scholarly journals Effects of root decomposition on plant-soil feedback of early- and mid-successional plant species

2016 ◽  
Vol 212 (1) ◽  
pp. 220-231 ◽  
Author(s):  
Naili Zhang ◽  
Wim H. Van der Putten ◽  
G. F. Ciska Veen
Author(s):  
E. R. Jasper Wubs ◽  
Tom van Heusden ◽  
Pauline D. Melchers ◽  
T. Martijn Bezemer

2016 ◽  
Vol 104 (5) ◽  
pp. 1243-1249 ◽  
Author(s):  
Conrad Schittko ◽  
Christian Runge ◽  
Marek Strupp ◽  
Sascha Wolff ◽  
Susanne Wurst

2021 ◽  
Author(s):  
Eka Purnamasari ◽  
Meine van Noordwijk ◽  
Rizky Maulana ◽  
Danny Saputra ◽  
Rika Ratna Sari ◽  
...  

Abstract Background and PurposeAbove- and belowground organic inputs feed decomposer communities in the soil enhancing soil organic matter (Corg) formation, depending on the vegetation, soil, contextual factors and human management of (agro)ecosystems. Plant-soil feedback in volcanic ash rapidly increases Corg during transformation to Andisols. We quantified fine root turnover in agroforestry systems, including the ash-adapted native tree Parasponia rigida, as part of the C accumulation process. MethodsFine root (<2 mm) decomposition was quantified with a total of 1440 litterbag samples, testing the effects of six tree species (Coffea canephora, Persea americana, Durio zibethinus, Gliricidia sepium, Falcataria moluccana and Parasponia rigida), three distances to the nearest coffee trees, two seasons (rainy and dry), two sites (with and without recent ash deposits), four time intervals (2, 4, 6 and 8 weeks) and five replicates. Soil temperature around the litterbags was used to derive equivalent decomposition rates at 20oC. The ratio of lignin plus phenolics over nitrogen was used as main litter quality indicator.ResultsDecomposition of fine tree roots was up to three times faster than that of aboveground litter with the same quality index measured in the same habitat. Root decomposition was slower in topsoils with recent volcanic ash, with a mean residence time extended by, on average, two weeks. Decomposition of roots of the ash-adapted native tree Parasponia rigida was especially rapid. ConclusionsFine root turnover contributes to the Corg accumulation that turns low-C volcanic ash into high-carbon andic soil and has relatively short necromass residence times.


Oecologia ◽  
2009 ◽  
Vol 162 (4) ◽  
pp. 1059-1069 ◽  
Author(s):  
Roy Hendrikus Antonius van Grunsven ◽  
Wim H. van der Putten ◽  
T. Martijn Bezemer ◽  
Elmar M. Veenendaal

2021 ◽  
Author(s):  
Rutger A. Wilschut ◽  
Mark van Kleunen

Abstract Aims Drought events can alter the composition of plant and soil communities, and are becoming increasingly common and severe due to climate change. However, how droughts affect plant-soil feedbacks is still poorly understood. Plants accumulate species-specific rhizosphere communities, and droughts may have varying impacts across plant species and soil biota. We therefore tested the hypothesis that drought alters plant-soil feedbacks differently among closely related plant species that differ in their preferences for soil moisture. Methods In a two-phase greenhouse experiment, we first conditioned grassland soil with seven Geranium species and, as controls, we conditioned soil with a grass species or left soil unplanted. In the second phase, we grew the Geranium species in conspecific, grass-conditioned and unplanted soil, maintained soil moisture at 5 %, 10 % or 20 % (w/w), and determined biomass responses after 35 days. Results Independent of conditioning, plants showed a weaker performance with decreasing soil moisture. Under the driest conditions, soil conditioning by conspecifics most negatively affected relative root weight in comparison to plants growing in unplanted control soil, while the effects of conspecific conditioning on relative root weights were species-specific when compared to plants grown in grass-conditioned control soil. Conclusions We conclude that decreased soil moisture modified plant-soil feedback effects on biomass allocation, and that these modifications acted in species-specific ways. However, drought effects on plant-soil feedbacks were subtle, and did not affect overall plant performance. Therefore, plant-soil feedback effects on plant performance during a drought event may be limited in comparison with the direct effects of drought.


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