«We're looking at changes in
zircon production on various continents throughout Earth's history and seeing how the changes correspond with the various icehouse and greenhouse transitions,» McKenzie said.
«Ultimately, we find that during intervals of high
zircon production we have greenhouse conditions, and as
zircon production diminishes, we see a shift into our icehouse conditions.»
Not exact matches
To better understand the cycle of magma
production, the researchers analyzed oxygen isotope ratios in quartz and
zircon, water - and heat - resistant minerals, from volcanic rocks in the Yellowstone caldera.