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  • 1
    ISSN: 1432-1041
    Keywords: Diltiazem ; immediate-release tablet ; controlled-release tablet ; steady state ; pharmacokinetics
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Medicine
    Notes: Abstract We have studied the controlled-release properties and relative systemic availabilities of two dosages of the same controlled-release (CR) diltiazem tablet formulation by comparing them at steady state with those of an immediate-release formulation. We measured 24-hour plasma concentration profiles during 4-day treatments with diltiazem 90 mg CR tablet bd diltiazem 120 mg CR tablet bd, and conventional diltiazem 60 mg immediate-release (IR) tablet tid. The study had a randomized, three-way crossover design. Twelve healthy men (38–52 y) participated. Trough plasma concentrations were determined on days 3 and 4. The 24-h plasma concentration-time profiles were assessed after the last morning dose on day 4 of each period. The following steady-state pharmacokinetic values were calculated: the minimum plasma concentration (Cmin), the maximum plasma concentration (Cmax), the time interval during which the plasma concentration exceeded 75% of Cmax (t75), the area under the plasma concentration-time curve (AUC72–96), the peak-to-trough fluctuation (PTF), and the area-under-the-curve fluctuation (AUCF). Steady state was achieved on day 3. The pharmacokinetics were comparable. For diltiazem CR 90 mg and diltiazem CR 120 mg, AUC84–96 (night) was approximately 75% of AUC72–84 (daytime). The diltiazem plasma concentration increased slowly from about 6 h after the evening dose of both CR tablets, resulting in relatively high plasma concentrations in the early morning hours. Only during treatment with diltiazem CR 120 mg were the plasma concentrations of diltiazem maintained above the minimum therapeutic plasma concentration of 50 μg·1−1 throughout the full 24 h. In conclusion, twice-daily treatment with diltiazem CR tablets can replace thrice-daily treatment with the conventional diltiazem IR tablet. The early morning rise of the diltiazem plasma concentration, which might lead to a lower incidence of ischaemic events, may be an important clinical advantage of both CR tablets. Because of the minimum therapeutic plasma concentration of 50 μg·1−1, twice-daily administration of the 120 mg CR tablet may be preferred from a therapeutic point of view. Diltiazem, a benzothiazepine, is a calcium antagonist used in the treatment of angina pectoris and hypertension. The anti-ischaemic mechanism of diltiazem seems to result from an increase of myocardial oxygen supply and a reduction in myocardial oxygen demand, respectively by coronary artery dilatation and/or direct and indirect haemodynamic effects, such as afterload reduction and heart rate decrease (Braunwald 1982). Its therapeutic effect is evident at daily dosages between 180 and 360 mg (Low et al. 1981). After oral administration it is almost completely absorbed from the gastrointestinal tract, but owing to extensive first-pass metabolism, its systemic availability is approximately 40–50% (Echizen and Eichelbaum 1986). The time to maximum plasma concentrations after oral administration of immediate-release formulations is approximately 3 to 4 h. The elimination half-life of diltiazem is 3.5–7 h, implying that frequent dosing is required to maintain effective plasma concentrations. Therefore, a controlled-release formulation of diltiazem, designed to be taken twice daily, has been developed. The aim of this crossover study was to compare the systemic availability and steady-state pharmacokinetics of a controlled-release diltiazem tablet formulation (90 and 120 mg) with those of a conventional diltiazem immediate-release tablet in healthy volunteers.
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    European journal of clinical pharmacology 48 (1995), S. 123-125 
    ISSN: 1432-1041
    Keywords: Hydrocortisone-17-butyrate ; Mometasone furoate ; plasma cortisol ; ACTH concentration ; Synacthen test ; healthy volunteers ; adrenal suppression ; fatty cream
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Medicine
    Notes: Abstract To compare the effect of multiple dose treatment with fatty cream 0.1% hydrocortisone-17-butyrate (LLFC) and fatty cream 0.1% mometasone furoate (EFC), under occlusion on adrenal function, we performed an open label, randomised, two-period crossover study, lasting 30 days, in 12 healthy, male volunteers (age 18–45 y). Morning plasma cortisol and ACTH concentrations were determined before, during, and after the treatments, and a Synacthen test was performed before and during the treatments. Both agents suppressed plasma cortisol concentrations, EFC significantly more than LLFC. ACTH concentrations were normal and were comparable between the two treatments throughout the studies, while the Synacthen tests showed normal rises in cortisol levels. Both treatments were well tolerated. We conclude that EFC has a stronger suppressive effect on plasma cortisol values than LLFC, although for short duration treatments both suppressive effects are transient.
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    International journal of earth sciences 70 (1981), S. 625-634 
    ISSN: 1437-3262
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Abstract Following a tentative evaluation of palynological information from Ladinian and, more particularly, Karnian successions, there seems to be every indication that qualitative and quantitative compositional differences of palynological assemblages could well be applied in testing concepts of Triassic phytogeography and palaeoclimatology. The following implications are emphasized: (1) There is sufficient palynological evidence that the Mediterranean region includes a domain of mixed northern (Laurasian) and southern (Gondwana) types of floras. (2) The concept of an essentially arid nature of a wide equatorial climatic belt during Triassic times finds palynological support. (3) Palynological evidence does not contradict a concept of pronounced decrease in precipitation towards the western part of the Mediterranean region. (4) In Europe, occurrences of hygrophytic palynofloras and coals within an arid climatic zone can be explained by the water-supply of extensive river-systems.
