Natural growth rates in Antarctic krill (Euphausia superba): II. Predictive models based on food, temperature, body length, sex, and maturity stage
By A. Atkinson, Rachael S. Shreeve, A. Hirst, P. Rothery, Geraint A. Tarling, D. Pond, R. Korb, E. Murphy, J. Watkins. 2006
198 citations recorded by the source corpus.
Subfields: Global and Planetary Change, Nature and Landscape Conservation
View Paper: https://www.semanticscholar.org/paper/e98bb268ee36a5bf24e2f62289ed7e3447dbe9be
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In Global and Planetary Change
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Citations in the corpus
- Developing integrated models of Southern Ocean food webs: Including ecological complexity, accounting for uncertainty and the importance of scale (2012, unknown): “…of temporal and regional temperature variation (around the Antarctic Peninsula and South Georgia) on magnitude and growth of krill cohorts, which have been used to explore the impacts of climate related change (Reid et al., 2002; Atkinson et al., 2006; Tarling et al., 2006; Murphy et al., 2007a).”
- Feeding and overwintering of Antarctic krill across its major habitats: The role of sea ice cover, water depth, and phytoplankton abundance (2014, background): “Both processes rely on a sufficient food quantity and quality, which for E. superba is best met during phytoplankton blooms (Cuzin-Roudy and Labat 1992; Atkinson et al. 2006).”
- Oceanic circumpolar habitats of Antarctic krill (2008, background): “Krill have a classic hyperbolic functional growth response, and this non-linearity means near maximal growth at chl a concentrations of ~1 mg chl a m–3 and substantial growth at half of this value (Ross et al. 2000, Atkinson et al. 2006).”
- The overwintering of Antarctic krill, Euphausia superba, from an ecophysiological perspective (2011, methodology): “Also recent growth studies using the instantaneous growth rate (IGR) method showed a mean positive growth even when shrinkage was observed (Atkinson et al. 2006; Meyer et al. 2010).”
- Seabed foraging by Antarctic krill: Implications for stock assessment, bentho‐pelagic coupling, and the vertical transfer of iron (2011, background): “100 times higher than what is required for their daily growth (assuming a growth rate of , 1% of body mass d21, Atkinson et al. 2006), suggesting that benthic feeding leads to a surplus of labile iron in krill stomachs.”
- Seasonal variation in body composition, metabolic activity, feeding, and growth of adult krill Euphausia superba in the Lazarev Sea (2010, unknown): “…using the IGR method, the growth rates of krill from the Lazarev Sea in December are moderate (0.076 mm d–1 on average), in contrast to those measured overall in the Scotia Sea in January and February, where growth rates reached 0.32 mm d–1, with mean values of 0.1 mm d–1 (Atkinson et al. 2006).”
- Long-term (1993-2013) changes in macrozooplankton off the Western Antarctic Peninsula (2015, background): “D.K. Steinberg et al. / Deep-Sea Research I 101 (2015) 54–70 63 does not occur above a temperature threshold (Atkinson et al., 2006).”
- Distribution, Biomass and Demography of Antarctic Krill, Euphausia superba (2016, methodology): “The first model was used to provide a circumpolar-scale prediction of daily growth rates in mm per day based on ambient food, temperature and krill length (Atkinson et al. 2006).”
- Variable food absorption by Antarctic krill: Relationships between diet, egestion rate and the composition and sinking rates of their fecal pellets (2012, result): “In contrast, a previous Scotia Sea study found that satellite-derived chl a was a good predictor of krill growth rate (Atkinson et al., 2006).”
- Variability and predictability of Antarctic krill swarm structure (2009, methodology): “described in Atkinson et al. (2006). Data were derived as the percentage of diatoms in the total cell count of diatoms, ciliates plus dinoflagellates.”