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  • 1
    Online Resource
    Online Resource
    Cham :Springer International Publishing :
    Keywords: Physical geography. ; Climatology. ; Water. ; Hydrology. ; Biotic communities. ; Environmental Law. ; Earth System Sciences. ; Climate Sciences. ; Water. ; Ecosystems. ; Environmental Law.
    Description / Table of Contents: The Stage. Planet Earth: Our Home in the Universe -- Act 1. Seven Connections that Set the Scene of Life on Earth -- Act 2. Four Major Connections that Make Living Organisms and Systems Key Players on the Earth’s Scene -- Act 3. Two Major Connections by which Human Actors Disturb the Action of the Play -- Final act. Connections regulate the Earth System scene.
    Abstract: Earth is, to our knowledge, the only life-bearing body in the Solar System. This extraordinary characteristic dates back almost 4 billion years. How to explain that Earth is teeming with organisms and that this has lasted for so long? What makes Earth different from its sister planets Mars and Venus? The habitability of a planet is its capacity to allow the emergence of organisms. What astronomical and geological conditions concurred to make Earth habitable 4 billion years ago, and how has it remained habitable since? What have been the respective roles of non-biological and biological characteristics in maintaining the habitability of Earth? This unique book answers the above questions by considering the roles of organisms and ecosystems in the Earth System, which is made of the non-living and living components of the planet. Organisms have progressively occupied all the habitats of the planet, diversifying into countless life forms and developing enormous biomasses over the past 3.6 billion years. In this way, organisms and ecosystems "took over" the Earth System, and thus became major agents in its regulation and global evolution. There was co-evolution of the different components of the Earth System, leading to a number of feedback mechanisms that regulated long-term Earth conditions. For millennia, and especially since the Industrial Revolution nearly 300 years ago, humans have gradually transformed the Earth System. Technological developments combined with the large increase in human population have led, in recent decades, to major changes in the Earth's climate, soils, biodiversity and quality of air and water. After some successes in the 20th century at preventing internationally environmental disasters, human societies are now facing major challenges arising from climate change. Some of these challenges are short-term and others concern the thousand-year evolution of the Earth's climate. Humans should become the stewards of Earth.
    Type of Medium: Online Resource
    Pages: IX, 572 p. 121 illus., 98 illus. in color. , online resource.
    Edition: 1st ed. 2021.
    ISBN: 9783030677732
    Series Statement: The Frontiers Collection,
    DDC: 550
    Language: English
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  • 2
    Call number: 4/M 95.0588
    In: Lecture notes in earth sciences
    Type of Medium: Monograph available for loan
    Pages: VIII, 187 S.
    ISBN: 3540591702
    Series Statement: Lecture notes in earth sciences 57
    Classification:
    Geochemistry
    Language: English
    Location: Reading room
    Branch Library: GFZ Library
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  • 3
    Description / Table of Contents: PREFACE The four-year period of activity of the Groupement de Recherche 942 (GDR) of the Centre National de la Recherche Scientifique (CNRS) came to an end in December 1993. This GDR was a scientific association grouping research teams from the academic sphere -- i.e. the Unités de Recherches Associées 723 & 724 of the CNRS as well as the Universities of Orléans and Paris-Sud -- and from the industrial world: Elf-Aquitaine Production, TOTAL and the Institut Français du Pétrole (IFP). The aim of the GDR was to understand the processes and the causes of organic carbon fossilization in sediments, especially when they can be modified by environmental conditions such as climate, eustatism, productivity etc., factors which can alko interact. This goal implies the simultaneous study of ancient geological formations (hydrocarbon source rocks from the famous Kimmeridge Clay Formation) and recent Quaternary sediments (the Lac du Bouchet or lake Bouchet maar, Massif Central, France). In the latter case, we benefit from a fine-scale stratigraphical framework as well as a reliable reconstruction of the local and regional environment. This volume is a collection of papers representing oral presentations given on December 7, 1993, at the Société Géologique de France in Paris, during the final meeting of the GDR. These articles thus report the latest developments of the studies carried out under the GDR. However, this is not the first publication of our results, which can be found in the papers referred to in each article. The Kimmeridge Clay Formation was previously studied in 1987, by the Yorkim Group from IFP, Elf-Aquitaine and the British Geological Survey, on the basis of a series of wells drilled across the Cleveland Basin of Yorkshire. In each well, the distribution with depth of the total organic content is cyclic. We have compared some of the organic cycles from two wells (Matron and Ebberston) based on mineralogy, organic and inorganic geochemistry and petrography, at a high resolution scale (centimetric). The main conclusion of this work is that the driving force for organic matter accumulation in the studied cycles was organic phytoplankton productivity. Oxygenation conditions seem to have played a secondary role as a positive feedback action enhancing organic matter storage. Lac du Bouchet is located on the Devès volcanic plateau, 15 km SW of Le Puy en Velay, at an altitude of 1205 m. The depth of the water column is 28 m. The lake has a subcircular shape (1 km in diameter) and a very restricted watershed. This site is exceptionally suitable for research on climate variations and palaeomagnetic field modifications (Euromaars EC Program). The GDR focused on sedimentary organic matter and its relationship to inorganic phases. An important result is that organic matter appears to be a good indicator of palaeoenvironmental reconstructions for over 350 000 years. In addition, the study of early diagenetic reactions in surficial sediments (porewater and solid phase) allows the specification of the processes of organic matter degradation and storage in such an oligothrophic lake.
