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  • NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS  (14)
  • Vitamin D  (5)
  • Apatite  (4)
  • PANGAEA  (14)
  • Springer  (9)
  • Nature Publishing Group
  • 1965-1969  (21)
  • 1935-1939  (2)
Collection
Keywords
Publisher
  • PANGAEA  (14)
  • Springer  (9)
  • Nature Publishing Group
Years
Year
  • 1
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    PANGAEA
    In:  Supplement to: Gulbrandsen, R A; Reeser, D W (1969): An occurrence of Permian manganese nodules near Dillon, Montana. In: Geological Survey Research 1969, Chapter C, U.S. Geological Survey Professional Paper; http://pubs.usgs.gov/pp/0650c/report.pdf, 650C, 49-57, hdl:10013/epic.46181.d003
    Publication Date: 2023-08-28
    Description: Concentrically ringed manganese nodules, similar in form to many found on modern ocean and sea floors, occur in a very fine grained argillaceous sandstone bed of the Permian Park City Formation near Dillon, Montana. They are enriched in many rare elements and contain us much as 2.5 percent zinc, l.3 percent nickel, and 0.22 percent cobalt. The manganese minerals are chalcophanite and todorokite. The nodules probably formed in a shallow marine oxidizing environment on the western side of the Permian sedimentary basin. The occurrence of an appreciable amount of fluorite in the bed suggests that the water was saline.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
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  • 2
    Publication Date: 2023-08-28
    Description: In the 1960s and 1970s, the Kennecott Corporation conducted a number of activities in the evaluation of manganese nodule deposits as well as in their possible hydrometallurgy.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
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  • 3
    Publication Date: 2023-08-28
    Description: This collection includes data on the chemical composition of ocean manganese nodules from the Pacific Ocean obtained with different methods.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
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  • 4
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    In:  Supplement to: Barnes, Steven S (1967): The formation of oceanic ferromanganese nodules (Ph.D. dissertation). University of California, San Diego, 118 pp
    Publication Date: 2023-08-28
    Description: Mineralogical and chemical analyses performed on 67 ferromanganese nodules from widely varying locations and depths within the marine environment of the Pacific Ocean indicate that the minor element composition is controlled by the mineralogy and that the formation of the mineral phases is depth dependent. The pressure effect upon the thermodynamics or kinetics of mineral formation is suggested as the governing agent in the depth dependence of the mineralogy. The minor elements, Pb and Co, appear concentrated in the dMnO2 phase, whereas Cu and Ni are more or less excluded from this phase. In the manganites, Pb and Co are relatively low in concentration, whereas Cu and Ni are spread over a wide range of values. The oxidation of Pb and Co from divalent forms in sea water to higher states can explain their concentration in the dMnO2 phase.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
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  • 5
    Publication Date: 2023-08-28
    Description: Manganese nodules recovered in the Pacific Ocean by the U. S. Bureau of Mines and by DeepSea Ventures Ltd. are studied for their chemical composition using X microprobe and X-ray fluorescence methods.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
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  • 6
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    PANGAEA
    In:  Supplement to: Isaeva, Alexandra B (1967): Chemical composition of ferromanganese nodules of the Indian ocean (in Russian). Lithology and Mineral Resources, 3, 43-56, hdl:10013/epic.46141.d001
    Publication Date: 2023-08-28
    Description: This paper presents data on the chemical composition of iron-manganese nodules and associated sediments collected during the 35th voyage of the R/V "Vityaz" in 1962. The samples were made available to the author by Prof, P. L. Bezrukov. Data on the general distribution of manganese nodules at the bottom of the Indian Ocean were already given by P. L. Bezrukov (1962, 1963). Here the author analyzed the geochemistry of nodules samples from seven stations and four samples from the associated sediments. The analysis separates the outer layer of nodules from their apparent internal core.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
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  • 7
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    In:  Supplement to: Mero, John L (1965): The Mineral Resources of the Sea. Elsevier Oceanography Series, 1, 312 pp, https://www.sciencedirect.com/bookseries/elsevier-oceanography-series/vol/1/suppl/C
    Publication Date: 2023-08-28
