Evidence map›Paper›PMID 25825729›Full record

ArticleProceedings of the National Academy of Sciences of the United States of America2015

Four hundred million years of silica biomineralization in land plants.

Elizabeth Trembath-Reichert, Jonathan Paul Wilson, Shawn E McGlynn, Woodward W Fischer

Open access · bronzeAbstract read
In one paragraph

Article in Proceedings of the National Academy of Sciences of the United States of America, 2015. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 33 papers.

0numbers the graph read from it
0cells of the map it votes in
33citing papers in PubMed
23.8field-weighted citation impact, top 1% 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

33 citing papers in PubMed, 148 citations in OpenAlex.

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  17. Review
  18. Phytolith Formation in Plants: From Soil to Cell.Plants (Basel, Switzerland) · 2019
    Review
  19. Article
  20. A Review on Si Uptake and Transport System.Plants (Basel, Switzerland) · 2019
    Review
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 2 institutions in 2 countries.

Elizabeth Trembath-ReichertDivision of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125; e.t.r@caltech.edu.
Jonathan Paul WilsonDepartment of Biology, Haverford College, Haverford, PA 19041; and.
Shawn E McGlynnDivision of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125; Graduate School of Science and Engineering, Tokyo Metropolitan University, Hachioji-shi, Tokyo 192-0397, Japan.
Woodward W FischerDivision of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125;
California Institute of Technology · USHaverford College · US

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Biomineralization plays a fundamental role in the global silicon cycle. Grasses are known to mobilize significant quantities of Si in the form of silica biominerals and dominate the terrestrial realm today, but they have relatively recent origins and only rose to taxonomic and ecological prominence within the Cenozoic Era. This raises questions regarding when and how the biological silica cycle evolved. To address these questions, we examined silica abundances of extant members of early-diverging land plant clades, which show that silica biomineralization is widespread across terrestrial plant linages. Particularly high silica abundances are observed in lycophytes and early-diverging ferns. However, silica biomineralization is rare within later-evolving gymnosperms, implying a complex evolutionary history within the seed plants. Electron microscopy and X-ray spectroscopy show that the most common silica-mineralized tissues include the vascular system, epidermal cells, and stomata, which is consistent with the hypothesis that biomineralization in plants is frequently coupled to transpiration. Furthermore, sequence, phylogenetic, and structural analysis of nodulin 26-like intrinsic proteins from diverse plant genomes points to a plastic and ancient capacity for silica accumulation within terrestrial plants. The integration of these two comparative biology approaches demonstrates that silica biomineralization has been an important process for land plants over the course of their >400 My evolutionary history.

Indexed as

Biological EvolutionFossilsPlant Physiological PhenomenaPlantsSilicon DioxideSilicon Dioxideaquaporinfernlycophytephytolithsilicon

Identifiers

PMID25825729
PMCPMC4418875
OpenAlexW2061929773

What OpenQuestion holds

Textmetadata
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.