Construction and morphogenesis of the chiral ultrastructure of coccoliths from the marine alga Emiliania huxleyi

1994 ◽  
Vol 258 (1353) ◽  
pp. 237-245 ◽  
2016 ◽  
Vol 210 (1) ◽  
pp. 88-96 ◽  
Author(s):  
Sergey Malitsky ◽  
Carmit Ziv ◽  
Shilo Rosenwasser ◽  
Shuning Zheng ◽  
Daniella Schatz ◽  
...  

2001 ◽  
Vol 67 (9) ◽  
pp. 3824-3831 ◽  
Author(s):  
Richard Laguna ◽  
Jesus Romo ◽  
Betsy A. Read ◽  
Thomas M. Wahlund

ABSTRACT Emiliania huxleyi is a unicellular marine alga that is considered to be the world's major producer of calcite. The life cycle of this alga is complex and is distinguished by its ability to synthesize exquisitely sculptured calcium carbonate cell coverings known as coccoliths. These structures have been targeted by materials scientists for applications relating to the chemistry of biomedical materials, robust membranes for high-temperature separation technology, lightweight ceramics, and semiconductor design. To date, however, the molecular and biochemical events controlling coccolith production have not been determined. In addition, little is known about the life cycle of E. huxleyi and the environmental and physiological signals triggering phase switching between the diploid and haploid life cycle stages. We have developed laboratory methods for inducing phase variation between the haploid (S-cell) and diploid (C-cell) life cycle stages of E. huxleyi. PlatingE. huxleyi C cells on solid media was shown to induce phase switching from the C-cell to the S-cell life cycle stage, the latter of which has been maintained for over 2 years under these conditions. Pure cultures of S cells were obtained for the first time. Laboratory conditions for inducing phase switching from the haploid stage to the diploid stage were also established. Regeneration of the C-cell stage from pure cultures of S cells followed a predictable pattern involving formation of large aggregations of S cells and the subsequent production of cultures consisting predominantly of diploid C cells. These results demonstrate the ability to manipulate the life cycle of E. huxleyi under controlled laboratory conditions, providing us with powerful tools for the development of genetic techniques for analysis of coccolithogenesis and for investigating the complex life cycle of this important marine alga.


Author(s):  
Andreas Ziegler ◽  
Xiaofei Yin ◽  
Erika Griesshaber ◽  
Lothar Miersch ◽  
Thorsten B. Reusch ◽  
...  

1979 ◽  
Vol 99 (3) ◽  
pp. 559-567 ◽  
Author(s):  
Elisabeth JONG ◽  
Lisette RENS ◽  
Peter WESTBROEK ◽  
Leendert BOSCH

1989 ◽  
Vol 36 (4) ◽  
pp. 368-373 ◽  
Author(s):  
P. WESTBROEK ◽  
J. R. YOUNG ◽  
K. LINSCHOOTEN

2008 ◽  
Vol 88 (7) ◽  
pp. 1343-1346 ◽  
Author(s):  
Suhaimi Suratman ◽  
Keith Weston ◽  
Tim Jickells ◽  
Rosie Chance ◽  
Tom Bell

Measurements of the release of dissolved organic nitrogen (DON) and carbon (DOC) were carried out on an axenic batch culture of the coccolithophorid Emiliania huxleyi. This unicellular marine alga was cultured using a media with nitrate as the sole N source and the changes of DOM concentrations measured over 14 days. Results showed that there was a significant release of DON, i.e.7.6 µM N day−1 during mid-exponential growth phase (days 5–7). The highest release of DOC was also recorded in the same growth phase and accounted for 24.0 μM C day−1.


1988 ◽  
Vol 234 (1277) ◽  
pp. 441-453 ◽  

Electron diffraction and high-resolution transmission electron microscopy indicate that the radial segments composing coccoliths of the marine alga Emiliania huxleyi are individual single crystalline units of calcite. The top and bottom surfaces of the plate-like lower element correspond to the (12̄10) and (1̄21̄0) faces, and the [0001] direction ( c axis) is oriented parallel to these faces and in the direction of elongation of the lower and upper elements. The [101̄0] direction is perpendicular to the direction of elongation and corresponds to the direction of growth of the hammer-head extension in the upper element. Each radial segment exhibits handedness when viewed from above. The peripheral edges of the lower element are truncated by (101̄4) and (1̄018) rhombohedral faces with the (1̄018) face being more extensively developed and always positioned to the left when viewed from above, indicating the specific growth of the (1̄21̄0) face on the surface of the underlying base plate. Energy-dispersive X-ray analysis (EDXA) showed no evidence for localized compositional changes in the coccolith components. A mechanism is proposed in which the biological control of the development of individual radial segments is determined by the initial orientation of calcite rhombohedra with the (1̄21̄0) face parallel to the organic base plate, followed by vectorial regulation of crystal growth in three dimensions through the spatial restrictions set by the developing ultrastructure of the surrounding coc­colith vesicle membrane. The geometric, stereochemical and symmetry requirements of molecular interactions between ions in the (1̄21̄0) face and macromolecules in the polysaccharide-containing base plate are dis­cussed.


2015 ◽  
Vol 74 (2) ◽  
pp. 173-185 ◽  
Author(s):  
LJ Darroch ◽  
M Lavoie ◽  
M Levasseur ◽  
I Laurion ◽  
WG Sunda ◽  
...  

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