4.7 Article

Evidence for glaciation in the Northern Hemisphere back to 44 Ma from ice-rafted debris in the Greenland Sea

Journal

EARTH AND PLANETARY SCIENCE LETTERS
Volume 265, Issue 1-2, Pages 112-122

Publisher

ELSEVIER SCIENCE BV
DOI: 10.1016/j.epsl.2007.09.045

Keywords

paleoclimate; Northern Hemisphere glaciation; ice-rafted debris; greenhouse-icehouse transition; Eocene-Oligocene transition; polar climate

Funding

  1. NERC [NE/D009049/1] Funding Source: UKRI
  2. Natural Environment Research Council [NE/C510583/1, NE/D009049/1] Funding Source: researchfish

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The widely accepted age estimate for the onset of glaciation in the Northern Hemisphere ranges between 2 and 15 million years ago (Ma). However, recent studies indicate the date for glacial onset may be significantly older. We report the presence of ice-rafted debris (IRD) in similar to 44 to 30 Ma sediments from the Greenland Sea, evidence for glaciation in the North Atlantic during the Middle Eocene to Early Oligocene. Detailed sedimentological evidence indicates that glaciers extended to sea level in the region, allowing icebergs to be produced. IRD may have been sourced from tidewater glaciers, small ice caps, and/or a continental ice sheet. (c) 2007 Elsevier B.V. All rights reserved.

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