@tsarstepan,
we have one in geology. Im not sure its got any use for the general public since its an inverse function based upon stratigraphy and magntic susceptibility.
We measure geologic epochs and smaller divisions in "Chrons"
When stratigraphic columns are produced , an effort to correlate these units worldwide is based upon the "chron" { time from present}.
Secondly In isotope chronology we use a value of "A" (loosely, an annum) which is a constant unit of seconds that we see in an average year. This defeats the assertion that Isotope "Time" is speeding up or slowing down) {Of course the actual second may be but who gives a ****, were all riding the same wave}.
All these chrons and anna are presented as n/A or n/C
where n = the time interval from its end to its base.
BUT, most often, when we are all likkered up, we usually say "its so many years old"
we only use the actual A's and C's in papers. (Nobody talks like that)