A forest fire and soil erosion event during the Late Devonian mass extinction

The Late Devonian mass extinction occurred in a stepwise manner and culminated close to the Frasnian–Famennian (F–F) boundary (372million years ago). Organic-molecular indices from marine sedimentary rocks at the Sinsin section, Belgium, indicate that the sequence of combustion of land vegetation, s...

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Veröffentlicht in:	Palaeogeography, palaeoclimatology, palaeoecology palaeoclimatology, palaeoecology, 2013-12, Vol.392, p.272-280
Hauptverfasser:	Kaiho, Kunio, Yatsu, Susumu, Oba, Masahiro, Gorjan, Paul, Casier, Jean-Georges, Ikeda, Masayuki
Format:	Artikel
Sprache:	eng
Schlagworte:	Atmospheric oxygen Combustion Devonian Mass extinction Soil erosion
Online-Zugang:	Volltext
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