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New constraints on the Middle-Late Pleistocene Campi Flegrei explosive activity and Mediterranean tephrostratigraphy (∼160 ka and 110–90 ka)

Giada Fernandez Orcid Logo, Biagio Giaccio Orcid Logo, Antonio Costa Orcid Logo, Lorenzo Monaco Orcid Logo, Sébastien Nomade, Paul Albert Orcid Logo, Alison Pereira, Molly Flynn, Niklas Leicher Orcid Logo, Federico Lucchi Orcid Logo, Paola Petrosino Orcid Logo, Danilo M. Palladino, Alfonsa Milia, Donatella Domenica Insinga Orcid Logo, Sabine Wulf Orcid Logo, Rebecca Kearney, Daniel Veres, Diana Jordanova Orcid Logo, Maria Luisa Putignano, Roberto Isaia, Gianluca Sottili

Quaternary Science Reviews, Volume: 331, Start page: 108623

Swansea University Authors: Paul Albert Orcid Logo, Molly Flynn

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DOI (Published version): 10.1016/j.quascirev.2024.108623

Abstract

The Campi Flegrei (CF) caldera, in southern Italy, is the source of some the most powerful Late Pleistocene eruptions of the European sub-continent (e.g., Campanian Ignimbrite, Neapolitan Yellow Tuff eruptions). Although the CF caldera has been continuously and intensively investigated for decades,...

