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  • 2015-2019  (4,516)
  • 2005-2009  (2,390)
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  • 1
    Monograph available for loan
    Monograph available for loan
    Princeton [u.a.] : Princeton Univ. Press
    Call number: PIK E 712-08-0168
    Type of Medium: Monograph available for loan
    Pages: XXII, 427 S.
    Edition: 2. ed.
    ISBN: 0691137153 , 978-0-691-13715-5 , 978-0-691-13714-8
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    London : The Geological Society
    Associated volumes
    Call number: 9/M 07.0421(320)
    In: Geological Society special publication
    Type of Medium: Monograph available for loan
    Pages: 272 S.
    ISBN: 9781862392816
    Series Statement: Geological Society special publication 320
    Location: Reading room
    Branch Library: GFZ Library
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  • 3
    Call number: IASS 19.93210
    Type of Medium: Monograph available for loan
    Pages: 145 Seiten , graphische Darstellungen
    Edition: first published in English in 2019
    ISBN: 9781771134071 , 9781771134088 (electronic; ePub) , 9781771134095 (electronic; PDF)
    Uniform Title: Die Konsultative : Mehr Demokratie durch Bürgerbeteiligung
    Language: English
    Branch Library: RIFS Library
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  • 4
    Monograph available for loan
    Monograph available for loan
    Princeton [u.a.] : Princeton Univ. Press
    Call number: PIK B 050-08-0167
    Type of Medium: Monograph available for loan
    Pages: XVII, 389 S. : graph. Darst.
    Edition: 2. pr.
    ISBN: 0691120382
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 5
    Call number: 9/M 07.0421(467)
    In: Geological Society Special Publication
    Description / Table of Contents: Gullies on Mars resemble terrestrial gullies involved in the transport of abundant material down steep slopes by liquid water. However, liquid water should not be stable at the Martian surface. The articles in this volume present the two main opposing theories for Martian gully formation: climate-driven melting of surficial water-ice deposits and seasonal dry-ice sublimation. The evidence presented ranges from remote-sensing observations, to experimental simulations, to comparison with Earth analogues. The opposing hypotheses imply either that Mars has been unusually wet in the last few million years or that it has remained a cold dry desert – both with profound implications for understanding the water budget of Mars and its habitability. The debate questions the limits of remote-sensing data and how we interpret active processes on extra-terrestrial planetary surfaces, even beyond those on Mars, as summarized by the review paper at the beginning of the book.
    Type of Medium: Monograph available for loan
    Pages: vi, 434 Seiten , Illustrationen
    ISBN: 978-1-78620-360-1
    Series Statement: Geological Society Special Publication 467
    Language: English
    Location: Reading room
    Branch Library: GFZ Library
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  • 6
    Description / Table of Contents: Periglacial and paraglacial environments, located outside ice sheet margins but responding to similar climate forcings, are key to identifying climate change effects upon the Earth system. These environments are relicts of cold Earth processes and so are most sensitive to global warming. Changes in the distribution and thickness of permafrost in continental interiors have implications for ecosystem and landscape stability. Periglacial Alpine environments are experiencing increased rockfall and mass movement, leading to rock glacier instability and sediment release to downstream rivers. In turn, these landscape effects impact on natural hazards and human activities in these sensitive and geologically transient environments. Papers in this volume explore some of these interrelated issues in field studies from Europe, North America and Asia. The volume will be of interest to geomorphologists, modellers, environmental managers, planners and engineers working on landscape, climate and environmental change in periglacial and paraglacial areas.