    Description: The book is a compilation of all available data at the time of publication (1965) on the subject of marine minerals together with the author's original ideas regarding their exploitation. It is one of the most significant publications on ocean resources. It is particularly focused on manganese deposits, their description, sedimentary setting, formation and geochemistry.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
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  • 8
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    PANGAEA
    In:  Supplement to: Winterhalter, Boris (1966): Pohjanlahden ja Suomenlahden rauta-mangaani-saostumista. Summary: Iron-manganese concretions from the gulf of Bothnia and the gulf of Finland. Geoteknillisiä julkaisuja - Geotekniska meddelanden - Geotechnical publications, 69, 77 pp, https://tupa.gtk.fi/julkaisu/geoteknillinen/gt_s_069.pdf
    Publication Date: 2023-08-28
    Description: Iron-manganese concretions, closely related to lacustrine ores and deep sea manganese nodules, are presently forming in different parts of Gulfs of Bothnia and Finland. They can be divided according to physical form into three distinct groups: (1) round pea-shaped concretions, (2) ring-shaped concrections, and (3) flat sheets and crusts of concretionary material. A definite correlation was found to exist between the form i.e. type of concretions and their chemical composition (Mn/Fe ratio). Trace element concentrations were generally rather high, although not as high as in deep sea manganese nodules. X-ray and DTA was used to study the mineralogy and crystal structure of the concretions. Surface concentrations and geographical distribution of the concretions were estimated on the basis of samples, diving observations and echo-grams.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
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  • 9
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    PANGAEA
    In:  Supplement to: Wiseman, J D H (1937): Basalts from the Carlsberg Ridge, Indian Ocean. In: Geological and Mineralogical Investigations, The John Murray Expedition 1933-1934 - Scientific Reports. British Museum ( Natural History ), London, United Kingdom, 3(1), 2-31, hdl:10013/epic.46160.d006
    Publication Date: 2023-08-28
    Description: During the cruise of the" Mabahiss" from Zanzibar to Colombo at Station 133 (1° 25' 54" S. to 1° 19' 42" S. and 66° 34' 12" E. to 66° 35' 18" E.) several small rock fragments were brought up in the Monegasque net; and, since at this position there is no possibility of the material being transferred by floating Ice, these specimens are of some interest as samples of oceanic rock foundations. All the rocks have a black appearance, but in the majority this skin is of negligible thickness. Exceptionally, however, it may attain to 1/3 in. (St. 133, 8), and then the specimens are rounded. The coating is made of dark opaque manganese material. At Station 166 one or two similar specimens of angular basalt were found in the trawl consisting mainly of manganese nodules.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
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  • 10
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    PANGAEA
    In:  Supplement to: Audley-Charles, M G (1965): A geochemical study of Cretaceous ferromanganiferous sedimentary rocks from Timor. Geochimica et Cosmochimica Acta, 29(11), 1153-1173, https://doi.org/10.1016/0016-7037(65)90067-0
    Publication Date: 2023-08-28
    Description: Seven manganese nodules, eight ferromanganiferous shales from the Cretaceous Wai Bua Formation of Timor, and a pelagic limestone with four ferromanganese enriched layers from the Middle Eocene of Timor have been analysed. The nodules are compared with modern deep-sea nodules, and the ferromanganiferous shales are contrasted with relatively shallow marine manganiferous shales. The conclusion is reached that these rocks from Timor were probably deposited in a bathypelagic environment. There is a total absence of any indication that volcanic material has contributed to these deposits. The chemical composition of the ferromanganiferous rocks are discussed and some indications of biogenic influences are noted. The Middle Eocene pelagic limestone is compared with a similar modern sediment described from the Easter Island Rise in the Pacific.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
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  • 11
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    PANGAEA
    In:  Supplement to: Barnes, Steven S; Dymond, Jack R (1967): Rates of accumulation of ferro-manganese nodules. Nature, 213(5082), 1218-1219, https://doi.org/10.1038/2131218a0
    Publication Date: 2023-08-28
