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Cycles in the ratio mirror climate changes in geologic history. The calculated ratio of the masses of each present in the sample is then compared to a standard, which can yield information about the temperature at which the sample was formed - see Proxy (climate) for details. Additional factors can affect the efficiency of the distillation, such as the direct precipitation of ice crystals, rather than liquid water, at low temperatures.Due to the intense precipitation that occurs in hurricanes, the HO ratio provides a record of ancient water temperature.Water 10 to 15 °C (50 to 59 °F) cooler than present represents glaciation.As colder temperatures spread toward the equator, water vapor rich in O content of oceanic water is lower.The carbon dioxide provides two of the oxygen atoms in the calcite. The isotope ratio in the calcite is therefore the same, after compensation, as the ratio in the water from which the microorganisms of a given layer extracted the material of the shell.A higher abundance of Earth’s dynamic oxygenation evolution is recorded in ancient sediments from the Republic of Gabon from between about 2,150 and 2,080 million years ago.A plot of ancient water temperature over time indicates that climate has varied cyclically, with large cycles and harmonics, or smaller cycles, superimposed on the large ones.

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Oxygen isotope ratio cycles are cyclical variations in the ratio of the abundance of oxygen with an atomic mass of 18 to the abundance of oxygen with an atomic mass of 16 present in some substances, such as polar ice or calcite in ocean core samples, measured with the isotope fractionation.

The ratio is linked to water temperature of ancient oceans, which in turn reflects ancient climates.

Responsible for these fluctuations in oxygenation were likely driven by the Lomagundi carbon isotope excursion.

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Limestone is deposited from the calcite shells of microorganisms.

Calcite, or calcium carbonate, chemical formula Ca CO, dissolved in the water.