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  • 1
    Monograph available for loan
    Monograph available for loan
    München : Oldenbourg
    Associated volumes
    Call number: MOP Per 719(33,2)
    In: Abhandlungen und Berichte
    Type of Medium: Monograph available for loan
    Pages: 59 S. , Ill.
    Series Statement: Abhandlungen und Berichte / Deutsches Museum 33,2
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 2
    Call number: AWI G5-96-0326
    In: NATO ASI series : I, Global and environmental change, Vol. 17
    Type of Medium: Monograph available for loan
    Pages: XII, 580 Seiten , Illustrationen
    ISBN: 3540575944
    Series Statement: NATO ASI series : I, Global and environmental change 17
    Language: English
    Note: TABLE OF CONTENTS FOREWORD LIST OF AUTHORS AND PARTICIPANTS I - OPERATION OF THE OCEAN-ATMOSPHERE CARBON CYCLE The recent state of carbon cycling through the atmosphere / I. Levin Glacial ocean carbon cycle modeling / Ch. Heinze Glacial-interglacial changes in continental weathering: possible implication for atmospheric CO2 / G. Munhoven and L.M.François II - VARIATIONS OF THE OCEANS CARBON RESERVOIR: FAUNAL VERSUS GEOCHEMCAL RECORDS The relationship between surface water masses, oceanographic fronts and paleoclimatic proxies in surface sediments of the Greenland, Iceland, Norwegian Seas / T. Johannessen, E. Jansen, A. Flatrøy, A. C. Ravelo. - Is there a relationship between atmospheric CO2 and manganese in the ocean? / A. Mangini, H.-J. Rutsch, M. Frank, A. Eisenhauer, J.-D. Eckhardt Benthic foraminiferal assemblages and the δ13C-signal in the Atlantic sector of the Southern Ocean: glacial-to-interglacial contrasts / A. Mackensen, H. Grobe, H.-W. Hubberten, G. Kuhn Foraminiferal population dynamics and stable carbon isotopes / Ch. Hemleben and J. Bijma A comparison of carbon isotopes and cadmium in the modern and glacial maximum ocean: can we account for the discrepancies? / E. A. Boyle Tracer-nutrient correlations in the upper ocean: observational and box model constraints on the use of benthic foraminiferal δ13C and Cd/Ca as paleo-proxies for the intermediate-depth ocean / R. Zahn and R. Keir IIΙ - GEOCHEMISTRY OF THE ORGANIC SEDIMENT FRACTION: CONSTRAINTS ON THE BIOLOGICAL CARBON PUMP Possible early diagenetic alteration of palaeo proxies / G.J. De Lange, B. Van Os, P.A. Pruysers, J.J. Middelburg, D. Castradori, P. Van Santvoort, P.J. Müller, H. Eggenkamp, F.G. Prahl Nitrogen isotope fractionation in the modern ocean: implications for the sedimentary record / J. P. Montoya The use of nitrogen isotopic ratio for reconstruction of past changes in surface ocean nutrient utilization / M.A. Altabet and R. Francois Variations in sedimentary organic δ13C as a proxy for past changes in ocean and atmospheric CO2 concentrations / G. H. Rau Reconstruction of paleoceanic PCO2 levels from carbon isotopic compositions of sedimentary biogenic components /J.P. Jasper and J.M. Hayes Late Quaternary PCO2 variations in the Angola Current: evidence from organic carbon δ13C and alkenone temperatures / P.J. Müller, R. Schneider, G. Ruhland PCO2 variations of equatorial surface water over the last 330,000 years: the δ13C record of organic carbon / L. Westerhausen, M. Sarnthein, U. Struck, H. Erlenkeuser, J. Poynter IV - GEOCHEMICAL AND MICROPALEONTOLOGICAL INDEXES OF PALEO-PRODUCTIVITY Paleoproductivity: flux proxies versus nutrient proxies and other problems concerning the Quaternary productivity record / W.H. Berger, J.C. Herguera, C.B. Lange, R. Schneider From modern flux to paleoflux: assessment from sinking assemblages to thanatocoenosis / K. Takahashi Late Quaternary paleoproductivity variations in the NE and equatorial Atlantic: diatom and Corg evidence / F. Abrantes, K. Winn, M. Sarnthein Glacial-Holocene paleoproductivity off western Australia: a comparison of proxy records / D.C. McCorkle, H. H. Veeh, D.J. Heggie Nutrient, mixing and export indices: A 250 Kyr paleoproductivity record from the western equatorial Pacific / J.C. Herguera Dinoflagellate cysts as paleoproductivity indicators: state of the art, potential, and limits / B. Dale and A. Fjeliså Deep-sea benthic foraminifers: food and bottom water masses / D. Schnitker The history of barium, biogenic silica and organic carbon accumulation in the Weddell Sea and Antarctic Ocean over the last 150,000 years / G. Shimmield, S. Derrick, A. Mackensen, H. Grobe, C. Pudsey SUBJECT INDEX
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 3
    Call number: ZSP-321-15
    In: GEOMAR-Report
    In: Berichte
    Type of Medium: Series available for loan
    Pages: 351 S. ; 30 cm
    Series Statement: GEOMAR-Report 15
    Branch Library: AWI Library
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  • 4
    Monograph available for loan
    Monograph available for loan
    Heidelberg
    Call number: AWI A8-97-0362
    Type of Medium: Monograph available for loan
    Pages: 215 S.
