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  • 2010-2014  (463)
  • 1995-1999  (231)
  • 1950-1954  (8)
  • 1935-1939  (12)
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  • 1
    Call number: 9/M 16.89728
    Description / Table of Contents: Seit der ersten Auflage 1964 hat sich dieses Werk als Standardwerk etabliert und liegt nun in vollständig neu bearbeiteter und aktualisierter 5. Auflage vor. Diese berücksichtigt die umfangreichen Forschungsergebnisse seit Erscheinen der 4. Aufl. (1991) und fasst den aktuellen geologischen Kenntnisstand in einem einzigen Band zusammen. Auf die einleitende Darstellung der mehr als zwei Jahrhunderte umfassenden Erforschungsgeschichte folgt eine Übersicht der Naturräume, des allgemeinen geologischen Aufbaus und der erdgeschichtlichen Entwicklung Baden-Württembergs. Den Hauptteil des Buches bildet — wie in den vorherigen Auflagen — die detaillierte Darstellung der Gesteinsfolge des Landes und ihrer regionalen Faziesentwicklungen. Dem Grundgebirge, dem nicht-metamorphen Paläozoikum sowie dem Tertiär und der landschaftsgeschichtlichen Entwicklung wird breiterer Raum gegeben als in früheren Auflagen. Erstmals wird dabei die aktuell gültige, in den vergangenen Jahren länderübergreifend abgestimmte stratigraphische Nomenklatur verwendet. Sedimentations- und Klimageschichte sowie die tektonische Entwicklung des Landesgebietes werden ebenfalls ausführlicher erläutert. Dabei werden die Zusammenhänge zwischen der Geologie Baden-Württembergs und benachbarter Regionen berücksichtigt. Abschließend sind den Wechselbeziehungen zwischen menschlicher Tätigkeit und ihren geologischen Voraussetzungen eigene Kapitel gewidmet.
    Type of Medium: Monograph available for loan
    Pages: X, 627 S. , Ill., graph. Darst., Kt.
    Edition: 5., völlig neu bearb. Aufl.
    ISBN: 9783510652679
    Language: German
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Weimar : Thüringer Landesanstalt für Geologie [u.a.]
    Call number: M 00.0352
    Type of Medium: Monograph available for loan
    Pages: 188 S. + 1 Faltbl., 1 Kt.-Beil.
    ISBN: 3980681114
    Series Statement: Naturschutz im Wartburgkreis 8/1999
    Classification:
    Regional Geology
    Language: German
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 3
    Series available for loan
    Series available for loan
    Stuttgart : Inst. für Geologie und Paläontologie, Univ. Stuttgart
    Associated volumes
    Call number: S 90.0060(16)
    In: Profil
    Type of Medium: Series available for loan
    Pages: 377 S.
    Series Statement: Profil 16
    Classification:
    A.3.1.
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 4
    Monograph available for loan
    Monograph available for loan
    Köln : Inst. für Geophysik und Meteorologie
    Associated volumes
    Call number: ZSP-560-118
    In: Mitteilungen aus dem Institut für Geophysik und Meteorologie der Universität zu Köln
    Type of Medium: Monograph available for loan
    Pages: 117 S. : Abb. ; 21 cm
    ISSN: 0069-5882
    Series Statement: Mitteilungen aus dem Institut für Geophysik und Meteorologie der Universität zu Köln 118
    Language: German
    Branch Library: GFZ Library
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  • 5
    Call number: S 93.0569(25)
    In: Beringeria
    Type of Medium: Series available for loan
    Pages: 173 S.
