(Q57532796)

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Progressive reduction in NE Atlantic intermediate water ventilation prior to Heinrich events: Response to NW European ice sheet instabilities?

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Progressive reduction in NE Atlantic intermediate water ventilation prior to Heinrich events: Response to NW European ice sheet instabilities? (English)

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I. R. Hall

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V. L. Peck

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R. Zahn

3

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J. D. Scourse

4

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publication date

January 2007

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G3: Geochemistry, Geophysics, Geosystems

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8

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1

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Heinrich events: Massive late Pleistocene detritus layers of the North Atlantic and their global climate imprint

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Molecular motors. Keeping the beat

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Multidecadal ocean variability and NW European ice sheet surges during the last deglaciation

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Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes

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High resolution evidence for linkages between NW European ice sheet instability and Atlantic Meridional Overturning Circulation

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The relationship of Heinrich events and their European precursors over the past 60ka BP: a multi-proxy ice-rafted debris provenance study in the North East Atlantic

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Evidence from the high-latitude North Atlantic for variations in Antarctic Intermediate water flow during the last deglaciation

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The origin of Heinrich layers: evidence from H2 for European precursor events

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Oxygen Isotope and Palaeomagnetic Stratigraphy of Equatorial Pacific Core V28-238: Oxygen Isotope Temperatures and Ice Volumes on a 105 Year and 106 Year Scale

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Catastrophic ice shelf breakup as the source of Heinrich event icebergs

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Hudson Bay-Hudson Strait jökulhlaups and Heinrich events: a hypothesis

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Changes in deep water hydrology during the Last Deglaciation

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Binge/purge oscillations of the Laurentide Ice Sheet as a cause of the North Atlantic's Heinrich events

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The δ13C in benthic foraminiferal tests ofFontbotia wuellerstorfi(Schwager) Relative to the δ13C of dissolved inorganic carbon in Southern Ocean Deep Water: Implications for glacial ocean circulation models

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Identifiers

10.1029/2006GC001321

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2007GGG.....8.1N10P

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