Shaoxiu Ma
Biographic Data
| ID | 7996512 |
|---|---|
| NAME | Shaoxiu Ma |
| GIVEN NAMES | Shaoxiu |
| FAMILY NAME | Ma |
| SIGNATURE | MA S |
| AFFILIATIONS | UNSW Sydney |
| ORCID | 0000-0002-3357-4647 |
| VERIFIED | Yes |
| TOTAL WORKS | 5 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 5 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2017 |
| LATEST PUBLICATION YEAR | 2024 |
| H-INDEX | 0 |
Vegetation restoration in dryland with shrub serves as a carbon sink: Evidence from a 13‐year observation at the Tengger Desert of Northern China
Dryland area accounts for approximately 40% of worldwide land area, which plays a significant role in regulating the carbon sequestration capacity of land. Vegetation restoration in drylands adopted to prevent land degradation, and may also serve as a carbon sink in the earlier stage. However, the persistence of the carbon sink for the revegetated ecosystem in drylands is still unknown. Can the well‐established restoration vegetation in dryland a…
Plant community changes determine the vegetation and soil δ 13 C and δ 15 N enrichment in degraded alpine grassland
δ 13 C and δ 15 N are extensively used to understand the biogeochemical mechanisms that moderate ecosystem carbon (C) and nitrogen (N) processes. Little is known about the responses of δ 13 C and δ 15 N to alpine grassland degradation on the Qinghai‐Tibetan Plateau (QTP), which prevents a full understanding of degradation‐induced changes in C and N cycling there. We investigated the vegetation δ 13 C and δ 15 N, soil δ 13 C and δ 15 N, soil prope…
Plant community change mediated heterotrophic respiration increase explains soil organic carbon loss before moderate degradation of alpine meadow
Alpine meadows on the Qinghai‐Tibet Plateau (QTP) store a huge amount of plant and soil carbon (C). The degradation of the alpine meadow has led to a significant loss of soil organic C (SOC), which endangers its weak C sink. The change in heterotrophic respiration was hypothesized as one of the primary biological processes for the SOC loss alongside the degradation of alpine meadow. However, little is known about how land degradation impacts R h …
Warming-induced shift towards forbs and grasses and its relation to the carbon sequestration in an alpine meadow
Global warming is often associated with changes in abiotic factors and the community composition across alpine ecosystems. However, the way that an altered community dynamics affects the ecosystem carbon (C) balance remains unclear. A warming experiment was initiated in 2010 to assess the potential impacts of warming-induced changes in the community composition and how these changes affect the C balance in mountain meadows located in the permafro…
Local land–atmosphere feedbacks limit irrigation demand
Irrigation is known to influence regional climate but most studies forecast and simulate irrigation with offline (i.e. land only) models. Using south eastern Australia as a test bed, we demonstrate that irrigation demand is fundamentally different between land only and land-atmosphere simulations. While irrigation only has a small impact on maximum temperature, the semi-arid environment experiences near surface moistening in coupled simulations o…
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Warming-induced shift towards forbs and grasses and its relation to the carbon sequestration in an alpine meadow
Global warming is often associated with changes in abiotic factors and the community composition across alpine ecosystems. However, the way that an altered community dynamics affects the ecosystem carbon (C) balance remains unclear. A warming experiment was initiated in 2010 to assess the potential impacts of warming-induced changes in the community composition and how these changes affect the C balance in mountain meadows located in the permafro…
Local land–atmosphere feedbacks limit irrigation demand
Irrigation is known to influence regional climate but most studies forecast and simulate irrigation with offline (i.e. land only) models. Using south eastern Australia as a test bed, we demonstrate that irrigation demand is fundamentally different between land only and land-atmosphere simulations. While irrigation only has a small impact on maximum temperature, the semi-arid environment experiences near surface moistening in coupled simulations o…
Plant community changes determine the vegetation and soil δ 13 C and δ 15 N enrichment in degraded alpine grassland
δ 13 C and δ 15 N are extensively used to understand the biogeochemical mechanisms that moderate ecosystem carbon (C) and nitrogen (N) processes. Little is known about the responses of δ 13 C and δ 15 N to alpine grassland degradation on the Qinghai‐Tibetan Plateau (QTP), which prevents a full understanding of degradation‐induced changes in C and N cycling there. We investigated the vegetation δ 13 C and δ 15 N, soil δ 13 C and δ 15 N, soil prope…
Plant community change mediated heterotrophic respiration increase explains soil organic carbon loss before moderate degradation of alpine meadow
Alpine meadows on the Qinghai‐Tibet Plateau (QTP) store a huge amount of plant and soil carbon (C). The degradation of the alpine meadow has led to a significant loss of soil organic C (SOC), which endangers its weak C sink. The change in heterotrophic respiration was hypothesized as one of the primary biological processes for the SOC loss alongside the degradation of alpine meadow. However, little is known about how land degradation impacts R h …
Vegetation restoration in dryland with shrub serves as a carbon sink: Evidence from a 13‐year observation at the Tengger Desert of Northern China
Dryland area accounts for approximately 40% of worldwide land area, which plays a significant role in regulating the carbon sequestration capacity of land. Vegetation restoration in drylands adopted to prevent land degradation, and may also serve as a carbon sink in the earlier stage. However, the persistence of the carbon sink for the revegetated ecosystem in drylands is still unknown. Can the well‐established restoration vegetation in dryland a…
Ecology (5 works) · Environmental Science (5 works) · Biology (4 works) · Climate change (3 works) · Climate change and permafrost (3 works) · Ecosystem (3 works) · Geography (3 works) · Grassland (3 works) · Peatlands and Wetlands Ecology (3 works) · Soil Carbon and Nitrogen Dynamics (3 works)