2016
DOI: 10.1111/gcb.13193
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Global spread of hypoxia in freshwater ecosystems during the last three centuries is caused by rising local human pressure

Abstract: The spread of hypoxia is a threat to aquatic ecosystem functions and services as well as to biodiversity. However, sparse long-term monitoring of lake ecosystems has prevented reconstruction of global hypoxia dynamics while inhibiting investigations into its causes and assessing the resilience capacity of these systems. This study compiles the onset and duration of hypoxia recorded in sediments of 365 lakes worldwide since AD 1700, showing that lacustrine hypoxia started spreading before AD 1900, 70 years prio… Show more

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Cited by 297 publications
(213 citation statements)
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“…Multiple sites need to be investigated to quantify a regional trend, as well as to evaluate local to regional heterogeneities. Only a few studies have interpreted the long-term trajectories of lakes (based on >100-year lake records) in terms of eutrophication on a regional scale by analyzing trends in nutrient and dissolved CO 2 concentrations (13,14), carbon burial rates (15), cyanobacterial dominance (16), and hypoxia development (17). However, only one of these studies (13) considered the temporal dynamics of land cover and use, and only a few studies (16,17) considered modern land cover.…”
mentioning
confidence: 99%
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“…Multiple sites need to be investigated to quantify a regional trend, as well as to evaluate local to regional heterogeneities. Only a few studies have interpreted the long-term trajectories of lakes (based on >100-year lake records) in terms of eutrophication on a regional scale by analyzing trends in nutrient and dissolved CO 2 concentrations (13,14), carbon burial rates (15), cyanobacterial dominance (16), and hypoxia development (17). However, only one of these studies (13) considered the temporal dynamics of land cover and use, and only a few studies (16,17) considered modern land cover.…”
mentioning
confidence: 99%
“…Only a few studies have interpreted the long-term trajectories of lakes (based on >100-year lake records) in terms of eutrophication on a regional scale by analyzing trends in nutrient and dissolved CO 2 concentrations (13,14), carbon burial rates (15), cyanobacterial dominance (16), and hypoxia development (17). However, only one of these studies (13) considered the temporal dynamics of land cover and use, and only a few studies (16,17) considered modern land cover. Our current lack of knowledge of the effects arising from cumulative environmental pressures presents the potential for serious underestimation of the long-term impacts of land use changes and hinders our ability to identify the relative importance of P sources to lake ecosystems (18).…”
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confidence: 99%
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