Recent technological advancement has revolutionized the field of non-traditional stable
metal and metalloid isotopes for their wide applications for the study of earth surface …

Large igneous province eruptions and their carbon emissions often coincide with, and are
hypothesized to have driven, severe environmental perturbations in the geological past …

The mid-Proterozoic, spanning 1.8 to 0.8 billion years ago, is recognized as a phase of
marine anoxia, low marine primary productivity (MPP), and constrained eukaryotic …

The drivers of the Middle Eocene Climatic Optimum (MECO) remain enigmatic. Here we
report a high-resolution terrestrial MECO record from the Bohai Bay Basin, eastern China …

To investigate the impact of riverine discharge and weathering intensity on lithium isotopes
(δ 7 Li) in a mono-lithological terrain, this study examines the dissolved load and leached …

Abstract The Ordovician-Silurian transition (OST) was characterised by climatic fluctuations
(warming in the Katian and glaciation in the Hirnantian) and mass extinctions. However, the …

The study of lithium isotopic (δ 7 Li) signatures in sedimentary deposits has become a
powerful tool to infer past silicate weathering regimes, thus informing our knowledge of the …

The understanding of silicate weathering and its role as a sink for atmospheric CO2 is
important to get a better insight into how the Earth shifts from warm to cool climates. The …

Abstract The Middle Eocene Climatic Optimum (MECO) is a transient warming episode
during an interval of long-term Cenozoic cooling that is recorded in deep-sea marine …

Recent evidence from marine sedimentary rocks suggests that clay minerals were important
in the supply of bioessential nutrients to seawater at the end of the Sturtian Snowball Earth …