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  • English  (14)
  • 2020-2023  (2)
  • 2015-2019  (12)
  • 1975-1979
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  • 1
    Monograph available for loan
    Monograph available for loan
    Sustainable innovation and regional development : rethinking innovative milieus (2017)
    Cheltenham, UK : Edward Elgar Pub.
    Details Availability
    Call number: PIK B 160-17-90501
    Type of Medium: Monograph available for loan
    Pages: xx, 267 Seiten , Illustrationen, Diagramme
    ISBN: 9781784712204 (hardback)
    Series Statement: New horizons in regional science
    Language: English
    Note: Contents: Introduction: Sustainability, Innovative Milieus And Territorial Development ; PART I SUSTAINABLE INNOVATION, GLOBAL ANCHORING OF TERRITORIAL PRODUCTIVE SYSTEMS, AND COMPETITIVENESS 1. The Territories of ‘Sustainable’ Innovation: From Local Milieus to ‘Responsible’ Communication: The Case of Photovoltaics and Sustainable Finance in Western Switzerland ; 2. Innovation in the Sustainable Renovation Sector in Île-De-France ; 3. Border-Crossing Sustainable Innovation Processes – German Knowledge-Intensive Business Services (KIBS) in Green Construction ; 4. Living PlanIT and the Development of the ‘PlanIT Urban Operating System tm’: The Geographies of an Innovation ; 5. The Sustainable Water Campus in Leeuwarden: Towards an Anchoring Milieu or a ‘Hollow Term’? ; PART II SUSTAINABLE INNOVATION TOWARDS AN INTEGRATED TERRITORIAL DEVELOPMENT ; 6. Bairro Alto Revisited: Sustainable Innovations, Reputation Building and Urban Development ; 7. Innovative Rurban Networks in Rome ; 8. Innovation in Sustainable Tourism Projects in Alpine Resorts ; PART III SUSTAINABLE INNOVATION, ECONOMIC RESTRUCTURING AND REGIONAL PRODUCTIVE SYSTEMS ; 9. The Great Basque Transformation Towards Sustainable Innovations ; 10. Atlantic Nautical Network: An Inter-Regional Organizational System to Promote Innovation in Support of Sustainable Development ; 11. From Regional Production System to Regional Innovation System – Evolutional Changes of Suwa Industrial Region in Japan ; Conclusion: Relaunching GREMI: A Scientific Trajectory
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  • 2
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    Marine isotope stage 3 in southern South America, 60 ka B.P.-30 ka B.P (2016)
    [Cham] : Springer
    Details
    Call number: 9783319400006 (e-book)
    Description / Table of Contents: This book presents isotope data reflecting changes in temperature derived from core samples in South America. Marine Isotope Stage (MIS) is examined in detail with respect to Stage 3. With over 20 chapters, this detailed treatise discusses high climatic variability, paleoclimatic events, Dansgaard-Oeschger cycles, continental vertebrates, sea level changes, vegetation and climate changes based on pollen records, and the non-Amazon landscape and fauna from 65 to 20 ka B.P. The book also looks at the earth’s magnetic field and climate change during MIS 3 and MIS 5 and presents a comparison between both stages with respect to marine deposits in Uruguay. With case studies drawn from Brazil, Argentina and Uruguay this book presents research from the some of the worlds experts in this field.
