After having provided a historical context and examples of how and why species migrate due to climate change this blog has decided to focus on two main aspects. The first is to deal with the debate over glacial refugia and species migrationary capacity to disperse following glaciation. The second being to look in further detail at species migration models and critically assess how future migrations can be predicted. Both of these aspects are linked, inferring past migrations from paleoecological data in to help model future major species migrations in response to climate change.
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