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  • 1
    Online Resource
    Online Resource
    Newark :John Wiley & Sons, Incorporated,
    Keywords: Biogeochemical cycles. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (150 pages)
    Edition: 1st ed.
    ISBN: 9781119136897
    DDC: 577/.14
    Language: English
    Note: Cover -- Title Page -- Copyright -- Contents -- Preface -- 1: The Chemical Forms of Silicon in the Marine Domain -- 1.1. The element "silicon" -- 1.2. Orthosilicic acid -- 1.3. Particulate silicas -- 1.3.1. Lithogenic silica -- 1.3.2. Biogenic silica -- 2: Techniques for Studying Stocks and Fluxes -- 2.1. Techniques for the chemical analysis of silicon -- 2.1.1. The sequential digestion method -- 2.1.2. The extraction kinetics method -- 2.1.3. The correction by aluminum method -- 2.2. Techniques for the analysis of silicon fluxes -- 2.2.1. Labeling with radioactive isotopes -- 2.2.2. Labeling with stable isotopes -- 2.3. Silica deposit labeling and cellular imaging -- 2.4. Isotopic fractionation of silicon and utilization of δ30 Si as a tracer in oceanography -- 2.4.1. Demonstration of the isotopic fractionation by the diatoms -- 2.4.2. Utilization of δ30 Si as a tracer in oceanography -- 2.4.3. The interest of analyses of the isotopic ratio of silicon -- 3: The Marine Producers of Biogenic Silica -- 3.1. Radiolarians -- 3.2. Silicoflagellates -- 3.3. Diatoms -- 3.4. Silicification within the scope of nanoplankton and picoplankton -- 3.5. Siliceous sponges -- 3.6. The functions of biogenic silica -- 3.7. The evolution of the siliceous organisms and the oceanic cycle of the silicon -- 3.8. Sedimentary opal deposits -- 4: Cellular Mechanisms of Silica Deposition by Diatoms -- 4.1. Influence of orthosilicic acid availability on uptake and diatom growth -- 4.1.1. General formulations and kinetics information -- 4.2. The chemical form of dissolved Si available for diatoms -- 4.2.1. The model of Riedel and Nelson [RIE 85] -- 4.2.2. The model of Del Amo and Brzezinski -- 4.2.3. The membrane transporters -- 4.3. Cellular mechanisms of orthosilicic acid uptake -- 4.4. Intervention of specific proteins in the deposition mechanism. , 4.4.1. The Hecky et al. conceptual model -- 4.4.2. Frustulins and silaffins -- 4.4.3. Frustule synthesis, a complex physiological process -- 4.5. The stoichiometric ratios Si/C/N of diatoms -- 4.5.1. Stoichiometry in diatoms and limitation by iron -- 4.5.2. The influence of trace metals on the uptake of orthosilicic acid -- 5: Dissolution of Biogenic Silica and Orthosilicic Acid Regeneration -- 5.1. Reactivity of the particulate silica and dissolution constants -- 5.2. Processes of control of the dissolution in aqueous phase -- 5.2.1. Variation of the solubility of opal with depth -- 5.2.2. Influence of pH -- 5.2.3. Role of temperature -- 5.2.4. Relationship with bacterial degradation process -- 5.2.5. Influence of aluminum concentration -- 5.3. The solubility of opal in natural conditions -- 6: The Control of Biogeochemistry by Silicon at Global Scale -- 6.1. The preservation of calcite in ocean sediments -- 6.1.1. Control of alkalinity by organic production -- 6.1.2. The CaCO3/Corg ratio (rain ratio) -- 6.1.3. The distribution of orthosilicic acid in the Global Ocean -- 6.2. The central role of the Southern Ocean -- 6.2.1. Subantarctic Mode Water (SAMW) -- 6.2.2. Si* tracer -- 6.2.3. The influence of SAMW in the Global Ocean -- 6.2.4. The conceptual model of Sarmiento et al. -- 6.3. The silicic acid leakage hypothesis (SALH) -- 6.3.1. The last glacial-interglacial transition -- 6.3.2. The sedimentary record -- 7: The Global Budget of Silicon in the Oceans -- 7.1. Estimates of production and export of biogenic silica -- 7.1.1. Estimation of the upper limit -- 7.1.2. Estimation of the lower limit -- 7.1.3. General overview of production and export -- 7.2. The biogeochemical cycle of silicon in the Global Ocean -- Bibliography -- Index -- Other titles from ISTE in Earth Systems - Environmental Engineering -- EULA.
