The contribution of leaching to nutrient release from leaf litter of two emergent tree species in a Malaysian tropical peat swamp forest

Ostracode faunas changed in Lake Bonneville as the lake rose in the closed basin and became more dilute, then overflowed, and eventually returned to closed-basin hydrology; alkalinity (carbonate + bicarbonate) increased throughout the lake history. Fossil-ostracode faunas in marl deposited in the lake between about 30 and 13 cal ka allow reconstruction of these geochemical changes (as shown by R. M. Forester), and permit stratigraphic correlations within the large lake basin, including into the Sevier subbasin, which was connected to the main body of the lake but had different inflowing rivers. The first ostracode to appear in Lake Bonneville deposits at low altitudes is Limnocythere staplini; it was replaced by L. ceriotuberosa as the lake got larger and the water became more dilute and alkaline. Candona adunca and several species of Fabaeformiscandona mark the freshest-water phases. Cytherissa lacustris appeared in lake-margin settings after lake level dropped and cold, fresh groundwater began to discharge into the lake. Candona sp. cf. eriensis lived in the Sevier subbasin during the transgressive phase of the lake, but did not appear in the main body until late in the regressive phase. Limnocythere sappaensis, which requires high alkalinity, showed up late in the regressive phase in the main body when lake level was very low.