  On Aug 22, 2016, a bright fireball was observed by the Desert Fireball
Network in South Australia. Its pre-atmosphere orbit suggests it was
temporarily captured by the Earth-Moon system before impact. A search was
conducted two years after the fall, and a meteorite was found after 6 days of
searching. The meteorite appeared relatively fresh, had a mass consistent with
fireball observation predictions, and was at the predicted location within
uncertainties. However, the meteorite did show some weathering and lacked
short-lived radionuclides ($^{58}$Co, $^{54}$Mn). A terrestrial age based on
cosmogenic $^{14}$C dating was determined; the meteorite has been on the
Earth's surface for $3.2\pm1.3$ kyr, ruling out it being connected to the 2016
fireball. Using an upper limit on the pleistieocene terrain age and the total
searched area, we find that the contamination probability from another fall is
$<2\%$. Thus, the retrieval of the "wrong" meteorite is at odds with the
contamination statistics. This is a key example to show that fireball-meteorite
pairings should be carefully verified.
