The fate of production in the central Arctic Ocean - top-down regulation by zooplankton expatriates?
By K. Olli, P. Wassmann, Marit Reigstad, T. Ratkova, E. Arashkevich, A. Pasternak, P. Matrai, J. Knulst, L. Tranvik, R. Klais and 1 more. 2007
137 citations recorded by the source corpus.
Subfields: Atmospheric Science, Oceanography
View Paper: https://www.semanticscholar.org/paper/2c296f91555e4e30f7d96c745f3d29a283423e42
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In Atmospheric Science
- R. Hopcroft
- Geoffrey W. Cowles
- S. Falk‐Petersen
- M. Koski
- H. Flores
- Carlos M. Duarte
- C. David
- S. Agustí
In Oceanography
- S. Falk‐Petersen
- Janne E. Søreide
- R. Hopcroft
- H. Hop
- Lena Seuthe
- Kriss Rokkan Iversen
- K. Kosobokova
- M. Ohman
Citations in the corpus
- Microbial processes in a high-latitude fjord (Kongsfjorden, Svalbard): II. Ciliates and dinoflagellates (2011, background): “The persistence and even low growth of protozooplankton in similar food-poor conditions have been related to possible patches of higher food concentration, which are successfully detected and exploited by protozoans (Jakobsen and Hansen 1997; Paffenhofer et al. 2007).”
- The Biological carbon pump in the North Atlantic (2014, background): “5 mg C m 2 d 1 or up to 100 mg C m 2 d 1 which have been reported for different areas of the Arctic Ocean (Olli et al., 2007; Caron et al., 2004).”
- DNA barcoding of Arctic Ocean holozooplankton for species identification and recognition (2010, background): “Seasonally, planktonic fauna of the Barents and Chukchi Seas can become dominated by such related expatriates from the adjoining ocean regions (Olli et al., 2007; Hopcroft and Kosobokova, 2010).”
- Life history and biogeography of Calanus copepods in the Arctic Ocean: An individual-based modeling study (2012, background): “…basin regions (e.g., Jaschnov, 1970; Conover, 1988; Hirche and Kwasniewski, 1997; Thibault et al., 1999; Kosobokova and Hirche, 2000, 2009; Ashjian et al., 2003; Wassman et al., 2006; Lane et al., 2008; Olli et al., 2007; Darnis et al., 2008; Campbell et al., 2009; Falk-Petersen et al., 2009).”
- Contributions of mesozooplankton to vertical carbon export in a coastal upwelling system (2013, background): “At times, mesozooplankton are also able to regulate carbon export rates by exerting top-down grazing pressure on phytoplankton (Goericke 2002, Olli et al. 2007, Landry et al. 2009) or consuming sinking particles (Wilson et al. 2010).”
- The importance of ice algae‐produced carbon in the central Arctic Ocean ecosystem: Food web relationships revealed by lipid and stable isotope analyses (2016, methodology): “…the most abundant herbivores, C. glacialis, C. hyperboreus and A. glacialis, was estimated by multiplying our proportional aIce derived from CSIA model b with ingestions rates (Olli et al. 2007) and observed species abundances under sea ice and in the water column (David et al. 2015; Ehrlich 2015).”
- Footprints of climate change in the Arctic marine ecosystem (2011, background): “…to the high Arctic (e.g. Carmack et al., 1997; Anderson et al., 2003), these have provided isolated data focussed largely on physical and chemical properties that cannot be used to assess climate change impacts on biota (but see e.g. Gosselin et al., 1997; Wheeler et al., 1997; Olli et al., 2007).”
- Seasonal feeding strategies of Calanus in the high-Arctic Svalbard region (2008, background): “The almost permanent ice cover and high occurrence of thick multi-year ice restrict both ice algal and phytoplankton production in the Arctic Ocean (Gosselin et al., 1997; Ollie et al., 2006).”
- Hydrodynamic control of mesozooplankton abundance and biomass in northern Svalbard waters (79–81°N) (2008, background): “The almost permanent ice cover and high occurrence of thick multi-year ice restrict both ice algal and phytoplankton production in the Arctic Ocean (Gosselin et al., 1997; Olli et al., 2006).”
- Diversity of the arctic deep-sea benthos (2011, background): “Consequently, carbon flux to the deep-sea floor is low ( Olli et al. 2006 ), but in the slope areas is complemented by carbon advected from some highly productive shelves and from turbidites (Grantz et al. 1996; Cooper et al. 1999; Soltwedel 2000).”