0000000000175285

AUTHOR

Ana Moreno

showing 3 related works from this author

Effects of glaciation on karst hydrology and sedimentology during the Last Glacial Cycle: The case of Granito cave, Central Pyrenees (Spain)

2021

In Alpine regions, speleothem development on karst systems largely occurs during warm interglacial or interstadial phases due to their limited growth during cold stages. Still, recent attention has been given to the role of clastic sediments in caves, less dependent on temperature conditions. Yet, only a small number of caves worldwide preserve both speleothems and detrital deposits. Here we present an outstanding record of fine-grain laminated sediments and carbonate speleothems from the Granito cave (South Central Pyrenees, Spain) associated with seasonal to annual hydroclimatic pulses through the Last Glacial Cycle (LGC). Analysis of cave clastic facies together with new absolute dates o…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesGeochemistrySpeleothemHydrological responseStalagmite04 agricultural and veterinary sciences580 Plants (Botany)Upper Pleistocene01 natural sciencesCaveMoraineInterglacial040103 agronomy & agriculture0401 agriculture forestry and fisheriesGlacial periodCave sedimentsCentral PyreneesGeologyHolocenePhreaticGlacier dynamics0105 earth and related environmental sciencesEarth-Surface Processes
researchProduct

Upper pleistocene interstratal piping-cave speleogenesis: The seso cave system (central pyrenees, northern spain)

2015

The Seso Cave System (SCS, South Central Pyrenees, Northeastern Spain) develops in poorly soluble marly interstratum between limestone beds of Eocene age. We propose an innovative and singular pseudokarstic speleogenetic model under vadose conditions based on cave morphological evidence, physicochemical and mineralogical characteristics of the Eocene marly host rock, U-Th dating of cave deposits, and local geological and geomorphological information. Eocene marls are shown to be sensitive to dispersion processes supported by their high clay content and the high concentration of sodium and low electrical conductivity in the seepage water. Runoff inside the cave results from water that infilt…

Marine isotope stagegeographygeography.geographical_feature_categoryCave speleogenesisPleistocenePyreneesPseudokarstUpper PleistocenePaleontologyCaveVadose zoneMarlPeriod (geology)Glacial periodSpeleogenesisGeologyEarth-Surface ProcessesMarl dispersion
researchProduct

The SISAL database: a global resource to document oxygen and carbon isotope records from speleothems

2018

Stable isotope records from speleothems provide information on past climate changes, most particularly information that can be used to reconstruct past changes in precipitation and atmospheric circulation. These records are increasingly being used to provide “out-of-sample” evaluations of isotope-enabled climate models. SISAL (Speleothem Isotope Synthesis and Analysis) is an international working group of the Past Global Changes (PAGES) project. The working group aims to provide a comprehensive compilation of speleothem isotope records for climate reconstruction and model evaluation. The SISAL database contains data for individual speleothems, grouped by cave system. Stable isotopes of oxyg…

010506 paleontologyClimate Research010504 meteorology & atmospheric sciencesClimate changeSpeleothemF800010502 geochemistry & geophysicscomputer.software_genre01 natural sciencesKlimatforskningCavePaleoclimatologylcsh:Environmental sciences0105 earth and related environmental scienceslcsh:GE1-350geographygeography.geographical_feature_categoryDatabaseStable isotope ratiospeleothemsPALEOCLIMATOLOGIAlcsh:QE1-996.5lcsh:GeologyMetadata13. Climate actionGeneral Earth and Planetary SciencesEnvironmental scienceClimate modelcomputerChronologyEarth System Science Data
researchProduct