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- W2003036006 endingPage "160" @default.
- W2003036006 startingPage "148" @default.
- W2003036006 abstract "Fossil charcoal has widely been accepted as a direct indicator for the occurrence of palaeo-wildfires. In Upper Palaeozoic sediments of Euramerica and Cathaysia, records of these remains are relatively common and (regionally and stratigraphically) more or less homogeneously distributed in terrestrial sequences. On the other hand, just a few records have been published for the Permian of Gondwana and only recently has it been demonstrated that macroscopic charcoals are also common here. Most Permian macroscopic charcoal from Gondwana is gymnospermous and has been reported from coal-bearing strata. Macroscopic charcoal occurrences are spread out in different sequences and also in distinct stratigraphic intervals in the Permian [e.g., Paraná Basin (Sakmarian/Artinskian of Brazil), Karoo Basin (Artinskian of South Africa), Damodar Basin (Lopingian of India) and Dead Sea area (Changhsingian of Jordan)]. They range from peri-glacial/post-glacial to warm temperate climatic systems throughout the Permian. Macro- and micro-charcoal occurrences are compared to inertinite incidences to support the pyrogenic origin for these coal macerals and to provide an up to date overview on the known evidences of Permian wildfires on Gondwana in space and time." @default.
- W2003036006 created "2016-06-24" @default.
- W2003036006 creator A5006886494 @default.
- W2003036006 creator A5018428863 @default.
- W2003036006 creator A5030507107 @default.
- W2003036006 creator A5060575343 @default.
- W2003036006 creator A5066010886 @default.
- W2003036006 creator A5077216435 @default.
- W2003036006 creator A5082465060 @default.
- W2003036006 date "2013-07-01" @default.
- W2003036006 modified "2023-10-18" @default.
- W2003036006 title "The burning of Gondwana: Permian fires on the southern continent—A palaeobotanical approach" @default.
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