0000000000363111

AUTHOR

Richard Hofmann

showing 2 related works from this author

Microbial deposits in the aftermath of the end-Permian mass extinction: A diverging case from the Mineral Mountains (Utah, USA)

2015

40 pages; International audience; The Lower Triassic Mineral Mountains area (Utah, USA) preserves diversified Smithian and Spathian reefs and bioaccumulations that contain fenestral-microbialites and various benthic and pelagic organisms. Ecological and environmental changes during the Early Triassic are commonly assumed to be associated with numerous perturbations (productivity changes, acidifica-tion, redox changes, hypercapnia, eustatism and temperature changes) post-dating the Permian–Triassic mass extinction. New data acquired in the Mineral Mountains sediments provide evidence to decipher the relationships between depositional environments and the growth and distribution of microbial …

Microbially induced sedimentary structurereef evolutionStratigraphyEarly Triassic10125 Paleontological Institute and Museum[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphySedimentary depositional environmentDepositional environmentsPaleontologyUtah14. Life underwaterReef1907 GeologyPermian–Triassic extinction event[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyOncoliteExtinction eventRed bedsgeographySpathiangeography.geographical_feature_categoryEarly Triassic recoverySmithianmicrobialitesGeology[ SDU.STU ] Sciences of the Universe [physics]/Earth Sciences15. Life on land560 Fossils & prehistoric life[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy1913 Stratigraphy[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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Transient metazoan reefs in the aftermath of the end-Permian mass extinction

2011

5 pages; International audience; Recovery from the devastating Permian-Triassic mass extinction about 252 million years ago is usually assumed to have spanned the entire 5 million years of the Early Triassic epoch1,2. The post-crisis interval was characterized by large-scale fluctuations of the global carbon cycle and harsh marine conditions, including a combination of ocean acidification, euxinia, and fluctuating productivity3. During this interval, metazoan-dominated reefs are thought to have been replaced by microbial deposits that are considered the hallmark of the Early Triassic4-7. Here we use field and microscopic investigations to document Early Triassic bioaccumulations and reefs f…

010506 paleontologyEarly Triassic10125 Paleontological Institute and Museum[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesCarbon cyclePaleontology14. Life underwaterReefPermian–Triassic extinction event[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesExtinction eventgeographygeography.geographical_feature_categoryExtinction1900 General Earth and Planetary SciencesfungiOcean acidificationsocial scienceshumanitiesOceanography560 Fossils & prehistoric life13. Climate actionBenthic zone[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyGeneral Earth and Planetary Sciences[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontologygeographic locationsGeologyNature Geoscience
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