When the jet stream got loopy In order to track the jet stream's behavior thousands of years ago, Bowen and his fellow researchers looked
at oxygen isotope ratios from lake cores and cave formations in the eastern and western United States.
Not exact matches
The
ratio of
oxygen isotopes in seawater depends on the water temperature; the value of this
ratio at any point in evolutionary time is «frozen» into the chemical composition of certain marine fossils.
They then compared the
oxygen isotope ratio in Yonderup dripwater with that predicted by a model (which simulated the dripwater δ18O based on measurements of rainwater δ18O), as well as that measured
at a different cave in the region.
Nevertheless, some scientists claim that
ratios of
oxygen isotopes in marine fossils from the east coast of the US indicate that the Antarctic ice sheet melted
at least partially during the Pliocene.
Environmental scientist Suzanna Richter and plant physiological ecologist Brent Helliker, both
at the University of Pennsylvania, measured the
ratio of two
isotopes of
oxygen — rarer
oxygen - 18 and more common
oxygen - 16 — in samples of wood.
Back
at their Georgia Tech lab, they analyzed the stalagmites for the
ratio of
oxygen isotopes contained in samples of calcium carbonate, the material from which the stalagmites were formed.
The analysis below used the
ratio of
oxygen isotopes in the stalagmites to estimate the water temperature
at the time they were formed.
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.
Looking
at the isotopic record from the PETM, scientists see both carbon and
oxygen isotope ratios spiking in exactly the way we expect to see in the Anthropocene record.