Evidence map›Paper›PMID 37463883›Full record

ArticleNature communications2023

Sulfate triple-oxygen-isotope evidence confirming oceanic oxygenation 570 million years ago.

Haiyang Wang, Yongbo Peng, Chao Li, Xiaobin Cao, Meng Cheng, Huiming Bao

Open access · goldAbstract read
In one paragraph

Article in Nature communications, 2023. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 3 papers.

0numbers the graph read from it
0cells of the map it votes in
3citing papers in PubMed
26.6field-weighted citation impact, top 1% of its field
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

3 citing papers in PubMed, 33 citations in OpenAlex.

  1. Review
  2. Article
  3. Review
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

6 authors at 4 institutions in 2 countries.

Haiyang WangInternational Center for Isotope Effects Research, Nanjing University, Nanjing, China.ORCID http://orcid.org/0009-0006-5786-4397
Yongbo PengInternational Center for Isotope Effects Research, Nanjing University, Nanjing, China. ybpeng@nju.edu.cn.ORCID http://orcid.org/0000-0001-6458-5552
Chao LiState Key Laboratory of Oil and Gas Reservoir Geology and Exploitation & Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, China. chaoli@cdut.edu.cn.ORCID http://orcid.org/0000-0001-9861-661X
Xiaobin CaoInternational Center for Isotope Effects Research, Nanjing University, Nanjing, China.
Meng ChengState Key Laboratory of Oil and Gas Reservoir Geology and Exploitation & Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, China.
Huiming BaoInternational Center for Isotope Effects Research, Nanjing University, Nanjing, China. bao@nju.edu.cn.ORCID http://orcid.org/0000-0002-1979-4395
Chengdu University of Technology · CNNanjing University · CNInternational Isotopes (United States) · USMinistry of Natural Resources · CN

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The largest negative inorganic carbon isotope excursion in Earth's history, namely the Ediacaran Shuram Excursion (SE), closely followed by early animal radiation, has been widely interpreted as a consequence of oceanic oxidation. However, the primary nature of the signature, source of oxidants, and tempo of the event remain contested. Here, we show that carbonate-associated sulfate (CAS) from three different paleocontinents all have conspicuous negative

Identifiers

PMID37463883
PMCPMC10354052
OpenAlexW4384662491

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.