The continental glaciations of the Pleistocene left signatures on the landscape in the form of glacial deposits and landforms; however, the best knowledge of the magnitude and timing of the various glacial and interglacial periods comes
from oxygen isotope records in ocean sediments.
Paleo temperatures
from oxygen isotope ratios from the greenland ice cores show that a temperature increase of 0.7 °C will not bring the current temperature up to the level of the Medieval Warm Period let alone the Roman optimum and the MInoan Warm period which were both warmer than the medieval warm period.
A study by Thomas, Dennis et al 2009 [8] derived a high resolution temperature proxy record
from oxygen isotope ratios from the ice core.
Calcareous nannofossils from approximately the past 7000 yr of the Holocene and
from oxygen isotope stage 5 are present at 39 analyzed sites in the central Arctic Ocean.
Figure 1: Temperature anomaly calculated
from oxygen isotope composition.
Here, we present a record of Holocene glacial ice discharge, derived
from the oxygen isotope composition of marine diatoms from Palmer Deep along the west Antarctic Peninsula continental margin.
The record tells the story of the sudden release of an isotopically light source of carbon, triggering a fast warming in the deep sea of about 5 degrees C. Both the carbon isotope signal and the temperature (inferred
from oxygen isotopes) then relaxed back toward their initial values in about 100,000 years.
These physical temperature measurements help calibrate the temperature record scientists obtain
from oxygen isotopes.
Holocene hydrologic balance of tropical South America
from oxygen isotopes of lake sediment opal, Venezuelan Andes.
Although a previous estimate based on this approach yielded a MAT of approximately — 5 °C, additional information
from oxygen isotopes in mosses at the site allowed us to calculate isotopic enrichment in the cellulose of fossil trees, thereby reducing assumptions and increasing the precision of our MAT estimates (see the Data Repository).
Not exact matches
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.
Analyses of samples brought back
from the Apollo missions in the 1970s showed that the Moon has the same abundances of the three stable
isotopes of
oxygen as Earth.
Terada told Space.com that the evidence for where the ions came
from was the
isotope oxygen - 16.
Retired University of Wisconsin, Madison, archaeologist Doug Price analyzed strontium,
oxygen, and carbon
isotopes in 20 teeth
from Tollense.
The team used records of
oxygen isotope ratios (which provide a record of ancient water temperature)
from microscopic plankton fossils recovered
from the Mediterranean Sea, spanning the last 5.3 million years.
The new sea - level record was then used in combination with existing deep - sea
oxygen isotope records
from the open ocean, to work out deep - sea temperature changes.
The reason
oxygen isotopes are present in a different pattern is because they are derived
from sustained chemical reactions occurring on the surface of the outer solar nebula, rather than
from a one - time event.
The researchers determined
from the
isotope ratio that the Taylor Glacier samples were 120,000 years old, and validated the estimate by comparing the results to well - dated ice core measurements of atmospheric methane and
oxygen from that same period.
To figure out those answers, Rybczynski turned to Ash Ballantyne, another grad student at Duke, who was using
oxygen isotopes from tree cores to determine historical temperatures.
It is measurable in terms of
oxygen and carbon
isotope ratios and was compared to «environmental archive» data
from other parts of the earth.
Barrick and Showers measured the relative ratios of the
isotopes oxygen - 16 and
oxygen - 18 in the phosphate
from 54 samples of a near - complete T. rex skeleton.
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.
Carbon and
oxygen isotope analyses of teeth
from the Ar.
David Hodell, Jason Curtis and Mark Brenner
from the University of Florida obtained their evidence
from the ratio of calcium carbonate to calcium sulphate in sediments
from Lake Chichancanab, in Yucátan, Mexico, and
from the proportion of heavy to light
isotopes of
oxygen in buried shells.
Warmer air temperatures cause more water containing the heavier
isotopes oxygen - 18 or deuterium to evaporate
from the surrounding ocean.
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.
«We identified the different
isotopes of hydrogen and
oxygen in the water, which allowed us to work out where the water came
from.