    Pages: Online-Ressource (272 Seiten)
    ISBN: 9781862392816
    Language: English
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  • 7
    Keywords: terrestrial analogues ; gully ; gully formation ; Mars
    Description / Table of Contents: Martian gullies and their Earth analogues: introduction / Susan J. Conway, Tjalling de Haas, Tanya N. Harrison, Paul A. Carling and Jonathan Carrivick / Geological Society, London, Special Publications, 467, 1-6, 7 December 2018, https://doi.org/10.1144/SP467.15 --- Martian gullies: a comprehensive review of observations, mechanisms and insights from Earth analogues / Susan J. Conway, Tjalling de Haas and Tanya N. Harrison / Geological Society, London, Special Publications, 467, 7-66, 25 October 2018, https://doi.org/10.1144/SP467.14 --- Martian remote sensing --- The formation of gullies on Mars today / Colin M. Dundas, Alfred S. McEwen, Serina Diniega, Candice J. Hansen, Shane Byrne and Jim N. McElwaine / Geological Society, London, Special Publications, 467, 67-94, 27 November 2017, https://doi.org/10.1144/SP467.5 --- Dune-slope activity due to frost and wind throughout the north polar erg, Mars / Serina Diniega, Candice J. Hansen, Amanda Allen, Nathan Grigsby, Zheyu Li, Tyler Perez and Matthew Chojnacki / Geological Society, London, Special Publications, 467, 95-114, 27 November 2017, https://doi.org/10.1144/SP467.6 --- Morphological characterization of landforms produced by springtime seasonal activity on Russell Crater megadune, Mars / Gwenaël Jouannic, Susan J. Conway, Julien Gargani, François Costard, Marion Massé, Olivier Bourgeois, John Carter, Frédéric Schmidt, Chiara Marmo, Gian G. Ori, Marion Nachon and Kelly Pasquon / Geological Society, London, Special Publications, 467, 115-144, 29 October 2018, https://doi.org/10.1144/SP467.16 --- Are different Martian gully morphologies due to different processes on the Kaiser dune field? / Kelly Pasquon, Julien Gargani, Marion Nachon, Susan J. Conway, Marion Massé, Gwenaël Jouannic, Matthew R. Balme, François Costard and Mathieu Vincendon / Geological Society, London, Special Publications, 467, 145-164, 18 July 2018, https://doi.org/10.1144/SP467.13 --- Time will tell: temporal evolution of Martian gullies and palaeoclimatic implications / T. de Haas, S. J. Conway, F. E. G. Butcher, J. Levy, P. M. Grindrod, T. A. Goudge and M. R. Balme / Geological Society, London, Special Publications, 467, 165-186, 27 November 2017, https://doi.org/10.1144/SP467.1 --- New slope-normalized global gully density and orientation maps for Mars / S. J. Conway, T. N. Harrison, R. J. Soare, A. W. Britton and L. J. Steele / Geological Society, London, Special Publications, 467, 187-197, 27 November 2017, https://doi.org/10.1144/SP467.3 --- Thermal inertia variations from gully and mass-wasting activity in Gasa crater, Mars / Tanya N. Harrison, Livio L. Tornabene, Gordon R. Osinski and Susan J. Conway / Geological Society, London, Special Publications, 467, 199-210, 4 December 2017, https://doi.org/10.1144/SP467.8 --- Periglacial complexes and the deductive evidence of ‘wet’-flows at the Hale impact crater, Mars / R. J. Soare, S. J. Conway, C. Gallagher, J. M. Dohm and D. Reiss / Geological Society, London, Special Publications, 467, 211-231, 6 March 2018, https://doi.org/10.1144/SP467.7 --- Geomorphological analysis of gullies on the central peak of Lyot Crater, Mars / Virginia C. Gulick, Natalie Glines, Shawn Hart and Patrick Freeman / Geological Society, London, Special Publications, 467, 233-265, 5 December 2018, https://doi.org/10.1144/SP467.17 --- Earth analogues --- Debris flows and water tracks in northern Victoria Land, continental East Antarctica: a new terrestrial analogue site for gullies and recurrent slope lineae on Mars / E. Hauber, C. Sassenroth, J.-P. de Vera, N. Schmitz, R. Jaumann, D. Reiss, H. Hiesinger and A. Johnsson / Geological Society, London, Special Publications, 467, 267-287, 3 April 2018, https://doi.org/10.1144/SP467.12 --- Gully formation in the McMurdo Dry Valleys, Antarctica: multiple sources of water, temporal sequence and relative importance in gully erosion and deposition processes / James L. Dickson, James W. Head, Joseph S. Levy, Gareth A. Morgan and David R. Marchant / Geological Society, London, Special Publications, 467, 289-314, 4 December 2017, https://doi.org/10.1144/SP467.4 --- Gullies and debris-flows in Ladakh Himalaya, India: a potential Martian analogue / Rishitosh K. Sinha, S. Vijayan, Anil D. Shukla, Priyabrata Das and Falguni Bhattacharya / Geological Society, London, Special Publications, 467, 315-342, 7 February 2018, https://doi.org/10.1144/SP467.9 --- Laboratory simulations --- CO2 sublimation in Martian gullies: laboratory experiments at varied