Silicon (Si) is the second‐most abundant element in the earth's crust. In the pedosphere,
however, huge spans of Si contents occur mainly caused by Si redistribution in soil profiles …

The glaciers of western Canada and the conterminous United States have dominantly
retreated since the end of the Little Ice Age (LIA) in the nineteenth century, although average …

Glaciers and Glaciation is the classic textbook for all students of glaciation. Stimulating and
accessible, it has established a reputation as a comprehensive and essential resource. In …

Understanding the controls on chemical weathering, especially of silicate minerals, remains
a major challenge, despite its importance in controlling the evolution of the Earth's surface …

During the Lomagundi Event, ca. 2.22 to 2.06 Ga, marine carbonates recorded the largest
and longest uninterrupted positive carbon isotope excursion, the earliest extensive marine …

Although variation in 87Sr/86Sr has been widely pursued as a tracer of provenance in
environmental studies, forensics, archeology and food traceability, accurate methods for …

The chemical weathering of silicate rocks can yield bicarbonate which is transported via
rivers to the ocean, followed by the deposition of carbonate, acting as a carbon sink on long …

Connections between glaciation, chemical weathering, and the global carbon cycle could
steer the evolution of global climate over geologic time, but even the directionality of …

Carbonate minerals constitute Earth's largest C reservoir. This reservoir is considered
unimportant to the global C cycle over long periods of time (eg,> 10 6 yrs) because it …

The main scope of this study is to investigate parameters controlling chemical weathering
rates for a large river system submitted to subarctic climate. More than 110 river water …