Right now? Not that we know of.
Historically? Yes.
https://www.iaea.org/newscenter/news/meet-oklo-the-earths-tw...
> A key factor that made the reaction possible was that [back then] the fissile isotope ²³⁵U made up about 3.1% of the natural uranium, which is comparable to the amount used in some of today's reactors.
Right now? Not that we know of.
Historically? Yes.
https://www.iaea.org/newscenter/news/meet-oklo-the-earths-tw...