Throughout most of Earth's geological history, its paleoclimate has remained hospitable to life—largely thanks to continental silicate weathering, which acts as a long-term planetary thermostat.
On a banana plantation in rural Australia, a second-generation farming family spreads crushed volcanic rock between rows of ripening fruit. Eight thousand kilometers away, two young men in central ...
Cover -- Title Page -- Copyright Page -- Contents -- Contributors -- Preface -- Acknowledgments -- Part I Biological Weathering -- Chapter 1 Biological Weathering in ...