Earlier this month I gave a seminar at the University of California Santa Cruz, Department of Earth & Planetary Sciences, in their Whole Earth Seminar series. A very enjoyable experience. Their campus is a redwood forest, and the people were very welcoming and interested. Though, I maybe should have talked about shells instead of hydrothermal vents, as that was apparently how they stumbled upon my work.
So how do you get a climate record from a shell or a coral? Well, a lot of organisms make growth bands like trees. And when looking at these bands one might see differences in width. Maybe the organism grew faster when temperatures were high, or when there was a lot of rain. So these growth bands are then effectively a record of temperature or rainfall amounts through time. But it goes further. Apart from the width of growth bands, we can look at their chemistry. The chemical composition of shells, or tree rings, or corals, can actually vary with temperature, or with the chemical composition of of the water that they live in.
When organisms become old enough to give a very long record of the past, or when we use shells from archaeological finds, this enables reconstruction of the climate far back in time, when there were no instrumental measurements. And that’s interesting, because it’s fun to find out about the history of our planet, but also because we need that information to understand current climate and model the future.