Conservation of Vital Ecosystems
I think one of the most important parts of the biological world to conserve is the carbon sinks of the Arctic. A recent expert assessment by scientists from the Permafrost Carbon Network, published in Nature, concluded that as much as 5%-15% of the terrestrial permafrost carbon pool is vulnerable to release in the form of greenhouse gases during this century. Stored over millennia in the Earth’s high latitudes, permafrost contains twice as much carbon as is currently in the atmosphere. As that region warms, permafrost will become vulnerable to a heightened rate of decomposition, resulting in a potentially enormous release of carbon dioxide to the atmosphere. It has been estimated that with continued warming, releases of carbon from microbial decay and other sources will overwhelm the capacity for plant carbon uptake in the Arctic, leading to a switch to net carbon emissions from permafrost ecosystems to the atmosphere possibly by the middle of the 21st century. Strengthening the northern carbon sink could help to curb rising air temperatures. A weakening of the sink would only worsen the global warming already taking place. The Arctic switching from a sink to a source would cause warming increases to become more rapid, which will further increase emissions, accelerating climate change in a self-reinforcing warming cycle. Though increased carbon emissions are the most pressing issue, there is also the threat of abnormally high temperatures thawing permafrost containing long dormant microbes, which could cause disease. Some researchers cite the concern of the diseases from thawing human and animal remains getting into groundwater that people then drink, or spreading through other ways.
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