    Note: Heidelberg, Univ., Diss., 1995
    Branch Library: AWI Library
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  • 5
    Call number: S 99.0038(469)
    In: Deutsche Geodätische Kommission bei der Bayerischen Akademie der Wissenschaften
    Type of Medium: Series available for loan
    ISBN: 3769695097
    Series Statement: Deutsche Geodätische Kommission bei der Bayerischen Akademie der Wissenschaften : Reihe C, Dissertationen 469
    Classification:
    Photogrammetry, Remote Sensing
    Language: German
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 6
  • 7
  • 8
    Call number: H G 6635
    In: Veröffentlichungen des Instituts für Meereskunde und des Geographischen Instituts
    Type of Medium: Monograph non-lending collection
    Pages: VI, 89 S. : Ill., 4 Kt.
    Series Statement: Veröffentlichungen des Instituts für Meereskunde und des Geographischen Instituts an der Universität Berlin 10
    Location: Pendulum room
    Branch Library: GFZ Library
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  • 9
    Series available for loan
    Series available for loan
    Warnemünde : Inst. für Ostseeforschung
    Associated volumes
    Call number: ZS-000(3)
    In: Meereswissenschaftliche Berichte
    Type of Medium: Series available for loan
    Pages: 59 S.
    Series Statement: Meereswissenschaftliche Berichte 3
    Language: German
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 10
    ISSN: 1432-041X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Description / Table of Contents: Zusammenfassung Die Untersuchungen wurden mit Eiern und Embryonen des Seeigels Sphaerechinus granularis Lam. durchgeführt, die bei 22° C unter sedimentationsverhinderndem Rühren und Belüftung bis zu 45 Std gehalten wurde. Die Änderung des DNA-Gehaltes, die Änderung der DNA-Polymerase Aktivitäten und die Änderung der DNase-Aktivitäten wurden als zeitabhängige Geschehnisse untersucht. 1. DNA-Gehalt der Embryonen. In den Embryonen wurde der DNA-Gehalt mit zwei verschiedenen Methoden bestimmt. Vor und unmittelbar nach der Befruchtung wurden DNA-Gehalte von 1,7±0,5·10−10 g pro Ei gefunden. Diese DNA-Menge entspricht dem 100fachen des diploiden Zellkernes. Drei Perioden unterschiedlicher DNA Syntheseraten können herausgestellt werden: Eine erste, die etwa mit dem Volumenmaximum im Blastula-Stadium erreicht ist, mit einer mittleren Synthesegeschwindigkeit von 1,2·10−2 g DNA pro Minute pro Embryo; eine zweite Periode, von dem vorherigen Punkt bis zum Erreichen des Gastrula-Stadiums, zeigt eine geringere Synthesegeschwindigkeit als die im ersten Abschnitt ablaufende, mit ca. 0,7·10−12 g DNA pro Minute pro Embryo; dieser folgt eine dritte, bis zum Ende der von uns gewählten Untersuchungsdauer im Pluteus-Stadium mit einer Synthese-geschwindigkeit von 2,3·10−12 g DNA pro Minute pro Embryo. Die relativen Synthesegeschwindigkeiten verhalten sich wie 100∶58∶192. Die cytoplasmatische, extramitochondriale DNA bleibt während der Anfangsphase der Entwicklung bis zum Blastula-Stadium erhalten. Die extranucleäre DNA nimmt in den ersten 6 Std der Entwicklung des Embryos sogar noch zu, um anschließend zu verschwinden. 2. DNA-abhängige DNA-Polymerase-Aktivität. Die DNA-Polymerase wurde aus den Embryonen isoliert, ihre Aktivität bestimmt und auf einen Embryo bzw. eine Zelle bezogen. Dabei war die Polymerase-Aktivität zu Beginn der Embryogenese wesentlich höher als in späteren Entwieklungsstadien. Die Polymerase-Aktivität durchläuft während des Blastula-Stadiums ein Minimum zu dem Zeitpunkt, an dem die cytoplasmatische DNA in den Embryonen aufgebraucht ist. In der anschließenden Entwicklungsphase ist die Höhe der DNA Polymerase-Aktivität proportional der DNA Syntheserate in vivo; dabei bleibt der Wert für die DNA Polymerase-Aktivität pro Zelle konstant. 