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rft.atitle Chronology of Middle Pleistocene Coastal Karst Evolution and Relative Sea-Level Changes in Mallorca
rft.epage 420
rft.genre article
rft.issn 0749-0208
1551-5036
rft.issue 2
rft.jtitle Journal of Coastal Research
rft.tpages 12
rft.pages 408-420
rft.pub Allen Press Publishing
rft.date 2021-03-01
x.date 2021-03-01T00:00:00Z
rft.spage 408
rft.volume 37
abstract <p>Sea-level change affects the geomorphic evolution of littoral regions in multiple ways. In carbonate coastal regions, sea-level oscillations control the type and occurrence of karst processes such as mixing corrosion, speleothem deposition, and collapse. A variety of cave deposits exist above, below, and at sea level. Among these, the vadose speleothems can provide indirect constraints on maximum sea-level boundaries, record changes from vadose to phreatic phases as littoral groundwaters flood the caves due to sea-level rise, and document different coastal speleogenetic stages. Here, new U-series ages for speleothems from three sites along the eastern coast of Mallorca (Cala Falcó, Dimoni, and Sa Ferradura) are presented and used to discuss the effects of relative sea-level oscillations upon coastal karst evolution between ~1500 and ~440 kyr before present. The paleo-speleothem record provides new timeframes for periods of vadose conditions allowing to place some relative sea-level constraints in the western Mediterranean, particularly for the Marine Isotope Stages 16 to 12. Periodic sea-level oscillations following glacial/interglacial cycles caused morphological changes within the paleo-caves. The sequences of collapsed karst features and vadose speleothems, coupled with geomorphological evidence and previous published sea-level records, support an interpretation for the occurrence of breakdown events during cold intervals following MIS 11, 9, and 7 sea-level high stands. Further collapses and dismantling of caves happened after MIS 5 high sea stands and throughout the Holocene.</p>
authors Array ( [rft.aulast] => Lucia [rft.aufirst] => Giuseppe )
Array ( [rft.aulast] => Polyak [rft.aufirst] => Victor J. )
Array ( [rft.aulast] => Ginés [rft.aufirst] => Joaquín )
Array ( [rft.aulast] => Fornós [rft.aufirst] => Joan J. )
Array ( [rft.aulast] => Ginés [rft.aufirst] => Angel )
Array ( [rft.aulast] => Asmerom [rft.aufirst] => Yemane )
Array ( [rft.aulast] => Onac [rft.aufirst] => Bogdan P. )
languages eng
url https://www.jstor.org/stable/27000342
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author Lucia, Giuseppe, Polyak, Victor J., Ginés, Joaquín, Fornós, Joan J., Ginés, Angel, Asmerom, Yemane, Onac, Bogdan P.
author_facet Lucia, Giuseppe, Polyak, Victor J., Ginés, Joaquín, Fornós, Joan J., Ginés, Angel, Asmerom, Yemane, Onac, Bogdan P., Lucia, Giuseppe, Polyak, Victor J., Ginés, Joaquín, Fornós, Joan J., Ginés, Angel, Asmerom, Yemane, Onac, Bogdan P.
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container_title Journal of Coastal Research
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description <p>Sea-level change affects the geomorphic evolution of littoral regions in multiple ways. In carbonate coastal regions, sea-level oscillations control the type and occurrence of karst processes such as mixing corrosion, speleothem deposition, and collapse. A variety of cave deposits exist above, below, and at sea level. Among these, the vadose speleothems can provide indirect constraints on maximum sea-level boundaries, record changes from vadose to phreatic phases as littoral groundwaters flood the caves due to sea-level rise, and document different coastal speleogenetic stages. Here, new U-series ages for speleothems from three sites along the eastern coast of Mallorca (Cala Falcó, Dimoni, and Sa Ferradura) are presented and used to discuss the effects of relative sea-level oscillations upon coastal karst evolution between ~1500 and ~440 kyr before present. The paleo-speleothem record provides new timeframes for periods of vadose conditions allowing to place some relative sea-level constraints in the western Mediterranean, particularly for the Marine Isotope Stages 16 to 12. Periodic sea-level oscillations following glacial/interglacial cycles caused morphological changes within the paleo-caves. The sequences of collapsed karst features and vadose speleothems, coupled with geomorphological evidence and previous published sea-level records, support an interpretation for the occurrence of breakdown events during cold intervals following MIS 11, 9, and 7 sea-level high stands. Further collapses and dismantling of caves happened after MIS 5 high sea stands and throughout the Holocene.</p>
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imprint Allen Press Publishing, 2021
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spelling Lucia, Giuseppe Polyak, Victor J. Ginés, Joaquín Fornós, Joan J. Ginés, Angel Asmerom, Yemane Onac, Bogdan P. 0749-0208 1551-5036 Allen Press Publishing RESEARCH ARTICLES https://www.jstor.org/stable/27000342 <p>Sea-level change affects the geomorphic evolution of littoral regions in multiple ways. In carbonate coastal regions, sea-level oscillations control the type and occurrence of karst processes such as mixing corrosion, speleothem deposition, and collapse. A variety of cave deposits exist above, below, and at sea level. Among these, the vadose speleothems can provide indirect constraints on maximum sea-level boundaries, record changes from vadose to phreatic phases as littoral groundwaters flood the caves due to sea-level rise, and document different coastal speleogenetic stages. Here, new U-series ages for speleothems from three sites along the eastern coast of Mallorca (Cala Falcó, Dimoni, and Sa Ferradura) are presented and used to discuss the effects of relative sea-level oscillations upon coastal karst evolution between ~1500 and ~440 kyr before present. The paleo-speleothem record provides new timeframes for periods of vadose conditions allowing to place some relative sea-level constraints in the western Mediterranean, particularly for the Marine Isotope Stages 16 to 12. Periodic sea-level oscillations following glacial/interglacial cycles caused morphological changes within the paleo-caves. The sequences of collapsed karst features and vadose speleothems, coupled with geomorphological evidence and previous published sea-level records, support an interpretation for the occurrence of breakdown events during cold intervals following MIS 11, 9, and 7 sea-level high stands. Further collapses and dismantling of caves happened after MIS 5 high sea stands and throughout the Holocene.</p> Chronology of Middle Pleistocene Coastal Karst Evolution and Relative Sea-Level Changes in Mallorca Journal of Coastal Research
spellingShingle Lucia, Giuseppe, Polyak, Victor J., Ginés, Joaquín, Fornós, Joan J., Ginés, Angel, Asmerom, Yemane, Onac, Bogdan P., Journal of Coastal Research, Chronology of Middle Pleistocene Coastal Karst Evolution and Relative Sea-Level Changes in Mallorca, RESEARCH ARTICLES
title Chronology of Middle Pleistocene Coastal Karst Evolution and Relative Sea-Level Changes in Mallorca
title_full Chronology of Middle Pleistocene Coastal Karst Evolution and Relative Sea-Level Changes in Mallorca
title_fullStr Chronology of Middle Pleistocene Coastal Karst Evolution and Relative Sea-Level Changes in Mallorca
title_full_unstemmed Chronology of Middle Pleistocene Coastal Karst Evolution and Relative Sea-Level Changes in Mallorca
title_short Chronology of Middle Pleistocene Coastal Karst Evolution and Relative Sea-Level Changes in Mallorca
title_sort chronology of middle pleistocene coastal karst evolution and relative sea-level changes in mallorca
topic RESEARCH ARTICLES
url https://www.jstor.org/stable/27000342