slope angle and regolith grain sizes / Matthew E. Sylvest, John C. Dixon, Susan J. Conway, Manish R. Patel, Jim N. McElwaine, Axel Hagermann and Adam Barnes / Geological Society, London, Special Publications, 467, 343-371, 26 February 2018, https://doi.org/10.1144/SP467.11 --- Downslope sediment transport by boiling liquid water under Mars-like conditions: experiments and potential implications for Martian gullies / Clémence Herny, Susan J. Conway, Jan Raack, Sabrina Carpy, Tanguy Colleu-Banse and Manish R. Patel / Geological Society, London, Special Publications, 467, 373-410, 6 February 2018, https://doi.org/10.1144/SP467.10 --- An experimental investigation into Martian gully formation: a slush-flow model / Katherine S. Auld and John C. Dixon / Geological Society, London, Special Publications, 467, 411-424, 27 November 2017, https://doi.org/10.1144/SP467.2
    Pages: Online-Ressource (VI, 434 Seiten) , Illustrationen, Diagramme
    ISBN: 9781786203625
    Language: English
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  • 8
    Publication Date: 2022-05-26
    Description: Author Posting. © Elsevier B.V., 2008. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Marine Pollution Bulletin 56 (2008): 1049-1056, doi:10.1016/j.marpolbul.2008.03.010.
    Description: The proposed plan for enrichment of the Sulu Sea, Philippines, a region of rich marine biodiversity, with thousands of tonnes of urea in order to stimulate algal blooms and sequester carbon is flawed for multiple reasons. Urea is preferentially used as a nitrogen source by some cyanobacteria and dinoflagellates, many of which are neutrally or positively buoyant. Biological pumps to the deep sea are classically leaky, and the inefficient burial of new biomass makes the estimation of a net loss of carbon from the atmosphere questionable at best. The potential for growth of toxic dinoflagellates is also high, as many grow well on urea and some even increase their toxicity when grown on urea. Many toxic dinoflagellates form cysts which can settle to the sediment and germinate in subsequent years, forming new blooms even without further fertilization. If large-scale blooms do occur, it is likely that they will contribute to hypoxia in the bottom waters upon decomposition. Lastly, urea production requires fossil fuel usage, further limiting the potential for net carbon sequestration. The environmental and economic impacts are potentially great and need to be rigorously assessed.
    Description: This paper was developed under the Global Ecology and Oceanography of Harmful Algal Blooms (GEOHAB) core research project on HABs and Eutrophication and the GEOHAB regional focus on HABs in Asia. GEOHAB is supported by the International Oceanographic Commission (IOC) of UNESCO and by the Scientific Committee on Oceanic Research (SCOR), which are, in turn, supported by multiple agencies, including NSF and NOAA of the USA.
    Keywords: Urea dumping ; Ocean fertilization ; Carbon credits ; Sulu Sea ; Carbon sequestration ; Harmful algae ; Toxic dinoflagellates ; Cyanobacteria ; Hypoxia
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
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  • 9
    Publication Date: 2018-12-31
    Description: Zircon crystals from the Jack Hills, Western Australia, are one of the few surviving mineralogical records of Earth’s first 500 million years and have been proposed to contain a paleomagnetic record of the Hadean geodynamo. A prerequisite for the preservation of Hadean magnetization is the presence of primary magnetic inclusions within pristine igneous zircon. To date no images of the magnetic recorders within ancient zircon have been presented. Here we use high-resolution transmission electron microscopy to demonstrate that all observed inclusions are secondary features formed via two distinct mechanisms. Magnetite is produced via a pipe-diffusion mechanism whereby iron diffuses into radiation-damaged zircon along the cores of dislocations and is precipitated inside nanopores and also during low-temperature recrystallization of radiation-damaged zircon in the presence of an aqueous fluid. Although these magnetites can be recognized as secondary using transmission electron microscopy, they otherwise occur in regions that are indistinguishable from pristine igneous zircon and carry remanent magnetization that postdates the crystallization age by at least several hundred million years. Without microscopic evidence ruling out secondary magnetite, the paleomagnetic case for a Hadean–Eoarchean geodynamo cannot yet been made.
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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  • 10
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