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  • 1
    In: Journal of plankton research, Oxford : Oxford Univ. Press, 1979, 30(2008), 12, Seite 1329-1342, 1464-3774
    In: volume:30
    In: year:2008
    In: number:12
    In: pages:1329-1342
    Beschreibung / Inhaltsverzeichnis: Zooplankton trade-offs to maximize fitness in highly dynamic environments such as estuaries have long been a question of central importance for understanding the ecology and evolution of estuarine populations. We present here the first comprehensive data set on the population dynamics of the copepod Eurytemmora affinis obtained from 50 h high-frequency sampling in the Seine estuary during spring. Maximum densities of E. affinis were associated with low salinities (0.5-10) and recorded during the ebb in the bottom layer. Vertical variations in population structure were observed between ebb and flood, as well as the spatial distribution of developmental stages. Nauplii were concentrated in the low salinity zone just above salinity 5, and copepodids and adults distributed more widely relative to salinity than nauplii in bottom waters, whereas the opposite pattern was observed in surface waters. The sex-ratio and the proportion "ovigerous females:non-ovigerous females" appeared to be related to tidal cycle and depth, with higher relative densities of non-ovigerous females in bottom waters and around low tide. The vertical variations noticed during the tidal cycle suggest a strategy by the species to avoid flushing by surface currents, although it may incur a cost due to the greater presence of predators in bottom waters.
    Materialart: Online-Ressource
    Seiten: graph. Darst
    ISSN: 1464-3774
    Sprache: Englisch
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    In: Limnology and oceanography, Oxford [u.a.] : Wiley-Blackwell, 1956, 53(2008), 4, Seite 1456-1467, 1939-5590
    In: volume:53
    In: year:2008
    In: number:4
    In: pages:1456-1467
    Beschreibung / Inhaltsverzeichnis: We investigated potential connections between climate and the population size of gelatinous carnivores in the northwestern Mediterranean. The interannual variability of large- and meso-scale climate factors was related to gelatinous carnivore dynamics by means of a multivariate regression model. Gelatinous carnivore population dynamics integrate the climate-related changes in the northwestern Mediterranean with close correlations between climate and the population size of the Calycophoran siphonophores Chelophyes appendiculata and Abylopsis tetragona and the Hydromedusae Rhopalonema velatum and Solmundella bitentaculata. We show that the sensitivity of particular gelatinous carnivore species to environmental forcing relates to their seasonal appearance and peak of abundance. Our results advocate the occurrence of short time windows, during which gelatinous carnivores appear more sensitive to environmental conditions, and favorable conditions may therefore substantially enhance their annual peaks. Furthermore, there were threshold values from which climate effects on gelatinous carnivores become noticeable, indicating that the climategelatinous carnivore relationship intensifies according to the strength of climate forcing. The possibility of using the North Atlantic climate variability for assessing and predicting interannual abundance changes of these organisms in the northwestern Mediterranean is considered.
    Materialart: Online-Ressource
    Seiten: graph. Darst.