From 1990 to 2010, the nitrogen
isotope record indicates that
oxygen content steadily decreased in the area, as expected.
What the team discovered was an odd
oxygen isotope telling them that the sulfates came
from gases that had undergone atmospheric reactions en route to the valley.
The Earth's water must have come
from its interior, according to a scientist who has studied the ratios of
oxygen isotopes in rocks.
The ice shelf had been thinning slowly, however, which was evidenced by a change in the
oxygen isotopes present in plankton preserved
from the underlying water column.
In the study, the researchers examined nitrogen and
oxygen isotopes in N2O samples collected
from permafrost peatland sites in northwestern Russia.
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 most convincing evidence for this, says Jouzel, comes
from isotope ratios; ice that has frozen in site has a higher proportion of water molecules containing the heavy form of
oxygen,
oxygen - 18, than that of ice that has been transported over long distances by weather systems.
Dust
from our own solar system has a characteristic ratio of heavy to light
oxygen isotopes.
The information about
oxygen concentration comes
from the isotopic composition of carbon or rather
from the ratio between the stable carbon
isotopes 12C and 13C.
The paleoclimate data, which included mainly changes in the
oxygen isotopes of the calcium carbonate deposits, were then compared to similar records
from other caves, ice cores, and sediment records as well as model predictions for water availability in the Middle East and west central Asia today and into the future.
Evidence for approximately contemporaneous global cooling in sediments that do contain YTT glass shards has been found in marine core
oxygen isotope records
from the South China Sea (3), as have terrestrial carbon
isotope and pollen records
from Northern India and Bengal (23).
This paper gives results
from a stable
oxygen isotope assessment of modern human and horse enamel δ18O values recovered
from tooth enamel.
To date, we have a full complement of analyses for about three years of growth for one tusk
from the Taimir Peninsula of Siberia (the Jarkov mammoth; ca. 20,300 rybp) and growth increment and tusk apatite carbon and
oxygen isotope ratios for two to three years of growth
from two tusks
from Wrangel Island (4,400 and 4,120 year bp).
Ancient sediments that once resided on a lake bed and the ocean floor show sulfur
isotope ratios unlike those found in other samples
from the same time, calling into question accepted ideas about when the Earth's atmosphere began to contain
oxygen, according to researchers
from the U.S., Canada and Japan.
u «The moon rocks, however, showed [
oxygen isotope] ratios markedly similar to those of rocks
from Earth.
Then the team restricted evidence to just three measurements that can be obtained
from shell samples in sediment cores: cadmium concentration and carbon and
oxygen isotope ratios in the calcium carbonate shells.
It's unknown where this space rock came
from, but a Mars origin had been ruled out because of the rock's concentration of
oxygen isotopes.
Sulfate sources and oxidation chemistry over the past 230 years
from sulfur and
oxygen isotopes of sulfate in a West Antarctic ice core.
The group of meteorites known as HED (howardite, eucrite, and diogenite) are thought to emanate
from Vesta, as their
oxygen isotope signatures are the same.
The
oxygen isotopes of a meteorite can act as a fingerprint to identify the parent body it originated
from.
Based on the temperature minimum recorded
from the early Late Oxfordian of Kachchh, it was suggested that the widening of the Trans - Gondwanan Seaway may have led to increased upwelling in the Malagasy Gulf and to a cooling recorded in the
oxygen isotopes of belemnites and other marine invertebrates
from Kachchh [38].
In any event, pretty early on in the book (a bit after box 2.2, «The World According to
Oxygen Isotopes») he says: that cores taken
from «Intermediate depths in the ocean... show warming of perhaps 5C» and that this warming was caused by CO2 the source of which is still controversial.
To date, we have a full complement of analyses for about three years of growth for one tusk
from the Taimir Peninsula of Siberia (the Jarkov mammoth; ca. 20,300 rybp) and growth increment and tusk apatite carbon and
oxygen isotope ratios for two to three years of growth
from two tusks
from Wrangel Island (4,400 and 4,120 year bp).