    Description: Although various models have been proposed to explain the origin of manganese nodules (see Goldberg and Arrhenius), two major hypotheses have received extensive attention. One concept suggests that manganese nodules form as the result of interaction between submarine volcanic products and sea water. The common association of manganese nodules with volcanic materials constitutes the main evidence for this theory. The second theory involves a direct inorganic precipitation of manganese from sea water. Goldberg and Arrhenius view this process as the oxidation of divalent manganese to tetravalent manganese by oxygen under the catalytic action of particulate iron hydroxides. Manganese accumulation by the Goldberg and Arrhenius theory would be a relatively slow and comparatively steady process, whereas Bonatti and Nayudu believe manganese nodule formation takes place subsequent to the eruption of submarine volcanoes by the acidic leaching of lava.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
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  • 12
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    PANGAEA
    In:  Supplement to: Ehrlich, A M (1968): Rare earth abundances in manganese nodules. Ph.D. Dissertation, Massachusetts Intitute of Technology, Boston, Massachusetts, U.S.A., 222 pp
    Publication Date: 2023-08-28
    Description: Concentrations of the rare earths have been determined in ten modern manganese nodules from the Atlantic, Pacific, and Indian Oceans, the Baltic Sea, and Lake Charlotte in Nova Scotia. A nodule from a Paleozoic era sea in Montana, a manganese film from a coral found on the Mid-Atlantic Ridge, and samples of the manganese and phosphorite pavements fround on the Blake Plateau were also analyzed. The manganese pavement, a mixed manganese-phosphate concretion from the Blake Plateau and one of the Atlantic nodules with its underlying red clay core were segmented and analyzed.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
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  • 13
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    PANGAEA
    In:  Supplement to: Kindle, Edward Martin (1936): The occurrence of lake-bottom manganiferous deposits in Canadian lakes. Economic Geology, 31(7), 755-760, https://doi.org/10.2113/gsecongeo.31.7.755
    Publication Date: 2023-08-28
    Description: It is the purpose of this paper to record information concerning the distribution and occurrence of manganiferous concretions and other manganese oxide deposits that develop on certain lake bottoms. During the summer of 1935 several days were devoted to a study of this type of lake bottom deposit in various parts of Nova Scotia. Lake studies in Ontario have extended the known distribution from lakes on or near the Atlantic coast to lakes in southern Ontario. During the writer's first work on lacustrine manganiferous deposits the concretions of manganese oxide which were found were almost entirely limited to the relatively shallow parts of the lakes examined. Other lakes are now known where the manganese oxide appears to occur only in the maximum depths.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
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  • 14
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    PANGAEA
    In:  Supplement to: Cronan, David S; Tooms, J S (1967): Geochemistry of manganese nodules from the N.W. Indian Ocean. Deep Sea Research and Oceanographic Abstracts, 14(2), 239-249, https://doi.org/10.1016/0011-7471(67)90009-5
    Publication Date: 2023-08-28
    Description: Manganese nodules collected from four sites in the N.W. Indian Ocean by R.R.S. Discovery have been analysed for a range of elements. At two of the sites, samples were collected from two morphological populations, at one of these sites each population being a distinct chemical population also. In addition, considerable differences have been observed in the composition of morphologically similar modules from sites a few miles apart. The information obtained is of significance in any consideration of the genesis of the nodules and could have practical implications in the event that manganese nodules become a potential source of manganese and other metallic elements.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
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  • 15
    Electronic Resource
    Electronic Resource
    Springer
    Calcified tissue international 2 (1968), S. 237-241 
    ISSN: 1432-0827
    Keywords: Carbonate ; Bone ; Fish ; Apatite
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Description / Table of Contents: Résumé D'après la littérature, il semble que les poissons soient obligées d'hyperventiler en CO2, pour recevoir suffisamment d'oxygène. Ils présenteraient par suite une quantité faible de bicarbonate circulant. Dans cet ordre d'idée, les arêtes de truites et de carpes ont été analysés pour établir si la composition du minéral osseux traduit la faible concentration en bicarbonate sérique. Le contenu en CO2 d'arêtes de poissons n'est pas significativement différent de celui des os normaux de mammifères. Des crîstaux d'apatite synthétique, préparés dans des conditions identiques de T, μ et (HCO 3 − ), ne contiennent que 1/7ème à 1/8ème du CO2 d'arêtes de poissons. Ces résultats indiquent que la composition des liquides dans l'os ne réfléchit pas simplement la composition du sérum circulant, ainsi qu'on l'admet généralement.
