OMZs are a consequence
of microbial respiration and can be hostile environments for marine life.
Not exact matches
They write, «We show that anaerobic microsites are important regulators
of soil carbon persistence, shifting
microbial metabolism to less efficient anaerobic
respiration and selectively protecting otherwise bioavailable, reduced organic compounds such as lipids and waxes from decomposition.
I also examine the partitioning
of soil
respiration into
microbial and root
respiration.
Estimates are that
microbial respiration will speed up as the soil warms, resulting in a net flux
of CO2 to the atmosphere.
One example is the global soil reservoir
of organic carbon (which is not a single «pool», but which is made up
of many components, some which are very labile (rapid turnover via
microbial and root
respiration) and some
of which are very long - lived (humic material).
Estimates are that
microbial respiration will speed up as the soil warms, resulting in a net flux
of CO2 to the atmosphere.
Responses are expressed through gross and net primary production,
microbial respiration, fire and insect disturbance, vegetation composition, species range expansion and contraction, surface energy balance and hydrology, active layer depth and permafrost thaw, and a range
of other inter-related variables.
Other effects
of SRM are expected to reduce soil
microbial respiration, enhancing carbon storage in soils too.
Carbon fixed into plants is then cycled through plant tissues, litter and soil carbon and can be released back into the atmosphere by plant,
microbial and animal
respiration and other processes (e.g. forest fires) on a very wide range
of time scales (seconds to millennia).
According to the paper, the results
of the radiocarbon data confirm that
microbial respiration of «old» carbon (carbon prior to nuclear tests in the 40s and 50s) has the potential to emit a significant amount
of carbon into the atmosphere.
The present paper presents a mathematical analysis
of a tipping point or runaway feedback that can arise when the heat from
microbial respiration is generated more rapidly than it can escape from the soil to the atmosphere.
Some
of this exchange is mediated by
microbial marine organisms through photosynthesis, in which carbon dioxide is converted into organic matter, and
respiration, in which the latter is metabolized.