Pliocene volcanic terrain of the South Caucasus as a missing link in Eurasian palaeobiogeography: Dating and palaeoenvironments of vertebrate assemblages of the Jradzor locality, Armenia

被引:2
作者
Lazarev, Sergei [1 ,2 ,3 ]
Maul, Lutz Christian [4 ]
Kuiper, Klaudia [5 ]
Becker, Damien [1 ,2 ]
Bukhsianidze, Maia [6 ]
Hovakimyan, Hayk [7 ]
Sahakyan, Lilit
Vasilyan, Davit [1 ,2 ]
机构
[1] Univ Fribourg, Dept Geosci, Chemin Musee 6, CH-1700 Fribourg, Switzerland
[2] JURASS Museum, Route Fontenais 21, CH-2900 Porrentruy, Switzerland
[3] Univ Utrecht, Dept Earth Sci, Princetonlaan 8A, NL-3584 CB Utrecht, Netherlands
[4] Senckenberg Res Inst, Res Stn Quaternary Palaeontol Weimar, Jakobskirchhof 4, D-99423 Weimar, Germany
[5] Vrije Univ Amsterdam, Fac Sci, Dept Earth Sci, Boelelaan 1085, NL-1081 HV Amsterdam, Netherlands
[6] Georgian Natl Museum, Purtseladze St 3, Tbilisi 0105, Georgia
[7] Natl Acad Sci Republ Armenia, Inst Geol Sci, Marshal Baghramyan Ave 24a, Yerevan 0019, Armenia
关键词
South Caucasus; Pliocene; MN15; Vertebrate fauna; Pyroclastic density currents; COLLISION ZONE MAGMATISM; LESSER CAUCASUS; QUATERNARY VOLCANISM; PYROCLASTIC FLOW; EVOLUTION; MIOCENE; GEOCHRONOLOGY; PLEISTOCENE; DEPOSITS; GEORGIA;
D O I
10.1016/j.palaeo.2023.111685
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Cenozoic faunal exchanges between Europe, Asia, Africa and America played a key role in shaping modern-day Eurasian ecosystems with dispersal pathways controlled by the dynamics of natural palaeogeographic barriers (e. g., deserts, isthmuses, large water bodies, etc.). The South Caucasus is a mountainous region between Asia and Europe, which served as an important dispersal route during the late Cenozoic for the intercontinental exchanges of diverse terrestrial vertebrates. The Pliocene geology of this region is dominated by volcanic and volcaniclastic deposits that are generally not favourable for fossil preservation. However, a few rich fossil vertebrate faunas do occur although they lack comprehensive palaeoenvironmental and age constraints. In this paper, we present an integrated study of the stratigraphy and palaeontology of the Jradzor section located in the Gegham volcanic province of Armenia, to improve knowledge of late Cenozoic dispersal pathways. The 57-m-thick succession comprises 19 fossiliferous horizons with at least 48 identified vertebrate taxa (excluding birds). The palaeoenvironmental reconstruction suggests that the succession was deposited within a short-lived dammed lake that was subject to pyroclastic density flows, and later evolved into soil catenas. Taphonomic observations indicate that pyroclastic flows caused a high mortality of small-size vertebrates in most fossiliferous horizons, while a catastrophic lahar buried the large vertebrate fauna. Multiproxy dating places the studied section between 4.3 and similar to 3.03 Ma and the mammalian fauna correlates to the MN15. Comparison with similar age localities from across the region shows that Jradzor comprises the most continuous Pliocene succession with the highest number of fossil taxa and fills the MN15 interregional gap. The rich fossil vertebrate faunas have Asian and primarily European affinities. Findings show that the South Caucasus was a significant dispersal route for terrestrial vertebrates between Europe, Asia and Africa, and is of crucial importance for understanding Eurasian palaeogeography.
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