Literature DB >> 28382964

Erratum: Potential microbial contamination during sampling of permafrost soil assessed by tracers.

Toke Bang-Andreasen, Morten Schostag, Anders Priemé, Bo Elberling, Carsten S Jacobsen.   

Abstract

Entities:  

Year:  2017        PMID: 28382964      PMCID: PMC5382581          DOI: 10.1038/srep46006

Source DB:  PubMed          Journal:  Sci Rep        ISSN: 2045-2322            Impact factor:   4.379


× No keyword cloud information.
The original HTML version of this Article contained formatting errors in the “Gravimetric water (ice) content (%)” row. The correct Table appears below.
Table 1

Physical-chemical parameters of the permafrost cores.

 ZackenbergAdventdalen 1Adventdalen 2
pH6.75.16.8
Total C (%)2.4 ± 0.0014.5 ± 0.0612.24
Total N (%)0.16 ± 0.0130.33 ± 0.0040.14
DOC (mg L−1)16.0 ± 0.6712.7 ± 0.2460.3
NH4+ (mg L−1)18.9 ± 6.41.5 ± 0.425.1
NO3− (mg L−1)46.3 ± 0.40.11 ± 0.0210.202
Gravimetric water (ice) content (%)27.444.159.5
Soil texture (% of clay (<2 μm); silt (2–63 μm); sand (>63 μm))7.6; 74.4; 18.05.5; 47.6; 46.94.1; 68.4; 27.5

The ± symbols indicate standard error of the mean, n = 3. Numbers without ± are measurements on a single replicate, n = 1, because too little soil was obtained to perform measurements on triplicates.

This error has been corrected in the HTML version of the Article; the PDF version was correct at the time of publication.
  1 in total

1.  Spatially resolved correlative microscopy and microbial identification reveal dynamic depth- and mineral-dependent anabolic activity in salt marsh sediment.

Authors:  Jeffrey Marlow; Rachel Spietz; Keun-Young Kim; Mark Ellisman; Peter Girguis; Roland Hatzenpichler
Journal:  Environ Microbiol       Date:  2021-08-04       Impact factor: 5.491

  1 in total

北京卡尤迪生物科技股份有限公司 © 2022-2023.