Terrestrial ecosystems and the global biogeochemical silica cycle

TLDR

The global silicon cycle has been largely studied through weathering and oceanic processes, overlooking the substantial terrestrial biogenic silica pool in plants and soils that fixes 60–200 Tmol yr⁻¹ and buffers riverine silicate fluxes, thereby influencing CO₂ sequestration and complicating weathering rate predictions. The study aims to evaluate how the terrestrial biogenic silica reservoir has shaped long‑term global silicon cycling and how human activities have altered both terrestrial and aquatic silicon pathways.

Abstract

Most research on the global Si cycle has focused nearly exclusively on weathering or the oceanic Si cycle and has not explored the complexity of the terrestrial biogeochemical cycle. The global biogeochemical Si cycle is of great interest because of its impact on global CO 2 concentrations through the combined processes of weathering of silicate minerals and transfer of CO 2 from the atmosphere to the lithosphere. A sizable pool of Si is contained as accumulations of amorphous silica, or biogenic silica (BSi), in living tissues of growing plants, known as phytoliths, and, after decomposition of organic material, as remains in the soil. The annual fixation of phytolith silica ranges from 60–200 Tmol yr −1 and rivals that fixed in the oceanic biogeochemical cycle (240 Tmol yr −1 ). Internal recycling of the phytolith pool is intense with riverine fluxes of dissolved silicate to the oceans buffered by the terrestrial biogeochemical Si cycle, challenging the ability of weathering models to predict rates of weathering and consequently, changes in global climate. Consideration must be given to the influence of the terrestrial BSi pool on variations in the global biogeochemical Si cycle over geologic time and the influence man has had on modifying both the terrestrial and aquatic biogeochemical cycles.