ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

Language
Number of Hits per Page
Default Sort Criterion
Default Sort Ordering
Size of Search History
Default Email Address
Default Export Format
Default Export Encoding
Facet list arrangement
Maximum number of values per filter
Auto Completion
Topics (search only within journals and journal articles that belong to one or more of the selected topics)
Feed Format
Maximum Number of Items per Feed
feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
Collection
Language
  • 1
    Monograph available for loan
    Monograph available for loan
    London : The Geological Society
    Associated volumes
    Call number: 9/M 99.0386 ; AWI G5-00-0204
    In: Geological Society special publication
    Description / Table of Contents: This book contains a co-ordinated series of papers considering how chemical changes in sediments, as they accumulate and lithify, affect their magnetization and how such changes can be monitored by studying their magnetic properties. It is especially relevant to sedimentologists, particularly those in exploration for hydrocarbons and sediment-hosted metals, as well as for geophysicists using the magnetization of sediments.
    Type of Medium: Monograph available for loan
    Pages: 214 S. , Ill., graph. Darst.
    ISBN: 1862390282
    Series Statement: Geological Society special publication 151
    Classification:
    Geomagnetism, Geoelectromagnetism
    Note: D. H. Tarling: Introduction: sediments and diagenesis / Geological Society, London, Special Publications, 151:1-8, doi:10.1144/GSL.SP.1999.151.01.21 --- C. M. Batt: Preliminary investigations into the acquisition of remanence in archaeological sediments / Geological Society, London, Special Publications, 151:9-19, doi:10.1144/GSL.SP.1999.151.01.02 --- S. A. Pisarevsky: Studies of post-depositional remanent magnetization and their relevance to the palaeomagnetic record / Geological Society, London, Special Publications, 151:21-26, doi:10.1144/GSL.SP.1999.151.01.03 --- Graham J. Borradaile: Viscous remanent magnetization of high thermal stability in limestone / Geological Society, London, Special Publications, 151:27-42, doi:10.1144/GSL.SP.1999.151.01.04 --- Barbara A. Maher and Mark W. Hounslow: The significance of magnetotactic bacteria for the palaeomagnetic and rock magnetic record of Quaternary sediments and soils / Geological Society, London, Special Publications, 151:43-46, doi:10.1144/GSL.SP.1999.151.01.05 --- Shmuel Marco, Hagai Ron, Michael O. McWilliams, and Mordechai Stein: The locking-in of remanence in upper Pleistocene sediments of Lake Lisan (palaeo Dead Sea) / Geological Society, London, Special Publications, 151:47-52, doi:10.1144/GSL.SP.1999.151.01.06 --- J. Dinarès-Turell and M. J. Dekkers: Diagenesis and remanence acquisition in the Lower Pliocene Trubi marls at Punta di Maiata (southern Sicily): palaeomagnetic and rock magnetic observations / Geological Society, London, Special Publications, 151:53-69, doi:10.1144/GSL.SP.1999.151.01.07 --- L. Vigliotti, L. Capotondi, and M. Torii: Magnetic properties of sediments deposited in suboxic-anoxic environments: relationships with biological and geochemical proxies / Geological Society, London, Special Publications, 151:71-83, doi:10.1144/GSL.SP.1999.151.01.08 --- Michael Urbat, Mark J. Dekkers, and Simon P. Vriend: The isolation of diagenetic groups in marine sediments using fuzzy c-means cluster analyses / Geological Society, London, Special Publications, 151:85-93, doi:10.1144/GSL.SP.1999.151.01.09 --- Gary S. Wilson and Andrew P. Roberts: Diagenesis of magnetic mineral assemblages in multiply redeposited siliciclastic marine sediments, Wanganui basin, New Zealand / Geological Society, London, Special Publications, 151:95-108, doi:10.1144/GSL.SP.1999.151.01.10 --- P. Turner, P. Chandler, D. Ellis, G. P. Leveille, and M. L. Heywood: Remanence acquisition and magnetostratigraphy of the Leman Sandstone Formation: Jupiter Fields, southern North Sea / Geological Society, London, Special Publications, 151:109-124, doi:10.1144/GSL.SP.1999.151.01.11 --- E. A. Hailwood, D. Bowen, F. Ding, P. W. M. Corbett, and P. Whattler: Characterizing pore fabrics in sediments by anisotropy of magnetic susceptibility analyses / Geological Society, London, Special Publications, 151:125-126, doi:10.1144/GSL.SP.1999.151.01.12 --- F. Hrouda and J. Ježek: Magnetic anisotropy indications of deformations associated with diagenesis / Geological Society, London, Special Publications, 151:127-137, doi:10.1144/GSL.SP.1999.151.01.13 --- Graham J. Borradaile, Philip W. Fralick, and France Lagroix: Acquisition of anhysteretic remanence and tensor subtraction from AMS isolates true palaeocurrent grain alignments / Geological Society, London, Special Publications, 151:139-145, doi:10.1144/GSL.SP.1999.151.01.14 --- B. D’Argenio, V. Ferreri, M. Iorio, A. Raspini, and D. H. Tarling: Diagenesis and remanence acquisition in the Cretaceous carbonate sediments of Monte Raggeto, southern Italy / Geological Society, London, Special Publications, 151:147-156, doi:10.1144/GSL.SP.1999.151.01.15 --- Emő Márton: Diagenesis in platform carbonate rocks: a palaeomagnetic study of an upper Triassic-lower Jurassic section, Tata (Hungary) / Geological Society, London, Special Publications, 151:157-165, doi:10.1144/GSL.SP.1999.151.01.16 --- Alla Shogenova: The influence of dolomitization on the magnetic properties of Lower Palaeozoic carbonate rocks in Estonia / Geological Society, London, Special Publications, 151:167-180, doi:10.1144/GSL.SP.1999.151.01.17 --- Herbert Haubold: Alteration of magnetic properties of Palaeozoic platform carbonate rocks during burial diagenesis (Lower Ordovician sequence, Texas, USA) / Geological Society, London, Special Publications, 151:181-203, doi:10.1144/GSL.SP.1999.151.01.18 --- Glossary / Geological Society, London, Special Publications, 151:205-208, doi:10.1144/GSL.SP.1999.151.01.19
