Skip to main content

Effects of N and P enrichment on plant photosynthetic traits in alpine steppe of the Qinghai-Tibetan Plateau

Abstract

Background

N (nitrogen) and P (phosphorus) play important roles in plant growth and fitness, and both are the most important limiting factors that affect grassland structure and function. However, we still know little about plant physiological responses to N and P enrichment in alpine grassland of the Qinghai-Tibetan Plateau. In our experiment, five dominant common herbaceous species were selected and their photosynthetic parameters, leaf N content, and aboveground biomass were measured.

Results

We found that species-specific responses to N and P enrichment were obvious at individual level. N addition (72 kg Nha−1 yr−1), P addition (36 kg Pha−1 yr−1) and NP addition (72 kg Nha−1 yr−1and 36 kg P ha−1 yr−1, simultaneously) significantly promoted net photosynthetic rate of Leymus secalinus. Differential responses also existed in the same functional groups. Responses of forb species to the nutrients addition varied, Aconitum carmichaeli was more sensitive to nutrients addition including N addition (72 kg Nha−1 yr−1), P addition (36 kg Pha−1 yr−1) and NP addition (72 kg Nha−1 yr−1and 36 kg P ha−1 yr−1). Responses of plant community photosynthetic traits were not so sensitive as those of plant individuals under N and P enrichment.

Conclusions

Our findings highlighted that photosynthetic responses of alpine plants to N and P enrichment were species-specific. Grass species Leymus secalinus had a higher competitive advantage compared with other species under nutrient enrichment. Additionally, soil pH variation and nutrients imbalance induced by N and P enrichment is the main cause that affect photosynthetic traits of plant in alpine steppe of the Qinghai-Tibetan Plateau.

Peer Review reports

Introduction

Nitrogen (N) and phosphorus (P) are the most important components that affect plant growth and development in terrestrial ecosystem [1,2,3]. N and P play an important role in the synthesis of chlorophyll and photosynthetic enzymes [4]. Therefore, N and P fertilization would have a large influence on plant photosynthetic processes [5]. Previous studies have showed that moderate N and P addition can increase plant photosynthetic capacity, enhance grassland productivity and shift community composition [6, 7]. However, N and P enrichment can also cause negative effects, such as soil acidification, soil nutrients imbalance and thus to cause plant diversity loss [8].

Photosynthetic traits are comprehensive reflection of plant physiological status, which can measure the growth difference among different plants and the degree of environmental influence, and is closely related to plant growth and biomass accumulation. So far, no consistent results have been showed about how N and P enrichment affects plant photosynthetic traits for plant species-specific attribution. Nitrogen always has a close relationship with photosynthetic capacity, for the photosynthetic machinery and proteins related with Calvin cycle and thylakoids are mostly made-up of N element [9,10,11]. N addition can enhance plant net photosynthetic rate by supplying more N resource in N-limited ecosystem, however N enrichment usually negatively undermine plant net photosynthetic rate of some N-sensitive species by breaking soil nutrients balance [12]. P is the main component of chemical substances such as nucleic acids, ATP (adenosine-triphosphate) and phospholipids in the photosynthetic process, and it is also the most easily fixed and transformed element in soil [5]. Projected N addition may also aggravate P limitation in terrestrial ecosystem [12, 13], as excessive N input is usually thought to cause soil acidification and P leaching losses [14]. Moderate P addition can stimulate plant net photosynthetic rate by enhancing plant light use efficiency and stomatal conductance [15, 16]. Additionally, P supply may also modify the relationship between N and photosynthetic processes [17, 18]. At present, the studies on P addition effects mostly focused on the form, conversion, availability of soil P, and soil microbe dynamics [19,20,21,22]. Compared with N addition, P addition and their coupling effects on plant photosynthetic traits have been scarcely experimented in grassland ecosystems. Some studies found that N and P enrichment may also restrict plant photosynthetic rate by reducing leaf area and excessive nutrient input [23, 24].

In the alpine grasslands, responses to nutrient limitation may differ among species, this may be associated with the contrasting carbon and nutrient economies of different forms [25, 26], and interspecific eco-physiological adaptations disparity [27, 28]. There are also studies demonstrated that plants of different functional types show different photosynthetic capacity when the availability of N and P changes [29]. Generally, plant community shift could be predicted from individuals before ecosystem processes are largely influenced [30]. Eco-physiological responses of dominant species can reflect underlying mechanisms that lead changes in grassland community under N and P addition to some degree [28].

The objective of this study is to determine the impacts of N and P enrichment on plant and soil properties involved in N and P cycling in alpine steppe. Compared with N addition experiments, most experiments of P addition and NP addition on grassland ecosystem are concentrated on community level. The effects of N addition, P addition and their coupling effects on eco-physiological responses of alpine plants still remains unclear at both individual and community level [31]. Here, we conducted an experiment in an alpine steppe of the Qinghai-Tibetan Plateau to examine the eco-physiological responses of dominant plant species and predict the responses of whole plant community to N addition, P addition and their coupling effects. As alpine regions are usually N-limited [32] or being shift to P-limited [33], so we hypothesized that: (1) N and P enrichment may promote the photosynthetic capacity of plant and thus to promote productivity in alpine steppe. In addition, Some studies found that different species have different patterns of N and P allocation and nutrient economies [25, 26]. Divergent adaptation mechanisms of among species may be due to their biological characteristics [28]. Based on this, we hypothesized that: (2) plant photosynthetic responses to N and P enrichment might be species-specific.

