Hostname: page-component-cd9895bd7-8ctnn Total loading time: 0 Render date: 2024-12-18T16:20:19.938Z Has data issue: false hasContentIssue false
  • English
  • Français

Stratigraphy, Chronology, and Paleoenvironmental Reconstruction of the Quaternary Sedimentary Infilling of a Volcanic Tube in Fuerteventura, Canary Islands

Published online by Cambridge University Press:  20 January 2017

Juan J. Coello ,
Carolina Castillo  and
Esther Martı́n González
Juan J. Coello
Affiliation:
Departamento de Edafologı́a y Geologı́a, Facultad de Biologı́a, Universidad de La Laguna, Avenida Astrofı́sico Fco. Sánchez, s/n, 38206, La Laguna, Tenerife, Spain
Carolina Castillo
Affiliation:
Departamento de Biologı́a Animal, Facultad de Biologı́a, Universidad de La Laguna, Avenida Astrofı́sico Fco. Sánchez, s/n, 38206, La Laguna, Tenerife, Spain
Esther Martı́n González
Affiliation:
Departamento de Biologı́a Animal, Facultad de Biologı́a, Universidad de La Laguna, Avenida Astrofı́sico Fco. Sánchez, s/n, 38206, La Laguna, Tenerife, Spain
Get access Rights & Permissions [Opens in a new window]

Abstract

La Cueva del Llano is a volcanic tube of Pleistocene age on Fuerteventura Island, in the Canary Islands. Part of it is infilled with sediments of external origin. These deposits are exceptional in stratigraphic complexity and thickness compared with other known tube infillings, and they comprise nine stratigraphic units deposited in five phases. In Phase I, which has not been dated, sedimentation of cinder from a nearby cone occurred. Phase II began ca. 16,830 ± 900 14C yr B.P., whereas phase IV dates to 9280 ± 370 14C yr B.P. The interpretation of sedimentary features shows that phases III and V correspond to a dry climate, similar to the present one, whereas the climate was much wetter during phases II and IV. This paleoclimatic sequence agrees with those suggested by the study of deposits formed in other sedimentary environments, not only in Fuerteventura but on other islands of the Canary group and the Sud-Maroc region.

Keywords

volcanic tubesQuaternary sedimentary infillingFuerteventuraCanary Islands
Type
Research Article
Information
Quaternary Research , Volume 52 , Issue 3 , November 1999 , pp. 360 - 368
Copyright
University of Washington