    Abstract: Résumé Suivant un essai d'évaluation des indications palynologiques recueillies dans les séries du Ladinien et plus particulièrement du Karnien, il semble qu'il y ait certaines indications pour que des différences qualitatives et quantitatives dans les assemblages palynologiques puissent très bien être mises en pratique pour tester des conceptions phytogéographiques et paléoclimatiques relatives au Trias. Les conclusions suivantes sont soulignées: (1) Il y a suffisamment de témoignage palynologique indiquant que la région méditerranéenne renferme un domaine avec un mélange de types de flores septentrionales (laurasiennes) et méridionales (gondwaniennes). (2) L'idée d'une nature essentiellement aride formée d'une large ceinture climatique équatoriale pendant les temps triasiques trouve un soutien palynologique. (3) Le témoignage palynologique ne conteste pas la conception d'une diminution manifeste des précipitations vers la partie occidentale de la région méditerranéenne. (4) En Europe, la présence de palynoflores hygrophitiques et de charbons dans une zone climatique aride peut s'expliquer par l'adduction d'eau de systèmes fluviaux de grande extension.
    Notes: Zusammenfassung Zufolge einer vorläufigen Auswertung palynologischer Information über ladinische und besonders karnische Schichtfolgen, scheint es deutliche Anzeichen zu geben, daß qualitative und quantitative Unterschiede in der Zusammensetzung palynologischer Assoziationen gut angewandt werden könnten beim Testen der Konzepte von triassischer Phytogeografie und Paläoklimatologie. Untenstehende Implikationen werden betont: (1) Es gibt genügend palynologischen Beweis, daß das Mittelmeergebiet auch einen Bereich enthält, der von gemischten, nördlichen (laurasischen) und südlichen (gondwanischen) Floratypen charakterisiert ist. (2) Das Konzept einer wesentlich ariden Natur einer breiten äquatorialen Zone wähwährend der Trias wird durch palynologische Forschung unterstützt. (3) Palynologische Daten wiedersprechen nicht dem Konzept, daß es eine ausgesprochene Abnahme von Niederschlag in westliche Richtung des Mittelmeergebiets gab. (4) In Europa kann die Anwesenheit von hygrophytischen Palynofloren und Kohlen in einer ariden klimatischen Zone erklärt werden durch die Wasserzufuhr von extensiven Flußsystemen.
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  • 4
    ISSN: 0016-7835
    Keywords: Key words Climate change ; CO2 ; Vegetation ; atmosphere interaction ; Stomatal density ; Stomatal index
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  The majority of the water flux from the earth’s land surface to the atmosphere passes through the tiny pores (stomata) in the leaves of land plants. The maximum conductance to diffusion of the leaves, determined by the number and geometry of stomata, has a profound effect on the terrestrial water and energy balance. Among tree species, there is ever increasing evidence that anthropogenic increase in atmospheric CO2 concentrations results in a decrease in stomatal frequency. The rate of historical CO2 responsiveness of individual tree species can be used to calibrate empirical models of non-linear (sigmoid) stomatal frequency response to CO2 increase. Modelled response curves for European tree birches (Betula pendula, Betula pubescens) and Durmast oak (Quercus petraea) predict different response limits to CO2 increase (∼350 and ∼400 ppmv, respectively), indicating that non-linear stomatal frequency responses may vary from one tree species to another. Information on a wider selection of species is needed, but the models suggest that the maximum effect of anthropogenic CO2 increase on stomatal frequency has already been reached. Further research is required to establish the effect of rapidly declining response rates on future stomatal conductance of the ecologically contrasting trees of boreal, temperate, subtropical and tropical forests.
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  • 5
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    In:  Mededelingen van het Botanisch Museum en Herbarium van de Rijksuniversiteit te Utrecht (2352-5754) vol.262 (1966) nr.2 p.316
    Publication Date: 2015-05-08
    Description: The Upper Hunter palynological assemblage described includes 54 species, assigned to 29 genera. Seven genera (Scabratisporites, Guttatisporites, Lapposisporites, Pseudogravisporites, Paralundbladispora, Taeniaepollenites and Tubantiapollenites) and 39 species are new; three generic descriptions are emended (Apiculatasporites, Colpectopollis and Angustisulcites) and three new combinations are proposed. Bisaccate pollen grains average 84 %; within this group no Upper Permian elements could be demonstrated. The assemblage is compared with other European Lower and Middle Triassic assemblages; there are no close similarities to assemblages outside Europe.
