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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
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cryosphere
TRANSIENT ELECTROMAGNETIC MONITORING OF THE CRYOLITHOZONE: MATHEMATICAL MODELING
Glacial isostatic adjustment driven by asymmetric ice sheet melt during the Last Interglacial causes multiple local sea-level peaks
Late Cretaceous glaciations in a hyper-arid plateau desert of the South China Coastal Mountains
Seismic discontinuity in the Martian crust possibly caused by water-filled cracks
Application of the 187 Re- 187 Os geochronometer to crustal materials: Systematics, methodology, data reporting, and interpretation
The Chemistry of Cave Ice: Two Examples from Slovenia
Ice-rafted dropstones at midlatitudes in the Cretaceous of continental Iberia
Eocene–Oligocene glaciation on a high central Tibetan Plateau
Drone applications in hydrogeophysics: Recent examples and a vision for the future
Identifying relict periglacial features in watershed landscape and deposits of Borisoglebsk Upland, Central European Russia
Impact of a northern-hemispherical cryosphere on late Pliensbachian–early Toarcian climate and environment evolution
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 an early Toarcian greenhouse. Parallel evolution of different environmental processes, including sea level, climate and carbon cycle, indicate a causal mechanism tied to astronomical forcing. Insolation-controlled variations in the extent of the cryosphere (ice caps and permafrost) facilitated orbitally paced sea-level cycles via waxing and waning of the polar ice caps, and negative carbon isotope excursions via the release of cryosphere-bound 12 C-enriched carbon. This review and synthesis of sedimentological, geochemical and palaeontological palaeoenvironment indicators, and of simulations from climate models, aims to reconstruction, in particular, the high-latitudinal environmental conditions of late Pliensbachian–early Toarcian times. Focus is laid on the extent of the regions that were potentially suitable for hosting a cryosphere. An environmental response to cryosphere dynamics is considered to have been a key component of the Jenkyns Event.