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  • Calcium  (23)
  • Ocean Drilling Program; ODP  (23)
  • PANGAEA  (23)
  • Springer  (23)
  • 2000-2004  (27)
  • 1970-1974  (19)
  • 1960-1964
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  • 1
    ISSN: 1432-0827
    Keywords: Amorphous ; Apatite ; Electron Microscopy ; Crystallization ; Precipitation ; Calcium
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Description / Table of Contents: Résumé Du phosphate de calcium amorphe (ACP) sèché peut se présenter sous forme discoide ou sphérique. Les particules discoides sont plus fréquents dans les specimens d'ACP sèché, isolés immédiatement après précipitation. Les formes sphériques dominent dans les specimens sèchés provenant de suspensions plus âgés. Les particules discoides résultent de la dessication de l'échantillon. Les sphères peuvent aussi se produire pendant la dessication, mais s'observent aussi dans la solution. Les disques et les sphères ont une origine commune sous la forme d'un agrégat d'ACP hautement hydraté de morphologie inconnue. La formation d'apatite cristallin en solution est intimement associée avec l'ACP. Les premiers cristaux apparaissent à la surface des sphères amorphes et en contact avec les disques amorphes. En cas de sphères, les cristaux initiaux augmentent de taille et forment de nouveaux cristaux par nucléation secondaire jusqu'à ce que les sphères soient enrobées par l'apatite. Cependant, lorsque la transformation est totale, l'apatite ne remplit pas l'espace occupé préalablement par les sphères amorphes dissoutes. Ces observations ne confirment pas le concept d'une conversion d'un état solidein situ dans ce cas mais suggèrent une transition hétérophasique d'un processus de translocation ionique par l'intermédiaire d'une solution. La production de cristaux dans les disques amorphes suggère que l'apatite peut aussi se former directement du précurseur dans la solution.
    Abstract: Zusammenfassung Getrocknetes amorphes Calciumphosphat (ACP) kann scheiben- und kugelförmig auftreten. Die scheibenförmigen Partikel herrschen in getrockneten ACP-Proben vor, welche direkt nach der Fällung isoliert wurden. Die kugeligen Formen herrschen in trockenen Proben aus älteren Suspensionen vor. Die Scheibenbildung ist ein Ergebnis des Trocknungsvorganges. Kugelige Formen können beim Trocknungsvorgang ebenfalls auftreten, sie sind aber in der nativen Suspension ebenfalls anwesend. Scheiben- und Kugelformen scheinen einen gemeinsamen Vorläufer in der Lösung zu haben, welcher ein hochhydratisiertes ACP-Aggregat unbekannter Morphologie zu sein scheint. Die Bildung von kristallinem Apatit in der Lösung steht in engem Zusammenhang mit ACP. Die ersten Kristalle erscheinen auf der Oberfläche der amorphen Kugeln und in Kontakt mit den amorphen Scheiben. Die ursprünglichen Kristalle auf den Kugeloberflächen nehmen an Größe zu und bilden durch sekundäre Nukleation weitere Kristalle, bis die Kugeln in Apatit eingehüllt werden. Wenn die Umwandlung abgeschlossen ist, füllt jedoch das Apatit den Platz nicht aus, der vorher von den aufgelösten amorphen Kugeln eingenommen wurde. Diese Beobachtungen bekräftigen die Auffassung einerin situ-Umwandlung in den festen Zustand bei dem beschriebenen Falle nicht, sondern deuten auf eine heterophasischen Übergang, welcher durch einen lösungsbedingten Ionenverschiebungs-Prozeß gefördert wird. Das Auftreten von Kristallen in den amorphen Scheiben deutet darauf hin, daß sich Apatit auch direkt aus dem Lösungsvorläufer bilden kann.
    Notes: Abstract Dried amorphous calcium phosphate (ACP) can exist in discoidal and spheroidal forms. The disk-shaped particles are most prominent in dried ACP specimens isolated immediately following precipitation. The spherical forms become dominant in dried specimens taken from older suspensions. The disk-like morphology is a result of sample drying. Spherules can also arise during the drying step but are present in the native suspension as well. Both the disks and spherules appear to have a common solution progenitor in the form of a highly hydrated ACP aggregate of unknown morphology. The formation of crystalline apatite in solution is intimately connected with ACP. The first crystals appear on the surface of the amorphous spherules and in contact with the amorphous disks. In the case of the spherules, the initial crystals increase in size and generate additional crystals by secondary nucleation until the spherules become enveloped by apatite. However, when conversion is completed, the apatite does not fill appreciably the space previously occupied by the dissolved amorphous spherules. These observations do not support the concept of anin situ solid state conversion in this case, but indicate a heterophase transition supported by a solution-mediated ion translocation process. The occurrence of crystals in the amorphous disks suggest that apatite can also form directly from the solution progenitor.
