Time lag between deformation and seismicity along monogenetic volcanic unrest periods: The case of El Hierro Island (Canary Islands)

2017 ◽  
Vol 44 (13) ◽  
pp. 6771-6777 ◽  
Author(s):  
Héctor Lamolda ◽  
Alicia Felpeto ◽  
Abelardo Bethencourt
2014 ◽  
Vol 119 (6) ◽  
pp. 5033-5051 ◽  
Author(s):  
S. Sainz-Maza Aparicio ◽  
J. Arnoso Sampedro ◽  
F. Gonzalez Montesinos ◽  
J. Martí Molist

2012 ◽  
Vol 39 (13) ◽  
pp. n/a-n/a ◽  
Author(s):  
C. López ◽  
M. J. Blanco ◽  
R. Abella ◽  
B. Brenes ◽  
V. M. Cabrera Rodríguez ◽  
...  

Geomorphology ◽  
2021 ◽  
Vol 381 ◽  
pp. 107661
Author(s):  
Mauro Rossi ◽  
Roberto Sarro ◽  
Paola Reichenbach ◽  
Rosa María Mateos

Author(s):  
Juan C. Santamarta ◽  
Luis E. Hernández-Gutiérrez ◽  
Jesica Rodríguez-Martín ◽  
Anastasia Hernández Alemán ◽  
José Luis Gutiérrez Villanueva ◽  
...  

2014 ◽  
Vol 199 (3) ◽  
pp. 1739-1750 ◽  
Author(s):  
Araceli García-Yeguas ◽  
Jesús M. Ibáñez ◽  
Ivan Koulakov ◽  
Andrey Jakovlev ◽  
M. Carmen Romero-Ruiz ◽  
...  

2013 ◽  
Vol 40 (12) ◽  
pp. 4411-4419 ◽  
Author(s):  
Alejandra C. Ordóñez ◽  
M. Arnay-de-la-Rosa ◽  
R. Fregel ◽  
A. Trujillo-Mederos ◽  
J. Pestano ◽  
...  

Author(s):  
Javier GONZÁLEZ-DIONIS ◽  
Carolina CASTILLO RUIZ ◽  
Penélope CRUZADO-CABALLERO ◽  
Elena CADAVID-MELERO ◽  
Vicente D. CRESPO

ABSTRACT Bats are one of the most abundant and important mammals in ecosystems. However, their fossil record is scarce and fragile, making them difficult to find. Accordingly, there is no record of this group in the volcanic islands of the mid-Atlantic Ocean apart from the Canary Islands. This paper studies the first bat fossil record of the Canary Islands (Spain). The material studied is found within two Quaternary lava tubes, Cueva de los Verdes on Lanzarote and Cueva Roja on the island of El Hierro. The dental and humeral morphology and biometry are analysed and compared with current specimens. Among our results we highlight the first fossil data of two species endemic to the islands of the mid-Atlantic Ocean, Plecotus teneriffae and Pipistrellus maderensis, the former from the Canary Islands and the latter from the Azores, Madeira and the Canary Islands. We also confirm the presence of Pipistrellus kuhlii in the fossil record of the island of Lanzarote. No differences are observed between the dental morphology of the current and the fossil populations of P. maderensis and Pl. teneriffae. In the case of P. kuhlii, the populations of the Canary Islands and the Iberian Peninsula show differences in the paraconule with respect to the populations from central Europe. Palaeoecological studies of these taxa suggest that these islands presented a similar habitat when the sites were formed to the present-day habitat.


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