Evidence map›Paper›PMID 39072083›Full record

ArticleACS omega2024

Elemental Geochemical Characteristics of Shales from Wufeng-Longmaxi Formations in the Southern Margin of the Qinling Orogenic Belt, China: Implications for Depositional Controls on Organic Matter.

Bin Xiao, Dongxu Guo, Zhongying Zhao, Shuzhen Xiong, Mingfei Feng, Zhonghai Zhao, Sheng Li

Abstract read
PubMed Full text at PMC Publisher
In one paragraph

Article in ACS omega, 2024. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 7 papers.

0numbers the graph read from it
0cells of the map it votes in
7citing 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

7 citing papers in PubMed.

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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

7 authors.

Bin XiaoCollege of Mining, Liaoning Technical University, Fuxin 123000, China.ORCID https://orcid.org/0000-0003-1006-7965
Dongxu GuoCollege of Mining, Liaoning Technical University, Fuxin 123000, China.
Zhongying ZhaoPetroChina Research Institute of Petroleum Exploration & Development, Beijing 100083, China.ORCID https://orcid.org/0000-0003-1370-2186
Shuzhen XiongCollege of Environmental Science and Engineering, Liaoning Technical University, Fuxin 123000, China.
Mingfei FengCollege of Mining, Liaoning Technical University, Fuxin 123000, China.
Zhonghai ZhaoCollege of Mining, Liaoning Technical University, Fuxin 123000, China.
Sheng LiLiaoning Geology Engineering Vocational College, Dandong 118000, China.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The tectonic background and sedimentary environment during the transition period from the Ordovician to Silurian have been widely studied by many scholars. This study focuses on the Upper Ordovician Wufeng Formation and Lower Silurian Longmaxi Formation in the Bajiaokou profile at the southern margin of the Qinling Orogenic Belt in southern China. In order to study the aggregation mechanism of organic matter, geochemical proxies were proposed, including redox proxies (V, V/Al, U, U/Al, Mo, and Mo/Al), paleoproductivity proxies (P, P/Ti, Ba, Ba/Al, and Si

Identifiers

PMID39072083
PMCPMC11270573

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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.