Confocal microscopy: an experimental set up for biomolecule structure investigation based on dynamical fluorescence spectroscopy

Author(s):  
A. Oldani ◽  
M. Collini ◽  
G. Chirico ◽  
L. D'Alfonso ◽  
G. Baldini ◽  
...  
2003 ◽  
Author(s):  
Amanda Oldani ◽  
Maddalena Collini ◽  
Giuseppe Chirico ◽  
Laura D'Alfonso ◽  
Giancarlo Baldini ◽  
...  

2019 ◽  
Vol 43 (8) ◽  
pp. 3332-3340 ◽  
Author(s):  
Ma. Concepción García ◽  
Gleb Turlakov ◽  
Ivana Moggio ◽  
Eduardo Arias ◽  
J. Humberto Valenzuela ◽  
...  

The staining of agrobacteria was successfully demonstrated through a benzoateethynylene by fluorescence spectroscopy, laser confocal microscopy and microRaman.


2011 ◽  
pp. 235-272 ◽  
Author(s):  
Anya Salih ◽  
Paul Wormell ◽  
K. Benjamin Garbutcheon-Singh ◽  
Benjamin Harper ◽  
Simon Myers ◽  
...  

1999 ◽  
Vol 5 (S2) ◽  
pp. 470-471
Author(s):  
Pier A. Benedetti ◽  
Valter Evangelista ◽  
Dante Guidarini ◽  
Stefano Vestri

State of the art in optical microscopyOptical microscopy is still and increasingly one of the most valuable tools in biological investigation. In particular, confocal microscopies are capable of achieving best performances in the study of three-dimensional fluorescent and reflecting specimens. Nevertheless, current techniques adopted in confocal microscopy present some drawbacks and limitations that stimulate to devise and set-up further techniques, suited to a wider range of applications.Advantages of confocal microscopes mainly correspond to an improved spatial resolution, especially in the axial direction. Depending on the narrow-field scanning approach used, there are two main forms of confocal microscopes: single-point (SP) and multi-point (MP) ones. Unfortunately, SP confocal microscopes require the use of lasers as illumination sources with consequent high costs and scarce spectral flexibility. Moreover, specimen photo-damage due to relatively high instantaneous irradiation doses involved, can often limit their investigative capabilities. On the other hand, proposed MP confocal microscopes still rely on the revolving-disk approach and exhibit a relatively low luminous efficiency, substantial constructional complexity, and limited contrast in the study of thick fluorescent objects.


2020 ◽  
Author(s):  
Baptiste Suchéras-Marx ◽  
Fabienne Giraud ◽  
Alexandre Simionovici ◽  
Rémi Tucoulou ◽  
Isabelle Daniel

Paleoceanographical reconstructions are often based on microfossil geochemical analyses. Coccoliths are the most ancient, abundant and continuous record of pelagic photic zone calcite producer organisms. Hence, they could be valuable substrates for geochemically based paleoenvironmental reconstructions but only Sr/Ca is exploited even if it remains poorly understood. For example, some murolith coccoliths species have very high Sr/Ca compared to the common 1-4 mmol/mol recorded in placolith coccoliths. In this study, we analyzed the elemental composition of the Middle Jurassic murolith Crepidolithus crassus by synchrotron-based nanoXRF (X-ray Fluorescence Spectroscopy) mapping focusing on Sr/Ca and compared the record to two placolith species, namely Watznaueria contracta and Discorhabdus striatus. In C. crassus, Sr/Ca is more than ten times higher than in both placoliths and seems higher in the proximal cycle. By comparison with the placoliths analyzed in the same analytical set-up and from the same sample, we exclude the impact of the diagenesis and seawater Sr/Ca to explain the high Sr/Ca in C. crassus. Based on comparisons to Pontosphaera discopora and Scyphosphaera apsteinii which also have high Sr/Ca, it seems more likely that high Sr/Ca in C. crassus is either due to the vertical elongation of the R-units of the proximal cycle or related to the action of the special polysaccharide controlling the growth of those vertically elongated R-units that may have affinities to Sr2+. In order to apply the Sr/Ca proxy to muroliths, further investigations are needed on cultured coccoliths.


2020 ◽  
Vol 9 (1) ◽  
pp. 141-160
Author(s):  
Bayu Achil Sadjab ◽  
I Putu Tedy Indrayana ◽  
Steven Iwamony ◽  
Rofiqul Umam

This research aimed to investigate the distribution, volume, and concentration of iron sand at Wari Ino Beach Tobelo. The resistivity method with Werner-Schlumberger configuration was applied to investigate the iron sand distribution. The measurements were set-up on 3 lines that run parallel along the coast of Wari Ino Village. The length of each trajectory was 150 meters with a spacing of 10 meters for each electrode. Data acquisition was carried out by using geoelectric instruments to obtain current injection (I) and voltage (V). The analysis was carried out by using RES2DINV and ROCKWORK software to obtain 2-D and 3-D cross-section models for interpreting the distribution and volume of the iron sand. The analysis and interpretation were supported by geological data of the location. Furthermore, the Fe content was characterized by using X-Ray Fluorescence Spectroscopy (XRF). There results show that the volume of the iron sand in each trajectory was 109,355 m3; 180,254 m3; and 120,556 m3. The total volume of iron sand along the three trajectories was up to 405,335 m3. The Fe content in the form of a free element is 67.41%, 57.12%, and 73.40%. The Fe content in the form of hematite mineral (Fe2O3) was 57.92%, 45.82%, and 65.47%.


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