Material and methods

Site description

The field experiment was carried out in an alpine steppe located at Tiebujia Town of Gonghe County (99°35′E, 37°02′N, 3270 m ASL) in Qinghai province, China (Fig. 1). The alpine steppe is with loam-clay soil. The mean annual temperature in alpine steppe is about 0 °C, the mean annual precipitation is about 377 mm, and the annual evaporation is about 1484 mm.

Fig. 1
figure 1

Location of the study site

Experimental design

In 2012, the grassland with an area of 20 m × 20 m was fenced with iron fence (1.2 m high). In 2018, four nutrient addition regimes were established in this area (randomized blocks design): control (CK, with neither N nor P addition); N addition (N, 72 kg Nha−1 yr−1); P addition (P, 36 kg P ha−1 yr−1); and combined N and P addition (NP, 72 kg Nha−1 yr−1and 36 kg P ha−1 yr−1, simultaneously). In alpine steppe, the N-saturated load is estimated by 40-50kgNha−1 yr−1 [34, 35], so the N addition rate largely simulated N critical load, while P addition rate was based on the requirement by the alpine plant communities [36]. Three plots in the fenced area (2 m by 5 m) were chosen as the replication of each treatment. All the plots in the treatments were similar in topographies and land use histories. Ammonium nitrate (NH4NO3) and calcium superphosphate (Ca(H2PO4)2) were applied as N fertilizer and P fertilizer form respectively in early May, July, and September each year since 2018. In this experiment, we selected five dominant species (according to their coverage) that exist in all plots to do the following parameters measurement (Table 1). Leymus secalinus is a perennial grass of Gramineae, with developed underground rhizomes and strong adaptability, and it is one of the main constructive and dominant species in the alpine grasslands on the Qinghai-Tibet Plateau. Agropyron cristatum is also a perennial grass of Gramineae, with well-developed fibrous roots and strong adaptability. Aster tataricus, Potentilla multifida and Aconitum carmichaeli are three perennial herbages belonging to Compositae, Rosaceae and Ranunculaceae, respectively. The five species have different morphological characteristics.

Table 1 List of selected species (dominant species) in this study site

Photosynthetic traits

In early August of 2019 (the peak growing period for alpine plants in this region), net photosynthetic rate (PN), transpiration rate (Tr), stomatal conductance (gs), and intercellular CO2 concentration (Ci) of each selected herbage species were measured using the Li-6800 (Li-Cor, Lincoln, NE, USA) with light availability of 1500 PAR between 9:00 and 12:00 am. The chamber CO2 concentration was maintained at 400 μmol·mol−1 with CO2 injection system, while leaf temperature was kept at 25 °C at a relative humidity between 60%-70%. Water use efficiency (WUE) was calculated as PN/Tr. Five fully expanded leaves in the upper portion of each herbage species were selected for measurements. Also, five replicates were used for each species in this study.

Sampling and measurement

The aboveground plant material of selected species were harvested and placed in sealed polyethylene bags and then dried at 70 ℃ for 48 h to constant weight. The dried materials were then ground to a fine powder with a vibrating sample mill (FW100, Tianjin Taisite Instrument Co., LTD, China) for subsequent analysis. Soil samples to the depth of 20 cm were collected by a 3.5 cm-diameter soil probe near the location of plant sampling. Then the soil samples were air-dried to constant weight and sieved through a 0.15-mm mesh. Plant and soil N content was measured by elemental analyzer (EA 3000, Italy). Soil NH4+-N and NO3-N content were measured using a flow injection auto‐analyzer (AACE, Germany). Soil Available phosphorus (AP) and available potassium (AK) was measured using an inductively coupled plasma spectrometer (SPECTRO ARCOS EOP, Germany). A glass electrode was used to measure soil pH in the supernatant by homogeneously mixing 5 g of soil and 25 ml of water [37].

Data analysis

We calculated the mean of measured plant traits for each species in each plot. The relative abundance of each selected species was calculated. The community-weighted means (CWM) of measure plant traits were calculated using the following formula [38]:

$$\mathrm{CWM}\;=\;\sum_{i=1}^n\;{\mathrm p}_{\mathit i}\;{\mathrm s}_i$$

where pi is the relative abundance of species i, and si is the mean value of plant traits in each treatment.

In addition, response ratio (RR) for each observation was calculated as the natural log of the response ratio RR = ln (Xt/Xc), where Xt is the mean of plant traits for each treatment and Xc is the mean of plant traits in associated unfertilized control [39]. More specifically, the mean, standard deviation (S) or standard error, and sample size for each observation were calculated to calculate the RR. The statistical analyses were performed using the software package R (4.0.3). Then, we used one-way ANOVA in SPSS 22.0 software (SPSS Inc) to estimate the effect of nutrients addition on all plant traits. Thereafter, the least square difference (LSD) tests were used to conduct post hoc mean comparisons of each plant traits of each species under different treatments. Additionally, in order to visualize the relationship among all plant and soil variables, a correlation matrix diagram and a PCA analysis were successfully developed in R.

Results

Effects of N and P addition on photosynthetic capacity of five dominant common plant species

Species-specific responses to nutrient additions were obvious (Fig. 2). N addition, P addition and NP addition significantly promoted net photosynthetic rate of Leymus secalinus (p < 0.05). The net photosynthetic rate of Agropyron cristatum and Aster tataricus showed no significant responses to N and P addition. Single N and P addition significantly promoted the net photosynthetic rate of Potentilla multifidi (p < 0.05). N and NP addition significantly decreased the net photosynthetic rate of Aconitum carmichaeli (p < 0.05), while P addition had no significant effects. All nutrient addition treatments significantly decreased the Gs of Aconitum carmichaeli (p < 0.05). Single N and P addition significantly promoted the Gs of Leymus secalinus, Agropyron cristatum and Aster tataricus (p < 0.05). All of nutrient addition treatments significantly increased the Ci of Aster tataricus (p < 0.05). Single N and P addition significantly increased the Tr of two grass species (p < 0.05). Leymus secalinus kept a significant higher WUE under all treatments of nutrient additions compared with other herbaceous species.