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Calcified tissue international 15 (1974), S. 303-314 
    ISSN: 1432-0827
    Keywords: Diphosphonates ; Calcium ; Mitochondria ; ATPase
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Notes: Abstract The effect of two diphosphonate compounds on calcium handling in rat kidney mitochondria has been studiedin vitro. Initial calcium uptake in the presence of an oxidisable substrate and ATP was not influenced by either diphosphonate tested. The release of accumulated calcium from the mitochondria was, however, delayed by these compounds and the effect was found to be dose dependent. Similarily, a second uptake of calcium, induced by re-addition of ATP following preliminary release, was also modified by diphosphonates, the mitochondrial suspensions incubated with diphosphonates accumulating more calcium than control suspensions. The effect of these compounds could not be detected on three mitochondrial ATPase systems. The results have been discussed in relation to knownin vivo effects of diphosphonates.
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Calcified tissue international 9 (1972), S. 95-108 
    ISSN: 1432-0827
    Keywords: Amorphous ; Calcium ; Phosphate ; Electron ; Microscopy ; Damage
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Description / Table of Contents: Résumé Cinq précipités non-cristallins de phosphate de calcium, préparés à partir de solutions qui varient en pH, degré de saturation et contenu en carbonate, sont examinés par des méthodes physico-chimiques et morphologiques. Des mesures de diffractions électronique et en rayons X et de spectrophotométrie infra-rouge confirment la nature amorphe de chaque précipité. Le microscope électronique par transmission et par balayage démontre que les particules élémentaires des 5 produits synthétiques sont de forme sphérique, quelque soit la méthode de préparation. Quatre des précipités contiennent de petites sphères de taille identique (200 à 1200 Å de diamètre), alors que le dernier précipité, riche en carbonate, contient des particules plus grandes (700 à 2000 Å de diamètre). Ces sphères sont de densité électronique uniforme lorsqu'une intensité de courant, la moins élevée, est utilisée. Un faisceau d'électrons, d'intensité plus élevée, permet de mettre en évidence de nombreux centres, transparents aux électrons, dans chaque particule. In chauffage sous vide à 600° ne modifie pas la nature amorphe des précipités ou la morphologie et la taille des particules élémentaires, bien que la presque totalité de l'eau, contenu dans ces précipités, soit éliminée. L'échauffement ne provoque pas la formation de centres transparents aux électrons. Au contraire, les sphères deviennent résistantes à des dommages, causés par le faisceau. Il semble que le faisceau d'électrons agit sur les atomes d'oxygène et d'hydrogène de la phase aqueuse du phosphate de calcium amorphe et que cette réaction initiale est suivie par le déplacement et/ou la perte d'autres atomes.
    Abstract: Zusammenfassung Fünf nicht-kristalline Calciumphosphat-Niederschläge, welche aus Lösungen mit variierendem pH, Übersättigungsgrad und Karbonatgehalt gewonnen wurden, wurden mit physikochemischen und morphologischen Methoden untersucht. Röntgendiffraktion, Infrarot-Spektrophotometrie und Elektronendiffraktionsmessungen bestätigten die amorphe Natur jedes Niederschlages. Sowohl Durchstrahlungs-, als auch Raster-Elektronenmikroskopie zeigten, daß die nativen Elementarpartikel aller 5 synthetischen Produkte von kugeliger Form und unabhängig von den angewandten Präparativ-Techniken waren. Vier der Niederschläge enthielten Kügelchen von der gleichen Größe (200–1200 Å Durchmesser), während jener mit relativ hohem Karbonatgehalt viel größere Partikel aufwies (700–2000 Å Durchmesser). Die Kügelchen waren für den Elektronenstrahl von einheitlicher Dichte, wenn mit der Stromdichte bei niedrigster brauchbarer Stufe betrachtet. Wurden die Proben stärkeren Elektronenströmen ausgesetzt, so entwickelten sich sogleich in jedem Teilchen zahlreiche elektronendurchlässige Zentren. Erhitzen in Vakuum bis zu Temperaturen von 600° veränderte weder die amorphe Beschaffenheit der Niederschläge noch die Morphologie und Größe ihrer elementaren Partikel, obwohl beinahe alles Wasser, welches in den ursprünglich vorliegenden Proben enthalten war, durch dieses Vorgehen entfernt wurde. Die Hitzebehandlung verursachte keine Bildung von elektronendurchlässigen Zentren sondern machte die Kügelchen im Gegenteil in zunehmendem Maße widerstandsfähig gegenüber Strahlenschädigungen. Diese Befunde lassen vermuten, daß sich die ausgestrahlten Elektronen und die Sauerstoff- oder Wasserstoffatome der wäßrigen Komponente des amorphen Calciumphosphates gegenseitig beeinflussen und daß diese anfängliche Reaktion von einer Verdrängung und/oder einem Verlust anderer Atome gefolgt wird.