    Pages: Online-Ressource (187 Seiten)
    ISBN: 9783540591702
    Language: English
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  • 4
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 364 (1993), S. 786-788 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The Kimmeridge Clay formation is well known as a lateral equivalent of the major oil source rock unit of the North Sea, outcropping in the Cleveland basin near Marton (England). It consists of alternating organic-rich shales and marls deposited in marginal shallow water under low energy conditions, ...
    Type of Medium: Electronic Resource
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  • 5
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Phase relations and mineral chemistry involving the phases garnet (Gt), spinel (Sp), hypersthene (Hy), sapphirine (Sa), cordierite (Cd), sillimanite (Sil) and quartz (Qz) have been experimentally determined in the system FMAS (FeO−MgO−Al2O2−SiO2) under low fO2 and for various H2O/CO2 conditions. Several compositions were studied with 100 (Mg/Mg+Fe) ratio ranging from 64 to 87 with excess quartz and sillimanite. Our data do not show any differences in Gt−Cd stability and composition as a function of H2O, CO2 and H2O−CO2 (±CH4) content, in good agreement with a previous experimental study at lower temperature (Aranovich and Podlesskii 1983). At 1,000° C and 11 kbar, under CO2-saturated conditions, cordierite grew from a crystalline mix unseeded with cordierite. Thus, under water-absent conditions, cordierite will have a high-P stability field in the presence of CO2. If water has a pressure stabilizing effect on cordierite, then our results would indicate that the effects of H2O and CO2 are of the same magnitude at high temperature. Our data support the theoretical P-T grid proposed by Hensen (1986) for high-T metapelites and are largely consistent with the high-temperature experimental data of Hensen and Green (1973). The univariant boundary Gt+Cd=Hy+Sil+Qz, which marks the disappearance of Hy−Sil−Qz assemblages, has a negative dP/dT slope above 1,000° C and a positive one below this temperature. Extrapolation of our data to iron-free systems shows that the high-P breakdown limit of Mg-cordierite has a negative slope in the range 1,025–1,300° C and probably positive below 1,000° C. This indicates a maximum of stability for Mg-cordierite at around 1,000° C and 13 kbar. Because of the curvature of the univariant reactions En+Sil=Py+Qz, Mg−Cd=En+Sil+Qz and Gt+Cd=Hy+Sil+Qz, the iron-free invariant point involving the phases Py, En, Cd, Sil and Qz probably does not exist. Sapphirine—Qz-bearing assemblages are stable only at temperatures above 1,050° C. At 1,075° C, the joint Gt−Sa is stable up to 11 kbar. At higher pressure, garnet, sapphirine and quartz react according to the reaction Gt+Sa+Qz=Hy+Sil. Reequilibrated sapphirines are more aluminous than the theoretical endmember Mg2Al4SiO10 due to AlAl=MgSi substitutions [100(Al2O3/Al2O3+FeO+MgO) in experimental sapphirines ranges from 50.5 to 52.2]. Sapphirine in the assemblage Sa−Cd−Sil−Qz shows a decrease in Al content with decreasing temperature and pressure, such that the alumina isopleths for sapphirine have a slight negative dP/dT slope. A similar decrease in Al content of sapphirine with temperature is also observed in Sa−Sil−Qz assemblages.
    Type of Medium: Electronic Resource
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  • 6
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    PANGAEA
    Publication Date: 2023-06-27
    Keywords: CALYPSO; Calypso Corer; IMAGES; IMAGES II; International Marine Global Change Study; Marion Dufresne (1995); MD105; MD962075; MD96-2075; Mozambique Basin
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  • 7
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    PANGAEA
    Publication Date: 2023-06-27
    Keywords: CALYPSO; Calypso Corer; IMAGES; IMAGES II; International Marine Global Change Study; Marion Dufresne (1995); MD105; MD962076; MD96-2076; Natal Valley
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    Format: unknown
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  • 8
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    PANGAEA
    Publication Date: 2023-06-27
    Keywords: GC; Gravity corer; IMAGES; IMAGES II; International Marine Global Change Study; Marion Dufresne (1995); MD105; MD962076G; MD96-2076G; Natal Valley
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    Format: unknown
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  • 9
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    PANGAEA
    Publication Date: 2023-06-27
    Keywords: CALYPSO; Calypso Corer; IMAGES; IMAGES II; International Marine Global Change Study; Marion Dufresne (1995); MD105; MD962077; MD96-2077; Natal Valley
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    Format: unknown
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  • 10
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    PANGAEA
    Publication Date: 2023-06-27
    Keywords: CALYPSO; Calypso Corer; IMAGES; IMAGES II; International Marine Global Change Study; Marion Dufresne (1995); MD105; MD962079; MD96-2079; Transkei Basin
    Type: Dataset
    Format: unknown
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