Systematics, palaeoecology and palaeobiogeography of the Neogene fossil sharks from the Azores (Northeast Atlantic)

被引:47
作者
Avila, Sergio P. [1 ,2 ]
Ramalho, Ricardo [3 ]
Vullo, Romain [4 ,5 ]
机构
[1] Univ Acores, InBIO Lab Assoc, Ctr Invest Biodiversidade & Recursos Genet, CIBIO, P-9501855 Ponta Delgada, Azores, Portugal
[2] Univ Acores, Dept Biol, Marine PalaeoBiogeog Working Grp,Univ Azores, MPB, P-9501855 Ponta Delgada, Azores, Portugal
[3] Univ Munster, Inst Geophys, D-48149 Munster 17, Germany
[4] Univ Rennes 1, Lab Paleontol, CNRS UMR 6118, F-35042 Rennes, France
[5] Museum Hist Nat, F-17000 La Rochelle, France
来源
ANNALES DE PALEONTOLOGIE | 2012年 / 98卷 / 03期
关键词
Elasmobranchii; Neoselachii; Neogene; Oceanic islands; Azores; NE Atlantic Ocean; SANTA-MARIA ISLAND; K-AR AGES; EARLY PLIOCENE; MIOCENE; PLEISTOCENE; RECORD; FAUNA;
D O I
10.1016/j.annpal.2012.04.001
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
The Azores Archipelago is a group of isolated islands located in the North Atlantic Ocean. One of these oceanic islands - Santa Maria - exhibits marine fossiliferous sediments of late Miocene/early Pliocene and also of Pleistocene age. Recent research provided new selachian fossil material, with three new records (Carcharias acutissima, Megaselachus megalodon, and Carcharhinus cf. leucas) increasing the number of fossil sharks reported from the Azores (Santa Maria Island) to seven species (Notorynchus primigenius, C. acutissima, Cosmopolitodus hastalis, Paratodus benedenii, Isurus oxyrinchus, M. megalodon, and C. cf. leucas). So far, no teeth of batoids or small sharks have been found despite the screen-washing of several sediment samples from Santa Maria. The Azorean Mio-Pliocene selachian fauna clearly differs from those described from sediments deposited on continental shelves, in which batoids and small benthic sharks (e.g., scyliorhinids) are usually well represented. During the late Miocene/early Pliocene, subtropical to warm-temperate seas were prevalent in the area of the Azores, as deduced from palaeontological, geological and isotopic data, all indicating a warmer climate than in the present. (C) 2012 Elsevier Masson SAS. All rights reserved.
引用
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页码:167 / 189
页数:23
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