Community-weighted mean traits but not functional diversity determine the changes in soil properties during wetland drying on the Tibetan Plateau
Climate change and human activities have caused a shift in vegetation composition and soil biogeochemical cycles of alpine wetlands on the Tibetan Plateau. The primary goal of this study was to test for associations between community-weighted mean (CWM) traits, functional diversity, and soil propert...
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doaj-13ca2db9f4f245508268b0c90e4a5b382020-11-24T22:19:26ZengCopernicus PublicationsSolid Earth1869-95101869-95292017-02-018113714710.5194/se-8-137-2017Community-weighted mean traits but not functional diversity determine the changes in soil properties during wetland drying on the Tibetan PlateauW. Li0H. E. Epstein1Z. Wen2J. Zhao3J. Jin4G. Jing5J. Cheng6G. Du7State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Northwest A&F University, Yangling 712100, ChinaDepartment of Environmental Sciences, University of Virginia, 291 McCormick Road, Charlottesville, VA 22904-4123, USAState Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Northwest A&F University, Yangling 712100, ChinaCollege of Animal Science and Technology, Northwest A&F University, Yangling 712100, ChinaState Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Northwest A&F University, Yangling 712100, ChinaInstitute of Soil and Water Conservation of Chinese Academy of Sciences & Ministry of Water Resource, Yangling 712100, ChinaState Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Northwest A&F University, Yangling 712100, ChinaSchool of Life Sciences, Lanzhou University, Lanzhou 730000, ChinaClimate change and human activities have caused a shift in vegetation composition and soil biogeochemical cycles of alpine wetlands on the Tibetan Plateau. The primary goal of this study was to test for associations between community-weighted mean (CWM) traits, functional diversity, and soil properties during wetland drying. We collected soil samples and investigated the aboveground vegetation in swamp, swamp meadow, and typical meadow environments. Four CWM trait values (specific leaf area is SLA, leaf dry matter content is LDMC, leaf area is LA, and mature plant height is MPH) for 42 common species were measured across the three habitats; three components of functional diversity (functional richness, functional evenness, and functional divergence) were also quantified at these sites. Our results showed that the drying of the wetland dramatically altered plant community and soil properties. There was a significant correlation between CWM of traits and soil properties, but not a significant correlation between functional diversity and soil properties. Our results further showed that CWM-LA, CWM-SLA, and CWM-LDMC had positive correlations with soil readily available nutrients (available nitrogen, AN; available phosphorus, AP), but negative correlations with total soil nutrients (soil organic carbon is SOC, total nitrogen is TN, and total phosphorus is TP). Our study demonstrated that simple, quantitative plant functional traits, but not functional diversity, are directly related to soil C and N properties, and they likely play an important role in plant–soil interactions. Our results also suggest that functional identity of species may be more important than functional diversity in influencing ecosystem processes during wetland drying.http://www.solid-earth.net/8/137/2017/se-8-137-2017.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
W. Li H. E. Epstein Z. Wen J. Zhao J. Jin G. Jing J. Cheng G. Du |
spellingShingle |
W. Li H. E. Epstein Z. Wen J. Zhao J. Jin G. Jing J. Cheng G. Du Community-weighted mean traits but not functional diversity determine the changes in soil properties during wetland drying on the Tibetan Plateau Solid Earth |
author_facet |
W. Li H. E. Epstein Z. Wen J. Zhao J. Jin G. Jing J. Cheng G. Du |
author_sort |
W. Li |
title |
Community-weighted mean traits but not functional diversity determine the changes in soil properties during wetland drying on the Tibetan Plateau |
title_short |
Community-weighted mean traits but not functional diversity determine the changes in soil properties during wetland drying on the Tibetan Plateau |
title_full |
Community-weighted mean traits but not functional diversity determine the changes in soil properties during wetland drying on the Tibetan Plateau |
title_fullStr |
Community-weighted mean traits but not functional diversity determine the changes in soil properties during wetland drying on the Tibetan Plateau |
title_full_unstemmed |
Community-weighted mean traits but not functional diversity determine the changes in soil properties during wetland drying on the Tibetan Plateau |
title_sort |
community-weighted mean traits but not functional diversity determine the changes in soil properties during wetland drying on the tibetan plateau |
publisher |
Copernicus Publications |
series |
Solid Earth |
issn |
1869-9510 1869-9529 |
publishDate |
2017-02-01 |
description |
Climate change and human activities have caused a shift in
vegetation composition and soil biogeochemical cycles of alpine wetlands on
the Tibetan Plateau. The primary goal of this study was to test for
associations between community-weighted mean (CWM) traits, functional
diversity, and soil properties during wetland drying. We collected soil
samples and investigated the aboveground vegetation in swamp, swamp meadow,
and typical meadow environments. Four CWM trait values (specific leaf area is SLA, leaf dry
matter content is LDMC, leaf area is LA, and mature plant height is MPH) for 42
common species were measured across the three habitats; three components of
functional diversity (functional richness, functional evenness, and
functional divergence) were also quantified at these sites. Our results
showed that the drying of the wetland dramatically altered plant community
and soil properties. There was a significant correlation between CWM of
traits and soil properties, but not a significant correlation between
functional diversity and soil properties. Our results further showed that
CWM-LA, CWM-SLA, and CWM-LDMC had positive correlations with soil readily
available nutrients (available nitrogen, AN; available phosphorus, AP), but
negative correlations with total soil nutrients (soil organic carbon is SOC,
total nitrogen is TN, and total phosphorus is TP). Our study demonstrated that
simple, quantitative plant functional traits, but not functional diversity,
are directly related to soil C and N properties, and they likely play an
important role in plant–soil interactions. Our results also suggest that
functional identity of species may be more important than functional
diversity in influencing ecosystem processes during wetland drying. |
url |
http://www.solid-earth.net/8/137/2017/se-8-137-2017.pdf |
work_keys_str_mv |
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