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2. Faunal turnover in the Azraq Basin, eastern Jordan 28,000 to 9000 cal yr BP, signalling climate change and human impact.

3. The palaeoenvironmental potential of the eastern Jordanian desert basins (Qe'an).

4. THE FORMATION OF EARLY NEOLITHIC COMMUNITIES IN THE CENTRAL ZAGROS: AN 11,500 YEAR‐OLD COMMUNAL STRUCTURE AT ASIAB.

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