Recruitment of Atlantic cod stocks in relation to temperature and advectlon of copepod populations

By S. Sundby. 2000

279 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/95fa78f7c1b8c659ca1b2d422e2412bdb53724ec

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In Global and Planetary Change

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Citations in the corpus

The combined effect of transport and temperature on distribution and growth of larvae and pelagic juveniles of Arcto-Norwegian cod (2005, background): “However, Sundby (2000) argues that temperature is a proxy for food abundance, since the core region of the C. finmarchicus has a higher temperature during the early juvenile stages than the adjacent shelves, i.e. the high correlation is due to advection of warm C. finmarchicus-rich water onto the…”
A general biophysical model of larval cod (Gadus morhua) growth applied to populations on Georges Bank (2005, background): “Calanus finmarchicus has been reported as the main prey for cod larvae and juveniles for most cod stocks in the North Atlantic (Sundby, 2000); however, on Georges Bank, Scotian Shelf and other more southerly latitudes, Pseudocalanus spp.”
Comparison of size-at-age of larval atlantic cod (Gadus morhua) from different populations based on size- and temperature-dependent growth models (2005, background): “On the other hand , the NA cod stock will typically benefit from higher temperatures caused by increased advection of relatively warm Atlantic water with abundant suitable plank - ton ( Sundby 2000 ) .”
Potential movement of fish and shellfish stocks from the sub-Arctic to the Arctic Ocean (2013, background): “Atlantic inflow is expected to advect Calanus finmarchicus into the Barents Sea in the spring and summer (Skjoldal and Rey, 1989; Sundby, 2000; Boitsov and Orlova, 2004), a result confirmed by direct measurements”
Thermal dynamics of ovarian maturation in Atlantic cod (Gadus Morhua) (2010, background): “Thus, the guidelines of Schmidt-Nielsen (1983) for further Q10 studies (see below) were followed strictly, including that the experimental temperatures should be ‘‘sufficiently far apart’’ but still fall within the natural temperature range of the fish (Sundby 2000; Brander 2005).”
Impacts of climate change on the complex life cycles of fish (2013, background): “stage, owing to the specific zooplanktonic prey requirements, which for the Northeast Arctic (NEA) cod is Calanus finmarchicus (Sundby, 2000).”
Macroecology of Calanus finmarchicus and C. helgolandicus in the North Atlantic Ocean and adjacent seas (2007, background): “…plankton organisms transfer energy from the phytoplankton to higher trophic levels (Mauchline 1998) and are often important in the diet of at least 1 developmental stage of economically important fish species such as cod, herring or mackerel (Sundby 2000, Orlova et al. 2005, Skreslet et al. 2005).”
Spawning and life history information for North Atlantic cod stocks (2005, background): “This implies that variable volume transport onto the northern Norwegian shelf and into the Barents Sea may cause variations in the zoö plankton biomass in these regions (Sundby, 2000).”
Major pathways by which climate may force marine fish populations (2010, background): “finmarchicus from their overwintering areas in the depths of the Norwegian Sea is a key factor in regulating recruitment to major fish stocks (Ottersen and Sundby, 1995; Sundby, 2000).”
Lipids and life strategy of Arctic Calanus (2009, background): “During late winter (February April) the population, now ready to spawn, migrates to surface waters, and the animals are transported by surface currents from Lipids and life strategy of Arctic Calanus 19 their centre of distribution in the Norwegian Sea to all bordering seas (Sundby 2000).”
Projecting changes in the distribution and productivity of living marine resources: A critical review of the suite of modelling approaches used in the large European project VECTORS (2016, background): “…can alter growth performance and the reproductive potential of adults (Marshall et l., 2000 and Kraus et al., 2002) as well as the rates of survival of their progeny (e.g. Sundby, 2000) whereas top-down processes can regulate lower trophic levels (Shurin et al., 2002 and Mueter et al., 2006).”
The response of Atlantic cod (Gadus morhua) to future climate change (2005, methodology): “in recruitment per unit change in SST and plotted against the mean annual bottom temperature of the stock (Sundby, 2000) (Figure 4).”