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  • 2
    Online Resource
    Online Resource
    London :ISTE Editions Ltd.,
    Keywords: Electronic books.
    Description / Table of Contents: Dans la dynamique biogéochimique des écosystèmes marins, le silicium est un élément majeur dont le rôle a longtemps été sousestimé. Il est pourtant indispensable à l'activité de plusieurs organismes biominéralisateurs marins, dont certains jouent un rôle essentiel dans la pompe biologique du carbone océanique. Cet ouvrage apporte les notions indispensables à la connaissance du cycle biogéochimique du silicium dans les systèmes océaniques en décrivant tout d'abord les principales techniques d'analyse quantitative et l'examen des organismes majeurs impliqués dans ce cycle. Il étudie ensuite les processus les plus courants pour contrôler l'utilisation du silicium et sa régénération dans les conditions naturelles, avant d'évoquer le rôle central joué par cet élément original dans la maîtrise de l'ensemble des cycles biogéochimiques de l'Océan mondial. Les informations disponibles permettent finalement de quantifier le bilan biogéochimique global du silicium dans le domaine marin.
    Type of Medium: Online Resource
    Pages: 1 online resource (146 pages)
    Edition: 1st ed.
    ISBN: 9781784061449
    DDC: 577.714
    Language: French
    Note: Cover -- Table des matières -- Avant-propos -- Chapitre 1. Les formes chimiques du silicium dans le domaine marin -- Chapitre 2. Les techniques d'étude des stocks et des flux -- Chapitre 3. Les producteurs marins de silice biogène -- Chapitre 4. Mécanismes cellulaires du dépôt de silice chez les diatomées -- Chapitre 5. Dissolution de la silice biogène et régénération de l'acide orthosilicique -- Chapitre 6. Le silicium et le contrôle de la biogéochimie à l'échelle globale -- Chapitre 7. Le bilan global du silicium dans les océans -- Bibliographie -- Index.
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  • 3
    Type of Medium: Book
    Pages: S. 559 - 912 , Ill.,graph. Darst., Kt
    Series Statement: Deep sea research 55.2008,5/7
    Language: English
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  • 4
    Online Resource
    Online Resource
    London, UK : ISTE, Ltd
    Keywords: Silicon Environmental aspects ; Ocean Environmental aspects ; Biogeochemical cycles
    Description / Table of Contents: The Chemical Forms of Silicon in the Marine Domain -- Techniques for Studying Stocks and Fluxes -- The Marine Producers of Biogenic Silica -- Cellular Mechanisms of Silica Deposition by Diatoms -- Dissolution of Biogenic Silica and Orthosilicic Acid Regeneration -- The Control of Biogeochemistry by Silicon at Global Scale -- The Global Budget of Silicon in the Oceans
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource
    Edition: Online-Ausg.]
