HISPANA | Directorio nacional de recursos digitales > Dades de registre

Está en:  › Dades de registre

Linked Open Data

A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin

Identificadores del recurso

Spatola D., del Moral-Erencia J.D., Micallef A., Camerlenghi A., Garcia-Castellanos D., Gupta S., Bohorquez P., Gutscher M.-A., Bertoni C. A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin. Marine Geology, 430: 10633, 2020. https://doi.org/10.1016/j.margeo.2020.106337

0025-3227

10.1016/j.margeo.2020.106337

https://doi.org/10.1016/j.margeo.2020.106337

https://hdl.handle.net/10953/1346

Procedència

(RUJA: Repositorio Institucional de Producción Científica de la Universidad de Jaén)

Fitxa

Títol:: A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin
Tema:: Zanclean flood; Megaflood; Geophysics; Numerical modelling; Messinian salinity crisis; Mediterranean Sea
Descripció:: The Messinian salinity crisis was an extraordinary event that resulted in the deposition of kilometre-thick evaporite sequences in the Mediterranean Sea after the latter became disconnected from the world's oceans. The return to fully and stable marine conditions at the end of the crisis is still subject to debate. Three main hypotheses, based on geophysical and borehole data, onshore outcrops and climate simulations, have been put forward. These include a single-stage catastrophic flood, a two-step reflooding scenario, and an overspill of Paratethyan water followed by Atlantic inflow. In this study, two research questions are addressed: (i) Which event marked the termination of the Messinian salinity crisis? (ii) What was the sea level in the eastern Mediterranean Sea during this event? Geophysical data from the western Ionian Basin are integrated with numerical simulations to infer that the termination of the crisis consisted of a single-stage megaflood following a sea level drawdown of 1900 m. This megaflood deposited an extensive sedimentary body with a chaotic to transparent seismic signature at the base of the Malta Escarpment. Fine, well-sorted sediments are predicted to have been deposited within the thicker sections of the flood deposit, whereas a more variable distribution of coarser sediments is expected elsewhere. The north-western Ionian Basin hosts evidence of episodic post-Messinian salinity crisis slope instability events in the last ~1.8 Ma. The largest of these emplaced a >200 km3 deposit and is associated with failure of the head of Noto Canyon (offshore SE Sicily). Apart from unravelling the final phase of the Messinian salinity crisis and the ensuing stratigraphic evolution of the western Ionian Basin, our results are also relevant to better understand megafloods, which are some of the most catastrophic geological processes on Earth and Mars.; The article is based upon work from COST Action CA15103 “Uncovering the Mediterranean salt giant” (MEDSALT) supported by (COST European Cooperation in Science and Technology). We are indebted to the CUMECS-2, CUMECS-3 and CIRCEE-HR shipboard parties, captains, crew and technicians for their assistance during data collection. The oceanographic surveys were possible following permits issued by the Italian and Maltese authorities. SPECTRUM (now TGS) are kindly acknowledged for providing access to their seismic reflection data. The use of CROP seismic profiles has been licensed to OGS by CNR, Banca Dati CROP (www.crop.cnr.it). The authors would also like to thank Emerson Paradigm for the use of the OGS academic licenses of the ECHOS and Geodepth processing software, and IHS Markit for the OGS license of the Kingdom software. DS is funded by EMODnet Bathymetry, which is financed by the European Union under Regulation 508/2014 of the European Parliament and of the Council of 15 May 2014 on the European Maritime and Fisheries Fund. This work was also supported by the Spanish Ministry of Science, Innovation and Universities (MICINN/FEDER, EU) under Grant SEDRETO CGL2015–70736-R. J.D.d.M.E. was supported by the PhD scholarship BES-2016-079117 (MINECO/FSE, EU) from the Spanish National Programme for the Promotion of Talent and its Employability (call 2016). This project has received funding from the European Union's Horizon 2020 research and innovation programme under the Marie Skłodowska-Curie grant agreement No. 765256 (SaltGiant ITN).
Idioma:: English
Relació:: Marine Geology 2020; 430: 10633
Autor/Productor:: Spatola, Daniele; del Moral-Erencia, José D.; Micallef, Aaron; Camerlenghi, Angelo; García-Castellanos, Daniel; Gupta, Sanjeev; Bohórquez, Patricio; Gutscher, Marc-André; Bertoni, Claudia
Editor:: Elsevier
Drets:: Atribución-NoComercial-SinDerivadas 3.0 España; http://creativecommons.org/licenses/by-nc-nd/3.0/es/; info:eu-repo/semantics/openAccess
Data:: 2023-11-29T07:36:38Z; 2020-09-10
Tipo de recurso:: info:eu-repo/semantics/article; info:eu-repo/semantics/acceptedVersion
Format:: application/pdf

oai_dc

Descarregar XML

<?xml version="1.0" encoding="UTF-8" ?>

<oai_dc:dc schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
1. <dc:title>A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin</dc:title>
2. <dc:creator>Spatola, Daniele</dc:creator>
3. <dc:creator>del Moral-Erencia, José D.</dc:creator>
4. <dc:creator>Micallef, Aaron</dc:creator>
5. <dc:creator>Camerlenghi, Angelo</dc:creator>
6. <dc:creator>García-Castellanos, Daniel</dc:creator>
7. <dc:creator>Gupta, Sanjeev</dc:creator>
8. <dc:creator>Bohórquez, Patricio</dc:creator>
9. <dc:creator>Gutscher, Marc-André</dc:creator>
10. <dc:creator>Bertoni, Claudia</dc:creator>
11. <dc:subject>Zanclean flood</dc:subject>
12. <dc:subject>Megaflood</dc:subject>
13. <dc:subject>Geophysics</dc:subject>
14. <dc:subject>Numerical modelling</dc:subject>
15. <dc:subject>Messinian salinity crisis</dc:subject>
16. <dc:subject>Mediterranean Sea</dc:subject>
17. <dc:description>The Messinian salinity crisis was an extraordinary event that resulted in the deposition of kilometre-thick evaporite sequences in the Mediterranean Sea after the latter became disconnected from the world's oceans. The return to fully and stable marine conditions at the end of the crisis is still subject to debate. Three main hypotheses, based on geophysical and borehole data, onshore outcrops and climate simulations, have been put forward. These include a single-stage catastrophic flood, a two-step reflooding scenario, and an overspill of Paratethyan water followed by Atlantic inflow. In this study, two research questions are addressed: (i) Which event marked the termination of the Messinian salinity crisis? (ii) What was the sea level in the eastern Mediterranean Sea during this event? Geophysical data from the western Ionian Basin are integrated with numerical simulations to infer that the termination of the crisis consisted of a single-stage megaflood following a sea level drawdown of 1900 m. This megaflood deposited an extensive sedimentary body with a chaotic to transparent seismic signature at the base of the Malta Escarpment. Fine, well-sorted sediments are predicted to have been deposited within the thicker sections of the flood deposit, whereas a more variable distribution of coarser sediments is expected elsewhere. The north-western Ionian Basin hosts evidence of episodic post-Messinian salinity crisis slope instability events in the last ~1.8 Ma. The largest of these emplaced a >200 km3 deposit and is associated with failure of the head of Noto Canyon (offshore SE Sicily). Apart from unravelling the final phase of the Messinian salinity crisis and the ensuing stratigraphic evolution of the western Ionian Basin, our results are also relevant to better understand megafloods, which are some of the most catastrophic geological processes on Earth and Mars.</dc:description>
18. <dc:description>The article is based upon work from COST Action CA15103 “Uncovering the Mediterranean salt giant” (MEDSALT) supported by (COST European Cooperation in Science and Technology). We are indebted to the CUMECS-2, CUMECS-3 and CIRCEE-HR shipboard parties, captains, crew and technicians for their assistance during data collection. The oceanographic surveys were possible following permits issued by the Italian and Maltese authorities. SPECTRUM (now TGS) are kindly acknowledged for providing access to their seismic reflection data. The use of CROP seismic profiles has been licensed to OGS by CNR, Banca Dati CROP (www.crop.cnr.it). The authors would also like to thank Emerson Paradigm for the use of the OGS academic licenses of the ECHOS and Geodepth processing software, and IHS Markit for the OGS license of the Kingdom software. DS is funded by EMODnet Bathymetry, which is financed by the European Union under Regulation 508/2014 of the European Parliament and of the Council of 15 May 2014 on the European Maritime and Fisheries Fund. This work was also supported by the Spanish Ministry of Science, Innovation and Universities (MICINN/FEDER, EU) under Grant SEDRETO CGL2015–70736-R. J.D.d.M.E. was supported by the PhD scholarship BES-2016-079117 (MINECO/FSE, EU) from the Spanish National Programme for the Promotion of Talent and its Employability (call 2016). This project has received funding from the European Union's Horizon 2020 research and innovation programme under the Marie Skłodowska-Curie grant agreement No. 765256 (SaltGiant ITN).</dc:description>
19. <dc:date>2023-11-29T07:36:38Z</dc:date>
20. <dc:date>2023-11-29T07:36:38Z</dc:date>
21. <dc:date>2020-09-10</dc:date>
22. <dc:type>info:eu-repo/semantics/article</dc:type>
23. <dc:type>info:eu-repo/semantics/acceptedVersion</dc:type>
24. <dc:identifier>Spatola D., del Moral-Erencia J.D., Micallef A., Camerlenghi A., Garcia-Castellanos D., Gupta S., Bohorquez P., Gutscher M.-A., Bertoni C. A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin. Marine Geology, 430: 10633, 2020. https://doi.org/10.1016/j.margeo.2020.106337</dc:identifier>
25. <dc:identifier>0025-3227</dc:identifier>
26. <dc:identifier>10.1016/j.margeo.2020.106337</dc:identifier>
27. <dc:identifier>https://doi.org/10.1016/j.margeo.2020.106337</dc:identifier>
28. <dc:identifier>https://hdl.handle.net/10953/1346</dc:identifier>
29. <dc:language>eng</dc:language>
30. <dc:relation>Marine Geology 2020; 430: 10633</dc:relation>
31. <dc:rights>Atribución-NoComercial-SinDerivadas 3.0 España</dc:rights>
32. <dc:rights>http://creativecommons.org/licenses/by-nc-nd/3.0/es/</dc:rights>
33. <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
34. <dc:format>application/pdf</dc:format>
35. <dc:publisher>Elsevier</dc:publisher>
</oai_dc:dc>

