Evidence map›Paper›PMID 26218096›Full record

ArticlePloS one2015

Phytoplankton Productivity in an Arctic Fjord (West Greenland): Estimating Electron Requirements for Carbon Fixation and Oxygen Production.

Kasper Hancke, Tage Dalsgaard, Mikael Kristian Sejr, Stiig Markager, Ronnie Nøhr Glud

Open access · goldAbstract read
In one paragraph

Article in PloS one, 2015. 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
3.8field-weighted citation impact, top 8% 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

4 citing papers in PubMed, 53 citations in OpenAlex.

  1. Article
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  3. Large-Scale Cultivation ofFrontiers in bioengineering and biotechnology · 2019
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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

5 authors at 3 institutions in 3 countries.

Kasper HanckeNordic Center for Earth Evolution (NordCEE), Department of Biology, University of Southern Denmark, Odense, Denmark; Greenland Climate Research Centre, Greenland Institute of Natural Resources, Nuuk, Greenland.
Tage DalsgaardArctic Research Center, Aarhus University, Aarhus, Denmark.
Mikael Kristian SejrGreenland Climate Research Centre, Greenland Institute of Natural Resources, Nuuk, Greenland; Arctic Research Center, Aarhus University, Aarhus, Denmark.
Stiig MarkagerInstitute for Bioscience, Aarhus University, Aarhus, Denmark.
Ronnie Nøhr GludNordic Center for Earth Evolution (NordCEE), Department of Biology, University of Southern Denmark, Odense, Denmark; Greenland Climate Research Centre, Greenland Institute of Natural Resources, Nuuk, Greenland; Arctic Research Center, Aarhus University, Aarhus, Denmark; Scottish Association for Marine Science, Scottish Marine Institute, Oban, United Kingdom.
Aarhus University · DKGrønlands Naturinstitut · GLUniversity of Southern Denmark · DK

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Accurate quantification of pelagic primary production is essential for quantifying the marine carbon turnover and the energy supply to the food web. Knowing the electron requirement (Κ) for carbon (C) fixation (ΚC) and oxygen (O2) production (ΚO2), variable fluorescence has the potential to quantify primary production in microalgae, and hereby increasing spatial and temporal resolution of measurements compared to traditional methods. Here we quantify ΚC and ΚO2 through measures of Pulse Amplitude Modulated (PAM) fluorometry, C fixation and O2 production in an Arctic fjord (Godthåbsfjorden, W Greenland). Through short- (2h) and long-term (24h) experiments, rates of electron transfer (ETRPSII), C fixation and/or O2 production were quantified and compared. Absolute rates of ETR were derived by accounting for Photosystem II light absorption and spectral light composition. Two-hour incubations revealed a linear relationship between ETRPSII and gross 14C fixation (R2 = 0.81) during light-limited photosynthesis, giving a ΚC of 7.6 ± 0.6 (mean ± S.E.) mol é (mol C)-1. Diel net rates also demonstrated a linear relationship between ETRPSII and C fixation giving a ΚC of 11.2 ± 1.3 mol é (mol C)-1 (R2 = 0.86). For net O2 production the electron requirement was lower than for net C fixation giving 6.5 ± 0.9 mol é (mol O2)-1 (R2 = 0.94). This, however, still is an electron requirement 1.6 times higher than the theoretical minimum for O2 production [i.e. 4 mol é (mol O2)-1]. The discrepancy is explained by respiratory activity and non-photochemical electron requirements and the variability is discussed. In conclusion, the bio-optical method and derived electron requirement support conversion of ETR to units of C or O2, paving the road for improved spatial and temporal resolution of primary production estimates.

Indexed as

Carbon CycleArctic RegionsBiodiversityElectron TransportFluorescenceFluorometryGreenlandLightOxygenPhotosynthesisPhotosystem II Protein ComplexPhytoplanktonOxygenPhotosystem II Protein Complex

Identifiers

PMID26218096
PMCPMC4517866
OpenAlexW1621226783

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.