Geochemists have long considered Li isotope composition of marine carbonates as one of
the most straightforward oceanic archives, tracing climate regulation by continental silicate …

In the Precambrian, reverse weathering—a process consuming oceanic silica, metal cations
and alkalinity to form marine clays—was a key control of the long-term carbon cycle …

Lithium and its isotopes can provide information on continental silicate weathering, which is
the primary natural drawdown process of atmospheric CO2 and a major control on climate …

Early marine and meteoric diagenesis is commonly proposed to alter the primary
geochemical signals of shallow-marine carbonates, hindering their use as a reliable archive …

Records of the lithium isotopic composition of seawater (δ 7 Li sw), preserved in the lithium
isotopic composition of shallow-marine carbonate sediments (δ 7 Li carb), provide …

Lithium isotope (δ 7 Li) variations in marine carbonate sediments and rocks have been
widely used to reconstruct global seawater Li isotope compositions and then trace the paleo …

Lithium isotopic (δ 7 Li) and elemental concentrations of pore fluids and carbonates from
IODP Site U1338 Hole A (eastern equatorial Pacific Ocean) suggest that clay authigenesis …

Lithium production has dramatically increased over the past decade, and the first cases of
environmental Li pollution have been recently reported in urban and mining regions. While …

Abstract The terminal Ediacaran (∼ 551–541 Ma) was a critical period in Earth's history
witnessing the coupled evolution of tectonism, climate, marine environment, and …

The lithium isotope composition (δ7Li) of seawater records important information on the
evolution of the carbon and silicon cycles over geologic time. Here we report δ7Li values in …