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Journal articles on the topic 'Plankton succession'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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1

Matveev, V. F., and L. K. Matveeva. "Seasonal succession and long-term stability of pelagic community in a productive reservoir." Marine and Freshwater Research 56, no. 8 (2005): 1137. http://dx.doi.org/10.1071/mf04289.

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In Lake Hume, a reservoir located in an active agricultural zone of the Murray River catchment, Australia, time series for the abundances of phytoplankton and zooplankton taxa, monitored from 1991 through to 1996, were stationary (without trends), and plankton taxonomic composition did not change. This indicated ecosystem resilience to strong fluctuations in reservoir water level, and to other potential agricultural impacts, for example eutrophication and pollution. Although biological stressors such as introduced fish and invertebrate predators are known to affect planktonic communities and r

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2

Havens III, Karl E., and John DeCosta. "Freshwater plankton community succession during experimental acidification." Archiv für Hydrobiologie 111, no. 1 (1987): 37–65. http://dx.doi.org/10.1127/archiv-hydrobiol/111/1987/37.

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3

Di Stefano, Agata, Marina Verducci, Antonio Cascella, and Silvia Maria Iaccarino. "Calcareous plankton events at the Early/Middle Miocene transition of DSDP Hole 608: comparison with Mediterranean successions for definition of the Langhian GSSP." Stratigraphy 8, no. 2-3 (2011): 145–61. http://dx.doi.org/10.29041/strat.08.2.05.

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We propose a revision of the calcareous plankton biostratigraphy of the upper Burdigalian/early Langhian interval (Early/Middle Miocene) of the DSDP Hole 608 succession (northeastern Atlantic Ocean), one of the most complete open-ocean Miocene sequences. We detected a set of calcareous plankton events through a 26m thick succession (320-346 mbsf), spanning the interval from 14.969 to 17.268 Ma, chronologically constrained through paleomagnetic and astrochronological data. "Standard" bioevents were tested and in some cases they resulted poorly applicable to the investigated succession. Converse

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4

Sommer, Ulrich, Rita Adrian, Lisette De Senerpont Domis, et al. "Beyond the Plankton Ecology Group (PEG) Model: Mechanisms Driving Plankton Succession." Annual Review of Ecology, Evolution, and Systematics 43, no. 1 (2012): 429–48. http://dx.doi.org/10.1146/annurev-ecolsys-110411-160251.

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5

Jamet, J. L., N. Jean, G. Bogé, S. Richard, and D. Jamet. "Plankton succession and assemblage structure in two neighbouring littoral ecosystems in the north-west Mediterranean Sea." Marine and Freshwater Research 56, no. 1 (2005): 69. http://dx.doi.org/10.1071/mf04102.

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We studied seasonal variations in bacterial abundance and succession in phyto- and zooplankton assemblages (particularly small taxa) in two neighbouring shallow bays (near Toulon, Mediterranean Sea, France): Little Bay (polluted, eutrophic), and Niel Bay (less polluted, oligotrophic). In Little Bay, bacteria developed in northern spring and phytoplankton (Dinophyceae > 20 µm) in late northern winter–early spring. Zooplankton levels peaked at the end of northern spring and in autumn; this community was dominated by Oithona nana. In Niel Bay, bacterial levels peaked during northern spring and

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6

Vanni, Michael J. "Ecological Succession: A Mechanistic Approach in Plankton Communities." Ecology 71, no. 4 (1990): 1630–31. http://dx.doi.org/10.2307/1938301.

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7

Mariani, Patrizio, Ken H. Andersen, André W. Visser, Andrew D. Barton, and Thomas Kiørboe. "Control of plankton seasonal succession by adaptive grazing." Limnology and Oceanography 58, no. 1 (2012): 173–84. http://dx.doi.org/10.4319/lo.2013.58.1.0173.

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8

Paul, Allanah Joy, Lennart Thomas Bach, Javier Arístegui, et al. "Upwelled plankton community modulates surface bloom succession and nutrient availability in a natural plankton assemblage." Biogeosciences 19, no. 24 (2022): 5911–26. http://dx.doi.org/10.5194/bg-19-5911-2022.

