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  • 1
    Online Resource
    Online Resource
    Dordrecht :Springer Netherlands,
    Keywords: Microalgae -- Congresses. ; Biogeochemical cycles -- Congresses. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (327 pages)
    Edition: 1st ed.
    ISBN: 9781402062148
    DDC: 579.8
    Language: English
    Note: 978-1-4020-6214-8_Book_OnlinePDF.pdf -- BIOG_83_1-3_bookprelim1.pdf -- BIOG_83_1-3_bookprelim2.pdf -- BIOG_83_1-3_bookprelim3.pdf -- BIOG_83_1-3_bookprelim4.pdf -- biog_83_1_Prelim_v_vi.pdf -- Introduction -- A taxonomic review of the genus Phaeocystis -- Abstract -- Introduction -- Molecular analysis -- Molecular clock -- Formally described species -- Undescribed species -- Outlook -- References -- Methods used to reveal genetic diversity in the colony-forming prymnesiophytes Phaeocystis antarctica, P. globosa and P. pouchetii-preliminary results -- Abstract -- Introduction -- AmpliWed fragment length polymorphism -- Microsatellite markers -- References -- The life cycle of Phaeocystis: state of knowledge and presumptive role in ecology -- Abstract -- Introduction -- Morphotypes among Phaeocystis species -- Morphotypes of P. globosa -- Colonial cells -- Haploid Xagellates -- Diploid Xagellates -- Morphotypes of P. pouchetii -- Colonial cells -- Flagellates -- Morphotypes of P. antarctica -- Colonial cells -- Flagellates -- Morphotypes of P. jahnii -- Colonial cells -- Flagellates -- Morphotype of P. cordata -- Morphotype of P. scrobiculata -- Synthesis of the observed morphotypes -- The Phaeocystis life cycle -- The haploid-diploid life cycle of P. globosa -- Phaeocystis globosa colony blooms result from sexual processes -- Vegetative reproduction in P. globosa -- Factors inducing phase changes within the P. globosa life cycle -- The life cycle of the other Phaeocystis species -- The haploid-diploid life cycle of Prymnesiophytes -- The ecological relevance of the haploid-diploid life cycle of P. globosa -- The advantage of haploid-diploid life cycles -- The ecology of P. globosa morphotypes -- Conclusions -- References. , Phaeocystis colony distribution in the North Atlantic Ocean since 1948, and interpretation of long-term changes in the Phaeocystis hotspot in the North Sea -- Abstract -- Introduction -- Materials and methods -- The Continuous Plankton Recorder -- Rijkswaterstaat-RIKZ survey -- Data presentation -- Results -- Discussion -- References -- Photosynthetic responses in Phaeocystis antarctica towards varying light and iron conditions -- Abstract -- Introduction -- Methods -- Culture conditions -- Photosynthetic parameters -- Sampling strategy and statistical analyses -- Results -- Discussion -- Acknowledgements -- References -- Effects of iron concentration on pigment composition in Phaeocystis antarctica grown at low irradiance -- Abstract -- Introduction -- Methods and materials -- Isolation of Phaeocystis antarctica -- Laboratory iron-addition dose-response experiment -- Ross Sea pigment samples -- HPLC pigment analyses -- Results and discussion -- Hex:Chl a ratios -- Fuco:Chl a ratios -- Chl c3:Chl a ratios -- Hex:Chl c3 ratios -- Fuco:Hex ratios -- Physiological and ecological implications -- Acknowledgements -- References -- Evidence for high iron requirements of colonial Phaeocystis antarctica at low irradiance -- Abstract -- Introduction -- Methods -- Field collections -- Shipboard iron-light manipulation experiment -- Laboratory dose-response iron-addition experiment -- Analytical methods -- Interpretation of experimental results -- Results and discussion -- Shipboard iron-light manipulation experiment -- Laboratory dose-response iron-addition experiment -- Conclusions and directions for future research -- Acknowledgements -- References -- The carbohydrates of Phaeocystis and their degradation in the microbial food web -- Abstract -- Introduction -- Phaeocystis carbohydrates and their characteristics -- Structural polysaccharides. , Mono- and oligosaccharides -- Storage glucan -- Mucopolysaccharides -- Contribution of mucopolysaccharides-C to POC -- Extra-colonial DOM -- Mechanisms of DOM release during a Phaeocystis bloom -- Formation of hydrogels by Phaeocystis carbohydrates -- Microbial degradation -- Microbial degradation of Phaeocystis carbohydrates -- Microbial degradation of hydrogels -- Conclusions -- Acknowledgements -- References -- The role of iron in the bacterial degradation of organic matter derived from Phaeocystis antarctica -- Abstract -- Introduction -- Materials and methods -- Experimental procedure -- Phaeocystis cultures -- Bacteria cultures -- Regrowth experiments -- Analytical procedures -- Nutrients -- Chlorophyll a and Phaeocystis antarctica biomass -- Organic carbon -- Bacterial biomass and activities -- Statistical