Pentacyclic triterpene methyl ethers in recent lacustrine sediments (Lagoa do Caçó, Brazil)
Section snippets
Introduction and setting
Since the isolation of isoarborinol from the Messel Oil Shale (Albrecht and Ourisson, 1969), the literature has been continuously enriched with information on new pentacyclic triterpenes which have been used in petroleum exploration or palaeoenvironmental studies (Cranwell, 1984). These compounds comprise higher plant triterpenes (e.g., oleanane, lupane and ursane derivatives) which occur widely in the plant kingdom in the free form or bound to glycosyl or phenolic moieties through a functional
Sediment samples
The context and sample handling have been described (Jacob et al., 2004a). Briefly, a core (MA98-3; 6 m long) was divided into two main intervals. The lower (ca. 3 m long), which dates back to the end of the LGM, consists of fine-grained sands and silts. The upper half (ca. 3 m long), consisting of organic matter-rich silts, is divided into greenish-brown organic silts (Late Glacial) and black organic silts (Holocene). Two samples, which best illustrate the distribution of PTMEs, were selected
Results
Total extract yields ranged between 0.5 and 4.2 mg g−1 sediment. The neutral fraction afforded between 0.4 and 3.5 mg g−1 sediment. The dominant compounds in this fraction were PTMEs and hopanoids. In total, at least sixteen compounds were distinguished using GC–MS. Two examples of the distribution of these compounds in Lagoa do Caçó sediments are shown in Fig. 2 together with a reconstructed total ion current (TIC) trace for reference compounds.
In total, 5 out of the 16 compounds were identified
Discussion
To our knowledge, the only previous record of methoxy triterpenes in geological samples was made by Ries-Kautt (1986), who identified in soils one compound displaying a similar mass spectrum to that of fern-9(11)-en-3β-ol ME and another unidentified one that could be related to taraxer-14-en-3β-ol ME.
Conclusions
The Quaternary filling of Lagoa do Caçó afforded a wide range of pentacyclic triterpene methyl ethers. These compounds dominate the neutral solvent-extractable fraction. The identity of five has unambiguously been assigned with available reference compounds. Based on an inventory of plants from which PTMEs have been isolated, Gramineae that grew in the watershed at the time of sediment deposition appear as the most probable source. The presence of PTMEs in Lagoa do Caçó sediments attests to
Acknowledgements
Professor R.M. Smith (Loughborough University, UK), Professor H.E. Connor (University of Canterbury, NZ) and Professor G. Eglinton (Bristol University, UK) are greatly acknowledged for providing reference compounds and valuable discussions about chemotaxonomy. The authors thank Professor G. Bouchoux (Ecole Polytechnique, France), Dr. P. Metzger (Ecole de Chimie de Paris, France) and Professor B. Simoneit (Oregon State University, US) for useful discussions on mass spectra interpretation. Dr. B.
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