Fig.2
figure 2

Photosynthetic parameters from five dominant common plant species (grasses and forbs) in the nutrient fertilization experiment fertilized with nitrogen (N), phosphorus (P) and both (NP). Panel (A), (B), (C) show response ratio of net photosynthetic rate (A) under N, P and both NP fertilization respectively. Panel (D), (E), (F) show response ratio of stomatal conductance (Gs) under N, P and both NP fertilization respectively. Panel (G), (H), (I) show response ratio of intercellular CO2 concentration (Ci) under N, P and both NP fertilization respectively. Panel (J), (K), (L) show response ratio of transpiration rate (Tr) under N, P and both NP fertilization respectively. Panel (M), (N), (O) show response ratio of water use efficiency (WUE) under N, P and both NP fertilization respectively. RR: response ratio

Effects of N and P addition on photosynthetic characteristics, N content, height and AGB of the whole plant community

N addition significantly promoted the A, Gs and Tr of the whole plant community (p < 0.05) (Fig. 3), but did not significantly affect the community Ci and WUE of the plant community. Both P and NP addition had no significant effects on photosynthetic capacity of the plant community (p > 0.05). Only N addition significantly increased N content of the community(p < 0.05, Fig. 4A), and N addition, P addition and their combination had no significant effects on the height and AGB of the whole community (Fig. 4B and C).

Fig. 3
figure 3

Effects of N and P fertilization on community weighed mean (CWM) of photosynthetic parameters. (A) A: net photosynthetic rate, (B) Gs: stomatal conductance, (C) Ci: intercellular CO2 concentration, (D) Tr: transpiration rate, (E) WUE: water use efficiency.CK: control, N: N fertilization, P: P fertilization, NP: N plus P fertilization.* indicates significant difference between treatments (p < 0.05)

Fig. 4
figure 4

Effects of N and P fertilization on total aboveground biomass (AGB) and community weighed mean (CWM) of N content and height. CK: control, N: N fertilization, P: P fertilization, NP: N plus P fertilization.* indicates significant difference between treatments (p < 0.05). (A) community N content, (B) community height, (C)community aboveground biomass

Relationship among plant eco-physiological traits and soil properties

CWMA was positively related with CWMGs (r = 0.82, p < 0.01), CWMTr (r = 0.80, p < 0.01), CWMWUE (r = 0.75, p < 0.01), CWMN (r = 0.88, p < 0.001), soil NH4+-N (r = 0.75, p < 0.01) and soil AP (r = -0.65, p < 0.05) (Fig. 5). PCA showed that PC1 and PC2 explained 62.3% of the variance of all plant and soil variables (Fig. 6). Although N, P and NP addition presented a clear separation with CK, no clear separation was found under N, P and NP addition treatments. Soil NH4+-N and soil AP presented the largest weight in all measured soil properties, while CWMA accounted for the largest weight in all measured plant traits.

Fig. 5
figure 5

Correlation of community weighed mean (CWM) values among all plant eco-physiological traits and soil nutrients. A: net photosynthetic rate, Gs: stomatal conductance, Ci: intercellular CO2 concentration, Tr: transpiration rate, WUE: water use efficiency.CK: control, N: N fertilization, P: P fertilization, NP: N plus P fertilization.* indicates significant difference at the level of p < 0.05,** indicates significant difference at the level of p < 0.01, ***indicates significant difference at the level of p < 0.001.Soil AP: Soil available phosphorus, Soil AK: Soil available potassium, Soil NH4+-N: Soil ammonium nitrogen, Soil NO3-N: Soil nitrate nitrogen

Fig. 6
figure 6

Principal component analysis (PCA) of plant and soil variables. The smaller angle between two variable arrows indicates stronger correlation, as the cosine of the angle between variable arrows equals their correlation coefficients. The length of vector arrows indicate weight of the variables. A: net photosynthetic rate, Gs: stomatal conductance, Ci: intercellular CO2 concentration, Tr: transpiration rate, WUE: water use efficiency.CK: control, N: N fertilization, P: P fertilization, NP: N plus P fertilization. Soil AP: Soil available phosphorus, Soil AK: Soil available potassium, Soil NH4+-N: Soil ammonium nitrogen, Soil NO3-N: Soil nitrate nitrogen

Discussion

Alpine regions are typically thought to be N-limited [32, 40] or being shifted to P-limited [33]. Cold temperatures, short growing seasons and low nutrient supply are usually the limiting factors of alpine grassland productivity [41, 42]. Generally, long-term moderate N and P supply in grassland can increase the biomass, leaf area, or shift species composition [43]. Although N and P addition can alleviate nutrient deficiency to some degree, such effects seem to be not so obvious in short term at the community level. However, N and P enrichment can obviously affect growth and photosynthesis of plant individual through the fertilization-induced soil nutrients imbalance and soil pH variation. In this study, soil acidification was not obvious under N and P addition, yet soil nutrients tended to fluctuate with nutrient addition (Table S1). And this suggested that soil nutrients balance is much more sensitive than soil pH, while hysteresis effect might exist for a short term nutrient addition experiment. In addition, soil AP and soil NH4+-N are the two most important factors that affect plant community traits in this study. Soil AP has a closely positive effects with plant community traits while soil NH4+-N has an obvious negative effects. This suggested that plants showed a more demand of P under nutrients enrichment, while N addition rate in this study is a critical load [35].

