Distribution of Calanus species in Kongsfjorden, a glacial fjord in Svalbard

By S. Kwaśniewski, H. Hop, S. Falk‐Petersen, G. Pedersen. 2003

229 citations recorded by the source corpus.

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

View Paper: https://www.semanticscholar.org/paper/15a6498fa374fa71d34ec356b17f74d589ae005c

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In Global and Planetary Change

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Citations in the corpus

Microbial processes in a high-latitude fjord (Kongsfjorden, Svalbard): II. Ciliates and dinoflagellates (2011, background): “Their abundance, however, depends noticeably on the timing and magnitude of the shelf-fjord water mass exchanges (Kwasniewski et al. 2003; Walkusz et al. 2009), and the phytoplankton bloom in spring may often develop in the absence of significant stocks of copepods (Willis et al.”
The Arctic sea butterfly Limacina helicina: lipids and life strategy (2005, background): “2002b), which were the dominant copepods in Kongsfjorden (Kwasniewski et al. 2003).”
Timing of blooms, algal food quality and Calanus glacialis reproduction and growth in a changing Arctic (2010, background): “Calanus specimens were identified to the species level based on morphology and prosome lengths of individual copepodite stages (Kwasniewski et al., 2003).”
Arctic zooplankton do not perform diel vertical migration (DVM) during periods of midnight sun (2006, unknown): “Such a temporal separation in reproduction in areas of cooccurrence most likely allows for avoidance of competition for food among offspring, and has been observed in other locations (e.g. Kwasniewski et al. 2003).”
Comparison of productivity and phytoplankton in a warm (Kongsfjorden) and a cold (Hornsund) Spitsbergen fjord in mid-summer 2002 (2009, methodology): “For this purpose, the procedures given by Harris et al. (2000) were applied, while guidelines of Kwasniewski et al. (2003) were used for the Calanus species identiWcation.”
Seasonal feeding strategies of Calanus in the high-Arctic Svalbard region (2008, background): “Prosome lengths were measured to identify Calanus copepodite stages to species (Kwasniewski et al., 2003).”
Distribution and abundance of euphausiids and pelagic amphipods in Kongsfjorden, Isfjorden and Rijpfjorden (Svalbard) and changes in their relative importance as key prey in a warming marine ecosystem (2016, background): “In years with a weak inflow of AW, the zooplankton community is represented with more abundant Arctic species, whereas in years of strong AW influence the community shifts towards boreal species (Kwasniewski et al. 2003).”
Life histories of the copepods Pseudocalanus minutus, P. acuspes (Calanoida) and Oithona similis (Cyclopoida) in the Arctic Kongsfjorden (Svalbard) (2005, background): “(Weslawski et al. 1991; Kwasniewski et al. 2003).”
Mesozooplankton distribution in northern Svalbard waters in relation to hydrography (2007, background): “Previous studies in this area have concentrated on a few easily accessible fjords along the western coast of Spitsbergen (e.g. Koszteyn and Kwasniewski 1989; Kwasniewski et al. 2003; Arnkvaern et al. 2005).”
Potential misidentifications of two climate indicator species of the marine arctic ecosystem: Calanus glacialis and C. finmarchicus (2012, background): “In the European Arctic, Calanus spp. are regarded as biological indicators of Arctic (Calanus glacialis and C. hyperboreus) and Atlantic (C. finmarchicus) water masses, respectively (Kwasniewski et al. 2003; Wassmann et al. 2006; Daase et al. 2007).”
Dynamics of coexisting Calanus finmarchicus, Calanus glacialis and Calanus hyperboreus populations in a high-Arctic fjord (2005, background): “finmarchicus were compared with literature data (Grainger 1961; Unstad and Tande 1991; Hirche et al. 1994; Kosobokova 1999; Kosobokova and Hirche 2001; Madsen et al. 2001; Kwasniewski et al. 2003).”
Timing of reproductive events in the marine copepod Calanus glacialis: a pan-Arctic perspective (2013, methodology): “Zooplankton samples were analyzed following procedures described by Kwasniewski et al. (2003) (Table 1).”
The influence of advection on zooplankton community composition in an Arctic fjord (Kongsfjorden, Svalbard) (2006, background): “Kwasniewski et al. (2003) proposed that populations of the boreal C. finmarchicus and Arctic C. glacialis in Kongsfjorden consist of local and advected individuals, with the proportions of each varying seasonally and annually depending on the timing and volume of AW and ArW intrusions.”
Hydrodynamic control of mesozooplankton abundance and biomass in northern Svalbard waters (79–81°N) (2008, methodology): “Representatives of Calanus were identified to species level based on morphology and prosome lengths of individual copepodid stages, which is similar to identification methods applied in other studies (e.g., Tande, 1991; Kwasniewski et al., 2003).”
Trophic interactions of macro-zooplankton (krill and amphipods) in the Marginal Ice Zone of the Barents Sea (2008, background): “1 and 2, Table 3 and from literature ( Kwasniewski et al., 2003 ).”