| scholarly article | Q13442814 |
| P819 | ADS bibcode | 2006GeoRL..3312604L |
| P356 | DOI | 10.1029/2006GL026011 |
| P50 | author | Allegra N. LeGrande | Q58096060 |
| Gavin A. Schmidt | Q1496443 | ||
| P2860 | cites work | Present-Day Atmospheric Simulations Using GISS ModelE: Comparison to In Situ, Satellite, and Reanalysis Data | Q55953662 |
| Oxygen isotopic composition ofGloborotalia truncatulinoidesas a proxy for intermediate depth density | Q58307089 | ||
| Modeling atmospheric stable water isotopes and the potential for constraining cloud processes and stratosphere-troposphere water exchange | Q58316121 | ||
| Global calibration of ecological models for planktic foraminifera from coretop carbonate oxygen-18 | Q58384625 | ||
| Error analysis of paleosalinity calculations | Q58384645 | ||
| How much deep water is formed in the Southern Ocean? | Q107047290 | ||
| P433 | issue | 12 | |
| P407 | language of work or name | English | Q1860 |
| P921 | main subject | seawater | Q184395 |
| P577 | publication date | 2006-01-01 | |
| P1433 | published in | Geophysical Research Letters | Q5535576 |
| P1476 | title | Global gridded data set of the oxygen isotopic composition in seawater | |
| P478 | volume | 33 |
| Q58304069 | A 6.5-year continuous record of sea surface salinity and seawater isotopic composition at Harbour of Ishigaki Island, southwest Japan |
| Q58303973 | A model-based test of accuracy of seawater oxygen isotope ratio record derived from a coral dual proxy method at southeastern Luzon Island, the Philippines |
| Q58410735 | Advancing Mg/Ca Analysis of Coralline Algae as a Climate Proxy by Assessing LA-ICP-OES Sampling and Coupled Mg/Ca-δ18 O Analysis |
| Q57532659 | Agulhas salt-leakage oscillations during abrupt climate changes of the Late Pleistocene |
| Q106957631 | An El Niño Mode in the Glacial Indian Ocean? |
| Q48262677 | Assessing kinetic fractionation in brachiopod calcite using clumped isotopes. |
| Q60058404 | Assessing spatial variability in El Niño-Southern Oscillation event detection skill using coral geochemistry |
| Q40848897 | Bipolar seesaw control on last interglacial sea level. |
| Q58060275 | Calibration and application of B/Ca, Cd/Ca, and δ11B in Neogloboquadrina pachyderma (sinistral) to constrain CO2 uptake in the subpolar North Atlantic during the last deglaciation |
| Q57213136 | Capturing the global signature of surface ocean acidification during the Palaeocene-Eocene Thermal Maximum |
| Q43928916 | Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate |
| Q99207548 | Combining genetic markers with stable isotopes in otoliths reveals complexity in the stock structure of Atlantic bluefin tuna (Thunnus thynnus) |
| Q58241765 | Comparing proxy and model estimates of hydroclimate variability and change over the Common Era |
| Q39843951 | Comparison of secondary ion mass spectrometry and micromilling/continuous flow isotope ratio mass spectrometry techniques used to acquire intra-otolith delta18O values of wild Atlantic salmon (Salmo salar). |
| Q61819113 | Considerations for Globigerinoides ruber (white and pink) paleoceanography: comprehensive insights from a long‐running sediment trap |
| Q58458689 | Corroborating ecological depth preferences of planktonic foraminifera in the tropical Atlantic with the stable oxygen isotope ratios of core top specimens |
| Q64025239 | Deciphering the Variability in Mg/Ca and Stable Oxygen Isotopes of Individual Foraminifera |
| Q28598027 | Dentine oxygen isotopes (δ (18)O) as a proxy for odontocete distributions and movements |
| Q105426320 | Developing a Coral Proxy System Model to Compare Coral and Climate Model Estimates of Changes in Paleo‐ENSO Variability |
| Q57892220 | Development and evaluation of a system of proxy data assimilation for paleoclimate reconstruction |
| Q64091260 | Distinguishing between sea turtle foraging areas using stable isotopes from commensal barnacle shells |
| Q58384445 | Early Pleistocene obliquity-scale pCO2 variability at ~1.5 million years ago |
| Q101245964 | Effects of Improved 17 O Correction on Interlaboratory Agreement in Clumped Isotope Calibrations, Estimates of Mineral‐Specific Offsets, and Temperature Dependence of Acid Digestion Fractionation |
| Q58307070 | Ensemble, water isotope-enabled, coupled general circulation modeling insights into the 8.2 ka event |
| Q58398529 | Environmental and biological controls on size-specific δ13 C and δ18 O in recent planktonic foraminifera |
| Q60669059 | Environmental change in the subtropics during the late middle Eocene greenhouse and global implications |
| Q37661260 | Episodic release of CO2 from the high-latitude North Atlantic Ocean during the last 135 kyr. |
| Q37369266 | Equatorial heat accumulation as a long-term trigger of permanent Antarctic ice sheets during the Cenozoic |
| Q58303866 | Evaluating the skills of isotope-enabled general circulation models against in situ atmospheric water vapor isotope observations |
| Q36498178 | Evolution of South Atlantic density and chemical stratification across the last deglaciation |
| Q60153407 | Freshwater input and abrupt deglacial climate change in the North Atlantic |
| Q104471899 | Gas hydrate versus seabed morphology offshore Lebu (Chilean margin) |
| Q57499743 | Glacial-interglacial changes in central tropical Pacific surface seawater property gradients |
| Q106957632 | Global Core Top Calibration ofδ18O in Planktic Foraminifera to Sea Surface Temperature |
