2021
DOI: 10.1111/oik.08718
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Diversity mediates the responses of invertebrate density to duration and frequency of rivers' annual drying regime

Abstract: Predicting the impacts of global change on highly dynamic ecosystems requires a better understanding of how communities respond to disturbance duration, frequency and timing. Intermittent rivers and ephemeral streams are dynamic ecosystems that are recognized as the most common fluvial ecosystem globally. The complexity of the drying process can give rise to different annual and antecedent hydrological conditions, but their effect on aquatic communities remains unclear. Here, using aquatic invertebrates from 3… Show more

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Cited by 21 publications
(7 citation statements)
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“…Although this metric has been widely used to effectively capture spatial differences in riparian vegetation and aquatic macroinvertebrates (Bruno et al., 2014 ; Sánchez‐Montoya et al., 2007 ), other metrics, such as the maximum duration of the dry period or the frequency of drying events, can also be relevant (Arias‐Real et al., 2021 ; Crabot et al., 2020 ; Pineda‐Morante et al., 2022 ; Sánchez‐Montoya et al., 2018 ). The use of in situ hydrological measurements (e.g., data loggers) can better capture recent (e.g., duration of the last dry period) and annual (e.g., annual drying duration and frequency) variability (Arias‐Real et al., 2021 ; Pineda‐Morante et al., 2022 ), but long‐term metrics that represent average conditions in the last decades, such as the mean number of dry days per year and proportion of years with no flow, are particularly relevant and indicated when sampling sites have been surveyed across several years (Bruno, Gutiérrez‐Cánovas, Velasco, et al., 2016a ; Bruno, Gutiérrez‐Cánovas, Sánchez‐Fernández, et al., 2016b ; Belmar et al., 2019 ; Stubbington et al., 2022 ). Finally, that biodiversity surveys were conducted at the end of the wet phase might also have masked flow intermittence effects on biological groups.…”
Section: Discussionmentioning
confidence: 99%
“…Although this metric has been widely used to effectively capture spatial differences in riparian vegetation and aquatic macroinvertebrates (Bruno et al., 2014 ; Sánchez‐Montoya et al., 2007 ), other metrics, such as the maximum duration of the dry period or the frequency of drying events, can also be relevant (Arias‐Real et al., 2021 ; Crabot et al., 2020 ; Pineda‐Morante et al., 2022 ; Sánchez‐Montoya et al., 2018 ). The use of in situ hydrological measurements (e.g., data loggers) can better capture recent (e.g., duration of the last dry period) and annual (e.g., annual drying duration and frequency) variability (Arias‐Real et al., 2021 ; Pineda‐Morante et al., 2022 ), but long‐term metrics that represent average conditions in the last decades, such as the mean number of dry days per year and proportion of years with no flow, are particularly relevant and indicated when sampling sites have been surveyed across several years (Bruno, Gutiérrez‐Cánovas, Velasco, et al., 2016a ; Bruno, Gutiérrez‐Cánovas, Sánchez‐Fernández, et al., 2016b ; Belmar et al., 2019 ; Stubbington et al., 2022 ). Finally, that biodiversity surveys were conducted at the end of the wet phase might also have masked flow intermittence effects on biological groups.…”
Section: Discussionmentioning
confidence: 99%
“…Presence/absence of water was registered from July 2018 to December 2019 using temperature data loggers deployed at each sampling site (Pineda‐Morante et al, 2022). This information was used to calculate different hydrological metrics: the total number of dry days or duration of drying events (hereafter TotDur), the frequency of drying events or number of drying events (hereafter TotNum) and the average length of each drying event (hereafter TotLeng) (Arias‐Real et al, 2021; Crabot et al, 2020; Pineda‐Morante et al, 2022). In addition, the flow permanence was calculated as the percentage of the days that reaches were wet along two different time windows: 50 days before each sampling campaign (FP50), and 100 days before each sampling campaign (FP100).…”
Section: Methodsmentioning
confidence: 99%
“…In this work, we used the entire 513‐day period to calculate all the spatiotemporal indices. Using the same flow state database obtained with the data loggers, we also calculated several local hydrological metrics commonly used to characterise surface flow state in temporary streams (Arias‐Real et al, 2021; Crabot et al, 2020; Pineda‐Morante et al, 2022), such as the total number of dry days (TotDur), the number of changes from wet to dry days (TotNum) and the average number of dry days for each drying event (TotLeng).…”
Section: Methodsmentioning
confidence: 99%
“…So far, flow data obtained using high‐frequency temperature data loggers have been used to characterise the local hydrological conditions of temporary streams (e.g. drying duration, number of consecutive dry days, days with disconnected pools, days after flow return) and its effects on aquatic communities (Arias‐Real et al, 2021; B‐Béres et al, 2019; Beesley & Prince, 2010; Crabot et al, 2020). However, this information has not yet been used to develop spatiotemporal connectivity measures.…”
Section: Introductionmentioning
confidence: 99%