A simple rule to determine which insolation cycles lead to interglacials.

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Title: A simple rule to determine which insolation cycles lead to interglacials.
Authors: Tzedakis PC; Environmental Change Research Centre, Department of Geography, University College London, London, UK., Crucifix M; Université catholique de Louvain, Earth and Life Institute, Georges Lemaître Centre for Earth and Climate Research, Louvain-la-Neuve, Belgium., Mitsui T; Université catholique de Louvain, Earth and Life Institute, Georges Lemaître Centre for Earth and Climate Research, Louvain-la-Neuve, Belgium., Wolff EW; Department of Earth Sciences, University of Cambridge, Cambridge, UK.
Source: Nature [Nature] 2017 Feb 22; Vol. 542 (7642), pp. 427-432.
Publication Type: Journal Article; Research Support, Non-U.S. Gov't
Journal Info: Publisher: Nature Publishing Group Country of Publication: England NLM ID: 0410462 Publication Model: Print Cited Medium: Internet ISSN: 1476-4687 (Electronic) Linking ISSN: 00280836 NLM ISO Abbreviation: Nature Subsets: PubMed not MEDLINE
Database: MEDLINE Ultimate
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  Data: <searchLink fieldCode="AU" term="%22Tzedakis+PC%22">Tzedakis PC</searchLink>; Environmental Change Research Centre, Department of Geography, University College London, London, UK.<br /><searchLink fieldCode="AU" term="%22Crucifix+M%22">Crucifix M</searchLink>; Université catholique de Louvain, Earth and Life Institute, Georges Lemaître Centre for Earth and Climate Research, Louvain-la-Neuve, Belgium.<br /><searchLink fieldCode="AU" term="%22Mitsui+T%22">Mitsui T</searchLink>; Université catholique de Louvain, Earth and Life Institute, Georges Lemaître Centre for Earth and Climate Research, Louvain-la-Neuve, Belgium.<br /><searchLink fieldCode="AU" term="%22Wolff+EW%22">Wolff EW</searchLink>; Department of Earth Sciences, University of Cambridge, Cambridge, UK.
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  Data: <searchLink fieldCode="JN" term="%220410462%22">Nature</searchLink> [Nature] 2017 Feb 22; Vol. 542 (7642), pp. 427-432.
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        Value: 10.1038/nature21364
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      – TitleFull: A simple rule to determine which insolation cycles lead to interglacials.
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