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Stable Isotope Analysis of Carbonates – (δ13C and δ18O)

recommended sample size Sample size recommended
  • 2 mg – Sample must be ready for measurement (pH neutral, clean and dry)
carbon dating services Turnaround time
  • 14 business days
recommended container Recommended container
  • Ziplock Bags (place in Aluminum foil if sample is small or can be crushed during shipment)
  • Please send your samples in small boxes instead of envelopes to protect the samples.
lab recommendation
  • Beta Analytic offers oxygen isotope measurements for carbonates on a standalone basis, without radiocarbon dating.

Beta ONLY accepts samples ready for measurement for stable isotope analysis not in conjunction with Carbon-14 dating. Samples must be ready for measurement (pH neutral, clean and dry).

printed sampleThe interpretation of d18O values, as applied in paleotemperature studies and paleoclimate reconstructions, lies with the submitter.

Submittal – Please use this online data sheet.

Please contact us if you are in doubt about the suitability or weight of your sample.

Stable Isotope Analysis Cost

To provide you with the appropriate prices, please let us know the material type. For formal estimates, please indicate in this form the number of samples per material type and the paying institution’s billing name and address.

Disclaimer: This video is hosted in a third-party site and may contain advertising
This video excerpt is part of Beta Analytic’s webinar: Isotopes 101: An Introduction to Isotopic Analysis

Applications of δ18O Stable Isotope Analysis

One of the major applications of d18O is in paleoclimatology – looking at oceans, glaciers and the fossils within them. The main processes that affect the Oxygen-18 (18O) / Oxygen-16 (16O) isotopic ratio are evaporation and condensation. Seawater typically has a higher 18O content than ice in glaciers.

The d18O ratio changed over time with temperature, thus measuring d18O is indicative of past climates and can differentiate between glacial and interglacial periods. During glacial periods, the oceans were enriched in 18O with the lighter 16O isotope trapped in glacial ice. The opposite was true during interglacial periods (warmer global average temperatures) when the ice melted releasing the 16O isotopes and the oceans had less 18O.


Holli Riebeek, Paleoclimatology: the Oxygen Balance (2005), NASA Earth Observatory

Note – Beta also automatically includes d18O and d13C values alongside radiocarbon dating results for carbonate samples. The d18O and d13C measurements are performed simultaneously on the carbonates in an isotope ratio mass spectrometer (IRMS) at no additional cost to the client. 

We also offer Oxygen-18 and Deuterium stable isotope measurements for water samples.

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Page last updated: June 2022