Mountain building results in high erosion rates and the interaction of rocks with the
atmosphere, water and life. Carbon transfers that result from increased erosion could control …

The silicon isotope composition of biogenic silica (δ 30 Si BSi) in the ocean is a function of
the δ 30 Si of the available dissolved Si (DSi; H 2 SiO 4), the degree of utilisation of the …

The principal nature-based solution for offsetting relative sea-level rise in the Ganges-
Brahmaputra delta is the unabated delivery, dispersal, and deposition of the rivers'~ 1 billion …

Silicate weathering is critical to global carbon cycle and climate change, and has attracted
considerable attention in Earth science studies. Chemical weathering intensity evaluation …

Water plays a critical role in erosion and sediment transport and this relationship is most
evident in the hyperarid Atacama Desert of Northern Chile, a region characterized by …

Geogenic enrichment of arsenic (As) in groundwater has been a topic of worldwide concern
over the past several decades due to the severe health threat to an estimated over one …

Abstract Reconstructing the Plio-Pleistocene sedimentary history of the Yellow Sea, is
important for understanding the long-term influence of the Yellow River (Huanghe) and/or …

During the Holocene there has been a gradual increase in the influence of humans on Earth
systems. High-resolution sedimentary records can help us to assess how erosion and …

Atmospheric CO 2 and global climate are closely coupled. Since 800 ka CO 2
concentrations have been up to 50% higher during interglacial compared to glacial periods …

Sediment accumulation rates and thermal trackers suggest a substantial and global
increase in erosion rates over the past few million years. That increase is commonly …