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Abstract. Upwelling of nutrient-rich waters into the sunlit surface layer of the ocean supports high primary productivity in eastern boundary upwelling systems (EBUSs). However, subsurface waters contain not only macronutrients (N, P, Si) but also micronutrients, organic matter and seed microbial communities that may modify the response to macronutrient inputs via upwelling. These additional factors are often neglected when investigating upwelling impacts on surface ocean productivity. Here, we investigated how different components of upwelled water (macronutrients, organic nutrients and seed

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9

Romagnan, Jean-Baptiste, Louis Legendre, Lionel Guidi, et al. "Comprehensive Model of Annual Plankton Succession Based on the Whole-Plankton Time Series Approach." PLOS ONE 10, no. 3 (2015): e0119219. http://dx.doi.org/10.1371/journal.pone.0119219.

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10

Robinson, G. A., J. Aiken, and H. G. Hunt. "Synoptic Surveys of the Western English Channel. The Relationships Between Plankton and Hydrography." Journal of the Marine Biological Association of the United Kingdom 66, no. 1 (1986): 201–18. http://dx.doi.org/10.1017/s0025315400039746.

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Variability in the distribution and abundance of the plankton of the western English Channel has been investigated in relation to the hydrography of the region by surveys using the Continuous Plankton Recorder (CPR) (Hardy, 1939) and the Undulating Oceanographic Recorder (UOR) (Aiken, 1981a). Previous surveys in the western English Channel have been restricted in area or in time. Harvey et al. (1935), Holligan & Harbour (1977) and Maddock, Boalch & Harbour (1981) have studied the seasonal succession of the plankton at point stations near Plymouth, with analysis of patterns of seasonal

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11

Di Stefano, Agata, Marina Verducci, Rosanna Maniscalco, Fabio Speranza, and Luca M. Foresi. "High-resolution stratigraphy of the Contrada Pesciarello borehole succession (SE Sicily): a lower Langhian reference section for the Mediterranean region." Stratigraphy 8, no. 2-3 (2011): 111–24. http://dx.doi.org/10.29041/strat.08.2.03.

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The results of a high-resolution multidisciplinary stratigraphic study of a lower Langhian succession, located in the Hyblean Plateau (SE Sicily, southern Italy), are here presented. The about 33m thick succession, which belongs to the “Ragusa Fm” (Auct.), has been recovered through a continuous coring survey and highly-spaced sampled. A total amount of 281 samples has been collected at an average interval of about 12cm for the following analyses: quantitative calcareous nannofossil and planktonic foraminifer biostratigraphy, paleomagnetism, CaCO3 content. The distribution pattern of biostrati

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12

Stoykova, Kristalina, Sava Juranov, and Marin Ivanov. "Calibration of calraceous nannofossils and planktonic foraminifers’ zonation in the Lower and Middle Paleocene of Bulgaria." Geologica Balcanica 35, no. 1-2 (2005): 3–9. http://dx.doi.org/10.52321/geolbalc.35.1-2.3.

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This study represents first attempt to juxtapose and correlate the zonal schemes of calcareous nannofossils and planktonic foraminifers in the Lower and Middle Paleocene of Bulgaria. The calibration of the two schemes is accomplished in the most complete and continuous sedimentary succession of Byala Fm., cropping out in the sections around the village of Goritsa, Varna District. In the Danian Stage the presence of NP1-NP4 nannofossil zones as well as of the planktic foraminifera zones Pα, P1a, P1b, P1c, P3a is documented. In despite of the scarce paleontological data, the presence of P0 zone

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13

Yu Afonina, E., and N. A. Tashlykova. "Dynamics of plankton biocenoses under water level fluctuations in steppe lakes." IOP Conference Series: Earth and Environmental Science 962, no. 1 (2022): 012002. http://dx.doi.org/10.1088/1755-1315/962/1/012002.

