While also using the international geologic time scale, many nations–especially those with isolated and therefore non-standard prehistories–use their own systems of dividing geologic time into epochs and
faunal stages.
In New Zealand, these epochs and stages use local place names (mainly
Māori in origin) back to the
Permian. Prior to this time, names mostly align to those in the Australian geologic time scale, and are not divided into epochs.[1] In practice, these earlier terms are rarely used, as most New Zealand geology is of a more recent origin. In all cases, New Zealand uses the same periods as those used internationally; the renaming only applies to subdivisions of these periods. Very few epochs and stages cross international period boundaries, and the exceptions are almost all within the Cenozoic Era. New Zealand updates will always be behind any significant international updates in the
International Geological Time Scale.
Although the New Zealand geologic time scale has not been formally adopted, it has been widely used by
earth scientists,
geologists and
palaeontologists in New Zealand since J. S. Crampton proposed it in 1995. The most recent calibrated update was in 2015.[2][3]
A standard abbreviation is used for these epochs and stages. These are usually in the form Xx, where the first letter is the initial letter of the epoch and the second (lower-case) letter is the initial letter of the stage. These are noted beside the stage names in the list below.
Currently, from the New Zealand perspective we are in the Haweran stage of the Wanganui epoch which is within the internationally defined
Holocene epoch of the
Quaternary period of the
Cenozoic era. The Haweran, which started some 340,000 years ago, is named after the
North Island town of
Hawera. The New Zealand stages and epochs are not the same as internationally defined periods and epochs (e.g. the Wanganui epoch started at 5.33 Ma which is within the
Neogene period and matches the start of the international
Pliocene epoch, but contains also the international
Holocene and
Pleistocene epochs).
List of New Zealand geologic time epochs and stages
Times given indicate the start of the respective stages and epochs. Several of these stages are further divided into upper and lower or upper, middle, and lower, although this has not been noted below unless unique names have been given to these sub-stages. As with the international geologic scale, these epochs and stages are largely named for locales where rock dating from these time periods is in evidence, with stage names predominantly but not always named for locales close to their epoch's namesake site. Where known, these places are also linked in the list below.[2]
Stages prior to the beginning of the Carboniferous Period use either international (Devonian/Silurian) or Australian (Ordovician/Cambrian) geologic stage names; very little New Zealand rock is known from these geologic periods.
^ This stage is sometimes further divided into Mangaoran (lower) and Waikatoan (upper). These are named after Mangaora Inlet (an arm of
Kawhia Harbour) and the
Waikato River.
^ This stage is sometimes further divided into Kiriteherean (lower) and Marokopan (upper). These are named after the
Marokopa River and the nearby
Kiritehere Stream.
^ Until the late 1960s, the Flettian and Barettian stages were together known as the Braxtonian stage (see Waterhouse 1969). This was named for
Braxton Burn, a stream near
Mossburn.
Where not subdivided usual reason is no stages recognised due to absent record
Bishop, D.G., and Turnbull, I.M. (compilers) (1996). Geology of the Dunedin Area. Lower Hutt, NZ: Institute of Geological & Nuclear Sciences.
ISBN0-478-09521-X.
Hollis, C.J., Beu, A.G., Crampton, J.S., Crundwell, M.P., Morgans, H.E.G., Raine, J.I., Jones, C.M., Boyes, A.F. (2010). Calibration of the New Zealand Cretaceous - Cenozoic Timescale to GTS2004, GNS Science Report, 2010/43, 20p.