Climatic warming causes regime shifts in lake food webs

By Marten Scheffer, D. Straile, E. V. van Nes, H. Hosper. 2001

264 citations recorded by the source corpus.

Subfields: Environmental Chemistry, Nature and Landscape Conservation, Oceanography

View Paper: https://www.semanticscholar.org/paper/31f330625ce865667e50254fa3afee89c8920699

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In Environmental Chemistry

In Nature and Landscape Conservation

In Oceanography

Citations in the corpus

CYLINDROSPERMOPSIS RACIBORSKII (CYANOBACTERIA) INVASION AT MID‐LATITUDES: SELECTION, WIDE PHYSIOLOGICAL TOLERANCE, ORGLOBALWARMING? 1 (2004, background): “The influence of the NAO on the lake temperatures particularly in winter and early spring could be more significant (Livingston and Dokulil 2001, Scheffer et al. 2001, Anneville et al. 2002, Straile 2002).”
Biodiversity, climate change, and ecosystem services (2009, background): “produce large (and often unexpected) changes in ecosystem services, and these changes may be very difficult to reverse [75].”
Can warm climate‐related structure of littoral predator assemblies weaken the clear water state in shallow lakes? (2007, methodology): “A model built on the correlation between the winter NAO index and a defined clear water state has predicted a shift in the timing and a higher probability of the occurrence of clear water phases in shallow temperate lakes (Scheffer et al., 2001), linked to an earlier development of submerged plants.”
Effects of common carp on nutrient dynamics and littoral community composition: roles of excretion and bioturbation (2007, background): “…referred to as a ‘regime shift’ (Scheffer et al. 2001a), has been reported to be modulated by excessive nutrient loads (Scheffer 1998), high abundances of planktivorous (Scheffer 1998) or benthivorous fish (Zambrano et al. 2001, Scheffer et al. 2003) and/or climate warming (Scheffer et al. 2001 b).”
The Response of Freshwater Ecosystems to Climate Variability Associated with the North Atlantic Oscillation (2013, unknown): “All Dutch lakes are very shallow, and a clear-water phase can be stabilized by macrophytes providing a refuge for Daphnia and suppressing phytoplankton by allelochemicals [Scheffer et al., 1993; Benndorf et al., 2002].”
Warming leads to higher species turnover in a coastal ecosystem (2010, background): “Observational data sets have been highly informative in detecting alterations in process rates and phenology in different ecosystems (Weyhenmeyer et al., 1999; Straile & Adrian, 2000; Scheffer, 2001; Blenckner & Hillebrand, 2002; Richardson & Schoeman, 2004; Blenckner et al., 2007).”
Why plankton communities have no equilibrium: solutions to the paradox (2004, background): “Redrawn from Scheffer et al. (2001), with permission from the American Society of Limnology and Oceanography, Inc. of chaos in noisy time series (Sugihara & May, 1990; Turchin & Taylor, 1992; Hastings et al., 1993; Wilson & Rand, 1993; Stone et al., 1996; Bjørnstad & Grenfell , 2001).”
Climate change: links to global expansion of harmful cyanobacteria. (2012, background): “Clear water phases, caused by grazing of zooplankton on microalgae, were studied in 71 shallow Dutch lakes and were found to occur earlier when water temperatures were higher (Scheffer et al., 2001, Scheffer, 2004).”
Long‐term changes within the invertebrate and fish communities of the Upper Rhône River: effects of climatic factors (2004, background): “…change impacts in freshwater were predictive (Coutant, 1990; Regier et al., 1990; Carpenter et al., 1992; Meyer et al., 1999), and those based on actual data essentially dealt with lakes (George, 2000; Gerten & Adrian, 2000; Straile & Adrian, 2000; Scheffer et al., 2001; Sorvari et al., 2002).”
Sixty years of environmental change in the world's largest freshwater lake – Lake Baikal, Siberia (2008, background): “This extraordinary long-term dataset from Lake Baikal demonstrates that the planktonic community has responded to environmental change over the past 60 years, as have aquatic systems worldwide (Scheffer et al., 2001; Hays et al., 2005).”