Tracing silicon cycling in the Okavango Delta, a sub-tropical flood-pulse wetland using silicon isotopes

Summary, in English

Chemical weathering of silicate minerals releases elements into solution whereas the neoformation of secondary minerals

works in the opposite direction, potentially confounding estimates of silicate weathering rates. Silicon isotopes (d30Si) may be

a useful tool to investigate these processes. Here, we present 82 d30Si measurements from surface waters, pore waters, biogenic

silica (BSi), clays, sand and vegetation from the Okavango Delta, Botswana, a freshwater sub-tropical, flood-pulse wetland.

Hydrologically, the Okavango is dominated by evapotranspiration water losses to the atmosphere. It receives an annual pulse

of water that inundates seasonal floodplains, while river baseflow is sufficient to maintain a permanent floodplain. d30Si in

dissolved silica (DSi) in surface waters along a 300 km transect at near-peak flood show a limited range (0.36–1.19&), imply-

ing the Delta is well buffered by a balance of processes adding and removing DSi from the surface water. A key control on DSi

concentrations is the uptake, production of BSi and recycling of Si by aquatic vegetation, although the net isotopic effect is

necessarily small since all BSi re-dissolves on short timescales. In the sediments, BSi d30Si (n = 30) ranges from