    Location: Reading room
    Location: Reading room
    Branch Library: GFZ Library
    Branch Library: AWI Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2022-05-25
    Description: Author Posting. © National Academy of Sciences, 2006. This article is posted here by permission of National Academy of Sciences for personal use, not for redistribution. The definitive version was published in Proceedings of the National Academy of Sciences of the United States of America 103 (2006): 1342-1346, doi:10.1073/pnas.0503198103.
    Description: Recent observations of changes in some tundra ecosystems appear to be responses to a warming climate. Several experimental studies have shown that tundra plants and ecosystems can respond strongly to environmental change, including warming; however, most studies were limited to a single location and were of short duration and based on a variety of experimental designs. In addition, comparisons among studies are difficult because a variety of techniques have been used to achieve experimental warming and different measurements have been used to assess responses. We used metaanalysis on plant community measurements from standardized warming experiments at 11 locations across the tundra biome involved in the International Tundra Experiment. The passive warming treatment increased plant-level air temperature by 1-3°C, which is in the range of predicted and observed warming for tundra regions. Responses were rapid and detected in whole plant communities after only two growing seasons. Overall, warming increased height and cover of deciduous shrubs and graminoids, decreased cover of mosses and lichens, and decreased species diversity and evenness. These results predict that warming will cause a decline in biodiversity across a wide variety of tundra, at least in the short term. They also provide rigorous experimental evidence that recently observed increases in shrub cover in many tundra regions are in response to climate warming. These changes have important implications for processes and interactions within tundra ecosystems and between tundra and the atmosphere.
    Description: The projects represented here were supported by many sources, including the National Science Foundation, Swedish Natural Science Research Council, United Kingdom Natural Environment Research Council, Natural Sciences and Engineering Research Council of Canada, Research Council of Norway, Icelandic Centre for Research, and the Academy of Finland. Coordination of activities was made possible with support from the Bonanza Creek Long-Term Ecological Research site.
    Keywords: Arctic and alpine ecosystems ; Biodiversity ; Climate change ; Vegetation change
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: 353582 bytes
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Biochemistry 28 (1989), S. 628-635 
    ISSN: 1520-4995
    Source: ACS Legacy Archives
    Topics: Biology , Chemistry and Pharmacology
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 4
    ISSN: 1520-5126
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Mineralium deposita 13 (1978), S. 245-258 
    ISSN: 1432-1866
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The Marl Slate, the English equivalent of the Kupferschiefer, has been studied with particular reference to the relationships between dolomitization and the origin of the metal sulphides. Dolomite occurs as: 1) discontinuous lenses of ferroan dolomicrite, 2) micronodules of finely crystalline dolospar in association with length-slow chalcedony and 3) discrete laminae of ferroan or non-ferroan dolospar. The ferroan dolomicrite has excess CaCO3, and is more abundant in the lower, sapropelic facies of the Marl Slate. It is considered to have formed by the penecontemporaneous alteration of calcium carbonate under hypersaline conditions. Small micronodules (typically about 0.3 mm in diameter) are also more abundant in the sapropelic Marl Slate. These frequently contain cores of length-slow chalcedony (quartzine) fibres and sometimes quartz megacrysts. Textural observations clearly indicate that this silica is of authigenic origin and the dolomite/chalcedony micronodules are interpreted as diagenetic replacements of a calcium sulphate mineral such as anhydrite. The discrete laminae of finely crystalline dolospar are often inter-laminated with calcite in the upper part of the Marl Slate. This dolomite is also calcium rich and represents a replacement, possibly of anhydrite, during a later phase of diagenesis. Metal sulphides occur in two distinct forms: as disseminated framboidal pyrite and as discrete lenses of pyrite, chalcopyrite, galena, sphalerite and rarer sulphides. The framboidal pyrite originated during early diagenesis by reaction of sulphide, produced by reduction of sulphate by organic material and micro-organisms, with iron also released in the reducing environment. The sulphide lenses are often in intimate association with dolospar, length-slow chalcedony and authigenic quartz megacrysts. This indicates that the lenses were produced during diagenesis by the reduction and replacement of calcium sulphate (anhydrite). Various sources, such as co-precipitation with dolomite precursors and the underlying Yellow Sands, may have supplied metals which were mobilized and transported by connate brines as diagenesis progressed.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 6