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Abstract Barun-Torey and Zun-Torey lakes are located in the arid steppe zone of the Central (Inner) Asia, Eastern Siberia, Russia. The Torey lakes are characterizes unstable hydrological regime. The water level variation is explained by the periodic filling and drying of the lakes due to cyclical climatic changes in humidity and temperature. We conducted our studies various water level phases of the climatic cycle: from high water level (1999, 2003) to drying out and the initial filling phase (2007, 2011, 2014, 2016, 2018, and 2020). The aim of this paper is to present long-term research resul

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14

Turco, Elena, Antonio Cascella, Rocco Gennari, Frits J. Hilgen, Silvia Maria Iaccarino, and Leonardo Sagnotti. "Integrated stratigraphy of the La Vedova section (Conero Riviera, Italy) and implications for the Burdigalian/Langhian boundary." Stratigraphy 8, no. 2-3 (2011): 89–110. http://dx.doi.org/10.29041/strat.08.2.02.

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We present a high resolution integrated stratigraphy (calcareous plankton biostratigraphy and magnetostratigraphy) of the upper Burdigalian to lower Langhian interval in the La Vedova section (Conero Riviera, Italy). The succession of planktonic foraminifer and calcareous nannofossil events and their relative position in the La Vedova section are comparable with those recorded in other Mediterranean sections suggesting a continuous deposition across the Burdigalian/Langhian boundary interval. The high resolution magnetostratigraphic record, integrated with calcareous plankton events, has been

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15

Urabe, Jotaro. "Midsummer succession of rotifer plankton in a shallow eutrophic pond." Journal of Plankton Research 14, no. 6 (1992): 851–66. http://dx.doi.org/10.1093/plankt/14.6.851.

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16

Chen, Ning, Ling Liu, Danying Qiao, Yanfeng Li, and Yiyan Lv. "Seasonal succession patterns of plankton in eutrophic rivers on plains." Annales de Limnologie - International Journal of Limnology 52 (2016): 217–33. http://dx.doi.org/10.1051/limn/2016007.

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17

Berge, Terje, Subhendu Chakraborty, Per Juel Hansen, and Ken H. Andersen. "Modeling succession of key resource-harvesting traits of mixotrophic plankton." ISME Journal 11, no. 1 (2016): 212–23. http://dx.doi.org/10.1038/ismej.2016.92.

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18

Peters, F. "On some relationships between storms and plankton dynamics." Advances in Geosciences 26 (June 30, 2010): 33–38. http://dx.doi.org/10.5194/adgeo-26-33-2010.

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Abstract. The physico-chemical fields of the pelagic environment are constantly fluctuating at different spatial and temporal scales. Storms are extreme events of such fluctuations that cascade down to small scales to alter nutrient availability to microscopic algae or swimming and mating behaviour of motile plankton. Mediterranean storms sometimes are also responsible for the transport of micro and macronutrients from Saharan origin, albeit the significance for marine production is still under question. In coastal ecosystems, storms represent dissolved nutrient injections via run-off and resu

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19

Straškrabová, Vera, Josef Hejzlar, Lidmila Procházková, and Vojtech Vyhnálek. "Eutrophication in stratified deep reservoirs." Water Science and Technology 30, no. 10 (1994): 273–79. http://dx.doi.org/10.2166/wst.1994.0537.

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The response of phytoplankton development to an increased nutrient input in deep canyon-shaped stratified reservoirs was shown in four case studies. In contrast to lakes, specific features were described: longitudinal succession of phytoplankton development along the valley, transport of algal biomass and the peculiarities of P loading to epilimnion during summer stratification. Long term studies in two reservoirs showed the fluctuations of particular plankton components due to variations in flushing rate on the one hand and fish succession leading to prevalence of planktivorous species on the

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20

Michaloudi, Evangelia, Maria Moustaka-Gouni, Kimon Pantelidakis, Matina Katsiapi, and Savvas Genitsaris. "Plankton Succession in the Temporary Lake Koronia after Intermittent Dry-Out." International Review of Hydrobiology 97, no. 5 (2012): 405–19. http://dx.doi.org/10.1002/iroh.201101498.

