The Thanetian (also known as the Landenian or Heersian) is the last stage of the Paleocene Epoch, corresponding to the Late Paleocene sub-epoch. It spans the time between 58.7 ± 0.2 Ma and 55.8 ± 0.2 Ma (million years ago). The name derives from the Thanet Beds, the oldest Paleocene deposits in the London Basin, named after the area of Kent known as the Isle of Thanet. Image:Mantell's Iguanodon restoration.jpg This article is a . You can help My English Wiki by expanding it.
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is fossil range of |