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Published in: Quaternary Science Reviews
ISSN: 0277-3791
Published: Elsevier BV 2024
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URI: https://cronfa.swan.ac.uk/Record/cronfa65879
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Although the CF caldera has been continuously and intensively investigated for decades, relatively little is known regarding its earliest volcanic activity. Here integrating existing and new tephrostratigraphic data we provide a comprehensive and updated framework for CF volcanic activity which has occurred at ~160 ka and between ~110 ka and ~90 ka. The new tephrostratigraphic, geochemical (EMPA + LA-ICP-MS), chronological (40Ar/39Ar dating) and grain-size distribution data relate to CF tephra deposits preserved in 41 mid-proximal (Campanian Plain), distal (Tyrrhenian Sea) and ultra-distal (Lower Danube area) sedimentary archives. Our results allow us to recognize the presence of at least 13 CF eruptions covering the investigated time frame, with 12 eruptions occurring between 110 and 90 ka. Our high-resolution stratigraphic and chronological investigation also allowed us to recognise that the Triflisco/C-22 tephra, previously considered as a single marker layer, can be actually separated into three different events, sourced from within the CF area in the short time interval of ~93-90 ka, suggesting a more complex and intense volcanic history than previously thought. Moreover, a Bayesian age-depth model, constrained by previous and new high precision 40Ar/39Ar ages, has led to a reliable estimate of the ages of those undated CF eruptions. Overall, the updated framework on the stratigraphy, chronology, dispersion, and geochemistry of the CF tephra of ~160 ka and between 110 ka and 90 ka consolidates the notion that the Middle-Late Pleistocene activity at CF area represents a significant stage of its volcanic evolution, characterised by intense and frequent explosive eruptions.</abstract><type>Journal Article</type><journal>Quaternary Science Reviews</journal><volume>331</volume><journalNumber/><paginationStart>108623</paginationStart><paginationEnd/><publisher>Elsevier BV</publisher><placeOfPublication/><isbnPrint/><isbnElectronic/><issnPrint>0277-3791</issnPrint><issnElectronic/><keywords>Tephrochronology; Campi Flegrei; Middle-Late Pleistocene; EMPA and LA-ICP-MS; 40Ar/39Ar geochronology; Grain-size</keywords><publishedDay>1</publishedDay><publishedMonth>5</publishedMonth><publishedYear>2024</publishedYear><publishedDate>2024-05-01</publishedDate><doi>10.1016/j.quascirev.2024.108623</doi><url/><notes/><college>COLLEGE NANME</college><department>Geography</department><CollegeCode>COLLEGE CODE</CollegeCode><DepartmentCode>SGE</DepartmentCode><institution>Swansea University</institution><apcterm>Another institution paid the OA fee</apcterm><funders>Dr. M. Mannetta is thanked for aiding the sample preparation process for the EMPA analyses. Dr. E. Braschi and A. Orlando are thanked for providing technical assistance during the EMPA analyses at Florence University. Dr. S. Tamburrino is thanked for sampling and providing grain-size data from the KC01B marine core. This research was financially supported by the project “The onset of alkaline-potassium magmatism in central Italy: how, when and why?” (PI: G. S.), funded by "Sapienza" University of Rome (Year 2020; prot. RM120172B9B69EB0). Field activities and grain-size analyses were financially supported by “Sapienza” University of Rome. WDS tephra analysis was supported by the projects FUTURE (MUR, PRIN 2017; grant 20177TKBXZ_003, G. Zanchetta coordinator) and COMET (MUR, PRIN 2022; grant 2022MS9KWR, B. Giaccio coordinator) financed by the Italian Research Ministry. PGA contribution was supported by a UKRI Future Leaders Fellowship (MR/S035478/1).</funders><projectreference>RM120172B9B69EB0 (Sapienza), MUR, PRIN 2017, grant 20177TKBXZ_003, MUR, 1100 PRIN 2022, grant 2022MS9KWR (Italian Research Ministry), MR/S035478/1 (UKRI)</projectreference><lastEdited>2024-04-17T14:52:35.6866289</lastEdited><Created>2024-03-22T09:08:30.5599820</Created><path><level id="1">Faculty of Science and Engineering</level><level id="2">School of Biosciences, Geography and Physics - Geography</level></path><authors><author><firstname>Giada</firstname><surname>Fernandez</surname><orcid>0000-0002-5925-5986</orcid><order>1</order></author><author><firstname>Biagio</firstname><surname>Giaccio</surname><orcid>0000-0002-7007-9127</orcid><order>2</order></author><author><firstname>Antonio</firstname><surname>Costa</surname><orcid>0000-0002-4987-6471</orcid><order>3</order></author><author><firstname>Lorenzo</firstname><surname>Monaco</surname><orcid>0000-0002-6555-0842</orcid><order>4</order></author><author><firstname>Sébastien</firstname><surname>Nomade</surname><order>5</order></author><author><firstname>Paul</firstname><surname>Albert</surname><orcid>0000-0002-6757-1452</orcid><order>6</order></author><author><firstname>Alison</firstname><surname>Pereira</surname><order>7</order></author><author><firstname>Molly</firstname><surname>Flynn</surname><order>8</order></author><author><firstname>Niklas</firstname><surname>Leicher</surname><orcid>0000-0002-3367-5982</orcid><order>9</order></author><author><firstname>Federico</firstname><surname>Lucchi</surname><orcid>0000-0001-5097-2463</orcid><order>10</order></author><author><firstname>Paola</firstname><surname>Petrosino</surname><orcid>0000-0002-5506-8753</orcid><order>11</order></author><author><firstname>Danilo M.