Hugo Bucher focuses on Paleontology, Extinction event, Early Triassic, Ecology and Permian–Triassic extinction event. His work in Paleontology addresses issues such as Ecological succession, which are connected to fields such as Habitat. His Extinction event study is associated with Extinction.
His Early Triassic study combines topics from a wide range of disciplines, such as Volcanic ash, Carbon cycle, Mesozoic and Fauna. Hugo Bucher usually deals with Permian–Triassic extinction event and limits it to topics linked to Terrestrial ecosystem and Siberian Traps and Paleoclimatology. His Permian research is multidisciplinary, relying on both Total organic carbon, Paleozoic, Palynology, Biostratigraphy and Helminthopsis.
His main research concerns Paleontology, Early Triassic, Extinction event, Permian and Fauna. His Paleontology research includes elements of Ecology and Permian–Triassic extinction event. His work deals with themes such as Ammonoidea, Mesozoic and Genus, which intersect with Early Triassic.
The concepts of his Extinction event study are interwoven with issues in Oceanography, Benthic zone and Carbon cycle. His Permian research focuses on subjects like Palynology, which are linked to Climate change and Ecological succession. Hugo Bucher combines subjects such as Taxon, Taxonomy and Species richness with his study of Fauna.
His primary areas of study are Paleontology, Early Triassic, Permian, Extinction event and Conodont. His Paleontology research is multidisciplinary, incorporating elements of Fauna, Extinction and Isotopes of carbon. His Early Triassic research incorporates elements of Ecology, Benthic zone, Actinopterygii and Clastic rock.
His research integrates issues of Stratotype, Pollen, Zircon and Unconformity in his study of Permian. His Extinction event research integrates issues from Palynology, Biodiversity and Carbon cycle. Hugo Bucher has researched Conodont in several fields, including Nekton, Hindeodus and Stratigraphy.
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Smithian-Spathian boundary event: Evidence for global climatic change in the wake of the end-Permian biotic crisis
Thomas Galfetti;Peter A. Hochuli;Arnaud Brayard;Hugo Bucher.
Good genes and good luck: Ammonoid diversity and the end-permian mass extinction
Arnaud Brayard;Gilles Escarguel;Hugo Bucher;Claude Monnet.
Timing of the Early Triassic carbon cycle perturbations inferred from new U–Pb ages and ammonoid biochronozones.
Thomas Galfetti;Hugo Bucher;Maria Ovtcharova;Urs Schaltegger.
Earth and Planetary Science Letters (2007)
New Early to Middle Triassic U–Pb ages from South China: Calibration with ammonoid biochronozones and implications for the timing of the Triassic biotic recovery
Maria Ovtcharova;Hugo Bucher;Urs Schaltegger;Thomas Galfetti.
Earth and Planetary Science Letters (2006)
The Early Triassic ammonoid recovery: Paleoclimatic significance of diversity gradients
Arnaud Brayard;Arnaud Brayard;Hugo Bucher;Gilles Escarguel;Frédéric Fluteau.
Palaeogeography, Palaeoclimatology, Palaeoecology (2006)
Climatic and biotic upheavals following the end-Permian mass extinction
Carlo Romano;Nicolas Goudemand;Torsten W. Vennemann;David Ware.
Nature Geoscience (2013)
Mode and Rate of Growth in Ammonoids
Hugo Bucher;Neil H. Landman;Susan M. Klofak;Jean Guex.
Late Early Triassic climate change: Insights from carbonate carbon isotopes, sedimentary evolution and ammonoid paleobiogeography.
Thomas Galfetti;Hugo Bucher;Arnaud Brayard;Arnaud Brayard;Peter A. Hochuli.
Palaeogeography, Palaeoclimatology, Palaeoecology (2007)
Mature Modifications and Dimorphism in Ammonoid Cephalopods
Richard Arnold Davis;Neil H. Landman;Jean-Louis Dommergues;Didier Marchand.
Transient metazoan reefs in the aftermath of the end-Permian mass extinction
Arnaud Brayard;Emmanuelle Vennin;Nicolas Olivier;Kevin G. Bylund.
Nature Geoscience (2011)
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