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Intensified continental chemical weathering and carbon-cycle perturbations linked to volcanism during the Triassic–Jurassic transition

Nature communications, 2022-01, Vol.13 (1), p.299-299, Article 299

2022

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Mercury anomalies and the timing of biotic recovery following the end-Triassic mass extinction

Nature communications, 2016-04, Vol.7 (1), p.11147-11147, Article 11147

2016

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Sponge grade body fossil with cellular resolution dating 60 Myr before the Cambrian

Proceedings of the National Academy of Sciences - PNAS, 2015-03, Vol.112 (12), p.E1453-E1460

2015

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The importance of oxygen for the disparate recovery patterns of the benthic macrofauna in the Early Triassic

Earth-science reviews, 2014-10, Vol.137, p.65-84

2014

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Complex marine bioturbation ecosystem engineering behaviors persisted in the wake of the end-Permian mass extinction

Scientific reports, 2020-01, Vol.10 (1), p.203-203, Article 203

2020

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Quantifying the effects of exceptional fossil preservation on the global availability of phylogenetic data in deep time

PloS one, 2024-02, Vol.19 (2), p.e0297637-e0297637

2024

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A new ecological-severity ranking of major Phanerozoic biodiversity crises

Palaeogeography, palaeoclimatology, palaeoecology, 2013-01, Vol.370, p.260-270

2013

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Sudden and extreme hyperthermals, low-oxygen, and sediment influx drove community phase shifts following the end-Permian mass extinction

Palaeogeography, palaeoclimatology, palaeoecology, 2016-06, Vol.451, p.183-196

2016

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Reconstruction of Early Triassic ocean redox conditions based on framboidal pyrite from the Nanpanjiang Basin, South China

Palaeogeography, palaeoclimatology, palaeoecology, 2014-10, Vol.412, p.68-79

2014

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Ecological ranking of Phanerozoic biodiversity crises: The Serpukhovian (early Carboniferous) crisis had a greater ecological impact than the end-Ordovician

Geology (Boulder), 2012-02, Vol.40 (2), p.147-150

2012

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Origin of Lower Triassic microbialites in mixed carbonate-siliciclastic successions: Ichnology, applied stratigraphy, and the end-Permian mass extinction

Palaeogeography, palaeoclimatology, palaeoecology, 2011-02, Vol.300 (1-4), p.158-178

2011

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Dental replacement in Mesozoic birds: evidence from newly discovered Brazilian enantiornithines

Scientific reports, 2021-09, Vol.11 (1), p.19349-19349, Article 19349

2021

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The double mass extinction revisited: reassessing the severity, selectivity, and causes of the end-Guadalupian biotic crisis (Late Permian)

Paleobiology, 2009-01, Vol.35 (1), p.32-50

2009

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Uppermost Triassic phosphorites from Williston Lake, Canada: link to fluctuating euxinic-anoxic conditions in northeastern Panthalassa before the end-Triassic mass extinction

Scientific reports, 2019-12, Vol.9 (1), p.18790-9, Article 18790

2019

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Additional records of ichnogenus Rhizocorallium from the Lower and Middle Triassic, South China: Implications for biotic recovery after the end-Permian mass extinction

Geological Society of America bulletin, 2018-07, Vol.130 (7-8), p.1197-1215

2018

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Paleoecology: past, present, and future

Bottjer, David J

1, 2016

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Paleogeographic trends in Late Triassic reef ecology from northeastern Panthalassa

Earth-science reviews, 2015-03, Vol.142, p.18-37

2015

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Andean sponges reveal long-term benthic ecosystem shifts following the end-Triassic mass extinction

Palaeogeography, palaeoclimatology, palaeoecology, 2015-02, Vol.420, p.193-209

2015

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Paleogenomics of echinoids reveals an ancient origin for the double-negative specification of micromeres in sea urchins

Proceedings of the National Academy of Sciences - PNAS, 2017-06, Vol.114 (23), p.5870-5877

