Over the past three decades, growing concerns about biodiversity loss have driven extensive research focused on experimentally manipulating plant species richness to investigate its impact on ecosystem functioning1,2. Experimental studies have demonstrated a positive relationship between plant diversity and ecosystem functioning1, which tends to increase over time3,4,5,6,7,8,9. This is a significant finding, as it suggests that experimental results obtained from young, recently established communities likely underestimate the consequences of biodiversity loss while emphasizing the importance of conserving older, species-rich ecosystems10.
Changes in biotic and abiotic processes over time, which can only be observed in long-term experiments, are one possible explanation for the amplifying effects of biodiversity on ecosystem functioning. High plant diversity has been associated with increases in soil carbon and nutrient concentrations3,9,11,12,13, optimized resource complementarity3,8,14, enhanced niche differentiation among plants15, accumulation of mutualists at all trophic levels10,16, and diminished threats from pathogens and herbivores via stronger top-down regulatory mechanisms17,18,19. Conversely, low plant diversity has been associated with selective pressure toward increased investment in plant defenses and less efficient resource use10,20,21,22. Taken together, differences in multitrophic community assembly and biotic interactions in high- versus low-diversity plant communities are hypothesized to influence plant performance by altering consumer community structure and function, as well as driving plastic or micro-evolutionary changes of plant species at the level of plant communities23,24,25,26. To resolve the complex interplay of community history, these effects were separated into two important components: plant history and soil history. Plant history refers to all plant responses to past abiotic and biotic selection pressures experienced in their respective communities, whereas soil history relates to all abiotic and biotic soil properties developed as a result of plant-soil interactions23,24,27,28. Both components are increasingly recognized as key drivers in long-term biodiversity effects29,30,31.
Experimental field studies provide valuable insights into the long-term effects of soil and plant history under realistic environmental conditions and on a large spatial scale32,33. However, field experiments are subject to various uncontrolled external factors, such as weather fluctuations, natural disturbances, and interactions with other organisms. In contrast, small-scale microcosm experiments, while limited in capturing the complexity and dynamics of natural ecosystems, offer precise control over abiotic factors like temperature, light, and water34. To combine the advantages of both approaches, novel experimental facilities called 'Ecotrons' emerged in the 1990s (e.g., Ecotron in Silkwood, UK34; Ecotron in Montpellier, France35; Ecotron in Hasselt, Belgium36). Roy et al. (2021)37 define an Ecotron as an experimental facility consisting of replicated enclosures designed to accomodate ecosystem samples, allowing realistic simulation of above- and below-ground environmental conditions while facilitating the simultaneous and automated measurement of ecosystem processes. Thus, Ecotrons enable the integrated study of complex ecosystem processes, multitrophic interactions, and ecosystem functions. They can harbor a variety of above- and below-ground organisms from multiple trophic levels in a large series of independent mesocosm chambers, enabling precise controlling and monitoring of environmental conditions in both above- and below-ground systems37,38.
In this study, we set up an experiment in the iDiv Ecotron38,39, referred to as the "JenaTron Experiment" (Figure 1 and Figure 2), to test whether biodiversity-ecosystem functioning (BEF) relationships in communities with different levels of plant species richness are modulated by soil history, shared plant history, or a combined effect of both. The iDiv Ecotron is specifically designed for multitrophic biodiversity experiments, focusing on the joint investigation of above- and below-ground interactions in terrestrial ecosystems38,39,40. It comprises 24 identical experimental units, termed 'EcoUnits' (Figure 2F,G), each capable of accommodating up to four individual ecosystems in isolated compartments (Figure 2K), allowing the construction of complex, near-natural ecosystems while minimizing the impact of environmental variability. One key advantage is the capacity to establish multiple replicates of intact soil monoliths (Figure 2A-C) under controlled environmental conditions, which enables the measurement of intricate ecosystem processes, including plant-plant and plant-soil feedback effects, that are often difficult to capture in small-scale microcosm experiments38,39.
