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Geologic age dating sequence

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Paleontology is limited to the study of sedimentary deposits where fossils are preserved, but can be used in establish relative ages of nearby igneous intrusion, faults, and other geologic features.

With the cumulative experience of centuries of paleontological research, the chronology of many fossil species are well established in context of both geologic time and distribution.

Palynologists separate pollen from sediments for correlation and paleoenvironmental reconstructions.

Typically, paleontological information is used in conjunction with other methods of relative or absolute age dating.

The Sr geochronology method involves extracting these isotopes from fossil shell material (only several milligrams of sample are necessary for X-ray fluorescence spectroscopy).

The ratio of these two isotopes derived from a sample is compared with a database of known samples to determine relative ages.

In Menlo Park, contact: Dwayne Champion for more information about the paleomagnetic lab.

A relative age of the original shell can be established by comparing the strontium isotope ratio of the shell material to published data for the time periods where this method is usable.

The method is most effective when used in conjunction with other dating methods. Stable Isotope Records - Stable isotope data derived from mineral and biological materials can provide a variety of insights into environmental conditions (past and present), and can be used in geochronology and correlation.

Great volcanic eruptions in the Western United States in the geologic past produced airfall deposits that have been recognized as far away as the East Coast.

The USGS maintains a tephrochronology laboratory in Menlo Park, CA.