Climate Impact on Plankton Ecosystems in the Northeast Atlantic

By Anthony J. Richardson, D. Schoeman. Science, 2004

837 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/fb40443eff3a5a94b5b5275b0ecb0716e4790e73

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Citations in the corpus

Projected impacts of climate change on marine fish and fisheries (2013, background): “In the North Atlantic, the total abundance of zooplankton changed with sea surface temperature (SST) change (Richardson and Schoeman, 2004).”
Impacts of climate change on marine organisms and ecosystems. (2009, background): “In the North Atlantic, phytoplankton biomass might collapse by half [100] and, because most zooplankton populations there are subject to bottom-up control (limited by availability of their phytoplankton food) [90], secondary production would be much reduced.”
Resolving the effect of climate change on fish populations (2009, background): “Changes in plankton have been linked to changes in climate (Beaugrand et al., 2002; Richardson and Schoeman, 2004).”
Major pathways by which climate may force marine fish populations (2010, background): “Sea surface warming accompanied by increasing phytoplankton abundance in cooler regions and decreasing phytoplankton abundance in warmer regions has been observed over the last 50 years (Richardson and Schoeman, 2004).”
Thermal niche, large‐scale movements and implications of climate change for a critically endangered marine vertebrate (2006, background): “Over the past 100 years, the global average temperature has increased by approximately 0.6 1C, and it is now widely accepted that this warming trend will continue, but how this warming affects the world’s oceans remains unclear (Edwards & Richardson, 2004; Richardson & Schoeman, 2004).”
Future climate‐driven shifts in distribution of Calanus finmarchicus (2011, background): “More specifically, climatic fluctuations affect whole pelagic ecosystems from phytoplankton to zooplankton to higher trophic levels (Richardson & Schoeman, 2004; Wanless et al., 2005).”
Perspectives on marine zooplankton lipids (2007, background): “Thus, it is timely to reflect on possible effects of a changing polar ocean climate upon the lipid dynamics of phytoplankton and zooplankton taxa and populations, particularly since food web linkages are affected by ocean climate (Aebischer et al. 1990; Richardson and Schoeman 2004 ).”
Effects of climate‐driven primary production change on marine food webs: implications for fisheries and conservation (2010, background): “Climate change has already been observed to strongly influence the distribution and abundance of ocean primary production (Richardson & Schoeman, 2004; Behrenfeld et al., 2006) and these changes have been linked to changes in higher trophic level organisms (Richardson & Schoeman, 2004; Beaugrand et…”
Assessing the relevance of nucleic acid content as an indicator of marine bacterial activity (2007, methodology): “This type of meta-analysis has been used to identify general trends of species interactions and mean temperature among regions (e.g. Worm & Myers 2003, Richardson & Schoeman 2004).”
The biological pump in a high CO 2 world (2012, background): “Diminished bloom biomass and smaller average cell sizes at elevated temperatures have also been observed in situ (Richardson & Schoeman 2004, Behrenfeld et al. 2006, Morán et al. 2010).”
Climate control on the long‐term anomalous changes of zooplankton communities in the Northwestern Mediterranean (2007, background): “Hence, quantifying how climate interacts with long-term changes of abundance and composition of plankton communities is useful to track changes in the functioning of marine ecosystems (Edwards & Richardson, 2004; Richardson & Schoeman, 2004).”
Ecological Networks in a Changing Climate (2010, background): “Figure 3) as well as in metastudies, and at the individual-level environmental temperature is a strong determinant of reproductive rates (Muller and Geller, 1993), cell size (Atkinson et al., 2003; Richardson and Schoeman, 2004), and movement rates (Petchey et al.”
DNA barcoding of Arctic Ocean holozooplankton for species identification and recognition (2010, background): “Changes in the phenology of species, as well as overall productivity, can be anticipated with effects cascading to even the highest trophic levels (Edwards and Richardson, 2004; Richardson and Schoeman, 2004).”