Evidence map›Paper›PMID 28246643›Full record

ArticleScience advances2017

Unexpected Early Triassic marine ecosystem and the rise of the Modern evolutionary fauna.

Arnaud Brayard, L J Krumenacker, Joseph P Botting, James F Jenks, Kevin G Bylund, Emmanuel Fara, Emmanuelle Vennin, Nicolas Olivier, Nicolas Goudemand, Thomas Saucède and 8 more

Abstract read
In one paragraph

Article in Science advances, 2017. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 27 papers.

0numbers the graph read from it
0cells of the map it votes in
27citing papers in PubMed
–field-weighted citation impact
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

27 citing papers in PubMed.

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  5. Geochronology of the Early Triassic based on coupled Bayesian zircon eruption age and Bayesian age-depth models.Proceedings of the National Academy of Sciences of the United States of America · 2025
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  14. Swiss ichthyosaurs: a review.Swiss journal of palaeontology · 2024
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4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

18 authors.

Arnaud BrayardBiogéosciences UMR 6282, CNRS, Université Bourgogne Franche-Comté, 6 Boulevard Gabriel, 21000 Dijon, France.ORCID 0000-0003-1304-6553
L J KrumenackerDepartment of Earth Sciences, Montana State University, P.O. Box 173480, Bozeman, MT 59717-3480, USA.ORCID 0000-0002-5990-3349
Joseph P BottingNanjing Institute of Geology and Palaeontology, 39 East Beijing Road, Nanjing 210008, China.; Department of Geology, National Museum of Wales, Cathays Park, Cardiff CF10 3NP, U.K.
James F Jenks1134 Johnson Ridge Lane, West Jordan, UT 84084, USA.
Kevin G Bylund140 South 700 East, Spanish Fork, UT 84660, USA.
Emmanuel FaraBiogéosciences UMR 6282, CNRS, Université Bourgogne Franche-Comté, 6 Boulevard Gabriel, 21000 Dijon, France.
Emmanuelle VenninBiogéosciences UMR 6282, CNRS, Université Bourgogne Franche-Comté, 6 Boulevard Gabriel, 21000 Dijon, France.ORCID 0000-0002-5899-0399
Nicolas OlivierUniversité Clermont Auvergne, CNRS, IRD, Observatoire de Physique du Globe de Clermont-Ferrand, Laboratoire Magmas et Volcans, 5 rue Kessler, F-63000 Clermont-Ferrand, France.
Nicolas GoudemandInstitute of Functional Genomics of Lyon, École Normale Supérieure de Lyon-CNRS 5242-Institut National de la Recherche Agronomique Unités Sous Contrat INRA USC 1370, 46 allée d'Italie, 69364 Lyon Cedex 07, France.
Thomas SaucèdeBiogéosciences UMR 6282, CNRS, Université Bourgogne Franche-Comté, 6 Boulevard Gabriel, 21000 Dijon, France.
Sylvain CharbonnierMuséum national d'Histoire naturelle (MNHN), Centre de Recherche sur la Paléobiodiversité et les Paléoenvironnements (UMR 7207), Sorbonne Universités-MNHN, CNRS, Université Pierre et Marie Curie, 57 rue Cuvier, 75005 Paris, France.ORCID 0000-0002-9496-3849
Carlo RomanoPaläontologisches Institut und Museum, Universität Zürich, 8006 Zürich, Switzerland.ORCID 0000-0003-4438-2736
Larisa DoguzhaevaDepartment of Palaeobiology, Swedish Museum of Natural History, P.O. Box 50007, SE-10405 Stockholm, Sweden.ORCID 0000-0002-1231-2488
Ben ThuyDepartment of Palaeontology, Natural History Museum Luxembourg, 25 rue Münster, L-2160 Luxembourg, Luxembourg.
Michael HautmannPaläontologisches Institut und Museum, Universität Zürich, 8006 Zürich, Switzerland.ORCID 0000-0002-7322-8749
Daniel A StephenDepartment of Earth Science, Utah Valley University, 800 West University Parkway, Orem, UT 84058, USA.
Christophe ThomazoBiogéosciences UMR 6282, CNRS, Université Bourgogne Franche-Comté, 6 Boulevard Gabriel, 21000 Dijon, France.
Gilles EscarguelUniv Lyon, Université Claude Bernard Lyon 1, CNRS, ENTPE, UMR 5023 Laboratoire d'Ecologie des Hydrosystèmes Naturels et Anthropisés, 27-43 Boulevard du 11 novembre 1918, 69622 Villeurbanne Cedex, France.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

In the wake of the end-Permian mass extinction, the Early Triassic (~251.9 to 247 million years ago) is portrayed as an environmentally unstable interval characterized by several biotic crises and heavily depauperate marine benthic ecosystems. We describe a new fossil assemblage-the Paris Biota-from the earliest Spathian (middle Olenekian, ~250.6 million years ago) of the Bear Lake area, southeastern Idaho, USA. This highly diversified assemblage documents a remarkably complex marine ecosystem including at least seven phyla and 20 distinct metazoan orders, along with algae. Most unexpectedly, it combines early Paleozoic and middle Mesozoic taxa previously unknown from the Triassic strata, among which are primitive Cambrian-Ordovician leptomitid sponges (a 200-million year Lazarus taxon) and gladius-bearing coleoid cephalopods, a poorly documented group before the Jurassic (~50 million years after the Early Triassic). Additionally, the crinoid and ophiuroid specimens show derived anatomical characters that were thought to have evolved much later. Unlike previous works that suggested a sluggish postcrisis recovery and a low diversity for the Early Triassic benthic organisms, the unexpected composition of this exceptional assemblage points toward an early and rapid post-Permian diversification for these clades. Overall, it illustrates a phylogenetically diverse, functionally complex, and trophically multileveled marine ecosystem, from primary producers up to top predators and potential scavengers. Hence, the Paris Biota highlights the key evolutionary position of Early Triassic fossil ecosystems in the transition from the Paleozoic to the Modern marine evolutionary fauna at the dawn of the Mesozoic era.

Indexed as

Biological EvolutionEcosystemFossilsPhylogenyAnimalsAquatic Organismsbiotic recoveryEarly TriassicEnd-Permian mass extinctionIdahomarine ecosystemsParis Biota

Identifiers

PMID28246643
PMCPMC5310825

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Registered trials

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Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.