BIOL321 Lecture Notes - Lecture 6: Theoretical Ecology, Nothofagus, Ecological Niche

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In the pleistocene, sea levels lowered because of glaciation, about 1. 9 mya. Areas that are now separated were once joined, allowing organisms and biota to move. Example isthmus of panama, when it formed 3mya, biota moved north and south in the. Great american interchange which we understand from the fossil record. Most species that came north went extinct, but many that went from north to south have extant relatives today! Usually when trying to understand when a speciation event was because of vicariance or dispersal, we test the phylogenetic relationship of the organisms, and compare them to geological and geographical changes in the past. If the event was due to vicariance, the speciation events in the phylogenetic tree and the geological changes match up. Example: gondwana breakup and southern beech trees: when we place together the separation of gondwana, with the molecular clock of the southern beech, it appears to match up and be vicariance.

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