didl

Descarregar XML

<?xml version="1.0" encoding="UTF-8" ?>

<d:DIDL schemaLocation="urn:mpeg:mpeg21:2002:02-DIDL-NS http://standards.iso.org/ittf/PubliclyAvailableStandards/MPEG-21_schema_files/did/didl.xsd">
1. <d:DIDLInfo>
  1. <dcterms:created schemaLocation="http://purl.org/dc/terms/ http://dublincore.org/schemas/xmls/qdc/dcterms.xsd">2023-11-29T07:36:38Z</dcterms:created>
  </d:DIDLInfo>
2. <d:Item id="hdl_10953_1346">
  1. <d:Descriptor>
    1. <d:Statement mimeType="application/xml; charset=utf-8">
      1. <dii:Identifier schemaLocation="urn:mpeg:mpeg21:2002:01-DII-NS http://standards.iso.org/ittf/PubliclyAvailableStandards/MPEG-21_schema_files/dii/dii.xsd">urn:hdl:10953/1346</dii:Identifier>
      </d:Statement>
    </d:Descriptor>
  2. <d:Descriptor>
    1. <d:Statement mimeType="application/xml; charset=utf-8">
      1. <oai_dc:dc schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
        <dc:title>A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin</dc:title>
        <dc:creator>Spatola, Daniele</dc:creator>
        <dc:creator>del Moral-Erencia, José D.</dc:creator>
        <dc:creator>Micallef, Aaron</dc:creator>
        <dc:creator>Camerlenghi, Angelo</dc:creator>
        <dc:creator>García-Castellanos, Daniel</dc:creator>
        <dc:creator>Gupta, Sanjeev</dc:creator>
        <dc:creator>Bohórquez, Patricio</dc:creator>
        <dc:creator>Gutscher, Marc-André</dc:creator>
        <dc:creator>Bertoni, Claudia</dc:creator>
        <dc:subject>Zanclean flood</dc:subject>
        <dc:subject>Megaflood</dc:subject>
        <dc:subject>Geophysics</dc:subject>
        <dc:subject>Numerical modelling</dc:subject>
        <dc:subject>Messinian salinity crisis</dc:subject>
        <dc:subject>Mediterranean Sea</dc:subject>
        <dc:description>The Messinian salinity crisis was an extraordinary event that resulted in the deposition of kilometre-thick evaporite sequences in the Mediterranean Sea after the latter became disconnected from the world's oceans. The return to fully and stable marine conditions at the end of the crisis is still subject to debate. Three main hypotheses, based on geophysical and borehole data, onshore outcrops and climate simulations, have been put forward. These include a single-stage catastrophic flood, a two-step reflooding scenario, and an overspill of Paratethyan water followed by Atlantic inflow. In this study, two research questions are addressed: (i) Which event marked the termination of the Messinian salinity crisis? (ii) What was the sea level in the eastern Mediterranean Sea during this event? Geophysical data from the western Ionian Basin are integrated with numerical simulations to infer that the termination of the crisis consisted of a single-stage megaflood following a sea level drawdown of 1900 m. This megaflood deposited an extensive sedimentary body with a chaotic to transparent seismic signature at the base of the Malta Escarpment. Fine, well-sorted sediments are predicted to have been deposited within the thicker sections of the flood deposit, whereas a more variable distribution of coarser sediments is expected elsewhere. The north-western Ionian Basin hosts evidence of episodic post-Messinian salinity crisis slope instability events in the last ~1.8 Ma. The largest of these emplaced a >200 km3 deposit and is associated with failure of the head of Noto Canyon (offshore SE Sicily). Apart from unravelling the final phase of the Messinian salinity crisis and the ensuing stratigraphic evolution of the western Ionian Basin, our results are also relevant to better understand megafloods, which are some of the most catastrophic geological processes on Earth and Mars.</dc:description>
        <dc:date>2023-11-29T07:36:38Z</dc:date>
        <dc:date>2023-11-29T07:36:38Z</dc:date>
        <dc:date>2020-09-10</dc:date>
        <dc:type>info:eu-repo/semantics/article</dc:type>
        <dc:identifier>Spatola D., del Moral-Erencia J.D., Micallef A., Camerlenghi A., Garcia-Castellanos D., Gupta S., Bohorquez P., Gutscher M.-A., Bertoni C. A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin. Marine Geology, 430: 10633, 2020. https://doi.org/10.1016/j.margeo.2020.106337</dc:identifier>
        <dc:identifier>0025-3227</dc:identifier>
        <dc:identifier>10.1016/j.margeo.2020.106337</dc:identifier>
        <dc:identifier>https://doi.org/10.1016/j.margeo.2020.106337</dc:identifier>
        <dc:identifier>https://hdl.handle.net/10953/1346</dc:identifier>
        <dc:language>eng</dc:language>
        <dc:relation>Marine Geology 2020; 430: 10633</dc:relation>
        <dc:rights>http://creativecommons.org/licenses/by-nc-nd/3.0/es/</dc:rights>
        <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
        <dc:rights>Atribución-NoComercial-SinDerivadas 3.0 España</dc:rights>
        <dc:publisher>Elsevier</dc:publisher>
        </oai_dc:dc>
      </d:Statement>
    </d:Descriptor>
  3. <d:Component id="10953_1346_1">
    1. <d:Resource mimeType="application/pdf" ref="http://ruja.ujaen.es/jspui/bitstream/10953/1346/1/MG2020.pdf" />
    </d:Component>
  </d:Item>
</d:DIDL>

