Zobrazeno 1 - 4 of 4 pro vyhledávání: '"Marina Verducci"'
1
Paleoenvironmental conditions preceding the Messinian Salinity Crisis in the Central Mediterranean: Integrated data from the Upper Miocene Trave section (Italy)
Autor: Fabrizio Lirer, Silvia Maria Iaccarino, Agata Di Stefano, Luciana Ferraro, Marina Verducci, Frits Hilgen, S. K. Hüsing
Publikováno v: Palaeogeography, palaeoclimatology, palaeoecology 297 (2010): 37–53. doi:10.1016/j.palaeo.2010.07.012
info:cnr-pdr/source/autori:A. Di Stefano; M. Verducci; F. Lirer; L. Ferraro; S. M Iaccarino; S. K. Hüsing; F. J. Hilgen/titolo:Paleoenvironmental conditions preceding the Messinian Salinity Crisis in Central Mediterranean: integrated data from the Upper Miocene Trave section (Italy)./doi:10.1016%2Fj.palaeo.2010.07.012/rivista:Palaeogeography, palaeoclimatology, palaeoecology/anno:2010/pagina_da:37/pagina_a:53/intervallo_pagine:37–53/volume:297
Integrated data of calcareous plankton and benthic foraminifers from the pre-evaporitic interval of Trave section (Central Italy) allowed the reconstruction of surface and bottom-water conditions in the Central Mediterranean during the interval from
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9018226d4f6676d200077092ef842d3f
https://doi.org/10.1016/j.palaeo.2010.07.012
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3
Integrated stratigraphy of the St. Thomas section (Malta Island): A reference section for the lower Burdigalian of the Mediterranean Region
Autor: Gianfranco Salvatorini, Luca Maria Foresi, Leonardo Sagnotti, Fabrizio Lirer, Marina Verducci, Niccolò Baldassini, Roberto Mazzei, Chiara Caricchi, A. Di Stefano
The 91.15 m thick St. Thomas section belongs to the Middle Globigerina Limestone, which is the intermediate member of the Globigerina Limestone Formation, and crops out along the eastern cliff of the Delimara Peninsula (the south-eastern part of Malt
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8e0c9459f4e3e0bcbd63330871fb4edb
http://hdl.handle.net/11365/48514
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4
The Middle Miocene Climatic Transition in the Southern Ocean: evidence of paleoclimatic and hydrographic changes at Kerguelen Plateau from planktonic foraminifers and stable isotopes
Autor: Mario Sprovieri, Fabrizio Lirer, George H Scott, Marina Verducci, Nicola Pelosi, Luca Maria Foresi
Publikováno v: Palaeogeography, palaeoclimatology, palaeoecology 280 (2009): 371–386. doi:10.1016/j.palaeo.2009.06.024
info:cnr-pdr/source/autori:Verducci M.; Foresi L.M.; Scott G.H.; Sprovieri M.; Lirer F.; Pelosi N./titolo:The Middle Miocene Climatic Transition in the Southern Ocean: evidence of paleoclimatic and hydrographic changes at Kerguelen Plateau from planktonic foraminifera and stable isotopes/doi:10.1016%2Fj.palaeo.2009.06.024/rivista:Palaeogeography, palaeoclimatology, palaeoecology/anno:2009/pagina_da:371/pagina_a:386/intervallo_pagine:371–386/volume:280
info:cnr-pdr/source/autori:Verducci M.; Foresi L.; Scott G.H.; Sprovieri M.; Lirer F.; Pelosi N./titolo:The Middle Miocene Climatic Transition in the Southern Ocean: evidence of paleoclimatic and hydrographic changes at Kerguelen Plateau from planktonic foraminifera and stable isotopes/doi:10.1016%2Fj.palaeo.2009.06.024/rivista:Palaeogeography, palaeoclimatology, palaeoecology/anno:2009/pagina_da:371/pagina_a:386/intervallo_pagine:371–386/volume:280
Middle Miocene (14.8–11.9 Ma) deep-sea sediments from ODP Hole 747A (Kerguelen Plateau, southern Indian Ocean) contain abundant, well-preserved and diverse planktonic foraminiferal assemblages. A detailed study of the climatic and hydrographic chan
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::35056318c629145bb6d28f9550f3a82b
http://hdl.handle.net/11573/1611865
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