Climate change and marine plankton.

By G. Hays, Anthony J. Richardson, C. Robinson. Trends in Ecology & Evolution, 2005

1,249 citations recorded by the source corpus.

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In Oceanography

Citations in the corpus

Novel microcosm system for investigating the effects of elevated carbon dioxide and temperature on intertidal organisms (2008, background): “While climate change is increasingly recognised as an © Inter-Research 2008 · www.int-res.com*Email: hefi@pml.ac.uk KEY WORDS: Ocean acidification · pH · Carbon dioxide · Climate change · Global warming · Microcosm · Intertidal · Larvae Resale or republication not permitted without written consent o”
Community ecology in a warming world: The influence of temperature on interspecific interactions in marine systems (2011, background): “) are also shifting earlier (Sims et al., 2001; Philippart et al., 2003; Edwards and Richardson, 2004; Hays et al., 2005).”
Fish, climate and the Gulf Stream: the influence of abiotic factors on the recruitment success of cyprinid fishes in lowland rivers (2007, neutral): “George & Taylor, 1995; Liebhold, Koenig & Bjornstad, 2004; Hays, Richardson & Robinson, 2005; Saether et al., 2007).”
Effects of climate‐driven primary production change on marine food webs: implications for fisheries and conservation (2010, background): “Furthermore, primary producers, particularly phytoplankton, are likely to show the most rapid response to climate change due to their small size and fast population turnover (Hays et al., 2005).”
Have jellyfish in the Irish Sea benefited from climate change and overfishing? (2011, background): “The past few decades have seen profound changes in the biota of marine systems (Hays et al., 2005) with, for example, the removal of top predators (Rogers & Ellis, 2000; Myers et al.”
Biogeographical patterns of rocky intertidal communities along the Pacific coast of North America (2008, background): “There is a strong scientific consensus that coastal marine ecosystems, along with the goods and services they provide, are threatened by anthropogenic global climate change (Hays et al., 2005; Hsieh et al., 2005; Harley et al., 2006; Helmuth et al., 2006b; Parmesan, 2006; Harvey, 2007).”
Mesozooplankton distribution in northern Svalbard waters in relation to hydrography (2007, background): “Plankton are in general found to be good indicators for ocean climate variability (Hays et al. 2005) and various responses of plankton communities are observed from temperate areas (Pershing et al. 2004).”
The effect of ocean acidification and temperature on the fertilization and embryonic development of the Sydney rock oyster Saccostrea glomerata (Gould 1850) (2009, background): “Such a reduction in fertilization is concerning given the levels in this experiment are within the expected range of global mean temperatures over the next century (Hiscock et al., 2004; Hays et al., 2005; Solomon et al., 2007).”
Direct and indirect trophic interactions of Aurelia sp. (Scyphozoa) in a stratified marine environment (Mljet Lakes, Adriatic Sea) (2007, background): “In many areas worldwide there is strong evidence for changes in plankton communities, over recent decades (Hays et al. 2005), an increase in the frequency and intensity of jellyfish outbreaks is among most evident (Purcell et al. 2001; Dumont et al. 2004).”
Australia's Biodiversity and Climate Change (2010, background): “Changes in timing of major climatic phenomena such as El Niño events Changes in seasonal cycles of plankton abundance, with potential for mismatch between phytoplankton blooms and zooplankton growth, leading to cascading effects to the rest of the marine food chain (Hays et al. 2005)”
Particulate nutrient fluxes over a fringing coral reef: relevant scales of phytoplankton production and mechanisms of supply (2010, background): “While corals themselves have often been thought to be one of the most sensitive indicators of climate change, planktonic communities may be equally, if not more, sensitive to global change, especially given their short life cycles (Hays et al. 2005, Hooff & Peterson 2006).”
Climate‐related increases in jellyfish frequency suggest a more gelatinous future for the North Sea (2007, background): “Additionally, we investigated past relations between North Sea pH and jellyfish frequency to test the prediction that future increasing acidity due to higher levels of CO2 in the atmosphere (Calderia and Wickett 2003) may be detrimental to calcareous, skeleton-forming plankton (Riebesell et al. 2000”
Hydrodynamic control of mesozooplankton abundance and biomass in northern Svalbard waters (79–81°N) (2008, background): “Plankton are in general perceived as good indicators for ocean climate variability (Hays et al., 2005), with induced changes in the species distribution (Greene and Pershing, 2000), in the seasonal timing (Edwards and Richardson, 2004), and pole wardmovement of boreal species (e.”