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Chronology of Middle Pleistocene Coastal Karst Evolution and Relative Sea-Level Changes in Mallorca
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Journal Title: | Journal of Coastal Research |
---|---|
Authors and Corporations: | , , , , , , |
In: | Journal of Coastal Research, 37, 2021, 2, p. 408-420 |
Type of Resource: | E-Article |
Language: | English |
published: |
Allen Press Publishing
|
Subjects: |
finc.format |
ElectronicArticle |
---|---|
finc.mega_collection |
sid-55-col-jstorlife JSTOR Life Sciences Archive |
finc.id |
ai-55-aHR0cHM6Ly93d3cuanN0b3Iub3JnL3N0YWJsZS8yNzAwMDM0Mg |
finc.source_id |
55 |
ris.type |
EJOUR |
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 |
version |
0.9 |
x.subjects |
RESEARCH ARTICLES |
openURL |
url_ver=Z39.88-2004&ctx_ver=Z39.88-2004&ctx_enc=info%3Aofi%2Fenc%3AUTF-8&rfr_id=info%3Asid%2Fvufind.svn.sourceforge.net%3Agenerator&rft.title=Chronology+of+Middle+Pleistocene+Coastal+Karst+Evolution+and+Relative+Sea-Level+Changes+in+Mallorca&rft.date=2021-03-01&genre=article&issn=1551-5036&volume=37&issue=2&spage=408&epage=420&pages=408-420&jtitle=Journal+of+Coastal+Research&atitle=Chronology+of+Middle+Pleistocene+Coastal+Karst+Evolution+and+Relative+Sea-Level+Changes+in+Mallorca&aulast=Onac&aufirst=Bogdan+P.&rft.language%5B0%5D=eng |
SOLR | |
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access_facet | Electronic Resources |
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. |
author_sort | lucia, giuseppe |
branch_nrw | Electronic Resources |
collection | sid-55-col-jstorlife |
container_issue | 2 |
container_start_page | 408 |
container_title | Journal of Coastal Research |
container_volume | 37 |
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> |
facet_avail | Online |
format | ElectronicArticle |
format_de105 | Article, E-Article |
format_de14 | Article, E-Article |
format_de15 | Article, E-Article |
format_de520 | Article, E-Article |
format_de540 | Article, E-Article |
format_dech1 | Article, E-Article |
format_ded117 | Article, E-Article |
format_degla1 | E-Article |
format_del152 | Buch |
format_del189 | Article, E-Article |
format_dezi4 | Article |
format_dezwi2 | Article, E-Article |
format_finc | Article, E-Article |
format_nrw | Article, E-Article |
geogr_code | not assigned |
geogr_code_person | not assigned |
id | ai-55-aHR0cHM6Ly93d3cuanN0b3Iub3JnL3N0YWJsZS8yNzAwMDM0Mg |
imprint | Allen Press Publishing, 2021 |
imprint_str_mv | Allen Press Publishing, 2021 |
institution | DE-15, DE-D13, DE-14 |
issn | 0749-0208, 1551-5036 |
issn_str_mv | 0749-0208, 1551-5036 |
language | English |
last_indexed | 2023-03-02T09:27:10.832Z |
match_str | lucia2021chronologyofmiddlepleistocenecoastalkarstevolutionandrelativesealevelchangesinmallorca |
mega_collection | JSTOR Life Sciences Archive |
physical | 408-420 |
publishDate | 2021 |
publishDateSort | 2021 |
publisher | Allen Press Publishing |
recordtype | ai |
score | 18,660866 |
series | Journal of Coastal Research |
source_id | 55 |
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 |