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Brassicasterol
IUPAC name	24-methyl cholest-5,22-dien-3β-ol
Other names	brassicasterol (3β,22E)-ergosta-5,22-dien-3-ol 24β-methylcholesta-5,22-dien-3 beta-ol ergosta-5,22-dien-3β-ol
Identifiers
CAS number	474-67-9
SMILES	CC(C)C(C)C=CC(C)C1(C2(C)(C(CC1) C3(C(CC2)C4(C(=CC3)CC(O)CC4)(C))))
Properties
Molecular formula	C28H46O
Molar mass	398.67 g/mol
Appearance	white solid
Density	? g/ml, solid at room temperature
Melting point	150-151°C
Solubility in water	? mg/l
Hazards
Flash point	non-flammable
Related Compounds
Related Sterols	cholesterol β-sitosterol campesterol stigmasterol
Except where noted otherwise, data are given for materials in their standard state (at 25 °C, 100 kPa) Infobox disclaimer and references

Brassicasterol (24-methyl cholest-5,22-dien-3β-ol) is a 28 carbon sterol synthesised by several unicellular algae (phytoplankton) and some terrestrial plants e.g. oilseed rape. This compound has frequently been used as a biomarker for the presence of (marine) algal matter in the environment.

Contents 1 Chemical Properties 1.1 Solubility 1.2 Degradation 1.3 Chemical Analysis 2 Formation and Occurrence 2.1 Algal Sources 2.2 Other Sources 3 Use as a Tracer for Marine Algae 3.1 Brassicasterol / Cholesterol Ratio 3.2 Multivariate Analysis 4 References

Brassicasterol has a low water solubility and consequently a high octanol – water partition coefficient (Kow = ??). This means that in most environmental systems, brassicasterol will be associated with the solid phase.

In anaerobic sediments and soils, brassicasterol is stable for many hundreds of years enabling it to be used as an indicator of past algal production (see below).

Since the molecule has a hydroxyl (-OH) group, it is frequently bound to other lipids including glycerols; most analytical methods, therefore, utilise a strong alkali (KOH or NaOH) to saponify the ester linkages. Typical extraction solvents include 6% KOH in methanol. The free sterols are then separated from the polar lipids by partitioning into a less polar solvent (e.g. hexane). Prior to analysis, the hydroxyl group is frequently derivatised with BSTFA (bis-trimethyl silyl trifluoroacetamide) to replace the hydrogen with the less exchangeable trimethylsilyl (TMS) group. Instrumental analysis is frequently conducted on Gas Chromatograph (GC) with either a Flame Ionisation Detector (FID) or Mass Spectrometer (MS). The mass spectrum for the TMS ether of brassicasterol can be seen in the Figure.

Brassicasterol is formed in plants from the isoprenoid squalene through campesterol as an intermediate. A list of the algae in which brassicasterol has been identified is shown below together with approximate composition (Data from an excellent review by Volkman, 1986).

Sterol content of selected dinoflagellates (as percentage). Data from Volkman, 1986

Species	A	B	C	D	E	F	G	H	others
Gonyaulax spp	100	0	0	0	0	0	0	0	0
Peridinium foliaceum	100	0	0	0	0	0	0	0	0
Peridinium foliaceum	80	20	0	0	0	0	0	0	0
Gonyaulax diegensis	39	0	0	0	0	0	0	29	32
Pyrocystis lunula	76	6	0	2	1	0	0	0	15
Gonyaulax polygramma	36	1	0	9	7	0	0	0	47
Gymnodinium wilczeki	26	39	0	35	1	0	0	0	0
Glenodinium hallii	8	50	0	0	0	42	0	0	0
Noctiluca milaris	0	1	1	5	73	0	6	0	14
Gymnodinium simplex	0	0	0	0	53	0	0	0	47
Prorocentrum cordatum	7	0	0	0	5	0	63	0	25

A = cholesterol

B = campesterol

C = sitosterol

D = 22-dehydrocholesterol ((22E)-cholesta-5,22-dien-3β-ol)

E = BRASSICASTEROL

F = stigmasterol

G = 24-methylene cholesterol

H = fucosterol

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The principal source of brassicasterol in the environment is from marine algae. Its relatively high concentration and stability allows it to be used in the assessment of the origin of organic matter in samples, especially sediments.

The concentration of brassicasterol in a core sample from Loch Striven, Scotland. Highest values may be seen in the top sections of the sediment which decrease with depth. However, the cholesterol behaves similarly and the ratio brassicasterol / cholesterol is fairly uniform at all depths indicating either a comparable degradation rate with no change in source or different degradation rates and a change in source.

Multivariate Statistical Analyses such as Principal Component Analysis of a range of lipid biomarkers (e.g. other sterols, fatty acids and fatty alcohols) enable identification of compounds that have similar origins or behaviour. An example can be seen in the loadings plot for sediment samples from the Mawddach Estuary, Wales.

The location of brassicasterol in this figure (shown in red) indicates that the distribution of this compound is similar to that of the short chain fatty acids and alcohols which are known to be of marine origin. The terrestrially derived biomarkers such as β-sitosterol are on the opposite side of the figure and are mutually exclusive.

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