Evolution of ocean temperature and ice volume through the mid-Pleistocene climate transition.

@article{Elderfield2012EvolutionOO,
  title={Evolution of ocean temperature and ice volume through the mid-Pleistocene climate transition.},
  author={Harry Elderfield and Patrizia Ferretti and Mervyn J. Greaves and Simon Crowhurst and I. Nick McCave and David A Hodell and Alexander M. Piotrowski},
  journal={Science},
  year={2012},
  volume={337 6095},
  pages={704-9}
}
Earth's climate underwent a fundamental change between 1250 and 700 thousand years ago, the mid-Pleistocene transition (MPT), when the dominant periodicity of climate cycles changed from 41 thousand to 100 thousand years in the absence of substantial change in orbital forcing. Over this time, an increase occurred in the amplitude of change of deep-ocean foraminiferal oxygen isotopic ratios, traditionally interpreted as defining the main rhythm of ice ages although containing large effects of… CONTINUE READING
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