Desafíos y oportunidades del cambio global para la sostenibilidad en Centroamérica

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[Introduction]: Global change presents pressing challenges for Central America, including increasing hydrometeorological disasters, environmental pollution, and soil degradation. [Objetive]: This study examines socio-environmental trends from 1990 to 2020 using comprehensive datasets from the World Bank and EM-DAT. [Methodology]: Through country-specific correlation analyses, we uncover complex statistical relationships between socioeconomic and environmental variables. [Results]: The findings highlight critical interactions, such as the link between economic diversification away from agriculture and GDP growth, which is paradoxically accompanied by rising CO2 emissions. Renewable energy consumption emerges as a pivotal factor in mitigating carbon footprints, while sustainable freshwater management is shown to be essential for long-term economic resilience. [Conclusions]: These results offer valuable insights into the dynamics of economic growth, agricultural practices, and environmental sustainability in the region. By addressing these multifaceted challenges through coordinated and integrated strategies, Central America could enhance regional perspective and potential research gaps, safeguard its natural resources, and foster a sustainable and resilient future through international, regional and national institutions initiatives and projects.

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Abstract. Agricultural land covers 5.1×109 ha (ca. 50 % of potentially suitable land area), and agriculture has immense effects on soil formation and degradation. Although we have an advanced mechanistic understanding of individual degradation processes of soils under agricultural use, general concepts of agropedogenesis are absent. A unifying theory of soil development under agricultural practices, of agropedogenesis, is urgently needed. We introduce a theory of anthropedogenesis – soil development under the main factor “humankind” – the sixth factor of soil formation, and deepen it to encompass agropedogenesis as the most important direction of anthropedogenesis. The developed theory of agropedogenesis consists of (1) broadening the classical concept of factors→processes→properties→functions along with their feedbacks to the processes, (2) a new concept of attractors of soil degradation, (3) selection and analysis of master soil properties, (4) analysis of phase diagrams of master soil properties to identify thresholds and stages of soil degradation, and, finally, (5) a definition of the multidimensional attractor space of agropedogenesis. The main feature of anthropedogenesis is the narrowing of soil development to only one function (e.g. crop production for agropedogenesis), and this function is becoming the main soil-forming factor. The focus on only one function and the disregard of other functions inevitably lead to soil degradation. We show that the factor humankind dominates over the effects of the five natural soil-forming factors and that agropedogenesis is therefore much faster than natural soil formation. The direction of agropedogenesis is largely opposite to that of natural soil development and is thus usually associated with soil degradation. In contrast to natural pedogenesis leading to divergence of soil properties, agropedogenesis leads to their convergence because of the efforts to optimize conditions for crop production. Agricultural practices lead soil development toward a quasi-steady state with a predefined range of measured properties – attractors (an attractor is a minimal or maximal value of a soil property toward which the property will develop via long-term intensive agricultural use from any natural state). Based on phase diagrams and expert knowledge, we define a set of “master properties” (bulk density and macroaggregates, soil organic matter content, C:N ratio, pH and electrical conductivity – EC, microbial biomass and basal respiration) as well as soil depth (A and B horizons). These master properties are especially sensitive to land use and determine the other properties during agropedogenesis. Phase diagrams of master soil properties help identify thresholds and stages of soil degradation, each of which is characterized by one dominating process. Combining individual attractors in a multidimensional attractor space enables predicting the trajectory and the final state of agrogenic soil development and developing measures to combat soil degradation. In conclusion, the suggested new theory of anthro- and agropedogenesis is a prerequisite for merging various degradation processes into a general view and for understanding the functions of humankind not only as the sixth soil-forming factor but also as an ecosystem engineer optimizing its environment to fulfil a few desired functions.

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