Global Change Biology · 2017 · 100 citations · 34 references
Life SciencesBotanyPlant BiologyNutrient CyclingPlant EcologyTerrestrial EcologyBiomass AccumulationCarbon CycleEcosystem MetabolismPlant-nutrient CyclingPlant-soil InteractionsPlant-soil Nutrient InteractionsOrganic Carbon CyclingPlant Nutrient FeedbacksSiliconSilicon CycleSilicon LimitationTerrestrial Carbon CycleTerrestrial Carbon Fluxes
Current climate and land-use changes affect regional and global cycles of silicon (Si), with yet uncertain consequences for ecosystems. The key role of Si in marine ecology by controlling algae growth is well recognized but research on terrestrial ecosystems neglected Si since not considered an essential plant nutrient. However, grasses and various other plants accumulate large amounts of Si, and recently it has been hypothesized that incorporation of Si as a structural plant component may substitute for the energetically more expensive biosynthesis of lignin. Herein, we provide evidence supporting this hypothesis. We demonstrate that in straw of rice (Oryza sativa) deriving from a large geographic gradient across South-East Asia, the Si concentrations (ranging from 1.6% to 10.7%) are negatively related to the concentrations of carbon (31.3% to 42.5%) and lignin-derived phenols (32 to 102 mg/g carbon). Less lignin may explain results of previous studies that Si-rich straw decomposes faster. Hence, Si seems a significant but hardly recognized factor in organic carbon cycling through grasslands and other ecosystems dominated by Si-accumulating plants.
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Persistence of soil organic matter as an ecosystem property
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