    ISSN: 1432-1866
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Continental red beds are the host rocks of a characteristic style of mineralization which suggests a genetic link between red bed formation and ore formation. Samples of unmineralized and mineralized Triassic sediments from Central England have been studied sedimentologically, petrographically and geochemically with the aim of clarifying this link which may provide valuable guides for exploration. On the basis of sedimentological and petrographic observations it is suggested that these red beds were formed as a result of diagenetic alteration whereby detrital silicates and oxides are progressively dissolved and the iron released is deposited as hematite. A model for mineralization is proposed involving the release of trace metals from detrital minerals during diagenesis, their retention in saline interstitial solutions, migration to suitable sites of precipitation and deposition by reaction with trapped hydrocarbons or reduced sulphur.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 7
    Electronic Resource
    Electronic Resource
    Springer
    European journal of clinical pharmacology 8 (1975), S. 107-113 
    ISSN: 1432-1041
    Keywords: Aspirin ; indomethacin ; plasma levels ; dissolution ; interaction ; toxicity
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Medicine
    Notes: Summary Plasma indomethacin levels have been compared in 10 subjects following 100 mg of indomethacin from two different formulations, with similar disintegration and dissolution profiles. In four of these ten subjects plasma indomethacin levels were estimated after pretreatment with, and concurrent administration of, a buffered aspirin. The percentage of protein binding of indomethacin in the presence of salicylate was also estimated. No significant differences between peak plasma indomethacin levels with or without buffered aspirin were detected, but the rate of indomethacin absorption as shown by plasma levels, was significantly increased by pretreatment with and concurrent administration of, buffered aspirin. This was associated with a marked increase in side effects.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 8
    Electronic Resource
    Electronic Resource
    Springer
    European journal of clinical pharmacology 28 (1985), S. 483-483 
    ISSN: 1432-1041
    Keywords: atenolol ; red blood cells ; deformability
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Medicine
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 9
    Electronic Resource
    Electronic Resource
    Springer
    European journal of clinical pharmacology 14 (1978), S. 83-85 
    ISSN: 1432-1041
    Keywords: Propranolol ; oxprenolol ; noradrenalineduced vasoconstriction
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Medicine
    Notes: Summary The effects of oxprenolol and propranolol on the venoconstrictor response to noradrenaline were studied in healthy volunteers by measuring superficial dorsal hand vein diameter at a standard congesting pressure. In 8 subjects dose response curves to noradrenaline (20–1280 ng/ml) were obtained with noradrenaline alone, with noradrenaline plus propranolol 10 µg/ml, with noradrenaline plus propranolol 10 µg/ml plus oxprenolol 3 µg/ml and with noradrenaline plus propranolol 13 µg/ml according to a double blind balanced randomised design. Propranolol 10 µg/ml significantly (P〈0.05) potentiated the vasoconstrictor response to noradrenaline and the addition of oxprenolol significantly (P〈0.05) reversed the potentiation giving a response similar to that seen with noradrenaline alone. The higher concentration of propranolol did not produce further potentiation, the response being similar to that obtained with the lower concentration of propranolol. It is suggested that the effect of oxprenolol may be attributable to alpha blocking properties, to partial beta agonism or to its membrane stabilising properties.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 10
    Electronic Resource
    Electronic Resource
    Springer
    European journal of clinical pharmacology 23 (1982), S. 435-440 
    ISSN: 1432-1041
    Keywords: erythromycin ; haemodialysis ; dosage adjustment ; pharmacokinetics ; protein-binding
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Medicine
    Notes: Summary Erythromycin kinetics were studied in 17 patients with end stage renal failure treated with maintenance haemodialysis and 9 normal volunteers to discover if dialysis patients needed a modified dose. The elimination half life in dialysis patients (on dialysis days) was similar to that reported in normal subjects. Only small amounts of drug appeared in the dialysate, no patient loosing more than 9 mg in one dialysis. Both patients and volunteers had similar plasma concentrations 8 h after the end of a 5-day course. Protein-binding did not change significantly during dialysis and was similar to that reported in normal subjects. We conclude that dialysis patients requiring 1.5 g of erythromycin stearate daily or less can be given normal doses.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...