pjb05 wrote on Mar 22
nd, 2008 at 8:50pm:
Here's a study which suggests higher CO2 levels will increase phytoplankton growth:
(First of all I promise not to cut and paste, except from my own articles.)
Fine. We need studies like that to fine-tune our understanding of the process. So far nothing that you have said so far has denied the fact that the Ocean pH is falling. I mentioned calcification earlier. That refers to the reliance on marine organisms to deposit calcium carbonate from sea water.
OK, the obvious organisms that are being affected by ocean acidification include corals, crustaceans and even some tiny plant-like creatures called coccolithophores which form calcium carbonate skeletons and drive a pump, essentially, where CO2 is absorbed by the ocean. They too are under threat. In the Southern Ocean, coccolithophores have been shown to be responsible for up to 30% of the CO2 absorption.
Then there are increasing cases of very interesting new diseases in crabs and lobsters which are basically caused because things are not calcifying anymore, and they're not calcifying at a rate that keeps up with the processes that take away that calcium carbonate.
Fish have a single crystal of calcium carbonate beneath their brain. They're called otiliths, and they're used for balance. Basically fish can't survive without them.
Otiliths grow during the lifetime of the fish if the conditions are right for the deposition of calcium carbonate. As the pH decreases, the rate of calcification also decreases.
It's not the absolute values that are important, rather the rate of change, and the somewhat different conditions that exist today compared with the past. We're talking extremely high human population, an almost unprecedented rate of change in atmospheric CO2 which is demonstratively derived from fossil fuels (from the isotope ratios) and we're talking about changes that are happening too fast for ecosystems to adapt.
I'll elaborate further, but first let's put temperature rise in some kind of perspective.
The most recent work on grain for example yields indicates that the small amount of warming that has already occurred has reduced what the yields are today over what they would have been just based on technological change. In other words the yields haven't been going down but they haven't been going up as fast as they might have because of the problems of crop varieties having thermal limits on them, particularly the world's feeding base which of course are those three famous grains- Wheat Rice and Corn.
Taking rice as an example - it's within two or three degrees of its limit over most of Asia.
http://news.bbc.co.uk/1/hi/sci/tech/1645590.stmWhat this is all about is averting human disasters. We currently have 6.77 billion people and counting. It's all very well to talk about the geological past, mass extinctions included, but the important issue is the here and now. What will be the effects on the staple foods now - fish stocks, rice, wheat and corn?
Of course, we should be able to breed new strains that will be able to do just great when the planet is 6°C or 7°C hotter. There are actually such seed banks, but what you do with seed banks is that you select organisms for storage attributes not for their ability to reproduce under new climatic conditions. The only way to save the genetic diversity of crops is to keep planting them out in diverse circumstances and diverse strains and subsidise farmers to grow less productive ones so you have the diversity safe.
However, they're not doing that - they're not even thinking about it over most of the world.
Times have changed since the beginning of the Eocene, and even since the medieval period.
- like the fact that we have 6.77 billion people instead of 150 Million during Medieval times, or the fact that we now have 1/100 of the Tropical rainforest that we did then, and that fish stocks are down by 99% on Viking days. The buffering effect of 'Gaia' has certainly declined considerably since the peak of the Eemian interglacial, 125,000 years ago, when global temperatures were higher than today and sea levels were some 4-6 metres higher. The current atmospheric carbon dioxide is now 383 ppm compared with a peak of 225ppm at the height of the Eemian.
The last time we had 383 ppm CO2 in the atmosphere was just after the Paleocene Eocene Thermal Maximum (PETM). Now that makes for some very interesting reading.