Lordovig: Difference between revisions

Content deleted Content added
No edit summary
Lien 70:
Glaciation locks up water from the world-ocean, and the interglacials free it, causing sea levels repeatedly to drop and rise; the vast shallow intra-continental Ordovician seas withdrew, which eliminated many ecological niches, then returned carrying diminished founder populations lacking many whole families of organisms, then withdrew again with the next pulse of glaciation, eliminating biological diversity at each change (Emiliani, 1992 p. 491). Nimabids te su mel zü kontinän bal ätopöls pädrefons sevärikumo (Stanley, 360). Lifafoms tropik pädrefons pato nämöfiko fa dadeadam balid, e nimabids se vats koldülik pädrefons badikumo dü dadeadam telid (Stanley, 360).
 
Nimabids älailiföls äbinons uts, kels äplöpons ad lönedikön ad dinäds ivotiköl ed äfulükons spadi pijaföl fa dadeadams. Geikam lifa pos
dönutuvatam laidüpik dilas gretik kontinänas primü [[Silur]] äblinon distöfi ägretiköl in roods no idadeadöls.
 
Finü jenot telid, glatäds äsmetöl äkodons löpikami seananivoda. Geikam lifa pos dönutuvatam laidüpik dilas gretik kontinänas primü [[Silur]] äblinon distöfi ägretiköl in roods no idadeadöls.
At the end of the second event, melting glaciers caused the sea level to rise and stabilise once more. The rebound of life's diversity with the permanent re-flooding of continental shelves at the onset of the Silurian saw increased biodiversity within the surviving Orders.
 
== Noets ==