Linked from

The 15 pages that link to Isotope fractionation, each with the reason it gives.

• Isotope geochemistryRelated: Fractionation creates systematic isotope differences that reveal processes such as evaporation, mineral growth, and metabolism.

• Oxygen isotope ratioRelated: It produces the ratio shifts used to infer environmental conditions.

• Kinetic isotope effectCompared with: Both phenomena depend on isotope-sensitive processes, but fractionation tracks isotope abundances rather than reaction rates.

• Isotope effectRelated: Isotope effects generate fractionation that records how materials were formed or transformed.

• Isotopic abundanceRelated: It explains why sample abundances can differ from their source material.

• CosmochemistryRelated: Its patterns help distinguish processes such as evaporation, condensation, and chemical exchange.

• Isotope analysisRelated: Fractionation explains how diet and metabolism alter the ratios preserved in tissues.

• Isotope hydrologyRelated: Evaporation and condensation fractionate water isotopes, creating traceable signatures.

• Carbon isotope excursionRelated: Fractionation gives carbon sources and processes distinct isotope signatures.

• Isotopes of oxygenRelated: It alters oxygen isotope ratios in water, minerals, and biological materials.

• PaleothermometerRelated: Temperature-dependent fractionation is the basis of several isotope paleothermometers.

• Carbon isotopesRelated: Processes preferentially handle carbon isotopes, leaving measurable signatures.

• Interstellar iceRelated: Isotopic signatures in ice-related molecules can constrain their formation temperatures and histories.

• Isotopes of nitrogenRelated: Biological nitrogen transformations often enrich or deplete nitrogen-15.

• δ18ORelated: Fractionation produces the δ18O differences measured between materials.