    Notes: Abstract Five non-crystalline calcium phosphate precipitates prepared from solutions varying in pH, degree of supersaturation and carbonate content were examined by physicochemical and morphological methods. X-ray diffraction, infrared spectrophotometry and electron diffraction measurements confirmed the amorphous nature of each precipitate. Both transmission and scanning electron microscopy demonstrated that the native elemental particles of all 5 synthetic products were spherical in shape and independent of the preparative procedures employed. Four of the precipitates contained spherules of similar sizes (200–1200 Å in diameter) while the one relatively rich in carbonate exhibited much larger particles (700–2000 Å in diameter). The spherules were uniformly dense to the electron beam when viewed with the current density at its lowest useful level. Exposure to higher electron currents immediately resulted in the development of numerous electron-lucent centers in each particle. Heating in vacuum to temperatures up to 600° did not change the amorphous nature of the precipitates or the morphology and size of their elemental particles even though almost all of the water contained in the original precipitates was removed by this process. Heat treatment did not induce formation of electron-lucent centers. On the contrary it, made the spherules increasingly resistant to beam damage. These findings suggest that the beam electrons interact with the oxygen or hydrogen atoms of the aqueous constituent of the amorphous calcium phosphate and that this initial reaction is followed by displacement and/or loss of other atoms.
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Journal of comparative physiology 170 (2000), S. 581-588 
    ISSN: 1432-136X
    Keywords: Key words Short chain fatty acids ; Calcium ; Rumen ; Sheep
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine
    Notes: Abstract Net Ca2+ and Mg2+ absorption rates were measured in vivo from buffer solutions placed in the washed reticulo-rumen, isolated in situ in 30 conscious, trained sheep. An increase in concentration of short chain fatty acids (SCFA) in the buffer, over the range 0–50 mM, was shown to stimulate the net rates of absorption of Ca2+ and Mg2+ ions from the rumen. Similarly, the results of in vitro experiments, carried out with ovine rumen epithelium mounted in short-circuited Ussing chambers, showed that the absence of SCFA from the chamber fluid resulted in a reduction in Jnet Ca2+ caused by reduced flux of Ca2+ ions in the mucosal to serosal direction (Jms Ca2+). The addition of 1 mM acetazolamide, an inhibitor of carbonic anhydrase, to the ruminal buffer used in the in vivo experiments led to significant reductions in the net absorption rates of Ca2+and Mg2+ ions in the presence of SCFA (50 mmol l−1) but not in the absence of SCFA. However, in the in vitro experiments, the addition of 60 μM ethoxyzolamide had no significant effect on Jnet Ca2+. A reduction in pH of the intraruminal buffer in vivo from 6.8 to 5.4 led to significant increases in the net absorption rates of Ca2+and Mg2+ ions, an effect which was duplicated for Ca2+ in preliminary in vitro experiments in which the pH of the mucosal buffer was reduced from 7.4 to 5.4. This stimulatory effect was confined to Jms Ca2+ and Jnet Ca2+. Ussing chambers were also used to demonstrate that Jnet Ca2+ was reduced by a high transmural potential difference (PD), caused by voltage clamping, independently of the mucosal K+ concentration. Both unidirectional Ca2+ fluxes consisted of a PD-dependent and a K+-insensitive PD-independent component. The latter may be represented by a Ca2+/2H+ antiporter. It is postulated that SCFA, and to a lesser extent H2CO3, can stimulate Jms Ca2+ by activation of an apical Ca2+/2H+ antiporter through the provision of protons within the ruminal epithelial cell. A mild reduction in ruminal pH may also lead to a similar stimulation of this putative electroneutral exchange.
