Laterisation is an uncontrolled natural process that was influenced by the synergetic effect of
atmospheric and geological conditions. Laterite soil 'leached residue'is the resultant from the …

The cycling of iron (Fe) is often closely linked with that of carbon, nitrogen, phosphorus and
manganese. Therefore, alterations in the Fe cycle may be indicative of concurrent overall …

Iron (Fe) isotopes can effectively unveil the Fe cycle mechanisms under redox and biological
conditions during the weathering and pedogenic processes. Fe contents and Fe isotope …

Significant iron (Fe) loss can occur during continental weathering and efflux to the ocean via
runoff, historically affecting global Fe cycling and marine ecosystems. Here, we report …

Weathering is a key process controlling V transport from the continental crust to the
hydrosphere. To understand V behavior during chemical weathering, we investigated the …

Zinc isotopes have been increasingly utilized as a proxy for (bio) geochemical cycles of
nutrient Zn in the ecosystem like soils, but the behavior and mechanism of Zn isotope …

Oceanic element inventories derived from marine sedimentary rocks place important
constraints on oxidative continental weathering in deep time, but there remains a scarcity in …

Goethite (α-FeOOH) is a source and sink for trace elements in surficial environments. Its
elemental and isotopic composition may be perturbed during recrystallization, particularly …

Several recent studies have reported a strong association between Sc and goethite (α-
FeOOH) in synthetic analogs and natural samples. However, the mechanism of Sc …

A paddy soil chronosequence consisting of five profiles derived from calcareous marine
sediments with cultivation history from 0 to 1000 years was studied to understand the …