    Abstract: Zusammenfassung Es ist in der Literatur berichtet worden, daß Fische, um genügend Sauerstoff zu erhalten, einen Überschuß von Kohlensäure einatmen müssen und folglich einen niedrigen Gehalt an Bicarbonaten im Kreislauf aufweisen. Knochen von Forellen und Karpfen wurden analysiert, um festzustellen, ob ihre Mineralsalzzusammensetzungen die niedrigen Serum-bicarbonate-konzentrationen wiederspiegeln. Die Resultate zeigten keinen wesentlichen Unterschied zwischen dem Carbonatgehalt der Knochen von Fischen und Säugetieren. Synthetische Apatitkristalle, die unter ähnlichen Bedingungen von T, μ und HCO3 bereitet wurden, wiesen nur 1/7–1/8 des Carbonatgehaltes der Fischknochen auf. Diese Ergebnisse deuten zweifellos darauf hin, daß zwischen der Zusammensetzung der Gewebeflüssigkeit der Knochen und des Serums kein einfacher Zusammenhang besteht.
    Notes: Abstract It has been reported in the literature that fish, to get sufficient oxygen, must overventilate with respect to CO2 and therefore exhibit a low circulating level of bicarbonate. Accordingly, the bones of trout and carp were analyzed to learn if the composition of their bone mineral reflects the low serum level of bicarbonate. It was found that the CO2 content of fish bone is not significantly different from that of normal mammalian bone. Synthetic apatite crystals, made under comparable conditions of T, μ, and (HCO 3 − ) were found to contain only 1/7th to 1/8th the CO2 of fish bone. These data strongly suggest that the composition of the fluids in bone does not reflect, in a simple way, the composition of the circulating serum as is generally assumed.
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  • 16
    Electronic Resource
    Electronic Resource
    Springer
    Calcified tissue international 3 (1969), S. 348-357 
    ISSN: 1432-0827
    Keywords: Inhibitors ; Nucleation ; Apatite ; Collagen
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Description / Table of Contents: Résumé Des ions de Mg, Sr et F sont inhibitoires pour la formation de l'apatite quand on les ajoute à un tampon de calcification, séparément ou en combinaisons. La précipitation de l'apatite causée par des cristaux d'apatite est moins sensible à l'action inhibitrice que la nucléation spontanée et que la précipitation catalysée par la collagène d'os de mouton. La précipitation spontanée ou catalysée sont approximativement aussi sensibles. L'inhibition par des combinaisons de Mg avec des ions de Sr ou de F est additive. Ces résultats montrent que ces inhibiteurs ont acucune action spécifique sur la catalysation par la collagène de l'os de mouton qui soit différente de celle sur la nucléation de l'apatite en soi.
    Abstract: Zusammenfassung Mg, Sr und F Ionen hemmten die Fällung von Apatit wenn sie zu einem Calciumphosphatpuffer einzeln oder zusammen hinzugefügt wurden. Die Fällung von Apatit durch Apatitkeime war weniger empfindlich hinsichtlich der Hemmung als die spontane Nucleation und als die Fällung von Apatit, welche von Schafsknochenkollagen katalysiert werden kann. Die spontane und katalysierte Fällung sind ungefähr gleich empfindlich. Die Hemmung von Mg in Kombination mit Sr oder F Ionen war additiv. Diese Resultate weisen darauf hin, daß keine spezifischen Effekte bei der Katalyse von Knochenkollagen vorliegen, welche von den Effekten bei der Nucleation von Apatit an sich verschieden sind.
    Notes: Abstract Mg, Sr and F ions acted as inhibitors of apatite formation when added to a calcification buffer separately or in combinations. The precipitation of apatite under the influence of apatite seeds was less susceptible to inhibition than were spontaneous nucleation and apatite formation catalyzed by sheep bone collagen, while the latter two were about equally susceptible. Combinations of Mg with Sr or F ions showed additive effects. These results suggest that no specific effects of these inhibitors occurred on the catalytic action of the bone collagen different from their effects on the nucleation of apatite as such.
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  • 17
    Electronic Resource
    Electronic Resource
    Springer
    Calcified tissue international 4 (1969), S. 78-83 
    ISSN: 1432-0827
    Keywords: Bone ; Calcification ; Osteomalacia ; Phosphorus ; Vitamin D
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Description / Table of Contents: Résumé Les effects d'une dose de 1 mg de vitamine D3 (40 000 Unités,) administrée par voie intra-veineuse, ont été étudiés sur l'histologie osseuse et le métabolisme du phosphore chez 19 sujets contrôles dont l'histologie était normale et 28 malades présentant les caractères histologiques de l'ostéomalacie par carence vitaminique D. L'administration de la vitamine D n'a entraîné aucune modification histologique ou biologique significative chez les sujets contrôles. Mais chez les ostéomalaciques, il est apparu en moins de sept jours une augmentation très significative du front de calcification à l'interface tissue-ostéoïde-tissue-calcifié. Cette modification s'accompagnait d'une ascension progressive de la phosphatémie et de la réabsorption tubulaire du phosphore atteignant dans le même délai des valeurs normales.
