Isoarborinol

Isoarborinol is a triterpenoid ubiquitously produced by angiosperms and is thus considered a biomarker for higher plants. Though no isoarborinol-producing microbe has been identified, isoarborinol is also considered a possible biomarker for marine bacteria, as its diagenetic end product, arborane, has been found in ancient marine sediments that predate the rise of plants. Importantly, isoarborinol may represent the phylogenetic link between hopanols and sterols. Isoarborinol is a triterpenoid ubiquitously produced by angiosperms and is thus considered a biomarker for higher plants. Though no isoarborinol-producing microbe has been identified, isoarborinol is also considered a possible biomarker for marine bacteria, as its diagenetic end product, arborane, has been found in ancient marine sediments that predate the rise of plants. Importantly, isoarborinol may represent the phylogenetic link between hopanols and sterols. Isoarborinol is a pentacyclic triterpenoid, a class of 30-carbon isoprenoid compounds commonly found in higher plants. It is primarily a hydrocarbon molecule composed of four cyclohexane rings, one cyclopentane ring, six methyl groups, one alcohol group and one isopropyl group. It is structurally similar to plant cyclics in the lupenoid series (including lupeol, betulin and lupane), primarily differing in the position of the isobutyl functional group (located on C21 of the cyclopental ring for isoarborinol, and on C19 for the lupenoids). Isoarborinol likely serves as a fluidity-buffering component of biological membranes, similar to sterols and hopanols. The known distribution of isoarborinol in extant organisms is predominantly limited to a few angiosperms (e.g., the Gramineae family), which led many to view isoarborinol as a biomarker for higher plants. In the 1990s, a series of papers published by Verena Hauke and colleagues presented compelling evidence for the existence of isoarborinol during the Permian and Triassic periods based on detection of arborane (the diagenetic product of isoarborinol) in ancient sediments. These geological periods significantly predate the late-Jurassic first appearance of angiosperms, precluding the possibility that isoarborinol was produced by higher plants. Furthermore, the arborane compounds detected had carbon isotopic signatures inconsistent with plant origin, and arborane was additionally isolated from lacustrine sediments that lacked angiosperms. Taken together, these observations support a microbial origin for isoarborinol, though no isoarborinol-producing microbe has yet been found. However, the marine heterotrophic bacterium Eudoraea adriatica was discovered to make adriaticol and eudoraenol, two isomers of isoarborinol, suggesting that an extant isoarborinol producer may exist. The enzyme responsible for making isoarborinol may represent the evolutionary link between the hopanol-producing enzymes in bacteria and the sterol-producing enzymes in eukaryotes. These enzymes are part of the class of terpene cyclases, which cyclize either squalene or oxidosqualene into four- or five-membered ring compounds through pathways that proceed through different structural conformations (all-chair or chair-boat-chair). Each terpene cyclase uses a different combination of these aspects to produce the final polycyclic triterpenoid compound, leading to great variety in the pathways of polycyclic triterpenoid production. Squalene-hopene cyclase (SHC) synthesizes hopanols and is generally assumed to have evolved before the sterol-producing enzyme oxidosqualene cyclase (OSC). Whereas SHC folds squalene into a five-membered ring via an all-chair conformation intermediate, OSC folds oxidosqualene into a four-membered ring via a chair-boat-chair conformation. Isoarborinol cyclase uses a combination of these aspects, cyclizing oxidosqualene into a five-membered ring via a chair-boat-chair conformation. Given the apparent intermediate nature of its pathway (between those used by SHC and OSC), isoarborinol cyclase has been proposed to represent the enzymatic intermediate of the evolutionary transition from SHC to OSC. However, phylogenetic analyses of the evolutionary relationships between terpene cyclases suggest that SHC and OSC diverged from a common ancestor, which renders the evolutionary significance of isoarborinol cyclase unclear. Though no extant microbe is known to produce isoarborinol, the discovery of eudoraenol synthase (which produces isoarborinol-like lipids through a similar pathway used by isoarborinol cyclase) in E. adriatica opens the door for future investigations into the mechanisms of polycyclic triterpenoid biomarker synthesis and the phylogenetic relationships between the enzymes involved.