Environmental changes in biodiversity hotspot ecosystems of
South Ecuador: RESPonse and feedback effECTs (FOR2730)

Abstract:

Ferns are known to have a lower incidence of mycorrhization than angiosperms. It has been suggested that this results from carbon being more limiting to fern growth than nutrient availability, but this assertion has not been tested yet. In the present study, we took advantage of a fertilization experiment with nitrogen and phosphorus on cloud forest plots of the Ecuadorean Andes for 15 years. A previous analysis revealed changes in the abundances of fern species in the fertilized plots compared to the control plots and hypothesized that this might be related to the responses of the mycorrhizal relationships to nutrient availability. We revisited the plots to assess the root-associated fungal communities of two epiphytic and two terrestrial fern species that showed shifts in abundance. We sampled and analyzed the roots of 125 individuals following a metabarcoding approach. We recovered 1382 fungal ASVs, with a dominance of members of Tremellales (Basidiomycota) and Heliotales (Ascomycota). The fungal diversity was highly partitioned with little overlap between individuals. We found marked differences between terrestrial and epiphytic species, with the latter fundamentally missing arbuscular mycorrhizal fungi (AMF). We found no effect of fertilization on the diversity or relative abundance of the fungal assemblages. Still, we observed a direct impact of phosphorus fertilization on its concentration in the fern leaves. We conclude that fern–fungi relationships in the study site are not restricted by nutrient availability and suggest the existence of little specificity on the fungal partners relative to the host fern species.

Abstract:

Ecosystem services, provided from tropical forests, are indispensable for human beings. Coherencies in the system, their networks, drivers and various underlying pathways are not completely understood yet. Elucidation on directions of key nutrients and changes in organisms delivers the opportunity to get an overview about these relations. Leaf functional traits are one important component to uncover those cascades and organizations. With their fast respond to environmental conditions, changes can be detected. Since, tropical regions suffer from increasing atmospheric inputs of nitrogen (N) and phosphorus (P), it is a need to investigate these progressions and predict future scenarios. The alarming fact, that these anthropogenic caused input have unknown consequences for the structure and functioning of tropical forests leads to a crucial study topic. Furthermore, questions should be answered if these increased inputs have a comparable influence on different elevations, based on identification the limiting nutrients. To forecast these impacts the Nutrient Manipulation Experiment (NUMEX) has been conducted since 2008. It gained to show, that Neotropical montane forests respond rapidly to moderate nutrient additions of N (50 kg ha-1 yr-1) and P (10 kg ha-1 yr-1). Within the present study, the eight most abundant tree species from the NUMEX sites were analyzed to their leaf functional traits from three elevations (altitude above sea level) in an Ecuadorian montane forest. The premontane forest in Bombuscaro (1,000 m) contains the species Clarisia racemosa and Pouteria torta. Further, in San Francisco (2,000 m), Alchornea lojaensis, Graffenrieda emarginata, Hieronyma fendleri, and Myrcia sp., were selected. In Cajanuma (3,000 m), the upper montane forest contains Hedyosmum purpurascens and Weinmannia loxensis. The fertilization effects were calculated, using a mixed effect model, including study year and treatment as fixed effects and block and individual as random effects. The results show, that foliar N decrease over the years, whereas, Foliar P conversely increases. Further, the relation of nitrogen and phosphorus (N:P) is decreasing during the study years. Upwards trends for ?15N are best replicated for the San Francisco site. With the leaf trait nutrient resorption efficiency (NuR) for N and P a decline over the study years is proceeding. In addition, leaf area (LA) and specific leaf area (SLA) tend to decrease. In conclusive processes over the study years might be the result of microclimatic events. The sites differ in that San Francisco and Cajanuma respond more similar in some leaf functional traits, compared to them from Bombuscaro. It can be deduced that changes in the analyzed leaf traits over the last eight years between the sites and species are not significantly different. Summarizing, results represent the emphasis on the considerable influence of nutrient addition with notably changing foliar nutrient and show that the predicted nutrient deposition will probably change the ecosystem dynamics sustained.

