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Author Title Type [ Year(Desc)]
Filters: Author is Ravaioli, M.  [Clear All Filters]
1999
Giglio F., Frignani M., Langone L., Morigi C., Pianosi G., Ravaioli M..  1999.  Biogenic silica and organic carbon in sediments from the Pacific sector of the Southern Ocean.--Abstract. 8th International Symposium on Antarctic Earch Sciences. :119.
Morigo C., Capotondi L., Ravaioli M., Giglio F., Turi B., Brilli M., Langone L..  1999.  Paleoceanographic changes in the Southern Ocean (Pacific Sector) during the last 14 ka.- -Abstract. Third International SO-JGOFS Symposium.
Morigi C., Capotondi L., Ravaioli M., Giglio F., Turi B., Brilli M., Frignani M., Langone L..  1999.  Planktic foraminifera and oxygen isotope as proxies for paleoceanographic reconstruction in the Southern Ocean during the last deglacial time--Abstract. Convegno Glaciologia e Paleoclima. :70-71.
2000
Giglio F., Langone L., Ravaioli M., Frignani M., Mangini A., Fonti P..  2000.  Glacial-Interglacial variations in the accumulation rates of major biogenic components in the Southern Pacific Ocean sediments--Abstract. Third International SO-JGOFS Symposium.
Langone L., Giglio F., Ravaioli M., Frignani M., Marozzi G., Rovatti G..  2000.  Late Quaternary sedimentary fluctuations of biogenic fluxes driven by climatic changes in the Southern Ocean--abstract. XXV General Assembly of European Geophysical Society.
Morigi C., Capotondi L., Ravaioli M., Giglio F., Turi B., Brilli M., Langone L..  2000.  Paleoceanographic changes in the Southern Ocean (Pacific sector) during the last 14 Ka.--Poster. Third International SO-JGOFS Symposium.
2001
Giglio F., Langone L., Morigi C., Frignani M., Ravaioli M..  2001.  Biogenic silica and organic carbon in sediments from the Pacific Sector of the Southern Ocean. Antarctic Earth Sciences at the close of a Millenium: Proceedings 8th International Symposium on Artarctic Earth Sciences. 8th:35.
Morigi C., Capotondi L., Giglio F., Langone L., Brilli M., Turi B., Ravaioli M..  2001.  Oceanic changes in the southern Pacific Ocean during the last deglaciation time, as recorded by planktic foraminifers and oxigen isotopes. --Extended abstract. ANTOSTRAT Symposium on "The geologic record of the Antarctic ice sheet from drilling, coring and seismic studies". :137.
Morigi C., Capotondi L., Giglio F., Langone L., Turi B., Brilli M., Ravaioli M..  2001.  Paleoceanographic changes in the Southern Ocean, during the last deglaciation time, as recorded by planktic foraminifers and oxygen isotopes--Poster. ANTOSTRAT Symposium on "The geologic record of the Antarctic ice sheet from drilling, coring and seismic studies"--Poster. :137.
Morigi C., Capotondi L., Langone L., Giglio F., Ravaioli M..  2001.  Possible record of the yunger dryas event in sediments of the southern ocean (Pacific sector)--abstract. AUG.
Morigi C., Capotondi L., Langone L., Giglio F., Ravaioli M..  2001.  Possible record of the yunger dryas event in sediments of the Southern Ocean (Pacific Sector)--Poster. AUG.
2003
Langone L., Capotondi L., Giglio F., Focaccia P., C M, Ravaioli M..  2003.  Late-Quaternary cold events recorded in the Southern Ocean sediments, Pacific Sector. Terra Antartica. 9:100-105.
Orsini G., Giglio F., Langone L., Ravaioli M..  2003.  Paleoenvironmental inferences from core Anta95-1 (Granite Harobr, Sw Ross Sea-Antarctica). Terra Antarctica reports. 8:133-138.
Morigi C., Capotondi L., Giglio F., Langone L., Brilli M., Turi B., Ravaioli M..  2003.  A possible record of the Younger Dryas event in deep-sea sediments of the Southern Ocean (Pacific sector). Palaeogeography Palaeoclimatology Palaeoecology. 198(1-2):265-278.
Frignani M., Giglio F., Accornero A., Langone L., Ravaioli M..  2003.  Sediment characteristics at selected sites of the Ross Sea continental shelf: does the sedimentary record reflect water column fluxes? Antarctic Science. 15(1):133-139.
2013
Tesi T., Langone L., Giani M., Ravaioli M., Miserocchi S..  2013.  Source, diagenesis, and fluxes of particulate organic carbon along the western Adriatic Sea (Mediterranean Sea). Marine Geology. 337:156-170.

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