Impact of a northern-hemispherical cryosphere on late Pliensbachian–early Toarcian climate and environment evolution

@article{Ruebsam2021ImpactOA,
  title={Impact of a northern-hemispherical cryosphere on late Pliensbachian–early Toarcian climate and environment evolution},
  author={Wolfgang Ruebsam and Lorenz Schwark},
  journal={Special Publications},
  year={2021},
  volume={514},
  pages={359 - 385}
}
Abstract The historical view of an equable Jurassic greenhouse world has been challenged by recent studies documenting recurrent alternation between contrasting climate modes. Cooling of high-latitudinal areas may have been caused by orogenic processes at the northern margin of the Tethys Ocean that reduced heat transport towards the polar regions. Warm phases correlate to periods of intensified volcanism. The Jenkyns Event occurred during the transition from a late Pliensbachian icehouse into… 

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