Livestock trampling regulates the soil carbon exchange by mediating surface roughness and biocrust cover

Yong-sheng, WU; Li, Xinrong; Jia, Ruibao; Yin, Rui-Ping; Liu, Tiejun

doi:10.1016/j.geoderma.2022.116275

Cited by 5 publications

(3 citation statements)

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“…We found strong evidence that a high intensity of recent livestock grazing was associated with reduced biocrust cover and richness since the previous survey. The trampling effect of livestock is well known to inhibit biocrusts, as organisms are physically crushed, sheared or buried by loose sediment (Wu et al, 2023; Zaady et al, 2016). Not only does trampling directly reduce biocrust cover but also species richness by excluding species that are particularly susceptible to crushing and shearing forces such as fruticose lichens and tall mosses (Concostrina‐Zubiri et al, 2017; Read et al, 2014).…”

Section: Discussionmentioning

confidence: 99%

“…be associated with a decline in biocrust cover and richness than an increase but only for livestock, whose hard hooves are known to trample biocrusts and destabilise the soil surface (Mallen-Cooper et al, 2018;Wu et al, 2023).…”

Section: Introductionmentioning

confidence: 99%

“…We also examined the extent to which livestock and kangaroo grazing intensity has moderated shifts in biocrust abundance and richness. We expected that high recent grazing pressure would be more likely to be associated with a decline in biocrust cover and richness than an increase but only for livestock, whose hard hooves are known to trample biocrusts and destabilise the soil surface (Mallen‐Cooper et al, 2018; Wu et al, 2023).…”

Section: Introductionmentioning

confidence: 99%

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Limited range shifting in biocrusts despite climate warming: A 25‐year resurvey

et al. 2023

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The ranges of many species globally have already shifted to maintain climatic equilibrium in the face of climate change. Biocrusts—soil surface dwelling communities of lichens, bryophytes and microbes—play important functional roles in many ecosystems, particularly in drylands. Compared to better studied animal and plant taxa, dryland biocrusts have different establishment requirements and have never been assessed for historical range shifts. Here, we revisited the sites (N = 204) of a 25‐year‐old biocrust survey across a large area (400,000 km2) of drylands in south‐eastern Australia. We used quadratic models to quantify changes in the climate niches of 15 lichen, eight moss and five liverwort taxa, as well as biocrust cover and richness. Our models showed that the observed climatic niches of most taxa have become hotter and drier in the past quarter century, yet the responses of the vast majority of taxa are consistent with remaining in the same geographic space. A similar pattern was observed at the community level, where the peak of biocrust cover and richness now occurs in a hotter, drier environment. Notable exceptions were the liverwort Riccia lamellosa and lichens in the genera Cladonia and Xanthoparmelia, which showed signs of contraction at their arid range edges. Unlike more mobile taxa, most biocrust species have yet to shift geographically and may already be lagging behind the pace of climate change. One explanation for the mortality lag is that long‐term climate variability in the system is extensive, which may have selected for the ability to withstand multi‐year warm periods as long as there is an eventual return to milder conditions. However, no forecasts of future climate include a return to milder conditions, suggesting there will be an eventual loss of ecosystem multifunctionality at the contracting front. Expansion lags are most likely due to delays in the mortality of competing vascular plants. Synthesis: Our study provides a valuable contribution to the knowledge of range shifts in understudied taxa and highlights a future need to promote the expansion of biocrusts to maintain the provision of ecosystem functions and services across their range.

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