The main panel 1 data is from
stable oxygen isotope measurements from the shells of macroscopic marine organisms («fossil shells»), collected by Veizer et al (1999), as re-interpreted by Royer et al (2004).
This proxy, known as the δ18O
stable oxygen isotope ratio, varies in proportion to the ambient moisture.
Uses a time series of hydrographic and
stable oxygen isotope (δ18O) measurements collected at a near - coastal site in Marguerite Bay to quantify the prevalence of meteoric freshwater (glacial melt plus precipitation) separately from sea ice melt
Stable oxygen isotope ratios contained in the shell can be used to infer past water temperatures.
Like the data used right through 0.02 to 66 My, the Freidrich et al collection comprises
stable oxygen isotope ratios from the shells of tiny bottom - dwelling, deep - water marine organisms (benthic foraminifera).
This paper gives results from
a stable oxygen isotope assessment of modern human and horse enamel δ18O values recovered from tooth enamel.
SALINITY (in strict physical oceanography terms - in PSU), mediates the amount of δ18O of seawater and ONLY the δ18O of seawater parameter along with temperature can physically change
the stable oxygen isotopes of foraminifera.
Not exact matches
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.
By carefully micro-sampling each shell along its direction of growth and analyzing for
stable carbon and
oxygen isotopes and trace elements, the team reconstructed a record of seasonal variation during the lifetimes of the organisms.
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.
I joined the team and undertook isotopic work using
oxygen, nitrogen and carbon
stable isotopes to assess his geographical origin and also his diet.
Lower amounts of
stable hydrogen and
oxygen isotopes in the ice indicate colder weather, Persoiu said.
One group of students has been drilling modern and fossil teeth to obtain samples that will be analyzed to examine
stable carbon and
oxygen isotope ratios.
We analyzed
stable carbon and
oxygen isotopes (δ13C, δ18O) of decade - old California mussel shells (Mytilus californianus) in the context of an instrumental seawater record of the same length.
Statistical analysis of the carbon and
oxygen stable isotope recordsr eveals variations in the periods around 100, 11 and 3 years.A century scale connection between the 13C / 12C record and solar activity is most evident.»
Shell material was analyzed for
stable isotopes of carbon (δ13C) and
oxygen (δ18O) in the Earth Systems History Laboratory at Brown University (Providence, RI).
Stable isotope ratios of
oxygen reflect water temperatures, with higher δ18O values indicating colder water [6], [9], [12], such as water upwelled from lower depths.
Inter - and intra-annual
stable carbon and
oxygen isotope signals in response to drought in Mediterranean pines
The ratio of
stable isotopes oxygen - 18 and
oxygen - 16 in the foraminifera is an indicator of ocean temperature.