Persististrombus coronatus (Mollusca: Strombidae) in the lower Pliocene of Santa Maria Island (Azores, NE Atlantic): Paleoecology, paleoclimatology and paleobiogeographic implications

被引:49
作者
Avila, Sergio P. [1 ,2 ]
Melo, Carlos [2 ,3 ]
Berning, Bjoern [4 ]
Cordeiro, Ricardo [1 ,2 ]
Landau, Bernard [5 ,6 ]
da Silva, Carlos Marques [6 ]
机构
[1] Univ Acores, Dept Biol, Ctr Invest Biodiversidade & Recursos Genet, CIBIO,InBIO Lab Associado,Polo Acores, P-9501801 Ponta Delgada, Acores, Portugal
[2] Univ Azores, MPB Marine PalaeoBiogeog Grp, Ponta Delgada, Portugal
[3] Univ Acores, Dept Geociencias, P-9501801 Ponta Delgada, Acores, Portugal
[4] Oberosterreich Landesmuseum, Geowissensch Sammlungen, A-4060 Leonding, Austria
[5] Naturalis Biodivers Ctr, Leiden, Netherlands
[6] Univ Lisbon, Fac Ciencias, Inst Dom Luiz, Dept Geol, P-1749016 Lisbon, Portugal
关键词
Strombidae; Persististrombus coronatus; Macaronesian islands; Paleobiogeographical molluscan provinces; Paleoclimatology; NE Atlantic; SEA-LEVEL; GEOCHEMICAL EVOLUTION; SYSTEMATICS; MIOCENE; COASTAL; BIOGEOGRAPHY; PREDATION; GASTROPOD; NEOGENE; WORLD;
D O I
10.1016/j.palaeo.2015.10.043
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The family Strombidae is one of the twenty-three families and subfamilies of gastropods associated with tropical environmental conditions, and therefore useful as a biogeographical and paleoclimatic proxy. Today, the strombid genus Persististrombus is represented in the NE Atlantic by a single species restricted to the tropical Mauritanian-Senegalese Province. This work reports the occurrence of Persististrombus coronatus from the lower Pliocene of Santa Maria Island in the Azores Archipelago. Based on this occurrence, and on the Mio-Pliocene fossil record of the NE Atlantic oceanic islands, paleoclimatological considerations are discussed, which allow, for the first time, to include the Azores and the other Macaronesian islands in a wider context of the NE Atlantic paleobiogeographical molluscan provinces. Late Miocene to present day molluscan biogeographic units, ranging in latitude from 60 degrees N down to 17 degrees S, are here defined and the boundaries of the proposed climatic zones are outlined. We suggest that during the upper Miocene-lower Pliocene, the paleoclimate at Santa Maria Island was drastically different from that seen at those latitudes today, with mean annual sea surface temperatures (SSTs) about 3.7 degrees C to 6.3 degrees C higher than the present-day 20.6 degrees C, and with mean monthly SSTs ranging from 20 degrees C to 28 degrees C, with six months with mean SSTs over 24 degrees C, conditions typical of a tropical setting. (C) 2015 Elsevier B.V. All rights reserved.
引用
收藏
页码:912 / 923
页数:12
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