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Borges, P.A.V. (1994). Conservation status of the Azorean lava tubes and pits. Oromı́, P. Proceedings, 7th International Symposium on Vulcanospeleology. 15–23.Google Scholar
Carrascosa, M.C., López-Martı́nez, N. (1988). The house mouse from a prehistoric site in Fuerteventura (Canary Islands, Spain). Bonner Zoologische Beiträge. 39, 237–256.Google Scholar
Castillo, C., Coello, J.J., Martı́n, M., González, C.C., Estévez, A., Meneses, M.D. (1996). Tafonomı́a de las concentraciones óseas de vertebrados en los tubos volcánicos de Canarias: Implicaciones paleoecológicas. Meléndez, G., Blasco, M.F., Pérez, I. II Reunión de Tafonomı́a y Fosilización. Instituto Fernando el Católico, CSIC, Zaragoza., 89–95.Google Scholar
Coello, J., Cantagrel, J.M., Hernán, F., Fúster, J.M., Ibarrola, E., Ancochea, E., Casquet, C., Jamond, C., Dı́az de Terán, J.R., Cendrero, A. (1992). Evolution of the Eastern Volcanic Ridge of the Canary Islands based on new K-Ar data. Journal of Volcanology and Geothermal Research. 53, 251–274.Google Scholar
Criado, C. (1991). La Evolución del Relieve de Fuerteventura.Google Scholar
Criado, C., Hansen, A. (1996). El cono aluvial holoceno del Barranco de la Ballena (Las Palmas de Gran Canaria). Grandal, A., Pagés, J. IV Reunión de Geomorfologı́a. Sociedad Española de Geomorfologı́a, La Coruña., 261–270.Google Scholar
Fúster, J.M., Carracedo, J.C. (1979). Magnetic polarity mapping of Quaternary volcanic activity of Fuerteventura and Lanzarote. Estudios Geológicos. 35, 59–65.Google Scholar
Fúster, J.M., Cendrero, A., Gastesi, P., Ibarrola, E., López-Ruiz, J. (1968). Geologı́a y volcanologı́a de las Islas Canarias: Fuerteventura. Instituto Lucas Mallada, CSIC, Madrid.Google Scholar
Goslar, T., Pazdur, M.F. (1985). Contamination studies on mollusk shell samples. Radiocarbon. 27, 33–42.Google Scholar
Hernández, F., Lomoschitz, A., Meco, J., Sánchez-Velázquez, D., Del Toro, A. (1988). The archaeological site of Cueva de Villaverde (Fuerteventura): Holocene palaeoenvironment and human occupation in a volcanic tube. Petit-Maire, N. Deserts, Past and Future Evolution. CNRS Marseille, France., 166–178.Google Scholar
Howarth, F.G. (1973). The cavernicolous fauna of Hawaiian volcanoes. 1. Introduction. Pacific Insects. 15, 139–151.Google Scholar
Hutterer, R., Oromi, P. (1993). La rata gigante de la isla Santa Cruz. Bacallado, J.J., Ortea, J. Resultados Cientı́ficos del Proyecto Galápagos TFMC. 63–76.Google Scholar
James, H.F., Stafford, T.W. Jr., Steadman, D.W., Olson, S.L., Martin, P.S., Jull, A.J.T., McCoy, P.C. (1987). Radiocarbon dates on bones of extinct birds from Hawaii. Proceedings of the National Academy of Sciences USA. 84, 2350–2354.Google Scholar
Kittleman, L.R. (1979). Geological methods in studies of Quaternary tephra. Sheets, P.D., Grayson, D.K. Volcanic Activity and Human ecology. Academic Press, London., 49–82.Google Scholar
Martin, J.L., González, J.M., Hernández, J.J. (1988). El tubo volcánico de las Cuevas Negras. Estudio genético y geomorfológico. Tenerife. Islas Canarias. Spélaion. 4, 31–36.Google Scholar
Montoriol-Pous, J., Romero, M., Montserrat, A. (1979). Estudio vulcanoespeleológico de la Cueva de Don Justo (Isla de El Hierro, Canarias). Speleon. 25, 83–91.Google Scholar
Montserrat, A., Romero, M. (1980). Introducción al conocimiento vulcanoespeleológico de la Isla de Fuerteventura (Islas Canarias). Speleon. 26, 93–98.Google Scholar
MOP-UNESCO, (1975). Estudio Cientı́fico de los Recursos de Agua en las Islas Canarias. SPA/69/515, Madrid.Google Scholar
Olson, S.L., James, H.F. (1982). Fossil birds from the Hawaiian Islands: Evidence for wholesale extinction by man before western contact. Science. 217, 633–635.Google Scholar
Pazdur, A., Pazdur, M.F. (1986). Aparatura pomiarowa Laboratorium C-14 w Gliwicach. Doswiadczenia konstrukcyjne i eksploatacyjne (Equipment of Radiocarbon Laboratory in Gliwice. The construction and exploitation experiences). Zeszyty Nankowe Politechnii Slaskiej, Seria Matematyka-Fisyka, Zeszyt 46, Geochronometria. 1, 55–70.Google Scholar
Peterson, D.W., Holcomb, R.T., Tilling, R.I., Christiansen, R.L. (1994). Development of lava tubes in the light of observations at Mauna Ulu, Kilauea Volcano, Hawaii. Bulletin of Volcanology. 56, 343–360.Google Scholar
Petit-Maire, N., Delibrias, G., Meco, J., Pomel, S., Rosso, J.C. (1986). Paléoclimatologie des Canaries Orientales (Fuerteventura). Compte Rendu de l'Académie des Sciences Paris. 303, 1241–1246.Google Scholar
Petit-Maire, N., Delibrias, G., Meco, J., Pomel, S., Rosso, J.C. (1987). Paleoclimats de Ile de Fuerteventura (Archipel Canarien). Paleoecology of Africa. 18, 351–356.Google Scholar
Rando, J.C., Castillo, C. (1993). First data of the diet of the Barn Owl (Tyto cf. alba) in the Quaternary in Fuerteventura (Canary Islands). First Symposium Fauna and Flora of the Atlantic Islands. p. 51.Google Scholar
Rognon, P., Coudé-Gaussen, G. (1987). Reconstitution paléoclimatique à partir des sèdiments du Pleistocène supérieur et d l'Holocène du nord de Fuerteventura (Canaries). Zeitschrift für Geomorphologie N. F.. 31, 1–19.CrossRefGoogle Scholar
Rognon, P., Coudé-Gaussen, G. (1996). Changements dans les circulations atmosphérique et océanique a la latitude des Canaries et du Maroc entre les stades isotopiques 2 et 1. Quatemaire. 7, 197–206.Google Scholar
Steadman, D.W. (1986). Holocene Vertebrate Fossils from Isla Floreana, Galápagos.Google Scholar
Steadman, D.W., Stafford, T.W., Donahue, D.J., Tull, A.J.T. (1991). Chronology of Holocene Vertebrate Extinction in the Galápagos Islands. Quaternary Research. 36, 126–133.Google Scholar
Stuiver, M., Polach, H.A. (1977). Reporting of 14C data. Radiocarbon. 19, 355–357.CrossRefGoogle Scholar
Ueno, S.I. (1973). The fauna of the lava caves in the Far East. Proceedings of the 6th International Congress of Speleology. Olomuc, Czechoslovakia., p. 237–242.Google Scholar