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  • Calcium  (39)
  • Springer  (39)
  • American Association for the Advancement of Science (AAAS)
  • 1980-1984  (20)
  • 1970-1974  (19)
Collection
Publisher
  • Springer  (39)
  • American Association for the Advancement of Science (AAAS)
Years
Year
  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Calcified tissue international 32 (1980), S. 45-53 
    ISSN: 1432-0827
    Keywords: Dentin ; Periodicity ; Allometry ; Calcium ; Sulfur
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Notes: Summary We have described differences in the aspects of biological rhythms for calcium and sulfur deposition on the labial and lingual sides of the growing rabbit incisor, where growth occurs along a spiral axis. The calcium oscillations appear to be smoother on the labial side than on the lingual side. The lingual side is characterized by high-frequency rhythms with high amplitudes which possess the greatest percent of the power (Fourier analysis). These observations also reflect a difference in behavior of the mean Ca concentration across the labial and lingual sides. Sulfur rhythms on the labial side have higher amplitudes than those on the lingual side, but systematic differences in distribution of power between high and low frequencies is not as pronounced as in the case of Ca. The differences in Ca rhythms reflect differences in the growth rates of incisors on either side of the spiral axis. The labial side grows slightly faster than the lingual side, and its odontoblasts secrete Ca along the spiral axis and toward the pulp cavity at the same time. Thus the resultant direction of growth is more nearly opposite the extension of the occlusal end on the labial side, and Ca is consequently deposited over a wider area relative to that on the lingual surfaces. On the lingual side, Ca is deposited within a more limited area, and growth must therefore be continuous at high frequencies. The distribution of Ca on both sides of the tooth reflects these differences in growth rate and periodicity in two ways. First, given a unit area of tooth, the calcium concentration on the labial side is less than that of the lingual side. Second, whereas the calcium concentration on the labial side declines rapidly from the enamel-dentin junction to the pulp cavity, it is uniformly high across the lingual side because its growth is more continuous at high frequencies.
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Calcified tissue international 32 (1980), S. 29-44 
    ISSN: 1432-0827
    Keywords: Rabbit ; Dentin ; Calcium ; Sulfur ; Periodicity ; Circadian ; Ultradian
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Notes: Summary We have identified a variety of biological rhythms involved in the apposition and mineralization of dentin in the rabbit incisor. Animals were injected during the day or night with lead acetate at 2-week intervals—to provide biological time markers in forming dentin—and transverse undecalcified sections of the lower incisors were prepared for electron microprobe analysis. The positions of the lead markers were identified, and the continuous distribution of calcium and sulfur was measured at 1 µm intervals between the markers. In thin sections stained with hematoxylin after decalcification, the widths of a series of structural increments (bands) were measured with an ocular micrometer. Fourier analysis of the data revealed spectra of structural and compositional rhythms with a range of periodicities which extended from a matter of hours [ultradian (〈24 h)] to days [infradian (〉24 h) and circadian (approximately 24 h)]. The structural and compositional rhythms appeared to be independent to the extent that they did not necessarily have the same periods, or amplitudes. Nor were there simple phase relationships between all of the rhythms. At some times, Ca and S fluctuations are inversely proportional (180° out of phase), but in other cases they are directly proportional or out of phase by varying degrees other than 180°. The analyses thus suggest that calcium and sulfur deposition (representing mineral and glycosaminoglycan deposition, respectively) are not simply inversely proportional, and that the hematoxylin-stained structural increments did not solely reflect differences in the distribution of the mineral components in dentin.
