Cryopreservation of Biological Systems–A Confocal Raman Microscopy Study

2010 ◽  
Author(s):  
Jinping Dong ◽  
Allison Hubel ◽  
John C. Bischof ◽  
Alptekin Aksan ◽  
P. M. Champion ◽  
...  
2018 ◽  
Vol 15 (141) ◽  
pp. 20170723 ◽  
Author(s):  
Kirti Ramesh ◽  
Frank Melzner ◽  
Andrew W. Griffith ◽  
Christopher J. Gobler ◽  
Caroline Rouger ◽  
...  

In vivo confocal Raman microscopy (CRM), polarized light microscopy and Fourier transform infrared spectroscopy (FTIR) were used to determine if a significant amount of amorphous calcium carbonate (ACC) exists within larval shells of Baltic mytilid mussels ( Mytilus edulis -like) and whether the amount of ACC varies during larval development. No evidence for ACC was found from the onset of shell deposition at 21 h post-fertilization (hpf) until 48 hpf. Larval Mytilus shells were crystalline from 21 hpf onwards and exhibited CRM and FTIR peaks characteristic of aragonite. Prior to shell deposition at 21 hpf, no evidence for carbonates was observed through in vivo CRM. We further analysed the composition of larval shells in three other bivalve species, Mercenaria mercenaria , Crassostrea gigas and Crassostrea virginica and observed no evidence for ACC, which is in contrast to previous work on the same species. Our findings indicate that larval bivalve shells are composed of crystalline aragonite and we demonstrate that conflicting results are related to sub-optimal measurements and misinterpretation of CRM spectra. Our results demonstrate that the common perception that ACC generally occurs as a stable and abundant precursor during larval bivalve calcification needs to be critically reviewed.


2012 ◽  
Vol 9 (7) ◽  
pp. 8273-8306 ◽  
Author(s):  
M. Wall ◽  
G. Nehrke

Abstract. Confocal Raman microscopy mapping was used to investigate the organic matrix distribution within the skeleton of the coral Porites lutea. Two types of growth lines could be identified: one corresponds to the well-known incremental growth layers, whereas the second type of growth lines showed an elemental composition that differed from the incremental growth layers. The position and shape of the latter growth lines resemble either denticle finger-like structures (most likely traces of former spines) or former skeletal surfaces. We hypothesize that these lines are involved in the three-dimensional arrangement of skeletal elements and represent the outer skeletal surface before another growth cycle of elongation, infilling and thickening of skeletal components continues. We show that high spatial resolution mapping can significantly improve our understanding of skeletal growth patterns in coral skeletons.


Cryobiology ◽  
2008 ◽  
Vol 57 (3) ◽  
pp. 325
Author(s):  
Jinping Dong ◽  
Allison Hubel ◽  
John C. Bischof ◽  
Alptekin Aksan

2016 ◽  
Vol 92 ◽  
pp. 1-7 ◽  
Author(s):  
François Courtecuisse ◽  
Feyza Karasu ◽  
Xavier Allonas ◽  
Céline Croutxé-Barghorn ◽  
Leendert van der Ven

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