The glaciation was favored by an interval when the Earth's orbit favored cool summers but
Oxygen isotope ratio cycle marker changes were too large to be explained by Antarctic ice - sheet growth alone indicating an ice age of some size.
Not exact matches
When the researchers analyzed the
oxygen isotope ratios over the past 8,000 years, they found that the jet stream became wavier — with colder Eastern winter weather and warmer Western winter weather — on about a 4,000 - year
cycle.
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.
Carbon and
oxygen isotope ratios both shift at the same boundary; the former shows disruption of the carbon
cycle, while the latter shows an abrupt warming of about 6 degrees.