Consequences of increased temperature and CO2 for phytoplankton community structure in the Bering Sea

By C. E. Hare, K. Leblanc, G. DiTullio, Raphael M. Kudela, Yaohong Zhang, Peter A. Lee, S. F. Riseman, D. Hutchins. 2007

263 citations recorded by the source corpus.

Subfields: Oceanography

View Paper: https://www.semanticscholar.org/paper/6df2435ad7cbc5f23044779df9f8b6ec50e14b2a

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In Oceanography

Citations in the corpus

Effects of increased atmospheric CO 2 on small and intermediate sized osmotrophs during a nutrient induced phytoplankton bloom (2007, background): “Proven synergetic effects (Fu et al., 2007; Hare et al., 2007) implies greater alterations when/if increased pCO2 is accompanied (as predicted) by elevated seawater temperatures.”
Meta-analysis reveals negative yet variable effects of ocean acidification on marine organisms. (2010, background): “Although not included in our analyses, increased temperatures both increased and decreased the severity of the effect size of ocean acidification (Reynaud et al. 2003, 2004; Hare et al. 2007; Anthony et al. 2008; Findlay et al. 2008; Byrne et al. 2009; Martin & Gattuso 2009; Munday et al. 2009).”
Effects of changing pCO2 and phosphate availability on domoic acid production and physiology of the marine harmful bloom diatom Pseudo‐nitzschia multiseries (2011, background): “Although some field incubation experiments have shown that growth of natural diatom assemblages was unaffected by the availability of pCO2 (Hare et al. 2007), Tortell et al. (2002) found that the relative abundance of diatoms in the equatorial Pacific was 50% lower in a low-pCO2 treatment compared…”
Harmful algal blooms and climate change: Learning from the past and present to forecast the future (2015, background): “…there is evidence that increasing CO2 concentrations will affect competition among major phytoplankton groups (Feng et al., 2009; Fu et al., 2007; Hare et al., 2007; Tortell et al., 2002), and toxic algal groups (Fu et al., 2008; Ratti et al., 2007; Rost et al., 2006), although very few species…”
The biological pump in a high CO 2 world (2012, background): “Shifts in phytoplankton composition due to ocean acidification (Tortell et al. 2002, Rochelle-Newall et al. 2004, Low-Décarie et al. 2011, Meakin & Wyman 2011) or increased temperatures (Hare et al. 2007) are commonly observed experimentally.”
Differing responses of marine N2 fixers to warming and consequences for future diazotroph community structure (2014, background): “In a Bering Sea shipboard manipulative experiment, as temperature increased, the community shifted away from diatoms and toward nanophytoplankton (Hare et al. 2007).”
Co2 and phosphate availability control the toxicity of the harmful bloom dinoflagellate Karlodinium veneficum. (2010, background): “…that elevated CO2 may increase phytoplankton growth (Hein & Sand-Jensen 1997, Burkhardt et al. 1999, Hutchins et al. 2007), or that CO2 concentrations could affect competition among major marine phytoplankton groups (Tortell et al. 2002, Fu et al. 2007, 2008, Hare et al. 2007, Feng et al. 2009).”
Climate change and ocean acidification effects on seagrasses and marine macroalgae (2013, background): “…and CO2 interactive effects have been shown to be synergistic in phytoplankton studies with highly species-specific results (Fu et al., 2007; Hare et al., 2007; Feng et al., 2009; Torstensson et al., 2012); thus, further studies are needed to understand these interactions in seagrasses and…”
The effects of changing climate on microzooplankton grazing and community structure: drivers, predictions and knowledge gaps (2013, background): “…study in the Bering Sea tested the individual and combined effects of increased temperature and CO2 and documented large shifts in the algal community away from diatoms and toward nanoflagellates, with warming rather than CO2 being the prime driver of these taxonomic changes (Hare et al., 2007).”
Understanding the responses of ocean biota to a complex matrix of cumulative anthropogenic change (2012, background): “An example of the former is the antagonistic interaction between ocean acidification (OA) and warming, whereby lowered CO2 solubility at higher ocean temperatures partially offsets CO2-driven increases in OA (Hare et al. 2007).”
Interactions between changing pCO2, N2 fixation, and Fe limitation in the marine unicellular cyanobacterium Crocosphaera (2008, methodology): “…with natural phytoplankton communities indicate that elevated CO2 could result in increased phytoplankton primary production in the open ocean (Hein and Sand-Jensen 1997) or in changes in competitive interactions among major marine phytoplankton groups (Tortell et al. 2002; Hare et al. 2007).”
Synergistic effects of iron and temperature on Antarctic phytoplankton and microzooplankton assemblages (2009, methodology): “…1974), and the interactions of temperature with other environmental variables such as risingpCO2, altered irradiance and nutrient utilization have been examined in a few field and lab studies (Feng et al., 2009; Goldman, 1979; Hare et al., 2007; Lomas and Glibert, 1999; Rose et al., 2009).”