dim

Descarregar XML

<?xml version="1.0" encoding="UTF-8" ?>

<dim:dim schemaLocation="http://www.dspace.org/xmlns/dspace/dim http://www.dspace.org/schema/dim.xsd">
1. <dim:field element="contributor" mdschema="dc" qualifier="author">Spatola, Daniele</dim:field>
2. <dim:field element="contributor" mdschema="dc" qualifier="author">del Moral-Erencia, José D.</dim:field>
3. <dim:field element="contributor" mdschema="dc" qualifier="author">Micallef, Aaron</dim:field>
4. <dim:field element="contributor" mdschema="dc" qualifier="author">Camerlenghi, Angelo</dim:field>
5. <dim:field element="contributor" mdschema="dc" qualifier="author">García-Castellanos, Daniel</dim:field>
6. <dim:field element="contributor" mdschema="dc" qualifier="author">Gupta, Sanjeev</dim:field>
7. <dim:field element="contributor" mdschema="dc" qualifier="author">Bohórquez, Patricio</dim:field>
8. <dim:field element="contributor" mdschema="dc" qualifier="author">Gutscher, Marc-André</dim:field>
9. <dim:field element="contributor" mdschema="dc" qualifier="author">Bertoni, Claudia</dim:field>
10. <dim:field element="date" mdschema="dc" qualifier="accessioned">2023-11-29T07:36:38Z</dim:field>
11. <dim:field element="date" mdschema="dc" qualifier="available">2023-11-29T07:36:38Z</dim:field>
12. <dim:field element="date" mdschema="dc" qualifier="issued">2020-09-10</dim:field>
13. <dim:field element="identifier" lang="es_ES" mdschema="dc" qualifier="citation">Spatola D., del Moral-Erencia J.D., Micallef A., Camerlenghi A., Garcia-Castellanos D., Gupta S., Bohorquez P., Gutscher M.-A., Bertoni C. A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin. Marine Geology, 430: 10633, 2020. https://doi.org/10.1016/j.margeo.2020.106337</dim:field>
14. <dim:field element="identifier" lang="es_ES" mdschema="dc" qualifier="issn">0025-3227</dim:field>
15. <dim:field element="identifier" lang="es_ES" mdschema="dc" qualifier="other">10.1016/j.margeo.2020.106337</dim:field>
16. <dim:field element="identifier" lang="es_ES" mdschema="dc" qualifier="uri">https://doi.org/10.1016/j.margeo.2020.106337</dim:field>
17. <dim:field element="identifier" mdschema="dc" qualifier="uri">https://hdl.handle.net/10953/1346</dim:field>
18. <dim:field element="description" lang="es_ES" mdschema="dc" qualifier="abstract">The Messinian salinity crisis was an extraordinary event that resulted in the deposition of kilometre-thick evaporite sequences in the Mediterranean Sea after the latter became disconnected from the world's oceans. The return to fully and stable marine conditions at the end of the crisis is still subject to debate. Three main hypotheses, based on geophysical and borehole data, onshore outcrops and climate simulations, have been put forward. These include a single-stage catastrophic flood, a two-step reflooding scenario, and an overspill of Paratethyan water followed by Atlantic inflow. In this study, two research questions are addressed: (i) Which event marked the termination of the Messinian salinity crisis? (ii) What was the sea level in the eastern Mediterranean Sea during this event? Geophysical data from the western Ionian Basin are integrated with numerical simulations to infer that the termination of the crisis consisted of a single-stage megaflood following a sea level drawdown of 1900 m. This megaflood deposited an extensive sedimentary body with a chaotic to transparent seismic signature at the base of the Malta Escarpment. Fine, well-sorted sediments are predicted to have been deposited within the thicker sections of the flood deposit, whereas a more variable distribution of coarser sediments is expected elsewhere. The north-western Ionian Basin hosts evidence of episodic post-Messinian salinity crisis slope instability events in the last ~1.8 Ma. The largest of these emplaced a >200 km3 deposit and is associated with failure of the head of Noto Canyon (offshore SE Sicily). Apart from unravelling the final phase of the Messinian salinity crisis and the ensuing stratigraphic evolution of the western Ionian Basin, our results are also relevant to better understand megafloods, which are some of the most catastrophic geological processes on Earth and Mars.</dim:field>
19. <dim:field element="description" lang="es_ES" mdschema="dc" qualifier="sponsorship">The article is based upon work from COST Action CA15103 “Uncovering the Mediterranean salt giant” (MEDSALT) supported by (COST European Cooperation in Science and Technology). We are indebted to the CUMECS-2, CUMECS-3 and CIRCEE-HR shipboard parties, captains, crew and technicians for their assistance during data collection. The oceanographic surveys were possible following permits issued by the Italian and Maltese authorities. SPECTRUM (now TGS) are kindly acknowledged for providing access to their seismic reflection data. The use of CROP seismic profiles has been licensed to OGS by CNR, Banca Dati CROP (www.crop.cnr.it). The authors would also like to thank Emerson Paradigm for the use of the OGS academic licenses of the ECHOS and Geodepth processing software, and IHS Markit for the OGS license of the Kingdom software. DS is funded by EMODnet Bathymetry, which is financed by the European Union under Regulation 508/2014 of the European Parliament and of the Council of 15 May 2014 on the European Maritime and Fisheries Fund. This work was also supported by the Spanish Ministry of Science, Innovation and Universities (MICINN/FEDER, EU) under Grant SEDRETO CGL2015–70736-R. J.D.d.M.E. was supported by the PhD scholarship BES-2016-079117 (MINECO/FSE, EU) from the Spanish National Programme for the Promotion of Talent and its Employability (call 2016). This project has received funding from the European Union's Horizon 2020 research and innovation programme under the Marie Skłodowska-Curie grant agreement No. 765256 (SaltGiant ITN).</dim:field>
20. <dim:field element="language" lang="es_ES" mdschema="dc" qualifier="iso">eng</dim:field>
21. <dim:field element="publisher" lang="es_ES" mdschema="dc">Elsevier</dim:field>
22. <dim:field element="relation" lang="es_ES" mdschema="dc" qualifier="ispartof">Marine Geology 2020; 430: 10633</dim:field>
23. <dim:field element="rights" lang="*" mdschema="dc">Atribución-NoComercial-SinDerivadas 3.0 España</dim:field>
24. <dim:field element="rights" lang="*" mdschema="dc" qualifier="uri">http://creativecommons.org/licenses/by-nc-nd/3.0/es/</dim:field>
25. <dim:field element="rights" lang="es_ES" mdschema="dc" qualifier="accessRights">info:eu-repo/semantics/openAccess</dim:field>
26. <dim:field element="subject" lang="es_ES" mdschema="dc">Zanclean flood</dim:field>
27. <dim:field element="subject" lang="es_ES" mdschema="dc">Megaflood</dim:field>
28. <dim:field element="subject" lang="es_ES" mdschema="dc">Geophysics</dim:field>
29. <dim:field element="subject" lang="es_ES" mdschema="dc">Numerical modelling</dim:field>
30. <dim:field element="subject" lang="es_ES" mdschema="dc">Messinian salinity crisis</dim:field>
31. <dim:field element="subject" lang="es_ES" mdschema="dc">Mediterranean Sea</dim:field>
32. <dim:field element="title" lang="es_ES" mdschema="dc">A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin</dim:field>
33. <dim:field element="type" lang="es_ES" mdschema="dc">info:eu-repo/semantics/article</dim:field>
34. <dim:field element="type" lang="es_ES" mdschema="dc" qualifier="version">info:eu-repo/semantics/acceptedVersion</dim:field>
</dim:dim>

etdms

Descarregar XML

<?xml version="1.0" encoding="UTF-8" ?>

<thesis schemaLocation="http://www.ndltd.org/standards/metadata/etdms/1.0/ http://www.ndltd.org/standards/metadata/etdms/1.0/etdms.xsd">
1. <title>A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin</title>
2. <creator>Spatola, Daniele</creator>
3. <creator>del Moral-Erencia, José D.</creator>
4. <creator>Micallef, Aaron</creator>
5. <creator>Camerlenghi, Angelo</creator>
6. <creator>García-Castellanos, Daniel</creator>
7. <creator>Gupta, Sanjeev</creator>
8. <creator>Bohórquez, Patricio</creator>
9. <creator>Gutscher, Marc-André</creator>
10. <creator>Bertoni, Claudia</creator>
11. <subject>Zanclean flood</subject>
12. <subject>Megaflood</subject>
13. <subject>Geophysics</subject>
14. <subject>Numerical modelling</subject>
15. <subject>Messinian salinity crisis</subject>
16. <subject>Mediterranean Sea</subject>
17. <description>The Messinian salinity crisis was an extraordinary event that resulted in the deposition of kilometre-thick evaporite sequences in the Mediterranean Sea after the latter became disconnected from the world's oceans. The return to fully and stable marine conditions at the end of the crisis is still subject to debate. Three main hypotheses, based on geophysical and borehole data, onshore outcrops and climate simulations, have been put forward. These include a single-stage catastrophic flood, a two-step reflooding scenario, and an overspill of Paratethyan water followed by Atlantic inflow. In this study, two research questions are addressed: (i) Which event marked the termination of the Messinian salinity crisis? (ii) What was the sea level in the eastern Mediterranean Sea during this event? Geophysical data from the western Ionian Basin are integrated with numerical simulations to infer that the termination of the crisis consisted of a single-stage megaflood following a sea level drawdown of 1900 m. This megaflood deposited an extensive sedimentary body with a chaotic to transparent seismic signature at the base of the Malta Escarpment. Fine, well-sorted sediments are predicted to have been deposited within the thicker sections of the flood deposit, whereas a more variable distribution of coarser sediments is expected elsewhere. The north-western Ionian Basin hosts evidence of episodic post-Messinian salinity crisis slope instability events in the last ~1.8 Ma. The largest of these emplaced a >200 km3 deposit and is associated with failure of the head of Noto Canyon (offshore SE Sicily). Apart from unravelling the final phase of the Messinian salinity crisis and the ensuing stratigraphic evolution of the western Ionian Basin, our results are also relevant to better understand megafloods, which are some of the most catastrophic geological processes on Earth and Mars.</description>
18. <date>2023-11-29</date>
19. <date>2023-11-29</date>
20. <date>2020-09-10</date>
21. <type>info:eu-repo/semantics/article</type>
22. <identifier>Spatola D., del Moral-Erencia J.D., Micallef A., Camerlenghi A., Garcia-Castellanos D., Gupta S., Bohorquez P., Gutscher M.-A., Bertoni C. A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin. Marine Geology, 430: 10633, 2020. https://doi.org/10.1016/j.margeo.2020.106337</identifier>
23. <identifier>0025-3227</identifier>
24. <identifier>10.1016/j.margeo.2020.106337</identifier>
25. <identifier>https://doi.org/10.1016/j.margeo.2020.106337</identifier>
26. <identifier>https://hdl.handle.net/10953/1346</identifier>
27. <language>eng</language>
28. <relation>Marine Geology 2020; 430: 10633</relation>
29. <rights>http://creativecommons.org/licenses/by-nc-nd/3.0/es/</rights>
30. <rights>info:eu-repo/semantics/openAccess</rights>
31. <rights>Atribución-NoComercial-SinDerivadas 3.0 España</rights>
32. <publisher>Elsevier</publisher>
</thesis>