The species-specific responses to N and P addition may depend largely on their eco-physiological adaptation in the plant community. Generally, compared with forbs and other functional types, grass can be much more competitive under nutrient addition for its higher nutrient and light use efficiency as well as high nutrient critical load [44,45,46]. The responsive variations also appeared in the same functional groups, i.e., grass species Leymus secalinus showed improved photosynthetic capacity under nutrients addition, while Agropyron cristatum tended to be non-responsive to N and P addition, implying that Leymus secalinus may possess a relatively higher nutrients use efficiency [47, 48]. This may also suggest that interspecific competition for resources existed in the same functional groups, and the ability for nutrients uptake varied among different species. Although previous studies have reported that N addition had no significant effect on forb [49], we found that the net photosynthetic rate of forb species (Aconitum carmichaeli) was obviously negatively affected by N and NP addition in this study. Aster tataricus showed non-responsive to nutrients addition, suggesting its high inner stability to exogenous nutrients input. Both single N and P addition promoted the photosynthetic capacity of Potentilla multifidim while NP addition had no significant effect. This may be because N and P coupling addition exceed the nutrients requirement of Potentilla multifidim, thus higher nutrients load might offset the positive effects brought by N and P addition. Overall, the different responses of plant photosynthetic capacity to N and P addition suggested different adaptation mechanism of these species. Although previous studies stated that the plants within the same functional group may persist similar responses to external environmental changes [50], species-specific responses in our study suggested individual disparity of the plants even from the same functional groups. Generally, moderate P addition could alleviate detrimental effects induced by excessive N input [51]. However, Agropyron cristatum and Aster tataricus were non-responsive to N and P addition in our study, this may be because high intraspecific and interspecific competition as well as low nutrient utilization efficiency of these species. N and P addition had no negative effects on grass species, indicating that grass species may possess a higher nutrients use efficiency or nutrient critical load than other species [52].

At the community level, significant photosynthetic response was only found in N addition treatment, suggesting the photosynthetic capacity of the whole community was still being limited by N resource. Despite obvious increase in plant N uptake of all species, some of the species photosynthetic capacity was not elevated in this study, implying that excessive nutrient uptake might have not partitioned to photosynthetic components with more nutrient supply [53]. In our study, photosynthetic capacity of the dominant common grass species, in contrast to forb species, had a much higher N critical load, suggesting that grasses can better adapt to high nutrients supply than forbs. In addition, N and P addition increased the net photosynthetic rate of some species via the increase of stomatal conductance, suggesting the close relations between photosynthetic capacity and stomatal behavior [54]. Higher stomatal conductance can increase CO2 supply to intercellular space for plant photosynthesis [55]. Nutrients addition could improve plant photosynthetic capacity by enlarging cell size and making the cell wall thinner to enhance stomatal conductance [56]. The variation of the net photosynthetic rate was inconsistent with that of stomatal conductance for some species, indicating that non-stomatal limitation (chlorophyll and carboxylation) may play an important role under N and P enrichment [28, 57, 58]. Overall, the different photosynthetic responses among the plant species in the alpine steppe suggested that long-term projected N and P addition may have the potential to change plant species composition and finally lead to the change of grassland community structure and function.

Alpine grassland productivity is usually limited by N and P supply [12]. However, the effects of N and P addition on grassland productivity is still inconsistent [59,60,61]. Some studies have showed strong effects of fertilization on plant productivity [62,63,64]. Positive effects of N and P addition on grassland community productivity may depend on various factors, such as nutrient addition rate [62] and precipitation [65]. We didn’t see obviously responses of plant productivity at the community level to N and P addition, indicating that grassland community productivity can remain much stable and non-responsive to short-term nutrient addition in alpine regions. This result may also be associated with the nutrient loss in the fertilization process induced by rainfall or other environmental factors [66].

Overall, we found that not all of the photosynthetic capacity were promoted by the N and P enrichment and the productivity was also not obviously promoted. Such result is inconsistent with our first hypothesis. This suggested that some species might be negatively sensitive to nutrient enrichment, through alpine grassland ecosystems are usually both N and P limited [67, 68]. However, we found that plant photosynthetic responses to N and P enrichment were indeed differential. This complied with our second hypothesis that plant photosynthetic responses to N and P enrichment are species-specific. Soil nutrients dynamics are important influencing factors for plant photosynthetic traits [69]. Soil properties change induced by N and P enrichment would influence plant photosynthesis, affect plant fitness and grassland productivity, and finally alter ecosystem functioning [12, 66, 70,71,72]. On the whole, different species have different patterns of N and P allocation to various components under N and P enrichment, and such differences can finally cause the disparity in photosynthetic traits among species.

Conclusion

Our study highlights that the plant photosynthetic responses to N and P addition are species-specific. Leymus secalinus has an absolute superiority of photosynthetic capacity under higher N and P supply. Not all forb species are sensitive in photosynthetic responses to higher N and P addition. Responses of plant community functional traits were not so sensitive as those of plant individuals. In the future, a long-term N and P fertilization with multi-level still should be applied to examine the photosynthetic traits variation of different species and community vegetation dynamics to optimize fertilization effects in alpine regions.

Availability of data and materials

All data generated or analyzed during this study are included in this article.

Abbreviations

A :

Net photosynthetic rate

Gs :

Stomatal conductance

Ci :

Intercellular CO2 concentration

Tr :

Transpiration rate

WUE :

Water use efficiency

CK:

Control

N:

N fertilization

P:

P fertilization

NP:

N plus P fertilization.