    Repository Name: National Museum of Natural History, Netherlands
    Type: Article / Letter to the editor
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  • 6
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    In:  Mededelingen van het Botanisch Museum en Herbarium van de Rijksuniversiteit te Utrecht (2352-5754) vol.307 (1968) nr.1 p.161
    Publication Date: 2015-05-08
    Description: A palynological assemblage obtained from marly limestones of the Dutch Lower Muschelkalk is discussed. A qualitative analysis has disclosed its great resemblance to Upper Bunter (Röt) assemblages ; however, differences in quantitative composition were demonstrated. Utilizing palynological data new information can be added to the knowledge of the European Middle Triassic flora.
    Repository Name: National Museum of Natural History, Netherlands
    Type: Article / Letter to the editor
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  • 7
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    In:  Mededelingen van het Botanisch Museum en Herbarium van de Rijksuniversiteit te Utrecht (2352-5754) vol.290 (1967) nr.1 p.151
    Publication Date: 2015-05-08
    Description: Both paleomagnetism and palynology may furnish useful diagnostic facts for recognizing long-distance movements of the earth’s crust. With respect to the relative positions of North America and Eurasia, paleomagnetic and palynological data contribute evidence in support of the theory of continental drift. However, the conclusions based on paleomagnetic measurements sometimes disagree with palynological observations. Paleomagnetic data obtained in northeastern Italy, southern France and northern Spain differ considerably from those from Mesc-Europe. In recent geotectonical considerations this has been attributed to the so-called Tethys twist having effected a post-Carboniferous westward displacement of the structural units of Italy, southern France and Spain. Palynology, however, reveals a highly uniform geological history of both Meso-Europe and a part of Alpine Europe during Permian and Triassic times. Biostratigraphical correlations between the two realms are possible by studying the palynological assemblages obtained from Permian and Triassic evaporites or associated sediments. Contemporaneous, short periods of evaporite deposition in both Meso-Europe and the Mediterranean region are suggested by the striking uniformities in Lower Mesophytic vegetations as reflected by sporae dispersae. There is every indication that there was a comparable evolution in the physiographical and climatological conditions which opposes the hypothesis of a mobile Tethys belt during Permian and Triassic times.
    Repository Name: National Museum of Natural History, Netherlands
    Type: Article / Letter to the editor
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  • 8
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    In:  Mededelingen van het Botanisch Museum en Herbarium van de Rijksuniversiteit te Utrecht (2352-5754) vol.296 (1968) nr.1 p.71
    Publication Date: 2015-06-04
    Description: The recognition of both Thuringian macroscopic plant remains ( Ullmannia bronni, Ullmannia frumentaria, Quadrocladus orobiformis, etc.) and miospores (Lueckisporites virkkiae, Nuskoisporites dulhuntyi, Falcisporites zapfei, Klausipollenites schaubergeri, etc.) in the Upper Palaeozoic deposits of the Estérel evidences the presence of Upper Permian sediments as well as an important centre of Late Permian volcanic activity in southern France.
    Repository Name: National Museum of Natural History, Netherlands
    Type: Article / Letter to the editor
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  • 9
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    In:  Mededelingen van het Botanisch Museum en Herbarium van de Rijksuniversiteit te Utrecht vol. 296 no. 1, pp. 71-83
    Publication Date: 2024-01-12
    Description: The recognition of both Thuringian macroscopic plant remains ( Ullmannia bronni, Ullmannia frumentaria, Quadrocladus orobiformis, etc.) and miospores (Lueckisporites virkkiae, Nuskoisporites dulhuntyi, Falcisporites zapfei, Klausipollenites schaubergeri, etc.) in the Upper Palaeozoic deposits of the Est\xc3\xa9rel evidences the presence of Upper Permian sediments as well as an important centre of Late Permian volcanic activity in southern France.
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 10
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    In:  Mededelingen van het Botanisch Museum en Herbarium van de Rijksuniversiteit te Utrecht vol. 290 no. 1, pp. 151-166
    Publication Date: 2024-01-12
    Description: Both paleomagnetism and palynology may furnish useful diagnostic facts for recognizing long-distance movements of the earth\xe2\x80\x99s crust. With respect to the relative positions of North America and Eurasia, paleomagnetic and palynological data contribute evidence in support of the theory of continental drift. However, the conclusions based on paleomagnetic measurements sometimes disagree with palynological observations. Paleomagnetic data obtained in northeastern Italy, southern France and northern Spain differ considerably from those from Mesc-Europe. In recent geotectonical considerations this has been attributed to the so-called Tethys twist having effected a post-Carboniferous westward displacement of the structural units of Italy, southern France and Spain.\nPalynology, however, reveals a highly uniform geological history of both Meso-Europe and a part of Alpine Europe during Permian and Triassic times. Biostratigraphical correlations between the two realms are possible by studying the palynological assemblages obtained from Permian and Triassic evaporites or associated sediments. Contemporaneous, short periods of evaporite deposition in both Meso-Europe and the Mediterranean region are suggested by the striking uniformities in Lower Mesophytic vegetations as reflected by sporae dispersae. There is every indication that there was a comparable evolution in the physiographical and climatological conditions which opposes the hypothesis of a mobile Tethys belt during Permian and Triassic times.
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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