    Type of Medium: 12
    Pages: 1 Online-Ressource (viii, 354 Seiten) , Illustrationen
    ISBN: 9783319400006 , 978-3-319-40000-6
    ISSN: 2197-9596 , 2197-960X
    Series Statement: Springer Earth System Sciences
    URL: Ebook (access only within the AWI network)
    DOI: 10.1007/978-3-319-40000-6
    Language: English
    Note: Contents Introduction / Germán Mariano Gasparini, Jorge Rabassa, Cecilia Deschamps and Eduardo Pedro Tonni The Heinrich and Dansgaard–Oeschger Climatic Events During Marine Isotopic Stage 3 / Jorge Rabassa and Juan Federico Ponce On the Origin of the Dansgaard–Oeschger Events and Its Time Variability / Silvia Duhau and Cornelis de Jager The Influence of the Geomagnetic Field in Climate Changes / María Julia Orgeira, Ana María Sinito and Rosa Hilda Compagnucci Abrupt Climate Changes During the Marine Isotope Stage 3 (MIS 3) / Eduardo Andrés Agosta and Rosa Hilda Compagnucci Active Deformation, Uplift and Subsidence in Southern South America Throughout the Quaternary: A General Review About Their Development and Mechanisms / Andrés Folguera, Guido Gianni, Lucía Sagripanti, Emilio Rojas Vera, Bruno Colavitto, Darío Orts and Víctor Alberto Ramos The Marine Isotopic Stage 3 (MIS 3) in Valleys of the Undulated Pampa, Buenos Aires Province, Argentina / Adriana María Blasi, Carola Castiñeira Latorre, Gabriela Catalina Cusminsky and Ana Paula Carignano Sea Level Changes During Marine Isotopic Stage 3 (MIS 3) in Argentina / Federico Ignacio Isla and Enrique Jorge Schnack Paleogeographic Evolution of the Atlantic Coast of South America During Marine Isotope Stage 3 (MIS 3) / Juan Federico Ponce and Jorge Rabassa The Continental Record of Marine Isotope Stage 3 (MIS 3; ~60–25 ka) in Central Argentina: Evidence from Fluvial and Aeolian Sequences / Marcelo Zárate, Adriana Mehl and Alfonsina Tripaldi Marine Isotope Stage 3 (MIS 3) and Continental Beds from Northern Uruguay (Sopas Formation): Paleontology, Chronology, and Climate / Martín Ubilla, Andrea Corona, Andrés Rinderknecht, Daniel Perea and Mariano Verde The Brazilian Intertropical Fauna from 60 to About 10 ka B.P.: Taxonomy, Dating, Diet, and Paleoenvironments / Mário André Trinidade Dantas and Mario Alberto Cozzuol Continental Vertebrates During the Marine Isotope Stage 3 (MIS 3) in Argentina / Germán Mariano Gasparini, Esteban Soibelzon, Cecilia Deschamps, Analía Francia, Elisa Beilinson, Leopoldo Héctor Soibelzon and Eduardo Pedro Tonni Marine Isotope Stage 3 (MIS 3) Versus Marine Isotope Stage 5 (MIS 5) Fossiliferous Marine Deposits from Uruguay / Alejandra Rojas and Sergio Martínez Vegetation and Climate in Southern South America during Marine Isotope Stage 3 (MIS 3): an Overview of Existing Terrestrial Pollen Records / Ana María Borromei and Lorena Laura Musotto Response of Diatoms to Late Quaternary Climate Changes / Marcela Alcira Espinosa Silicophytolith Studies in South America and Argentina: Scope and Limitations for Paleoenvironmental Reconstruction of the Marine Isotope Stage 3 (MIS3) / Margarita Osterrieth, María Fernanda Alvarez, Mariana Fernández Honaine and Georgina Erra Index
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  • 3
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    Governing Forest Restoration: Social, Environmental and Institutional Dimensions (2015)
    Basel, Beijing, Wuhan : MDPI
    Details
    Keywords: forest restoration ; landscape restoration ; global policy ; payment for environmental services ; natural forest regeneration ; multiscalar governance
    Description / Table of Contents: Negotiation, reconciliation of multiple scales through both ecological and social dimensions and minimization of power imbalances are considered critical challenges to overcome for effective governance of forest restoration. Finding the right mix of “command and control” in forest restoration vs. “environmental governance”, which includes non-state actors, regulatory flexibility, and market based instruments is at the heart of these challenges. This Special Issue attempts at shedding light on these challenges with case studies from South and Central America, Africa, and Asia. Some provide within-country as well as cross-country comparisons. A few others present case studies at the household level. Both policy and legal constraints towards implementing forest restoration are also discussed as a function of top down vs. bottom up approaches. The effectiveness of payments for environmental services is examined as catalyzers of forest restoration initiatives. Finally, two papers deal with the legal and policy constraints in making restoration through natural regeneration a viable and cost-effective tool. In the face of renewed perspectives for expanding forest restoration programs globally, governance issues will likely play a key role in eventually determining success. As many of the papers in this Special Issue suggest, the fate of forest restoration outcomes is, more often than not, associated with overall governance challenges, some of which are often overlooked particularly across multiple scales.
