There are at least ~ 1500 billion tons
of organic carbon in permafrost zone soils, almost twice as much as currently exists in the atmosphere.
They then used those measurements to calculate the
amount of organic carbon stored in permafrost at each site and in areas with similar terrain.
The oceans and forests are a much greater
source of organic carbon than anthropogenic emissions and they change naturally as evidenced by the annual cycle.
The dimming was shown to be accompanied by significant atmospheric absorption of solar radiation by black and brown carbon (a
form of organic carbon).
The study will also investigate the types
of organic carbon present in the ground to help understand how it influences uranium behavior.
We found that cells produced more calcium carbonate under future ocean conditions, but had the same amount
of organic carbon as in present conditions.
The
accumulation of organic carbon in the deep ocean would limit the release of carbon into the atmosphere as CO2, limiting further warming by this greenhouse gas.
Arbuscular mycorrhizal fungi live in symbiosis with plant roots and are able to store up to 70 percent
of organic carbon from leaf litter.
Regarding the Paleocene - Eocene event itself, the field seems to be coming around to the idea that it had something to do with a greatly accelerated oxidation
of organic carbon stored on land, perhaps associated with the drying up of interior shallow seaways.
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).
«The evolutionary innovation and expansion of land biota could permanently increase [chemical] weathering intensity and [clay] formation, establishing a new level
of organic carbon burial and oxygen accumulation.»
Even in the absence of oxygen, the research team found that the
respiration of organic carbon occurring in the anoxic waters of the Black Sea is not as different from that occurring in the deep ocean.
And the agency at work in this unexpected process could be biology: the researchers found evidence that tiny microbes in the mountain soils were consuming sources
of organic carbon trapped in the rock, and releasing CO2 into the atmosphere.
Permafrost — subsurface soil that remains frozen year - round — covers nearly 19 million square kilometers of the circumpolar Arctic and is thought to contain around 1700 billion
tons of organic carbon [Schuur and Abbott, 2011].
Matyas Ripszam has also examined the effects of higher temperature and different
concentration of organic carbon content on the distribution of pollutants in modelled real - life marine ecosystems, so called mesocosms.
The opportunity to pour carbon back into the soil exists because farming over the past century has depleted its
levels of organic carbon, Rice notes.
Lead author PhD student Adam Hejnowicz said: «Seagrass meadows could play a vital role in combating climate change as they are regarded as a net global sink for carbon.They have the capacity to bury significant
deposits of organic carbon beneath the sediment, up to many metres thick in places and over millenary time scales.»
Using samples collected from the Liwu and Wulu river basins in Taiwan, which run off the central range, the team compared the radiocarbon
profiles of organic carbon in the rock with the soil directly above it.
«Our original plan was to understand the
fate of organic carbon released from viral lysis of picocyanobacteria» said Feng Chen.
«After examining rocks 450 million years old or older, we believe the drop was caused by a massive burial
of organic carbon during the time period,» Quinton said.
In the spirit of an ongoing series of new discoveries which could be titled «whoops, things are a lot worse than we thought» Yahoo News / AFP is reporting that according to new research coming out to the University of Alaska Fairbanks, and published in Nature Geoscience, the
stock of organic carbon stored in Arctic permafrost is 60 % higher than previous estimates.
Researchers in the US have calculated that, thanks to climate change, melting glaciers will have spilled an extra 15 million
tonnes of organic carbon into the seas by 2050.
They found that erosion of permafrost releases a total of 36 million
kilograms of organic carbon from the Yukon Coastal Plain into the Beaufort Sea annually.
The study included carbon dioxide emissions from burning fossil fuels and producing chemicals and cement but excluded emissions from activities like deforestation and logging, forest and peat fires, the decay of biomass after burning and
decomposition of organic carbon in drained peat soils.
They key, scientists explain, lies in ensuring that a sufficiently high enough percentage
of organic carbon produced during the blooms reaches middle - depth waters, at which point it would remain in deeper underwater currents for decades.
However, the toys themselves provide a source of nutrients: the plastic materials — often low - quality polymers — release substantial amounts
of organic carbon compounds.
As plants in and around the lake grow larger and / or proliferate, the amount
of organic carbon available when they die and the rate at which they break down in soil increases.
Given the right conditions, this genetic acquisition set the stage for the microbe to undergo a dramatic growth spurt, rapidly consuming a vast
reserve of organic carbon in the ocean sediments.
We have shown that hydrothermal vent fluids contain almost
none of the organic carbon which accumulates in the oceans, which means that vents are a sink for this unreactive «stored» carbon.»
Dr Jeff Hawkes, the lead author of this study, from the NOC said: «There has been a long outstanding question about whether hydrothermal vents are a source or
sink of organic carbon to the oceans.
Co-author Professor Eric Achterberg, from the University of Southampton, said: «The beauty of this approach is that with both field and laboratory experiments we were able to prove how the mechanisms operate for the
removal of organic carbon in the deep ocean.»
«The
presence of organic carbon at or near the Martian surface provides a potential nutrient source for putative life,» says co-author Francis McCubbin.
«Insights into oceanic carbon transformations — including the oxygen
dependence of organic carbon respiration — can be gained by studying the anoxic Black Sea,» said Margolin.