scholarly journals Belowground plant biomass allocation in tundra ecosystems and its relationship with temperature

2016 ◽  
Vol 11 (5) ◽  
pp. 055003 ◽  
Author(s):  
Peng Wang ◽  
Monique M P D Heijmans ◽  
Liesje Mommer ◽  
Jasper van Ruijven ◽  
Trofim C Maximov ◽  
...  
2021 ◽  
Vol 12 ◽  
Author(s):  
Chunhui Zhang ◽  
Nianxun Xi

In theory, changes in the amount of rainfall can change plant biomass allocation and subsequently influence coupled plant-soil microbial processes. However, testing patterns of combined responses of plants and soils remains a knowledge gap for terrestrial ecosystems. We carried out a comprehensive review of the available literature and conducted a meta-analysis to explore combined plant and soil microbial responses in grasslands exposed to experimental precipitation changes. We measured the effects of experimental precipitation changes on plant biomass, biomass allocation, and soil microbial biomass and tested for trade-offs between plant and soil responses to altered precipitation. We found that aboveground and belowground plant biomass responded asynchronically to precipitation changes, thereby leading to shifts in plant biomass allocation. Belowground plant biomass did not change under precipitation changes, but aboveground plant biomass decreased in precipitation reduction and increased in precipitation addition. There was a trade-off between responses of aboveground plant biomass and belowground plant biomass to precipitation reduction, but correlation wasn't found for precipitation addition. Microbial biomass carbon (C) did not change under the treatments of precipitation reduction. Increased root allocation may buffer drought stress for soil microbes through root exudations and neutralize microbial responses to precipitation reduction. However, precipitation addition increased microbial biomass C, potentially reflecting the removal of water limitation for soil microbial growth. We found that there were positive correlations between responses of aboveground plant biomass and microbial biomass C to precipitation addition, indicating that increased shoot growth probably promoted microbial responses via litter inputs. In sum, our study suggested that aboveground, belowground plant biomass and soil microbial biomass can respond asynchronically to precipitation changes, and emphasizes that testing the plant-soil system as a whole is necessary for forecasting the effects of precipitation changes on grassland systems.


Author(s):  
Haozhi Ma ◽  
Lidong Mo ◽  
Thomas W. Crowther ◽  
Daniel S. Maynard ◽  
Johan van den Hoogen ◽  
...  

2017 ◽  
Vol 68 (2) ◽  
pp. 212-220 ◽  
Author(s):  
D. Wang ◽  
H. L. He ◽  
Q. Gao ◽  
C. Z. Zhao ◽  
W. Q. Zhao ◽  
...  

2020 ◽  
Vol 455 (1-2) ◽  
pp. 53-64
Author(s):  
Jing Tian ◽  
Brian A. Branfireun ◽  
Zoë Lindo

Fire Ecology ◽  
2010 ◽  
Vol 6 (2) ◽  
pp. 13-25 ◽  
Author(s):  
Sonali Saha ◽  
Alessandro Catenazzi ◽  
Eric S. Menges

2020 ◽  
Vol 10 (1) ◽  
Author(s):  
Jing Zhang ◽  
Xiaoan Zuo ◽  
Xueyong Zhao ◽  
Jianxia Ma ◽  
Eduardo Medina-Roldán

Abstract Extreme climate events and nitrogen (N) deposition are increasingly affecting the structure and function of terrestrial ecosystems. However, the response of plant biomass to variations to these global change drivers is still unclear in semi-arid regions, especially in degraded sandy grasslands. In this study, a manipulative field experiment run over two years (from 2017 to 2018) was conducted to examine the effect of rainfall alteration and nitrogen addition on biomass allocation of annuals and perennial plants in Horqin sandy grassland, Northern China. Our experiment simulated extreme rainfall and extreme drought (a 60% reduction or increment in the growing season rainfall with respect to a control background) and N addition (20 g/m2) during the growing seasons. We found that the sufficient rainfall during late July and August compensates for biomass losses caused by insufficient water in May and June. When rainfall distribution is relatively uniform during the growing season, extreme rainfall increased aboveground biomass (AGB) and belowground biomass (BGB) of annuals, while extreme drought reduced AGB and BGB of perennials. Rainfall alteration had no significant impacts on the root-shoot ratio (R/S) of sandy grassland plants, while N addition reduced R/S of grassland species when there was sufficient rainfall in the early growing season. The biomass of annuals was more sensitive to rainfall alteration and nitrogen addition than the biomass of perennials. Our findings emphasize the importance of monthly rainfall distribution patterns during the growing season, which not only directly affect the growth and development of grassland plants, but also affect the nitrogen availability of grassland plants.


2013 ◽  
Vol 41 (7) ◽  
pp. 657-664 ◽  
Author(s):  
Hai Wang ◽  
Zheng-Xin Chen ◽  
Xiao-Yu Zhang ◽  
Si-Xi Zhu ◽  
Ying Ge ◽  
...  

Oikos ◽  
2014 ◽  
Vol 123 (7) ◽  
pp. 800-806 ◽  
Author(s):  
G. F. Ciska Veen ◽  
Saskia de Vries ◽  
Elisabeth S. Bakker ◽  
Wim H. van der Putten ◽  
Han Olff

HortScience ◽  
1995 ◽  
Vol 30 (4) ◽  
pp. 859F-859
Author(s):  
Jill C. Larimer ◽  
Dan Struve

ln Spring 1993, red oaks (Quercus rubra) were propagated from seed. From June through October, plants were fertilized twice daily with 1.4 liters of 20N–10P–20K water-soluble fertilizer solution at concentrations of 0, 25, 50, 100, 200, or 400 ppm N. Destructive harvests were conducted six times at intervals from June through Dec. 1993. Leaf area, stem height, root length, root area, and dry weights of roots, stem, and leaves of harvested plants were measured and tissue nutrient concentrations were analyzed. There was no relationship between whole-plant N concentration and total plant biomass (r = 0). However, there were some linear relationships between total plant N and total plant biomass for an individual fertilizer treatment. Biomass allocation between root, stems, and leaves was very consistent across all fertilizer levels at any one harvest. Percent total N in roots, stems, and leaves also was fairly consistent across fertilizer levels. This was true at each harvest, except the first two, in which a greater percentage of total N was partitioned to the leaves and a smaller percentage was partitioned to the roots in the high (100, 200, 400 ppm N) fertilizer treatments. Whole-plant K concentrations increased with increasing fertilizer level, but decreased over time. Whole-plant P concentrations increased linearly with whole-plant dry weight in the higher (100, 200, 400 ppm N) fertilizer treatments.


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