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The two main faunas identified in the South Island include: 1.

The fauna of the high rainfall west coast beech (Nothofagus) forests that included Anomalopteryx didiformis (bush moa) and Dinornis robustus (South Island giant moa); and 2.

Its bones have been found in caves in the northwest Nelson and Karamea districts (such as Honeycomb Hill Cave), and some sites around the Wanaka district. However, it also occurred down to sea level where there was suitable steep and rocky terrain (such as Punakaiki on the west coast and Central Otago).

Moa extinction occurred around 1300 CE Although moa skeletons were traditionally reconstructed in an upright position to create impressive height, analysis of their vertebral articulation indicates that they probably carried their heads forward, in the manner of a kiwi.

This has resulted in a reconsideration of the height of larger moa.

Although there is no surviving record of what sounds moa made, some idea of their calls can be gained from fossil evidence.

The fauna of the dry rainshadow forest and shrublands east of the Southern Alps that included Pachyornis elephantopus (heavy-footed moa), Euryapteryx gravis, Emeus crassus and Dinornis robustus.

The two other moa species that existed in the South Island; Pachyornis australis and Megalapteryx didinus might be included in a ‘subalpine fauna’, along with the widespread Dinornis robustus. australis is the rarest of the moa species, and the only one not yet found in Maori middens. Its name "upland moa" reflects the fact its bones are commonly found in the subalpine zone.If you happen to know what she has been up to let us know.