</firstname><surname>Palladino</surname><order>12</order></author><author><firstname>Alfonsa</firstname><surname>Milia</surname><order>13</order></author><author><firstname>Donatella Domenica</firstname><surname>Insinga</surname><orcid>0000-0002-2147-0146</orcid><order>14</order></author><author><firstname>Sabine</firstname><surname>Wulf</surname><orcid>0000-0003-0229-7656</orcid><order>15</order></author><author><firstname>Rebecca</firstname><surname>Kearney</surname><order>16</order></author><author><firstname>Daniel</firstname><surname>Veres</surname><order>17</order></author><author><firstname>Diana</firstname><surname>Jordanova</surname><orcid>0000-0003-0595-3153</orcid><order>18</order></author><author><firstname>Maria Luisa</firstname><surname>Putignano</surname><order>19</order></author><author><firstname>Roberto</firstname><surname>Isaia</surname><order>20</order></author><author><firstname>Gianluca</firstname><surname>Sottili</surname><order>21</order></author></authors><documents><document><filename>65879__30050__e79ec662cbd54f4491710a922a84f669.pdf</filename><originalFilename>65879.VoR.pdf</originalFilename><uploaded>2024-04-17T14:51:02.6484228</uploaded><type>Output</type><contentLength>27268241</contentLength><contentType>application/pdf</contentType><version>Version of Record</version><cronfaStatus>true</cronfaStatus><documentNotes>© 2024 The Authors. 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spelling v2 65879 2024-03-22 New constraints on the Middle-Late Pleistocene Campi Flegrei explosive activity and Mediterranean tephrostratigraphy (∼160 ka and 110–90 ka) 7f8db9327402511d4d92849cb79af644 0000-0002-6757-1452 Paul Albert Paul Albert true false 49bb30c2c56d91e7987cc285f20ec657 Molly Flynn Molly Flynn true false 2024-03-22 SGE The Campi Flegrei (CF) caldera, in southern Italy, is the source of some the most powerful Late Pleistocene eruptions of the European sub-continent (e.g., Campanian Ignimbrite, Neapolitan Yellow Tuff eruptions). Although the CF caldera has been continuously and intensively investigated for decades, relatively little is known regarding its earliest volcanic activity. Here integrating existing and new tephrostratigraphic data we provide a comprehensive and updated framework for CF volcanic activity which has occurred at ~160 ka and between ~110 ka and ~90 ka. The new tephrostratigraphic, geochemical (EMPA + LA-ICP-MS), chronological (40Ar/39Ar dating) and grain-size distribution data relate to CF tephra deposits preserved in 41 mid-proximal (Campanian Plain), distal (Tyrrhenian Sea) and ultra-distal (Lower Danube area) sedimentary archives. Our results allow us to recognize the presence of at least 13 CF eruptions covering the investigated time frame, with 12 eruptions occurring between 110 and 90 ka. Our high-resolution stratigraphic and chronological investigation also allowed us to recognise that the Triflisco/C-22 tephra, previously considered as a single marker layer, can be actually separated into three different events, sourced from within the CF area in the short time interval of ~93-90 ka, suggesting a more complex and intense volcanic history than previously thought. Moreover, a Bayesian age-depth model, constrained by previous and new high precision 40Ar/39Ar ages, has led to a reliable estimate of the ages of those undated CF eruptions. Overall, the updated framework on the stratigraphy, chronology, dispersion, and geochemistry of the CF tephra of ~160 ka and between 110 ka and 90 ka consolidates the notion that the Middle-Late Pleistocene activity at CF area represents a significant stage of its volcanic evolution, characterised by intense and frequent explosive eruptions. Journal Article Quaternary Science Reviews 331 108623 Elsevier BV 0277-3791 Tephrochronology; Campi Flegrei; Middle-Late Pleistocene; EMPA and LA-ICP-MS; 40Ar/39Ar geochronology; Grain-size 1 5 2024 2024-05-01 10.1016/j.quascirev.2024.108623 COLLEGE NANME Geography COLLEGE CODE SGE Swansea University Another institution paid the OA fee Dr. M. Mannetta is thanked for aiding the sample preparation process for the EMPA analyses. Dr. E. Braschi and A. Orlando are thanked for providing technical assistance during the EMPA analyses at Florence University. Dr. S. Tamburrino is thanked for sampling and providing grain-size data from the KC01B marine core. This research was financially supported by the project “The onset of alkaline-potassium magmatism in central Italy: how, when and why?” (PI: G. S.), funded by "Sapienza" University of Rome (Year 2020; prot. RM120172B9B69EB0). Field activities and grain-size analyses were financially supported by “Sapienza” University of Rome. WDS tephra analysis was supported by the projects FUTURE (MUR, PRIN 2017; grant 20177TKBXZ_003, G. Zanchetta coordinator) and COMET (MUR, PRIN 2022; grant 2022MS9KWR, B. Giaccio coordinator) financed by the Italian Research Ministry. PGA contribution was supported by a UKRI Future Leaders Fellowship (MR/S035478/1). RM120172B9B69EB0 (Sapienza), MUR, PRIN 2017, grant 20177TKBXZ_003, MUR, 1100 PRIN 2022, grant 2022MS9KWR (Italian Research Ministry), MR/S035478/1 (UKRI) 2024-04-17T14:52:35.6866289 2024-03-22T09:08:30.5599820 Faculty of Science and Engineering School of Biosciences, Geography