analysis -- Results -- Characteristics of LFe and HFe Phaeocystis cultures -- Bacterial regrowth experiments -- Time evolution of organic carbon -- Bacterial communities -- Bacterial activities -- Discussion -- Fe control on P. antarctica-derived organic matter concentration and quality -- Fe control on the bacterial community composition and activities -- Fe control on organic matter remineralization in a Phaeocystis-dominated ecosystem -- Conclusion -- Acknowledgments -- References -- The colonization of two Phaeocystis species (Prymnesiophyceae) by pennate diatoms and other protists: a signiWcant contribution to colony biomass -- Abstract -- Introduction -- Material and methods -- Results -- Discussion -- References -- Zooplankton grazing on Phaeocystis: a quantitative review and future challenges -- Abstract -- Introduction -- Grazing on Phaeocystis: quantitative patterns in published data -- Crustacean zooplankton grazing on Phaeocystis: is there a general pattern? -- Treatment of literature data -- Statistical methods. , Results from statistical analysis -- Quantitative results from data on crustacean grazing -- Grazing by protozooplankton and other microzooplankton -- Cell-type and life-stage-speciWc interactions with grazers -- Colony formation and its potential role in morphological defense -- Chemical defense -- Does DMS aVect grazing on Phaeocystis? -- Does nutritional value aVect grazing on Phaeocystis? -- Survival of gut passage? -- Conclusions and future challenges -- References -- The influence of Phaeocystis globosa on microscale spatial patterns of chlorophyll a and bulk-phase seawater viscosity -- Abstract -- Introduction -- Materials and methods -- Study site -- Microscale sampling device -- Chlorophyll a analysis -- Bulk-phase seawater viscosity measurements -- Potential biases and limitations -- Data analyses -- Identifying spatial structure -- Statistical analyses -- Results -- Environmental conditions -- Microscale spatial variability -- Microscale spatial correlation -- Microscale spatial structure -- Discussion -- Microscale spatial patterns and Phaeocystis globosa bloom dynamics -- Type of spatial patterns and patch sizes -- Small-scale versus microscale variability -- On the potential role of biologically increased seawater viscosity in P. globosa ecology -- Conclusions -- Acknowledgements -- References -- Haemolytic activity of live Phaeocystis pouchetii during mesocosm blooms -- Abstract -- Introduction -- Material and methods -- Mesocosm set up -- Sampling -- Phytoplankton analysis -- Erythrocyte lysis analysis (ELA) -- Data analysis -- Results -- Bloom description -- Haemolytic activity -- Correlation of haemolysis with phytoplankton groups -- Dose response curves at diVerent temperatures -- Light eVects -- Discussion -- References -- Phaeocystis and its interaction with viruses -- Abstract -- Introduction. , Isolation and characterization of viruses infecting Phaeocystis -- Occurrence and dynamics of Phaeocystis viruses -- Diversity of Phaeocystis viruses and its ecological role -- Resistance to viral infection -- Environmental factors inXuencing virus-host interactions -- Virally induced mortality of Phaeocystis -- Impact of viral lysis of Phaeocystis on the microbial food web and element cycling -- Future perspectives -- References -- Does Phaeocystis spp. contribute significantly to vertical export of organic carbon? -- Abstract -- Introduction -- Methods -- Sampling sites and sediment trap measurements -- Analysis and calculations -- Results and discussion -- How to define vertical export of Phaeocystis-derived matter? -- The morphological challenge: cells and colonies -- The relative importance of Phaeocystis spp. cell carbon to vertical POC export -- Does mucus contribute significantly to the vertical export of Phaeocystis spp-derived C? -- Mucus carbon estimates -- Estimated mucus contribution to carbon export -- Fate of Phaeocystis colonies visualised through TEP -- Mechanisms for vertical export -- Concluding remarks -- Acknowledgement -- References -- Vernal sedimentation trends in north Norwegian fjords: temporary anomaly in 234Th particulate fluxes related to Phaeocystis pouchetii proliferation -- Abstract -- Introduction -- Material and methods -- Study area -- Measurements -- Irreversible scavenging model of 234Th -- Results -- Hydrography, Phaeocystis and DMSP distribution in the three fjords -- Vertical distribution of 234Th -- Particulate fluxes of 234Th -- Discussion -- 234Th fluxes and trap collection efficiencies -- Impact of Phaeocystis proliferation on settling flux -- Conclusions -- Acknowledgments -- References. , Environmental constraints on the production and removal of the climatically active gas dimethylsulphide (DMS) and implications for ecosystem modelling.
