Feuchtmayr H, McKee D, Harvey IF, Atkinson D, Moss B
Global climate change, temperature, Sampling technique, Sweep net, Gasterosteus aculeatus, mesocosm, Ness Gardens, Liverpool, 3 m3, UK
Feuchtmayr H, McKee D, Harvey IF, Atkinson D, Moss B
Global climate change, temperature, Sampling technique, Sweep net, Gasterosteus aculeatus, mesocosm, Ness Gardens, Liverpool, 3 m3, UK
DeYoe HR, Buskey EJ, Jochem FJ
Aureoumbra, Brown tide, Harmful algal bloom, mesocosm, nitrogen, Synechococcus, Corpus Christi, Texas, 1.2-1.4 m3, USA
Davidson K, Gilpin LC, Hart MC, Fouilland E, Mitchell E, Calleja IA, Laurent C, Miller AEJ, Leakey RJG
mesocosm, nitrogen limitation, Diatoms, 1.5 m3, Hopavagen, Norway
Castilho-Noll MSM, Arcifa MS
Chaoborus predation, Copepod, Daphnia, enclosure, population dynamics, mesocosm, lake Monte Alegre, Sao Paulo, Brazil, 6.6 m3
Carotenuto Y, Putzeys S, Simonelli P, Paulino A, Meyerhofer M, Suffrian K, Antia A, Nejstgaard JC
mesocosm, co2, climate change, Zooplankton, Bergen, Norway, 10 m3
Berger SA, Diehl S, Stibor H, Trommer G, Ruhenstroth M, Wild A, Weigert A, Jäger CG, Striebel M
algal spring bloom, clear-water, Daphnia, enclosure, experiment, phytoplankton, Zooplankton, climate change, NORTH-ATLANTIC OSCILLATION, DIEL VERTICAL MIGRATION, LIFE-HISTORY, PARAMETERS, FOOD CONCENTRATION, EUROPEAN LAKES, Dynamics
In many lakes, the most conspicuous seasonal events are the phytoplankton spring bloom and the subsequent clear-water phase, a period of low-phytoplankton biomass that is frequently caused by mesozooplankton (Daphnia) grazing. In Central European lakes, the timing of the clear-water phase is linked to large-scale climatic forcing, with warmer winters being followed by an earlier onset of the clear-water phase. Mild winters may favour an early build-up of Daphnia populations, both directly through increased surface temperatures and indirectly by reducing light limitation and enhancing algal production, all being a consequence of earlier thermal stratification. We conducted a field experiment to disentangle the separate impacts of stratification depth (affecting light supply) and temperature on the magnitude and timing of successional events in the plankton. We followed the dynamics of the phytoplankton spring bloom, the clear-water phase and the spring peak in Daphnia abundance in response to our experimental manipulations. Deeper mixing delayed the timing of all spring seasonal events and reduced the magnitudes of the phytoplankton bloom and the subsequent Daphnia peak. Colder temperatures retarded the timing of the clear-water phase and the subsequent Daphnia peak, whereas the timing of the phytoplankton peak was unrelated to temperature. Most effects of mixing depth (light) and temperature manipulations were independent, effects of mixing depth being more prevalent than effects of temperature. Because mixing depth governs both the light climate and the temperature regime in the mixed surface layer, we propose that climate-driven changes in the timing and depth of water column stratification may have far-reaching consequences for plankton dynamics and should receive increased attention.
Benthien A, Zondervan I, Engel A, Hefter J, Terbruggen A, Riebesell U
CO2 enrichment, Primary production, Emiliania huxleyi, isotopic fractionation, 11 m3, mesocosm, Espegrend, Raunefjord, Bergen, Norway
Aberle N, Lengfellner K, Sommer U
microzooplankton, Baltic, climate change, global change, phytoplankton blooms, north-sea, trophic interactions, helgoland roads, marine plankton, coastal waters, size selection, regime shifts, feeding rates, mesocosm, Kiel, 1.4 m3, Germany
This study aimed at simulating different degrees of winter warming and at assessing its potential effects on ciliate succession and grazing-related patterns. By using indoor mesocosms filled with unfiltered water from Kiel Bight, natural light and four different temperature regimes, phytoplankton spring blooms were induced and the thermal responses of ciliates were quantified. Two distinct ciliate assemblages, a pre-spring and a spring bloom assemblage, could be detected, while their formation was strongly temperature-dependent. Both assemblages were dominated by Strobilidiids; the pre-spring bloom phase was dominated by the small Strobilidiids Lohmaniella oviformis, and the spring bloom was mainly dominated by large Strobilidiids of the genus Strobilidium. The numerical response of ciliates to increasing food concentrations showed a strong acceleration by temperature. Grazing rates of ciliates and copepods were low during the pre-spring bloom period and high during the bloom ranging from 0.06 (Delta 0 degrees C) to 0.23 day(-1) (Delta degrees C) for ciliates and 0.09 Delta degrees C) to 1.62 day(-1) (Delta degrees C) for copepods. During the spring bloom ciliates and copepods showed a strong dietary overlap characterized by a wide food spectrum consisting mainly of Chrysochromulina sp., diatom chains and large, single-celled diatoms.
Vogt M, Turner S, Yassaa N, Steinke M, Williams J, Liss P
Dimethylsulphide, DMS, Seawater, Solid-phase microextraction, Purge and trap, Sample preparation, Norwegian Fjord, mesocosm, 20 m3, Raunefjord, Bergen, Norway
Vogt M, Steinke M, Turner S, Paulino A, Meyerhofer M, Riebesell U, LeQuere C, Liss P
DMS, Dimethylsulfide, co2, enrichment, phytoplankton, mesocosm, Raunefjord, Bergen, 25 m3, Espegrend, Norway