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Calcimator

Paleoclimate Proxy Converter Calculator

Temperature from oxygen isotope ratios (delta18O).

Inputs

Results

Estimated temperature (°C)

26.06

Temperature anomaly (°C)11.06
δD estimate (‰)-6
Sea level change (m)181.8
Ice volume index (0-100)0
Deuterium excess (‰)10
How to Use This Calculator
  1. Select the Proxy type: 0 for marine carbonates (Shackleton calibration), 1 for ice cores (Jouzel slope), or 2 for speleothems (Kim & O'Neil).
  2. Enter the measured δ18O (‰) value from mass spectrometry — typical marine carbonate values range from −2 to +5 ‰ VPDB.
  3. For marine or speleothem proxies, set δ18O seawater (‰) to account for ice-volume effects on ocean isotope composition.
  4. Enter the Modern reference temp (°C) to compute the Temperature anomaly relative to present.
  5. Read Estimated temperature (°C), Sea level change (m), and Ice volume index to place the sample in a paleoclimate context.
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