    Abstract: Zusammenfassung Bei 19 Patienten mit normaler Knochenhistologie und bei 28 Patienten mit histologisch gesicherter Osteomalacie wurde die Wirkung von 1 mg Vitamin D3 (40000 Iv) i.v. auf die Knochenhistologie und den Phosphatmetabolismus untersucht. Bei den Kontrollpatienten konnten keine signifikanten Änderungen nach Vitamin D festgestellt werden, wogegen die Osteomalacie-patienten innerhalb von 7 Tagen eine deutliche Zunahme der Verkalkungszone an der Grenze zwischen Osteoid- und Knochengewebe zeigten. Diese Änderung war von einer fortschreitenden Zunahme des Serum-Phosphates, verbunden mit einer gesteigerten renalen tubulären Rückabsorption des Phosphates begleitet; beide kehrten anschließend gleichzeitig wieder zur Norm zurück.
    Notes: Abstract The effect of a 1 mg dose of intravenous Vitamin D3 (40,000 i.u.) on bone histology and phosphate metabolism was investigated in 19 patients with normal bone histology and 28 patients with histological evidence of osteomalacia. No significant changes occurred in the control patients after Vitamin D but the patients with osteomalacia showed a marked increase, within seven days, in the proportion of osteoid having a calcification front. This was accompanied by a progressive rise in the serum phosphate, which was associated with an increase in the renal tubular reabsorption of phosphate to normal.
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  • 18
    Electronic Resource
    Electronic Resource
    Springer
    Calcified tissue international 3 (1969), S. 67-73 
    ISSN: 1432-0827
    Keywords: Bones ; Vitamin D ; Enzymes ; Phosphatases ; Hydrolases
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Description / Table of Contents: Résumé On a fait des recherches sur les conséquences d'un manque de la vitamine D par rapport a la croissance, a la composition ionique du sang et de l'activité encymatique dans l'os chez le rat. La diét contenait 0,6% de calcium et 0,6% de phosphore. Sans apport de vitamine D la croissance était lente, la cendre de la métaphyse diminuait, le serum calcium abaissait le serum phosphore augmentait. L'activité des encymes dans la métaphyse et la diaphyse de la tibia et du femur était la suivante: alkaline phosphatase, acide β-glycerophosphatase, activité protéolytique a pH 8, ta leucin-aminopéptidase et la glutamatdehydrogenase était augmenté dans la métaphyse; la lactatdehydrogenase et l'acide phénylphosphatase était diminué. Des changements comparables étaient decouvertes dans la diaphyse a l'éxception d'une activité de lactatdehydrogenase et de phenylphosphatase non alterée; en outre l'activité proteolytique a pH 5 était augmentée. Le manque de la vitamine D restait sans influence sur l'aspartattrans-aminase et alanintransaminase. L'activité proteolytique a pH 3,7 n'était pas changée. Ces altération encymatiques ne peuvent pas etre provoquées par une malnutrition parce que'elles n'etaient pas observées chez des animales avec une nuriture identique mais a, laquelle on avait ajouté de la vitamin D. Les encymes cataboliques ne manquait pas, la calcémie basse n'est donc pas éxpliquable par une réduction de la résorption osseuse. Les résultats sont plustôt en faveur d'une résorption osseuse très active.