marc

Descarregar XML

<?xml version="1.0" encoding="UTF-8" ?>

<record schemaLocation="http://www.loc.gov/MARC21/slim http://www.loc.gov/standards/marcxml/schema/MARC21slim.xsd">
1. <leader>00925njm 22002777a 4500</leader>
2. <datafield ind1=" " ind2=" " tag="042">
  1. <subfield code="a">dc</subfield>
  </datafield>
3. <datafield ind1=" " ind2=" " tag="720">
  1. <subfield code="a">Spatola, Daniele</subfield>
  2. <subfield code="e">author</subfield>
  </datafield>
4. <datafield ind1=" " ind2=" " tag="720">
  1. <subfield code="a">del Moral-Erencia, José D.</subfield>
  2. <subfield code="e">author</subfield>
  </datafield>
5. <datafield ind1=" " ind2=" " tag="720">
  1. <subfield code="a">Micallef, Aaron</subfield>
  2. <subfield code="e">author</subfield>
  </datafield>
6. <datafield ind1=" " ind2=" " tag="720">
  1. <subfield code="a">Camerlenghi, Angelo</subfield>
  2. <subfield code="e">author</subfield>
  </datafield>
7. <datafield ind1=" " ind2=" " tag="720">
  1. <subfield code="a">García-Castellanos, Daniel</subfield>
  2. <subfield code="e">author</subfield>
  </datafield>
8. <datafield ind1=" " ind2=" " tag="720">
  1. <subfield code="a">Gupta, Sanjeev</subfield>
  2. <subfield code="e">author</subfield>
  </datafield>
9. <datafield ind1=" " ind2=" " tag="720">
  1. <subfield code="a">Bohórquez, Patricio</subfield>
  2. <subfield code="e">author</subfield>
  </datafield>
10. <datafield ind1=" " ind2=" " tag="720">
  1. <subfield code="a">Gutscher, Marc-André</subfield>
  2. <subfield code="e">author</subfield>
  </datafield>
11. <datafield ind1=" " ind2=" " tag="720">
  1. <subfield code="a">Bertoni, Claudia</subfield>
  2. <subfield code="e">author</subfield>
  </datafield>
12. <datafield ind1=" " ind2=" " tag="260">
  1. <subfield code="c">2020-09-10</subfield>
  </datafield>
13. <datafield ind1=" " ind2=" " tag="520">
  1. <subfield code="a">The Messinian salinity crisis was an extraordinary event that resulted in the deposition of kilometre-thick evaporite sequences in the Mediterranean Sea after the latter became disconnected from the world's oceans. The return to fully and stable marine conditions at the end of the crisis is still subject to debate. Three main hypotheses, based on geophysical and borehole data, onshore outcrops and climate simulations, have been put forward. These include a single-stage catastrophic flood, a two-step reflooding scenario, and an overspill of Paratethyan water followed by Atlantic inflow. In this study, two research questions are addressed: (i) Which event marked the termination of the Messinian salinity crisis? (ii) What was the sea level in the eastern Mediterranean Sea during this event? Geophysical data from the western Ionian Basin are integrated with numerical simulations to infer that the termination of the crisis consisted of a single-stage megaflood following a sea level drawdown of 1900 m. This megaflood deposited an extensive sedimentary body with a chaotic to transparent seismic signature at the base of the Malta Escarpment. Fine, well-sorted sediments are predicted to have been deposited within the thicker sections of the flood deposit, whereas a more variable distribution of coarser sediments is expected elsewhere. The north-western Ionian Basin hosts evidence of episodic post-Messinian salinity crisis slope instability events in the last ~1.8 Ma. The largest of these emplaced a >200 km3 deposit and is associated with failure of the head of Noto Canyon (offshore SE Sicily). Apart from unravelling the final phase of the Messinian salinity crisis and the ensuing stratigraphic evolution of the western Ionian Basin, our results are also relevant to better understand megafloods, which are some of the most catastrophic geological processes on Earth and Mars.</subfield>
  </datafield>
14. <datafield ind1="8" ind2=" " tag="024">
  1. <subfield code="a">Spatola D., del Moral-Erencia J.D., Micallef A., Camerlenghi A., Garcia-Castellanos D., Gupta S., Bohorquez P., Gutscher M.-A., Bertoni C. A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin. Marine Geology, 430: 10633, 2020. https://doi.org/10.1016/j.margeo.2020.106337</subfield>
  </datafield>
15. <datafield ind1="8" ind2=" " tag="024">
  1. <subfield code="a">0025-3227</subfield>
  </datafield>
16. <datafield ind1="8" ind2=" " tag="024">
  1. <subfield code="a">10.1016/j.margeo.2020.106337</subfield>
  </datafield>
17. <datafield ind1="8" ind2=" " tag="024">
  1. <subfield code="a">https://doi.org/10.1016/j.margeo.2020.106337</subfield>
  </datafield>
18. <datafield ind1="8" ind2=" " tag="024">
  1. <subfield code="a">https://hdl.handle.net/10953/1346</subfield>
  </datafield>
19. <datafield ind1=" " ind2=" " tag="653">
  1. <subfield code="a">Zanclean flood</subfield>
  </datafield>
20. <datafield ind1=" " ind2=" " tag="653">
  1. <subfield code="a">Megaflood</subfield>
  </datafield>
21. <datafield ind1=" " ind2=" " tag="653">
  1. <subfield code="a">Geophysics</subfield>
  </datafield>
22. <datafield ind1=" " ind2=" " tag="653">
  1. <subfield code="a">Numerical modelling</subfield>
  </datafield>
23. <datafield ind1=" " ind2=" " tag="653">
  1. <subfield code="a">Messinian salinity crisis</subfield>
  </datafield>
24. <datafield ind1=" " ind2=" " tag="653">
  1. <subfield code="a">Mediterranean Sea</subfield>
  </datafield>
25. <datafield ind1="0" ind2="0" tag="245">
  1. <subfield code="a">A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin</subfield>
  </datafield>
</record>

