Variable littoral-pelagic coupling as a food-web response to seasonal changes in pelagic primary production

2017 ◽  
Vol 62 (12) ◽  
pp. 2008-2025 ◽  
Author(s):  
Simon D. Stewart ◽  
David P. Hamilton ◽  
W. Troy Baisden ◽  
Michel Dedual ◽  
Piet Verburg ◽  
...  
Water ◽  
2021 ◽  
Vol 13 (21) ◽  
pp. 3085
Author(s):  
Edward Laws ◽  
Kanchan Maiti

Knowledge of the relationship between net primary production (NPP) and export production (EP) in the ocean is required to estimate how the ocean’s biological pump is likely to respond to climate change effects. Here, we show with a theoretical food web model that the relationship between NPP and EP is obscured by the following phenomena: (1) food web dynamics, which cause EP to be a weighted average of new production (NP) over a previous temperature-dependent time interval that can vary between several weeks at 25 °C to several months at 0 °C and, hence, to be much less temporally variable than NP and (2) the temperature dependence of the resiliency of the food web to perturbations, which causes the return to equilibrium to vary from roughly 50 days at 0 °C to 5–10 days at 25 °C. The implication is that the relationship between NPP and EP can be discerned at tropical and subtropical latitudes if measurements of NPP and EP are averages or climatologies over a timeframe of roughly one month. At high latitudes, however, measurements may need to be averaged over a timeframe of roughly one year because the food webs at high latitudes are very likely far from equilibrium with respect to NPP and EP much of the time, and the model can describe only the average behavior of such physically dynamic systems.


Author(s):  
A. D. Boney

SynopsisAnalysis of the factors influencing the seasonal changes in biomass of the ‘net’ phytoplankton in 1972– 73 snowed that the dynamics of the spring waxing of the diatom populations were controlled by narrow ‘windows’ of climatic events, and that subsequent fluctuations in cell numbers were linked with the interplay between zooplankton grazing and wind induced dispersion. Data for 1976–77, set against a similar background of events with the ‘net’ plankton, showed that the nanophytoplankton constituted a less variable biomass through the seasons and, on an annual basis, contributed some 50% of the total carbon fixed.


2020 ◽  
Vol 652 ◽  
pp. 15-32 ◽  
Author(s):  
MR Landry ◽  
MR Stukel ◽  
M Décima

We investigated how the network of food-web flows in open-ocean systems might support high rates of mesozooplankton respiration and production by comparing predicted rates from empirical relationships to independently determined solutions from an inverse model based on tightly constrained field-measured rates for the equatorial Pacific. Model results were consistent with estimates of gross:net primary production (GPP:NPP), bacterial production:NPP, sinking particulate export, and total export for the equatorial Pacific, as well as general literature values for growth efficiencies of bacteria, protozooplankton, and metazooplankton. Mean rate estimates from the model compared favorably with the respiration predictions from Ikeda (1985; Mar Biol 85:1-11) (146 vs. 144 mg C m-2 d-1, respectively) and with production estimates from the growth rate equation of Hirst & Sheader (1997; Mar Ecol Prog Ser 154:155-165) (153 vs. 144 mg C m-2 d-1). Metazooplankton nutritional requirements are met with a mixed diet of protozooplankton (39%), phytoplankton (36%), detritus (15%), and carnivory (10%). Within the food-web network, NPP of 896 mg C m-2 d-1 supports a total heterotrophic carbon demand from bacteria, protozoa, and metazooplankton that is 2.5 times higher. Scaling our results to primary production and zooplankton biomass at Stn ALOHA suggests that zooplankton nutritional requirements for high growth might similarly be met in oligotrophic subtropical waters through a less efficient trophic structure. Metazooplankton production available to higher-level consumers is a significant contributor to the total export needed for an overall biogeochemical balance of the region and to export requirements to meet carbon demand in the mesopelagic depth range.


2020 ◽  
Vol 636 ◽  
pp. 235-241 ◽  
Author(s):  
HM McNair ◽  
S Menden-Deuer

Grazing by herbivorous protists (microzooplankton) is a major loss pathway of primary production in the surface ocean, yet its impact below the well-lit surface ocean is largely unknown. The upper boundary of the twilight zone is critically important to understanding carbon cycling and is often the depth of highest attenuation of particulate carbon flux. Available measurements of primary production and grazing below the well-lit surface ocean suggest that the upper boundary of the twilight zone may harbor active but poorly constrained food web processes. Previous grazing rates from the base of the euphotic zone were measured in subtropical and tropical environments. Thus, the impact of protist grazing on prey populations remains unknown in colder conditions at higher latitudes. To advance understanding and provide mechanistic insight into processes occurring at the base of the euphotic zone (0.4-0.7% PAR), we measured predation rates on both phytoplankton and heterotrophic prokaryotes in the North Pacific, using a novel method that amplified the grazing signal by concentrating the predator community, enabling detection of grazing rates far below previous limits. Protists consumed 0.6% of the phytoplankton population daily and 12% of daily heterotrophic prokaryote growth. These conservative rate measurements document marginal removal of phytoplankton even in these colder regimes, implying flows of energy from single-cell primary producers and prokaryotes to single-cell protists at rates far below previous detection limits in this twilight region of a low-productivity system.


1987 ◽  
Vol 65 (12) ◽  
pp. 3116-3132 ◽  
Author(s):  
Gabriel Lamarche ◽  
Pierre Brunel

Bimonthly quantitative day and night samples from one monitoring station located in the St. Lawrence Estuary (in silt–clay, at a depth of 119 m), with a constant yearly temperature (1–4 °C), reveal that densities of the detrivorous and necrophagous lysianassid amphipod Hippomedon propinquus were similar (0.4–9.7 individuals/100 m3 in 1970, 1971, and 1973) to densities at another station in Chaleur Bay with comparable sediments, temperature, and depth (4.2–7.5 individuals/100 m3 in 1969 and 1971). However, its rank among the gammaridean community (10th to 15th in the bay, 3rd to 5th in the estuary) and a faster growth in the estuary suggest better "success" in the latter. Vertical migrations are mainly diurnal and of higher amplitude in the bay than in the estuary, where these are mostly nocturnal, except in June and July. Life expectancy is over 2 years with a maximum of 13 molts, 4 to 5 of which occur in the adult stage. Growth is slower, life expectancy is shorter, but rank is higher (third) at another Chaleur Bay station where H. propinquus also displays increased swimming activity. In both ecosystems, reproduction is mostly a continuous, year-round process, but juvenile recruitment is more important in spring and summer, conforming to our prediction that life cycle is more independent of primary production and seasonal sestonic fallout when species occupy higher positions in the food web. Average size of ovigerous females decreases while fecundity increases in summer. Females produce larger eggs in Chaleur Bay. Poorer and less predictable primary production in the St. Lawrence Estuary gives opportunistic species like H. propinquus an advantage over more strictly detrivorous crustacean species.


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