More on marine algae etc. Of course, one does not need to pyrolyse the (oil expressed) algae into charcoal. Maybe fertilising the growth of coccolithophores would be even quicker for Branson. Chalk is formed in shallow waters by the gradual accumulation of the calcite mineral remains of phytoplanton micro-organisms (coccolithophores), over millions of years. Chalk is a very stable form of carbon sequestration... BTW I was surprised to see that the ocean Ph is already decreasing in line with the increased levels of CO2 and that this may get to a point where it interferes with the natural sequestration of atmospheric CO2 by coccolithophores thus acting as a rather serious positive feedback effect. To those who worry about unstoppable climate change happening whether we like it or not, I thought (correct me if I am wrong) that the normal expectation was that Earth should have been cooling down, heading towards the next glacial period? The fact that temperatures seem to be increasing holds out the promise that we can balance our emissions of CO2 etc to a lower optimum level that stabilises our climate and prevents the slide into an ice age. Or not - who knows?

Nick Palmer


Reply via email to