Evidence map›Paper›PMID 40770177›Full record

ArticleNature communications2025

Preconditioning of sediment failure by astronomically paced weak-layer deposition.

Xingxing Wang, Vittorio Maselli, Luca Flessati, Hongbin Wang, Zhilei Sun, Qing Wang, Jie Chen, Qing Li, Stefano Alberti, Markus Kienast and 2 more

Abstract read
In one paragraph

Article in Nature communications, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 1 paper.

0numbers the graph read from it
0cells of the map it votes in
1citing 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

1 citing paper in PubMed.

  1. 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

12 authors.

Xingxing WangHubei Key Laboratory of Marine Geological Resources, China University of Geosciences, Wuhan, China.
Vittorio MaselliDepartment of Chemical and Geological Sciences, University of Modena and Reggio Emilia, Modena, Italy.
Luca FlessatiFaculty of Civil Engineering and Geosciences, Delft University of Technology, Delft, The Netherlands.
Hongbin WangKey Laboratory of Gas Hydrate, Ministry of Natural Resources, Qingdao Institute of Marine Geology, Qingdao, China.
Zhilei SunKey Laboratory of Gas Hydrate, Ministry of Natural Resources, Qingdao Institute of Marine Geology, Qingdao, China.
Qing WangHubei Key Laboratory of Marine Geological Resources, China University of Geosciences, Wuhan, China.
Jie ChenSchool of Geosciences, China University of Petroleum (East China), Qingdao, China.
Qing LiKey Laboratory of Gas Hydrate, Ministry of Natural Resources, Qingdao Institute of Marine Geology, Qingdao, China.
Stefano AlbertiCollege of Forestry, Oregon State University, Corvallis, OR, USA.ORCID http://orcid.org/0000-0002-3756-0963
Markus KienastDepartment of Oceanography, Dalhousie University, Halifax, Nova Scotia, Canada.ORCID http://orcid.org/0000-0002-5698-8105
Shucheng XieState Key Laboratory of Geobiogeology and Environmental Changes, China University of Geosciences, Wuhan, China.ORCID http://orcid.org/0000-0002-5763-2928
Qiliang SunHubei Key Laboratory of Marine Geological Resources, China University of Geosciences, Wuhan, China. sunqiliang@cug.edu.cn.ORCID http://orcid.org/0000-0002-8335-5004

Funding

National Natural Science Foundation of China (National Science Foundation of China) 42222607National Natural Science Foundation of China (National Science Foundation of China) 42476252Natural Science Foundation of Shandong Province (Shandong Provincial Natural Science Foundation) ZR2020QD034
6 · The paper itself

Abstract

Low-strength sediment layers within continental slope strata precondition submarine sediment for failure, potentially leading to destructive tsunamis. Using geophysical and Ocean Drilling Program well data, here we show that the glide planes of widespread submarine failures in the northern South China Sea, dated to the glacial stages following the Mid-Pleistocene Transition, have higher opal content, particle size, and porosity, which reduce the undrained shear strength. Cyclic weak-layer deposition, modulated at Milankovitch time scale, was controlled by increased ocean primary productivity and sedimentation rates linked to high-amplitude sea-level fluctuations and intensified winter monsoons. This study represents an important step forward for understanding how climate influences the formation of weak layers and the stability of continental slope globally.

Identifiers

PMID40770177
PMCPMC12328812

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.