3. DNA-abbauende Aktivität. Die DNase Aktivität im alkalischen Bereich wurde mit der Lanthan-Nitrat-Methode bestimmt, wobei sich drei sehr deutliche Maxima zeigen. Das erste Maximum findet sich unmittelbar nach der Bespermung, das zweite fällt mit der Mesenchymbildung während der Blastula zusammen und das dritte korrespondiert mit dem Ende der Gastrulation. Die durchschnittliche spezifische Aktivität ergibt sich zu etwa 10−6 g DNase I Äquivalent/g Embryo. Die Möglichkeiten, ob die Aktivitätsmaxima dieser nucleolytischen Enzyme jeweils Differenzierungsvorgänge in den Keimen einleiten, werden diskutiert. Abschließend wird der Einfluß der in vitro bestimmten DNA-Polymerase-Aktivität und der DNase-Aktivität auf die in vivo ablaufende DNA-Syntheserate diskutiert.
    Notes: Summary The investigations were performed with the eggs of the sea urchin speciesSphaerechinus granularis Lam. They were kept at 22° C under continuous aeration for up to 45 hours with stirring to compensate for sedimentation. 1. The change in DNA content, 2. the change in DNA dependent DNA polymerase activity, and 3. the change in DNase activity with time have been evaluated. 1. DNA Content of Embryos. The DNA content of the embryo development was determined by two different methods. Before and immediately after fertilization DNA content has been found to be 1.7±0.5·10−10 g per egg. This amount is about 100 times higher than in diploid nuclei. Three periods with different rates of DNA synthesis may be distinguished: a) the first one, lasting from fertilization to about the time of the volume maximum just before the onset of gastrulation with an average rate of synthesis of 1.2·10−10g DNA per minute per embryo; b) a second one, lasting from then on to the gastrula stage with a lower average rate of synthesis of about 0.7·10−12 g DNA per minute per embryo; c) a third one, starting from the gastrula stage up to the experimental end point in the pluteus stage. The rate of synthesis in this case is 2.3·10−12 g DNA per minute per embryo. On a relative base the rates of synthesis are 100∶58∶192. The cytoplasmic, extramitochondrial DNA persists through the stage of the first period of the embryogenesis, up to the blastula stage. The amount of extranuclear DNA increases in the first 6 hours of embryo development; then the cytoplasmic DNA disappears. 2. DNA Dependent DNA Polymerase Activity. The DNA polymerase has been isolated from embryos. Its activity has been determined in relation to the activity of the total embryo as well as per embryonic cell. The polymerase activity is much higher at the start of the development than in later stages, reaching a minimum in the blastula stage, the time at which cytoplasmic DNA has been exhausted. In the subsequent period the polymerase activity parallels the rate of DNA synthesis in vivo. The level of the DNA polymerase activity per cell remains constant. 3. DNase Activity. The DNase activity has been determined using the Lanthanum-Nitrate-Method. Three distinct maxima were found: A first maximum is reached immediately upon fertilization. The second one coincides with the onset of mesenchyme formation in the blastula, and the third one coincides with the end of gastrulation. The average specific activity is roughly equivalent to about 10−6 g DNase I per g of embryo. The possibility is discussed that rises in nucleolytic activities may trigger differentiation events in the developing egg. The influence of DNA polymerase activity and DNase activity on in vivo DNA synthesis is discussed.
    Type of Medium: Electronic Resource
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