The dynamics of biologic Si cycling in grassland ecosystems are largely unknown and likely to impact mineral weathering rates regionally and diatom productivity globally; key regulatory processes in the global Si cycle are closely tied to the global carbon cycle. Across a bioclimatic sequence spanning major grassland ecosystems in the Great Plains, soil biogenic silica depth distributions are similar to that of soil organic carbon; however, unlike soil organic carbon, quantities of soil biogenic silica decrease with increasing precipitation, despite an increase in annual biogenic inputs through litterfall across the same gradient. Though comprising only 1–3% of the total Si pool, faster turnover of biogenic Si and annual cycling by grasses should positively impact mineral dissolution. Our results suggest that the largest reservoir of biogenic Si in terrestrial ecosystems resides in soils, and emphasize the potential significance of grasslands in the global biogeochemical cycle of Si.
Digital Object Identifier (DOI)
Blecker, S. W.; McCulley, Rebecca L.; Chadwick, O. A.; and Kelly, E. F., "Biologic Cycling of Silica across a Grassland Bioclimosequence" (2006). Plant and Soil Sciences Faculty Publications. 39.
gbc1304-sup-0002-ts01.txt (1 kB)
Table S1. SGS short grass site.
gbc1304-sup-0003-ts02.txt (1 kB)
Table S2. Arikaree short grass site.
gbc1304-sup-0004-ts03.txt (1 kB)
Table S3. Smokey Valley mixed grass site.
gbc1304-sup-0005-ts04.txt (1 kB)
Table S4. Hays mixed grass site.
gbc1304-sup-0006-ts05.txt (1 kB)
Table S5. Wilson mixed grass site.
gbc1304-sup-0007-ts06.txt (1 kB)
Table S6. Konza tall grass site.
gbc1304-sup-0008-ts07.txt (1 kB)
Table S7. WKT tall grass site.
gbc1304-sup-0009-t01.txt (1 kB)
Tab-delimited Table 1.
gbc1304-sup-0010-t02.txt (1 kB)
Tab-delimited Table 2.
gbc1304-sup-0011-t03.txt (1 kB)
Tab-delimited Table 3.