Delayed CO2 emissions from mid-ocean ridge volcanism as a possible cause of late-Pleistocene glacial cycles

The coupled 100,000 year variations in ice volume, temperature, and atmospheric CO2 during the late Pleistocene are generally considered to arise from a combination of orbital forcing, ice dynamics, and ocean circulation. Also previously argued is that changes in glaciation influence atmospheric CO2...

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Veröffentlicht in:	Earth and planetary science letters 2017-01, Vol.457, p.238-249
Hauptverfasser:	Huybers, Peter, Langmuir, Charles H.
Format:	Artikel
Sprache:	eng
Schlagworte:	Atmospherics Carbon dioxide Earth glacial cycles Oceans Oscillations Parametrization Pleistocene Ridges Volcanic activity volcanism
Online-Zugang:	Volltext
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