Abstract

PurposeGrasslands play a crucial role in offsetting greenhouse gas emissions and mitigating climate change. A moderate change in grassland carbon (C) and nitrogen (N) stocks may substantially alter the global C and N cycle and thereby influence climate. But how grassland C and N stocks respond to grazing and slope position remains uncertain. This research investigates how C and N stocks respond to cattle grazing along a landscape slope.Materials and methodsWe studied a grassland that has been grazed by cattle at four cattle stocking rates (0, 1.2, 2.4, and 4.8 animal unit months (AUM) ha−1) since 1949, representing control (CK), light (L), heavy (H), and very heavy (VH) grazing intensities, respectively. Samples were taken from the top and bottom slope positions within each paddock (only the top position in CK); C and N stocks in soil, roots, litter, and standing crop were estimated. Soil C and N stocks were estimated based on equivalent mass (1500 Mg ha−1). Root C and N stocks were estimated to the depth of 15 cm.Results and discussionAll parameters, except for litter N stock and standing crop C stock, significantly responded to the interaction of grazing intensity and slope position. In the bottom position, soil and standing crop C and N stocks as well as litter C stock were higher with the L treatment than with VH, while no significant differences were found among the three grazed treatments for root C and litter N stocks. In the top position, soil and root C and N stocks were higher with the VH treatment than with L, whereas litter C and N stocks and standing crop C stock were lower with VH than with L.ConclusionsOur results provide evidence that slope position plays an important role in regulating the response of C and N stocks to grazing and may need to be considered when developing optimal grazing management strategies.

Highlights

  • Grasslands play a crucial role in sequestering C due to their vast geographic distribution around the world (Conant et al 2001) and high potential to absorb C from the atmosphere (Lal 2004)

  • Soil and standing crop C and N stocks as well as litter C stock were higher with the L treatment than with very heavy (VH), while no significant differences were found among the three grazed treatments for root C and litter N stocks

  • Soil and root C and N stocks were higher with the VH treatment than with L, whereas litter C and N stocks and standing crop C stock were lower with VH than with L

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Summary

Introduction

Grasslands play a crucial role in sequestering C due to their vast geographic distribution around the world (Conant et al 2001) and high potential to absorb C from the atmosphere (Lal 2004). It has been estimated that grasslands account for 20% of the total global C in both soil and vegetation (Adams et al 1990) and the C sequestration rate in grassland soils is perhaps as much as 0.5 Pg C year−1 (Scurlock and Hall 1998). This indicates that even a moderate change in grassland C and N stocks may substantially alter the global C and N cycle. There is a need to understand how grassland C and N stocks change with human disturbances. Herbivory can directly affect the growth, survival, and fitness of most plants,

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