He sort of knows me for some time here. Some things get known. I prefer the term ocean scientist myself.
If so, he should be able to explain
this:
What's there to explain? Forams exist, they form shells, of different types. So? You were talking about chalk deposits, which are predominantly formed by coccoliths.
Yes, one experiment reported increase in calcification. Most show a decrease in calcification. That's biology for you, the same exact group can make two identical experiments and come out with different results. However, my position stands: from what we know, with enough acidification, coccoliths will stop producing shells.
Recall: "Can you guess what happens to the CO2 when it gets "stored" in the ocean?"
Dissolved CO2 is biologically sequestered. In a talk at the University of Hawaii, Richard Alley argued against the strategy of CO2 mitigation through oceanic biological sequestration with oceanic fertilization and precipitation (by, e.g., forams and other organisms with calcite shells) on the grounds that it would give us only 200 years. That's a long time to find a better solution.
I very much doubt that Prof. Alley stressed what I bolded. The strategy of ocean fertilization does not, in any shape or form, depend on the sequestration of CO2 by calcifying organisms.
The whole strategy is based on the existence of eddies of high-nutrient, low chlorophyll waters. When those waters are fertilized by iron, a lerge bloom of phytoplankton occurs. This will normally be diatoms. as the bloom dies out it starts aggregating, and creating large, heavier particles that will settle to the ocean floor. Since this is done in the open ocean, if all of the settled carbon gets remineralized, it will still take some 2000 years to come in contact with the atmosphere again. However, most of the bloom will be consumed in the upper layer of the ocean, meaning that on average in the next 200 years that water will be in contact with the atmosphere. Those are the 200 years we're buying.
More normal objections relate to the accumulation of high-carbon loads in a small area, creating anoxic patches that can originate substantial amounts of methane. If that methane bubbles up and is above the level that can be by free-living methanotrophs, we are replacing one GHG withanother, more potent one.
My personal view is that if we let the whale population recover, their role as iron concentrators and ocean fertilizers will not have to be outsourced. We will observe higher ocean productivities, and the ocean will start taking up much more carbon that at the present. There will be no chalk deposits in 100M years, though.
There's a report button, if you want to call the mods.
What happened to "Address the argument, not the arguer"?
I will refrain from further superfluous comments. I will however thank you if you start paying attention to what I write, instead of creating strawmen.