Fatty acid-clay mineral association in artificial and natural sea water solutions

1971 ◽  
Vol 35 (6) ◽  
pp. 628-632 ◽  
Author(s):  
Phillip A. Meyers ◽  
James G. Quinn
Desalination ◽  
1972 ◽  
Vol 10 (4) ◽  
pp. 319-328 ◽  
Author(s):  
J.D. Isdale ◽  
C.M. Spence ◽  
J.S. Tudhope

2020 ◽  
Vol 10 (12) ◽  
pp. 4398
Author(s):  
Sofoklis Bouras ◽  
Nikolaos Katsoulas ◽  
Dimitrios Antoniadis ◽  
Ioannis T. Karapanagiotidis

The simultaneous use of crude glycerol and effluent from anaerobic digestate, both wastes derived from the biofuel industry, were tested in the frame of circular economy concept, as potential low-cost nutrient sources for the cultivation of rich in docosahexaenoic acid (DHA) oil microalgae strain Schizochytrium limacinum SR21. Initially, the optimal carbon and nitrogen concentration levels for high S. limacinum biomass and lipids production were determined, in a culture media containing conventional, high cost, organic nitrogen sources (yeast extract and peptone), micronutrients and crude glycerol at varying concentrations. Then, the effect of a culture media composed of crude glycerol (as carbon source) and effluent digestate at varying proportions on biomass productivity, lipid accumulation, proximate composition, carbon assimilation and fatty acid content were determined. It was shown that the biomass and total lipid content increased considerably with varying effluent concentrations reaching 49.2 g L−1 at 48% (v/v) of effluent concentration, while the lipid yield at the same effluent concentration reached 10.15 g L−1, compared to 17.0 g L−1 dry biomass and 10.2 g L−1 lipid yield when yeast extract and peptone medium with micronutrients was used. Compared to the control treatment, the above production was obtained with 48% less inorganic salts, which are needed for the preparation of the artificial sea water. It was shown that Schizochytrium limacinum SR21 was able to remediate 40% of the total organic carbon content of the biofuel wastes, while DHA productivity remained at low levels with saturated fatty acids comprising the main fraction of total fatty acid content. The results of the present study suggest that the simultaneous use of two waste streams from the biofuel industry can serve as potential nutrient sources for the growth of Schizochytrium limacinum SR21, replacing the high cost organic nutrients and up to one half the required artificial sea water salts, but upregulation of DHA productivity through optimization of the abiotic environment is necessary for industrial application, including aqua feed production.


Lipids ◽  
1972 ◽  
Vol 7 (2) ◽  
pp. 90-95 ◽  
Author(s):  
J. B. Saddler ◽  
K. V. Koski ◽  
R. D. Cardwell

1963 ◽  
Vol 8 (2) ◽  
pp. 292-294 ◽  
Author(s):  
H. BARNES ◽  
D. M. FINLAYSON

Desalination ◽  
1973 ◽  
Vol 13 (1) ◽  
pp. 37-51 ◽  
Author(s):  
Chen S.F. ◽  
Chan R.C. ◽  
S.M. Read ◽  
L.A. Bromley
Keyword(s):  

Clay Minerals ◽  
1998 ◽  
Vol 33 (3) ◽  
pp. 483-500 ◽  
Author(s):  
M. Ortega ◽  
I. Palomo ◽  
F. Martinez ◽  
I. Gonzalez

AbstractThe clay mineral associations in the Cretaceous-Tertiary Boundary (KTB) and in the Danian and Maastrichtian levels of sections from the Mediterranean and the Atlantic Domains have been studied. The Mediterranean sections have a single mineral association consisting of smectiteiltite and kaolinite, whereas the Atlantic sections have several associations: illite-chlorite, illite-R1 I-S-kaolinite and illite-R 1 I-S-chlorite. Data are presented relating to the influence of K-feldspars and Fe oxide sphemles on the clay mineral associations. Study of rare-earth elements shows that regional geological factors affect the clay mineralogy of the KTB, examples showing significant anthigenesis in the Mediterranean sections, and important detrital supply in all the Atlantic sections. We propose that the KTB studied in these marine sections is equivalent to the uppermost layer of the two-layered clay unit originating in a cloud of a vapourized bolide. Regional tectonic conditions have been responsible for differences in clay sedimentation in these geological domains and among the stratigraphic sections of the Atlantic Domain.


Author(s):  
J. H. Wickstead

Larvae of Branchiostoma lanceolatum (Pallas), of a late pre-metamorphosis stage and characterized by a bright fluorescent green around the ilio-colonic ring, were taken in the Plymouth area plankton in August 1965.Adults were kept in 0.04% thiouracil to determine the general effect at this concentration. It was lethal over a period of weeks.The larvae were kept in the dark at a constant temperature of 10° C, individu-ally or in pairs, in 0.04%, 0.02%, 0.01%, 0.005% and 0.0025% thiouracil, in saturated solutions and suspensions of thyroxine and triiodothyronine, and in ordinary sea water. Solutions were changed weekly. The flagellate Dunaliella primolecta Butcher was supplied as food.All the larvae metamorphosed at approximately the same time and rate, two exceptions being that 0.04% thiouracil was a more obviously toxic concentration and the thyroxine and triiodothyronine larvae were rather more precocious in their metamorphosis.It is suggested that metamorphosis is a ‘triggered’ process and is self-sustaining. Thus once it has begun it cannot be delayed or accelerated significantly. All the larvae caught were at a stage when this ‘triggering’ had been released.It is considered possible that the metabolism of the larva and the initiation of metamorphosis is controlled by a secretion of the club-shaped gland.INTRODUCTIONThe position of the amphioxides larva has already been discussed (Wick-stead, 1964). No clear demarcation could be made between the usual type of acraniate larva and amphioxides. It was suggested that the amphioxides was a giant larva, a phenomenon not uncommon in oceanic plankton.IntroductionThe position of the amphioxides larva has already been discussed (Wickstead, 1964).


Sign in / Sign up

Export Citation Format

Share Document