Evidence map›Paper›PMID 35767613›Full record

ArticleScience advances2022

Resilience of infaunal ecosystems during the Early Triassic greenhouse Earth.

Xueqian Feng, Zhong-Qiang Chen, Michael J Benton, Chunmei Su, David J Bottjer, Alison T Cribb, Ziheng Li, Laishi Zhao, Guangyou Zhu, Yuangeng Huang and 1 more

Abstract read
In one paragraph

Article in Science advances, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 6 papers.

0numbers the graph read from it
0cells of the map it votes in
6citing 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

6 citing papers in PubMed.

  1. Article
  2. 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
    Article
  3. Article
  4. Article
  5. Article
  6. Article
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

11 authors.

Xueqian FengState Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China.ORCID 0000-0002-3765-9824
Zhong-Qiang ChenState Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China.ORCID 0000-0001-5341-6913
Michael J BentonSchool of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK.ORCID 0000-0002-4323-1824
Chunmei SuState Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China.
David J BottjerDepartment of Earth Sciences, University of Southern California, Los Angeles, CA 90089, USA.
Alison T CribbDepartment of Earth Sciences, University of Southern California, Los Angeles, CA 90089, USA.ORCID 0000-0002-8604-6100
Ziheng LiState Key Laboratory of Geological Process and Mineral Resources, China University of Geosciences, Wuhan 430074, China.
Laishi ZhaoState Key Laboratory of Geological Process and Mineral Resources, China University of Geosciences, Wuhan 430074, China.
Guangyou ZhuResearch Institute of Petroleum Exploration and Development, PetroChina, Beijing 100083, China.
Yuangeng HuangState Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China.ORCID 0000-0002-2900-3331
Zhen GuoState Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The Permian-Triassic mass extinction severely depleted biodiversity, primarily observed in the body fossil of well-skeletonized animals. Understanding how whole ecosystems were affected and rebuilt following the crisis requires evidence from both skeletonized and soft-bodied animals; the best comprehensive information on soft-bodied animals comes from ichnofossils. We analyzed abundant trace fossils from 26 sections across the Permian-Triassic boundary in China and report key metrics of ichnodiversity, ichnodisparity, ecospace utilization, and ecosystem engineering. We find that infaunal ecologic structure was well established in the early Smithian. Decoupling of diversity between deposit feeders and suspension feeders in carbonate ramp-platform settings implies that an effect of trophic group amensalism could have delayed the recovery of nonmotile, suspension-feeding epifauna in the Early Triassic. This differential reaction of infaunal ecosystems to variable environmental controls thus played a substantial but heretofore little appreciated evolutionary and ecologic role in the overall recovery in the hot Early Triassic ocean.

Identifiers

PMID35767613
PMCPMC9242451

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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.