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. Analysis of cosmogenic nuclides produced in surface rocks and sediments is avaluable tool for assessing the rates of processes and the timing of events thatshaped the Earth surface. The various nuclides that are used have specificadvantages and limitations that depend on the time range over which they areuseful, the type of material they are produced in and not least thefeasibility of the analytical effort. Anticipating novel applications inEarth surface sciences, we develop in situ-produced terrestrial cosmogenickrypton (Krit) as a new tool, the motivation being the availability ofsix stable and one radioactive isotope (81Kr, half-life 229 kyr) and ofan extremely weathering-resistant target mineral (zircon). We provide proofof principle that terrestrial Krit can be quantified and used tounravel Earth surface processes.

In situ-produced cosmogenic krypton in zircon and its potential for Earth surface applications