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(1996) Climate change, plant extinctions and vegetational recovery during the Middle-Late Pennsylvanian Transition: the Case of tropical peat-forming environments in North America, in Biotic Recovery from Mass Extinction Events. Special Publication, 102. Geological Society of London. 201-221 doi:10.1144/gsl.sp.1996.001.01.14

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Reference TypeReport (article/chapter)
TitleClimate change, plant extinctions and vegetational recovery during the Middle-Late Pennsylvanian Transition: the Case of tropical peat-forming environments in North America
ReportSpecial Publication
Year1996Volume102
PublisherGeological Society of London
DOIdoi:10.1144/gsl.sp.1996.001.01.14Search in ResearchGate
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Mindat Ref. ID427689Long-form Identifiermindat:1:5:427689:4
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Full Reference(1996) Climate change, plant extinctions and vegetational recovery during the Middle-Late Pennsylvanian Transition: the Case of tropical peat-forming environments in North America, in Biotic Recovery from Mass Extinction Events. Special Publication, 102. Geological Society of London. 201-221 doi:10.1144/gsl.sp.1996.001.01.14
Plain Text(1996) Climate change, plant extinctions and vegetational recovery during the Middle-Late Pennsylvanian Transition: the Case of tropical peat-forming environments in North America, in Biotic Recovery from Mass Extinction Events. Special Publication, 102. Geological Society of London. 201-221 doi:10.1144/gsl.sp.1996.001.01.14
In(1996) Biotic Recovery from Mass Extinction Events. Special Publication Vol. 102. Geological Society of London

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(1996) Recovery of North Caucasus foraminiferal assemblages after the pre-Danian extinctions, in Biotic Recovery from Mass Extinction Events. Special Publication, 102. Geological Society of London. 337-342 doi:10.1144/gsl.sp.1996.001.01.25
(1996) Recovery of post—Late Ordovician extinction graptolites: a western North American perspective, in Biotic Recovery from Mass Extinction Events. Special Publication, 102. Geological Society of London. 119-126 doi:10.1144/gsl.sp.1996.001.01.09
(1996) Biotic recovery after mass extinction: the role of climate and ocean-state in the post-glacial (Late Ordovician-Early Silurian) recovery of the conodonts, in Biotic Recovery from Mass Extinction Events. Special Publication, 102. Geological Society of London. 105-117 doi:10.1144/gsl.sp.1996.001.01.08
(1996) Ostracode speciation following Middle Ordovician extinction events, north central United States, in Biotic Recovery from Mass Extinction Events. Special Publication, 102. Geological Society of London. 97-104 doi:10.1144/gsl.sp.1996.001.01.07
(1996) Recovery of the food chain after the Late Cenomanian extinction event, in Biotic Recovery from Mass Extinction Events. Special Publication, 102. Geological Society of London. 265-277 doi:10.1144/gsl.sp.1996.001.01.20
(1996) The importance of crisis progenitors in recovery from mass extinction, in Biotic Recovery from Mass Extinction Events. Special Publication, 102. Geological Society of London. 15-39 doi:10.1144/gsl.sp.1996.001.01.02
(1996) Recovery of the marine fauna in Europe after the end-Triassic and Early Toarcian mass Extinctions, in Biotic Recovery from Mass Extinction Events. Special Publication, 102. Geological Society of London. 231-236 doi:10.1144/gsl.sp.1996.001.01.16
(1996) Reef ecosytem recovery after the Early Cambrian extinction, in Biotic Recovery from Mass Extinction Events. Special Publication, 102. Geological Society of London. 79-96 doi:10.1144/gsl.sp.1996.001.01.06
(1996) The mid-Carboniferous rugose coral recovery, in Biotic Recovery from Mass Extinction Events. Special Publication, 102. Geological Society of London. 187-199 doi:10.1144/gsl.sp.1996.001.01.13
(1996) Models for biotic survival following mass extinction, in Biotic Recovery from Mass Extinction Events. Special Publication, 102. Geological Society of London. 41-60 doi:10.1144/gsl.sp.1996.001.01.03
(1996) Recovery of the naticid gastropod predator-prey system from the Cretaceous-Tertiary and Eocene-Oligocene extinctions, in Biotic Recovery from Mass Extinction Events. Special Publication, 102. Geological Society of London. 373-386 doi:10.1144/gsl.sp.1996.001.01.27
 
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