and Physics - Geography Giada Fernandez 0000-0002-5925-5986 1 Biagio Giaccio 0000-0002-7007-9127 2 Antonio Costa 0000-0002-4987-6471 3 Lorenzo Monaco 0000-0002-6555-0842 4 Sébastien Nomade 5 Paul Albert 0000-0002-6757-1452 6 Alison Pereira 7 Molly Flynn 8 Niklas Leicher 0000-0002-3367-5982 9 Federico Lucchi 0000-0001-5097-2463 10 Paola Petrosino 0000-0002-5506-8753 11 Danilo M. Palladino 12 Alfonsa Milia 13 Donatella Domenica Insinga 0000-0002-2147-0146 14 Sabine Wulf 0000-0003-0229-7656 15 Rebecca Kearney 16 Daniel Veres 17 Diana Jordanova 0000-0003-0595-3153 18 Maria Luisa Putignano 19 Roberto Isaia 20 Gianluca Sottili 21 65879__30050__e79ec662cbd54f4491710a922a84f669.pdf 65879.VoR.pdf 2024-04-17T14:51:02.6484228 Output 27268241 application/pdf Version of Record true © 2024 The Authors. This is an open access article under the CC BY license. true eng http://creativecommons.org/licenses/by/4.0/
title New constraints on the Middle-Late Pleistocene Campi Flegrei explosive activity and Mediterranean tephrostratigraphy (∼160 ka and 110–90 ka)
spellingShingle New constraints on the Middle-Late Pleistocene Campi Flegrei explosive activity and Mediterranean tephrostratigraphy (∼160 ka and 110–90 ka)
Paul Albert
Molly Flynn
title_short New constraints on the Middle-Late Pleistocene Campi Flegrei explosive activity and Mediterranean tephrostratigraphy (∼160 ka and 110–90 ka)
title_full New constraints on the Middle-Late Pleistocene Campi Flegrei explosive activity and Mediterranean tephrostratigraphy (∼160 ka and 110–90 ka)
title_fullStr New constraints on the Middle-Late Pleistocene Campi Flegrei explosive activity and Mediterranean tephrostratigraphy (∼160 ka and 110–90 ka)
title_full_unstemmed New constraints on the Middle-Late Pleistocene Campi Flegrei explosive activity and Mediterranean tephrostratigraphy (∼160 ka and 110–90 ka)
title_sort New constraints on the Middle-Late Pleistocene Campi Flegrei explosive activity and Mediterranean tephrostratigraphy (∼160 ka and 110–90 ka)
author_id_str_mv 7f8db9327402511d4d92849cb79af644
49bb30c2c56d91e7987cc285f20ec657
author_id_fullname_str_mv 7f8db9327402511d4d92849cb79af644_***_Paul Albert
49bb30c2c56d91e7987cc285f20ec657_***_Molly Flynn
author Paul Albert
Molly Flynn
author2 Giada Fernandez
Biagio Giaccio
Antonio Costa
Lorenzo Monaco
Sébastien Nomade
Paul Albert
Alison Pereira
Molly Flynn
Niklas Leicher
Federico Lucchi
Paola Petrosino
Danilo M. Palladino
Alfonsa Milia
Donatella Domenica Insinga
Sabine Wulf
Rebecca Kearney
Daniel Veres
Diana Jordanova
Maria Luisa Putignano
Roberto Isaia
Gianluca Sottili
format Journal article
container_title Quaternary Science Reviews
container_volume 331
container_start_page 108623
publishDate 2024
institution Swansea University
issn 0277-3791
doi_str_mv 10.1016/j.quascirev.2024.108623
publisher Elsevier BV
college_str Faculty of Science and Engineering
hierarchytype
hierarchy_top_id facultyofscienceandengineering
hierarchy_top_title Faculty of Science and Engineering
hierarchy_parent_id facultyofscienceandengineering
hierarchy_parent_title Faculty of Science and Engineering
department_str School of Biosciences, Geography and Physics - Geography{{{_:::_}}}Faculty of Science and Engineering{{{_:::_}}}School of Biosciences, Geography and Physics - Geography
document_store_str 1
active_str 0
description The Campi Flegrei (CF) caldera, in southern Italy, is the source of some the most powerful Late Pleistocene eruptions of the European sub-continent (e.g., Campanian Ignimbrite, Neapolitan Yellow Tuff eruptions). Although the CF caldera has been continuously and intensively investigated for decades, relatively little is known regarding its earliest volcanic activity. Here integrating existing and new tephrostratigraphic data we provide a comprehensive and updated framework for CF volcanic activity which has occurred at ~160 ka and between ~110 ka and ~90 ka. The new tephrostratigraphic, geochemical (EMPA + LA-ICP-MS), chronological (40Ar/39Ar dating) and grain-size distribution data relate to CF tephra deposits preserved in 41 mid-proximal (Campanian Plain), distal (Tyrrhenian Sea) and ultra-distal (Lower Danube area) sedimentary archives. Our results allow us to recognize the presence of at least 13 CF eruptions covering the investigated time frame, with 12 eruptions occurring between 110 and 90 ka. Our high-resolution stratigraphic and chronological investigation also allowed us to recognise that the Triflisco/C-22 tephra, previously considered as a single marker layer, can be actually separated into three different events, sourced from within the CF area in the short time interval of ~93-90 ka, suggesting a more complex and intense volcanic history than previously thought. Moreover, a Bayesian age-depth model, constrained by previous and new high precision 40Ar/39Ar ages, has led to a reliable estimate of the ages of those undated CF eruptions. Overall, the updated framework on the stratigraphy, chronology, dispersion, and geochemistry of the CF tephra of ~160 ka and between 110 ka and 90 ka consolidates the notion that the Middle-Late Pleistocene activity at CF area represents a significant stage of its volcanic evolution, characterised by intense and frequent explosive eruptions.
published_date 2024-05-01T14:52:32Z
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score 11.013776

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