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Grasses (Poaceae) are distributed across the world in broad latitudinal belts and are an important source of C4 biomass in the geological record of soils as well as lake and marine sediments. We examined long-chain leaf wax components of thirty-five C4 grasses of the subfamilies Aristidoideae, Chloridoideae and Panicoideae from the southern African grasslands and savannas and three C3 grasses of the subfamily Pooideae from Peru and Australia and review the relevant botanical, phytogeographic and leaf wax compositional background information. Contents, distribution patterns and molecular stable carbon isotopic compositions of long-chain n-alkanes (n-C27 to n-C35) and n-alkan-1-ols (n-C22 to n-C32) were used to estimate the chemotaxonomic relevance of wax signatures of whole plants, separately for different subfamilies and for members of the three C4 subtypes (NADP–ME, NAD–ME and PCK). Two grass species were separated into flower heads, leaves and stems and the parts analysed separately. Grass flowers contain remarkable amounts of short-chain n-alkanes, which may have a significant influence on the chemical signature of the whole plant, whereas n-alkanol distribution patterns exhibit no systematics. The stable carbon isotopic composition of both biomarker types in different plant parts is remarkably uniform. Chemotaxonomic differentiation was not possible on a species level based on whole plant samples, but was more successful for averages of subfamily and photosynthetic subtype data. Wax signatures of C4 grasses are generally distinguishable from those of C3 species by heavier isotopic values, higher contents of n-C31 and n-C33 alkanes and the abundance of the n-C32 n-alkanol, which is largely absent in C3 grass waxes. Especially the waxes of the NAD–ME and PCK C4-subtype grasses, which thrive in extremely arid tropical and subtropical areas, contain high relative amounts of longer-chain n-alkane homologues. The chemical classification on a subfamily level, which is in agreement with previously reported subfamilial phylogeny of grasses, implies an evolutionary wax adaptation of C4 grasses to warm and arid habitats. Our results confirm the validity of the contents, distribution patterns and molecular stable carbon isotopic compositions of long-chain n-alkanes and alkan-1-ols as indirect proxies of continental climate conditions in environmental studies of the tropics. |
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