2012
DOI: 10.1371/journal.pone.0045205
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Water- and Plant-Mediated Responses of Ecosystem Carbon Fluxes to Warming and Nitrogen Addition on the Songnen Grassland in Northeast China

Abstract: BackgroundUnderstanding how grasslands are affected by a long-term increase in temperature is crucial to predict the future impact of global climate change on terrestrial ecosystems. Additionally, it is not clear how the effects of global warming on grassland productivity are going to be altered by increased N deposition and N addition.Methodology/Principal FindingsIn-situ canopy CO2 exchange rates were measured in a meadow steppe subjected to 4-year warming and nitrogen addition treatments. Warming treatment … Show more

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Cited by 38 publications
(40 citation statements)
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“…Experimental warming also reduced average GPP and AGB in 2012 in the alpine meadow at the low elevation [52] and it was also a drier year of 2012 (312.8 mm) compared to the mean precipitation of 1963–2015 (Fig 1). These implied that the response directions of plant growth to experimental warming varied with years and experimental warming did not have a continuous negative effect on biomass production at the low elevation, which was in line with previous studies [2729,53,54]. The variable response directions may be due to the variable environmental temperature and humidity among years [27,29] and plant growth was more sensitive to moisture than temperature change when water was lower than a certain threshold value [53,55].…”
Section: Resultssupporting
confidence: 91%
See 1 more Smart Citation
“…Experimental warming also reduced average GPP and AGB in 2012 in the alpine meadow at the low elevation [52] and it was also a drier year of 2012 (312.8 mm) compared to the mean precipitation of 1963–2015 (Fig 1). These implied that the response directions of plant growth to experimental warming varied with years and experimental warming did not have a continuous negative effect on biomass production at the low elevation, which was in line with previous studies [2729,53,54]. The variable response directions may be due to the variable environmental temperature and humidity among years [27,29] and plant growth was more sensitive to moisture than temperature change when water was lower than a certain threshold value [53,55].…”
Section: Resultssupporting
confidence: 91%
“…These implied that the response directions of plant growth to experimental warming varied with years and experimental warming did not have a continuous negative effect on biomass production at the low elevation, which was in line with previous studies [2729,53,54]. The variable response directions may be due to the variable environmental temperature and humidity among years [27,29] and plant growth was more sensitive to moisture than temperature change when water was lower than a certain threshold value [53,55]. The precipitation in 2014 was 38.6 mm higher compared to the mean precipitation (398.7 mm), whereas the precipitation in 2012 and 2015 was 85.88 mm and 98.48 mm lower compared to the mean precipitation, respectively.…”
Section: Resultssupporting
confidence: 91%
“…In general, ecosystem C fluxes are closely related to SWC in grassland ecosystem [28], [29]. However, we found no significant relationship between ecosystem C fluxes and SWC in our freshwater wetland.…”
Section: Discussionmentioning
confidence: 60%
“…In addition to GPP, ecosystem respiration is also sensitive to warming and changes in phenology [37,52]. Warmer air and soil temperatures will have direct effects on plant autotrophic and soil heterotrophic respiration.…”
Section: Discussionmentioning
confidence: 99%