    Series Statement: Focus series
    Language: English
    Note: Includes bibliographical references and index , Owing to Legal Deposit regulations this resource may only be accessed from within National Library of Scotland. For more information contact enquiriesnls.uk StEdNL
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  • 5
    Publication Date: 2019-05-14
    Description: We estimate the global rate of biogenic silica production in the ocean to be between 200 and 280 × 1012 mol Si yr−1. The upper limit is derived from information on the primary productivity of the oceans, the relative contribution of diatoms to primary production and diatom Si/C ratios. The lower limit is derived independently using a multi‐compartment model of nutrient transport and biogenic particle flux, and field data on the balance between silica production and dissolution in the upper ocean. Our upper limit is 30–50% lower than several previous estimates, due to new data indicating lower values for both the relative contribution of diatoms to primary productivity and their Si/C ratios. Globally, at least 50% of the silica produced by diatoms in the euphotic zone dissolves in the upper 100 m, resulting in an estimated export of 100–140 × 1012 mol Si yr−l to the deep ocean. Our estimates correspond to a global mean rate of biogenic silica production between 0.6 and 0.8 mol Si m−2 yr−1. Incubation experiments indicate that silica production rates exceed that mean by a factor of 3–12 in coastal areas and are 2–4 times less than the global average in the oligotrophic mid‐ocean gyres. The mean silica production rate in waters overlying diatomaceous sediments (approximately 10–12% of the surface area of the oceans) is 0.7–1.2 mol Si m−2 yr−1. That rate is only slightly higher than the global average, indicating that the silica produced in those regions is only 10–25% of the global total. The estimated production of biogenic silica in surface waters of the mid‐ocean gyres is approximately equal to that for all major areas of opal sediment accumulation combined. Regional comparison of silica production and accumulation rates suggests a strongly bimodal character in the efficiency of opal preservation in the sea. In waters overlying diatom‐rich sediments 15–25% of the silica produced in the surface layer accumulates in the seabed, while virtually none of the silica produced in other areas is preserved. The global burial/production ratio of ˜ 3% is a composite of those two very different systems. The mechanisms leading to more efficient opal preservation in regions of silica accumulation are presently unknown, but they have no simple relationship to primary productivity. Regional differences in opal preservation appear to be controlled by factors such as low surface temperature, selective grazing and aggregate formation, which diminish the rate of silica dissolution in surface waters and/or accelerate its transport to the seafloor.
    Type: Article , PeerReviewed
    Format: text
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  • 6
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The availability of iron limits primary productivity and the associated uptake of carbon over large areas of the ocean. Iron thus plays an important role in the carbon cycle, and changes in its supply to the surface ocean may have had a significant effect on atmospheric carbon dioxide ...
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1432-2056
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary In order to simulate the fate of biogenic silica generated in the surface waters of the Southern Ocean, the dissolution of silica frustules was studied for seven natural assemblages of diatoms, collected during summer 1984 in the Indian sector, and two typical Antarctic diatoms (Nitzschia cylindrus and Chaetoceros deflandrei), following the procedure of Kamatani and Riley (1979). For mean summer conditions in the surface waters of the Southern Ocean (2〈T°C〈12; 7.5〈pH〈8) rate coefficients of dissolution range from 2.2 to 18.5x10-3d-1 for the natural assemblages. The silica frustules trapped by fecal pellets and by gelatinous aggregates, and rapidly transported through the cold waters of the Circumpolar Current, reach the sea bottom of either the continental shelves of the abysses without loosing much of the initial amount of silica (less than 10%). A model based on Stokes' law, modified to take in account of non ideal conditions and of the upwelling rate, is used in order to simulate the fate of silica of unaggregated particles settling down in the cold waters of the Antarctic Divergence. It supports the ideas that 1-the cycle of siliceous particles which radii are 〈2 μm (i.e., of a part of the nanoplankton) is completely achieved in the surface layer, 2-although the biogenic silica of large unaggregated particles (radii over 25 μm) may reach the seabottom (within one month to a few years) without complete dissolution, the main explanation for the accumulation of biogenic silica on Antarctic abysses remains transport by fecal pellets and gelatinous aggregates.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Polar biology 15 (1995), S. 381-392 
    ISSN: 1432-2056
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Size-fractionated primary production was measured by carbon-14 uptake incubations on three transects between 47°S and 59°30′S along 6°W in October/November 1992. Open Antarctic Circumpolar Current and ice-covered Weddell Gyre water showed comparable low productivity (∼0.3 gCm−2 day−1) and size distribution. Picoplankton (〈2 μm) was the dominant size fraction, contributing approximately half to the total water column production. The significance of larger (〉20 μm) phytoplankton was only minor. Productivity in the Polar Front Zone north of 50°S, with higher water column stability, was up to 10 times higher with microplankton (〉20 μm) being predominant. No ice-edge bloom occurred over the 2 months study period; this is explained by non-favourable hydrographic conditions for blooming and the lack of melt-water lenses upon ice retreat. Picoplankton tended to make higher contributions at lower water column stability, and microplankton to make higher contributions at higher stability. Mixing, together with light climate, are discussed as the driving forces for Antarctic primary production and for its size structure.