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21

Triantaphyllou, M. V., A. Antonarakou, H. Drinia, et al. "HIGH RESOLUTION BIOSTRATIGRAPHY AND PALEOECOLOGY OF THE EARLY PLIOCENE SUCCESSION OF PISSOURI BASIN (CYPRUS ISLAND)." Bulletin of the Geological Society of Greece 43, no. 2 (2017): 763. http://dx.doi.org/10.12681/bgsg.11242.

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The Pissouri basin (Cyprus Island) corresponds to a small tectonically controlled depression elongated NNW-SSE and widening southward in the direction of the deep Mediterranean domain. In the centre of the basin, the section Pissouri South, about 100 m thick, consists of well-preserved cyclic marine sediments including laminated brownish layers alternating with grey homogeneous marls. Plankton biostratigraphy (calcareous nannofossil and planktonic foraminifera) revealed a remarkable number of biovents bracketing the Zanclean-Piacenzian boundary. In particular the Highest Occurrence (HO) of Ret

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22

Maniscalco, Rosanna, Martina Forzese, Viviana Barbagallo, et al. "Toward an Astrochronology-Based Age-Model for a Messinian Pre-Evaporitic Succession: The Example of Torrente Vaccarizzo Section in Sicily (Italy)." Journal of Marine Science and Engineering 11, no. 5 (2023): 915. http://dx.doi.org/10.3390/jmse11050915.

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Tectonic, paleoenvironmental, and paleoclimatic unstable conditions preceding the onset of the Messinian Salinity Crisis (MSC) highly affected marine life. Changes in calcareous plankton association are overall registered in the Mediterranean. They consist of a general transition from abundant and well-diversified planktonic associations to strictly oligotypic assemblages that precede their total disappearance at the onset of evaporitic precipitation. In this work, an accurate quantitative analysis of calcareous plankton, both foraminifers and nannofossils, has been carried out in the Torrente

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23

Yamada, Machiko, Yoshifumi Hanada, Akio Miyazaki, Arao Tsuruta, and Yoichi Yoshida. "Succession of the plankton community during coastal reclamation with the solid wastes." NIPPON SUISAN GAKKAISHI 56, no. 5 (1990): 729–34. http://dx.doi.org/10.2331/suisan.56.729.

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24

Albarico, Frank Paolo Jay B., Yee Cheng Lim, Chiu-Wen Chen, Chih-Feng Chen, Ming-Huang Wang, and Cheng-Di Dong. "Linking seasonal plankton succession and cellular trace metal dynamics in marine assemblages." Science of The Total Environment 907 (January 2024): 167805. http://dx.doi.org/10.1016/j.scitotenv.2023.167805.

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25

Riforgiato, Federica. "Revision of the Messinian-Early Zanclean Sediments from ODP Hole 953C (Canary Island Archipelago, North-Eastern Atlantic): Biostratigraphy, Cyclostratigraphy, and Astronomical Tuning." Paleontology Journal 2013 (March 21, 2013): 1–17. http://dx.doi.org/10.1155/2013/947839.

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A quantitative study was performed on calcareous plankton of the Messinian-early Zanclean succession recovered at ODP Leg 157 Hole 953C (Canary Island Archipelago, North-Eastern Atlantic). This revision allowed to recognize some events typically recorded in the Mediterranean region, highlighting affinities between the Mediterranean and North Atlantic Ocean, in the considered time interval. The presence of such events in an open-ocean succession provides the possibility to substantially improve the biostratigraphic resolution and supplies useful correlation tools between the Mediterranean and o

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26

Arumugam, PT, and MC Geddes. "Effects of golden perch (Macquaria ambigua (Richardson)) larvae, fry and fingerlings on zooplankton communities in larval-rearing ponds: An enclosure study." Marine and Freshwater Research 47, no. 6 (1996): 837. http://dx.doi.org/10.1071/mf9960837.

