Shifts in landscape heterogeneity and climate can influence animal movement in ways that profoundly alter disease transmission. Water sources that are foci of animal activity have great potential to promote disease transmission, but it is unknown how this varies across a range of hosts and climatic contexts. For fecal-oral parasites, water resources can aggregate many different hosts in small areas, concentrate infectious material, and function as disease hotspots. This may be exacerbated where water is scarce and for species requiring frequent water access. Working in an East African savanna, we show via experimental and observational methods that water sources increase the density of wild and domestic herbivore feces and thus, the concentration of fecal-oral parasites in the environment, by up to two orders of magnitude. We show that this effect is amplified in drier areas and drier periods, creating dynamic and heterogeneous disease landscapes across space and time. We also show that herbivore grazing behaviors that expose them to fecal-oral parasites often increase at water sources relative to background sites, increasing potential parasite transmission at these hotspots. Critically, this effect varies by herbivore species, with strongest effects for two animals of concern for conservation and development: elephants and cattle.
Shifts in landscape heterogeneity and climate can influence animal behavior and movement in ways that profoundly alter disease transmission. Amid accelerating climate and land use changes, it is increasingly important to identify and monitor hotspots of increased animal activity and overlap where disease transmission is likely to occur. Water sources that are foci of animal activity have great potential to promote disease transmission, but there has been very little work to quantify this, nor any comparison across a range of hosts and climatic contexts. In the case of fecal-oral parasites, water resources can aggregate large groups of many different host species in small areas, concentrate infectious material, and function as disease hotspots. This may be exacerbated where water is scarce and for species that require frequent drinking water access. Working in an East African savanna, we show via experimental and observational methods that water sources increase the density of wild and domestic herbivore feces and thus, the concentration of fecal-oral parasites in the environment, by up to two orders of magnitude. Our results show that this effect is amplified in drier areas and following periods of low rainfall, creating dynamic and heterogeneous disease landscapes across space and time. In addition, we show via camera trapping methods that herbivore grazing behaviors that expose them to fecal-oral parasites are often increased at water sources relative to background sites, thereby creating landscape hotspots of potential disease transmission. Critically, this effect varies markedly by herbivore species, with strongest effects observed for two large, water-dependent animals that are of critical concern for conservation and development: elephants and cattle. When water availability is reduced – a global pattern that is increasing amid climate changes and growing anthropogenic water use – risk of parasite exposure may increase substantially, posing multiple threats to critical taxa. These findings are important for understanding shifting parasite dynamics for several threatened wildlife species and for pastoral livelihoods in response to changing water supply due to climate changes.
Los aportes de aguas continentales hacia la zona costera son uno de los impactos más significativos que reciben los ecosistemas a nivel mundial. Las aguas continentales aportan nutrientes en diferente magnitud y su distribución está condicionada por la dinámica de circulación marina local y la estacionalidad de los aportes fluviales. El Río Balsas, uno de los más importantes de México, descarga sus aguas hacia la Bahía de Petacalco, con un considerable contenido de nutrientes. En el presente trabajo se estudia la variabilidad espaciotemporal del contenido de ortofosfatos y fósforo total y se analiza su relación con otros parámetros como salinidad, turbiedad y circulación costera. En la bahía se registraron contenidos máximos de ortofosfatos de 19.56 µM en abril-mayo, 10.50 µM en febrero y 9.31 µM en agosto. Para el fósforo total sobresalieron 40.98 µM en abril-mayo y 20.54 µM en agosto que indicaron un ambiente costero eutroficado, resultado de las descargas de actividades industriales asentadas en el estuario del río y dispersadas a toda la bahía a través de las corrientes locales. En la mayoría de los meses estudiados (febrero, junio, agosto, octubre y diciembre), hacia la porción centro-oriental de la bahía se registró una acumulación del agua proveniente del Río Balsas, con pequeños giros ciclónicos-anticiclónicos superficiales frente al Estero de Petacalco que en ocasiones conservaron su sentido a 10 m de profundidad o se invirtieron en abril y diciembre, con un desplazamiento hacia el E-NE que permitió justificar la difusión del fósforo.
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