2017

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Westermann Morphospace displays ammonoid shell shape and hypothetical paleoecology

Paleobiology, 2012-06, Vol.38 (3), p.424-446

2012

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Reorganization of sea urchin gene regulatory networks at least 268 million years ago as revealed by oldest fossil cidaroid echinoid

Scientific reports, 2015-10, Vol.5 (1), p.15541-15541, Article 15541

2015

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A global marine sedimentary response to the end-Permian mass extinction: Examples from southern Turkey and the western United States

Earth-science reviews, 2006-10, Vol.78 (3), p.193-206

2006

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Diversity and species abundance patterns of the Early Cambrian (Series 2, Stage 3) Chengjiang Biota from China

Paleobiology, 2014-01, Vol.40 (1), p.50-69

2014

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Proliferation of Early Triassic wrinkle structures: Implications for environmental stress following the end-Permian mass extinction

Geology (Boulder), 2004-05, Vol.32 (5), p.461

2004

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Analysis of ancient mass extinction recoveries in marine environments: generating strategies for managing outcomes of the current mass extinction

National science review, 2024-01, Vol.11 (1), p.nwad240-nwad240

Bottjer, David J

2024

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Intensified continental chemical weathering and carbon-cycle perturbations linked to volcanism during the Triassic–Jurassic transition

Mercury anomalies and the timing of biotic recovery following the end-Triassic mass extinction

Sponge grade body fossil with cellular resolution dating 60 Myr before the Cambrian

The importance of oxygen for the disparate recovery patterns of the benthic macrofauna in the Early Triassic

Complex marine bioturbation ecosystem engineering behaviors persisted in the wake of the end-Permian mass extinction

Quantifying the effects of exceptional fossil preservation on the global availability of phylogenetic data in deep time

A new ecological-severity ranking of major Phanerozoic biodiversity crises

Sudden and extreme hyperthermals, low-oxygen, and sediment influx drove community phase shifts following the end-Permian mass extinction

Reconstruction of Early Triassic ocean redox conditions based on framboidal pyrite from the Nanpanjiang Basin, South China

Ecological ranking of Phanerozoic biodiversity crises: The Serpukhovian (early Carboniferous) crisis had a greater ecological impact than the end-Ordovician

Origin of Lower Triassic microbialites in mixed carbonate-siliciclastic successions: Ichnology, applied stratigraphy, and the end-Permian mass extinction

Dental replacement in Mesozoic birds: evidence from newly discovered Brazilian enantiornithines

The double mass extinction revisited: reassessing the severity, selectivity, and causes of the end-Guadalupian biotic crisis (Late Permian)

Uppermost Triassic phosphorites from Williston Lake, Canada: link to fluctuating euxinic-anoxic conditions in northeastern Panthalassa before the end-Triassic mass extinction

Additional records of ichnogenus Rhizocorallium from the Lower and Middle Triassic, South China: Implications for biotic recovery after the end-Permian mass extinction

Paleoecology: past, present, and future

Paleogeographic trends in Late Triassic reef ecology from northeastern Panthalassa

Andean sponges reveal long-term benthic ecosystem shifts following the end-Triassic mass extinction

Paleogenomics of echinoids reveals an ancient origin for the double-negative specification of micromeres in sea urchins

Westermann Morphospace displays ammonoid shell shape and hypothetical paleoecology

Reorganization of sea urchin gene regulatory networks at least 268 million years ago as revealed by oldest fossil cidaroid echinoid

A global marine sedimentary response to the end-Permian mass extinction: Examples from southern Turkey and the western United States

Diversity and species abundance patterns of the Early Cambrian (Series 2, Stage 3) Chengjiang Biota from China

Proliferation of Early Triassic wrinkle structures: Implications for environmental stress following the end-Permian mass extinction

Analysis of ancient mass extinction recoveries in marine environments: generating strategies for managing outcomes of the current mass extinction

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