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In the absence of fish, the plankton community in enclosures in a larval-rearing pond showed a marked successional pattern from rotifers and Moina to copepod and then Daphnia-calanoid dominance. The impact of growing larvae and fry, with densities of 40-118 m-2 at harvest, on zooplankton was conspicuous only after Day 22 when Daphnia became rare and calanoid numbers were suppressed. Predation by fry caused reductions in the size of Moina, cyclopoids and calanoids found. An increase in Daphnia size, 'gigantism', occurred because of limitations in the mouth gape of the fry. Low densities of fing

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27

Zhikharev, Vyacheslav, Ekaterina Vodeneeva, Ivan Kudrin, et al. "The Species Structure of Plankton Communities as a Response to Changes in the Trophic Gradient of the Mouth Areas of Large Tributaries to a Lowland Reservoir." Water 15, no. 1 (2022): 74. http://dx.doi.org/10.3390/w15010074.

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The mouth areas of large rivers can serve as a good model of heterogeneity sites with a pronounced trophic gradient to assess the impact of the degree of eutrophication on different plankton communities. The aim of this research was to identify the possible response of the diversity indicators of phyto- and zooplankton communities to trophic gradients in the mouth area of two large tributaries of the reservoir, formed in the Middle Volga River (Russia). Both linear regression models and canonical correlation analysis (CCA) were used to assess the role of abiotic and biotic predictors in the st

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28

Kivi, K., S. Kaitala, H. Kuosa, et al. "Nutrient limitation and grazing control of the Baltic plankton community during annual succession." Limnology and Oceanography 38, no. 5 (1993): 893–905. http://dx.doi.org/10.4319/lo.1993.38.5.0893.

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29

Mangesh, Gauns, Kurian Siby, Shenoy M. Damodar, Naik Hema, and S. W. A. Naqvi. "Cyclone Phyan-Induced Plankton Community Succession in the Coastal Waters off Goa, India." Current Science 111, no. 6 (2016): 1091. http://dx.doi.org/10.18520/cs/v111/i6/1091-1097.

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30

BERGER, STELLA A., SEBASTIAN DIEHL, HERWIG STIBOR, GABRIELE TROMMER, and MIRIAM RUHENSTROTH. "Water temperature and stratification depth independently shift cardinal events during plankton spring succession." Global Change Biology 16, no. 7 (2010): 1954–65. http://dx.doi.org/10.1111/j.1365-2486.2009.02134.x.

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31

Paris, G., G. Rossetti, G. Giordani, C. Manzoni, and I. Ferrari. "Plankton seasonal succession in a small mountain lake (Lago Scuro Parmense, Northern Italy)." SIL Proceedings, 1922-2010 25, no. 2 (1993): 776–79. http://dx.doi.org/10.1080/03680770.1992.11900247.

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32

Roelke, Daniel, Yesim Buyukates, Mike Williams, and Jason Jean. "Interannual variability in the seasonal plankton succession of a shallow, warm-water lake." Hydrobiologia 513, no. 1 (2004): 205–18. http://dx.doi.org/10.1023/b:hydr.0000018185.41861.07.

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33

García-Oliva, Ovidio, Florian M. Hantzsche, Maarten Boersma, and Kai W. Wirtz. "Phytoplankton and particle size spectra indicate intense mixotrophic dinoflagellates grazing from summer to winter." Journal of Plankton Research 44, no. 2 (2022): 224–40. http://dx.doi.org/10.1093/plankt/fbac013.

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Abstract Mixotrophic dinoflagellates (MTD) are a diverse group of organisms often responsible for the formation of harmful algal blooms. However, the development of dinoflagellate blooms and their effects on the plankton community are still not well explored. Here we relate the species succession of MTD with parallel changes of phytoplankton size spectra during periods of MTD dominance. We used FlowCAM analysis to acquire size spectra in the range 2–200 μm every one or two weeks from July to December 2007 at Helgoland Roads (Southern North Sea). Most size spectra of dinoflagellates were bimoda

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34

Bazhenova, O. P., and N. N. Barsukova. "New and rare species of algae in the plankton of the Ob River." Проблемы ботаники южной сибири и монголии 20, no. 1 (2021): 41–44. http://dx.doi.org/10.14258/pbssm.2021008.