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Journal of comparative physiology 170 (2000), S. 225-229 
    ISSN: 1432-136X
    Keywords: Key words Strontium ; Calcium ; Rumen
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine
    Notes: Abstract The net absorption rates of strontium ions from the ovine reticulo-rumen, isolated in situ in trained conscious animals, were measured under controlled conditions. A linear positive response was obtained from the addition of Sr2+ ions to the artificial rumen fluid. This increase in the absorption of Sr was reflected in an increase in the plasma Sr concentration. In contrast to the discrimination observed elsewhere in favour of the absorption of Ca relative to Sr, the absorption rate of Sr from the reticulo-rumen was significantly greater than that of Ca, from solutions containing the same molar concentration. A graded increase in the Sr concentration in the ruminal fluid from 1 mmol/l to 4 mmol/l led to a corresponding reduction in the absorption rate of Ca but an increase in that of phosphate. The latter result is similar to that observed when the intra-ruminal concentration of Ca2+ ions is increased. It is suggested that Ca and Sr share a common pathway for absorption from the reticulo-rumen and that this may involve coupling with the absorption of phosphate ions.
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  • 6
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    PANGAEA
    In:  Supplement to: White, Lisa D (2000): Diatom biostratigraphy of Sites 1039-1043, Costa Rica margin. In: Silver, EA; Kimura, G; Shipley, TH (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 170, 1-22, https://doi.org/10.2973/odp.proc.sr.170.003.2000
    Publication Date: 2024-01-09
    Description: The following data paper summarizes diatom biostratigraphic data from sediments drilled in the Costa Rica accretionary wedge during Ocean Drilling Program Leg 170. Quaternary through lower Miocene diatom zones characteristic of the equatorial Pacific region are recognized in the reference section, Site 1039, which was drilled on the downgoing Cocos plate. At Sites 1040-1043, where the recovered silty clay units are primarily wedge and apron sediments that overlie the underthrust sections, diatoms are generally low in abundance, and complete zonation of the cores was not possible above the décollement surface.
    Keywords: Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 7
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    PANGAEA
    In:  Supplement to: Summit, Melanie; Peacock, Aaron D; Ringelberg, David; White, David C; Baross, John A (2000): Phospholipid fatty acid-derived microbial biomass and community dynamics in hot, hydrothermally influenced sediments from Middle Valley, Juan De Fuca Ridge. In: Zierenberg, RA; Fouquet, Y; Miller, DJ; Normark, WR (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 169, 1-19, https://doi.org/10.2973/odp.proc.sr.169.117.2000
    Publication Date: 2024-01-09
    Description: Phospholipid fatty acids were measured in samples of 60°-130°C sediment taken from three holes at Site 1036 (Ocean Drilling Program Leg 169) to determine microbial community structure and possible community replacement at high temperatures. Five of six samples had similar concentrations of phospholipid fatty acids (2-6 pmol/g dry weight of sediment), and biomass estimates from these measurements compare favorably with direct microscopic counts, lending support to previous microscopic measures of deep sedimentary biomass. Very long-chain phospholipid fatty acids (21 to 30 carbons) were detected in the sediment and were up to half the total phospholipid fatty acid measured; they appear to increase in abundance with temperature, but their significance is not known. Community composition from lipid analysis showed that samples contained standard eubacterial membrane lipids but no detectable archaeal lipids, though archaea would be expected to dominate the samples at high temperatures. Cluster analysis of Middle Valley phospholipid fatty acid compositions shows that lipids in Middle Valley sediment samples are similar to each other at all temperatures, with the exception of very long-chain fatty acids. The data neither support nor deny a shift to a high-temperature microbial community in hot cores, so at the present time we cannot draw conclusions about whether the microbes observed in these hot sediments are active.
    Keywords: Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 8
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    PANGAEA
    In:  Supplement to: Lawrie, Darren; Miller, D Jay (2000): Data report: Sulfide mineral chemistry and petrography from Bent Hill, ODP Mound, and TAG massive sulfide deposits. In: Zierenberg, RA; Fouquet, Y; Miller, DJ; Normark, WR (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 169, 1-34, https://doi.org/10.2973/odp.proc.sr.169.106.2000
    Publication Date: 2024-01-09
    Description: Sulfide mineral major and trace element analyses were performed on more than 50 polished slabs representing mineralization from three seafloor hydrothermal massive sulfide deposits. Samples from the Bent Hill and ODP Mound massive sulfide deposits, both on the Juan de Fuca Ridge, can be contrasted with samples from the Trans-Atlantic Geotraverse (TAG) hydrothermal mound on the Mid-Atlantic Ridge. The massive sulfide at Bent Hill is predominantly pyrite and pyrrhotite, with increasing amounts of copper-bearing sulfide minerals at the base of the massive sulfide body and through the stockwork to an interval 200 m below seafloor that hosts high copper mineralization (Deep Copper Zone). ODP Mound contains much more abundant sphalerite and copper-bearing sulfides as compared to either Bent Hill or TAG, which are predominantly pyrite with much less abundant chalcopyrite. Copper-bearing sulfides from the Deep Copper Zone beneath Bent Hill and the lowest sampled interval of ODP Mound are petrographically and chemically similar, but distinct from copper-bearing minerals higher in either sequence.