    Type of Medium: Electronic Resource
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  • 9
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    PANGAEA
    In:  EPIC3Smetacek, Victor; de Baar, Hein JW; Bathmann, Ulrich; Lochte, Karin; Rutgers van der Loeff, Michiel M (1997): Ecology and biogeochemistry of the Antarctic circumpolar current during austral spring: Southern Ocean JGOFS Cruise ANT X/6 of R.V. Polarstern. D, Bremerhaven, PANGAEA, pp. 00100-2
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
    Format: application/pdf
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  • 10
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    Unknown
    PANGAEA
    In:  Supplement to: Lasbleiz, Marine; Leblanc, Karine; Armand, Leanne K; Christaki, Urania; Georges, Clément; Obernosterer, Ingrid; Quéguiner, Bernard; King, Gary M (2016): Composition of diatom communities and their contribution to plankton biomass in the naturally iron-fertilized region of Kerguelen in the Southern Ocean. FEMS Microbiology Ecology, 92(11), fiw171, https://doi.org/10.1093/femsec/fiw171
    Publication Date: 2023-07-09
    Description: In the naturally iron-fertilized surface waters of the northern Kerguelen Plateau region, the early spring diatom community composition and contribution to plankton carbon biomass were investigated and compared with the High Nutrient Low Chlorophyll (HNLC) surrounding waters (October-November 2011, KEOPS 2). The large iron-induced blooms were dominated by small diatom species belonging to the genera Chaetoceros (Hyalochaete) and Thalassiosira, which rapidly responded to the onset of favorable light-conditions in the meander of the Polar Front. In comparison, the iron-limited HNLC area was typically characterized by autotrophic nanoeukaryote-dominated communities and by larger and more heavily silicified diatom species (e.g. Fragilariopsis spp.). Our results support the hypothesis that diatoms are valuable vectors of carbon export to depth in naturally iron-fertilized systems of the Southern Ocean. Comparison with the diatom assemblage composition of a sediment trap deployed in the iron-fertilized area suggests that the dominant Chaetoceros (Hyalochaete) cells were less efficiently exported than the less abundant yet heavily silicified cells of Thalassionema nitzschioides and Fragilariopsis kerguelensis. Our observations emphasize the strong influence of species-specific diatom cell properties combined with trophic interactions on matter export efficiency, and illustrate the tight link between the specific composition of phytoplankton communities and the biogeochemical properties characterizing the study area.
    Keywords: Actinocyclus curvatulus; Actinocyclus curvatulus, biomass as carbon; Asteromphalus hookeri; Asteromphalus hookeri, biomass as carbon; Asteromphalus hyalinus; Asteromphalus hyalinus, biomass as carbon; Asteromphalus parvulus; Asteromphalus parvulus, biomass as carbon; Azpeitia tabularis; Azpeitia tabularis, biomass as carbon; Biomass estimation after Cornet-Barthaux et al. (2007); Bottle number; Chaetoceros aequatoriale, biomass as carbon; Chaetoceros aequatorialis; Chaetoceros aequatorialis, biomass as carbon; Chaetoceros atlanticus; Chaetoceros atlanticus, biomass as carbon; Chaetoceros atlanticus var. neapolitanus; Chaetoceros atlanticus var. neapolitanus, biomass as carbon; Chaetoceros bulbosus; Chaetoceros bulbosus, biomass as carbon; Chaetoceros concavicornis; Chaetoceros concavicornis, biomass as carbon; Chaetoceros convolutus; Chaetoceros convolutus, biomass as carbon; Chaetoceros criophilus; Chaetoceros criophilus, biomass as carbon; Chaetoceros decipiens; Chaetoceros decipiens, biomass as carbon; Chaetoceros dichaeta; Chaetoceros dichaeta, biomass as carbon; Chaetoceros flexuosus; Chaetoceros flexuosus, biomass as carbon; Chaetoceros mitra; Chaetoceros mitra, biomass as carbon; Chaetoceros