Phytolith-occluded carbon sequestration potential in three major steppe
types along a precipitation gradient in Northern China
Abstract
Phytolith-occluded carbon (PhytOC) is an important long-term stable
carbon fraction in grassland ecosystems, and plays a promising role in
global carbon sequestration. Determination of the PhytOC traits of
different plants in major grassland types is crucial for precisely
assessing their PhytOC sequestration potential. Precipitation is the
predominant factor in controlling net primary productivity (NPP) and
species composition of the semiarid steppe grasslands. We selected three
representative steppe communities of desert steppe, dry typical steppe
and wet typical steppe in Northern Grasslands of China along a
precipitation gradient, to investigate their species composition,
biomass production and PhytOC content for quantifying its long-term
carbon sequestration potential. Our results showed that (i) the
phytolith and PhytOC contents in plants differed significantly among
species, with dominant grass and sedge species having relatively high
contents, and the contents are significantly higher in below- than the
aboveground parts. (ii) The phytolith contents of plant communities were
16.68, 17.94 and 15.85 g kg-1 in the above- and 85.44, 58.73 and 76.94 g
kg-1 in the belowground biomass of desert steppe, dry typical steppe and
wet typical steppe, respectively; and the PhytOC contents were 0.68,
0.48 and 0.59 g kg-1 in the above- and 1.11, 0.72 and 1.02 g kg-1 in the
belowground biomass of the three steppe types. (iii) Climatic factors
affected phytolith and PhytOC production of steppe communities mainly
through altering plant production, whereas their effects on phytolith
and PhytOC contents were relatively small. Plant aboveground biomass and
PhytOC content were strongly associated with the current-year climate
and soil bio-available Si content; while plant belowground biomass and
PhytOC content were relatively stable, and their variation across the
sites is in accordance with the spatial variation in the long-term means
of climatic and soil factors, reflecting the perenniality of plant
belowground part.