    Abstract: Zusammenfassung Der Effekt von Vitamin D-Mangel auf Wachstum, Serumionen und Enzymaktivität im Knochen wurde bei der Ratte untersucht. Die Diät enthielt 0,6% Calcium und 0,6% Phosphor. Vitamin D-freie Diät hatte verzögertes Wachstum, Abnahme der Knochenasche in der Metaphyse, erniedrigtes Serumcalcium und erhöhtes Serumphosphat zur Folge. Die enzymatische Aktivität in der Metaphyse und Diaphyse von Tibia und Femur veränderte sich: alkalische Phosphatase, saure β-Glycerophosphatase, proteolytische Aktivität bei pH 8, Leucin-Aminopeptidase und Glutamatdehydrogenase waren in Knochenproben der Metaphyse vermehrt, Lactatdehydrogenase und saure Phenylphosphatase vermindert. Ähnliche Veränderungen der Enzymaktivität im Knochen fanden sich in der Diaphyse, mit Ausnahme unveränderter Aktivität von Lactatdehydrogenase und saurer Phenyphosphatase sowie erhöhter proteolytischer Aktivität bei pH 5. Der Vitamin D-Mangel ließ die Aspartat-und Alanin-Transaminasen sowie die proteolytische Aktivität bei pH 3,7 unverändert. Die Enzymveränderungen sind nicht durch geringere Nahrungsaufnahme bedingt, weil sie bei Tieren mit identischer Ernährung, aber ohne Vitamin D-Entzug, nicht beobachtet wurden. Ein Mangel an Abbaufermenten, welcher Hemmung der Knochenresorption bewirken und für den Abfall des Serumcalciums verantwortlich sein könnte, ließ sich nicht finden. Die Resultate sprechen eher für vermehrte Knochenresorption.
    Notes: Abstract The effect of vitamin D deficiency on growth, serum ions and bone enzymatic activity has been studied in rats. The diet contained 0.6% calcium and 0.6% phosphorus. Omission of vitamin D from the diet resulted in decreased growth, decreased metaphyseal bone ash, decreased serum calcium and increased serum phosphorus. Changes in enzymatic activity in metaphyseal and diaphyseal bone from the tibia and femur also occurred. Alkaline phosphatase, acid β-glycerophosphatase, proteolytic activity at pH 8.0, leucine aminopeptidase, and glutamate dehydrogenase were increased in metaphyseal bone samples. Lactate dehydrogenase and acid phenylphosphatase were decreased. Similar changes in bone enzymatic activity occurred in the diaphysis except that the lactate dehydrogenase and acid phenylphosphatase activities were not decreased and proteolytic activity at pH 5.6 was increased. The vitamin D deficiency did not affect aspartate or alanine transaminase or proteolytic activity at pH 3.7. These enzyme changes were not due to decreased food consumption because they did not occur in pair-fed animals. There was no lack of degradative enzymes that would impair bone resorption and lead to a fall in serum calcium. Rather the results were more consistent with an increase in bone resorption.
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  • 19
    Electronic Resource
    Electronic Resource
    Springer
    Calcified tissue international 3 (1969), S. 74-83 
    ISSN: 1432-0827
    Keywords: Vitamin D ; Calcium Homeostasis ; Adrenalectomy
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Description / Table of Contents: Résumé On a étudié l'effet de la suppression des capsules surrénales au point de vue de la distribution du radiocalcium chez des rats rachitiques et chez des rats traités par la vitamine D. Cette opération a produit une augmentation du dépôt de radiocalcium dans les fémurs des rats rachitiques et également des rats traités par la vitamine D comparés à leurs contrôles respectifs ayant eu une opération simulée. Cependant, une analyse kinétique des données sur l'assimilation squelettique du radiocalcium a démontré que les degrés de déposition du minéral de l'os étaient amoindris par la suppression des capsules surrénales du moins chez les animaux traités par la vitamine D. D'autre part, la vitamine D a augmenté le degré de déposition plus que celui des contrôles rachitiques à la fois chez les animaux ayant eu ou non leurs capsules surrénales supprimées. De plus on a démontré que la vitamine D a rehaussé l'absorption intestinale autant que la déposition squelettique du radiocalcium chez le rat rachitique à qui on a enlevé les capsules surrénales.
