Palmer LTER: Patterns of distribution of five dominant zooplankton species in the epipelagic zone west of the Antarctic Peninsula, 1993–2004
By R. Ross, L. Quetin, D. Martinson, R. Iannuzzi, S. Stammerjohn, Raymond C. Smith. 2008
127 citations recorded by the source corpus.
Subfields: Ecology, Oceanography
View Paper: https://www.semanticscholar.org/paper/10532ac6a22fcfeff7396a8e643adeef1019e66d
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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): “…such as primary production, zooplankton species development and community structure, krill dispersal dynamics and the spatial dynamics of predator foraging (Fraser and Hofmann, 2003; Massom et al., 2006; Murphy et al., 2007a,b; Trathan et al., 2007; Murphy et al., 2008; Ross et al., 2008) (Fig.”
- The overwintering of Antarctic krill, Euphausia superba, from an ecophysiological perspective (2011, background): “A range of correlation studies in the SW Atlantic between krill abundance and winter sea ice duration (Loeb et al. 1997; Atkinson et al. 2004) and seasonal sea ice dynamic (Ross et al. 2008) suggested that krill is vulnerable to environmental changes related to climate variability.”
- Time series of vertical flux of zooplankton fecal pellets on the continental shelf of the western Antarctic Peninsula (2012, background): “…studies in non-polar 19 regions which indicate euphausiid pellets contribute in similar or lower amounts to pellet flux as ovoid copepod pellets (Carroll et al., 1998; Wilson et al., 2008), the Antarctic marginal ice zone is dominated by euphausiids (Le Fevre et al., 1998; Ross et al., 2008).”
- Penguin responses to climate change in the Southern Ocean (2009, background): “…changes that affect phytoplankton also change zooplankton assemblages, which are observed in the open ocean and continental shelf areas (Loeb et al., 1997; Moline et al., 2004; Ross et al., 2008), particularly in years of short seaice season duration and sea-ice extent (Atkinson et al., 2004).”