Mid-late Holocene vegetation response to climatic drivers and biotic disturbances in the Banni grasslands of western India

• Published in: Palaeogeography, palaeoclimatology, palaeoecology palaeoclimatology, palaeoecology, 2017-11, Vol.485, p.869-878
• Main Authors: Pillai, Anusree A.S., Anoop, Ambili, Sankaran, Mahesh, Sanyal, Prasanta, Jha, Deepak K., Ratnam, Jayashree
• Format: Article
• Language: English
• Subjects: Charcoal; Dung fungal spore; Isotope; Monsoon; Paleoecology; Tropical grassland
• ISSN: 0031-0182; 1872-616X
• DOI: 10.1016/j.palaeo.2017.07.036

Tropical grasslands and savannas are globally extensive, and are of significant environmental, economic, and ecological importance. These ecosystems are anticipated to be particularly sensitive to future changes in climate, and understanding how these systems have responded to climatic changes in the past can provide us with insights into their potential responses to future global change. In this study, the temporal dynamics of C3-C4 vegetation changes in response to changes in moisture availability, local fire events and changing levels of herbivory in a summer-rainfall region of Western India are reconstructed for the past ~4600calyrBP. Paleodata such as stable carbon isotope of bulk organic matter (δ13Corg), oxygen isotope from carbonate shells (δ18Oshell), macro-charcoal and herbivore dung fungal spores are reported from the retrieved cores of two wetland sites located in the Banni grasslands of Western India. Results show that vegetation in the Banni was composed mostly of C3 vegetation from ~4600 to ~2500calyrBP, after which there was a decline in C3 vegetation. From the late-Holocene to the present, there was a mix of both C3 and C4 vegetation, with C4 grasses being more abundant in the ecosystem. These shifts were coincident with rainfall changes from more mesic conditions during ~4600 to ~2500calyrBP to more arid conditions towards the present as indicated by δ18Oshell isotope data. The period of increase in C4 vegetation also coincides with a period of increased biotic disturbances in the ecosystem, particularly fire. Given the current scenarios of global warming, recurrent drought events and increased anthropogenic use of similar ecosystems, such studies can provide us insights into potential future trajectories of these ecosystems. •C3 – C4 vegetation changes in a tropical savanna through mid-late Holocene.•Climatic and biotic disturbance drivers of vegetation was also studied.•More C3 vegetation, rainfall and lower levels of local fire and herbivory in mid Holocene•More C4 vegetation, aridity and higher but fluctuating levels of biotic disturbances until ca. 1000calyrBP•A slight increase in C3 vegetation, rainfall and a decrease in local fire towards the present