Our previous understanding of how the Antarctic Ice Sheet responded to warming at the end of the last ice age 10 to 20 thousand years ago was based on only a few ocean sediment cores. From sediment cores in the North Atlantic we have been able to piece together a decent map of how and…
A gigaton per year in the Marcellus Shale alone? Findings from the University of Virginia show we can permanently and safely dispose of much larger amounts of CO2 than previously understood using played out fracked wells. Once pumped in, most of it the CO2 does not come back out. It is captured by kerogens in shale….
