Evidence map›Paper›PMID 39427002›Full record

ArticleNature communications2024

Expanded subsurface ocean anoxia in the Atlantic during the Paleocene-Eocene Thermal Maximum.

Weiqi Yao, Tianshu Kong, Xingchen Tony Wang, Ruixiang Zhai, Ruiling Zhang, Yilin Liu

Abstract read
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. Cited by 3 papers.

0numbers the graph read from it
0cells of the map it votes in
3citing 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

3 citing papers in PubMed.

  1. Article
  2. Review
  3. Millennial-timescale thermogenic CONature communications · 2025
    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

6 authors.

Weiqi YaoDepartment of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen, Guangdong, China. yaowq@sustech.edu.cn.ORCID http://orcid.org/0000-0002-8177-7035
Tianshu KongDepartment of Earth and Environmental Sciences, Boston College, Chestnut Hill, MA, USA.ORCID http://orcid.org/0000-0002-5052-6911
Xingchen Tony WangDepartment of Earth and Environmental Sciences, Boston College, Chestnut Hill, MA, USA. xingchen.wang@bc.edu.ORCID http://orcid.org/0000-0001-5316-789X
Ruixiang ZhaiDepartment of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen, Guangdong, China.
Ruiling ZhangDepartment of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen, Guangdong, China.
Yilin LiuDepartment of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen, Guangdong, China.

Funding

Ministry of Science and Technology of the People's Republic of China (Chinese Ministry of Science and Technology) 2022YFF0802900National Natural Science Foundation of China (National Science Foundation of China) 42376049Natural Science Foundation of Guangdong Province (Guangdong Natural Science Foundation) 2024A1515012537Shenzhen Science and Technology Innovation Commission 20231114150312001
6 · The paper itself

Abstract

The ocean has experienced substantial oxygen loss over recent decades, affecting marine ecosystems and fisheries. Investigating ocean deoxygenation during hyperthermal events, such as the Paleocene-Eocene Thermal Maximum (PETM), offers insights into its future dynamics. Here, sediment cores from the South Atlantic reveal a pronounced decline in foraminifera-bound δ

Identifiers

PMID39427002
PMCPMC11490573

What OpenQuestion holds

Textmetadata
LicenceCC BY-NC-ND
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.