Growth limitation in young Euphausia superba under field conditions

By R. Ross, L. Quetin, K. Baker, M. Vernet, Raymond C. Smith. 2000

146 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Nature and Landscape Conservation, Oceanography

View Paper: https://www.semanticscholar.org/paper/040b68e255c4a3a254fa5e616bf50eeb59f0a85a

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Global and Planetary Change

1. A. Atkinson
2. B. Meyer
3. V. Siegel
4. P. Ward
5. K. Schmidt
6. R. Ross
7. L. Quetin
8. E. Murphy

In Nature and Landscape Conservation

1. B. Meyer
2. A. Atkinson
3. V. Siegel
4. K. Schmidt
5. P. Ward
6. R. Ross
7. L. Quetin
8. D. Pond

In Oceanography

1. A. Atkinson
2. Miram R. Gleiber
3. V. Siegel
4. P. Ward
5. R. Ross
6. L. Quetin
7. E. Murphy
8. Geraint A. Tarling

Citations in the corpus

• An overview of Southern Ocean zooplankton data: abundance, biomass, feeding and functional relationships (2012, background): “superba based on their food, body, length, temperature and time of year can be predicted to an some extent (Ross et al., 2000; Kawaguchi et al., 2006; Atkinson et al., 2006; Tarling et al., 2006) and such empirical models have been used to predict their response to climatic change scenarios (Wiedenm”
• Environmental Variability and Its Impact on the Reproductive Cycle of Antarctic Krill1 (2001, unknown): “Recently Ross et al. (2000) showed that growth rates of young krill increase as a function both of total chlorophyll a concentration and the phytoplankton community composition, supporting the concept that the two species fare best with different phytoplankton communities.”
• Phytoplankton spatial distribution patterns along the western Antarctic Peninsula (Southern Ocean) (2003, result): “This assumption is based on previous studies performed in the area that revealed a uniform vertical distribution of carotenoid pigments (diagnostic of different algae groups), suggesting no major phytoplankton composition variations with depth (Ross et al. 2000, Garibotti et al. 2003).”
• Physiology, growth, and development of larval krill Euphausia superba in autumn and winter in the Lazarev Sea, Antarctica (2009, background): “At such high Chl a concentrations, larval krill can reach maximum carbon ration and growth (Ross et al. 2000; Meyer et al. 2002).”
• Protozoans as a food source for Antarctic krill, Euphausia superba: Complementary insights from stomach content, fatty acids, and stable isotopes (2006, background): “Despite this, few studies have related in situ growth rates of Euphausia superba to their nutritional history, either indicated by ambient phytoplankton communities (Ross et al. 2000, Atkinson et al. 2006) or by krill’s content of specific fatty acids (Pond et al. 2005).”
• Oceanic circumpolar habitats of Antarctic krill (2008, methodology): “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).”
• Biogeographic Atlas of the Southern Ocean (2014, background): “…and the capacity to withstand starvation using a body combustion strategy results in a negative growth rate for adults that regress in size and to a sub-adult stage (loosing petasma or thelycum) and to a lesser degree for larvae and juveniles (Daly 1998, Quetin et al. 2003, Ross et al. 2000).”
• Long-term (1993-2013) changes in macrozooplankton off the Western Antarctic Peninsula (2015, background): “superba growth and reproduction is dependent on food availability (Ross et al., 2000; Quetin and Ross, 2001; Atkinson et al., 2006).”
• Marine pelagic ecosystems: the West Antarctic Peninsula (2007, background): “Higher growth rates of young krill in the field were also observed when phytoplankton communities were dominated by diatoms and not prymnesiophytes (Ross et al. 2000).”
• Natural growth rates in Antarctic krill (Euphausia superba): I. Improving methodology and predicting intermolt period (2006, methodology): “Relating this back to the premolt length of the original krill (Lpre, mm) allows the daily growth rate (DGR, mm d21) to be determined using the equation of Ross et al. (2000):”
• Overwintering growth and development of larval Euphausia superba: an interannual comparison under varying environmental conditions west of the Antarctic Peninsula (2004, background): “2–10b 18 (7–40) Field experiment Ross et al. (2000)”
• Natural growth rates in Antarctic krill (Euphausia superba): II. Predictive models based on food, temperature, body length, sex, and maturity stage (2006, methodology): “Comparison of average DGR values from each site (Table 1) with available spring/summer literature data from IGR measurements (Morris and Keck 1984; Buchholz 1985; Daly 1998; Ross et al. 2000) and net-derived length frequency data (Kanda et al.”
• Composition and biomass of phytoplankton assemblages in coastal Antarctic waters: a comparison of chemotaxonomic and microscopic analyses (2003, methodology): “Thus, multiple regression analysis continues to be a widespread technique in field studies (Moline et al. 2000, Prézelin et al. 2000, Ross et al. 2000, Marty et al. 2002).”
• Episodic recruitment in Antarctic krill Euphausia superba in the Palmer LTER study region (2003, background): “The rapid growth usually seen in the second spring/summer (Ross et al. 2000) will tend to merge the 2 modes, leading to a single mode found as later year classes.”
• Diet of the Antarctic krill (Euphausia superba Dana): II. Selective grazing in mixed phytoplankton assemblages (2003, unknown): “in the phytoplankton community (Ross et al., 2000).”