Evidence map›Paper›PMID 39875402›Full record

ArticleNature communications2025

Enhanced phosphorus weathering contributed to Late Miocene cooling.

Yi Zhong, Zhiguo Li, Xuefa Shi, Terry Isson, Jimin Yu, Sev Kender, Zhou Liang, George E A Swann, Alex Pullen, Michael E Weber and 12 more

Abstract read
PubMed Full text at PMC Publisher
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. 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

22 authors.

Yi ZhongCentre for Marine Magnetism (CM2), Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen, China. zhongy@sustech.edu.cn.ORCID http://orcid.org/0000-0002-4298-8737
Zhiguo LiState Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences, China University of Geosciences, Wuhan, China.
Xuefa ShiKey Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, State Oceanic Administration, Qingdao, China.ORCID http://orcid.org/0000-0001-8204-8021
Terry IssonTe Aka Mātuatua, University of Waikato (Tauranga), BOP, Tauranga, New Zealand.
Jimin YuLaoshan Laboratory, Qingdao, China.
Sev KenderCamborne School of Mines, Department of Earth and Environmental Sciences, University of Exeter, Cornwall, UK.ORCID http://orcid.org/0000-0003-4216-3214
Zhou LiangDepartment of Earth, Ocean and Atmospheric Science, Florida State University, Tallahassee, FL, USA.ORCID http://orcid.org/0000-0002-4999-7097
George E A SwannSchool of Geography, University of Nottingham, Nottingham, UK.ORCID http://orcid.org/0000-0002-4750-9504
Alex PullenDepartment of Environmental Engineering and Earth Sciences, Clemson University, Clemson, South Carolina, USA.ORCID http://orcid.org/0000-0002-5583-5844
Michael E WeberInstitute for Geosciences, Department of Geochemistry and Petrology, University of Bonn, Bonn, Germany.ORCID http://orcid.org/0000-0003-2175-8980
Jinlong DuState Key Laboratory of Marine Geology, Tongji University, Shanghai, China.ORCID http://orcid.org/0000-0003-2671-3765
Juan C LarrasoañaDepartment of Science, Universidad Pública de Navarra, Campus de Arrosadia, Pamplona, Spain.ORCID http://orcid.org/0000-0003-4568-631X
Jingyu ZhangCentre for Marine Magnetism (CM2), Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen, China.ORCID http://orcid.org/0000-0002-9507-3223
Yafang SongChinese Academy of Sciences Key Laboratory of Crust-Mantle Materials and Environments, University of Science and Technology of China, Hefei, China.
F J GonzálezGeological Survey of Spain (IGME), Rios Rosas 23, Madrid, Spain.ORCID http://orcid.org/0000-0002-6311-1950
Stefanie Kaboth-BahrInstitute of Geological Sciences, Freie Universität Berlin, Berlin, Germany.
Hai LiSouthern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou, China.
Qi ZhangSchool of Geophysics and Information Technology, China University of Geosciences, Beijing, China.
Debo ZhaoKey Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, China.ORCID http://orcid.org/0000-0002-4406-8985
Wei CaoCentre for Marine Magnetism (CM2), Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen, China.
Mingyu ZhaoState Key Laboratory of Lithospheric and Environmental Coevolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China. mingyu.zhao@mail.iggcas.ac.cn.ORCID http://orcid.org/0000-0002-6230-8399
Qingsong LiuCentre for Marine Magnetism (CM2), Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen, China. qsliu@sustech.edu.cn.

Funding

National Natural Science Foundation of China (National Science Foundation of China) 42261144739National Natural Science Foundation of China (National Science Foundation of China) 42274094National Natural Science Foundation of China (National Science Foundation of China) 42304082National Natural Science Foundation of China (National Science Foundation of China) 92158208
6 · The paper itself

Abstract

Late Miocene climate evolution provides an opportunity to assess Earth's climate sensitivity to carbon cycle perturbation under warmer-than-modern conditions. Despite its relevance for understanding the climate system, the driving mechanisms underlying profound climate and carbon cycle changes - including the enigmatic Late Miocene cooling from 7 to 5.4 million years ago - remain unclear. Here, we present magnetic and geochemical paleoceanographic proxies from a hydrogenetic ferromanganese crust retrieved in the northwestern Pacific Ocean. Our results indicate a striking 50% surge in deep ocean phosphorus concentrations occurred 7 - 4 million years ago, synchronous with enhanced deep ocean oxygen consumption. Employing a global biogeochemical model, we show that increased continental phosphorus weathering, without a concurrent rise in silicate weathering, contributed to the decline in atmospheric CO

Identifiers

PMID39875402
PMCPMC11775330

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.