Guiyao Zhou

Dr. Guiyao Zhou

orcid

Research Focus & Metrics

Academic Career Length

11Years (2016-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

View All Publications
7 June 2018 in Plant, Cell & Environment
Verified
Journal Article
Closed access
PDF file
GZGuiyao Zhou
Guiyao Zhou
XZXuhui Zhou
Xuhui Zhou
YNYuanyuan Nie
Yuanyuan Nie
SBShahla Hosseini Bai
Shahla Hosseini Bai
LZLingyan Zhou
Lingyan Zhou
YFYuling Fu
Yuling Fu

10 October 2024 in Nature Communications
Verified
Journal Article
Open access
PDF file
JTJialing Teng
Jialing Teng
RHRuixing Hou
Ruixing Hou
JDJennifer A. J. Dungait
Jennifer A. J. Dungait
GZGuiyao Zhou
Guiyao Zhou
YKYakov Kuzyakov
Yakov Kuzyakov
MDManuel Delgado-Baquerizo
Manuel Delgado-Baquerizo
Climate warming threatens global food security by exacerbating pressures on degraded soils under intensive crop production. Conservation agriculture is promoted as a sustainable solution that improves soil health and sustains crop yields in a changing climate, but these benefits may be affected by long-term warming. Here, we investigate the effects of conservation agriculture compared to conventional agriculture on 17 soil properties, microbial diversity and crop yields, during eight-years’ experimental warming. An overall positive effect of warming on soil health over time under conservation agriculture is characterized by linear increases in soil organic carbon and microbial biomass carbon. Warming-triggered shifts in microbial biomass carbon and fungal diversity (saprogen richness) are directly linked to a 9.3% increase in wheat yields over eight years, but only under conservation agriculture. Overall, conservation agriculture results in an average 21% increase in soil health and supports similar levels of crop production after long-term warming compared to conventional agriculture. Our work provides insights into the potential benefits of conservation agriculture for long-term sustainable food production because improved soil health improves resilience to the effects of climate warming.

1 September 2019 in Ecological Indicators
Verified
Journal Article
Closed access
AHAn Huang
An Huang
YXYueqing Xu
Yueqing Xu
PSPiling Sun
Piling Sun
GZGuiyao Zhou
Guiyao Zhou
CLChao Liu
Chao Liu
HWHui Wang
Hui Wang

1 May 2023 in Nature Geoscience
Verified
Journal Article
Closed access
PDF file
DEDavid J. Eldridge
David J. Eldridge
Emilio GuiradoEmilio Guirado
Emilio Guirado
PRPeter B. Reich
Peter B. Reich
Raúl Ochoa-HuesoRaúl Ochoa-Hueso
Raúl Ochoa-Hueso
MVMiguel Berdugo Vega
Miguel Berdugo Vega
MDManuel Delgado-Baquerizo
Manuel Delgado-Baquerizo

20 August 2022 in Nature Communications
Verified
Journal Article
Open access
PDF file
LZLingyan Zhou
Lingyan Zhou
XZXuhui Zhou
Xuhui Zhou
YHYanghui He
Yanghui He
YFYuling Fu
Yuling Fu
ZDZhenggang Du
Zhenggang Du
MTMadhav P. Thakur
Madhav P. Thakur
Biomass allocation in plants is fundamental for understanding and predicting terrestrial carbon storage. Yet, our knowledge regarding warming effects on root: shoot ratio (R/S) remains limited. Here, we present a meta-analysis encompassing more than 300 studies and including angiosperms and gymnosperms as well as different biomes (cropland, desert, forest, grassland, tundra, and wetland). The meta-analysis shows that average warming of 2.50 °C (median = 2 °C) significantly increases biomass allocation to roots with a mean increase of 8.1% in R/S. Two factors associate significantly with this response to warming: mean annual precipitation and the type of mycorrhizal fungi associated with plants. Warming-induced allocation to roots is greater in drier habitats when compared to shoots (+15.1% in R/S), while lower in wetter habitats (+4.9% in R/S). This R/S pattern is more frequent in plants associated with arbuscular mycorrhizal fungi, compared to ectomycorrhizal fungi. These results show that precipitation variability and mycorrhizal association can affect terrestrial carbon dynamics by influencing biomass allocation strategies in a warmer world, suggesting that climate change could influence belowground C sequestration.

14 August 2023 in Global Change Biology
Verified
Journal Article
Open access
SLShengen Liu
Shengen Liu
CPCésar Plaza
César Plaza
Raúl Ochoa-HuesoRaúl Ochoa-Hueso
Raúl Ochoa-Hueso
CTChanda Trivedi
Chanda Trivedi
JWJuntao Wang
Juntao Wang
MDManuel Delgado-Baquerizo
Manuel Delgado-Baquerizo
The decomposition of litter and the supply of nutrients into and from the soil are two fundamental processes through which the above‐ and belowground world interact. Microbial biodiversity, and especially that of decomposers, plays a key role in these processes by helping litter decomposition. Yet the relative contribution of litter diversity and soil biodiversity in supporting multiple ecosystem services remains virtually unknown. Here we conducted a mesocosm experiment where leaf litter and soil biodiversity were manipulated to investigate their influence on plant productivity, litter decomposition, soil respiration, and enzymatic activity in the littersphere. We showed that both leaf litter diversity and soil microbial diversity (richness and community composition) independently contributed to explain multiple ecosystem functions. Fungal saprobes community composition was especially important for supporting ecosystem multifunctionality (EMF), plant production, litter decomposition, and activity of soil phosphatase when compared with bacteria or other fungal functional groups and litter species richness. Moreover, leaf litter diversity and soil microbial diversity exerted previously undescribed and significantly interactive effects on EMF and multiple individual ecosystem functions, such as litter decomposition and plant production. Together, our work provides experimental evidence supporting the independent and interactive roles of litter and belowground soil biodiversity to maintain ecosystem functions and multiple services.