Evaluating the hypothesis of New Zealand’s total submersion during the Oligocene requires the strictest tests, including sound phylogenetic data and dating of phylogenies. Although New Zealand has been traditionally considered to host ancient biota that originated by vicariance after it separated from Australia ~80 Mya, the ancient origins of its biota have been recently questioned, with some authors even suggesting that all current land organisms had to arrive to the islands after it re-emerged from the ocean 22 million years ago. Here we examine examples of short-range endemic soil-dwelling invertebrates and find compelling evidence that at least some of them are the result of old lineages that diversified in New Zealand before the hypothesised submersion event 22 million year ago. We conclude that New Zealand indeed has old lineages as well as recently diversified lineages and compare this situation with that of other more stable areas of the Neotropics.