Evidence map›Paper›PMID 28262764›Full record

ArticleNature communications2017

The origin of carbon isotope vital effects in coccolith calcite.

H L O McClelland, J Bruggeman, M Hermoso, R E M Rickaby

Open access · goldAbstract read
In one paragraph

Article in Nature communications, 2017. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 6 papers.

0numbers the graph read from it
0cells of the map it votes in
6citing papers in PubMed
12.3field-weighted citation impact, top 2% of its field
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

6 citing papers in PubMed, 90 citations in OpenAlex.

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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

4 authors at 4 institutions in 3 countries.

H L O McClellandDepartment of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, UK.
J BruggemanPlymouth Marine Laboratory, Prospect Place, The Hoe, Plymouth PL1 3DH, UK.
M HermosoDepartment of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, UK.ORCID 0000-0003-1427-1891
R E M RickabyDepartment of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, UK.
Centre National de la Recherche Scientifique · FRPlanetary Science Institute · USPlymouth Marine Laboratory · GBUniversity of Oxford · GB

Funding

European Research Council 200915
6 · The paper itself

Abstract

Calcite microfossils are widely used to study climate and oceanography in Earth's geological past. Coccoliths, readily preserved calcite plates produced by a group of single-celled surface-ocean dwelling algae called coccolithophores, have formed a significant fraction of marine sediments since the Late Triassic. However, unlike the shells of foraminifera, their zooplankton counterparts, coccoliths remain underused in palaeo-reconstructions. Precipitated in an intracellular chemical and isotopic microenvironment, coccolith calcite exhibits large and enigmatic departures from the isotopic composition of abiogenic calcite, known as vital effects. Here we show that the calcification to carbon fixation ratio determines whether coccolith calcite is isotopically heavier or lighter than abiogenic calcite, and that the size of the deviation is determined by the degree of carbon utilization. We discuss the theoretical potential for, and current limitations of, coccolith-based CO

Identifiers

PMID28262764
PMCPMC5343501
OpenAlexW2592574471

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.