A reconstruction of sea surface warming in the northern North Atlantic during MIS 3 ice-rafting events

L Jonkers, M Moros, MA Prins, T Dokken… - Quaternary Science …, 2010 - Elsevier
Marine isotope stage 3 (29–59 kyr BP) is characterised by rapid shifts from cold stadial to
warm interstadial periods, which may be linked to changes in the vigour of the Atlantic …
被引用次数：54 相关文章

A reconstruction of sea surface warming in the northern North Atlantic during MIS 3 ice-rafting events

L Jonkers, M Moros, MA Prins, T Dokken… - Quaternary Science …, 2010 - infona.pl
Marine isotope stage 3 (29–59 kyr BP) is characterised by rapid shifts from cold stadial to
warm interstadial periods, which may be linked to changes in the vigour of the Atlantic …
[PDF] academia.edu

[PDF][PDF] A reconstruction of sea surface warming in the northern North Atlantic during MIS 3 ice-rafting events

L Jonkers, M Moros, MA Prins, T Dokken… - Quaternary Science …, 1791 - academia.edu
abstract Marine isotope stage 3 (29e59 kyr BP) is characterised by rapid shifts from cold
stadial to warm interstadial periods, which may be linked to changes in the vigour of the …

A reconstruction of sea surface warming in the northern North Atlantic during MIS 3 ice-rafting events

L Jonkers, M Moros, MA Prins, T Dokken… - Quaternary Science …, 2010 - research.vu.nl
Abstract Marine isotope stage 3 (29-59 kyr BP) is characterised by rapid shifts from cold
stadial to warm interstadial periods, which may be linked to changes in the vigour of the …

A reconstruction of sea surface warming in the northern North Atlantic during MIS 3 ice-rafting events

L Jonkers, M Moros, MA Prins… - Quaternary Science …, 2010 - ui.adsabs.harvard.edu
Abstract Marine isotope stage 3 (29-59 kyr BP) is characterised by rapid shifts from cold
stadial to warm interstadial periods, which may be linked to changes in the vigour of the …

A reconstruction of sea surface warming in the northern North Atlantic during MIS 3 ice-rafting events

L Jonkers, M Moros, MA Prins, T Dokken… - Quaternary Science …, 2010 - orca.cardiff.ac.uk
Marine isotope stage 3 (29–59 kyr BP) is characterised by rapid shifts from cold stadial to
warm interstadial periods, which may be linked to changes in the vigour of the Atlantic …

A reconstruction of sea surface warming in the northern North Atlantic during MIS 3 ice-rafting events

L Jonkers, M Moros, MA Prins, T Dokken… - Quaternary Science …, 2010 - orca.cardiff.ac.uk
Marine isotope stage 3 (29–59 kyr BP) is characterised by rapid shifts from cold stadial to
warm interstadial periods, which may be linked to changes in the vigour of the Atlantic …
[PDF] academia.edu

[PDF][PDF] A reconstruction of sea surface warming in the northern North Atlantic during MIS 3 ice-rafting events

L Jonkers, M Moros, MA Prins, T Dokken… - Quaternary Science …, 1791 - academia.edu
abstract Marine isotope stage 3 (29e59 kyr BP) is characterised by rapid shifts from cold
stadial to warm interstadial periods, which may be linked to changes in the vigour of the …