mets

Descarregar XML

<?xml version="1.0" encoding="UTF-8" ?>

<mets ID=" DSpace_ITEM_10953-1346" OBJID=" hdl:10953/1346" PROFILE="DSpace METS SIP Profile 1.0" TYPE="DSpace ITEM" schemaLocation="http://www.loc.gov/METS/ http://www.loc.gov/standards/mets/mets.xsd">
1. <metsHdr CREATEDATE="2024-09-19T00:34:47Z">
  1. <agent ROLE="CUSTODIAN" TYPE="ORGANIZATION">
    1. <name>Repositorio Institucional de Produccion Cientifica de la Universidad de Jaen</name>
    </agent>
  </metsHdr>
2. <dmdSec ID="DMD_10953_1346">
  1. <mdWrap MDTYPE="MODS">
    1. <xmlData schemaLocation="http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-1.xsd">
      1. <mods:mods schemaLocation="http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-1.xsd">
        <mods:name>
        <mods:role>
        <mods:roleTerm type="text">author</mods:roleTerm>
        </mods:role>
        <mods:namePart>Spatola, Daniele</mods:namePart>
        </mods:name>
        <mods:name>
        <mods:role>
        <mods:roleTerm type="text">author</mods:roleTerm>
        </mods:role>
        <mods:namePart>del Moral-Erencia, José D.</mods:namePart>
        </mods:name>
        <mods:name>
        <mods:role>
        <mods:roleTerm type="text">author</mods:roleTerm>
        </mods:role>
        <mods:namePart>Micallef, Aaron</mods:namePart>
        </mods:name>
        <mods:name>
        <mods:role>
        <mods:roleTerm type="text">author</mods:roleTerm>
        </mods:role>
        <mods:namePart>Camerlenghi, Angelo</mods:namePart>
        </mods:name>
        <mods:name>
        <mods:role>
        <mods:roleTerm type="text">author</mods:roleTerm>
        </mods:role>
        <mods:namePart>García-Castellanos, Daniel</mods:namePart>
        </mods:name>
        <mods:name>
        <mods:role>
        <mods:roleTerm type="text">author</mods:roleTerm>
        </mods:role>
        <mods:namePart>Gupta, Sanjeev</mods:namePart>
        </mods:name>
        <mods:name>
        <mods:role>
        <mods:roleTerm type="text">author</mods:roleTerm>
        </mods:role>
        <mods:namePart>Bohórquez, Patricio</mods:namePart>
        </mods:name>
        <mods:name>
        <mods:role>
        <mods:roleTerm type="text">author</mods:roleTerm>
        </mods:role>
        <mods:namePart>Gutscher, Marc-André</mods:namePart>
        </mods:name>
        <mods:name>
        <mods:role>
        <mods:roleTerm type="text">author</mods:roleTerm>
        </mods:role>
        <mods:namePart>Bertoni, Claudia</mods:namePart>
        </mods:name>
        <mods:extension>
        <mods:dateAccessioned encoding="iso8601">2023-11-29T07:36:38Z</mods:dateAccessioned>
        </mods:extension>
        <mods:extension>
        <mods:dateAvailable encoding="iso8601">2023-11-29T07:36:38Z</mods:dateAvailable>
        </mods:extension>
        <mods:originInfo>
        <mods:dateIssued encoding="iso8601">2020-09-10</mods:dateIssued>
        </mods:originInfo>
        <mods:identifier type="citation">Spatola D., del Moral-Erencia J.D., Micallef A., Camerlenghi A., Garcia-Castellanos D., Gupta S., Bohorquez P., Gutscher M.-A., Bertoni C. A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin. Marine Geology, 430: 10633, 2020. https://doi.org/10.1016/j.margeo.2020.106337</mods:identifier>
        <mods:identifier type="issn">0025-3227</mods:identifier>
        <mods:identifier type="other">10.1016/j.margeo.2020.106337</mods:identifier>
        <mods:identifier type="uri">https://doi.org/10.1016/j.margeo.2020.106337</mods:identifier>
        <mods:abstract>The Messinian salinity crisis was an extraordinary event that resulted in the deposition of kilometre-thick evaporite sequences in the Mediterranean Sea after the latter became disconnected from the world's oceans. The return to fully and stable marine conditions at the end of the crisis is still subject to debate. Three main hypotheses, based on geophysical and borehole data, onshore outcrops and climate simulations, have been put forward. These include a single-stage catastrophic flood, a two-step reflooding scenario, and an overspill of Paratethyan water followed by Atlantic inflow. In this study, two research questions are addressed: (i) Which event marked the termination of the Messinian salinity crisis? (ii) What was the sea level in the eastern Mediterranean Sea during this event? Geophysical data from the western Ionian Basin are integrated with numerical simulations to infer that the termination of the crisis consisted of a single-stage megaflood following a sea level drawdown of 1900 m. This megaflood deposited an extensive sedimentary body with a chaotic to transparent seismic signature at the base of the Malta Escarpment. Fine, well-sorted sediments are predicted to have been deposited within the thicker sections of the flood deposit, whereas a more variable distribution of coarser sediments is expected elsewhere. The north-western Ionian Basin hosts evidence of episodic post-Messinian salinity crisis slope instability events in the last ~1.8 Ma. The largest of these emplaced a >200 km3 deposit and is associated with failure of the head of Noto Canyon (offshore SE Sicily). Apart from unravelling the final phase of the Messinian salinity crisis and the ensuing stratigraphic evolution of the western Ionian Basin, our results are also relevant to better understand megafloods, which are some of the most catastrophic geological processes on Earth and Mars.</mods:abstract>
        <mods:language>
        <mods:languageTerm authority="rfc3066">eng</mods:languageTerm>
        </mods:language>
        <mods:accessCondition type="useAndReproduction">Atribución-NoComercial-SinDerivadas 3.0 España</mods:accessCondition>
        <mods:subject>
        <mods:topic>Zanclean flood</mods:topic>
        </mods:subject>
        <mods:subject>
        <mods:topic>Megaflood</mods:topic>
        </mods:subject>
        <mods:subject>
        <mods:topic>Geophysics</mods:topic>
        </mods:subject>
        <mods:subject>
        <mods:topic>Numerical modelling</mods:topic>
        </mods:subject>
        <mods:subject>
        <mods:topic>Messinian salinity crisis</mods:topic>
        </mods:subject>
        <mods:subject>
        <mods:topic>Mediterranean Sea</mods:topic>
        </mods:subject>
        <mods:titleInfo>
        <mods:title>A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin</mods:title>
        </mods:titleInfo>
        <mods:genre>info:eu-repo/semantics/article</mods:genre>
        </mods:mods>
      </xmlData>
    </mdWrap>
  </dmdSec>
3. <amdSec ID="TMD_10953_1346">
  1. <rightsMD ID="RIG_10953_1346">
    1. <mdWrap MDTYPE="OTHER" MIMETYPE="text/plain" OTHERMDTYPE="DSpaceDepositLicense">
      1. <binData>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</binData>
      </mdWrap>
    </rightsMD>
  </amdSec>
4. <amdSec ID="FO_10953_1346_1">
  1. <techMD ID="TECH_O_10953_1346_1">
    1. <mdWrap MDTYPE="PREMIS">
      1. <xmlData schemaLocation="http://www.loc.gov/standards/premis http://www.loc.gov/standards/premis/PREMIS-v1-0.xsd">
        <premis:premis>
        <premis:object>
        <premis:objectIdentifier>
        <premis:objectIdentifierType>URL</premis:objectIdentifierType>
        <premis:objectIdentifierValue>http://ruja.ujaen.es/jspui/bitstream/10953/1346/1/MG2020.pdf</premis:objectIdentifierValue>
        </premis:objectIdentifier>
        <premis:objectCategory>File</premis:objectCategory>
        <premis:objectCharacteristics>
        <premis:fixity>
        <premis:messageDigestAlgorithm>MD5</premis:messageDigestAlgorithm>
        <premis:messageDigest>f7d3f4219af1c56134ac4432d0bcded8</premis:messageDigest>
        </premis:fixity>
        <premis:size>10488433</premis:size>
        <premis:format>
        <premis:formatDesignation>
        <premis:formatName>application/pdf</premis:formatName>
        </premis:formatDesignation>
        </premis:format>
        </premis:objectCharacteristics>
        <premis:originalName>MG2020.pdf</premis:originalName>
        </premis:object>
        </premis:premis>
        </xmlData>
      </mdWrap>
    </techMD>
  </amdSec>
5. <fileSec>
  1. <fileGrp USE="ORIGINAL">
    1. <file ADMID="FO_10953_1346_1" CHECKSUM="f7d3f4219af1c56134ac4432d0bcded8" CHECKSUMTYPE="MD5" GROUPID="GROUP_BITSTREAM_10953_1346_1" ID="BITSTREAM_ORIGINAL_10953_1346_1" MIMETYPE="application/pdf" SEQ="1" SIZE="10488433">
      1. <FLocat LOCTYPE="URL" href="http://ruja.ujaen.es/jspui/bitstream/10953/1346/1/MG2020.pdf" type="simple" />
      </file>
    </fileGrp>
  </fileSec>
6. <structMap LABEL="DSpace Object" TYPE="LOGICAL">
  1. <div ADMID="DMD_10953_1346" TYPE="DSpace Object Contents">
    1. <div TYPE="DSpace BITSTREAM">
      1. <fptr FILEID="BITSTREAM_ORIGINAL_10953_1346_1" />
      </div>
    </div>
  </structMap>
</mets>