Abstract:

Tropical montane forests of the Andes belong to the hotspots of biodiversity. But these nutrient poor ecosystems are simultaneously threatened by increased element inputs of nitrogen and phosphor in nutrient cycles. NUMEX-Projekt simulates the expected nutrient inputs in the for-ests and quantifies the changes of this ecosystem. In line of this study litter samples were collected by littertraps during a working period from February till May 2016. Leaf litter produc-tion, parameters of leaf morphology (leaf area and specific leaf area) and litter nutrients of nitrogen and phosphor were determined. Additionally, the parameters of herbivory (leaf mass loss and leaf area loss) were calculated by measuring holes area. The variation of these pa-rameters along an altitudinal gradient from 1.000 m.a.s.l. to 3.000 m.a.s.l. was investigated. Besides the variation after nitrogen and/or phosphor addition was explored. Furthermore, the extend of nutrients, lost through herbivory, was identified for the stand level. Terminatory the influence of two soil parameters (C/N ratio and Presin) was discussed. There is a significant influence of altitude (p<0,05) on leaf morphology (leaf area: 1.000 m.a.s.l: 26,4±1,6 cm², 3.000 m.a.s.l: 7,4±1,0 cm², specific leaf area: 1.000 m.a.s.l: 99,7±4,1 cm²·g-1, 3.000 m.a.s.l: 56,1±6,6 cm²·g-1), leaf nutrients of nitrogen (1.000 m.a.s.l: 15,3±0,5 g·kg-1, 3.000 m.a.s.l: 6,6±0,7 g·kg-1) and phosphor (1.000 m.a.s.l: 0,54±0,03 g·kg-1, 3.000 m.a.s.l: 0,25±0,03 g·kg-1) and also on the parameters of herbivory: holes area (1.000 m.a.s.l: 1,8±0,2 cm², 3.000 m.a.s.l: 0,3±0,1 cm²) and leaf area loss (1.000 m.a.s.l: 6,8±0,4 %, 3.000 m.a.s.l: 3,6±0,6 %). Nutrient addition did not lead to distinct results according to the variation of measured param-eters. NP fertilization had a positive effect on leaf area and P fertilization a positive effect on specific leaf area. Leaf nutrients showed various answers. For this parameter, NP fertilization causes significantly raised nitrogen and phosphor concentrations in litter in each site. Leaf litter production in 1.000 m.a.s.l site significantly decreased through NP fertilization. Referring to herbivory only a little number of significant effects were detected. Holes area increased on 2.000 m.a.s.l site by NP addition while leaf area loss in 1.000 m.a.s.l site – as well as leaf area production – decreased. On stand level, there was no variation of leaf area loss. Soil parameters have a higher impact on measured parameters on stand level. Specific leaf area and leaf area loss correlate positively with soil C/N of upper mineral soil. Correlations of these parameters with plant available phosphor Presin is negative. Nutrient losses on stand level decrease with altitude. There was a negative effect of NP addition on nitrogen loss in 1.000 m.a.s.l site and a positive effect of NP addition on phosphor loss in all sites.

Abstract:

