摘要：Abstract The solid earth plays a major role in controlling Earth’s surface climate. Volcanic degassing of carbon dioxide (CO 2 ) and silicate chemical weathering are known to regulate the evolution of climate on a geologic timescale (> 10 6 yr), but the relationship between the solid earth and the shorter ( 10 6 yr) causality that has been conventionally considered.
其他摘要：Abstract The solid earth plays a major role in controlling Earth’s surface climate. Volcanic degassing of carbon dioxide (CO 2 ) and silicate chemical weathering are known to regulate the evolution of climate on a geologic timescale (> 10 6 yr), but the relationship between the solid earth and the shorter ( 10 6 yr) causality that has been conventionally considered.
