Such rock, known as basalt, might be better than other sites, such as deep saline aquifers or nearly empty oil wells, because the rock not only stores CO2 but also over a relatively short period of
years forms carbonate minerals out of it — in other words, limestone.
Not exact matches
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What's more, the
carbonates appear in rocks that seem to be younger — between 3.5 billion and 3.9 billion
years old — than those in which the sulphates seen by Opportunity
formed.
The team examined a range of fossils unearthed from limestone rocks in Siberia, which
formed millions of
years ago from seawater with high levels of calcium
carbonate.
And so now there are something like 4,400 on Earth which is at least as far as we can see completely unique, and there was a period which Dr. Hazen called red earth about a couple of billion, two billion
years ago, when life first gets going when there's some, you know, early
forms of life and about 2,000 or so minerals arise [there], microorganisms make sheaths of minerals like calcium
carbonate that we now see in animals with shells.
(Either way, the chance is very small that a carbon atom in the ocean will be incorporated into organic matter or chemically combined with a
carbonate cation to
form calcium
carbonate that will end up sequestered in sediments, where it might remain for hundreds of millions of
years.)
Researchers can only speculate about how the
carbonate globules in ALH84001
formed, billions of
years ago and millions of miles away.
Also over 10s - 1,000 s of
years the dissolved CO2 reacts with rock minerals to
form carbonates - immobilising the CO2 further (we can do some of these experiments in the lab and we observe them in nature).
A
year - long laboratory study of coccolithophores — an important type of phytoplankton — found they remained capable of
forming their calcium
carbonate skeletons even in warmer, more acidic water.
All the CO2 we emit will finally end up either in the ocean and then in the
form of
carbonate rocks or in the
form of biomass and then possibly part of it in the
form of fossil hydrocarbons in a 100 millions of
years.
At some times of
year, acidification has already reached a critical threshold for organisms living on Alaska's continental shelves.145 Certain algae and animals that
form shells (such as clams, oysters, and crab) use
carbonate minerals (aragonite and calcite) that dissolve below that threshold.
``... Southern Ocean surface waters will begin to become undersaturated with respect to aragonite, a metastable
form of calcium
carbonate, by the
year 2050.