| Affiliation: | 1. Institute for Peat and Mire Research, State Environmental Protection Key Laboratory of Wetland Ecology and Vegetation Restoration, Northeast Normal University, Changchun, China;2. National Research Center for Geoanalysis, Chinese Academy of Geological Sciences, Beijing, China;3. Department of Geography, Ohio University, Athens, Ohio, USA;4. Surface Waters – Research and Management, Eawag, Swiss Federal Institute of Aquatic Science and Technology, Dübendorf, Switzerland Department of Earth Sciences, ETH Zürich, Zürich, Switzerland;5. College of Urban and Environmental Science, Peking University, Beijing, China;6. College of Resource and Environment Science, Hunan Normal University, Changsha, China;7. School of Resources Environment and Tourism, Anyang Normal University, Anyang, China;8. School of Life Science, Jilin Normal University, Siping, China |
| Abstract: | Ecological responses to past climate change as determined from palaeorecords offer insights into responses that may accompany future climate change. In arid and semi-arid lands, the interactions between regional vegetation and climate change are not yet well understood, partly due to a lack of suitable palaeovegetation proxies that can provide accurate and continuous tracers for past vegetation dynamics. To gain a better understanding of long-term vegetation dynamics, this study employs a multiproxy approach applied to sand-palaeosol sediments of northeastern China's Songnen grasslands. Phytolith analyses and data on the stable carbon isotope composition (δ13C) of organic matter are used to reconstruct palaeovegetation composition, namely, the changing abundance of C3 and C4 species, whereas a geochemical weathering index (Fed/Fet ratios) tracks past East Asian summer monsoon (EASM) intensity. The phytolith assemblages and indices and δ13C of the soil indicate that C4 species' abundance has been increasing in the Songnen grasslands since the mid-Holocene, although C3 vegetation is still dominant. Statistically significant negative correlations between the δ13C data and Fet/Fed ratios suggest that continuous weakening of the EASM since the mid-Holocene may be responsible for the 13C-enrichment of the sediments in the Songnen grasslands. Field vegetation surveys, modern topsoil phytoliths and δ13C calibration data indicate that the expansion of C4 species since the mid-Holocene is mainly due to their ability to cope with aridity when growing season temperature is not undergoing a significant decrease. Future precipitation decreases in arid and semi-arid lands should make C4 species more competitive in the grasslands of northeastern China. Highlights - A continuous grassland landscape history is reconstructed from a sand-palaeosol sequence via phytolith analysis.
- Multiple independent approaches were used to reconstruct past EASM intensity and palaeovegetation patterns.
- Phytolith and δ13C analyses indicate an increase in C4 species since the mid-Holocene.
- Aridification drives the increase in C4 species within the grassland ecosystem.
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