Marino R, Chan F, Howarth RW, Pace M, Likens GE
nitrogen fixation, estuaries, eutrophication, nitrogen limitation, grazing, heterocystic cyanobacteria, mesocosm, Naragansett Bay, Rhode island, land based, 3 m3, USA
Marino R, Chan F, Howarth RW, Pace M, Likens GE
nitrogen fixation, estuaries, eutrophication, nitrogen limitation, grazing, heterocystic cyanobacteria, mesocosm, Naragansett Bay, Rhode island, land based, 3 m3, USA
Kraufvelin P, Christie H, Olsen M
coastal eutrophication, rocky shores, macrofauna, BACIP, mesocosm, whole-ecosystem experiment, Norway, Solbergstrand, Oslofjord, 12 m3
Macrofauna secondary responses to controlled eutrophication within two MARICULT/MAST-III projects, EULITand COMWEB, are compared. EULIT utilises a nutrient gradient established in eight hard bottom mesocosms,whereas the data from COMWEB originate from a whole-ecosystem study – the case of experimental nutrientaddition to Hopavågen lagoon. In both systems, nutrient addition started in May 1998, after initial studies of thebackground macrofauna communities, thus allowing application of Before-After-Control-Impact-Pairs techniques(BACIP). The main objectives have been to investigate the macrofauna responses to eutrophication in littoral rockyshore ecosystems and to evaluate if similar responses could occur in mesocosm and ‘field’ systems, despite theirinherent differences. Apart from a distinct increase in numbers of Littorina littorea L. and some indications ofincreased abundance of the genus Jaera, no significant changes, caused by 2.5 years of nutrient addition, couldbe detected in the mesocosm fauna. It is interesting, however, that these two possibly stimulated animal groupshave two things in common: (1) both belong to the rather few mobile taxa, which are not flushed out of thesystem through the mesocosm outlets, (2) both feed on microalgae and green algae in the upper littoral zone,i.e., algal groups that have shown the clearest response to the nutrient addition. In Hopavågen, 1.5 years ofnutrient addition only caused modest plant and animal responses in the rocky shore ecosystem, although therewas a markedly increased settlement of Mytilus edulis L. at one lagoon site. This increase was probably due toelevated levels of digestible particles (increased phytoplankton production) caused by the nutrient addition. Therewere also some indications of increased production of filamentous algae at this same lagoon site. All in all, bothstudies demonstrate only minor responses to increased nutrient levels within the littoral community (both plantsand animals). One explanation to this may be that longer time-scales are needed in order for clear-cut changes tooccur. Several observations also indicate that wave exposure (significant in both systems) may largely modulatethe impact of increased nutrient load on the structure of littoral communities. Another explanation is the highdegree of stability among littoral macroalgae-dominated communities with internal biological regulation factors(like grazing) possibly being able to counteract effects.