    Series Statement: Beringeria 25
    Classification:
    Regional Geology
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Glycoconjugate journal 14 (1997), S. 785-793 
    ISSN: 1573-4986
    Keywords: glycoprotein ; glycosylation ; gp120 ; HIV ; MALDI-TOF-MS
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology
    Notes: Abstract Neutral complex-type N-glycans of the envelope glycoprotein 120 of HIV-2, propagated in different host cells, display cell-type specific variations. In order to identify typical structural elements, glycans were analysed by gel filtration, by enzymic sequencing and, in part, by matrix-assisted laser desorption/ionization time-of-flight mass spectrometry. The characteristic substituents of di- tri- and tetraantennary carbohydrate units thus observed include N-acetyllactosamine repeats, bisecting N-acetylglucosamine and fucose linked to the chitobiose core as well as to N-acetyllactosamine antennae. Each glycoprotein preparation displayed a characteristic set of glycoforms. Abbreviations: endo H, endo-β-N-acetylglucosaminidase H; E-PHA, Phaseolus vulgaris agglutinin E4; GlcNAcOH, N-acetyl-glucosaminitol; gp120/HUT78(MOLT4/Mφ/PBL/U937), external envelope glycoprotein 120 of HIV-2, strain D194, propagated in HUT78 (MOLT4, Mφ, PBL, U937) cells; gu, glucose units; HPAEC, high-pH anion-exchange chromatography; MALDI-TOF-MS, matrix-assisted laser desorption/ionization time-of-flight mass spectrometry; Mφ, human monocytes/macrophages; PBL, human peripheral blood lymphocytes; PNGase F, peptide-N4-(N-acetyl-β-glucosaminyl)asparagine amidase F
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Biogeochemistry 47 (1999), S. 219-238 
    ISSN: 1573-515X
    Keywords: dissolved humic substances ; FTIR spectroscopy ; land use history ; peat ; synchronous fluorescence spectroscopy ; UV/VIS spectroscopy
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Notes: Abstract The elemental composition and spectroscopic properties of dissolved fulvic acids isolated from different sampling media (topsoil, ground and surface water) of a natural fen area (high portion of organic soils) were examined to reveal the effects of land use history. These effects need to be known if dissolved humic substances are to be a major factor in identifying the impact of present and future changes in land use. Dissolved fulvic acids (topsoil, groundwater) from highly degraded peatlands (due to a long-term agricultural use) exhibit lower C/N ratios, higher absorption in the UV spectra, and higher absorption at 1,620 cm−1 in the FTIR spectra compared with fulvic acids from relatively intact peatlands. These properties illustrate that long-term agricultural use with high inputs results in increased aromatic structures and a further humification of dissolved fulvic acids due to very strong peat decomposition compared with relatively intact peatlands. Synchronous fluorescence spectra also indicate the higher level of aromatic structures within fulvic acids isolated from sites with long-term agricultural use (high peat decomposition) compared with a land use history resulting in a lower peat decomposition. The different sources of fulvic acids in surface water (precipitation, runoff, interflow, groundwater) are the main reason for these effects not being detected in fulvic acids isolated from surface water. Short-term changes in land use characterized by a transition from crop farming to an unimproved grassland were found not to affect the spectroscopic properties of dissolved fulvic acids. A humification index deduced from the synchronous fluorescence spectra is proposed. We have strong evidence that dissolved humic substances indicate changes in the environmental conditions (both anthropogenic and natural) of wetlands with a high proportion of organic soils.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Biogeochemistry 47 (1999), S. 219-238 
    ISSN: 1573-515X
    Keywords: dissolved humic substances ; FTIR spectroscopy ; land use history ; peat ; synchronous fluorescence spectroscopy ; UV/VIS spectroscopy
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Notes: Abstract The elemental composition and spectroscopic properties of dissolved fulvic acids isolated from different sampling media (topsoil, ground and surface water) of a natural fen area (high portion of organic soils) were examined to reveal the effects of land use history. These effects need to be known if dissolved humic substances are to be a major factor in identifying the impact of present and future changes in land use. Dissolved fulvic acids (topsoil, groundwater) from highly degraded peatlands (due to a long-term agricultural use) exhibit lower C/N ratios, higher absorption in the UV spectra, and higher absorption at 1,620 cm−1 in the FTIR spectra compared with fulvic acids from relatively intact peatlands. These properties illustrate that long-term agricultural use with high inputs results in increased aromatic structures and a further humification of dissolved fulvic acids due to very strong peat decomposition compared with relatively intact peatlands. Synchronous fluorescence spectra also indicate the higher level of aromatic structures within fulvic acids isolated from sites with long-term agricultural use (high peat decomposition) compared with a land use history resulting in a lower peat decomposition. The different sources of fulvic acids in surface water (precipitation, runoff, interflow, groundwater) are the main reason for these effects not being detected in fulvic acids isolated from surface water. Short-term changes in land use characterized by a transition from crop farming to an unimproved grassland were found not to affect the spectroscopic properties of dissolved fulvic acids. A humification index deduced from the synchronous fluorescence spectra is proposed. We have strong evidence that dissolved humic substances indicate changes in the environmental conditions (both anthropogenic and natural) of wetlands with a high proportion of organic soils.
    Type of Medium: Electronic Resource
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  • 9
  • 10
    Publication Date: 1999-11-01
    Print ISSN: 0168-2563
    Electronic ISSN: 1573-515X
    Topics: Chemistry and Pharmacology , Geosciences
    Published by Springer
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