Dinornis Giganteus
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Dinornis Giganteus
The North Island giant moa (''Dinornis novaezealandiae'') is an extinct moa in the genus ''Dinornis''. Even though it might have walked with a lowered posture, standing upright, it would have been the tallest bird ever to exist, with a height estimated up to 3.6 metres (12 feet). Taxonomy It was a ratite and a member of the order Dinornithiformes.Davies, S.J.J.F. (2003). "Moas". In Hutchins, Michael (ed.). Grzimek's Animal Life Encyclopedia. 8 Birds I Tinamous and Ratites to Hoatzins (2 ed.). Farmington Hills, MI: Gale Group. pp. 95–98. ISBN 0-7876-5784-0. The ''Dinornithiformes'' were flightless birds with a sternum but without a keel. They also had a distinctive palate. Origin The origin of ''ratites'' is becoming clearer, as it is now believed that early ancestors of these birds were able to fly (Davies, 2003). From such fossil evidence it is believed that the early flying ratites originated in the Northern Hemisphere and flew to the Southern Hemisphere (Davies, 20 ...
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Late Pleistocene
The Late Pleistocene is an unofficial Age (geology), age in the international geologic timescale in chronostratigraphy, also known as Upper Pleistocene from a Stratigraphy, stratigraphic perspective. It is intended to be the fourth division of the Pleistocene Epoch within the ongoing Quaternary Period. It is currently defined as the time between c. 129,000 and c. 11,700 years ago. The Late Pleistocene equates to the proposed Tarantian Age of the geologic time scale, preceded by the officially ratified Chibanian (formerly known as Middle Pleistocene) and succeeded by the officially ratified Greenlandian. The estimated beginning of the Tarantian is the start of the Eemian interglacial period (Marine Isotope Stage 5). It is held to end with the termination of the Younger Dryas, some 10th millennium BC, 11,700 years ago when the Holocene Epoch began. The term Upper Pleistocene is currently in use as a provisional or "quasi-formal" designation by the International Union of Geological ...
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