October 2024
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Trends in Ecology & Evolution
The movement, distribution, and relative proportions of essential elements across the landscape should influence the structure and functioning of biological communities. Yet, our basic understanding of the spatial distribution of elements, particularly bioavailable elements, across landscapes is limited. Here, we propose a quantitative framework to study the causes and consequences of spatial patterns of elements. Specifically, we integrate distribution models, dissimilarity metrics, and spatial smoothing to predict how the distribution of bioavailable elements changes with spatial extent. Our community and landscape ecology perspective on elemental diversity highlights the characteristic relationships that emerge among elements in landscapes and that can be measured empirically to help us pinpoint ecosystem control points. This step forward provides a mecha-nistic link between community and ecosystem processes. Biotic-abiotic feedbacks connect ecosystems across landscapes The distribution and relative abundance of the 25 chemical elements (see Glossary) necessary for life influence the structure and function of biological communities. However, our basic understanding of the causes and consequences of the spatial distribution of elements is limited. Historically , geological processes and abiotic factors have been the focus for predicting elemental concentrations at small, well-defined spatial extents (e.g., ponds) [1]. More recently, research has shed light on the significance of biotic ecosystem components, particularly biotic-abiotic feedback loops, on elemental distribution and abundance (Figure 1) [2-6]. Thus, the analyses of the spatial distribution of elements may be critical for forecasting the fate of biological communities in the Anthropocene. Spatial patterns of elemental abundances result from combined feedbacks of passive abiotic flows and biotic ecosystem components (e.g., animal deposition of materials) acting at different spatial and temporal scales (Figure 1). At a broad spatial extent, weathering of bedrock builds an elemental pool that is then distributed via abiotic and biotic processes [7]. At smaller spatial extents, abiotic processes, such as the mixing of nutrient-rich ground water and nutrient-poor surface water, create local elemental hotspots or elemental coldspots of inorganic nitrogen (N) [8,9]. These hotspots of N can then get redistributed via abiotic and biotic processes, including daily movements of organisms (Figure 1). At small spatial extents, animals with relatively small home ranges (e.g., snowshoe hares, Lepus americanus, or Arctic foxes, Vulpes lagopus), may contribute to localized elemental hotspots [10], such as the build-up of nutrients around Arctic fox den sites [11]. Biotic processes can also operate at larger spatial scales. For example, moose (Alces alces) home ranges include a diversity of habitats, including early successional forests used for foraging and mature forests used for shelter. Selective herbivory by moose in foraging patches removes nutritious understory plants with relatively high N and P content [12]. Highlights Complex biotic and abiotic feedbacks affect the spatial distribution of the 25 elements necessary for life, but most studies focus on only biotic or abiotic components at small spatial extents. Plants and animals not only affect, but also respond to the distribution and stoichiometry of elements; thus, understanding geodiversity is critical to improve our understanding of species distributions and ecosystem function. Meta-ecosystem theory has already started to demonstrate how the feedback between biotic and abiotic components of ecosystems can impact community structure and function; however, we need an empirical parallel. Here, we propose a framework that applies tools from community and landscape ecology to study and analyze spatial scaling of elements across landscapes. This will allow us to quantify how spatial patterns in elements vary across spatial scales.