Variations in the carbon isotope composition of late-Holocene plant macrofossils : A comparison of whole-leaf and cellulose trends
Stable carbon isotope measurements (δ13C) made on Quaternary sequences of terrestrial plant subfossils are frequently used to infer palaeoclimatic trends. However, differential decomposition of individual constituents during incorporation of plant material into lake sediments could influence these interpretations. Therefore, we investigated down-core variations in the carbon isotope composition (δ