mods

Descarregar XML

<?xml version="1.0" encoding="UTF-8" ?>

<mods:mods schemaLocation="http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-1.xsd">
1. <mods:name>
  1. <mods:namePart>Spatola, Daniele</mods:namePart>
  </mods:name>
2. <mods:name>
  1. <mods:namePart>del Moral-Erencia, José D.</mods:namePart>
  </mods:name>
3. <mods:name>
  1. <mods:namePart>Micallef, Aaron</mods:namePart>
  </mods:name>
4. <mods:name>
  1. <mods:namePart>Camerlenghi, Angelo</mods:namePart>
  </mods:name>
5. <mods:name>
  1. <mods:namePart>García-Castellanos, Daniel</mods:namePart>
  </mods:name>
6. <mods:name>
  1. <mods:namePart>Gupta, Sanjeev</mods:namePart>
  </mods:name>
7. <mods:name>
  1. <mods:namePart>Bohórquez, Patricio</mods:namePart>
  </mods:name>
8. <mods:name>
  1. <mods:namePart>Gutscher, Marc-André</mods:namePart>
  </mods:name>
9. <mods:name>
  1. <mods:namePart>Bertoni, Claudia</mods:namePart>
  </mods:name>
10. <mods:extension>
  1. <mods:dateAvailable encoding="iso8601">2023-11-29T07:36:38Z</mods:dateAvailable>
  </mods:extension>
11. <mods:extension>
  1. <mods:dateAccessioned encoding="iso8601">2023-11-29T07:36:38Z</mods:dateAccessioned>
  </mods:extension>
12. <mods:originInfo>
  1. <mods:dateIssued encoding="iso8601">2020-09-10</mods:dateIssued>
  </mods:originInfo>
13. <mods:identifier type="citation">Spatola D., del Moral-Erencia J.D., Micallef A., Camerlenghi A., Garcia-Castellanos D., Gupta S., Bohorquez P., Gutscher M.-A., Bertoni C. A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin. Marine Geology, 430: 10633, 2020. https://doi.org/10.1016/j.margeo.2020.106337</mods:identifier>
14. <mods:identifier type="issn">0025-3227</mods:identifier>
15. <mods:identifier type="other">10.1016/j.margeo.2020.106337</mods:identifier>
16. <mods:identifier type="uri">https://doi.org/10.1016/j.margeo.2020.106337</mods:identifier>
17. <mods:identifier type="uri">https://hdl.handle.net/10953/1346</mods:identifier>
18. <mods:abstract>The Messinian salinity crisis was an extraordinary event that resulted in the deposition of kilometre-thick evaporite sequences in the Mediterranean Sea after the latter became disconnected from the world's oceans. The return to fully and stable marine conditions at the end of the crisis is still subject to debate. Three main hypotheses, based on geophysical and borehole data, onshore outcrops and climate simulations, have been put forward. These include a single-stage catastrophic flood, a two-step reflooding scenario, and an overspill of Paratethyan water followed by Atlantic inflow. In this study, two research questions are addressed: (i) Which event marked the termination of the Messinian salinity crisis? (ii) What was the sea level in the eastern Mediterranean Sea during this event? Geophysical data from the western Ionian Basin are integrated with numerical simulations to infer that the termination of the crisis consisted of a single-stage megaflood following a sea level drawdown of 1900 m. This megaflood deposited an extensive sedimentary body with a chaotic to transparent seismic signature at the base of the Malta Escarpment. Fine, well-sorted sediments are predicted to have been deposited within the thicker sections of the flood deposit, whereas a more variable distribution of coarser sediments is expected elsewhere. The north-western Ionian Basin hosts evidence of episodic post-Messinian salinity crisis slope instability events in the last ~1.8 Ma. The largest of these emplaced a >200 km3 deposit and is associated with failure of the head of Noto Canyon (offshore SE Sicily). Apart from unravelling the final phase of the Messinian salinity crisis and the ensuing stratigraphic evolution of the western Ionian Basin, our results are also relevant to better understand megafloods, which are some of the most catastrophic geological processes on Earth and Mars.</mods:abstract>
19. <mods:language>
  1. <mods:languageTerm>eng</mods:languageTerm>
  </mods:language>
20. <mods:accessCondition type="useAndReproduction">http://creativecommons.org/licenses/by-nc-nd/3.0/es/</mods:accessCondition>
21. <mods:accessCondition type="useAndReproduction">info:eu-repo/semantics/openAccess</mods:accessCondition>
22. <mods:accessCondition type="useAndReproduction">Atribución-NoComercial-SinDerivadas 3.0 España</mods:accessCondition>
23. <mods:subject>
  1. <mods:topic>Zanclean flood</mods:topic>
  </mods:subject>
24. <mods:subject>
  1. <mods:topic>Megaflood</mods:topic>
  </mods:subject>
25. <mods:subject>
  1. <mods:topic>Geophysics</mods:topic>
  </mods:subject>
26. <mods:subject>
  1. <mods:topic>Numerical modelling</mods:topic>
  </mods:subject>
27. <mods:subject>
  1. <mods:topic>Messinian salinity crisis</mods:topic>
  </mods:subject>
28. <mods:subject>
  1. <mods:topic>Mediterranean Sea</mods:topic>
  </mods:subject>
29. <mods:titleInfo>
  1. <mods:title>A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin</mods:title>
  </mods:titleInfo>
30. <mods:genre>info:eu-repo/semantics/article</mods:genre>
</mods:mods>

ore

Descarregar XML

<?xml version="1.0" encoding="UTF-8" ?>

<atom:entry schemaLocation="http://www.w3.org/2005/Atom http://www.kbcafe.com/rss/atom.xsd.xml">
1. <atom:id>https://doi.org/10.1016/j.margeo.2020.106337/ore.xml</atom:id>
2. <atom:link href="https://doi.org/10.1016/j.margeo.2020.106337" rel="alternate" />
3. <atom:link href="https://doi.org/10.1016/j.margeo.2020.106337/ore.xml" rel="http://www.openarchives.org/ore/terms/describes" />
4. <atom:link href="https://doi.org/10.1016/j.margeo.2020.106337/ore.xml#atom" rel="self" type="application/atom+xml" />
5. <atom:published>2023-11-29T07:36:38Z</atom:published>
6. <atom:updated>2023-11-29T07:36:38Z</atom:updated>
7. <atom:source>
  1. <atom:generator>Repositorio Institucional de Produccion Cientifica de la Universidad de Jaen</atom:generator>
  </atom:source>
8. <atom:title>A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin</atom:title>
9. <atom:author>
  1. <atom:name>Spatola, Daniele</atom:name>
  </atom:author>
10. <atom:author>
  1. <atom:name>del Moral-Erencia, José D.</atom:name>
  </atom:author>
11. <atom:author>
  1. <atom:name>Micallef, Aaron</atom:name>
  </atom:author>
12. <atom:author>
  1. <atom:name>Camerlenghi, Angelo</atom:name>
  </atom:author>
13. <atom:author>
  1. <atom:name>García-Castellanos, Daniel</atom:name>
  </atom:author>
14. <atom:author>
  1. <atom:name>Gupta, Sanjeev</atom:name>
  </atom:author>
15. <atom:author>
  1. <atom:name>Bohórquez, Patricio</atom:name>
  </atom:author>
16. <atom:author>
  1. <atom:name>Gutscher, Marc-André</atom:name>
  </atom:author>
17. <atom:author>
  1. <atom:name>Bertoni, Claudia</atom:name>
  </atom:author>
18. <atom:category label="Aggregation" scheme="http://www.openarchives.org/ore/terms/" term="http://www.openarchives.org/ore/terms/Aggregation" />
19. <atom:category scheme="http://www.openarchives.org/ore/atom/modified" term="2023-11-29T07:36:38Z" />
20. <atom:category label="DSpace Item" scheme="http://www.dspace.org/objectModel/" term="DSpaceItem" />
21. <atom:link href="http://ruja.ujaen.es/jspui/bitstream/10953/1346/1/MG2020.pdf" length="10488433" rel="http://www.openarchives.org/ore/terms/aggregates" title="MG2020.pdf" type="application/pdf" />
22. <oreatom:triples>
  1. <rdf:Description about="https://doi.org/10.1016/j.margeo.2020.106337/ore.xml#atom">
    1. <rdf:type resource="http://www.dspace.org/objectModel/DSpaceItem" />
    2. <dcterms:modified>2023-11-29T07:36:38Z</dcterms:modified>
    </rdf:Description>
  2. <rdf:Description about="http://ruja.ujaen.es/jspui/bitstream/10953/1346/1/MG2020.pdf">
    1. <rdf:type resource="http://www.dspace.org/objectModel/DSpaceBitstream" />
    2. <dcterms:description>ORIGINAL</dcterms:description>
    </rdf:Description>
  3. <rdf:Description about="http://ruja.ujaen.es/jspui/bitstream/10953/1346/2/license_rdf">
    1. <rdf:type resource="http://www.dspace.org/objectModel/DSpaceBitstream" />
    2. <dcterms:description>CC-LICENSE</dcterms:description>
    </rdf:Description>
  4. <rdf:Description about="http://ruja.ujaen.es/jspui/bitstream/10953/1346/3/license.txt">
    1. <rdf:type resource="http://www.dspace.org/objectModel/DSpaceBitstream" />
    2. <dcterms:description>LICENSE</dcterms:description>
    </rdf:Description>
  </oreatom:triples>
</atom:entry>

