Primary and Secondary Production in the Arctic Seas

By E. Sakshaug. 2004

582 citations recorded by the source corpus.

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In Food Science

Citations in the corpus

Seasonal and interannual phytoplankton production in a sub-Arctic tidewater outlet glacier fjord, SW Greenland (2015, background): “…is ultimately determined by light availability, i.e. the seasonal incoming solar radiation (insolation) in relation to the latitude of observation (Sakshaug 2004, Leu et al. 2011) combined with snow and sea-ice cover reducing light penetration into the water column (Rysgaard & Glud 2007, Søgaard…”
Trophic relationships along a bathymetric gradient at the deep-sea observatory HAUSGARTEN (2009, background): “In addition, the deep Arctic is—like other regions of the ocean—characterised by a great retention of carbon in the twilight zone (Wassmann et al., 2003; Buesseler et al., 2007) further reducing food availability compared to open ocean waters (Klages et al., 2003; Sakshaug, 2003).”
Does Phaeocystis spp. contribute significantly to vertical export of organic carbon? (2007, background): “is favoured in regions with deeper and well-mixed waters (60–80 m) (Goffart et al. 2000; Lancelot et al. 1998; Sakshaug 2004).”
Methane cold seeps as biological oases in the high‐Arctic deep sea (2018, background): “Marine environments in the Arctic are characterized by strong seasonality with respect to input of photosynthetically derived organic matter during a short and intense productivity season (Sakshaug 2004; Søreide et al. 2006; Ardyna et al. 2013).”
Phytoplankton productivity on the Canadian Shelf of the Beaufort Sea (2004, background): “Little work has been published on phytoplankton productivity on interior Arctic shelves in general and the mainland Canadian Shelf in particular (cf. Sakshaug 2003).”
Spatial and temporal changes in the Barents Sea pelagic compartment during the recent warming (2017, background): “The mean annual primary production for the Barents Sea is estimated to be about 100 g C m 2 y (1), with a suggested increase of possibly 20– 30% associated with the warming and loss of sea ice during the two last decades (Sakshaug, 2004; Wassmann et al., 2006b; Arrigo et al., 2008; Reigstad et al., ”
Recent research on Arctic benthos: common notions need to be revised (2005, background): “This notion is still not totally false but novel findings have called for a rectification of the estimates of annual (particulate) primary production by one order of magnitude (from 2 g C m 2 year 1 to 15–30 g C m 2 year (1); MacDonald and Carmack 1991; Macdonald et al. 1993; Wheeler et al. 1996; Go”
Rapid ecosystem change and polar bear conservation (2013, background): “Productivity and prey are higher over the continental shelf (Sakshaug 2004; Harwood et al. 2012) but pack ice is now retreating beyond this area.”
The sub-ice algal community in the Chukchi sea: large- and small-scale patterns of abundance based on images from a remotely operated vehicle (2005, background): “It does appear, however, that on a large-scale ice algae are a relatively more important component of the Arctic marine ecosystem with increasing latitude (Sakshaug 2004).”
Major pathways by which climate may force marine fish populations (2010, background): “However, the primary production does not differ much (Sakshaug, 2004; Hunt and Megrey, 2005).”
Primary production and climatic variability in the European sector of the Arctic Ocean prior to 2007: preliminary results (2010, background): “Far more than 50% of the total primary production of the Arctic Ocean takes place here (Sakshaug 2004; Pabi et al. 2008).”
Fatty acid dynamics during the spring bloom in a High Arctic fjord: importance of abiotic factors versus community changes (2006, background): “…ice breakup (Wiktor 1999; Engelsen et al. 2002; Sakshaug 2004) and usually follows the retreating ice edge northwards (Sakshaug and Slagstad 1991; Sakshaug 2004), with the bulk of autotrophic biomass concentrated in the nutrient-rich meltwater layer close to the surface, stabilized by a…”
The Arctic sea butterfly Limacina helicina: lipids and life strategy (2005, background): “The marginal seas of the Arctic are characterised by a pronounced seasonality in light conditions, temperature, and ice cover resulting in short and intensive blooms of primary producers (Sakshaug 2003).”