Optimum Temperatures for Common Zooplankton Species in the White Sea

Zubakha, M. A.; Usov, Nikolay

doi:10.1023/b:rumb.0000046547.26708.3e

Cited by 6 publications

(1 citation statement)

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“…On the whole, P. minutus appeared in our study to be much less sensitive to temperature variations than Calanus glacialis, both on aggregated scales and when looking at the seasonal development of the individual life stages. This is consistent with the wider temperature range of the Arctic-boreal P. minutus (−1.8 to 15.5°C), compared to that of the Arctic C. glacialis (−0.39 to 4.86°C) (Prygunkova 1974, Zubakha & Usov 2004. The temperature effects found for P. minutus (Table 3) suggest slightly earlier development in warm years (Figs.…”

Section: Discussionsupporting

confidence: 77%

Scale-dependent effects of climate on two copepod species, Calanus glacialis and Pseudocalanus minutus, in an Arctic-boreal sea

Persson¹,

Stige²,

Stenseth³

et al. 2012

Mar. Ecol. Prog. Ser.

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Climate-driven changes in the phenology and composition of plankton affect ecosystem structure and function, but knowledge about such changes is limited by the scarcity of highquality, high-resolution, long-term monitoring data. Using a high-resolution observation series from the White Sea, spanning > 50 yr, we explored how water temperature and salinity influenced 2 key copepod species, Calanus glacialis and Pseudocalanus minutus. The results of the analysis depended critically on the temporal and life-stage resolution of the analysis. Copepod biomass was negatively correlated with salinity, but not correlated with temperature, when using annually aggregated data. However, salinity showed very small effects at a monthly resolution, failing to support a causal effect of salinity. On the other hand, temperature did show effects: in warm years, the biomass of C. glacialis increased earlier in spring and declined earlier in autumn. Analysis of stage-resolved data revealed a new level of complexity. The increase of biomass in spring at warmer temperatures mainly consisted of young life stages, whereas the decrease in autumn was mainly caused by reductions in older life stages. Temperature affected the phenology of several life stages of P. minutus, but not its total biomass, implying that climate effects on different life stages cancelled each other out. We argue that such climate-driven fluctuations in zooplankton phenology and age structure are likely to influence the role of the zooplankton as predators, competitors and prey, but that these effects of climate could remain unnoticed when using the coarser resolution of many sampling programs.KEY WORDS: Scale dependence · Copepods · Developmental stages · Temperature · Marine · White Sea · Phenology · Generalized additive modelling Resale or republication not permitted without written consent of the publisherMar Ecol Prog Ser 468: [71][72][73][74][75][76][77][78][79][80][81][82][83] 2012 temperature−size rule), although the mechanisms causing such a shift are not clear. Changes in the structure of marine ecosystems can affect their function, which, in turn, may feed back on the structure. For example, shifts in the timing and size spectra of prey (copepods) influence the survival of juvenile cod (Munk 1997, Beaugrand et al. 2003), a key species in many North Atlantic shelf systems. In order to understand how climate affects the dynamics of marine ecosystems, it is therefore important to consider the associated changes in ecosystem structure, which requires data with sufficient resolution in space, time (season) and species' stage and size composition.In recent decades we have seen significant changes in the distribution and phenology of zooplankton. For example, the copepod biomass peak in the Central North Sea has advanced by 10 d in 45 yr (reviewed by Richardson 2008). In the Arctic, changes in the circulation and temperature of water and air, as well as changes in ice cover, have been shown to lead to increased primary production and altered zooplan...

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Section: Discussionsupporting

confidence: 77%