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		<summary type="html">&lt;p&gt;Move 1 url. &lt;a href=&quot;/wiki143/index.php?title=User:GreenC/WaybackMedic_2.5&amp;amp;action=edit&amp;amp;redlink=1&quot; class=&quot;new&quot; title=&quot;User:GreenC/WaybackMedic 2.5 (page does not exist)&quot;&gt;Wayback Medic 2.5&lt;/a&gt; per &lt;a href=&quot;/wiki143/index.php?title=WP:URLREQ&amp;amp;action=edit&amp;amp;redlink=1&quot; class=&quot;new&quot; title=&quot;WP:URLREQ (page does not exist)&quot;&gt;WP:URLREQ#paleodb.org&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;{{Short description|Period of geologic time equivalent with the Middle Miocene}}&lt;br /&gt;
The &amp;#039;&amp;#039;&amp;#039;Astaracian&amp;#039;&amp;#039;&amp;#039; age is a period of [[geologic time]] ({{Mya|16.0|11.6|[[Mya (unit)|Ma]]}}), equivalent with the [[Middle Miocene]] and used more specifically with [[European Land Mammal Ages]]. It precedes the [[Vallesian]] age and follows the [[Orleanian]] age. The Astaracian overlaps the [[Langhian]] and [[Serravallian ]] ages.&amp;lt;ref&amp;gt;[https://paleodb.org/cgi-bin/bridge.pl?action=displayInterval&amp;amp;interval_no=292 Paleo Database: Astaracian]&amp;lt;/ref&amp;gt;&lt;br /&gt;
&lt;br /&gt;
During the Late Orleanian and Astaracian ({{Mya|17.0|10.7|Ma}}), oscillating sea levels resulted in a succession of palaeogeographic changes in the Eastern [[Mediterranean]]; the opening and closing of the [[Tethys Ocean|Tethys]] seaway resulted in temporary land-bridges between Africa and Eurasia.  Three short periods of faunal migrations between the continents can be distinguished:&amp;lt;ref name=&amp;quot;Koufos-etal-2005&amp;quot;&amp;gt;{{Cite journal&lt;br /&gt;
 |last1      = Koufos&lt;br /&gt;
 |first1     = George D.&lt;br /&gt;
 |last2      = Kostopoulos&lt;br /&gt;
 |first2     = Dimitris S.&lt;br /&gt;
 |last3      = Vlachou&lt;br /&gt;
 |first3     = Theodora D.&lt;br /&gt;
 |title      = Neogene/Quaternary mammalian migrations in Eastern Mediterranean&lt;br /&gt;
 |journal    = Belgian Journal of Zoology&lt;br /&gt;
 |volume     = 135&lt;br /&gt;
 |issue      = 2&lt;br /&gt;
 |pages      = 181–190&lt;br /&gt;
 |date       = July 2005&lt;br /&gt;
 |oclc       = 716880430&lt;br /&gt;
 |url        = http://www.naturalsciences.be/institute/associations/rbzs_website/bjz/back/pdf/BJZ%20135(2)/Volume%20135(2),%20pp.%20181-190.pdf&lt;br /&gt;
 |accessdate = 19 November 2012&lt;br /&gt;
}}{{Dead link|date=October 2018 |bot=InternetArchiveBot |fix-attempted=yes }}&amp;lt;/ref&amp;gt;&lt;br /&gt;
&lt;br /&gt;
During the Late Orleanian, [[MN zonation|MN]] 5 ({{Mya|17.0|15.0|Ma}}), a first wave of migrations from Africa correspond to fossil fauna from Greece.  The Antonios locality (MN 4/5, {{Mya|17|Ma}}) on the [[Chalkidiki]] peninsula includes the small [[Tragulidae|tragulid]] &amp;#039;&amp;#039;[[Dorcatherium]]&amp;#039;&amp;#039;, the [[giraffid]] &amp;#039;&amp;#039;[[Palaeomeryx]]&amp;#039;&amp;#039;, and the [[Suiformes|suiform]] &amp;#039;&amp;#039;[[Sanitheres]]&amp;#039;&amp;#039;.  The Thymiana locality (MN 5, {{Mya|15.5|Ma}}) on [[Chios]] includes both the giraffid &amp;#039;&amp;#039;[[Georgiomeryx]]&amp;#039;&amp;#039;, &amp;#039;&amp;#039;Dorcatherium&amp;#039;&amp;#039;, the [[Ctenodactylidae|ctenodactylid]] &amp;#039;&amp;#039;[[Sayimys]]&amp;#039;&amp;#039; as well as an immigrant from Asia, the [[proboscidea]]n &amp;#039;&amp;#039;[[Choerolophodon]]&amp;#039;&amp;#039; known from the [[Bugti Hills|Bugti]] fauna (MN 3, {{Mya|18.3|Ma}}) in India.  Primates also arrived during MN5: &amp;#039;&amp;#039;[[Pliopithecus]]&amp;#039;&amp;#039; is known from [[Elgg]] in Switzerland and [[Pontlevoy]]-[[Thenay, Loir-et-Cher|Thenay]] in France and prevailed until the end of the Vallesian.&amp;lt;ref name=&amp;quot;Koufos-etal-2005&amp;quot; /&amp;gt;&lt;br /&gt;
