User:Lalatheplatypus/Desmosterol

Desmosterol (Cholesta-5,24-dien-3β-ol) is a lipid present in the membrane of phytoplankton. These are autotrophic organisms which undergo photosynthesis and rely on sunlight for energy, living in shallower waters. Structurally, desmosterol has a similar backbone to cholesterol, with the exception of an additional double bond in the structure of desmosterol. Biologically, the similarity can be seen through the synthesis of cholesterol in the human body, as desmosterol is the immediate precursor to cholesterol.



Background
Desmosterol is classified as a cholestadienol, a subgroup of a wider known group of sterols, which are organic compounds naturally occurring in eukaryotes. The presence of desmosterol in oceans and lakes has potential to diagnose anoxic conditions and for studying trends in steroid chemistry during the early stages of diagenesis. Desmosterol has been found in samples of Rhizosolenia setigera Brightwell in Western Svalbard and from surface sediment off the Peruvian Shelf sediment-water interface.

Desmosterol was first described and isolated in 1955 from chick embryo sterol with a 2% yield and postulated as being a biological precursor to cholesterol by Stokes et al. The first known isolation of desmosterol in invertebrates was published in 1957 by Fagerlund and Idler. This new sterol was isolated in large amounts from balanus glandula, a barnacle species found on the North American Pacific coast. Additionally, small amounts of desmosterol have been found in other crustaceans such as lobster and shrimp in the homarus americanus and pandalus borealis species. This strengthens the conclusion that desmosterol must be created exogenously as crustaceans have not been seen to biosynthesise sterols.

Biological Occurence
Desmosterol has been largely found within a large population of marine invertebrates. Major sources include: barnacles, red algae , annelida , thalassiosirales , and molluscs. This has led to the idea of an exogenous origin of desmosterol in phytoplankton. Desmsterol was identified in red algae: Laurencia pinnatifida, Polusiphonia nigrescens, Porphyra purpurea, and dulse (Rhodymenia palmata), in 1967, after no previous identification.

In the 1968 paper by Idler, Saito and Wiseman, dulse samples were analysed and the sterols present were determined by gas liquid chromatography. Samples were collected near Grand Manan Island, New York in 1964 and 1965 gave a significant difference in presence of desmosterol, with the latter collected sample with over 70% desmosterol. The samples collected in June and July of 1967 showed a smaller difference, of 30%.



Biosynthesis
There are two major pathways for cholesterol biosynthesis, being the Kandutsch-Russell and Bloch pathways. The Bloch pathway, named after Konrad Bloch, occurs naturally alongside the mevalonate pathway in humans within the cell. The discovery of this pathway led to Bloch, joint with Feodor Lynen, to receive a Nobel Prize in Physiology or Medicine in 1964. The award was awarded “for their discoveries concerning the mechanism and regulation of the cholesterol and fatty acid metabolism”.



Preservation
Desmosterol has been seen to be present in marine sponges as a biomarker. However, bacterial symbiont Sterol 24-C-methyltransferases is capable of the alkylation of desmosterol to other sponge biomarkers, 24-isopropenylcholesterol, and 24-isopropylidenecholesterol. It should be noted there is insignificant data which shows that desmosterol has good preservation potential.

Use as a Biomarker
Desmosterol is important through its use as a biomarker for the Chaetoceros calcitrans and R. setigera and N. closterium diatoms as well as Rhodophyceae. However, desmosterol has potential to be used as a taxonomic marker for diatoms where it exists as the dominant sterol, such as Rhizosolenia.

Peruvian Shelf
Diatoms and Silicoflagellates are classes of phytoplankton present in sedimentary material from the sediment water interface in the Peruvian Shelf region. Mineralogical analysis of these suggested large volumes of phytoplankton. Researchers at the University of Bristol examined the sterol composition of these sedimentary rocks which have gone through oxygen depletion, leading to anoxic conditions. These conditions have enhanced preservation of lipids present during the time of formation, around 1 year prior, and limited degradation of these compounds.

Measurement techniques
Desmosterol has seen to be identified most commonly through chemical constants, ozonolysis, infrared, NMR, and mass spectrometry techniques. The use of thin-layer and gas-liquid chromatography to measure desmosterol is less common from the development of more advanced techniques.

GC-MS
Samples from water sources are first extracted and partially purified before analysis. Sterols are commonly first derivatised after purification. Lipid extracts can be separated into their fragments by ionisation using Gas Chromatography followed by Mass Spectroscopy analysis. Desmosterol has a characteristic m/z peak at 384, seen in the mass spectra.

Ozonolysis
Desmosterol has been identified through ozonolysis of the sample, with the ozonolysis product of desmosterol having a melting point of 128°C, and an Rf value of 0.31 with paper-chromatography with n-hexane and N,N-dimethyl formamide. The ozonolysis product also has ratios C: 45.68; H: 4.45; N: 23.21.