Evidence map›Paper›PMID 38678037›Full record

ArticleNature communications2024

Climate-forced Hg-remobilization associated with fern mutagenesis in the aftermath of the end-Triassic extinction.

Remco Bos, Wang Zheng, Sofie Lindström, Hamed Sanei, Irene Waajen, Isabel M Fendley, Tamsin A Mather, Yang Wang, Jan Rohovec, Tomáš Navrátil and 2 more

Abstract read
PubMed Full text at PMC Publisher
In one paragraph

Article in Nature communications, 2024. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

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

0 citing papers in PubMed.

No citing paper in PubMed yet.

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

12 authors.

Remco BosDepartment of Earth Sciences, Faculty of Geosciences, Utrecht University, Princetonlaan 8, 3584, CB, Utrecht, The Netherlands. r.bos@uu.nl.ORCID http://orcid.org/0000-0002-3664-3265
Wang ZhengInstitute of Surface-Earth System Science, School of Earth System Science, Tianjin University, 300072, Tianjin, China. zhengw3@tju.edu.cn.ORCID http://orcid.org/0000-0002-3413-9700
Sofie LindströmDepartment of Geosciences and Natural Resource Management, Copenhagen University, Øster Voldgade 10, DK-1350, Copenhagen K, Denmark.ORCID http://orcid.org/0000-0001-8278-1055
Hamed SaneiLithospheric Organic Carbon (LOC) Group, Department of Geoscience, Aarhus University, Høegh-Guldbergs gade 2, 8000C, Aarhus, Denmark.ORCID http://orcid.org/0000-0002-2961-9654
Irene WaajenDepartment of Earth Sciences, Faculty of Geosciences, Utrecht University, Princetonlaan 8, 3584, CB, Utrecht, The Netherlands.ORCID http://orcid.org/0009-0006-1150-6746
Isabel M FendleyDepartment of Earth Sciences, University of Oxford, Parks Road, Oxford, OX1 3PR, UK.ORCID http://orcid.org/0000-0001-8142-6799
Tamsin A MatherDepartment of Earth Sciences, University of Oxford, Parks Road, Oxford, OX1 3PR, UK.ORCID http://orcid.org/0000-0003-4259-7303
Yang WangInstitute of Surface-Earth System Science, School of Earth System Science, Tianjin University, 300072, Tianjin, China.
Jan RohovecInstitute of Geology of the Czech Academy of Sciences, Rozvojová 269, Prague, 6 165 00, Czech Republic.
Tomáš NavrátilInstitute of Geology of the Czech Academy of Sciences, Rozvojová 269, Prague, 6 165 00, Czech Republic.ORCID http://orcid.org/0000-0002-6213-5336
Appy SluijsDepartment of Earth Sciences, Faculty of Geosciences, Utrecht University, Princetonlaan 8, 3584, CB, Utrecht, The Netherlands.ORCID http://orcid.org/0000-0003-2382-0215
Bas van de SchootbruggeDepartment of Earth Sciences, Faculty of Geosciences, Utrecht University, Princetonlaan 8, 3584, CB, Utrecht, The Netherlands.ORCID http://orcid.org/0000-0003-2270-6285

Funding

National Natural Science Foundation of China (National Science Foundation of China) grant No. 41973009Nederlandse Organisatie voor Wetenschappelijk Onderzoek (Netherlands Organisation for Scientific Research) NWO ALWOP.623
6 · The paper itself

Abstract

The long-term effects of the Central Atlantic Magmatic Province, a large igneous province connected to the end-Triassic mass-extinction (201.5 Ma), remain largely elusive. Here, we document the persistence of volcanic-induced mercury (Hg) pollution and its effects on the biosphere for ~1.3 million years after the extinction event. In sediments recovered in Germany (Schandelah-1 core), we record not only high abundances of malformed fern spores at the Triassic-Jurassic boundary, but also during the lower Jurassic Hettangian, indicating repeated vegetation disturbance and stress that was eccentricity-forced. Crucially, these abundances correspond to increases in sedimentary Hg-concentrations. Hg-isotope ratios (δ

Indexed as

Extinction, BiologicalFernsFossilsGeologic SedimentsMercuryClimateGermanyMutagenesisSporesVolcanic EruptionsMercury

Identifiers

PMID38678037
PMCPMC11519498

What OpenQuestion holds

Textmetadata
LicenceCC BY
Read underepoch 390

Registered trials

None linked

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.