    Abstract: Zusammenfassung In dieser Arbeit wurde die Auswirkung der Nebennierenentfernjng auf die Verteilung radioaktivem Calciums in rachitischen und Vitamin D behandelten Ratten untersucht. Entfernung der Nebennieren hatte eine erhöhte Ablagerung von radioaktivem Calcium in den Obserschenkelknochen der rachitischen und mit Vitamin D behandelten Ratten gegenüber den jeweiligen scheinoperierten Kontrollen zur Folge. Jedoch konnte durch kinetische Analyse der Ablagerungswerte von radioaktivem Calcium im Skelet festgestellt werden, daß die Menge der abgelagerten Knochenmineralien durch Entfernung der Nebennieren zumindest bei den mit Vitamin D behandelten Ratten herabgesetzt wurde. Auf der anderen Seite hat die Verabreichung von Titamin D die Ablagerungsmenge bei Ratten, denen die Nebennieren entfernt wurden und in solchen, die nicht operiert wurden, den rachitischen Kontrollen gegenüber erhöht. Zusätzlich konnte gezeigt werden, daß bei rachitischen Ratten nach Nebennierenentfernung und nach Behandlung mit Vitamin D erhöhte Darmabsorption und Skeletablagerung radioaktiven Calciums stattfand.
    Notes: Abstract The effect of adrenalectomy on radiocalcium distribution in rachitic and vitamin D-treated rats was studied. Adrenalectomy resulted in an increased deposition of radiocalcium in the femurs of both rachitic and vitamin D-treated rats when compared with their respective shamoperated controls. However, kinetic analysis of the data on the skeletal uptake of radiocalcium demonstrated that accretion rates of bone mineral were decreased by adrenalectomy at least in vitamin D-treated animals. Vitamin D administration, on the other, hand increased the accretion rate over that of rachitic controls in both adrenalectomized and non-adrenalectomized animals. In addition vitamin D was shown to enhance intestinal absorption as well as skeletal deposition of radiocalcium in the adrenalectomized rachitic rat.
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  • 20
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    Calcified tissue international 2 (1968), S. 343-352 
    ISSN: 1432-0827
    Keywords: Nucleation ; Mineralization ; Bone ; Collagen ; Apatite
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Description / Table of Contents: Résumé Nous avons utilisé de la collagène d'os de mounton et de tendons de queues de rats et des cristaux d'apatite pour étudier dans un système modèle la catalysation de la nucléation et la déposition de minéral dans un tampon métastabile. La collagène d'os de mouton se trouvait être un bon catalysateur, tandis que des expériences antérieures ont démontré que la collagène de tendons de queues de rats était un catalysateur très faible. Le phase rapide de la déposition de l'apatite dans la collagène se termine aussitôt que le contenu du minéral a attaint au plus 50 à 60 pour cent, bien que la supersaturation du tampon est encore bien èlevée. Les résultats montrent que dans un tel système modèle la quantité du depôt minéral est réglée par des facteurs semblables à ceux qui opèrent pendant la calcification biologique.
    Abstract: Zusammenfassung Kollagen aus Schafsknochen und Rattenschwanzsehnen und Apatitkeime wurden verwendet in einem Modell-System zur Untersuchung der katalytischen Nukleation und der Fällung von Mineral in einem metastabilen Calciumphosphatpuffer. Kollagen aus Schafsknochen war ein guter Katalysator für die Nukleation, während in früheren Versuchen sich herausstellte, daß Rattenschwanzkollagen ein ganz schlechter Katalysator ist. Die schnelle Phase der Apatitfällung im Kollagen war beendet, wenn der Mineralgehalt bis zu 50–60% angestiegen war, obwohl der Puffer noch stark übersättigt war. Die Resultate weisen daraufhin, daß die Menge des gefällten Minerals in einem solchen Modell-System von ähnlichen Faktoren reguliert wird wie die biologische Verkalkung.
    Notes: Abstract Sheep bone collagen, rat tail tendon collagen and apatite seeds were used in a model system to study nucleation catalysis and mineral deposition in a metastable calcification buffer. Sheep bone collagen was shown to be a good nucleation catalyst, while earlier experiments have shown that rat tail tendon collagen was a very poor catalyst. The rapid phase of apatite deposition in the collagen was terminated as soon as a mineral content of not more than 50–60 per cent was reached, although the buffer was still highly supersaturated. The results suggest that the amount of mineral deposited in such a model system is regulated by factors similar to those operating in biological calcification.