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  • 3
    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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  • 4
    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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  • 5
    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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  • 6
    ISSN: 1615-6102
    Keywords: Calcium ; Contraction ; Discophrya ; Ionophore A23187 ; Ruthenium red ; Tentacles
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary The tentacles of the suctorian protozoonDiscophrya collini are stimulated to contract by externally applied Ca2+. The role of extracellular Ca2+ in tentacle contraction was studied by monitoring45Ca2+ uptake, using ionophore A23187 to facilitate membrane transport of calcium and ruthenium red (RR) as an inhibitor of transport. The degree of tentacle retraction was dependent upon external Ca2+ concentration and studies with45Ca2+ using scintillation counting indicated a linear relationship between external Ca2+ concentration and Ca2+ uptake. Uptake of Ca2+ was enhanced in the presence of the ionophore while RR caused little inhibition.45Ca2+ uptake was only partially inhibited by RR when cells were subjected to a Ca2+, ionophore and RR mixture. Grain counts from light microscope autoradiographs after treatment of cells with45Ca2+/ionophore,45Ca2+/RR or45Ca2+ alone showed heavy, light and intermediate labelling respectively. In all instances the grains were evenly distributed within the cell. These observations are interpreted as supporting the suggestion that the ionophore enhances both the uptake of extracellular Ca2+ and release of Ca2+from an internal source, while the RR could only partially prevent movement of Ca2+ through the plasma mebrane. A model is presented suggesting that tentacle retraction is mediated by cytosolic Ca2+ levels which are determined by the fluxing of Ca2+ across the plasma membrane and the membrane of elongate dense bodies which act as internal Ca2+ reservoirs.
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Calcified tissue international 15 (1974), S. 85-92 
    ISSN: 1432-0827
    Keywords: Calcitonin ; Calcium ; Uptake ; bone culture
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Notes: Abstract The effect of calcitonin (CT) on calcium metabolism by bone was investigated in a stationary organ culture system, using half-calvaria from 5-day-old mice. CT induced the uptake of calcium by bones from the culture medium. This uptake was not accompanied by phosphate, so that the final Ca:P ratio of CT-treated bones (1.80±0.06) was significantly (p〈0.02) higher than the initial values before culture (1.59±0.03). The calcium uptake reached a plateau after approximately 48 hours of culture, and was reversed by PTH within 48 hours. Calcium uptake rppears to be an active effect of CT, and cannot be explained fully by an inhibition of bone aesorption, stimulation of new bone formation, or maturation of the mineral phase.
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Calcified tissue international 13 (1973), S. 217-225 
    ISSN: 1432-0827
    Keywords: Fluoride ; Parathyroid ; Calcitonin ; Bone ; Calcium
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Description / Table of Contents: Résumé L'effet du fluor, de la parathormone et de la calcitonine sur le métabolisme du calcium osseux a été étudié en culture de tissu en utilisant des demi-calottes crâniennes de souris âgées de cinq jours. Les concentrations de fluor dans les cendres des calottes crâniennes de 0,007% (groupe peu fluoré), 0,041% (groupe moyennement fluoré) et 0,107% (groupe hautement fluoré) ont été obtenues en variant l'ingestion maternelle et post-natale en fluor. Le fluor inhibe la perte de calcium des os cultivés dans le milieu témoin et celui contenant la parathormone et favorise l'enrichissement en laccium des os cultivés dans un milieu contenant de la calcitonine. De l'os mort des groupes fortement et moyennement fluorés s'enrichit plus en calcium à partir du milieu de culture que les os du groupe pauvre en fluor. Le fluor semble agir sur le métabolisme du calcium osseux essentiellement par diminution de la solubilité minérale.
    Abstract: Zusammenfassung Der Einfluß von Fluorid, Parathormon und Calcitonin auf den Calciumstoffwechsel im Knochen wurde in einem Knochenkultur-System untersucht, wobei Halbcalvarien von 5 Tage alten Mäusen verwendet wurden. Fluoridgehalte in der Asche der Halbcalvarien von 0,007% (Gruppe mit niedrigem Fluoridgehalt), 0,041% (Gruppe mit mittlerem Fluoridgehalt) und 0,1075 (Gruppe mit hohem Fluoridgehalt) wurden erhalten, indem die Fluorideinnahme der Mütter oder der Neugeborenen verändert wurde. Fluorid hemmte den Calciumverlust aus Knochen, welche im Kontrollmedium oder in Parathormon-enthaltenden Medien kultiviert worden waren, und es förderte die Calciumaufnahme von Knochen, welche in Calcitoninenthaltendem Medium kultiviert worden waren. Die toten Knochen der Gruppen mit mittlerem und hohem Fluoridgehalt nehmen mehr Calcium aus dem Kulturmedium auf als die Knochen der Gruppe mit niederem Fluorid. Fluorid scheint vor allem durch eine Herabsetzung der Mineral-Löslichkeit auf den Calciumstoffwechsel der Knochen zu wirken.
