Paleovegetation reconstruction using δ 13 C of Soil Organic Matter

Abstract. The relative contributions of C 3 and C 4 plants to vegetation at a given locality may be estimated by means of δ 13 C of soil organic matter. This approach holds a great potential for paleoecological reconstruction using paleosols. However, two main uncertainties exist, which limits the accuracy of this application. One is δ 13 C-enrichment as the plant carbon becomes incorporated into soil organic matter. The other is due to environmental influences on δ 13 C of plants. Two types of data were collected and analyzed with an objective of narrowing the error of paleovegetation reconstruction. First, we investigated δ 13 C variations of 557 C 3 and 136 C 4 plants along a precipitation gradient in North China. A strong negative correlation is found between the δ 13 C value of C 3 plants averaged for each site and the annual precipitation with a coefficient of −0.40‰/100mm, while no significant coefficients were found for C 4 plants. Second, we measured δ 13 C of soil organic matters for 14 soil profiles at three sites. The isotopic difference between vegetation and soil organic matter are evaluated to be 1.8‰ for the surface soil and 2.8‰ for the soil at the bottom of soil profiles. We conducted a sample reconstruction of paleovegetation at the central Chinese Loess Plateau during the Holocene and the Last Glacial (LG), and conclude that, without corrections for δ 13 C-enrichment by decomposition, the C 4 abundance would be overestimated. The importance and uncertainties of other corrections are also discussed.