Short CommunicationPhytolith-occluded organic carbon as a mechanism for long-term carbon sequestration in a typical steppe: The predominant role of belowground productivity

- Occlusion of organic carbon in phytolith (phytOC) is a mechanism for long-term C sequestration.
- PhytOC content and production in the above and belowground parts of steppe plants were determined.
- PhytOC concentration was significantly higher in below than above ground plant parts.
- PhytOC production was at least one order of magnitude greater from below than above ground parts.
- Belowground part plays a dominant role in biogeochemical silica cycle and C sequestration.

Phytolith-occluded organic carbon (phytOC) has recently been demonstrated to be an important terrestrial carbon (C) fraction resistant to decomposition and thus has potential for long-term C sequestration. Existing studies show that plant leaves and sheath normally have high phytOC concentration, thus most of phytOC studies are limited to the aboveground plant parts. Grassland communities comprise herbaceous species, especially grasses and sedges which have relatively high concentrations of phytoliths, but the phytOC production from grassland, especially from its belowground part, is unknown. Here we determined the phytOC concentration in different parts of major plant species in a typical steppe grassland on the Mongolian Plateau, and estimated the phytolith C sequestration potential. We found that the phytOC concentration of major steppe species was significantly (p < 0.05) higher in belowground (0.67 g kg− 1) than aboveground biomass (0.20 g kg− 1) and that the belowground net primary productivity (BNPP) was 8-15 times the aboveground net primary productivity (ANPP). Consequently, the phytOC stock in belowground biomass (12.50 kg ha− 1) was about 40 times of that in aboveground biomass (0.31 kg ha− 1), and phytOC production flux from BNPP (8.1-15.8 kg ha− 1 yr− 1) was 25-51 times of that from ANPP. Our results indicate that BNPP plays a dominant role in the biogeochemical silica cycle and associated phytOC production in grassland ecosystems, and suggests that potential phytolith C sequestration of grasslands may be at least one order of magnitude greater than the previous estimation based on ANPP only. Our results emphasize the need for more research on phytolith and phytOC distribution and flux in both above and below ground plant parts for quantifying the phytolith C sequestration.

277