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  • 2
    Type of Medium: Book
    Pages: 100 S , graph. Darst., Kt.
    Series Statement: NIOZ Rapport 1988,4
    Language: English
    Note: Literaturverz
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  • 3
    Publication Date: 2011-01-29
    Description: The potentially significant role of the biogenic trace gas dimethylsulfide (DMS) in determining the Earth's radiation budget makes it necessary to accurately reproduce seawater DMS distribution and quantify its global flux across the sea/air interface. Following a threefold increase of data (from 15,000 to over 47,000) in the global surface ocean DMS database over the last decade, new global monthly climatologies of surface ocean DMS concentration and sea-to-air emission flux are presented as updates of those constructed 10 years ago. Interpolation/extrapolation techniques were applied to project the discrete concentration data onto a first guess field based on Longhurst's biogeographic provinces. Further objective analysis allowed us to obtain the final monthly maps. The new climatology projects DMS concentrations typically in the range of 1–7 nM, with higher levels occurring in the high latitudes, and with a general trend toward increasing concentration in summer. The increased size and distribution of the observations in the DMS database have produced in the new climatology substantially lower DMS concentrations in the polar latitudes and generally higher DMS concentrations in regions that were severely undersampled 10 years ago, such as the southern Indian Ocean. Using the new DMS concentration climatology in conjunction with state-of-the-art parameterizations for the sea/air gas transfer velocity and climatological wind fields, we estimate that 28.1 (17.6–34.4) Tg of sulfur are transferred from the oceans into the atmosphere annually in the form of DMS. This represents a global emission increase of 17% with respect to the equivalent calculation using the previous climatology. This new DMS climatology represents a valuable tool for atmospheric chemistry, climate, and Earth System models.
    Print ISSN: 0886-6236
    Electronic ISSN: 1944-9224
    Topics: Biology , Chemistry and Pharmacology , Geography , Geosciences , Physics
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  • 4
    Publication Date: 2018-03-06
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 5
    Publication Date: 2017-11-13
    Description: Antarctic pack ice is inhabited by a diverse and active microbial community reliant on nutrients for growth. Seeking patterns and overlooked processes, we performed a large-scale compilation of macro-nutrient data (hereafter termed nutrients) in Antarctic pack ice (306 ice-cores collected from 19 research cruises). Dissolved inorganic nitrogen and silicic acid concentrations change with time, as expected from a seasonally productive ecosystem. In winter, salinity-normalized nitrate and silicic acid concentrations (C*) in sea ice are close to seawater concentrations (Cw), indicating little or no biological activity. In spring, nitrate and silicic acid concentrations become partially depleted with respect to seawater (C* 〈 Cw), commensurate with the seasonal build-up of ice microalgae promoted by increased insolation. Stronger and earlier nitrate than silicic acid consumption suggests that a significant fraction of the primary productivity in sea ice is sustained by flagellates. By both consuming and producing ammonium and nitrite, the microbial community maintains these nutrients at relatively low concentrations in spring. With the decrease in insolation beginning in late summer, dissolved inorganic nitrogen and silicic acid concentrations increase, indicating imbalance between their production (increasing or unchanged) and consumption (decreasing) in sea ice. Unlike the depleted concentrations of both nitrate and silicic acid from spring to summer, phosphate accumulates in sea ice (C* 〉 Cw). The phosphate excess could be explained by a greater allocation to phosphorus-rich biomolecules during ice algal blooms coupled with convective loss of excess dissolved nitrogen, preferential remineralization of phosphorus, and/or phosphate adsorption onto metal-organic complexes. Ammonium also appears to be efficiently adsorbed onto organic matter, with likely consequences to nitrogen mobility and availability. This dataset supports the view that the sea ice microbial community is highly efficient at processing nutrients but with a dynamic quite different from that in oceanic surface waters calling for focused future investigations.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , peerRev
    Format: application/pdf
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  • 6
    Publication Date: 2018-09-12
    Repository Name: EPIC Alfred Wegener Institut
    Type: Miscellaneous , notRev
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  • 7
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 8
    Publication Date: 2020-03-27
