Glacio-eustatic forcing on Middle Pleistocene fluvial–lacustrine depositional processes: a case history from the Tyrrhenian Sea margin of central Italy Article Swipe
Giovanni Maria Di Buduo
,
Mario Gaeta
,
Fabrizio Marra
,
Sébastien Nomade
,
Danilo M. Palladino
,
Alison Pereira
·
YOU?
·
· 2025
· Open Access
·
· DOI: https://doi.org/10.1007/s00531-025-02494-2
YOU?
·
· 2025
· Open Access
·
· DOI: https://doi.org/10.1007/s00531-025-02494-2
The complex stratigraphic setting of alternating volcanic and fluvial–lacustrine sedimentary deposits in the surroundings of Castel Cellesi village (Latium region, central Italy) offers an unprecedented opportunity to examine the influence of glacio-eustatic forcing on the depositional processes during Pleistocene times in the upper catchment of the Tiber River, in the inland sector of the Tyrrhenian Sea margin of Italy. Tight geochronologic constraints on the timing of sediment deposition have been established through precise 40 Ar/ 39 Ar dating of intervening volcanic layers. These new age constraints reveal a clear chronological correlation between sediment aggradation phases and sea-level rises, as evidenced by the δ 18 O record and relative sea-level (RSL) curve. The analysis of pyroclastic-flow deposits within incised paleo-valleys further indicates a relationship between periods of erosion or non-deposition and sea-level lowstands. Specifically, twelve 40 Ar/ 39 Ar dates have delineated three successive aggradational fluvial–lacustrine successions deposited during the sea-level rises of Marine Isotope Stages (MIS) 13, 11, and 9, as well as the erosional features associated with the sea-level drops of MIS 12 and 10. Graphical abstract 40 Ar/39Ar age constraints on the timing of sediment deposition reveal a direct chronological correlation between sediment aggradation phases and sea-level rises, as evidenced by the benthic Oxygen isotopes curve.
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- Type
- article
- Language
- en
- Landing Page
- https://doi.org/10.1007/s00531-025-02494-2
- https://link.springer.com/content/pdf/10.1007/s00531-025-02494-2.pdf
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All OpenAlex metadata
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https://doi.org/10.1007/s00531-025-02494-2Digital Object Identifier
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Glacio-eustatic forcing on Middle Pleistocene fluvial–lacustrine depositional processes: a case history from the Tyrrhenian Sea margin of central ItalyWork title
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articleOpenAlex work type
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enPrimary language
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2025Year of publication
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2025-03-10Full publication date if available
- Authors
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Giovanni Maria Di Buduo, Mario Gaeta, Fabrizio Marra, Sébastien Nomade, Danilo M. Palladino, Alison PereiraList of authors in order
- Landing page
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https://doi.org/10.1007/s00531-025-02494-2Publisher landing page
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https://link.springer.com/content/pdf/10.1007/s00531-025-02494-2.pdfDirect link to full text PDF
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hybridOpen access status per OpenAlex
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https://link.springer.com/content/pdf/10.1007/s00531-025-02494-2.pdfDirect OA link when available
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Geology, Sedimentology, Sedimentary depositional environment, Fluvial, Pleistocene, Paleontology, Structural geology, Quaternary, Structural basinTop concepts (fields/topics) attached by OpenAlex
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0Total citation count in OpenAlex
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| abstract_inverted_index.drops | 171 |
| abstract_inverted_index.rises | 151 |
| abstract_inverted_index.three | 142 |
| abstract_inverted_index.times | 40 |
| abstract_inverted_index.upper | 43 |
| abstract_inverted_index.Castel | 16 |
