New constraints on Middle-Late Pleistocene large-magnitude eruptions from Campi Flegrei

Autor: Giada Fernandez, Biagio Giaccio, Antonio Costa, Lorenzo Monaco, Paul Albert, Sebastien Nomade, Alison Pereira, Niklas Leicher, Federico Lucchi, Paola Petrosino, Alfonsa Milia, Donatella Insinga, Sabine Wulf, Rebecca Kearney, Daniel Veres, Diana Jordanova, Gianluca Sottili

Assessing the history, dynamics and magnitude of pre-historic explosive volcanic eruptions relies heavily on the completeness of the stratigraphic records, the spatial distribution, and the sedimentological features of the pyroclastic deposits. Near-

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::9bba867adc91f4fa69d5b105da71bb2e
https://doi.org/10.5194/egusphere-egu23-6552

On the occurrence of the Neapolitan Yellow Tuff tephra in the Northern Phlegraean Fields offshore (Eastern Tyrrhenian margin; Italy)

Autor: Gemma Aiello, Agostino Meo, Maria Rosaria Senatore, Marina Iorio, Donatella Insinga

Publikováno v: Italian Journal of Geosciences. 136:263-274

A main volcanic marker has been identified for the first time on the continental shelf of the northern Phlegraean Fields in the Gaeta Gulf (Campania region, eastern Tyrrhenian margin, Italy) by means of Subbottom Chirp profile grid and stratigraphic

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::0ec387448312ae094ef4042cbf3234c4
https://doi.org/10.3301/ijg.2017.06

The palaeoclimatic and palaeoceanographic history of the Gulf of Taranto (Mediterranean Sea) in the last 15 ky

Autor: Paola Rumolo, F. Molisso, Salvatore Passaro, V. Di Donato, M. Iorio, C. Cardines, Donatella Insinga

Publikováno v: Global and planetary change
172 (2019): 278–297. doi:10.1016/j.gloplacha.2018.10.014
info:cnr-pdr/source/autori:Di Donato, V.; Insinga, D. D.; Iorio, M.; Molisso, F.; Rumolo, P.; Cardines, C.; Passaro S./titolo:The palaeoclimatic and palaeoceanographic history of the Gulf of Taranto (Mediterranean Sea) in the last 15 ky/doi:10.1016%2Fj.gloplacha.2018.10.014/rivista:Global and planetary change (Print)/anno:2019/pagina_da:278/pagina_a:297/intervallo_pagine:278–297/volume:172

A multidisciplinary study, which includes micropaleontology, sedimentology and geochemistry, was carried out on the TEA-C6 core, raised in the Gulf of Taranto (north-western Ionian Sea). The chronological framework was yielded by tephrostratigraphy c

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4d9e82205f4b359367f841fff7369259
http://hdl.handle.net/11588/758594

Seismic stratigraphy of upper Quaternary shallow-water contourite drifts in the Gulf of Taranto (Ionian Sea, southern Italy)

Autor: Donatella Insinga, Fabrizio Pepe, F. Molisso, V. Di Donato, R. Dera, Luigi Ferranti, Carla Faraci, Marco Sacchi, Salvatore Passaro

Publikováno v: Marine geology
397 (2018): 79–92. doi:10.1016/j.margeo.2017.12.004
info:cnr-pdr/source/autori:Pepe, F.; Di Donato, V.; Insinga, D.; Molisso, F.; Faraci, C.; Sacchi, M.; Dera, R.; Ferranti, L.; Passaro, S./titolo:Seismic stratigraphy of upper Quaternary shallow-water contourite drifts in the Gulf of Taranto (Ionian Sea, southern Italy)/doi:10.1016%2Fj.margeo.2017.12.004/rivista:Marine geology (Print)/anno:2018/pagina_da:79/pagina_a:92/intervallo_pagine:79–92/volume:397

The occurrence of articulated seafloor morphology over continental shelf-upper slope environments, may result in a significant change in the patterns and intensity of basin-scale thermohaline circulation during eustatic sea-level fluctuations. These

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::40f764ab3e86ad83e6629bcdadd3ef44
http://hdl.handle.net/11570/3121352

Benthic foraminifera as indicators of relative sea-level fluctuations: Paleoenvironmental and paleoclimatic reconstruction of a Holocene marine succession (Calabria, south-eastern Tyrrhenian Sea)

Autor: Giovanna Scopelliti, Donatella Insinga, Flavia Molisso, Antonio Caruso, Fabrizio Pepe, Marco Sacchi, Carmine Lubritto, Claudia Cosentino

Publikováno v: Quaternary international 439 (2017): 79–101. doi:10.1016/j.quaint.2016.10.012
info:cnr-pdr/source/autori:Cosentino, C.; Molisso, F.; Scopelliti, G.; Caruso, A.; Insinga, D. D.; Lubritto, C.; Pepe, F.; Sacchi, M./titolo:Benthic foraminifera as indicators of relative sea-level fluctuations: Paleoenvironmental and paleoclimatic reconstruction of a Holocene marine succession (Calabria, south-eastern Tyrrhenian Sea)/doi:10.1016%2Fj.quaint.2016.10.012/rivista:Quaternary international/anno:2017/pagina_da:79/pagina_a:101/intervallo_pagine:79–101/volume:439
Quaternary international (2017).
info:cnr-pdr/source/autori:C. Cosentino a, *, F. Molisso b, G. Scopelliti a, A. Caruso a, D.D. Insinga b, C. Lubritto c, F. Pepe a, M. Sacchi b/titolo:Benthic foraminifera as indicators of relative sea-level fluctuations: Paleoenvironmental and paleoclimatic reconstruction of a Holocene marine succession (Calabria, south-eastern Tyrrhenian Sea)/doi:/rivista:Quaternary international/anno:2017/pagina_da:/pagina_a:/intervallo_pagine:/volume

This study presents the results of an integrated stratigraphic analysis conducted on a marine gravity core (MSK-12 C4) recovered from the outer continental shelf (82 mwater depth) of western Calabria, ~2.6 km, NE of Capo Vaticano (Eastern Tyrrhenian

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b390b176490cafd25dff44955826ef13