Soil AP:

Soil available phosphorus

Soil AK:

Soil available potassium

Soil NH4 +-N:

Soil ammonium nitrogen

Soil NO3 -N:

Soil nitrate nitrogen

CWM:

Community-weighted means

References

  1. Elser JJ, Bracken ME, Cleland EE, Gruner DS, Harpole WS, Hillebrand H, Smith JE. Global analysis of nitrogen and phosphorus limitation of primary producers in freshwater, marine and terrestrial ecosystems. Ecol Lett. 2007;10(12):1135–42.

    Article  PubMed  Google Scholar 

  2. Mo Q, Chen Y, Yu S, Fan Y, Peng Z, Wang W, Wang F. Leaf nonstructural carbohydrate concentrations of understory woody species regulated by soil phosphorus availability in a tropical forest. Ecol Evol. 2020;10(15):8429–38.

    Article  PubMed  PubMed Central  Google Scholar 

  3. Zheng Z, Lu J, Su Y, Yang Q, Wang X. Differential effects of n and p additions on foliar stoichiometry between species and community levels in a subtropical forest in eastern china. Ecol Indic. 2020;117: 106537.

    Article  CAS  Google Scholar 

  4. Raven JA, Handley LL, Wollenweber B. Plant nutrition and water use efficiency. In: Bacon MA, editor. Water use efficiency in plant biology. Boca Raton: CRC Press; 2004. p. 171–97.

    Google Scholar 

  5. Reich PB, Oleksyn J, Wright IJ. Leaf phosphorus influences the photosynthesis–nitrogen relation: a cross-biome analysis of 314 species. Oecologia. 2009;160(2):207–12.

    Article  PubMed  Google Scholar 

  6. Suding KN, Collins SL, Gough L, Clark C, Cleland EE, Gross KL, Pennings S. Functional-and abundance-based mechanisms explain diversity loss due to N fertilization. P Natl Acad Sci USA. 2005;102(12):4387–92.

    Article  CAS  Google Scholar 

  7. Bai Y, Wu J, Clark CM, Naeem S, Pan Q, Huang J, Han X. Tradeoffs and thresholds in the effects of nitrogen addition on biodiversity and ecosystem functioning: evidence from inner Mongolia Grasslands. Global Change Biol. 2010;16(1):358–72.

    Article  Google Scholar 

  8. Liang T, Xu W, Wei Y, Lin W, Pang Y, Liu F, Liu X. Atmospheric nitrogen deposition in the Loess area of China. Atmos Pollut Res. 2016;7(3):447–53.

    Article  Google Scholar 

  9. Wright IJ, Reich PB, Westoby M, Ackerly DD, Baruch Z, Bongers F, Flexas J. The worldwide leaf economics spectrum. Nature. 2004;428(6985):821–7.

    Article  CAS  PubMed  Google Scholar 

  10. Kattge J, Knorr W, Raddatz T, Wirth C. Quantifying photosynthetic capacity and its relationship to leaf nitrogen content for global-scale terrestrial biosphere models. Global Change Biol. 2009;15(4):976–91.

    Article  Google Scholar 

  11. Pasquini SC, Santiago LS. Nutrients limit photosynthesis in seedlings of a lowland tropical forest tree species. Oecologia. 2012;168(2):311–9.

    Article  CAS  PubMed  Google Scholar 

  12. Li Y, Niu S, Yu G. Aggravated phosphorus limitation on biomass production under increasing nitrogen loading: a meta-analysis. Global Change Biol. 2016;22(2):934–43.

    Article  Google Scholar 

  13. Deng Q, Hui D, Dennis S, Reddy KC. Responses of terrestrial ecosystem phosphorus cycling to nitrogen addition: A meta-analysis. Global Ecol Biogeogr. 2017;26(6):713–28.

    Article  Google Scholar 

  14. Holzmann S, Missong A, Puhlmann H, Siemens J, Bol R, Klumpp E, Wilpert KV. Impact of anthropogenic induced nitrogen input and liming on phosphorus leaching in forest soils. J Plant Nutr Soil Sc. 2016;179(4):443–53.

    Article  CAS  Google Scholar 

  15. Cordell S, Goldstein G, Meinzer FC, Vitousek PM. Regulation of leaf life-span and nutrient-use efficiency of Metrosideros polymorpha trees at two extremes of a long chronosequence in Hawaii. Oecologia. 2001;127(2):198–206.

    Article  CAS  PubMed  Google Scholar 

  16. Thomas DS, Montagu KD, Conroy JP. Leaf inorganic phosphorus as a potential indicator of phosphorus status, photosynthesis and growth of Eucalyptus grandis seedlings. Forest Ecol Manag. 2006;223(1–3):267–74.

    Article  Google Scholar 

  17. Conroy JP, Smillie RM, Küppers M, Bevege DI, Barlow EW. Chlorophyll a fluorescence and photosynthetic and growth responses of Pinus radiata to phosphorus deficiency, drought stress, and high CO2. Plant Physiol. 1986;81(2):423–9.

    Article  CAS  PubMed  PubMed Central  Google Scholar 

  18. Walker AP, Beckerman AP, Gu L, Kattge J, Cernusak LA, Domingues TF, Woodward FI. The relationship of leaf photosynthetic traits–Vcmax and Jmax–to leaf nitrogen, leaf phosphorus, and specific leaf area: a meta-analysis and modeling study. Ecol Evol. 2014;4(16):3218–35.