    ISSN: 1939-5590
    Sprache: Englisch
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    In: Global Ocean Ecosystem Dynamics, GLOBEC international newsletter, Plymouth : GLOBEC International Project Office, 1993, 14(2008), 2, Seite 7-9
    In: volume:14
    In: year:2008
    In: number:2
    In: pages:7-9
    Materialart: Online-Ressource
    Seiten: graph. Darst
    Sprache: Englisch
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Schlagwort(e): Hochschulschrift
    Materialart: Online-Ressource
    Seiten: 1 Online-Ressource (144 Blatt = 4 MB) , Illustrationen, Diagramme
    Sprache: Englisch
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
    In: Journal of plankton research, Oxford : Oxford Univ. Press, 1979, 32(2010), 1, Seite 97-98, 1464-3774
    In: volume:32
    In: year:2010
    In: number:1
    In: pages:97-98
    Materialart: Online-Ressource
    ISSN: 1464-3774
    Sprache: Englisch
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 6
    In: Royal Society (London), Proceedings of the Royal Society of London. Series B, Biological sciences, London : The Royal Society, 1905, (2008), 1471-2954
    In: year:2008
    In: extent:9
    Materialart: Online-Ressource
    Seiten: 9 , graph. Darst
    ISSN: 1471-2954
    Sprache: Englisch
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 7
    In: Biological invasions, Dordrecht [u.a.] : Kluwer, 1999, (2008), 1387-3547
    In: year:2008
    In: extent:10
    Materialart: Online-Ressource
    Seiten: 10
    ISSN: 1387-3547
    Sprache: Englisch
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 8
    In: Hydrobiologia, Dordrecht [u.a.] : Springer Science + Business Media B.V, 1948, (2008), 1573-5117
    In: year:2008
    In: extent:14
    Beschreibung / Inhaltsverzeichnis: Spatial and temporal changes of the copepod community have been investigated and related to the environmental variability of the Balearic Sea (Western Mediterranean). The period studied spans from 1994 to 1999 during which we analyzed the abundance and structure copepod variability over a cross-shore transect. Results showed a close link between hydrological changes and the variations of copepod abundance. The synchronous variability of copepods and hydrography indicated the rapid response of this zooplankton group to the inflow of cold and warm water masses coming through the study area. Cluster analysis revealed four main copepod assemblages that distinguished the coastal from the oceanic species and those species with different water masses preference. The copepod assemblage composed of Calanus helgolandicus, Clausocalanus arcuicornis, C. pergens, C. paululus, Calocalanus tenuis and Pleuromamma gracilis was associated with cool salty waters, whereas the assemblage formed by Temora stylifera, C. pavo, C. styliremis, Centropages bradyi and Acartia danae was related to warmer less saline Mediterranean waters. Moreover, it is suggested that changes in sea water temperature and salinity are linked to large-scale changes likely occurring at a basin scale, which is reflected in the Western Mediterranean mesoscale hydrographic changes. Therefore, it is stressed that changes in the Balearic copepod community can be used as potential tracers of the western Mediterranean water masses.
    Materialart: Online-Ressource
    Seiten: 14 , graph. Darst
    ISSN: 1573-5117
    Sprache: Englisch
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 9
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Lebrato, Mario; Molinero, Juan-Carlos; Cartes, Joan E; Lloris, Domingo; Melin, Frederic; Beni-Casadella, Laia (2013): Sinking Jelly-Carbon Unveils Potential Environmental Variability along a Continental Margin. PLoS ONE, 8(12), e82070, https://doi.org/10.1371/journal.pone.0082070
    Publikationsdatum: 2023-10-28
    Beschreibung: Particulate matter export fuels benthic ecosystems in continental margins and the deep sea, removing carbon from the upper ocean. Gelatinous zooplankton biomass provides a fast carbon vector that has been poorly studied. Observational data of a large-scale benthic trawling survey from 1994 to 2005 provided a unique opportunity to quantify jelly-carbon along an entire continental margin in the Mediterranean Sea and to assess potential links with biological and physical variables. Biomass depositions were sampled in shelves, slopes and canyons with peaks above 1000 carcasses per trawl, translating to standing stock values between 0.3 and 1.4 mg C m2 after trawling and integrating between 30,000 and 175,000 m2 of seabed. The benthopelagic jelly-carbon spatial distribution from the shelf to the canyons may be explained by atmospheric forcing related with NAO events and dense shelf water cascading, which are both known from the open Mediterranean. Over the decadal scale, we show that the jelly-carbon depositions temporal variability paralleled hydroclimate modifications, and that the enhanced jelly-carbon deposits are connected to a temperature-driven system where chlorophyll plays a minor role. Our results highlight the importance of gelatinous groups as indicators of large-scale ecosystem change, where jelly-carbon depositions play an important role in carbon and energy transport to benthic systems.
