Evidence map›Paper›PMID 33825155›Full record

ArticleAmbio2021

Key periods of peatland development and environmental changes in the middle taiga zone of Western Siberia during the Holocene.

Andrey N Tsyganov, Evgeny A Zarov, Yuri A Mazei, Mikhail G Kulkov, Kirill V Babeshko, Svetlana Y Yushkovets, Richard J Payne, Joshua L Ratcliffe, Yulia A Fatyunina, Elya P Zazovskaya and 1 more

Abstract read
PubMed Full text at PMC Publisher
In one paragraph

Article in Ambio, 2021. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 4 papers.

0numbers the graph read from it
0cells of the map it votes in
4citing 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

4 citing papers in PubMed.

  1. Article
  2. Article
  3. Article
  4. 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

11 authors.

Andrey N TsyganovDepartment of General Ecology and Hydrobiology, Lomonosov Moscow State University, Leninskie Gory 1, building 12, Moscow, Russia, 119234. andrey.tsyganov@bk.ru.ORCID http://orcid.org/0000-0002-5660-8432
Evgeny A ZarovResearch Education Center of Environmental Dynamics and Climate Change (UNESCO Chair), Yugra State University, Chekhova str. 16, Khanty-Mansiysk, Russia, 628007.ORCID http://orcid.org/0000-0003-2871-2731
Yuri A MazeiDepartment of General Ecology and Hydrobiology, Lomonosov Moscow State University, Leninskie Gory 1, building 12, Moscow, Russia, 119234.ORCID http://orcid.org/0000-0002-5443-8919
Mikhail G KulkovResearch Education Center of Environmental Dynamics and Climate Change (UNESCO Chair), Yugra State University, Chekhova str. 16, Khanty-Mansiysk, Russia, 628007.
Kirill V BabeshkoDepartment of General Biology and Biochemistry, Penza State University, Lermontova str. 37, building 15, Penza, Russia, 440026.
Svetlana Y YushkovetsDepartment of Zoology and Ecology, Penza State University, Lermontova str. 37, building 15, Penza, Russia, 440026.
Richard J PayneEnvironment Department, University of York, York, YO10 5DD, UK.
Joshua L RatcliffeDepartment of Forest Ecology and Management, Swedish University of Agricultural Sciences, Umeå, Sweden.
Yulia A FatyuninaDepartment of General Biology and Biochemistry, Penza State University, Lermontova str. 37, building 15, Penza, Russia, 440026.
Elya P ZazovskayaLaboratory of Radiocarbon Dating and Electron Microscopy, Institute of Geography of the Russian Academy of Science (IG RAS), Staromonetniy Lane 29, Moscow, Russia, 119017.
Elena D LapshinaResearch Education Center of Environmental Dynamics and Climate Change (UNESCO Chair), Yugra State University, Chekhova str. 16, Khanty-Mansiysk, Russia, 628007.ORCID http://orcid.org/0000-0001-5571-7787

Funding

grant of the Yugra State University 13-01-20/39INTERACT-II PEATSUREINTERACT-II TREEPEATRussian Foundation for Basic Research 18-44-860017Russian Science Foundation 19-14-00102
6 · The paper itself

Abstract

The response of peatlands to climate change can be highly variable. Through understanding past changes we can better predict the response of peatlands to future climate change. We use a multi-proxy approach to reconstruct the surface wetness and carbon accumulation of the Mukhrino mire (Western Siberia), describing the development of the mire since peat formation in the early Holocene, around 9360 cal. year BP. The mire started as a rich fen which initiated after paludification of a spruce forest (probably in response to a wetter climate), while the Mukhrino mire progressed to ombrotrophic bog conditions (8760 cal. year BP). This transition coincided with the intensive development of mires in Western Siberia and was associated with active carbon accumulation (31 g m

Indexed as

EcosystemTaigaCarbon SequestrationSiberiaSoilSoilCarbon contentn-AlkanesPeat humificationPeatland developmentPlant macrofossilsTestate amoebae

Identifiers

PMID33825155
PMCPMC8497661

What OpenQuestion holds

Textmetadata
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Registered trials

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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.