More persistent weather causes a pronounced soil microbial legacy but does not impact subsequent plant communities

Turning Up the Heat: More Persistent Precipitation Regimes Weaken the Micro-Climate Buffering Capacity of Forage Grasses During a Hot Summer

Developing climate-proof forage grasslands does not only require developing plant communities that are soil drought resistant, but also adept at buffering elevated atmospheric temperatures to minimize heat stress for plant and soil. Previous studies indicate that the emerging trend towards rainfall regimes with longer dry and wet spells negatively affects forage grass performance (i.e., greater physiological plant stress and yield loss) in Western Europe. We conducted a 120-day open-air experiment testing whether a hot summer (+3°C for the first 60 days) exacerbates the negative effects of increased persistence in precipitation regimes (PR) (3 vs. 30 days consecutive wet/dry) on the performance of four distinct forage varieties (Dactylis glomerata, Festuca arundinacea, Lolium perenne (tetraploid) and Lolium perenne (diploid)) across two soils differing in management history (permanent vs. temporary grasslands). Our results indicate that climate warming indeed worsens negative effects of more persistent PR on forage grass productivity and physiological plant stress by inducing more extreme soil drought and elevated micro-climatic temperatures, but permanent grassland soils with elevated organic carbon can buffer yields. Moreover, higher yielding varieties are more proficient at buffering soil surface and canopy temperatures and maintaining plant greenness and stomatal opening under water shortage and elevated temperatures (Dactylis and Festuca) were impacted less than those which could not (both Lolium cultivars). These results indicate that not only differences in resource-extraction traits but also the ability of a species to buffer its surrounding microclimatic conditions shapes its response to future climate change. Given the indirect positive effects such temperature-buffering traits may have on soil functioning (e.g., reduced soil respiration during heat waves limiting carbon loss), we argue that managers should also incorporate such traits when developing climate-proof forage grasslands.

Legacy effects of precipitation change: Theories, dynamics, and applications

The intensification of climate-induced precipitation change poses a dual challenge to terrestrial ecosystems: immediate effects on their structure and function, coupled with legacy effects that persist beyond the cessation of precipitation change. Quantifying these legacy effects accurately can greatly assist in assessing the long-term impact of precipitation change. However, their broader understanding is just beginning. Therefore, this review endeavors to synthesize the existing knowledge concerning the legacy effects of precipitation change, elucidating their nature, characteristics, driving factors, and implications, thereby fostering further advancements in this research domain. To begin, we define that precipitation legacies are carried by the information and/or material remnants arising from previous precipitation change, with the enduring impacts of these remnants (precipitation legacy carriers) on the current ecosystem being termed the precipitation legacy effects. To comprehensively investigate the performances of precipitation legacy effects, we introduce a multi-faceted characterization framework, encompassing magnitude, direction, duration, and spatial-temporal variability. This framework is complemented by a proposed sequential analysis approach, spanning the pre-, during, and post-precipitation change phases. Next, we emphasize that the nature of precipitation legacy carriers and the pattern of precipitation change jointly determine the characteristics of precipitation legacy effect. Subsequently, we elucidate the possible carriers of precipitation legacies across species, community, and ecosystem levels, as well as the linkages among these carriers and levels, thereby introducing the underlying formation mechanism of precipitation legacy effects. Lastly, from the perspective of ecosystem stability debt, we propose potential applications of precipitation legacy effects in future climate change research. The viewpoints and methodologies outlined in this review can deepen our comprehension of precipitation legacy effects, contributing to the comprehensive assessment of precipitation impact on soil-vegetation systems and providing guidance for formulating effective strategies to address future climate change.

Can permanent grassland soils with elevated organic carbon buffer negative effects of more persistent precipitation regimes on forage grass performance?

Agricultural practices enhancing soil organic carbon (SOC) show potential to buffer negative effects of climate change on forage grass performance. We tested this by subjecting five forage grass varieties differing in fodder quality and drought/flooding resistance to increased persistence in summer precipitation regimes (PR) across sandy and sandy-loam soils from either permanent (high SOC) or temporary grasslands (low SOC) in adjacent parcels. Over the course of two consecutive summers, monoculture mesocosms were subjected to rainy/dry weather alternation either every 3 days or every 30 days, whilst keeping total precipitation equal. Increased PR persistence induced species-specific drought damage and productivity declines. Soils from permanent grasslands with elevated SOC buffered plant quality, but buffering effects of SOC on drought damage, nutrient availability and yield differed between texture classes. In the more persistent PR, Festuca arundinacea FERMINA was the most productive species but had the lowest quality under both ample water supply and mild soil drought, whilst under the most intense soil droughts, Festulolium FESTILO maintained the highest yields. The hybrid Lolium × boucheanum kunth MELCOMBI had intermediate productivity and both Lolium perenne varieties showed the lowest yields under soil drought, but the highest forage quality (especially the tetraploid variety MELFORCE). Performance varied with plant maturity stage and across seasons/years and was driven by altered water and nutrient availability and related nitrogen nutrition among species during drought and upon rewetting. Moreover, whilst permanent grassland soils showed the most consistent positive effects on plant performance, their available water capacity also declined under increased PR persistence. We conclude that permanent grassland soils with historically elevated SOC likely buffer negative effects of increasing summer weather persistence on forage grass performance, but may also be more sensitive to degradation under climate change.