A stalactite record of four relative sea-level highstands during the Middle Pleistocene Transition
Ice-sheet and sea-level fluctuations during the Early and Middle Pleistocene are as yet poorly understood. A stalactite from a karst cave in North West Sicily (Italy) provides the first evidence of four marine inundations that correspond to relative sea-level highstands at the time of the Middle Ple...
Published in: | Quaternary Science Reviews |
---|---|
Main Authors: | , , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2017
|
Subjects: | |
Online Access: | https://www.vliz.be/imisdocs/publications/00/314100.pdf |
id |
ftnioz:oai:imis.nioz.nl:288522 |
---|---|
record_format |
openpolar |
spelling |
ftnioz:oai:imis.nioz.nl:288522 2023-05-15T13:47:57+02:00 A stalactite record of four relative sea-level highstands during the Middle Pleistocene Transition Stocchi, P. Antonioli, F. Montagna, P. Pepe, F. Lo Presti, V. Caruso, A. Corradino, M. Dardanelli, G. Renda, P. Frank, N. Douville, E. Thil, F. de Boer, B. Ruggieri, R. Sciortino, R. Pierre, C. 2017 application/pdf https://www.vliz.be/imisdocs/publications/00/314100.pdf en eng info:eu-repo/semantics/altIdentifier/wos/000412266500006 info:eu-repo/semantics/altIdentifier/doi/doi.org/10.1016/j.quascirev.2017.08.008 https://www.vliz.be/imisdocs/publications/00/314100.pdf info:eu-repo/semantics/openAccess %3Ci%3EQuat.+Sci.+Rev.+173%3C%2Fi%3E%3A+92-100.+%3Ca+href%3D%22https%3A%2F%2Fdx.doi.org%2F10.1016%2Fj.quascirev.2017.08.008%22+target%3D%22_blank%22%3Ehttps%3A%2F%2Fdx.doi.org%2F10.1016%2Fj.quascirev.2017.08.008%3C%2Fa%3E info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2017 ftnioz https://doi.org/10.1016/j.quascirev.2017.08.008 2022-05-01T14:05:56Z Ice-sheet and sea-level fluctuations during the Early and Middle Pleistocene are as yet poorly understood. A stalactite from a karst cave in North West Sicily (Italy) provides the first evidence of four marine inundations that correspond to relative sea-level highstands at the time of the Middle Pleistocene Transition. The speleothem is located ∼97 m above mean sea level as result of Quaternary uplift. Its section reveals three marine hiatuses and a coral overgrowth that fixes the age of final marine ingression at 1.124 ± 0.2, thus making this speleothem the oldest stalactite with marine hiatuses ever studied to date. Scleractinian coral species witness light-limited conditions and water depth of 20–50 m. Integrating the coral-constrained depth with the geologically constrained uplift rate and an ensemble of RSL scenarios, we find that the age of the last marine ingression most likely coincides with Marine Isotope Stage 35 on the basis of a probabilistic assessment. Our findings are consistent with a significant Antarctic ice-sheet retreat. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet NIOZ Repository (Royal Netherlands Institute for Sea Research) Antarctic Quaternary Science Reviews 173 92 100 |
institution |
Open Polar |
collection |
NIOZ Repository (Royal Netherlands Institute for Sea Research) |
op_collection_id |
ftnioz |
language |
English |
description |
Ice-sheet and sea-level fluctuations during the Early and Middle Pleistocene are as yet poorly understood. A stalactite from a karst cave in North West Sicily (Italy) provides the first evidence of four marine inundations that correspond to relative sea-level highstands at the time of the Middle Pleistocene Transition. The speleothem is located ∼97 m above mean sea level as result of Quaternary uplift. Its section reveals three marine hiatuses and a coral overgrowth that fixes the age of final marine ingression at 1.124 ± 0.2, thus making this speleothem the oldest stalactite with marine hiatuses ever studied to date. Scleractinian coral species witness light-limited conditions and water depth of 20–50 m. Integrating the coral-constrained depth with the geologically constrained uplift rate and an ensemble of RSL scenarios, we find that the age of the last marine ingression most likely coincides with Marine Isotope Stage 35 on the basis of a probabilistic assessment. Our findings are consistent with a significant Antarctic ice-sheet retreat. |
format |
Article in Journal/Newspaper |
author |
Stocchi, P. Antonioli, F. Montagna, P. Pepe, F. Lo Presti, V. Caruso, A. Corradino, M. Dardanelli, G. Renda, P. Frank, N. Douville, E. Thil, F. de Boer, B. Ruggieri, R. Sciortino, R. Pierre, C. |
spellingShingle |
Stocchi, P. Antonioli, F. Montagna, P. Pepe, F. Lo Presti, V. Caruso, A. Corradino, M. Dardanelli, G. Renda, P. Frank, N. Douville, E. Thil, F. de Boer, B. Ruggieri, R. Sciortino, R. Pierre, C. A stalactite record of four relative sea-level highstands during the Middle Pleistocene Transition |
author_facet |
Stocchi, P. Antonioli, F. Montagna, P. Pepe, F. Lo Presti, V. Caruso, A. Corradino, M. Dardanelli, G. Renda, P. Frank, N. Douville, E. Thil, F. de Boer, B. Ruggieri, R. Sciortino, R. Pierre, C. |
author_sort |
Stocchi, P. |
title |
A stalactite record of four relative sea-level highstands during the Middle Pleistocene Transition |
title_short |
A stalactite record of four relative sea-level highstands during the Middle Pleistocene Transition |
title_full |
A stalactite record of four relative sea-level highstands during the Middle Pleistocene Transition |
title_fullStr |
A stalactite record of four relative sea-level highstands during the Middle Pleistocene Transition |
title_full_unstemmed |
A stalactite record of four relative sea-level highstands during the Middle Pleistocene Transition |
title_sort |
stalactite record of four relative sea-level highstands during the middle pleistocene transition |
publishDate |
2017 |
url |
https://www.vliz.be/imisdocs/publications/00/314100.pdf |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic Ice Sheet |
genre_facet |
Antarc* Antarctic Ice Sheet |
op_source |
%3Ci%3EQuat.+Sci.+Rev.+173%3C%2Fi%3E%3A+92-100.+%3Ca+href%3D%22https%3A%2F%2Fdx.doi.org%2F10.1016%2Fj.quascirev.2017.08.008%22+target%3D%22_blank%22%3Ehttps%3A%2F%2Fdx.doi.org%2F10.1016%2Fj.quascirev.2017.08.008%3C%2Fa%3E |
op_relation |
info:eu-repo/semantics/altIdentifier/wos/000412266500006 info:eu-repo/semantics/altIdentifier/doi/doi.org/10.1016/j.quascirev.2017.08.008 https://www.vliz.be/imisdocs/publications/00/314100.pdf |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1016/j.quascirev.2017.08.008 |
container_title |
Quaternary Science Reviews |
container_volume |
173 |
container_start_page |
92 |
op_container_end_page |
100 |
_version_ |
1766248048900440064 |