qdc

Descarregar XML

<?xml version="1.0" encoding="UTF-8" ?>

<qdc:qualifieddc schemaLocation="http://purl.org/dc/elements/1.1/ http://dublincore.org/schemas/xmls/qdc/2006/01/06/dc.xsd http://purl.org/dc/terms/ http://dublincore.org/schemas/xmls/qdc/2006/01/06/dcterms.xsd http://dspace.org/qualifieddc/ http://www.ukoln.ac.uk/metadata/dcmi/xmlschema/qualifieddc.xsd">
1. <dc:title>A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin</dc:title>
2. <dc:creator>Spatola, Daniele</dc:creator>
3. <dc:creator>del Moral-Erencia, José D.</dc:creator>
4. <dc:creator>Micallef, Aaron</dc:creator>
5. <dc:creator>Camerlenghi, Angelo</dc:creator>
6. <dc:creator>García-Castellanos, Daniel</dc:creator>
7. <dc:creator>Gupta, Sanjeev</dc:creator>
8. <dc:creator>Bohórquez, Patricio</dc:creator>
9. <dc:creator>Gutscher, Marc-André</dc:creator>
10. <dc:creator>Bertoni, Claudia</dc:creator>
11. <dc:subject>Zanclean flood</dc:subject>
12. <dc:subject>Megaflood</dc:subject>
13. <dc:subject>Geophysics</dc:subject>
14. <dc:subject>Numerical modelling</dc:subject>
15. <dc:subject>Messinian salinity crisis</dc:subject>
16. <dc:subject>Mediterranean Sea</dc:subject>
17. <dcterms:abstract>The Messinian salinity crisis was an extraordinary event that resulted in the deposition of kilometre-thick evaporite sequences in the Mediterranean Sea after the latter became disconnected from the world's oceans. The return to fully and stable marine conditions at the end of the crisis is still subject to debate. Three main hypotheses, based on geophysical and borehole data, onshore outcrops and climate simulations, have been put forward. These include a single-stage catastrophic flood, a two-step reflooding scenario, and an overspill of Paratethyan water followed by Atlantic inflow. In this study, two research questions are addressed: (i) Which event marked the termination of the Messinian salinity crisis? (ii) What was the sea level in the eastern Mediterranean Sea during this event? Geophysical data from the western Ionian Basin are integrated with numerical simulations to infer that the termination of the crisis consisted of a single-stage megaflood following a sea level drawdown of 1900 m. This megaflood deposited an extensive sedimentary body with a chaotic to transparent seismic signature at the base of the Malta Escarpment. Fine, well-sorted sediments are predicted to have been deposited within the thicker sections of the flood deposit, whereas a more variable distribution of coarser sediments is expected elsewhere. The north-western Ionian Basin hosts evidence of episodic post-Messinian salinity crisis slope instability events in the last ~1.8 Ma. The largest of these emplaced a >200 km3 deposit and is associated with failure of the head of Noto Canyon (offshore SE Sicily). Apart from unravelling the final phase of the Messinian salinity crisis and the ensuing stratigraphic evolution of the western Ionian Basin, our results are also relevant to better understand megafloods, which are some of the most catastrophic geological processes on Earth and Mars.</dcterms:abstract>
18. <dcterms:dateAccepted>2023-11-29T07:36:38Z</dcterms:dateAccepted>
19. <dcterms:available>2023-11-29T07:36:38Z</dcterms:available>
20. <dcterms:created>2023-11-29T07:36:38Z</dcterms:created>
21. <dcterms:issued>2020-09-10</dcterms:issued>
22. <dc:type>info:eu-repo/semantics/article</dc:type>
23. <dc:identifier>Spatola D., del Moral-Erencia J.D., Micallef A., Camerlenghi A., Garcia-Castellanos D., Gupta S., Bohorquez P., Gutscher M.-A., Bertoni C. A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin. Marine Geology, 430: 10633, 2020. https://doi.org/10.1016/j.margeo.2020.106337</dc:identifier>
24. <dc:identifier>0025-3227</dc:identifier>
25. <dc:identifier>10.1016/j.margeo.2020.106337</dc:identifier>
26. <dc:identifier>https://doi.org/10.1016/j.margeo.2020.106337</dc:identifier>
27. <dc:identifier>https://hdl.handle.net/10953/1346</dc:identifier>
28. <dc:language>eng</dc:language>
29. <dc:relation>Marine Geology 2020; 430: 10633</dc:relation>
30. <dc:rights>http://creativecommons.org/licenses/by-nc-nd/3.0/es/</dc:rights>
31. <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
32. <dc:rights>Atribución-NoComercial-SinDerivadas 3.0 España</dc:rights>
33. <dc:publisher>Elsevier</dc:publisher>
</qdc:qualifieddc>

rdf

Descarregar XML

<?xml version="1.0" encoding="UTF-8" ?>

<rdf:RDF schemaLocation="http://www.openarchives.org/OAI/2.0/rdf/ http://www.openarchives.org/OAI/2.0/rdf.xsd">
1. <ow:Publication about="oai:ruja.ujaen.es:10953/1346">
  1. <dc:title>A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin</dc:title>
  2. <dc:creator>Spatola, Daniele</dc:creator>
  3. <dc:creator>del Moral-Erencia, José D.</dc:creator>
  4. <dc:creator>Micallef, Aaron</dc:creator>
  5. <dc:creator>Camerlenghi, Angelo</dc:creator>
  6. <dc:creator>García-Castellanos, Daniel</dc:creator>
  7. <dc:creator>Gupta, Sanjeev</dc:creator>
  8. <dc:creator>Bohórquez, Patricio</dc:creator>
  9. <dc:creator>Gutscher, Marc-André</dc:creator>
  10. <dc:creator>Bertoni, Claudia</dc:creator>
  11. <dc:subject>Zanclean flood</dc:subject>
  12. <dc:subject>Megaflood</dc:subject>
  13. <dc:subject>Geophysics</dc:subject>
  14. <dc:subject>Numerical modelling</dc:subject>
  15. <dc:subject>Messinian salinity crisis</dc:subject>
  16. <dc:subject>Mediterranean Sea</dc:subject>
  17. <dc:description>The Messinian salinity crisis was an extraordinary event that resulted in the deposition of kilometre-thick evaporite sequences in the Mediterranean Sea after the latter became disconnected from the world's oceans. The return to fully and stable marine conditions at the end of the crisis is still subject to debate. Three main hypotheses, based on geophysical and borehole data, onshore outcrops and climate simulations, have been put forward. These include a single-stage catastrophic flood, a two-step reflooding scenario, and an overspill of Paratethyan water followed by Atlantic inflow. In this study, two research questions are addressed: (i) Which event marked the termination of the Messinian salinity crisis? (ii) What was the sea level in the eastern Mediterranean Sea during this event? Geophysical data from the western Ionian Basin are integrated with numerical simulations to infer that the termination of the crisis consisted of a single-stage megaflood following a sea level drawdown of 1900 m. This megaflood deposited an extensive sedimentary body with a chaotic to transparent seismic signature at the base of the Malta Escarpment. Fine, well-sorted sediments are predicted to have been deposited within the thicker sections of the flood deposit, whereas a more variable distribution of coarser sediments is expected elsewhere. The north-western Ionian Basin hosts evidence of episodic post-Messinian salinity crisis slope instability events in the last ~1.8 Ma. The largest of these emplaced a >200 km3 deposit and is associated with failure of the head of Noto Canyon (offshore SE Sicily). Apart from unravelling the final phase of the Messinian salinity crisis and the ensuing stratigraphic evolution of the western Ionian Basin, our results are also relevant to better understand megafloods, which are some of the most catastrophic geological processes on Earth and Mars.</dc:description>
  18. <dc:date>2023-11-29T07:36:38Z</dc:date>
  19. <dc:date>2023-11-29T07:36:38Z</dc:date>
  20. <dc:date>2020-09-10</dc:date>
  21. <dc:type>info:eu-repo/semantics/article</dc:type>
  22. <dc:identifier>Spatola D., del Moral-Erencia J.D., Micallef A., Camerlenghi A., Garcia-Castellanos D., Gupta S., Bohorquez P., Gutscher M.-A., Bertoni C. A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin. Marine Geology, 430: 10633, 2020. https://doi.org/10.1016/j.margeo.2020.106337</dc:identifier>
  23. <dc:identifier>0025-3227</dc:identifier>
  24. <dc:identifier>10.1016/j.margeo.2020.106337</dc:identifier>
  25. <dc:identifier>https://doi.org/10.1016/j.margeo.2020.106337</dc:identifier>
  26. <dc:identifier>https://hdl.handle.net/10953/1346</dc:identifier>
  27. <dc:language>eng</dc:language>
  28. <dc:relation>Marine Geology 2020; 430: 10633</dc:relation>
  29. <dc:rights>http://creativecommons.org/licenses/by-nc-nd/3.0/es/</dc:rights>
  30. <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  31. <dc:rights>Atribución-NoComercial-SinDerivadas 3.0 España</dc:rights>
  32. <dc:publisher>Elsevier</dc:publisher>
  </ow:Publication>
</rdf:RDF>