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  • 21
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    Calcified tissue international 2 (1968), S. 299-300 
    ISSN: 1432-0827
    Keywords: Phosphate ; Absorption ; Vitamin D ; Osteomalacia
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
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  • 22
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    Calcified tissue international 2 (1968), S. 301-313 
    ISSN: 1432-0827
    Keywords: Calcium ; Absorption ; Vitamin D
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
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  • 23
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    Calcified tissue international 2 (1968), S. 38-48 
    ISSN: 1432-0827
    Keywords: Apatite ; Calcium Phosphates ; Crystallization ; Precipitation ; X-ray Diffraction
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Description / Table of Contents: Résumé Le premier solide qui se forme au cours de la précipitation des phosphates de calcium, à partir de solutions basiques, est non-cristallin au point de vue structural. L'existence d'une solution saline non-cristalline d'orthophosphate n'est, cependant, pas propre au système des phosphates de calcium. Des phosphates de magnésium et des phosphates de magnésium — ammonium non-cristallins peuvent également être préparés dans des conditions similaires: mais, contrairement au sel calcique, qui se transforme en hydroxyl-apatite, ces composés sont apparemment stable. Des solutions basiques d'orthophosphates de strontium et de baryum ne forment pas de produits intermédiaires non-cristallins. Pour le strontium, la phase intermédiaire est constituée par le Sr3(PO4)2·4H2O, alors que le phosphate de baryum se précipite immédiatement sous forme d'un hydroxyl-apatite de baryum stable. Le phosphate de tristrontium se transforme cependant par autocatalyse en hydroxylapatite de strontium. La stoïchiométrie similaire et le comportement cinétique identique du produit intermédiaire de strontium avec ceux du phosphate de calcium amorphe semblent indiquer que ce dernier est constitué par un phosphate tricalcique plutôt que par une hydroxyl-apatite crypto-cristalline, déficiente en calcium. Ces faits semblent confirmer la possibilité non-apatitique de la phase non-cristalline du minéral osseux. Il peut s'agir d'un composé séparé et distinct.
    Abstract: Zusammenfassung Der erste feste Bestandteil, welcher beim Fällen von Calciumphosphat aus alkalischen Lösungen erscheint, ist strukturmäßig nicht-kristallin. Allerdings ist das Vorkommen eines nicht-kristallinen, aus einer Lösung hergestellten Orthophosphatsalzes nicht nur dem Calcium-phosphat-System eigen, können doch auch nicht-kristalline Magnesiumphosphate und Magnesiumammoniumphosphate unter ähnlichen Bedingungen gewonnen werden. Im Gegensatz zum Calciumsalz sind diese Verbindungen jedoch in Lösung anscheinend stabil. Alkalisch hergestellte Lösungen von Strontium- und Barium-Orthophosphaten ergeben keine nicht-kristalline Zwischenverbindungen. Für Strontium ist die intermediäre Phase Sr3(PO4)2·4H2O, während das Barium sogleich als Bariumhydroxyapatit ausfällt. Das Tristrontiumphosphat hingegen verwandelt sich autokatalytisch zu Strontiumhydroxyapatit. Die ähnliche stöchiometrische Form und das identische kinetische Verhalten der Strontium-Zwischenverbindung mit jener des amorphen Calciumphosphates läßt den Schluß zu, daß das Calciumphosphat eher ein Tricalciumphosphat als ein kryptokristallines, calciumarmes Hydroxyapatit sein könnte. Diese Annahme erhärtet die These, wonach die nichtkristalline Phase im Knochenmineral kein Apatit, sondern eine bestimmte, eigenständige Verbindung wäre.
    Notes: Abstract The first solid to appear in the precipitation of calcium phosphates from basic solutions is structurally non-crystalline. The existence, however, of a solution-prepared, non-crystalline orthophosphate salt is not unique only to the calcium phosphate system. Non-crystalline magnesium phosphates and magnesium ammonium phosphates can also be prepared under comparable conditions, but unlike the calcium salt, which converts into hydroxyapatite, these latter compounds are apparently solution stable. Preparations of strontium and barium orthophosphates from basic solution do not yield non-crystalline intermediates. For strontium, the intermediate phase is Sr3(PO4)2·4H2O, whereas the barium precipitates immediately as a stable barium hydroxyapatite. The tristrontium phosphate, however, converts autocatalytically into strontium hydroxyapatite. The analogous stoichiometry and identical kinetic behavior of the strontium intermediate with that of the amorphous calcium phosphate suggest that the latter could be a tricalcium phosphate rather than a cryptocrystalline Ca-deficient hydroxyapatite. This supports the possibility that the non-crystalline phase in bone mineral may not be an apatite but instead a distinct and separate compound.
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