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According to the study of summer phytoplankton of the Ob River, 153 new species and intraspecific taxa(SIT) of algae from 8 divisions were found, including Cyanoprokaryota – 14, Dinophyta – 2, Chrysophyta – 17, Xantophyta –6, Euglenophyta – 34, Bacillariophyta – 2, Chlorophyta – 72, Charophyta – 6. New taxa are dominated by small-cell greenalgae, phytoflagellates and non-heterocyst cyanoprokaryotes. The intensive succession of the phytoplanktocenosis speciescomposition and the taxonomic structure of the new SIT algae are signs of anthropogenic eutrophication.

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35

Bruhn, Claudia Sabine, Sylke Wohlrab, Bernd Krock, Nina Lundholm, and Uwe John. "Seasonal plankton succession is in accordance with phycotoxin occurrence in Disko Bay, West Greenland." Harmful Algae 103 (March 2021): 101978. http://dx.doi.org/10.1016/j.hal.2021.101978.

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36

Naas, KE, T. van der Meeren, and DL Aksnes. "Plankton succession and responses to manipulations in a marine basin for larval fish rearing." Marine Ecology Progress Series 74 (1991): 161–73. http://dx.doi.org/10.3354/meps074161.

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37

Adrian, Rita, Norbert Walz, Thomas Hintze, Sigrid Hoeg, and Renate Rusche. "Effects of ice duration on plankton succession during spring in a shallow polymictic lake." Freshwater Biology 41, no. 3 (1999): 621–34. http://dx.doi.org/10.1046/j.1365-2427.1999.00411.x.

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38

Liukkonen, M., J. Keto, and T. Kairesalo. "Seasonal succession of diatoms in Lake Vesijärvi: comparison of sediment record with plankton counts." SIL Proceedings, 1922-2010 29, no. 5 (2006): 2309–12. http://dx.doi.org/10.1080/03680770.2006.11903105.

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39

David, Valérie, Sébastien Tortajada, Olivier Philippine, et al. "Ecological succession and resilience of plankton recovering from an acute disturbance in freshwater marshes." Science of The Total Environment 709 (March 2020): 135997. http://dx.doi.org/10.1016/j.scitotenv.2019.135997.

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40

Gorbunov, Mikhail Yu, Svetlana V. Bykova, Natalia G. Tarasova, Ekaterina S. Krasnova, and Marina V. Umanskaya. "Planktonic Pro- and Microeukaryotes of the Kuibyshev Reservoir and Its Bays During the Cyanobacterial Bloom Period." Water 17, no. 11 (2025): 1602. https://doi.org/10.3390/w17111602.

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Kuibyshev Reservoir, the largest in the Volga basin, is poorly covered by modern molecular studies. The results of a metabarcoding study of pro- and eukaryotic microbial plankton in its lower section during the summer period are presented. Bacterioplankton composition was typical for most temperate freshwater bodies and characterized by the dominance of cyanobacteria, Pseudomonadota, Bacteroidota, Actinomycetota, and PVC superphylum (Verrucomicrobiota and Planctomycetota), with a somewhat increased proportion of the latter. The protist community was dominated by Cryptista, principally phototro

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41

Flynn, Kevin J., Darren R. Clark, Aditee Mitra, et al. "Ocean acidification with (de)eutrophication will alter future phytoplankton growth and succession." Proceedings Of The Royal Society B-biological Sciences 282, no. 1804 (2015): 1–6. https://doi.org/10.1098/rspb.2014.2604.

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Human activity causes ocean acidification (OA) though the dissolution of anthropogenically generated CO<sub>2</sub> into seawater, and eutrophication through the addition of inorganic nutrients. Eutrophication increases the phytoplankton biomass that can be supported during a bloom, and the resultant uptake of dissolved inorganic carbon during photosynthesis increases water-column pH (bloom-induced basification). This increased pH can adversely affect plankton growth. With OA, basification commences at a lower pH. Using experimental analyses of the growth of three contrasting phytoplankton und

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42

Khan, M. A. "The phytoplankton periodicities of two warm-climate lakes subject to marked seasonal variability." Journal of Tropical Ecology 12, no. 4 (1996): 461–74. http://dx.doi.org/10.1017/s0266467400009706.