    Schlagwort(e): Abundance; Abundance per area; Area; Area/locality; Biomass; Biomass as carbon per area; Biomass as nitrogen per area; Bottom trawl; BT; Carbon, organic, particulate; Climate - Biogeochemistry Interactions in the Tropical Ocean; Cornide_1994_81; Cornide_1994_82; Cornide_1995_2; Cornide_1995_30; Cornide_1995_36; Cornide_1995_38; Cornide_1995_39; Cornide_1995_48; Cornide_1995_50; Cornide_1995_51; Cornide_1995_53; Cornide_1995_54; Cornide_1995_55; Cornide_1995_70; Cornide_1995_71; Cornide_1996_105; Cornide_1996_106; Cornide_1996_12; Cornide_1996_18; Cornide_1996_20; Cornide_1996_24; Cornide_1996_31; Cornide_1996_32; Cornide_1996_33; Cornide_1996_34; Cornide_1996_35; Cornide_1996_36; Cornide_1996_37; Cornide_1996_38; Cornide_1996_39; Cornide_1996_41; Cornide_1996_42; Cornide_1996_43; Cornide_1996_50; Cornide_1996_52; Cornide_1996_53; Cornide_1996_54; Cornide_1996_55; Cornide_1996_56; Cornide_1996_57; Cornide_1996_58; Cornide_1996_59; Cornide_1996_60; Cornide_1996_62; Cornide_1996_63; Cornide_1996_64; Cornide_1996_67; Cornide_1996_73; Cornide_1996_74; Cornide_1996_75; Cornide_1996_76; Cornide_1996_78; Cornide_1996_79; Cornide_1996_80; Cornide_1996_83; Cornide_1997_102; Cornide_1997_53; Cornide_1997_54; Cornide_1997_56; Cornide_1997_68; Cornide_1997_73; Cornide_1997_74; Cornide_1997_75; Cornide_1997_78; Cornide_1997_81; Cornide_1998_11; Cornide_1998_12; Cornide_1998_14; Cornide_1998_19; Cornide_1998_48; Cornide_1998_6; Cornide_1999_32; Cornide_1999_47; Cornide_1999_56; Cornide_1999_81; Cornide_2000_10; Cornide_2000_19; Cornide_2000_36; Cornide_2000_6; Cornide_2000_84; Cornide_2000_91; Cornide_2001_106; Cornide_2001_107; Cornide_2001_108; Cornide_2001_11; Cornide_2001_18; Cornide_2001_30; Cornide_2001_32; Cornide_2001_41; Cornide_2001_42; Cornide_2001_43; Cornide_2001_44; Cornide_2001_5; Cornide_2001_51; Cornide_2001_55; Cornide_2001_63; Cornide_2001_64; Cornide_2001_69; Cornide_2001_71; Cornide_2001_85; Cornide_2001_86; Cornide_2002_10; Cornide_2002_100; Cornide_2002_103; Cornide_2002_104; Cornide_2002_105; Cornide_2002_106; Cornide_2002_108; Cornide_2002_110; Cornide_2002_111; Cornide_2002_114; Cornide_2002_115; Cornide_2002_116; Cornide_2002_117; Cornide_2002_118; Cornide_2002_119; Cornide_2002_120; Cornide_2002_21; Cornide_2002_22; Cornide_2002_23; Cornide_2002_24; Cornide_2002_34; Cornide_2002_50; Cornide_2002_58; Cornide_2002_62; Cornide_2002_63; Cornide_2002_72; Cornide_2002_73; Cornide_2002_75; Cornide_2002_78; Cornide_2002_98; Cornide_2003_10; Cornide_2003_100; Cornide_2003_101; Cornide_2003_104; Cornide_2003_105; Cornide_2003_106; Cornide_2003_107; Cornide_2003_108; Cornide_2003_109; Cornide_2003_11; Cornide_2003_111; Cornide_2003_114; Cornide_2003_115; Cornide_2003_12; Cornide_2003_13; Cornide_2003_15; Cornide_2003_18; Cornide_2003_23; Cornide_2003_24; Cornide_2003_26; Cornide_2003_27; Cornide_2003_28; Cornide_2003_4; Cornide_2003_44; Cornide_2003_45; Cornide_2003_46; Cornide_2003_47; Cornide_2003_48; Cornide_2003_49; Cornide_2003_50; Cornide_2003_51; Cornide_2003_52; Cornide_2003_53; Cornide_2003_54; Cornide_2003_55; Cornide_2003_56; Cornide_2003_57; Cornide_2003_58; Cornide_2003_6; Cornide_2003_68; Cornide_2003_69; Cornide_2003_70; Cornide_2003_71; Cornide_2003_72; Cornide_2003_73; Cornide_2003_74; Cornide_2003_75; Cornide_2003_76; Cornide_2003_77; Cornide_2003_78; Cornide_2003_79; Cornide_2003_8; Cornide_2003_80; Cornide_2003_81; Cornide_2003_82; Cornide_2003_83; Cornide_2003_84; Cornide_2003_86; Cornide_2003_87; Cornide_2003_89; Cornide_2003_90; Cornide_2003_91; Cornide_2003_92; Cornide_2003_93; Cornide_2003_94; Cornide_2003_95; Cornide_2003_96; Cornide_2003_97; Cornide_2004_100; Cornide_2004_107; Cornide_2004_108; Cornide_2004_122; Cornide_2004_15; Cornide_2004_23; Cornide_2004_27; Cornide_2004_28; Cornide_2004_29; Cornide_2004_30; Cornide_2004_32; Cornide_2004_33; Cornide_2004_34; Cornide_2004_37; Cornide_2004_38; Cornide_2004_39; Cornide_2004_40; Cornide_2004_43; Cornide_2004_44; Cornide_2004_47; Cornide_2004_48; Cornide_2004_49; Cornide_2004_51; Cornide_2004_52; Cornide_2004_53; Cornide_2004_54; Cornide_2004_55; Cornide_2004_56; Cornide_2004_57; Cornide_2004_58; Cornide_2004_60; Cornide_2004_61; Cornide_2004_67; Cornide_2004_68; Cornide_2004_70; Cornide_2004_75; Cornide_2004_76; Cornide_2004_84; Cornide_2004_85; Cornide_2004_86; Cornide_2004_89; Cornide_2004_90; Cornide_2005_36; Cornide_2005_54; Cornide_2005_67; Cornide_2005_68; Cornide_2005_74; Cornide_2005_89; Dry mass; Event label; Height; Length; Nitrogen, organic, particulate; Sector; SFB754; Speed; Volume; Wet mass
    Materialart: Dataset
    Format: text/tab-separated-values, 4446 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 10
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Courtney, Travis A; Lebrato, Mario; Bates, Nicolas R; Collins, Andrew; de Putron, Samantha J; Garley, Rebecca; Johnson, Rod; Molinero, Juan-Carlos; Noyes, Timothy J; Sabine, Christopher L; Andersson, Andreas J (2017): Environmental controls on modern scleractinian coral and reef-scale calcification. Science Advances, 3(11), e1701356, https://doi.org/10.1126/sciadv.1701356
    Publikationsdatum: 2024-03-15
    Beschreibung: Modern reef-building corals sustain a wide range of ecosystem services because of their ability to build calcium carbonate reef systems. The influence of environmental variables on coral calcification rates has been extensively studied, but our understanding of their relative importance is limited by the absence of in situ observations and the ability to decouple the interactions between different properties. We show that temperature is the primary driver of coral colony (Porites astreoides and Diploria labyrinthiformis) and reef-scale calcification rates over a 2-year monitoring period from the Bermuda coral reef. On the basis of multimodel climate simulations (Coupled Model Intercomparison Project Phase 5) and assuming sufficient coral nutrition, our results suggest that P. astreoides and D. labyrinthiformis coral calcification rates in Bermuda could increase throughout the 21st century as a result of gradual warming predicted under a minimum CO2 emissions pathway [representative concentration pathway (RCP) 2.6] with positive 21st-century calcification rates potentially maintained under a reduced CO2 emissions pathway (RCP 4.5). These results highlight the potential benefits of rapid reductions in global anthropogenic CO2 emissions for 21st-century Bermuda coral reefs and the ecosystem services they provide.
    Schlagwort(e): Alkalinity, total; Animalia; Aragonite saturation state; Benthic animals; Benthos; Bicarbonate ion; Brightness; Calcification/Dissolution; Calcification rate; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Chlorophyll a; Cnidaria; Coast and continental shelf; Crescent_Reef; Date; Diploria labyrinthiformis; Entire community; Event label; EXP; Experiment; Field observation; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Hog_Reef; LATITUDE; LONGITUDE; Month; North Atlantic; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Porites astreoides; Rocky-shore community; Salinity; Score on PC1; Single species; Temperate; Temperature, water; Type; Years
    Materialart: Dataset
    Format: text/tab-separated-values, 2280 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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