&lt;br /&gt;
{{Gallery&lt;br /&gt;
 |File:Choerolophodon molar.jpg|&amp;#039;&amp;#039;Choerolophodon&amp;#039;&amp;#039; molar&lt;br /&gt;
 |File:Pliopithecus antiquus.jpg|&amp;#039;&amp;#039;Pliopithecus antiquus&amp;#039;&amp;#039;&lt;br /&gt;
}}&lt;br /&gt;
&lt;br /&gt;
A second wave from Africa in the Early Astaracian, MN 6 ({{Mya|15.0|13.5|Ma}}), included the hominoid &amp;#039;&amp;#039;[[Griphopithecus]]&amp;#039;&amp;#039;; a Eurasian relative to the African &amp;#039;&amp;#039;[[Kenyapithecus]]&amp;#039;&amp;#039; found at the Pasalar and Candir localities in Turkey. and at Neudorf-Sandberg in Slovakia.  The primate genus was accompanied by the [[aardvark]] &amp;#039;&amp;#039;[[Orycteropus]]&amp;#039;&amp;#039;.  From Asia came the [[Hyracoidae|hyracoid]] &amp;#039;&amp;#039;[[Pliohyrax]]&amp;#039;&amp;#039;, the [[Cervidae|cervid]] &amp;#039;&amp;#039;[[Dicrocerus]]&amp;#039;&amp;#039;, and the suid &amp;#039;&amp;#039;[[Listriodon]]&amp;#039;&amp;#039;.  Asian [[Bovidae|bovids]] such as &amp;#039;&amp;#039;[[Protragocerus]]&amp;#039;&amp;#039;, &amp;#039;&amp;#039;[[Tethytragus]]&amp;#039;&amp;#039;, and &amp;#039;&amp;#039;[[Hypsodontus]]&amp;#039;&amp;#039; known from Asia Minor and Chios during MN 5 migrated into Africa as part of this wave.&amp;lt;ref name=&amp;quot;Koufos-etal-2005&amp;quot; /&amp;gt;&lt;br /&gt;
&lt;br /&gt;
{{Gallery&lt;br /&gt;
 |File:Kenyapithecus wickeri.JPG|&amp;#039;&amp;#039;Kenyapithecus&amp;#039;&amp;#039;&lt;br /&gt;
 |File:Dicrocerus elegans MHNT.PRE.2012.0.jpg|&amp;#039;&amp;#039;Dicrocerus elegans&amp;#039;&amp;#039;&lt;br /&gt;
 |File:Protragocerus labidotus.JPG|&amp;#039;&amp;#039;Protragocerus labidotus&amp;#039;&amp;#039;&lt;br /&gt;
}}&lt;br /&gt;
&lt;br /&gt;
A third wave during MN 7/8 ({{Mya|13.5|10.7|Ma}}) probably took place, but the late Astaracian is poorly documented.  A seaway most likely joined the [[Paratethys]] and the Mediterranean, preventing migrations.  The hominoid &amp;#039;&amp;#039;[[Dryopithecus]]&amp;#039;&amp;#039; appeared in Europe {{Mya|12.5|Ma}} together with the Asian suid &amp;#039;&amp;#039;[[Propotamochoerus]]&amp;#039;&amp;#039;.  The rodent genus &amp;#039;&amp;#039;[[Cricetulodon]]&amp;#039;&amp;#039; is known from Western and Central Europe from MN 3 and from the end of MN 7/8 in Turkey and Greece.&amp;lt;ref name=&amp;quot;Koufos-etal-2005&amp;quot; /&amp;gt;&lt;br /&gt;
&lt;br /&gt;
{{Gallery&lt;br /&gt;
 |File:Dryopithecus fontani 3.JPG|&amp;#039;&amp;#039;Dryopithecus fontani&amp;#039;&amp;#039; mandible&lt;br /&gt;
 |File:Propotamochoerus giganteus.JPG|&amp;#039;&amp;#039;Propotamochoerus giganteus&amp;#039;&amp;#039;&lt;br /&gt;
}}&lt;br /&gt;
&lt;br /&gt;
== References ==&lt;br /&gt;
{{Reflist}}&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
{{Neogene Footer}}&lt;br /&gt;
&lt;br /&gt;
[[Category:Miocene]]&lt;br /&gt;
[[Category:Miocene geochronology]]&lt;br /&gt;
&lt;br /&gt;
{{geochronology-stub}}&lt;/div&gt;</summary>
		<author><name>imported&gt;GreenC bot</name></author>
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