    Description: Historical sea ice core chlorophyll-a (Chla) data are used to describe the seasonal, regional, and vertical distribution of ice algal biomass in Antarctic landfast sea ice. The analyses are based on the Antarctic Fast Ice Algae Chlorophyll-a data set, a compilation of currently available sea ice Chla data from landfast sea ice cores collected at circum-Antarctic nearshore locations between 1970 and 2015. Ice cores were typically sampled from thermodynamically grown first-year ice and have thin snow depths (mean=0.0520.097m). The data set comprises 888 ice cores, including 404 full vertical profile cores. Integrated ice algal Chla biomass (range: 〈0.1-219.9mg/m(2), median=4.4mg/m(2), interquartile range=9.9mg/m(2)) peaks in late spring and shows elevated levels in autumn. The seasonal Chla development is consistent with the current understanding of physical drivers of ice algal biomass, including the seasonal cycle of irradiance and surface temperatures driving landfast sea ice growth and melt. Landfast ice regions with reported platelet ice formation show maximum ice algal biomass. Ice algal communities in the lowermost third of the ice cores dominate integrated Chla concentrations during most of the year, but internal and surface communities are important, particularly in winter. Through comparison of biomass estimates based on different sea ice sampling strategies, that is, analysis of full cores versus bottom-ice section sampling, we identify biases in common sampling approaches and provide recommendations for future survey programs: for example, the need to sample fast ice over its entire thickness and to measure auxiliary physicochemical parameters. Plain Language Summary Antarctic sea ice is a key driver of physical, chemical, and biological processes in the Southern Ocean. Importantly, sea ice serves as a substrate for microscopic algae which grow in the bottom, interior, and surface layers of the ice. These algae are considered an important food source for Antarctic marine food webs. Using a newly collated database of historical sea ice core chlorophyll-a data (a proxy for ice algal biomass) from coastal sites, we describe the seasonal and vertical variability of algal biomass in Antarctic landfast sea ice. The seasonal chlorophyll-a development is consistent with the current understanding of physical drivers of ice algal biomass, including the seasonal cycle of irradiance and surface temperatures driving landfast sea ice growth and melt. Our analyses show that algae in the lowermost third of ice cores drive the annual cycle of integrated biomass, but internal and surface communities are also important. Through comparison of biomass estimates based on different sea ice sampling strategies, that is, analysis of full cores versus bottom-ice section sampling, we identify biases in common sampling approaches and provide recommendations for future survey programs: for example, the need to sample fast ice over its entire thickness and to measure auxiliary physical parameters, in particular snow-thickness data.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 9
    Publication Date: 2019-04-26
    Description: The west Antarctic Peninsula (WAP) region has undergone significant changes in temperature and seasonal ice dynamics since the mid-twentieth century, with strong impacts on the regional ecosystem, ocean chemistry and hydrographic properties. Changes to these long-term trends of warming and sea ice decline have been observed in the 21st century, but their consequences for ocean physics, chemistry and the ecology of the high-productivity shelf ecosystem are yet to be fully established. The WAP shelf is important for regional krill stocks and higher trophic levels, whilst the degree of variability and change in the physical environment and documented biological and biogeochemical responses make this a model system for how climate and sea ice changes might restructure high-latitude ecosystems. Although this region is arguably the best-measured and best-understood shelf region around Antarctica, significant gaps remain in spatial and temporal data capable of resolving the atmosphere-ice-ocean-ecosystem feedbacks that control the dynamics and evolution of this complex polar system. Here we summarise the current state of knowledge regarding the key mechanisms and interactions regulating the physical, biogeochemical and biological processes at work, the ways in which the shelf environment is changing, and the ecosystem response to the changes underway. We outline the overarching cross-disciplinary priorities for future research, as well as the most important discipline-specific objectives. Underpinning these priorities and objectives is the need to better-define the causes, magnitude and timescales of variability and change at all levels of the system. A combination of traditional and innovative approaches will be critical to addressing these priorities and developing a co-ordinated observing system for the WAP shelf, which is required to detect and elucidate change into the future.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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  • 10
    Publication Date: 2022-06-26
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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