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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
Publikováno v:
Journal of Wildlife Management. 74:1395-1399