about
Global patterns of insect diversification: towards a reconciliation of fossil and molecular evidence?Canopy flow analysis reveals the advantage of size in the oldest communities of multicellular eukaryotesEnvironmental and biotic controls on the evolutionary history of insect body sizeProlonged Permian Triassic ecological crisis recorded by molluscan dominance in Late Permian offshore assemblagesPhanerozoic trends in the global diversity of marine invertebrates.Organism activity levels predict marine invertebrate survival during ancient global change extinctions.Ancient origin of high taxonomic richness among insects.Multiple episodes of extensive marine anoxia linked to global warming and continental weathering following the latest Permian mass extinction.Acidification, anoxia, and extinction: A multiple logistic regression analysis of extinction selectivity during the Middle and Late PermianEnd-Permian Mass Extinction in the Oceans: An Ancient Analog for the Twenty-First Century?Arthropods in modern resins reveal if amber accurately recorded forest arthropod communitiesA new ecological-severity ranking of major Phanerozoic biodiversity crisesFaunal evidence for a cool boundary current and decoupled regional climate cooling in the Permian of western LaurentiaExtinction selectivity among marine fishes during multistressor global change in the end-Permian and end-Triassic crisesComparative size evolution of marine clades from the Late Permian through Middle TriassicPaleoecology and geochemistry of Early Triassic (Spathian) microbial mounds and implications for anoxia following the end-Permian mass extinctionIDENTIFYING THE TICKS OF BIVALVE SHELL CLOCKS: SEASONAL GROWTH IN RELATION TO TEMPERATURE AND FOOD SUPPLYEcological consequences of the Guadalupian extinction and its role in the brachiopod-mollusk transitionTaphonomic biases in the insect fossil record: shifts in articulation over geologic timePopulation structure of the oldest known macroscopic communities from Mistaken Point, NewfoundlandExtinction: End-Permian Mass ExtinctionPaleoecology of brachiopod communities during the late Paleozoic ice age in Bolivia (Copacabana Formation, Pennsylvanian–Early Permian)Taxonomic composition and environmental distribution of post-extinction rhynchonelliform brachiopod faunas: Constraints on short-term survival and the role of anoxia in the end-Permian mass extinctionOrdination Methods and the Evaluation of Ediacaran CommunitiesThe double mass extinction revisited: reassessing the severity, selectivity, and causes of the end-Guadalupian biotic crisis (Late Permian)WUCHIAPINGIAN (LOPINGIAN, LATE PERMIAN) BRACHIOPODS FROM THE EPISKOPI FORMATION OF HYDRA ISLAND, GREECEUnderstanding mechanisms for the end-Permian mass extinction and the protracted Early Triassic aftermath and recoveryPermian marine paleoecology and its implications for large-scale decoupling of brachiopod and bivalve abundance and diversity during the Lopingian (Late Permian)Evolutionary Paleoecology of Ediacaran Benthic Marine AnimalsDeep valley incision in the terminal Neoproterozoic (Ediacaran) Johnnie Formation, eastern California, USA: Tectonically or glacially driven?Paleoenvironmental analysis of the late Neoproterozoic Mistaken Point and Trepassey formations, southeastern NewfoundlandLessons from the fossil record: the Ediacaran radiation, the Cambrian radiation, and the end-Permian mass extinctionThe spatial structure of Phanerozoic marine animal diversity
P50
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P50
description
Canadian paleoecologist
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paleontoloog
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name
Matthew E. Clapham
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Matthew E. Clapham
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Matthew E. Clapham
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Matthew E. Clapham
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Matthew E. Clapham
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Matthew E. Clapham
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Matthew E. Clapham
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Matthew E. Clapham
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Matthew E. Clapham
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Matthew E. Clapham
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Matthew E. Clapham
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Matthew E. Clapham
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Matthew E. Clapham
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Matthew E. Clapham
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Matthew E. Clapham
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P106
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P27
P31
P496
0000-0003-4867-7304