| abstract_inverted_index.Italy) | 22 |
| abstract_inverted_index.Italy. | 59 |
| abstract_inverted_index.Marine | 153 |
| abstract_inverted_index.Oxygen | 206 |
| abstract_inverted_index.River, | 48 |
| abstract_inverted_index.Stages | 155 |
| abstract_inverted_index.curve. | 111, 208 |
| abstract_inverted_index.dating | 78 |
| abstract_inverted_index.direct | 191 |
| abstract_inverted_index.during | 38, 148 |
| abstract_inverted_index.inland | 51 |
| abstract_inverted_index.margin | 57 |
| abstract_inverted_index.offers | 23 |
| abstract_inverted_index.phases | 95, 197 |
| abstract_inverted_index.record | 106 |
| abstract_inverted_index.reveal | 87, 189 |
| abstract_inverted_index.rises, | 98, 200 |
| abstract_inverted_index.sector | 52 |
| abstract_inverted_index.timing | 65, 185 |
| abstract_inverted_index.twelve | 134 |
| abstract_inverted_index.within | 117 |
| abstract_inverted_index.(Latium | 19 |
| abstract_inverted_index.Ar/39Ar | 180 |
| abstract_inverted_index.Cellesi | 17 |
| abstract_inverted_index.Isotope | 154 |
| abstract_inverted_index.benthic | 205 |
| abstract_inverted_index.between | 92, 124, 194 |
| abstract_inverted_index.central | 21 |
| abstract_inverted_index.complex | 2 |
| abstract_inverted_index.erosion | 127 |
| abstract_inverted_index.examine | 28 |
| abstract_inverted_index.forcing | 33 |
| abstract_inverted_index.further | 120 |
| abstract_inverted_index.incised | 118 |
| abstract_inverted_index.layers. | 82 |
| abstract_inverted_index.periods | 125 |
| abstract_inverted_index.precise | 73 |
| abstract_inverted_index.region, | 20 |
| abstract_inverted_index.setting | 4 |
| abstract_inverted_index.through | 72 |
| abstract_inverted_index.village | 18 |
| abstract_inverted_index.Abstract | 0 |
| abstract_inverted_index.abstract | 178 |
| abstract_inverted_index.analysis | 113 |
| abstract_inverted_index.deposits | 11, 116 |
| abstract_inverted_index.features | 166 |
| abstract_inverted_index.isotopes | 207 |
| abstract_inverted_index.relative | 108 |
| abstract_inverted_index.sediment | 67, 93, 187, 195 |
| abstract_inverted_index.volcanic | 7, 81 |
| abstract_inverted_index.Graphical | 177 |
| abstract_inverted_index.catchment | 44 |
| abstract_inverted_index.deposited | 147 |
| abstract_inverted_index.erosional | 165 |
| abstract_inverted_index.evidenced | 100, 202 |
| abstract_inverted_index.indicates | 121 |
| abstract_inverted_index.influence | 30 |
| abstract_inverted_index.processes | 37 |
| abstract_inverted_index.sea-level | 97, 109, 131, 150, 170, 199 |
| abstract_inverted_index.Tyrrhenian | 55 |
| abstract_inverted_index.associated | 167 |
| abstract_inverted_index.delineated | 141 |
| abstract_inverted_index.deposition | 68, 188 |
| abstract_inverted_index.lowstands. | 132 |
| abstract_inverted_index.successive | 143 |
| abstract_inverted_index.Pleistocene | 39 |
| abstract_inverted_index.aggradation | 94, 196 |
| abstract_inverted_index.alternating | 6 |
| abstract_inverted_index.constraints | 62, 86, 182 |
| abstract_inverted_index.correlation | 91, 193 |
| abstract_inverted_index.established | 71 |
| abstract_inverted_index.intervening | 80 |
| abstract_inverted_index.opportunity | 26 |
| abstract_inverted_index.sedimentary | 10 |
| abstract_inverted_index.successions | 146 |
| abstract_inverted_index.depositional | 36 |
| abstract_inverted_index.relationship | 123 |
| abstract_inverted_index.surroundings | 14 |
| abstract_inverted_index.Specifically, | 133 |
| abstract_inverted_index.aggradational | 144 |
| abstract_inverted_index.chronological | 90, 192 |
| abstract_inverted_index.paleo-valleys | 119 |
| abstract_inverted_index.stratigraphic | 3 |
| abstract_inverted_index.unprecedented | 25 |
| abstract_inverted_index.geochronologic | 61 |
| abstract_inverted_index.non-deposition | 129 |
| abstract_inverted_index.glacio-eustatic | 32 |
| abstract_inverted_index.pyroclastic-flow | 115 |
| abstract_inverted_index.fluvial–lacustrine | 9, 145 |
| cited_by_percentile_year | |
| countries_distinct_count | 0 |
| institutions_distinct_count | 6 |
| citation_normalized_percentile.value | 0.06935454 |
| citation_normalized_percentile.is_in_top_1_percent | False |
| citation_normalized_percentile.is_in_top_10_percent | False |