2 research outputs found
Cellular internalization and intracellular biotransformation of silver nanoparticles in <i>Chlamydomonas reinhardtii</i>
<p>It is necessary to elucidate cellular internalization and intracellular biotransformation in order to accurately assess the toxicity and fate of nanoparticles after interaction with organisms. Therefore, this work employed a combination of high resolution imaging and <i>in situ</i> detection spectroscopic techniques to systematically investigate the intracellular localization, morphology and chemical speciation of silver in the cells of <i>Chlamydomonas reinhardtii</i>, a unicellular freshwater green alga, after exposure to AgNPs coated with polyvinylpyrrolidone at a concentration of 2.0 mg/L. High resolution secondary ion mass spectrometry and high-angle annular dark field scanning transmission electron microscopy together with energy dispersive spectroscopy and selected area electron diffraction collectively confirmed that after 48 h of exposure, AgNPs entered the periplasmic space after cellular internalization into the algal cells. Silver was also found to coexist with sulfur inside the cytoplasm in both crystalline and amorphous forms, which were further identified as β-Ag<sub>2</sub>S and silver thiolates with synchrotron X-ray absorption spectroscopy. In combination, these analyses demonstrated that silver inside algae could be attributed to the uptake and sequestration of Ag<sup>+</sup> ion released from AgNPs, which was further sequestrated into cellular compartments. This study provides solid evidence for particle internalization and biotransformation of AgNPs after interaction with algae.</p
Molecular-Scale Investigation with ESI-FT-ICR-MS on Fractionation of Dissolved Organic Matter Induced by Adsorption on Iron Oxyhydroxides
Adsorption
by minerals is a common geochemical process of dissolved
organic matter (DOM) which may induce fractionation of DOM at the
mineral-water interface. Here, we examine the molecular fractionation
of DOM induced by adsorption onto three common iron oxyhydroxides
using electrospray ionization coupled with Fourier-transform ion cyclotron
resonance mass spectrometry (ESI-FT-ICR-MS). Ferrihydrite exhibited
higher affinity to DOM and induced more pronounced molecular fractionation
of DOM than did goethite or lepidocrocite. High molecular weight (>500
Da) compounds and compounds high in unsaturation or rich in oxygen
including polycyclic aromatics, polyphenols and carboxylic compounds
had higher affinity to iron oxyhydroxides and especially to ferrihydrite.
Low molecular weight compounds and compounds low in unsaturation or
containing few oxygenated groups (mainly alcohols and ethers) were
preferentially maintained in solution. This study confirms that the
double bond equivalence and the number of oxygen atoms are valuable
parameters indicating the selective fractionation of DOM at mineral
and water interfaces. The results of this study provide important
information for further understanding the behavior of DOM in the natural
environment