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Diatoms as potential “green” nanocomposite and nanoparticle synthesizers: challenges, prospects, and future materials applications

Published online by Cambridge University Press:  08 March 2018

Nathalie Pytlik
Affiliation:
Bioanalytical Chemistry, TU Dresden, Dresden 01062, Germany
Eike Brunner*
Affiliation:
Bioanalytical Chemistry, TU Dresden, Dresden 01062, Germany
*
Address all correspondence to Eike Brunner at eike.brunner@tu-dresden.de

Abstract

Diatoms are unicellular, eukaryotic microalgae inhabiting nearly all aquatic habitats. They are famous for their micro- and nanopatterned silica-based cell walls, which are envisioned for various technologic purposes. Within this review article, we summarize recent in vivo modifications of diatom biosilica with respect to the following questions: (i) Which metals are taken up by diatoms and eventually processed into nanoparticles (NPs)? (ii) Are these NPs toxic for the diatoms and––if so––what factors influence toxicity? (iii) What is the mechanism underlying NP synthesis and subsequent metabolism? (iv) How can the obtained materials be useful for materials science?

Information

Type
Prospective Articles
Copyright
Copyright © Materials Research Society 2018 
Figure 0

Figure 1. SEM images of different diatom species. (a) Cyclotella sp., (b) Aulacoseira granulate, (c) Stephanodiscus niagarae, (d) Eucampia zodiacus, (e) Amphora perpusilla, (f) Thalassiosira pseudonana, (g) Cymatopleura solea, (h) Melosira varians, (i) Stephanodiscus minutulus, (j) Stephanopyxis turris, (k) Lindavia bodanica, (l) Caloneis sp. Reproduced from Ref. 7 (Fischer, 2017).

Figure 1

Figure 2. Structure of aluminum in the silica framework with Men+ as counter ion. Reproduced from Ref. 38 (MDPI, 2017) (https://creativecommons.org/licenses/by/4.0/).

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Figure 3. Comparison of the EPR spectra of biosilica and iron-containing silicagel (pH 7) measured at (a) 300 K and (b) 10 K. Note the presence of a broad signal at g = 2.3 in biosilica which disappears after cooling to 10 K. This signal is due to Fe2O3 clusters. In contrast, Fe is mainly dispersed in silicagel and gives rise to signals at 4.3 and 2.0 which are also present at 10 K. Reproduced from Ref. 42 (Springer Nature, 2017). * denotes a weak Mn2+ signal due to a minor impurity in the silicagel.

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Figure 4. Schematic procedure for NP biosynthesis by diatoms.

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Figure 5. (a) SAED result of biosynthesized Au NPs (black) in comparison with the reflexes from Au crystals with the face-centered cubic space group Fm-3m (blue) and (b) EDX line measurement of biosynthesized Au NPs. Adapted from Ref. 64 (Elsevier, 2017).

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Figure 6. Three-dimensional image of an Stephanopyxis turris cell (22 µm × 67 µm × 45 µm) with schematic chloroplasts (green) and SERS spectra (red) from different perspectives. Adapted from Ref. 64 (Elsevier, 2017).

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Figure 7. Possible ways for transport and synthesis of Ag and Au NPs by photosynthetic microorganisms. Uptake of Ag+ into the cell by (a) Cu(I)-ATPase or (b) diffusion. (c) Extracellular gold reduction by extracellular polymeric substances. (d) Binding of intracellular Au NPs to organelle membrane surfaces. Intracellular gold reduction by photosynthetically produced (e) electrons or (f) redox mediators. (g) Export of Au NPs and (h) release of the Au NPs from the extracellular matrix. Reproduced from Ref. 14 (Elsevier, 2015).

Figure 7

Figure 8. Different endocytic pathways for cellular uptake depending on the size, the nature of the cargo (ligands, receptors, and lipids), and the mechanism of vesicle formation. Reproduced from Ref. 65 (Springer Nature, 2003).