| Q61080113 | Gridded data set of the stable isotopic composition of precipitation over the eastern and central Mediterranean |
| Q59335069 | High frequency environmental changes and deposition processes in a 2 kyr-long sedimentological record from the Cap-Breton canyon (Bay of Biscay) |
| Q58474289 | Impact of recently upwelled water on productivity investigated using in situ and incubation-based methods in Monterey Bay |
| Q61444473 | Influence of surface ocean density on planktonic foraminifera calcification |
| Q58070874 | Interpreting Precession-Driven δ18 O Variability in the South Asian Monsoon Region |
| Q28604065 | Jurassic climate mode governed by ocean gateway |
| Q38948766 | Latitudinal gradients in greenhouse seawater δ(18) O: evidence from Eocene sirenian tooth enamel |
| Q28655062 | Listening in on the past: what can otolith δ18O values really tell us about the environmental history of fishes? |
| Q58458671 | Meridional shifts of the Atlantic intertropical convergence zone since the Last Glacial Maximum |
| Q58309649 | Mg/Ca thermometry in planktic foraminifera: Improving paleotemperature estimations forG. bulloidesandN. pachydermaleft |
| Q58090239 | Millennial-scale glacial meltwater pulses and their effect on the spatiotemporal benthic δ18O variability |
| Q57580056 | Mindanao Dome variability over the last 160 kyr: Episodic glacial cooling of the West Pacific Warm Pool |
| Q61118478 | Most Earth-surface calcites precipitate out of isotopic equilibrium |
| Q57532641 | Multicentennial Agulhas leakage variability and links to North Atlantic climate during the past 80,000 years |
| Q92782866 | Natural drivers of multidecadal Arctic sea ice variability over the last millennium |
| Q57950276 | North Atlantic mid-latitude surface-circulation changes through the Plio-Pleistocene intensification of northern hemisphere glaciation |
| Q30903409 | Ocean currents generate large footprints in marine palaeoclimate proxies. |
| Q57774060 | Oxygen Isotope Seasonality Determinations of Marsh Clam Shells from Prehistoric Shell Middens in Nicaragua |
| Q36345455 | Oxygen and carbon isoscapes for the Baltic Sea: Testing their applicability in fish migration studies. |
| Q53095875 | Paleoceanography. Antarctic role in Northern Hemisphere glaciation. |
| Q58457991 | Precipitation variability within the West Pacific Warm Pool over the past 120 ka: Evidence from the Davao Gulf, southern Philippines |
| Q48158187 | Pronounced centennial-scale Atlantic Ocean climate variability correlated with Western Hemisphere hydroclimate |
| Q58303961 | Proxy interpretation of coral-recorded seawater δ18O using 1-D model forced by isotope-incorporated GCM in tropical oceanic regions |
| Q42282665 | Pteropods are excellent recorders of surface temperature and carbonate ion concentration. |
| Q58391877 | Quantifying errors in coral-based ENSO estimates: Toward improved forward modeling ofδ18O |
| Q57892228 | Quantifying the effect of seasonal and vertical habitat tracking on planktonic foraminifera proxies |
| Q58458672 | Reconstructing the upper water column thermal structure in the Atlantic Ocean |
| Q57089775 | Reduced ENSO variability at the LGM revealed by an isotope-enabled Earth system model |
| Q30884631 | Reduced El Niño-Southern Oscillation during the Last Glacial Maximum |
| Q64064583 | Resolving the controls of water vapour isotopes in the Atlantic sector |
| Q58070428 | Seasonal variability in the salinity and oxygen isotopic composition of seawater from the Cariaco Basin, Venezuela: Implications for paleosalinity reconstructions |
| Q58307077 | Seawater isotope constraints on tropical hydrology during the Holocene |
| Q58387809 | Segregation of SE Pacific and SW Atlantic southern blue whiting stocks: integrating evidence from complementary otolith microchemistry and parasite assemblage approaches |
| Q58307053 | Sensitivity of seawater oxygen isotopes to climatic and tectonic boundary conditions in an early Paleogene simulation with GISS ModelE-R |
| Q58081033 | Stable water isotopes in the ECHAM5 general circulation model: Toward high-resolution isotope modeling on a global scale |
| Q57532650 | Surface changes in the eastern Labrador Sea around the onset of the Little Ice Age |
| Q59139339 | Temperature calibration of Mg/Ca ratios in the intermediate water benthic foraminiferHyalinea balthica |
| Q98568870 | The Connected Isotopic Water Cycle in the Community Earth System Model Version 1 |
| Q57066364 | The Future of Large‐Scale Stable Isotope Networks |
| Q57880730 | The influence of snow sublimation and meltwater evaporation on δD of water vapor in the atmospheric boundary layer of central Europe |
| Q34340027 | The use of otolith chemistry to characterize diadromous migrations. |
| Q37676712 | Timing and nature of AMOC recovery across Termination 2 and magnitude of deglacial CO2 change |
| Q58392099 | Timing of the descent into the last Ice Age determined by the bipolar seesaw |
| Q112291622 | Using Oxygen Isotope Sclerochronology to Evaluate the Role of Small Islands Among the Guale (AD 1325 to 1700) of the Georgia Coast, USA |
| Q57596764 | Variations ofδ18O in rainwater from southwestern Oregon |
| Q98568844 | Volcanic Eruption Signatures in the Isotope‐Enabled Last Millennium Ensemble |
| Q58307081 | Water isotope expressions of intrinsic and forced variability in a coupled ocean-atmosphere model |
| Q58307058 | Water isotopologues as a quantitative paleosalinity proxy |
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