Abstract:<p>The Late Miocene flora and paleogeography of north-western Wairarapa were determined by examining and sampling the Upper Miocene marine and non-marine deposits of the Mangaoranga Formation. This formation unconformably overlies Mesozoic greywacke basement in areas of north-west Wairarapa and contains the oldest sediments preserved immediately overlying basement in this area. Little work has been carried out previously to fully understand the depositional history of the formation or the surrounding veg… Show more
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