TY - JOUR
KW - Event stratigraphy
KW - North Atlantic
KW - Palaeoclimate
KW - Radiocarbon
KW - Tephrochronology
AU - W. Austin
AU - F. Hibbert
AU - S. Rasmussen
AU - C. Peters
AU - P. Abbott
AU - C. Bryant
AB - Two high resolution marine sediment cores located 83 km apart in the NE Atlantic have been studied: MD95-2006 (Barra Fan; 57\textdegree01.82 N, 10\textdegree03.48 W; 2120 m water depth) and MD04-2822 (Rockall Trough; 56\textdegree50.54 N, 11\textdegree22.96 W; 2344 m water depth). The records are anchored to the NGRIP ice core stratigraphy and GICC05 chronology by the presence of geochemically characterized Fugloyarbanki tephra and further tested by radiocarbon age control. Replicated sea surface temperature (SST) records show evidence for an abrupt and short-lived warming within Greenland Stadial (GS)-3, to which we tentatively assign an age of ca 25.6\textendash24.8 kyr GICC05 b2k. Based on these and another marine palaeoclimate record (LINK17) from the Faroe-Shetland Channel, we propose a new three-fold event stratigraphy for GS-3 within the North East Atlantic region. The recognition of this warming event within GS-3 in NE Atlantic SST records demonstrates that such events may not readily be identified within the coldest stadials of the Greenland ice cores, highlights the need for carefully constructed event stratigraphies (independently tested by the use of tephra isochrones and radiocarbon) and illustrates pervasive millennial-scale climate variability of the North Atlantic region (Dansgaard-Oeschger (D/O) events) is deeply embedded in the dynamics of Atlantic Meridional Overturning Circulation (AMOC).
BT - Quaternary Science Reviews
N1 - doi: 10.1016/j.quascirev.2010.12.014
N2 - Two high resolution marine sediment cores located 83 km apart in the NE Atlantic have been studied: MD95-2006 (Barra Fan; 57\textdegree01.82 N, 10\textdegree03.48 W; 2120 m water depth) and MD04-2822 (Rockall Trough; 56\textdegree50.54 N, 11\textdegree22.96 W; 2344 m water depth). The records are anchored to the NGRIP ice core stratigraphy and GICC05 chronology by the presence of geochemically characterized Fugloyarbanki tephra and further tested by radiocarbon age control. Replicated sea surface temperature (SST) records show evidence for an abrupt and short-lived warming within Greenland Stadial (GS)-3, to which we tentatively assign an age of ca 25.6\textendash24.8 kyr GICC05 b2k. Based on these and another marine palaeoclimate record (LINK17) from the Faroe-Shetland Channel, we propose a new three-fold event stratigraphy for GS-3 within the North East Atlantic region. The recognition of this warming event within GS-3 in NE Atlantic SST records demonstrates that such events may not readily be identified within the coldest stadials of the Greenland ice cores, highlights the need for carefully constructed event stratigraphies (independently tested by the use of tephra isochrones and radiocarbon) and illustrates pervasive millennial-scale climate variability of the North Atlantic region (Dansgaard-Oeschger (D/O) events) is deeply embedded in the dynamics of Atlantic Meridional Overturning Circulation (AMOC).
PY - 2011
SN - 0277-3791
SP - 154
EP - 163
T2 - Quaternary Science Reviews
TI - The synchronization of palaeoclimatic events in the NorthAtlantic region during Greenland Stadial 3 (ca 27.5 to 23.3 kyr b2k)
UR - http://www.sciencedirect.com/science/article/pii/S0277379110004452
VL - 36
ER -