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Persistent influence of obliquity on ice age terminations since the Middle Pleistocene transition.

Accepted version
Peer-reviewed

Type

Article

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Authors

Abstract

Radiometric dating of glacial terminations over the past 640,000 years suggests pacing by Earth's climatic precession, with each glacial-interglacial period spanning four or five cycles of ~20,000 years. However, the lack of firm age estimates for older Pleistocene terminations confounds attempts to test the persistence of precession forcing. We combine an Italian speleothem record anchored by a uranium-lead chronology with North Atlantic ocean data to show that the first two deglaciations of the so-called 100,000-year world are separated by two obliquity cycles, with each termination starting at the same high phase of obliquity, but at opposing phases of precession. An assessment of 11 radiometrically dated terminations spanning the past million years suggests that obliquity exerted a persistent influence on not only their initiation but also their duration.

Description

Keywords

37 Earth Sciences, 3709 Physical Geography and Environmental Geoscience, 3705 Geology

Journal Title

Science

Conference Name

Journal ISSN

0036-8075
1095-9203

Volume Title

367

Publisher

American Association for the Advancement of Science (AAAS)

Rights

All rights reserved
Sponsorship
Royal Society (RP\R\180003)
Natural Environment Research Council (NE/R000204/1)