TY - JOUR A1 - Schneider, Ingo T1 - Variante Pflanzen aus Gewebekulturen : Mutation oder epigenetische Veränderungen? Y1 - 1991 ER - TY - JOUR A1 - Schneider, Ingo A1 - Köhler, Brigitte T1 - Amitrole tolerance in cell and tissue cultures and regenerated plants from Nicotiana plumbaginifolia : II. Selection system: suspension culture Y1 - 1992 ER - TY - JOUR A1 - Schneider, Ingo T1 - Zusammensetzung der Mikrobionta auf Rieselfelderböden Y1 - 1992 ER - TY - JOUR A1 - Schneider, Ingo T1 - Untersuchungen zur Dynamik, physiologischen Aktivitäten und ökologischen Bedeutung ausgewählter Mikroorganismengruppen in Rieselfeldböden Y1 - 1992 ER - TY - GEN A1 - Altenberger, Uwe T1 - Stress-induced natural transformation of ortho- to clinohypersthene in metagabbros of the Ivrea Zone, Northern Italy N2 - Orthopyroxenes of a high temperature protomylonite of the Ivrea Zone, Northern Italy show twin like polysynthetic lamellae parallel to {210} of the hypersthene host. The transformation is caused by plastic deformation under high metamorphic conditions which has resulted in dynamic recrystallization of pyroxene and plagioclase. The lamellae consist of clinohypersthene. The twin plane and the lamellar clino-orthoinversion of hypersthene due to natural deformation have not been described hitherto. N2 - Orthopyroxene aus hoch temperierten Protomyloniten der Ivrea-Zone, Nord Italien zeigen polysynthetische Lamellen parallel {210} des Wirtes. Ihr Erscheinungsbild entspricht Deformationszwillingen. Die Lamellen sind invertiert zu Klinohypersthen. Die Ortho-Klino-Transformation ist auf eine Hochtemperaturdeformation zurückzuführen, wie dies anhand der dynamischen Rekristallisation der Pyroxene und Plagioklase bewiesen werden kann. Weder die speziellen Verwachsungsflächen noch die Ortho-Klino-Inversion durch natürliche Deformation wurden bisher beschrieben. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - paper 099 Y1 - 1992 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus-40778 ER - TY - BOOK ED - Wallschläger, Hans-Dieter T1 - OTIS : Zeitschrift der Arbeitsgemeinschaft Berlin-Brandenburgischer Ornithologen Y1 - 1993 ER - TY - BOOK ED - Pötsch, Joachim ED - Weinert, Erich T1 - Botanische Wanderungen in deutschen Ländern : [Die schönsten Exkursionen] Y1 - 1993 PB - Urania-Verl. CY - Leipzig [u.a.] ER - TY - JOUR A1 - Schneider, Ingo A1 - Müller, Bernd A1 - Wilke, U.-B T1 - Saisonal variation of microorganisms in a sewage farm ares south of Berlin Y1 - 1993 ER - TY - JOUR A1 - Budzinski, Hubertus A1 - Rötzler, Jochen A1 - Budzinski, Gertraud T1 - Evidence for early variscan very high temperature (1000o C) - high pressure metamorphism of garnet- clinopyroxene granulites in the Saxon Granulite Massif, Germany Y1 - 1994 ER - TY - GEN A1 - Elsenbeer, Helmut A1 - West, Adam A1 - Bonell, Mike T1 - Hydrologic pathways and stormflow hydrochemistry at South Creek, northeast Queensland N2 - Earlier investigations at South Creek in northeastern Queensland established the importance of overland flow as a hydrologic pathway in this tropical rainforest environment. Since this pathway is ‘fast’, transmitting presumably ‘new’ water, its importance should be reflected in the stormflow chemistry of South Creek: the greater the volumentric contribution to the stormflow hydrograph, the more similarity between the chemical composition of streamwater and of overland flow is to be expected. Water samples were taken during two storm events in an ephemeral gully (gully A), an intermittent gully (gully B) and at the South Creek catchment outlet; additional spot checks were made in several poorly defined rills. The chemical composition of ‘old’ water was determined from 45 baseflow samples collected throughout February. The two events differed considerably in their magnitudes, intensities and antecedent moisture conditions. In both events, the stormflow chemistry in South Creek was characterized by a sharp decrease in Ca, Mg, Na, Si, Cl, EC, ANC, alkalinity and total inorganic carbon. pH remained nearly constant with discharge, whereas K increased sharply, as did sulfate in an ill-defined manner. In event 1, this South Creek stormflow pattern was closely matched by the pattern in gully A, implying a dominant contribution of ‘new’ water. This match was confirmed by the spot samples from rills. Gully B behaved like South Creek itself, but with a dampened ‘new’ water signal, indicating less overland flow generation in its subcatchment. In event 2, which occurred five days later, the initial ‘new’ water signal in gully A was rapidly overwhelmed by a different signal which is attributed to rapid drainage from a perched water table. This study shows that stormflow in this rainforest catchment consists predominantly of ‘new’ water which reaches the stream channel via ‘fast’ pathways. Where the ephemeral gullies delivering overland flow are incised deeply enough to intersect a perched water table, a delayed, ‘old’ water-like signal may be transmitted. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - paper 046 Y1 - 1994 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus-16904 ER -