Climatic and palaeoceanographic changes during the Pliensbachian (Early Jurassic) inferred from clay mineralogy and stable isotope (C-O) geochemistry (NW Europe)

The Early Jurassic was broadly a greenhouse climate period that was punctuated by short warm and cold climatic events, positive and negative excursions of carbon isotopes, and episodes of enhanced organic matter burial. Clay minerals from Pliensbachian sediments recovered from two boreholes in the P...

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Veröffentlicht in:	Global and planetary change 2017-02, Vol.149, p.139-152
Hauptverfasser:	Bougeault, Cédric, Pellenard, Pierre, Deconinck, Jean-François, Hesselbo, Stephen P., Dommergues, Jean-Louis, Bruneau, Ludovic, Cocquerez, Théophile, Laffont, Rémi, Huret, Emilia, Thibault, Nicolas
Format:	Artikel
Sprache:	eng
Schlagworte:	Clay minerals Climatology Early Jurassic Earth Sciences Geochemistry Glacio-eustasy Mineralogy Pliensbachian Runoff Sciences of the Universe Stable isotope Stratigraphy
Online-Zugang:	Volltext
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