    Notes: Abstract The influence of fluoride, parathyroid hormone and calcitonin on bone calcium metabolism was investigated in a bone culture system using half-calvaria of five-day old mice. Fluoride levels in the ash of half-calvaria of 0.007% (low fluoride group), 0.041% (moderate fluoride group), and 0.107% (high fluoride group) were achieved by varying the maternal and neonatal intake of fluoride. Fluoride inhibited the loss of calcium from bones cultured in control medium and parathyroid hormone-containing media, and promoted the uptake of calcium by bones cultured in medium containing calcitonin. Dead bones of the moderate and high fluoride groups took up more calcium from the culture medium than bones of the low fluoride group. Fluoride appears to exert its effect on bone calcium metabolism predominantly via a reduction in mineral solubility.
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  • 9
    ISSN: 1432-0827
    Keywords: Hydroxyapatite ; Dissolution ; Pyrophosphate, Diphosphonates ; Calcium ; Phosphate
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Notes: Summary Pyrophosphate and diphosphonate ions have been said to diminish the dissolution of hydroxyapatite crystals, because they lower the equilibrium concentrations of calcium and phosphate ions in the bulk solution around hydroxyapatite crystals in a closed system. However, in a closed system these effects are not necessarily due to an effect on dissolution alone. In this paper we have used a continuous flow system to study the effects of pyrophosphate and two diphosphonates, ethane-1-hydroxy-1,1-diphosphonate and dichloromethane diphosphonate, on the dissolution of hydroxyapatite. All three compounds decreased markedly the rate of dissolution of hydroxyapatite as well as the exchangeable pools of calcium and phosphate ions around the cystals.
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  • 10
    ISSN: 1432-0827
    Keywords: 1α-Hydroxy vitamin D3 ; 1,25-Dihydroxyvitamin D3 ; Calcium ; Transport ; Intestine
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Notes: Summary The timed sequence of events following the oral administration of 1α-hydroxy vitamin D3 (1αOHD3) to rachitic chicks was compared to that following a comparable dose of 1α,25-dihydroxyvitamin D3 (1,25(OH)2D3). RNA polymerase activity was maximally increased 20% by 1αOHD3 within 1 to 2 h and returned to control values after 8 h. Alkaline phosphatase activity was stimulated by 4 h and was maximal (3- to 5-fold increase) at 24 h. Calcium binding protein (CaBP) was detected initially within epithelial cells at the proximal end of the villus (just above the crypt) 6 to 8 h after 1αOHD3 administration, in epithelial cells lining the proximal half of the villus by 24 h, and in epithelial cells along nearly the entire villus by 48 h. At no time did goblet cells contain CaBP. Serum calcium concentrations were significantly elevated in 2 h and maximal by 12 h (an increase of 3.6 mg/dl). Calcium accumulation by the intestinal mucosa in vitro was increased by 6 to 8 h and maximal (60% increase over controls) at 24 h. Phosphate accumulation by the intestinal mucosa in vitro was increased by 6 h and maximal (105% increase over controls) between 8 and 24 h. 1,25(OH)2D3 increased CaBP and calcium accumulation by 4 h, 2 h sooner than did 1αOHD3. 1,25(OH)2D3 decreased serum calcium levels and increased serum phosphate levels at 2 h unlike 1αOHD3. No difference in the effects of these compounds on alkaline phosphatase activity, RNA polymerase activity, and phosphate accumulation could be demonstrated. These results are consistent with the possibility that 1αOHD3 may not require conversion to 1,25(OH)2D3 for all of its biological effects.
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