Atmospheric nutrient deposition and climate change are expected to endanger the diversity of tropical forest ecosystems. Nitrogen (N) deposition might influence nutrient fluxes beyond the N cycle by a concomitant increased demand for other nutritional elements such as phosphorus (P). Organisms might respond to the increased P demand by enhanced activity of enzymes involved in releasing inorganic P from organic matter (OM). Our aims were to assess the effect of i) climate shifts (approximated by an altitudinal gradient), and ii) nutrient addition (N, P, N+P) on phosphatase activity (PA) in organic layer and mineral soil of a tropical montane rainforest in Southern Ecuador. A nutrient manipulation experiment (NUMEX) was set up along an altitudinal gradient (1000, 2000, and 3000 m a.s.l.). We determined PA and inorganic and total P concentrations. PA at 1000 m was significantly lower (mean ± standard error: 48 ± 20 µmol p-NP g-1 dm h-1) as compared to 2000 m and 3000 m (119 ± 11 and 137 ± 19, respectively). One explanation might be that very rapid decomposition of OM at 1000 m results in very thin organic layers reducing the stabilization of enzymes and thus, resulting in leaching loss of enzymes under the humid tropical climate. We found no effect of N addition on PA neither in the organic layer nor in mineral soil, probably because of the low nutrient addition rates that showed ambiguous results so far on productivity measures as a proxy for P demand. In the organic layers of P and N+P treatments, we found decreased PA and increased concentrations of inorganic P. This indicates that the surplus of inorganic P reduced the biosynthesis of phosphatase enzymes. PA in megadiverse montane rainforests is likely to be unaffected by increased atmospheric N deposition but reduced upon atmospheric P deposition.

Abstract:

Regarding woody plant responses on higher atmospheric inputs of the macronutrients nitrogen (N) and phosphorous (P) on tropical forests in the future, an adaptive modification of wood anatomical traits on the cellular level of woody plants is expected. As part of an interdisciplinary nutrient manipulation experiment (NUMEX) carried out in Southern Ecuador, we present here the first descriptive and quantitative wood anatomical analysis of the tropical evergreen tree species Alchornea lojaensis (Euphorbiaceae). We sampled branch wood of nine individual trees belonging to treatments with N fertilization, N+P fertilization, and a control group, respectively. Quantitative evaluations of eleven different vessel parameters were conducted. The results showed that this endemic tree species will be able to adapt well to the future effects of climate change and higher nutrient deposition. This was firstly implied by an increase in vessel diameter and consequently a higher theo. area-specific hydraulic conductivity with higher nutrient availability. Secondly, the percentage of small vessels (0–20 ?m diameter) strongly increased with fertilization. Thirdly, the vessel arrangement (solitary vessels vs. multiple vessel groupings) changed toward a lower percentage of solitary vessel fraction (VS), and concurrently toward a higher total vessel grouping index (VG) and a higher mean group size of non-solitary vessels (VM) after N and N+P addition. We conclude that higher nutrient availability of N and N+P triggered higher foliage amount and water demand, leading to higher cavitation risk in larger vessels. This is counteracted by a stronger grouping of vessels with smaller risk of cavitation to ensure water supply during drier periods that are expected to occur in higher frequency in the near future.

Abstract:

A tropical smallholder cash crop farming system in a semi-arid Inter-Andean valley of Ecuador was investigated. Intensive irrigated agriculture with up to 400 kg of urea-N fertilization ha?1·a?1 prevails in colluvial sites whereas urea application in the steep eroded sites is lower. Farmers did recently introduce manure to partly replace urea fertilization. Knowledge about the effects of mineral and organic fertilizers on nitrogen and carbon cycling needs to be improved to maintain sustainable agriculture in the research area. Therefore, a laboratory incubation experiment was conducted to investigate effects of urea and guinea pig manure on microbial activity of colluvial foot slope and eroded upper slope soils. Soil samples were treated with 200 kg·N·ha?1 either applied as urea, guinea pig manure or a combination of both and compared to a control. Urea fertilizer was labeled with 15N to trace its fate. Microbial biomass and basal respiration were determined in different time intervals. Urea fertilization induced an acceleration of soil organic matter (SOM) mineralization (positive priming effect) in the first seven days of incubation. The combined fertilization served as a positive alternative to the present urea management since it increased the amount of microbial biomass and provided mineral nitrogen for immediate plant uptake. Moreover, low recovery rates suggested an immobilization of fertilized nitrogen into the microbial biomass inducing an efficient and sustained nutrient release throughout the entire growing season. SOM stocks in colluvial soils were 40% below those of eroded soils which was partly due to the positive priming effect after urea fertilization. Microbial activity and efficiency were not reduced by soil erosion.