Joint I, Henriksen P, Fonnes G, Bourne D, Thingstad F, Riemann B
Phytoplankton/bacterial competition, Nutrient uptake, Pigment taxonomy, mesocosm, Holbek, Roskilde, Denmanrk, 1.7 m3
Jacquet S, Heldal M, Rodriguez ID, Larsen A, Wilson W, Bratbak G
Diel variations, Dynamics, Emiliania huxleyi, Flow cytometry, mesocosm, virus, Espegrend, Bergen, 11 m3, Norway
Jacquet S, Havskum H, Thingstad TF, Vaulot D
carbon, Competition, Flow cytometry, Food web, mesocosms, picoplankton, Nutrients, virus, Isefjord, Denmark, 3 m3
Using flow cytometry (FCM), microbial populations were followed in a mesoscosmexperiment manipulated with daily additions of mineral nutrients (as phosphates and nitrates in Redfieldequilibrium), of degradable organic carbon (as glucose-C), or with the 2 treatments combined.Intensive sampling was performed in order to assess the short time-scale variability of the microbialcommunity. Five autotrophic groups (including Synechococcus spp. and cryptophytes), 2 groups ofheterotrophic bacteria, and 2 groups of viruses could be discriminated by FCM. The control enclosure(no addition) revealed that heterotrophic bacteria were carbon-limited. Synechococcus spp. abundanceincreased in the control, presumably because they experienced little competition from heterotrophicbacteria (which were C-limited) and from larger phytoplankton (which were not as efficientin nutrient uptake at low nutrient concentration and could not, therefore, sustain high growth rates).When N and P were added, however, larger-celled autotrophic populations were favoured. Whenglucose was added, alone or together with inorganic elements, the abundance of Synechococcus spp.and small eukaryotes was reduced, suggesting that, when released from C-limitation, heterotrophicbacteria are the best competitors for mineral nutrients. The addition of both inorganic and organicnutrients also enhanced cryptophytes in contrast to all other autotrophs, probably because of theirheterotrophic capacity. Our results agree with recent evidence suggesting that heterotrophic bacteriaare limited by both carbon and mineral nutrients, and demonstrate how this has important consequencesfor the success of their trophic neighbours in the microbial food web.
Gismervik I, Olsen Y, Vadstein O
nutrent enrichment, ciliates, mesozooplankton, egg production, species composition, mesocosm, 38 m3, Trondheim fjord, Norway
Escaravage V, Prins TC
Diatoms, Phaeocystis, Cerataulina marina, stratification, ciliates, copepods, mesocosm, 3 m3, landbased, Oosterschelde estuary, Netherlands
Engel A, Goldthwait S, Passow U, Aldredge A
Biogeochemichal fluxes, redfield, Diatoms, TEP, mesocosm, 1 m3, organic matter, land based, Santa Barbara channel, USA
Elser JJ, Frost P, Kyle M, Urabe J, Andersen T
P limitation, mesocosm, light intensity, nutrient addition, algae, Experimental Lake Area, Ontario, Canada, 25 m3, freshwater
Diehl S, Berger S, Ptacnik R, Wild A
We studied the effects of water column mixing depth and background turbidity on phytoplankton biomass, light climate, and nutrients in two field enclosure experiments designed to test predictions of a dynamical model. In 1997 and 1998, we created gradients of mixing depth by enclosing the 100-μm-filtered phytoplankton community of a phosphorus-deficient lake in cylindrical plastic bags of varying depth (1.5-15 m) which were continuously mixed. To mimic different levels of background turbidity, we surrounded the transparent enclosure walls with a layer of opaque white (1997) or black (1998) plastic. The experiments were run for 4 wk (1997) and 6 wk (1998). The results supported two key assumptions of the model: specific production and specific sedimentation losses both decreased with increasing mixing depth. At all mixing depths, fast-sinking diatoms dominated the communities. In accordance with model predictions, algal biomass concentration and standing stock (summed over the mixed layer) showed a unimodal relationship to mixing depth when background turbidity was high (1998). When background turbidity was lower (1997), only the ascending limbs of the corresponding relationships were found, which supports the prediction that the mixing depth at which biomass peaks (i.e., becomes predominantly limited by light) increases with decreasing background turbidity. Also in accordance with predictions, light intensity at the bottom of the mixed layer decreased with increasing mixing depth and with increasing background turbidity. Finally, the data supported only the ascending limbs of the predicted inverse unimodal relationships among mixing depth and dissolved inorganic and total water column phosphorus. The absence of descending limbs in these relationships at low mixing depths was probably due to deviations of the experimental systems from two model assumptions. First, the remineralization rate of sedimented phosphorus may have been too slow to equilibrate with sedimentation losses over the experimental periods. Second, biomass yield per unit nutrient (the ratio of seston carbon to phosphorus) was not constant, but decreased with increasing mixing depth. To our knowledge, these are the first field experiments in which the effects of mixing depth on phytoplankton and its resources have been investigated systematically along a large gradient.