The accumulation of methane hydrate in marine sediments is controlled by a number of
physical and biogeochemical parameters including the thickness of the gas hydrate stability …

A new box model for the global carbon-calcium-strontium cycle is developed to simulate the
evolution of Cretaceous and Cenozoic seawater and atmosphere. The model accounts for …

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 …

The silicate rock weathering followed by the formation of carbonate rocks in the ocean,
transfers CO2 from the atmosphere to the lithosphere. This CO2 uptake plays a major role in …

Because there remains a lack of knowledge about the spatially explicit distribution of
chemical weathering rates at the global scale, a model that considers prominent first-order …

The debris-rich basal ice layers of a high Arctic glacier were shown to contain metabolically
diverse microbes that could be cultured oligotrophically at low temperatures (0.3 to 4° C) …

A new digital map of the lithology of the continental surfaces is proposed in vector mode (n≈
8300, reaggregated at 0.5°× 0.5° resolution) for 15 rock types (plus water and ice) targeted …

On geological time‐scales (≥ 106 years), the global geochemical cycles of carbon and
silicon are coupled by the drawdown of atmospheric CO2 through chemical weathering of …

A negative feedback between silicate weathering rates and climate is hypothesized to play a
central role in moderating atmospheric CO 2 concentrations on geologic timescales …

Using the data of the CAMREX project (1982–1984) on the water geochemistry of the
Amazon river and its main tributaries, it was possible to assess the silicate rock weathering …