2020
DOI: 10.1016/j.epsl.2019.115875
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End-Permian (252 Mya) deforestation, wildfires and flooding—An ancient biotic crisis with lessons for the present

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Cited by 130 publications
(119 citation statements)
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“…This floral change is observed in many areas of Gondwana and was, until recently, interpreted as the terrestrial equivalent of the marine end-Permian biotic crisis 37,38 . More recent discoveries from the Sydney Basin in Australia, however, showed that the collapse of glossopterid dominated forests occurred about 370k years prior to the marine event 6 , although we note the presence there of a long diastem between the last Permian taxa characteristic of the Glossopteris flora and the first post-extinction pollen record 39,40 .…”
Section: Resultscontrasting
confidence: 59%
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“…This floral change is observed in many areas of Gondwana and was, until recently, interpreted as the terrestrial equivalent of the marine end-Permian biotic crisis 37,38 . More recent discoveries from the Sydney Basin in Australia, however, showed that the collapse of glossopterid dominated forests occurred about 370k years prior to the marine event 6 , although we note the presence there of a long diastem between the last Permian taxa characteristic of the Glossopteris flora and the first post-extinction pollen record 39,40 .…”
Section: Resultscontrasting
confidence: 59%
“…Hg and TOC values are the average of triplicate analyses of each horizon sampled. Palynological zone assignments, correlated with Australia 39,40 , appear against recovered pollen-and-spore assemblages. See supplemental information for legend.…”
Section: Resultsmentioning
confidence: 94%
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“…Stephen is currently Professor and Senior Curator at the Swedish Museum of Natural History in Stockholm, and is recognized internationally for his ground breaking work on Gondwanan Paleozoic and Mesozoic floras, and especially those from the Australasian region. Recently, Stephen and colleagues published a highly detailed investigation of the dramatic floral turnover across the Permian-Triassic boundary (251.9 million years ago), which is marked at southern palaeolatitudes by the extinction of Glossopteridales-iconic Gondwanan arborescent plants ubiquitous in Late Permian peat-forming forests (Vajda et al 2020).…”
mentioning
confidence: 99%