    Pages: Online-Ressource (XVII, 195 Seiten)
    Edition: Printed Edition of the Special Issue Published in Forests
    ISBN: 9783038420439
    URL: http://www.mdpi.com/books/pdfview/book/110
    Language: English
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  • 4
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    Railway Ecology (2017)
    Cham : Springer
    Details
    Keywords: Environment ; Environmental sciences ; Urban geography ; Applied ecology ; Biodiversity ; Nature conservation ; Environment ; Nature Conservation ; Applied Ecology ; Biodiversity ; Urban Geography / Urbanism (inc. megacities, cities, towns) ; Environmental Science and Engineering
    Description / Table of Contents: Part 1 --- Introduction --- 1. Railway Ecology --- 2. Wildlife Mortality in Railways --- 3. Railways as Barriers for Wildlife: Current Knowledge and Future Steps --- Part 2. Introduction --- Case Studies --- Conclusions --- What’s Next? Railway Ecology in the 21st Century
    Pages: Online-Ressource (XXX, 320 pages) , 53 illustrations, 28 illustrations in color
    ISBN: 9783319574967
    URL: https://link.springer.com/openurl?genre=book&isbn=978-3-319-57496-7
    Language: English
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  • 5
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    Contemporaneous assembly of Western Gondwana and final Rodinia break-up: Implications for the supercontinent cycle (2018)
    Details
    Publication Date: 2021-03-29
    Description: Geological, geochronological and isotopic data are integrated in order to present a revised model for the Neoproterozoic evolution of Western Gondwana. Although the classical geodynamic scenario assumed for the period 800e700 Ma is related to Rodinia break-up and the consequent opening of major oceanic basins, a significantly different tectonic evolution can be inferred for most Western Gondwana cratons. These cratons occupied a marginal position in the southern hemisphere with respect to Rodinia and recorded subduction with back-arc extension, island arc development and limited formation of oceanic crust in internal oceans. This period was thus characterized by increased crustal growth in Western Gondwana, resulting from addition of juvenile continental crust along convergent margins. In contrast, crustal reworking and metacratonization were dominant during the subsequent assembly of Gondwana. The Río de la Plata, Congo-São Francisco, West African and Amazonian cratons collided at ca. 630 e600 Ma along the West Gondwana Orogen. These events overlap in time with the onset of the opening of the Iapetus Ocean at ca. 610e600 Ma, which gave rise to the separation of Baltica, Laurentia and Amazonia and resulted from the final Rodinia break-up. The East African/Antarctic Orogen recorded the subsequent amalgamation of Western and Eastern Gondwana after ca. 580 Ma, contemporaneously with the beginning of subduction in the Terra Australis Orogen along the southern Gondwana margin. However, the Kalahari Craton was lately incorporated during the Late EdiacaraneEarly Cambrian. The proposed Gondwana evolution rules out the existence of Pannotia, as the final Gondwana amalgamation postdates latest connections between Laurentia and Amazonia. Additionally, a combination of introversion and extroversion is proposed for the assembly of Gondwana. The contemporaneous record of final Rodinia break-up and Gondwana assembly has major implications for the supercontinent cycle, as supercontinent amalgamation and break-up do not necessarily represent alternating episodic processes but overlap in time.
