient availability (Berg et al., 1996; Berg, 2000; Berg and Meentemeyer, this volume).”
- Litter production, leaf litter decomposition and nutrient return in Cunninghamia lanceolata plantations in south China: effect of planting conifers with broadleaved species (2007, result): “In the present study, the decomposition rate of leaf litter was correlated with initial N concentration, which was consistent with results reported by Sundarapandian and Swamy (1999) who also found that litter with higher N content decomposed faster and Berg (2000) who observed the mass-loss rate ”
- Mixed-species plantations of Eucalyptus with nitrogen-fixing trees: A review (2006, background): “However, longer-term rates of decomposition may be slower for litter with high N concentrations because N can retard the later stages of lignin decay (Berg and Ekbohm, 1991; Berg, 2000).”
- Plant canopy effects on litter accumulation and soil microbial biomass in two temperate forests (2008, neutral): “Beech leaves are also particularly rich in lignin and tannin compared to other deciduous leaves (Berg 2000).”
- Laccases: toward disentangling their diversity and functions in relation to soil organic matter cycling (2010, background): “Accordingly, decomposition is a complex suite of biotic and abiotic processes and constitutes the principal pathway for the return of nutrients to soil (Berg 2000; Berg and McClaugherty 2003; Prescott 2005).”
- Effects of Tree Species Diversity on Litter Quality and Decomposition (2005, background): “2; Berg 2000). Fagus sylvatica, for example, exhibits differences in lignin concentration from 25–50 % and nitrogen concentration ranges from 0.8–1.7 % among different sites sampled over large geographical regions.As Berg pointed out(2000), the different species graphically displayed in Fig.”
- Litterfall and litter nutrient dynamics under cocoa ecosystems in lowland humid Ghana (2010, background): “Forest litter acts as an input-output system of nutrients and the rates at which forest litter falls contribute to the regulation of nutrient cycling, fertility sustenance and primary productivity in forest and tree-based ecosystems (Berg 2000; Ranger et al. 2003).”
- Arbuscular mycorrhizal fungi reduce decomposition of woody plant litter while increasing soil aggregation (2015, background): “Berg (2000) proposed that N availability is the factor that is simultaneously responsible for increased initial decomposition and decreased subsequent decomposition of litter.”
- Rates of litter decomposition over 6 years in Canadian forests: influence of litter quality and climate (2002, background): “Three major causes for these restrictions include climate (temperature and moisture), substrate quality (chemical and physical characteristics), and the composition and abundance of the soil biotic communities (Berg 2000; Prescott et al. 2000).”
- Nitrogen transfer between decomposing leaves of different N status (2007, background): “Because microbes decomposing fresh litter are frequently N-limited (Berg, 2000), the effect of net movement from one litter species to another would likely accelerate the decomposition of the low-N species.”