    Article  PubMed  PubMed Central  Google Scholar 

  19. He M, Dijkstra FA. Phosphorus addition enhances loss of nitrogen in a phosphorus-poor soil[J]. Soil Biol Biochem. 2015;82:99–106.

    Article  CAS  Google Scholar 

  20. Liu L, Gundersen P, Zhang T, Mo J. Effects of phosphorus addition on soil microbial biomass and community composition in three forest types in tropical China. Soil Biol Bioch. 2012;44(1):31–8.

    Article  CAS  Google Scholar 

  21. Mori T, Lu X, Aoyagi R, Mo J. Reconsidering the phosphorus limitation of soil microbial activity in tropical forests. Funct Ecol. 2018;32(5):1145–54.

    Article  Google Scholar 

  22. Feng J, Zhu B. A global meta-analysis of soil respiration and its components in response to phosphorus addition. Soil Biol Bioch. 2019;135:38–47.

    Article  CAS  Google Scholar 

  23. Rodríguez D, Zubillaga MM, Ploschuk EL, Keltjens WG, Goudriaan J, Lavado RS. Leaf area expansion and assimilate production in sunflower (Helianthus annuus L.) growing under low phosphorus condition. Plant Soil. 1998;202(1):133–47.

    Article  Google Scholar 

  24. Turnbull TL, Warren CR, Adams MA. Novel mannose-sequestration technique reveals variation in subcellular orthophosphate pools do not explain the effects of phosphorus nutrition on photosynthesis in Eucalyptus globulus seedlings. New Phytol. 2007;176(4):849–61.

    Article  CAS  PubMed  Google Scholar 

  25. Defoliart LS, Griffith M, Chapin III FS, Jonasson S. Seasonal patterns of photosynthesis and nutrient storage in Eriophorum vaginatum L. an arctic sedge. Funct Ecol. 1988;2:185–94.

  26. Chapin III FS, Shaver,GR. Differences in growth and nutrient use among arctic plant growth forms. Funct Ecol. 1989;3:73–80.

  27. Bubier JL, Smith R, Juutinen S, Moore TR, Minocha R, Long S, Minocha S. Effects of nutrient addition on leaf chemistry, morphology, and photosynthetic capacity of three bog shrubs. Oecologia. 2011;167(2):355–68.

    Article  PubMed  Google Scholar 

  28. Chen ZF, Xiong PF, Zhou JJ, Lai SB, Jian CX, Wang Z, Xu BC. Photosynthesis and nutrient-use efficiency in response to N and P addition in three dominant grassland species on the semiarid Loess Plateau. Photosynthetica. 2020;58(4):1028–39.

    Article  CAS  Google Scholar 

  29. Hikosaka K. Interspecific difference in the photosynthesis–nitrogen relationship: patterns, physiological causes, and ecological importance. J Plant Res. 2004;117(6):481–94.

    Article  PubMed  Google Scholar 

  30. Mao Q, Lu X, Mo H, Gundersen P, Mo J. Effects of simulated N deposition on foliar nutrient status, N metabolism and photosynthetic capacity of three dominant understory plant species in a mature tropical forest. Sci Total Environ. 2018;610:555–62.

    Article  PubMed  CAS  Google Scholar 

  31. Liu M, Wang Y, Li Q, Xiao W, Song X. Photosynthesis, ecological stoichiometry, and non-structural carbohydrate response to simulated nitrogen deposition and phosphorus addition in chinese fir forests. Forests. 2019;10(12):1068.

    Article  Google Scholar 

  32. Simpson AC, Zabowski D, Rochefort RM, Edmonds RL. Increased microbial uptake and plant nitrogen availability in response to simulated nitrogen deposition in alpine meadows. Geoderma. 2019;336:68–80.

    Article  CAS  Google Scholar 

  33. Yan Y & Xuyang, L. Are N, P, and N: P stoichiometry limiting grazing exclusion effects on vegetation biomass and biodiversity in alpine grassland?. Glob Ecol Conse. 2020;24:e01315.

  34. Liu Y, Xu X, Wei D, Wang Y, Wang Y. Plant and soil responses of an alpine steppe on the Tibetan Plateau to multi-level nitrogen addition. Plant Soil. 2013;373(1–2):515–29.

    Article  CAS  Google Scholar 

  35. Zong N, Shi P, Song M, Zhang X, Jiang J, Chai X. Nitrogen critical loads for an alpine meadow ecosystem on the Tibetan Plateau. Environ Manage. 2016;57(3):531–42.

    Article  PubMed  Google Scholar 

  36. Xiao J, Dong S, Shen H, Li S, Zhi Y, Mu Z, Ding C. Phosphorus addition promotes Nitrogen retention in alpine grassland plants while increasing N deposition. CATENA. 2022;210: 105887.

    Article  CAS  Google Scholar 

  37. Han Y, Dong S, Zhao Z, Sha W, Li S, Shen H, Yeomans JC. Response of soil nutrients and stoichiometry to elevated nitrogen deposition in alpine grassland on the Qinghai-Tibetan Plateau. Geoderma. 2019;343:263–8.

    Article  CAS  Google Scholar 

  38. Niu K, He JS, Lechowicz MJ. Grazing-induced shifts in community functional composition and soil nutrient availability in Tibetan alpine meadows. J Appl Ecol. 2016;53(5):1554–64.

    Article  CAS  Google Scholar 

  39. Benítez-López A, Santini L, Gallego-Zamorano J, Milá B, Walkden P, Huijbregts MA, Tobias JA. The island rule explains consistent patterns of body size evolution in terrestrial vertebrates. Nat Ecol Evol. 2021;5(6):768–86.