    Keywords: Brasiliano-Pan-African Orogeny; Neoproterozoic; Collisional tectonics; Pannotia; Metacratonization; Introversion-extroversion ; 551
    Language: English
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  • 6
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    Dolomitic slates from Uruguay: petrophysical and petromechanical characterization and deposit evaluation (2018)
    Springer-Verlag | Berlin/Heidelberg
    Details
    Publication Date: 2021-03-29
    Description: Slates are internationally known as roof and façade-cladding material since prehistoric times. The methods required to mine and manufacture these dimensional stones are relatively simple in comparison to those utilized in granitic dimensional stones. This has led to a worldwide rentable commercialization of slate in the last centuries and also to the development of characteristic cultural landscapes. In Uruguay several slates are mined and used in architecture, especially as façade cladding and floor slabs. The most important slates regarding their production and utilization are the dolomitic slates. These dolomitic slates are associated with the Neoproterozoic thrust and fold belt of the Dom Feliciano belt. Representative samples have been geochemically and petrographically characterized, as well as petrophysically and petromechanically analyzed. The petrophysical and petromechanical properties were investigated in a very systematic way with respect to the new European standards, showing values comparable to those registered for internationally known slates. Detailed structural and deposit analysis were carried out in Uruguay in order to evaluate the dolomitic slate deposits. The slates are linked to calc-silicate strata in a greenschist facies volcano-sedimentary sequence and the deposits are located in the limb of a regional fold, where bedding and cleavage are parallel. The main lithotype is a layered and fine-grained dolomitic slate with a quite diverse palette of colors: light and dark green, gray, dark gray, reddish and black. The mined slate is split into slabs 0.5–2 cm thick. In the past, the average production in Uruguay was around 4,000 tons/year and a historical maximum of 13,000 tons was reached in 1993 (Oyhantçabal et al. in Z dt Ges Geowiss 158(3):417–428, 2007). The oscillations in the regional demand were the cause of several flourishing and decay cycles in the activity, but our investigation shows a considerable volume of indicated resources and therefore a very good potential.
    Keywords: Slates; Dimensional stones; Petrophysical properties; Petrography; Uruguay ; 551 ; Earth Sciences; Geology
    Language: English
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  • 7
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    Granitic dimensional stones in Uruguay: evaluation and assessment of potential resources (2018)
    Springer-Verlag | Berlin/Heidelberg
    Details
    Publication Date: 2021-03-29
    Description: In Uruguay commercial granite varieties comprise mafic rocks, granitoids, and syenitoids. There is a long tradition in Uruguay, as well as worldwide, of using dimensional stones in architecture and art, specially granitic ones. Some of the present applications of these dimensional stones are as façade cladding, countertops, and outdoor and indoor floor slabs. The color spectrum of the Uruguayan granitic dimensional stones varies from black to light gray, covering a wide variety of red and pink and minor greenish-gray. The décor of these granitic dimensional stones is mainly determined by their fabric, fundamentally the grain size and the color distribution between the different minerals that compose the rocks. In the present research the most important commercial granites were sampled to analyze their petrography and petrophysical properties. A detailed structural analysis has been performed in several deposits, as well as the application of the software 3D Block Expert for modeling the possible raw block size distribution. Other factors controlling the mining viability of the deposits were also studied (e.g., homogeneity/heterogeneity of color and décor) and the possible reserves were calculated.
    Keywords: Granitic dimensional stones; Petrophysical properties; Petrography; Deposit characterization; Uruguay ; 551 ; Earth Sciences; Geology
    Language: English
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  • 8
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    The transpressional connection between Dom Feliciano and Kaoko Belts at 580–550 Ma (2018)
    Springer-Verlag | Berlin/Heidelberg
    Details
    Publication Date: 2021-03-29
    Description: A new U–Pb SHRIMP age of 551 ± 4 Ma on a mylonitic porphyry that intruded into the Sierra Ballena Shear Zone (Southernmost Dom Feliciano Belt, Uruguay) and a review of relevant published data make possible a more refined correlation and reconstruction of Brasiliano/Pan-African transpressional events. Paleogeographic reconstruction, kinematics and timing of events indicate a connection between the shear systems of the Dom Feliciano and Kaoko Belts at 580–550 Ma. Sinistral transpression recorded in shear zones accommodates deformation subsequent to collision between the Congo and Río de la Plata Cratons. The correlation is strengthened by the similarity of magmatic and metamorphic ages in the Coastal Terrane of the Kaoko Belt and the Punta del Este Terrane of the Dom Feliciano Belt. This post-collisional sinistral transpression brought these units near to their final position in Gondwana and explains the different evolution at 550–530 Ma. While in the Kaoko Belt, an extensional episode resulted in exhumation as a consequence of collision in the Damara Belt, in the Dom Feliciano Belt, sinistral transpression occurred associated with the closure of the southern Adamastor Ocean due to Kalahari-Río de la Plata collision.
