Laminación anual en un espeleotema del Holoceno inferior (Cueva de Kaite, Complejo Kárstico de Ojo Guareña, Burgos). Implicaciones paleoclimáticas
Annual laminations have been recognized in a rapid-growing, early Holocene, calcite stalagmite from Kaite cave (Ojo Guareña Karst Complex, N Spain) using petrographic analysis and U/Th dating performed with inductively coupled plasma mass spectrometry (ICP-MS). Each lamination reflects the annual gr...
| Autores: | , , |
|---|---|
| Tipo de recurso: | artículo |
| Fecha de publicación: | 2004 |
| País: | España |
| Institución: | Universidad Complutense de Madrid (UCM) |
| Repositorio: | Docta Complutense |
| Idioma: | español |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/52558 |
| Acceso en línea: | https://hdl.handle.net/20.500.14352/52558 |
| Access Level: | acceso abierto |
| Palabra clave: | 551.7 56:551.8 Paleoclimate Speleothems Annual laminations Early Holocene N Spain Geología estratigráfica 2506.19 Estratigrafía |
| Sumario: | Annual laminations have been recognized in a rapid-growing, early Holocene, calcite stalagmite from Kaite cave (Ojo Guareña Karst Complex, N Spain) using petrographic analysis and U/Th dating performed with inductively coupled plasma mass spectrometry (ICP-MS). Each lamination reflects the annual growth of the speleothem, and the vertical changes in thickness of successive laminae are interpreted as changes in paleoprecipitation over the cave. |
|---|