Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Roland Neofitu"'
Autor:
Roland Neofitu, Chris Mark, Suzanne O'Connell, Samuel Kelley, Delia Rösel, Thomas Zack, Michael Flowerdew, J. Stephen Daly
Antarctic ice-sheet instability is recorded by ice-rafted debris (IRD) in mid- to high-latitude marine sediment, especially throughout climate transitions. The middle Miocene climatic transition (MMCT), 14.2 to 13.8 Ma, which marks the end of a signi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e2e33046881b07d58fce90e47170b276
https://doi.org/10.5194/egusphere-egu22-6484
https://doi.org/10.5194/egusphere-egu22-6484
Autor:
Delia Rösel, Suzanne O'Connell, Roland Neofitu, Samuel E. Kelley, Thomas Zack, Chris Mark, J. Stephen Daly
Antarctic ice-sheet instability is recorded by ice-rafted debris (IRD) in mid- to high-latitude marine sediment, especially throughout climate transitions. The middle Miocene climatic transition (MMCT), 14.2 to 13.8 Ma, which marks the end of a signi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::498bd31a2e35edce0cf3b85df353eec7
https://doi.org/10.5194/egusphere-egu21-4719
https://doi.org/10.5194/egusphere-egu21-4719
Autor:
N. Douss, Michele Rebesco, J. S. Daly, Renata G. Lucchi, Roland Neofitu, Chris Mark, Samuel E. Kelley, Caterina Morigi
Late Quaternary Antarctic ice-sheet instability is recorded by ice-rafted debris (IRD) in mid- to high-latitude marine sediment, especially during marine isotope stages (MIS) 2-3, but drivers of this instability remain enigmatic (Labeyrie et al., 198
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::06fdf3831cbfbbc8b5b0e8bce7ec1f9d
https://doi.org/10.5194/egusphere-egu2020-5011
https://doi.org/10.5194/egusphere-egu2020-5011
Autor:
Stefano Miserocchi, Ester Colizza, Nessim Douss, Chris Mark, Michele Rebesco, Renata G. Lucchi, Giuliana Villa, Rudy Conte, Patrizia Macrì, Paola Del Carlo, Aldo Winkler, Yanguang Liu, Davide Persico, Leonardo Langone, Caterina Morigi, Roland Neofitu, Andrea Caburlotto, Alessio Di Roberto
The Ross Ice Shelf is the Antarctic region that over the last deglaciation experienced the greatest change in areal ice cover. Today, cold, dense and saline water masses (brines) produced in the Ross Sea polynya, flow from the shelf to the deep ocean
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::55788c745298982518648bd9827fc3be
https://doi.org/10.5194/egusphere-egu2020-12940
https://doi.org/10.5194/egusphere-egu2020-12940