xoai

Descarregar XML

<?xml version="1.0" encoding="UTF-8" ?>

<metadata schemaLocation="http://www.lyncode.com/xoai http://www.lyncode.com/xsd/xoai.xsd">
1. <element name="dc">
  1. <element name="contributor">
    1. <element name="author">
      1. <element name="none">
        <field name="value">Spatola, Daniele</field>
        <field name="value">del Moral-Erencia, José D.</field>
        <field name="value">Micallef, Aaron</field>
        <field name="value">Camerlenghi, Angelo</field>
        <field name="value">García-Castellanos, Daniel</field>
        <field name="value">Gupta, Sanjeev</field>
        <field name="value">Bohórquez, Patricio</field>
        <field name="value">Gutscher, Marc-André</field>
        <field name="value">Bertoni, Claudia</field>
        </element>
      </element>
    </element>
  2. <element name="date">
    1. <element name="accessioned">
      1. <element name="none">
        <field name="value">2023-11-29T07:36:38Z</field>
        </element>
      </element>
    2. <element name="available">
      1. <element name="none">
        <field name="value">2023-11-29T07:36:38Z</field>
        </element>
      </element>
    3. <element name="issued">
      1. <element name="none">
        <field name="value">2020-09-10</field>
        </element>
      </element>
    </element>
  3. <element name="identifier">
    1. <element name="citation">
      1. <element name="es_ES">
        <field name="value">Spatola D., del Moral-Erencia J.D., Micallef A., Camerlenghi A., Garcia-Castellanos D., Gupta S., Bohorquez P., Gutscher M.-A., Bertoni C. A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin. Marine Geology, 430: 10633, 2020. https://doi.org/10.1016/j.margeo.2020.106337</field>
        </element>
      </element>
    2. <element name="issn">
      1. <element name="es_ES">
        <field name="value">0025-3227</field>
        </element>
      </element>
    3. <element name="other">
      1. <element name="es_ES">
        <field name="value">10.1016/j.margeo.2020.106337</field>
        </element>
      </element>
    4. <element name="uri">
      1. <element name="es_ES">
        <field name="value">https://doi.org/10.1016/j.margeo.2020.106337</field>
        </element>
      2. <element name="none">
        <field name="value">https://hdl.handle.net/10953/1346</field>
        </element>
      </element>
    </element>
  4. <element name="description">
    1. <element name="abstract">
      1. <element name="es_ES">
        <field name="value">The Messinian salinity crisis was an extraordinary event that resulted in the deposition of kilometre-thick evaporite sequences in the Mediterranean Sea after the latter became disconnected from the world's oceans. The return to fully and stable marine conditions at the end of the crisis is still subject to debate. Three main hypotheses, based on geophysical and borehole data, onshore outcrops and climate simulations, have been put forward. These include a single-stage catastrophic flood, a two-step reflooding scenario, and an overspill of Paratethyan water followed by Atlantic inflow. In this study, two research questions are addressed: (i) Which event marked the termination of the Messinian salinity crisis? (ii) What was the sea level in the eastern Mediterranean Sea during this event? Geophysical data from the western Ionian Basin are integrated with numerical simulations to infer that the termination of the crisis consisted of a single-stage megaflood following a sea level drawdown of 1900 m. This megaflood deposited an extensive sedimentary body with a chaotic to transparent seismic signature at the base of the Malta Escarpment. Fine, well-sorted sediments are predicted to have been deposited within the thicker sections of the flood deposit, whereas a more variable distribution of coarser sediments is expected elsewhere. The north-western Ionian Basin hosts evidence of episodic post-Messinian salinity crisis slope instability events in the last ~1.8 Ma. The largest of these emplaced a >200 km3 deposit and is associated with failure of the head of Noto Canyon (offshore SE Sicily). Apart from unravelling the final phase of the Messinian salinity crisis and the ensuing stratigraphic evolution of the western Ionian Basin, our results are also relevant to better understand megafloods, which are some of the most catastrophic geological processes on Earth and Mars.</field>
        </element>
      </element>
    2. <element name="sponsorship">
      1. <element name="es_ES">
        <field name="value">The article is based upon work from COST Action CA15103 “Uncovering the Mediterranean salt giant” (MEDSALT) supported by (COST European Cooperation in Science and Technology). We are indebted to the CUMECS-2, CUMECS-3 and CIRCEE-HR shipboard parties, captains, crew and technicians for their assistance during data collection. The oceanographic surveys were possible following permits issued by the Italian and Maltese authorities. SPECTRUM (now TGS) are kindly acknowledged for providing access to their seismic reflection data. The use of CROP seismic profiles has been licensed to OGS by CNR, Banca Dati CROP (www.crop.cnr.it). The authors would also like to thank Emerson Paradigm for the use of the OGS academic licenses of the ECHOS and Geodepth processing software, and IHS Markit for the OGS license of the Kingdom software. DS is funded by EMODnet Bathymetry, which is financed by the European Union under Regulation 508/2014 of the European Parliament and of the Council of 15 May 2014 on the European Maritime and Fisheries Fund. This work was also supported by the Spanish Ministry of Science, Innovation and Universities (MICINN/FEDER, EU) under Grant SEDRETO CGL2015–70736-R. J.D.d.M.E. was supported by the PhD scholarship BES-2016-079117 (MINECO/FSE, EU) from the Spanish National Programme for the Promotion of Talent and its Employability (call 2016). This project has received funding from the European Union's Horizon 2020 research and innovation programme under the Marie Skłodowska-Curie grant agreement No. 765256 (SaltGiant ITN).</field>
        </element>
      </element>
    </element>
  5. <element name="language">
    1. <element name="iso">
      1. <element name="es_ES">
        <field name="value">eng</field>
        </element>
      </element>
    </element>
  6. <element name="publisher">
    1. <element name="es_ES">
      1. <field name="value">Elsevier</field>
      </element>
    </element>
  7. <element name="relation">
    1. <element name="ispartof">
      1. <element name="es_ES">
        <field name="value">Marine Geology 2020; 430: 10633</field>
        </element>
      </element>
    </element>
  8. <element name="rights">
    1. <element name="*">
      1. <field name="value">Atribución-NoComercial-SinDerivadas 3.0 España</field>
      </element>
    2. <element name="uri">
      1. <element name="*">
        <field name="value">http://creativecommons.org/licenses/by-nc-nd/3.0/es/</field>
        </element>
      </element>
    3. <element name="accessRights">
      1. <element name="es_ES">
        <field name="value">info:eu-repo/semantics/openAccess</field>
        </element>
      </element>
    </element>
  9. <element name="subject">
    1. <element name="es_ES">
      1. <field name="value">Zanclean flood</field>
      2. <field name="value">Megaflood</field>
      3. <field name="value">Geophysics</field>
      4. <field name="value">Numerical modelling</field>
      5. <field name="value">Messinian salinity crisis</field>
      6. <field name="value">Mediterranean Sea</field>
      </element>
    </element>
  10. <element name="title">
    1. <element name="es_ES">
      1. <field name="value">A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin</field>
      </element>
    </element>
  11. <element name="type">
    1. <element name="es_ES">
      1. <field name="value">info:eu-repo/semantics/article</field>
      </element>
    2. <element name="version">
      1. <element name="es_ES">
        <field name="value">info:eu-repo/semantics/acceptedVersion</field>
        </element>
      </element>
    </element>
  </element>
2. <element name="bundles">
  1. <element name="bundle">
    1. <field name="name">ORIGINAL</field>
    2. <element name="bitstreams">
      1. <element name="bitstream">
        <field name="name">MG2020.pdf</field>
        <field name="originalName">MG2020.pdf</field>
        <field name="description">Spatola D., del Moral-Erencia J.D., Micallef A., Camerlenghi A., Garcia-Castellanos D., Gupta S., Bohorquez P., Gutscher M.-A., Bertoni C. A single-stage megaflood at the termination of the Messinian Salinity Crisis: Geophysical and modelling evidence from the eastern Mediterranean Basin. Marine Geology, 430: 10633, 2020. https://doi.org/10.1016/j.margeo.2020.106337</field>
        <field name="format">application/pdf</field>
        <field name="size">10488433</field>
        <field name="url">http://ruja.ujaen.es/jspui/bitstream/10953/1346/1/MG2020.pdf</field>
        <field name="checksum">f7d3f4219af1c56134ac4432d0bcded8</field>
        <field name="checksumAlgorithm">MD5</field>
        <field name="sid">1</field>
        </element>
      </element>
    </element>
  2. <element name="bundle">
    1. <field name="name">CC-LICENSE</field>
    2. <element name="bitstreams">
      1. <element name="bitstream">
        <field name="name">license_rdf</field>
        <field name="originalName">license_rdf</field>
        <field name="format">application/rdf+xml; charset=utf-8</field>
        <field name="size">811</field>
        <field name="url">http://ruja.ujaen.es/jspui/bitstream/10953/1346/2/license_rdf</field>
        <field name="checksum">4d01a8abc68801ab758ec8c2c04918c3</field>
        <field name="checksumAlgorithm">MD5</field>
        <field name="sid">2</field>
        </element>
      </element>
    </element>
  3. <element name="bundle">
    1. <field name="name">LICENSE</field>
    2. <element name="bitstreams">
      1. <element name="bitstream">
        <field name="name">license.txt</field>
        <field name="originalName">license.txt</field>
        <field name="format">text/plain; charset=utf-8</field>
        <field name="size">2026</field>
        <field name="url">http://ruja.ujaen.es/jspui/bitstream/10953/1346/3/license.txt</field>
        <field name="checksum">58a3afe832e73c48f36f43ccc991428d</field>
        <field name="checksumAlgorithm">MD5</field>
        <field name="sid">3</field>
        </element>
      </element>
    </element>
  </element>
3. <element name="others">
  1. <field name="handle">10953/1346</field>
  2. <field name="identifier">oai:ruja.ujaen.es:10953/1346</field>
  3. <field name="lastModifyDate">2023-11-29 08:36:38.857</field>
  </element>
4. <element name="repository">
  1. <field name="name">Repositorio Institucional de Produccion Cientifica de la Universidad de Jaen</field>
  2. <field name="mail">webmaster@ujaen.es</field>
  </element>
5. <element name="license">
  1. <field name="bin">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</field>
  </element>
</metadata>