In Europe, semi-natural grasslands are among the most biodiverse and complex terrestrial ecosystems, providing vital ecosystem services. However, since the early 20th century, these extensively managed grasslands have faced increasing threats from land-use change, making them a key focus for biodiversity conservation and research. One of the world's longest-running biodiversity experiments on extensively managed grasslands is the Jena Experiment32,33, located in Jena, Germany (50.951°N, 11.621°E, 139 m a.s.l.; website: https://the-jena-experiment.de). Established in 2002, the experiment investigates the relationships between grassland plant diversity and ecosystem functioning, particularly focusing on nutrient cycling and trophic interactions32,33. For the installation of the JenaTron Experiment within the iDiv Ecotron, we utilized the Trait-Based Experiment41 (TBE), a component of the Jena Experiment initiated in 2010 and completed in 2021. In 2022, 23 plots of the TBE were selected to establish a plant diversity gradient ranging from one to six species, spanning over 24 plant communities within the iDiv Ecotron. These communities comprised six grassland plant species, which overlapped with the Main Experiment of the Jena Experiment and represented three grass species (Anthoxanthum odoratum L., Dactylis glomerata L., Holcus lanatus L.) and three forb species (Leucanthemum vulgare agg., Plantago lanceolata L., and Ranunculus acris L.; see Table 1 for details on plant species composition and replicates for each plant diversity level). These species, widespread and frequently coexisting in semi-natural European grasslands, additionally differ in their temporal resource acquisition traits, making them ideal for comprehensive studies of temporal resource use, such as plant phenology41. The 24 plant compositions were randomly assigned to all EcoUnits (Figure 1C), with each EcoUnit further subdivided into four compartments to accommodate the factorial combinations of soil history and plant history treatments.
Soil history (Figure 1A) was established by excavating a total of 96 soil monoliths from the Jena Experiment. The soil of the site is a nutrient-rich floodplain soil classified as Eutric Fluvisol, developed from loamy river sediments32,33. Detailed information regarding soil pH, changes in soil texture, and organic matter within the Jena Experiment soil profile can be found in Lange et al. (2023)9. Of the 96 monoliths, 48 were sourced by excavating two monoliths from each of 22 TBE plots, encompassing monocultures, two- and three-species mixtures. Additionally, four monoliths were taken from an eight-species plot, which will serve as a six-species mixture in the JenaTron Experiment. Each of these 48 soil monoliths (depth: 0.8 m; diameter: 0.5 m) harbored a plot-specific residence community since 2010, thus representing a plant community-specific soil history (+SH). The remaining 48 monoliths were excavated from four bare ground plots that were kept free of vegetation since the initiation of the Jena Experiment in 2002, thus lacking any plant community-specific soil history (-SH). From each of the four bare-ground plots, 12 monoliths were excavated. The two soil history treatments (+SH; -SH) were factorially combined with two plant history treatments by planting pre-grown plants that reflected the plant community-specific composition of the TBE at an equal density, with individual plants spaced 6 cm apart.
Plant history (Figure 1B) was established using two distinct seed sources for each of the selected plant species from the Jena Experiment species pool: The first source consisted of seeds collected from plants that had experienced a community-specific history since 2010, corresponding to the exact Trait-Based Experiment (TBE) plots from which the soil monoliths were excavated (+PH). These seeds were collected from May to September 2019 dependent on species flowering phenology, ensuring a minimum of five individuals per species and plot were sampled. After collection, seeds were cleaned and stored at -20°C until the initiation of the JenaTron Experiment. The second seed source comprised seeds obtained from a commercial seed supplier producing seeds of regional provenances. These seeds were used to establish the TBE plots in 2010, thus representing plants without a community-specific selection history within the Jena Experiment (-PH) and were stored at -20°C from 2010 until the start of the JenaTron Experiment. Both histories of the six perennial plant species were pre-cultivated from February to May 2022 in four chambers of the iDiv research greenhouse located in Leipzig, Germany (51.330°N, 12.393°E, 120 m a.s.l.).
The factorial combination of soil history (SH) and plant history (PH) at each level of plant species richness resulted in four treatments within each of the 24 EcoUnits: (1) with soil history, with plant history (+SH/+PH), (2) with soil history, without plant history (+SH/-PH), (3) without soil history, with plant history (-SH/+PH), and (4) without soil history, without plant history (-SH/-PH; Figure 1C). The primary objective of the JenaTron Experiment is to investigate whether the strengthening relationship between biodiversity and ecosystem functioning is due to soil history, plant history, or a combination of both. We hypothesize that plant communities with shared plant and soil community-specific history will show the strongest BEF relationship, whereas an experimental exclusion of soil history, plant history, or both may have detrimental effects on the positive relationships of plant diversity and ecosystem functioning. Ultimately, if soil or plant history were to alter the relationship between plant species richness and ecosystem functioning, this would serve as an important consideration for the conservation and monitoring of locally preserved and novel restored communities.