    Keywords: Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 9
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    PANGAEA
    In:  Supplement to: Underwood, Michael B; Hoke, Kimberly D (2000): Composition and provenance of turbidite sand and hemipelagic mud in northwestern Cascadia Basin. In: Fisher, A; Davis, EE; Escutia, C (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 168, 1-15, https://doi.org/10.2973/odp.proc.sr.168.012.2000
    Publication Date: 2024-01-09
    Description: Sequences of late Pliocene to Holocene sediment lap onto juvenile igneous crust within 20 km of the Juan de Fuca Ridge in northwestern Cascadia Basin, Pacific Ocean. The detrital modes of turbidite sands do not vary significantly within or among sites drilled during Leg 168 of the Ocean Drilling Program. Average values of total quartz, total feldspar, and unstable lithic fragments are Q = 35, F = 35, and L = 30. Average values of monocrystalline quartz, plagioclase, and K-feldspar are Qm = 46, P = 49, and K = 5, and the average detrital modes of polycrystalline quartz, volcanic-rock fragments, and sedimentary-rock plus metamorphic-rock fragments are Qp = 16, Lv = 43, and Lsm = 41. Likely source areas include the Olympic Peninsula and Vancouver Island; sediment transport was focused primarily through the Strait of Juan de Fuca, Juan de Fuca Channel, Vancouver Valley, and Nitinat Valley. Relative abundance of clay minerals (〈2-µm-size fraction) fluctuate erratically with depth, stratigraphic age, and sediment type (mud vs. turbidite matrix). Mineral abundance in mud samples are 0%-35% smectite (mean = 8%), 18%-59% illite (mean = 40%), and 29%-78% chlorite + kaolinite (mean = 52%). We attribute the relatively low content of smectite to rapid mechanical weathering of polymictic source terrains, with little or no input of volcanic detritus from the Columbia River. The scatter in clay mineralogy probably was caused by converging of surface currents, turbidity currents, and near-bottom nepheloid clouds from several directions, as well as subtle changes in glacial vs. interglacial weathering products.
    Keywords: Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 10
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    PANGAEA
    In:  Supplement to: Peterson, Larry S; Haug, Gerald H; Murray, Richard W; Yarincik, K M; King, John W; Bralower, Timothy J; Kameo, Koji; Rutherford, Scott D; Pearce, Richard B (2000): Late Quaternary stratigraphy and sedimentation at site 1002, Cariaco basin (Venezuela). In: Leckie, RM; Sigurdsson, H; Acton, GD; Draper, G (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 165, 1-15, https://doi.org/10.2973/odp.proc.sr.165.017.2000
    Publication Date: 2024-01-09
    Description: Ocean Drilling Program Site 1002 in the Cariaco Basin was drilled in the final two days of Leg 165 with only a short transit remaining to the final port of San Juan, Puerto Rico. Because of severe time constraints, cores from only the first of the three long replicate holes (Hole 1002C) were opened at sea for visual description, and the shipboard sampling was restricted to the biostratigraphic examination of core catchers. The limited sampling and general scarcity of biostratigraphic datums within the late Quaternary interval covered by this greatly expanded hemipelagic sequence resulted in a very poorly defined age model for Site 1002 as reported in the Leg 165 Initial Reports volume of the Proceedings of the Ocean Drilling Program. Here, we present for the first time a new integrated stratigraphy for Site 1002 based on the standard of late Quaternary oxygen-isotope variations linked to a suite of refined biostratigraphic datums. These new data show that the sediment sequence recovered by Leg 165 in the Cariaco Basin is continuous and spans the time interval from 0 to ~580 ka, with a basal age roughly twice as old as initially suspected from the tentative shipboard identification of a single biostratigraphic datum. Lithologic subunits recognized at Site 1002 are here tied into this new stratigraphic framework, and temporal variations in major sediment components are reported. The biogenic carbonate, opal, and organic carbon contents of sediments in the Cariaco Basin tend to be high during interglacials, whereas the terrigenous contents of the sediments increase during glacials. Glacioeustatic variations in sea level are likely to exert a dominant control on these first-order variations in lithology, with glacial surface productivity and the nutrient content of waters in the Cariaco Basin affected by shoaling glacial sill depths, and glacial terrigenous inputs affected by narrowing of the inner shelf and increased proximity of direct riverine sources during sea-level lowstands.
    Keywords: Ocean Drilling Program; ODP
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