TY - JOUR
KW - Heinrich events
KW - ice-rafting
KW - North Atlantic
KW - origins
KW - Sr and Nd isotopes
AU - Hilde Snoeckx
AU - Francis Grousset
AU - Marie Revel
AU - An Boelaert
AB - This paper reports the Sr\textendashNd isotopic composition of the carbonate-free sand (63 μm\textendash1 mm) fraction of Heinrich layers 3 and 4 from about 17 cores from the northern Atlantic Ocean (38\textdegreeN to 68\textdegreeN). The results indicate that the transporting icebergs were calved from many ice sheets from around the North Atlantic (at least the Fennoscandian, Icelandic and Laurentide). Our isotopic data show a more distinctly European origin for ice-rafted debris (IRD) deposited during the \textquoteleftatypical Heinrich event H3 than for background IRD. In contrast, Heinrich layer H4, a representative of \textquotelefttypical Heinrich events H1, H2, H4, and H5, presents a clear dominant Laurentide signal. This result confirms that these \textquotelefttypical Heinrich events are associated with a massive discharge of icebergs from the Laurentide ice sheet. However, the theory that the Laurentide ice sheet set the events into motion [Alley, R.B., MacAyeal, D.R., 1993. Ice-rafted debris associated with binge/purge oscillations of the Laurentide Ice Sheet. Paleoceanography 9 (4), 503\textendash511] cannot explain the fact that a European signal of an early-H4 sample has been observed prior to the Laurentide signature of a late-H4 sample in the same core, along the European margin. This observation indicates that the European ice sheets may have surged before the North American ones, and suggests that the Laurentide ice sheet was not the sole motor behind the Heinrich events. Moreover, in the Norwegian Sea, IRD has a Scandinavian origin in both H3 and H4.
BT - Marine Geology
M1 - 1-4
N1 - doi: 10.1016/S0025-3227(98)00168-6
N2 - This paper reports the Sr\textendashNd isotopic composition of the carbonate-free sand (63 μm\textendash1 mm) fraction of Heinrich layers 3 and 4 from about 17 cores from the northern Atlantic Ocean (38\textdegreeN to 68\textdegreeN). The results indicate that the transporting icebergs were calved from many ice sheets from around the North Atlantic (at least the Fennoscandian, Icelandic and Laurentide). Our isotopic data show a more distinctly European origin for ice-rafted debris (IRD) deposited during the \textquoteleftatypical Heinrich event H3 than for background IRD. In contrast, Heinrich layer H4, a representative of \textquotelefttypical Heinrich events H1, H2, H4, and H5, presents a clear dominant Laurentide signal. This result confirms that these \textquotelefttypical Heinrich events are associated with a massive discharge of icebergs from the Laurentide ice sheet. However, the theory that the Laurentide ice sheet set the events into motion [Alley, R.B., MacAyeal, D.R., 1993. Ice-rafted debris associated with binge/purge oscillations of the Laurentide Ice Sheet. Paleoceanography 9 (4), 503\textendash511] cannot explain the fact that a European signal of an early-H4 sample has been observed prior to the Laurentide signature of a late-H4 sample in the same core, along the European margin. This observation indicates that the European ice sheets may have surged before the North American ones, and suggests that the Laurentide ice sheet was not the sole motor behind the Heinrich events. Moreover, in the Norwegian Sea, IRD has a Scandinavian origin in both H3 and H4.
PY - 1999
SN - 0025-3227
SP - 197
EP - 208
T2 - Marine Geology
TI - European contribution of ice-rafted sand to Heinrich layers H3 and H4
UR - http://www.sciencedirect.com/science/article/pii/S0025322798001686
VL - 158
ER -