    Article  PubMed  Google Scholar 

  40. Fang H, Cheng S, Yu G, Zheng J, Zhang P, Xu M, Yang X. Responses of CO2 efflux from an alpine meadow soil on the Qinghai Tibetan Plateau to multi-form and low-level N addition. Plant Soil. 2012;351(1–2):177–90.

    Article  CAS  Google Scholar 

  41. Ding J, Yang T, Zhao Y, Liu D, Wang X, Yao Y, Piao S. Increasingly important role of atmospheric aridity on Tibetan alpine grasslands. Geophys Res Lett. 2018;45(6):2852–9.

    Article  Google Scholar 

  42. Möhl P, Hiltbrunner E, Körner C. Halving sunlight reveals no carbon limitation of aboveground biomass production in alpine grassland. Global Change Biol. 2020;26(3):1857–72.

    Article  Google Scholar 

  43. Gough L, Osenberg CW, Gross KL, Collins SL. Fertilization effects on species density and primary productivity in herbaceous plant communities. Oikos. 2000;89(3):428–39.

    Article  Google Scholar 

  44. Xu B, Gao Z, Wang J, Xu W, Palta JA, Chen Y. N: P ratio of the grass Bothriochloa ischaemum mixed with the legume Lespedeza davurica under varying water and fertilizer supplies. Plant Soil. 2016;400(1–2):67–79.

    Article  CAS  Google Scholar 

  45. Shen H, Dong S, Li S, Xiao J, Han Y, Yang M, Yeomans JC. Effects of simulated N deposition on photosynthesis and productivity of key plants from different functional groups of alpine meadow on Qinghai-Tibetan plateau. Environ Pollut. 2019;251:731–7.

    Article  CAS  PubMed  Google Scholar 

  46. Shen H, Dong S, DiTommaso A, Li S, Xiao J, Yang M, Xu J. Eco-physiological processes are more sensitive to simulated N deposition in leguminous forbs than non-leguminous forbs in an alpine meadow of the Qinghai-Tibetan Plateau. Sci Total Environ. 2020;744: 140612.

    Article  CAS  PubMed  Google Scholar 

  47. Ye XH, Yu FH, Dong M. A trade-off between guerrilla and phalanx growth forms in Leymus secalinus under different nutrient supplies. Ann Bot. 2006;98(1):187–91.

    Article  PubMed  PubMed Central  Google Scholar 

  48. Cui G, Li B, He W, Yin X, Liu S, Lian L, Zhang P. Physiological analysis of the effect of altitudinal gradients on Leymus secalinus on the Qinghai-Tibetan Plateau. PLoS ONE. 2018;13(9): e0202881.

    Article  PubMed  PubMed Central  CAS  Google Scholar 

  49. You C, Wu F, Gan Y, Yang W, Hu Z, Xu Z, Ni X. Grass and forbs respond differently to nitrogen addition: a meta-analysis of global grassland ecosystems. Sci Rep. 2017;7(1):1–10.

    Article  CAS  Google Scholar 

  50. Elmqvist T, Folke C, Nyström M, Peterson G, Bengtsson J, Walker B, Norberg J. Response diversity, ecosystem change, and resilience. Front Ecol Environ. 2003;1(9):488–94.

    Article  Google Scholar 

  51. Lü XT, Reed S, Yu Q, He NP, Wang ZW, Han XG. Convergent responses of nitrogen and phosphorus resorption to nitrogen inputs in a semiarid grassland. Global Change Biol. 2013;19(9):2775–84.

    Article  Google Scholar 

  52. Holub P, Tůma I, Záhora J, Fiala K. Different nutrient use strategies of expansive grasses Calamagrostis epigejos and Arrhenatherum elatius. Biologia. 2012;67(4):673–80.

    Article  Google Scholar 

  53. Bauer GA, Bazzaz FA, Minocha R, Long S, Magill A, Aber J, Berntson GM. Effects of chronic N additions on tissue chemistry, photosynthetic capacity, and carbon sequestration potential of a red pine (Pinus resinosa Ait.) stand in the NE United States. Forest Ecol Manag. 2004;196(1):173–86.

    Article  Google Scholar 

  54. Bai T, Li C, Li C, Liang D, Ma F. Contrasting hypoxia tolerance and adaptation in Malus species is linked to differences in stomatal behavior and photosynthesis. Physiol Plantarum. 2013;147(4):514–23.

    Article  CAS  Google Scholar 

  55. Messinger SM, Buckley TN, Mott KA. Evidence for involvement of photosynthetic processes in the stomatal response to CO2. Plant Physiol. 2006;140(2):771–8.

    Article  CAS  PubMed  PubMed Central  Google Scholar 

  56. Xiong D, Liu XI, Liu L, Douthe C, Li Y, Peng S, Huang J. Rapid responses of mesophyll conductance to changes of CO2 concentration, temperature and irradiance are affected by N supplements in rice. Plant Cell Environ. 2015;38(12):2541–50.

    Article  CAS  PubMed  Google Scholar 

  57. Chen S, Bai Y, Zhang L, Han X. Comparing physiological responses of two dominant grass species to nitrogen addition in Xilin River Basin of China. Environ Exp Bot. 2005;53(1):65–75.

    Article  Google Scholar 

  58. Varone L, Ribas-Carbo M, Cardona C, Gallé A, Medrano H, Gratani L, Flexas J. Stomatal and non-stomatal limitations to photosynthesis in seedlings and saplings of Mediterranean species pre-conditioned and aged in nurseries: Different response to water stress. Environ Exp Bot. 2012;75:235–47.