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ABSTRACTThe phytoplankton periodicity of a tropical upland reservoir in Nigeria (Liberty Dam, Jos Plateau) and a temperate-type lake (L. Naranbagh) from the Kashmir Himalaya were compared. Variations in the phytoplankton communities in the water-bodies were both quantitative and qualitative. Liberty Dam conformed to the oligotrophic-desmid plankton type whilst in L.Naranbagh, phytoplankton resembled the eutrophic chlorococcales-diatom plankton type. Contrary to the general belief of muted (or lack of) seasonal changes in tropical regions, phytoplankton succession in the Jos reservoir was prono

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43

Hooker, Laura J. "Using Seasonal Succession in Lake Plankton to Illustrate Concepts of Community Structure & Species Diversity." American Biology Teacher 71, no. 8 (2009): 474–81. http://dx.doi.org/10.2307/20565360.

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44

Georges, Anna A., Heba El-Swais, Susanne E. Craig, William KW Li, and David A. Walsh. "Metaproteomic analysis of a winter to spring succession in coastal northwest Atlantic Ocean microbial plankton." ISME Journal 8, no. 6 (2014): 1301–13. http://dx.doi.org/10.1038/ismej.2013.234.

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45

Yan, Qingyun, Yuhe Yu, Weisong Feng, et al. "Plankton Community Succession in Artificial Systems Subjected to Cyanobacterial Blooms Removal using Chitosan-Modified Soils." Microbial Ecology 58, no. 1 (2008): 47–55. http://dx.doi.org/10.1007/s00248-008-9434-3.

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46

Economou-Amilli, A., and T. Tafas. "Distribution patterns of Cyclotella trichonidea EC.AM. sensu lato in the plankton succession of the lakes Trichonis and Avrakia, Greece." Fundamental and Applied Limnology 147, no. 4 (2000): 559–75. http://dx.doi.org/10.1127/archiv-hydrobiol/147/2000/559.

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Bürgi, H. R., and P. Stadelmann. "Plankton succession in Lake Sempach, Lake Hallwil and Lake Baldegg before and during internal restoration measures." SIL Proceedings, 1922-2010 24, no. 2 (1991): 931–36. http://dx.doi.org/10.1080/03680770.1989.11898884.

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Havens, Karl E. "Seasonal succession in the plankton of a naturally acidic, highly humic lake in Northeastern Ohio, USA." Journal of Plankton Research 11, no. 6 (1989): 1321–27. http://dx.doi.org/10.1093/plankt/11.6.1321.

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Flynn, Kevin J., Darren R. Clark, Aditee Mitra, et al. "Ocean acidification with (de)eutrophication will alter future phytoplankton growth and succession." Proceedings of the Royal Society B: Biological Sciences 282, no. 1804 (2015): 20142604. http://dx.doi.org/10.1098/rspb.2014.2604.

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Abstract:

Human activity causes ocean acidification (OA) though the dissolution of anthropogenically generated CO 2 into seawater, and eutrophication through the addition of inorganic nutrients. Eutrophication increases the phytoplankton biomass that can be supported during a bloom, and the resultant uptake of dissolved inorganic carbon during photosynthesis increases water-column pH (bloom-induced basification). This increased pH can adversely affect plankton growth. With OA, basification commences at a lower pH. Using experimental analyses of the growth of three contrasting phytoplankton under differe

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Illyová, Marta, František Hindák, Alica Hindáková, Eva Tirjaková, and Ján Machava. "Seasonal Succession of the Plankton and Microbenthos in a Hypertrophic Shallow Water Reservoir at Modra (W Slovakia)." Journal of Environmental Protection 04, no. 11 (2013): 36–44. http://dx.doi.org/10.4236/jep.2013.411a005.

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