    Keywords: Dom Feliciano Belt; Kaoko Belt; Brasiliano; Pan-African; Transpressional deformation; Shear Zones ; 551 ; Earth Sciences; Geophysics/Geodesy; Geology
    Language: English
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  • 9
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    The Río de la Plata Craton: a review of units, boundaries, ages and isotopic signature (2018)
    Springer-Verlag | Berlin/Heidelberg
    Details
    Publication Date: 2021-03-29
    Description: A review of the lithostratigraphic units in the Río de la Plata Craton and of new and previously published geochronological, isotopic and geophysical data is presented. Sm–Nd TDM model ages between 2.6 and 2.2 Ga characterize the Piedra Alta Terrane of this craton. Crystallization ages between 2.2 and 2.1 Ga for the metamorphic protoliths and 2.1–2.0 Ga for the post-orogenic granitoids indicate juvenile crust, followed by a short period of crustal recycling. Cratonization of this terrane occurred during the late Paleoproterozoic. Younger overprinting is not observed, suggesting it had a thick and strong lithosphere in the Neoproterozoic. A similar scenario is indicated for the Tandilia Belt of Argentina. Sm–Nd TDM model ages for the Nico Pérez Terrane show two main events of crustal growth (3.0–2.6 and 2.3–1.6 Ga). The crystallization ages on zircon ranges between 3.1 and 0.57 Ga, which is evidence for long-lived crustal reworking. The age for cratonization is still uncertain. In the Taquarembó Block, which is considered the prolongation of the Nico Pérez Terrane in southern Brazil, a similar scenario can be observed. These differences together with contrasting geophysical signatures support the redefinition of the Río de la Plata Craton comprising only the Piedra Alta Terrane and the Tandilia Belt. The Sarandí del Yí Shear Zone is regarded as the eastern margin of this Craton.
    Keywords: Precambrian; Transamazonian cycle; South American platform; Río de la Plata Craton ; 551 ; Earth Sciences; Geophysics/Geodesy; Geology
    Language: English
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  • 10
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    The Sierra Ballena Shear Zone in the southernmost Dom Feliciano Belt (Uruguay): evolution, kinematics, and deformation conditions (2018)
    Springer-Verlag | Berlin/Heidelberg
    Details
    Publication Date: 2021-03-29
    Description: The Sierra Ballena Shear Zone (SBSZ) is part of a high-strain transcurrent system that divides the Neoproterozoic Dom Feliciano Belt of South America into two different domains. The basement on both sides of the SBSZ shows a deformation stage preceding that of the transcurrent deformation recognized as a high temperature mylonitic foliation associated with migmatization. Grain boundary migration and fluid-assisted grain boundary diffusion enhanced by partial melting were the main deformation mechanisms associated with this foliation. Age estimate of this episode is 〉658 Ma. The second stage corresponds to the start of transpressional deformation and the nucleation and development of the SBSZ. During this stage, pure shear dominates the deformation, and is characterized by the development of conjugate dextral and sinistral shear zones and the emplacement of syntectonic granites. This event dates to 658–600 Ma based on the age of these intrusions. The third stage was a second transpressional event at about 586 to 〈560 Ma that was associated with the emplacement of porphyry dikes and granites that show evidence of flattening. Deformation in the SBSZ took place, during the late stages, under regional low-grade conditions, as indicated by the metamorphic paragenesis in the supracrustals of the country rocks. Granitic mylonites show plastic deformation of quartz and brittle behavior of feldspar. A transition from magmatic to solid-state microstructures is also frequently observed in syntectonic granites. Mylonitic porphyries and quartz mylonites resulted from the deformation of alkaline porphyries and quartz veins emplaced in the shear zone. Quartz veins reflect the release of silica associated with the breakdown of feldspar to white mica during the evolution of the granitic mylonites to phyllonites, which resulted in shear zone weakening. Quartz microstructures characteristic of the transition between regime 2 and regime 3, grain boundary migration and incipient recrystallization in feldspar indicate deformation under lower amphibolite to upper greenschist conditions (550–400°C). On the other hand, the mylonitic porphyries display evidence of feldspar recrystallization suggesting magmatic or high-T solid-state deformation during cooling of the dikes.
    Keywords: Brasiliano; Pan-African; Shear zone; Dom Feliciano Belt; Uruguay; Kinematic analysis ; 551 ; Earth Sciences; Geology ; Geophysics/Geodesy
    Language: English
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