This is balanced by an equivalent amount that is removed by
chemical weathering of rocks.
Life on land, argues Schwartzman, has intensified
the chemical weathering of rocks such that carbon dioxide has been removed from the atmosphere and the surface temperature of the Earth has remained cooler than if life had not been present - a kind of inverted global warming.
Working with Professors Joydip Mukhopadhyay and Gautam Ghosh and other colleagues from the Presidency University in Kolkata, India, the geologists found evidence for
chemical weathering of rocks leading to soil formation that occurred in the presence of O2.
The mighty winds coming from the sea causes a big part to the displacement of minerals and the instinctive and
chemical weathering of this rock formation.
Not exact matches
For example,
rock records
of an isotope
of strontium — 87Sr — seem to show an increase in so - called
chemical weathering, or
weathering that is not simply the result
of rain or other natural but not life - related processes.
To understand
weathering, water quality, and soil formation on Earth and Mars, look no further than associate professor
of geoscience Elisabeth «Libby» Hausrath, who investigates
chemical interactions between water and
rocks as well as the plant and microbial influences on those reactions.
Plants are major contributors to the
chemical weathering of continental
rocks, a key process in the carbon cycle that regulates Earth's atmosphere and climate over millions
of years.
This
chemical weathering process is too slow to damp out shorter - term fluctuations, and there are some complexities — glaciation can enhance the mechanical erosion that provides surface area for
chemical weathering (some
of which may be realized after a time delay — ie when the subsequent warming occurs — dramatically snow in a Snowball Earth scenario, where the frigid conditions essentially shut down all
chemical weathering, allowing CO2 to build up to the point where it thaws the equatorial region, at which point runaway albedo feedback drives the Earth into a carbonic acid sauna, which ends via rapid carbonate
rock formation), while lower sea level may increase the oxidation
of organic C in sediments but also provide more land surface for erosion... etc..
And outside the energy sector: Biological CO2 capture via photosynthesis and storage in ecosystems (e.g. forests, grasslands, wetlands, oceans) and / or agricultural lands (e.g. soils, biomass); and
chemical CO2 capture via enhanced
weathering of rocks that natural react (albeit quite slowly) with CO2 in the air.
For decades, it has been a given that heavy rainfall on steep mountain slopes is likely to chemically
weather the exposed
rock and precipitate a
chemical reaction that ends with carbonate minerals on the ground and with less
of the greenhouse gas carbon dioxide in the atmosphere.
«The rest is removed by slower processes that take up to several hundreds
of thousands
of years, including
chemical weathering and
rock formation.