Aliveri revisited, a biogeographical appraisal of the early Miocene mammals from the eastern Mediterranean

被引:19
作者
Ostende, Lars W. van den Hoek [1 ]
Mayda, Serdar [2 ]
Oliver, Adriana [3 ]
Madern, Anneke [1 ,4 ]
Hernandez-Ballarin, Veronica [3 ]
Pelaez-Campomanes, Pablo [3 ]
机构
[1] Naturalis Biodivers Ctr, NL-2333 CR Leiden, Netherlands
[2] EGE Univ, Nat Hist Museum, Izmir, Turkey
[3] CSIC, Museo Nacl Ciencias Nat, E-28006 Madrid, Spain
[4] Inst Catala Paleontol, Barcelona 08193, Spain
关键词
Biogeography; Migrations; Palaeoenvironments; Greece; Centre of origin; INSECTIVORE FAUNAS; SOUTHERN GERMANY; RODENT FAUNAS; EVIA; GREECE; ISLAND; ARTIODACTYLA; ANATOLIA; BASIN; PALEOECOLOGY;
D O I
10.1007/s12549-015-0199-7
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
At the time of its discovery, over 25 years ago, the Greek locality of Aliveri preserved the easternmost occurrence for the early Miocene of cricetodontine hamsters such as Cricetodon, Megacricetodon and Democricetodon. As knowledge on the early Miocene history of the eastern Mediterranean increased, the faunal composition became more enigmatic, because of the presence of typical European elements (Pseudotheridomys, Heterosorex, Plesiodimylus, Myxomygale), absent from Anatolia. Recently, the ungulates from the locality were rediscovered, expanding the faunal list with the equid Anchitherium and the pecorans Lagomeryx (two species), Eotragus and Palaeomerycidae gen. et sp. indet. In this paper, we examine the fauna of Aliveri in the light of the current state of knowledge. The assemblage is typical for MN 4, but is believed to pre-date European localities of that biochronological unit. Similarity with Anatolian MN 3 localities suggests that the origin of the fauna lies mostly in that region, whereas the major differences with European localities suggest relative isolation, in line with palaeogeographic reconstructions of the period. However, when isolation was lifted, a number of European elements were added to the local fauna, but, presumably because of an ecological barrier, did not move further into Anatolia. Migrations at the onset of MN 4 can explain the composition of the Greek fauna, but we are still far from completely understanding the complex history of the eastern Mediterranean during the early Miocene.
引用
收藏
页码:271 / 284
页数:14
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