F
F.T. Gillan
Researcher at University of Melbourne
Publications - 7
Citations - 800
F.T. Gillan is an academic researcher from University of Melbourne. The author has contributed to research in topics: Polyunsaturated fatty acid & Monobasic acid. The author has an hindex of 6, co-authored 7 publications receiving 772 citations.
Papers
More filters
Journal ArticleDOI
Microbial lipids of an intertidal sediment—I. Fatty acids and hydrocarbons
TL;DR: In this article, a detailed study was made of the solvent extractable monocarboxylic, dicarboxylated and hydroxylated fatty acids and n-alkanes in a surface intertidal sediment, and the distributions compared to microorganisms cultured from the sediment.
Journal ArticleDOI
A comparison of lipid components of the fresh and dead leaves and pneumatophores of the mangrove Avicennia marina
TL;DR: This resistance to degradation shown by the cutin derived acids (α,ω-dibasic, ω-hydroxy and long-chain monobasic acids) relative to the cellular and wax derived lipids may allow these cutin components to be used as quantitative markers of A. marina in mangrove associated sediments.
Journal ArticleDOI
Early diagenesis of phytyl esters in a contemporary temperate intertidal sediment
TL;DR: In this paper, a sediment core for hydrolysed chlorins (acidic chlorins e.g. pheophorbide a) and free, bound and esterified alcohols have been performed and the results have been interpreted in terms of input and sedimentary interconversions.
Journal ArticleDOI
trans-Monounsaturated Acids in a Marine Bacterial Isolate.
TL;DR: A sedimentary bacterial isolate has been shown to contain trans-monounsaturated fatty acids, implying that the trans-acids which have been reported in recent sediments could derive, in whole or part, from direct bacterial input.
Journal ArticleDOI
Kerogen precursors: chemical and biological alteration of lipids in the sedimentary surface layer
TL;DR: The starting point for the formation of a sediment is not the initial biological inputs to a sediment but rather those organic molecules which survive the active upper 1 to 2 cm of surface sediment where biological diagenesis is most marked as discussed by the authors.