FN Archimer Export Format PT J TI Towards a quaternary time scale BT AF BERGGREN, W.A. HAYS, J.D. BURCKLE, L.H. KENNETT, J.P. CITA, M.B. OPDYKE, N.D. COOKE, H.B.S. PASTOURET, Léo FUNNELL, B.M. SHACKLETON, N.J. GARTNER, S. TAKAYANAGI, Y. AS 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:; FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:; TC 0 UR https://archimer.ifremer.fr/doc/1978/publication-5316.pdf LA English DT Article DE ;Histoire Ifremer AB The stratigraphic subdivision of the Quaternary deep-sea record is not only of significance to stratigraphers but also to those who seek to understand processes that are recorded in these sediments : for example, climatic change and its causes, ocean chemistry and its variation through time, the phenomena of faunal and floral evolution and extinction, and many others. [NOT CONTROLLED OCR] PY 1978 PD NOV SO Quaternary Research BP 113 EP 138 ID 5316 ER EF