Unravelling large-scale patterns and drivers of biodiversity in dry rivers
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2024
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Springer Nature
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Foulquier, A., Datry, T., Corti, R., von Schiller, D., Tockner, K., Stubbington, R., Gessner, M. O., Boyer, F., Ohlmann, M., Thuiller, W., Rioux, D., Miquel, C., Albariño, R., Allen, D. C., Altermatt, F., Arce, M. I., Arnon, S., Banas, D., Banegas-Medina, A., et al. (2024). Unravelling large-scale patterns and drivers of biodiversity in dry rivers. Nature Communications, 15(1). https://doi.org/10.1038/S41467-024-50873-1
Abstract
More than half of the world’s rivers dry up periodically, but our understanding of the biological communities in dry riverbeds remains limited. Specifically, the roles of dispersal, environmental filtering and biotic interactions in driving biodiversity in dry rivers are poorly understood. Here, we conduct a large-scale coordinated survey of patterns and drivers of biodiversity in dry riverbeds. We focus on eight major taxa, including microorganisms, invertebrates and plants: Algae, Archaea, Bacteria, Fungi, Protozoa, Arthropods, Nematodes and Streptophyta. We use environmental DNA metabarcoding to assess biodiversity in dry sediments collected over a 1-year period from 84 non-perennial rivers across 19 countries on four continents. Both direct factors, such as nutrient and carbon availability, and indirect factors such as climate influence the local biodiversity of most taxa. Limited resource availability and prolonged dry phases favor oligotrophic microbial taxa. Co-variation among taxa, particularly Bacteria, Fungi, Algae and Protozoa, explain more spatial variation in community composition than dispersal or environmental gradients. This finding suggests that biotic interactions or unmeasured ecological and evolutionary factors may strongly influence communities during dry phases, altering biodiversity responses to global changes.
Description
Molecular analyses were funded by Université Grenoble Alpes (UGA) through the AGIR-POLE-PAGE program (DRIME project, AGIR-POLE-PAGE 2016). Further funding was provided by the H2020 European Research and Innovation action Grant Agreement N°869226 (DRYvER). We thank the landholders who enabled the collection of samples from private land and the Commonwealth Environmental Water Office for support. We also thank S. O. Díaz Huezo, F. Erzinger, J. Gelbrecht, M.A.S. Graça, J. López, C.T. Robinson, V. Rosset for their help in collecting samples in the field and B. Obrador for sediment texture analyses. DvS and NB are Serra Húnter Fellows. PRL was supported by a Margalida Comas postdoctoral contract (PD/031/2018) funded by the Government of the Balearic Islands and the European Social Fund, and by a Juan de la Cierva-Incorporación fellowship (IJC2019-041601-I). MTB was supported by a David H. Smith Conservation Research Fellowship. PP and MP were supported by the Czech Science Foundation grant no. GA23-05268S.