    Article  CAS  Google Scholar 

  59. Kinugasa T, Tsunekawa A, Shinoda M. Increasing nitrogen deposition enhances post-drought recovery of grassland productivity in the Mongolian steppe. Oecologia. 2012;170(3):857–65.

    Article  PubMed  Google Scholar 

  60. Fay PA, Prober SM, Harpole WS, Knops JM, Bakker JD, Borer ET, Adler PB. Grassland productivity limited by multiple nutrients. Nat Plants. 2015;1(7):1–5.

    Article  CAS  Google Scholar 

  61. Zhang Y, Feng J, Isbell F, Lü X, Han X. Productivity depends more on the rate than the frequency of N addition in a temperate grassland. Sci Rep. 2015;5(1):1–12.

    Google Scholar 

  62. Siemann E. Experimental tests of effects of plant productivity and diversity on grassland arthropod diversity. Ecology. 1998;79(6):2057–70.

    Article  Google Scholar 

  63. Yang Z, Hautier Y, Borer ET, Zhang C, Du G. Abundance-and functional-based mechanisms of plant diversity loss with fertilization in the presence and absence of herbivores. Oecologia. 2015;179(1):261–70.

    Article  PubMed  Google Scholar 

  64. Waring BG, Pérez-Aviles D, Murray JG, Powers JS. Plant community responses to stand-level nutrient fertilization in a secondary tropical dry forest. Ecology. 2019;100(6): e02691.

    Article  PubMed  Google Scholar 

  65. Bowman WD, Cleveland CC, Halada Ĺ, Hreško J, Baron JS. Negative impact of nitrogen deposition on soil buffering capacity. Nat Geosci. 2008;1(11):767–70.

    Article  CAS  Google Scholar 

  66. Wu Q, Ren H, Wang Z, Li Z, Liu Y, Wang Z, Han G. Additive negative effects of decadal warming and nitrogen addition on grassland community stability. J Ecol. 2020;108(4):1442–452.

  67. Mo J, Zhang WEI, Zhu W, Gundersen PER, Fang Y, Li D, Wang HUI. Nitrogen addition reduces soil respiration in a mature tropical forest in southern China. Global Change Biol. 2008;14(2):403–12.

    Article  Google Scholar 

  68. Seastedt TR, Vaccaro L. Plant species richness, productivity, and nitrogen and phosphorus limitations across a snowpack gradient in alpine tundra, Colorado. USA Arct Antarct Alp Res. 2001;33(1):100–6.

    Article  Google Scholar 

  69. Lu X, Mao Q, Gilliam FS, Luo Y, Mo J. Nitrogen deposition contributes to soil acidification in tropical ecosystems. Global Change Biol. 2014;20(12):3790–801.

    Article  Google Scholar 

  70. Xu D, Fang X, Zhang R, Gao T, Bu H, Du G. Influences of nitrogen, phosphorus and silicon addition on plant productivity and species richness in an alpine meadow. AoB Plants. 2015;7:1–12.

  71. Nie X, Yang L, Li F, Xiong F, Li C, Zhou G. Storage, patterns and controls of soil organic carbon in the alpine shrubland in the Three Rivers Source Region on the Qinghai-Tibetan Plateau. CATENA. 2019;178:154–62.

    Article  CAS  Google Scholar 

  72. Nie X, Wang D, Ren L, Ma K, Chen Y, Yang L, Zhou G. Distribution characteristics and controlling factors of soil total nitrogen: phosphorus ratio across the northeast tibetan plateau shrublands. Front Plant Sci. 2022;13:825817.

Download references

Acknowledgements

We would like to express our sincere thanks to all the co-authors of this study. We are also grateful to editors and anonymous reviewers for their productive comments.

Funding

This work was supported by grants from the Second Tibetan Plateau Scientific Expedition and Research Program (2019QZKK0307), National Key R & D Program of China (2016YFC0501906), Qinghai Provincial Key R & D program in Qinghai Province (2019-SF-145 & 2018-NK-A2).

Author information

Authors and Affiliations

Authors

Contributions

H.S. analyzed the data and wrote this paper. J. X. and Y. Z. gave field and laboratory assistance of this study. S. D. helped revising this paper. The author(s) read and approved the final manuscript.

Corresponding author

Correspondence to Shikui Dong.

Ethics declarations

Ethics approval and consent to participate

Experimental research and field studies on plants complies with relevant institutional, national, and international guidelines and legislation.

All plant species are not rare plants for protection. We have the permission to collect the plant samples by the local government. Our work reported here complies with the current laws of China and the IUCN Policy Statement on Research Involving Species at Risk of Extinction.

Consent for publication

Not applicable.

Competing interests

The authors declare that they have no competing interests.

Additional information

Publisher’s Note

Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Supplementary Information

Additional file 1: Table S1

. Soil pH and available nutrients variation under N and P addition.

Rights and permissions

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/. The Creative Commons Public Domain Dedication waiver (http://creativecommons.org/publicdomain/zero/1.0/) applies to the data made available in this article, unless otherwise stated in a credit line to the data.

Reprints and Permissions

About this article

Verify currency and authenticity via CrossMark

Cite this article

Shen, H., Dong, S., Xiao, J. et al. Effects of N and P enrichment on plant photosynthetic traits in alpine steppe of the Qinghai-Tibetan Plateau. BMC Plant Biol 22, 396 (2022). https://doi.org/10.1186/s12870-022-03781-9

Download citation

  • Received:

  • Accepted:

  • Published:

  • DOI: https://doi.org/10.1186/s12870-022-03781-9

Keywords

  • Qinghai-Tibetan plateau; alpine steppe
  • N and P enrichment
  • Photosynthesis
  • Biomass