A new database brings together
water isotope data from many sources, providing an integrated resource for studying changes in Earth's hydroclimate over the past 2,000 years.
This interpretation was based on
water isotope data from central Greenland ice cores.
Not exact matches
Sedimentary layers, stalact.ites,
water erosion over time, ice core
data, tree rings,
isotope decay rates.
By looking at the chemistry of rocks deposited during that time period, specifically coupled carbon and sulfur
isotope data, a research team led by University of California, Riverside biogeochemists reports that oxygen - free and hydrogen sulfide - rich
waters extended across roughly five percent of the global ocean during this major climatic perturbation — far more than the modern ocean's 0.1 percent but much less than previous estimates for this event.
For the first time, the researchers have proved that both the worldwide measurement network NDACC with its ground stations and modern weather satellites provide reliable global
data for the
isotope composition of tropospheric
water vapor.
They also used satellite precipitation
data to «backsolve» the brine's origins using sodium concentrations, oxygen and hydrogen
isotopes, as the isotopic composition of
water reflects the condensation temperature and precipitation rate over time.
That, combined with nitrogen
isotope data, points to carbonaceous chondrites as the most likely common source of
water.
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.
They limited
data sources to locations around the world in which paleoceanographic
data also exist, using seven variables: salinity; potential temperature; oxygen
isotope ratios in
water; carbon
isotope ratios in dissolved inorganic carbon; and concentrations of phosphate, nitrate, and dissolved oxygen.
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).