peruvianus; Chaetoceros peruvianus, biomass as carbon; Chaetoceros radicans; Chaetoceros radicans, biomass as carbon; Chaetoceros socialis; Chaetoceros socialis, biomass as carbon; Chaetoceros spp.; Chaetoceros spp., biomass as carbon; Chaetoceros spp. resting spores; Chaetoceros spp. resting spores, biomass as carbon; Corethron inerme; Corethron inerme, biomass as carbon; Corethron pennatum; Corethron pennatum, biomass as carbon; Coscinodiscus sp.; Coscinodiscus sp., biomass as carbon; CTD/Rosette; CTD-RO; Dactyliosolen antarcticus; Dactyliosolen antarcticus, biomass as carbon; Dactyliosolen tenuijunctus; Dactyliosolen tenuijunctus, biomass as carbon; DATE/TIME; DEPTH, water; Diatoms; Diatoms, biomass as carbon; Diatoms, centrales; Diatoms, centrales, biomass as carbon; Diatoms, pennales; Diatoms, pennales indeterminata; Diatoms, pennales indeterminata, biomass as carbon; Elevation of event; Eucampia antarctica; Eucampia antarctica, biomass as carbon; Event label; Fragilariopsis kerguelensis; Fragilariopsis kerguelensis, biomass as carbon; Fragilariopsis pseudonana; Fragilariopsis pseudonana, biomass as carbon; Fragilariopsis separanda; Fragilariopsis separanda, biomass as carbon; Guinardia cylindrus; Guinardia cylindrus, biomass as carbon; Kerguelen Plateau; Latitude of event; Leptocylindrus danicus; Leptocylindrus danicus, biomass as carbon; Leptocylindrus mediterraneus; Leptocylindrus mediterraneus, biomass as carbon; Longitude of event; Marion Dufresne (1995); MD188; MD188_A3-2_CTD-108; MD188_E-1_CTD-028; MD188_E-3_CTD-051; MD188_E-4E_CTD-095; MD188_E-4W_CTD-081; MD188_E-5_CTD-115; MD188_F-L_CTD-064; MD188_R-2_CTD-018; Membraneis challengeri; Membraneis challengeri, biomass as carbon; Membraneis imposter; Membraneis imposter, biomass as carbon; Membraneis sp.; Membraneis sp., biomass as carbon; Navicula spp.; Navicula spp., biomass as carbon; Nitzschia bicapitata; Nitzschia bicapitata, biomass as carbon; Nitzschia closterium; Nitzschia closterium, biomass as carbon; Nitzschia longissima; Nitzschia longissima, biomass as carbon; Odontella weissflogii; Odontella weissflogii, biomass as carbon; OISO_20, KEOPS 2; Paralia spp.; Paralia spp., biomass as carbon; Plagiotropis spp.; Plagiotropis spp., biomass as carbon; Pleurosigma sp.; Pleurosigma sp., biomass as carbon; Proboscia alata; Proboscia alata, biomass as carbon; Proboscia inermis; Proboscia inermis, biomass as carbon; Proboscia truncata; Proboscia truncata, biomass as carbon; Pseudo-nitzschia spp.; Pseudo-nitzschia spp., biomass as carbon; Quantitative phytoplankton method (Utermöhl, 1958); Radiation, photosynthetically active; Rhizosolenia antennata; Rhizosolenia antennata, biomass as carbon; Rhizosolenia chunii; Rhizosolenia chunii, biomass as carbon; Rhizosolenia crassa; Rhizosolenia crassa, biomass as carbon; Rhizosolenia pungens; Rhizosolenia pungens, biomass as carbon; Rhizosolenia simplex; Rhizosolenia simplex, biomass as carbon; Rhizosolenia styliformis; Rhizosolenia styliformis, biomass as carbon; Rhizosolenia styliformis var. longispina; Rhizosolenia styliformis var. longispina, biomass as carbon; Thalassionema nitzschioides var. lanceolata; Thalassionema nitzschioides var. lanceolata, biomass as carbon; Thalassionema nitzschioides var. nitzschioides; Thalassionema nitzschioides var. nitzschioides, biomass as carbon; Thalassionema nitzschioides var. parva; Thalassionema nitzschioides var. parva, biomass as carbon; Thalassiosira gracilis; Thalassiosira gracilis, biomass as carbon; Thalassiosira lentiginosa; Thalassiosira lentiginosa, biomass as carbon; Thalassiosira spp.; Thalassiosira spp., biomass as carbon; Thalassiosira tumida; Thalassiosira tumida, biomass as carbon; Thalassiothrix antarctica; Thalassiothrix antarctica, biomass as carbon
    Type: Dataset
    Format: text/tab-separated-values, 11715 data points
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