ALBERT

Description / Table of Contents: Chapter 1-Introduction -- Chapter 2-Historical perspective -- Chapter 3-Geology and stratigraphy -- Chapter 4-Indian late cretaceous dinosaur nesting sites -- Chapter 5-Discussion. Chapter -- 6-Summary and conclusions.

Description / Table of Contents: Molecular imaging of the human emotion circuit -- The neurocognitive mechanisms of unconscious emotional responses -- Social and Affective Neuroscience of Embodiment -- The neuroscience of beauty -- Mirror Neurons … in action: ERPs and neuroimaging evidence -- Sex differences in social cognition -- Development of morality and emotional processing -- Trust in Social Interaction: From Dyads to Civilizations -- The time has come to be mindwanderful: Mind wandering and the intuitive psychology mode -- Social Cognition development and socio affective dysfunction in childhood and adolescence -- Clinical neuroscience meets second-person neuropsychiatry -- EEG and ERPs in the study of Language and Social Knowledge -- fMRI and fNIRS methods for social brain studies: hyperscanning possibilities -- Modulating the Social and Affective Brain with transcranial stimulation techniques -- What our eyes can tell us about our social and affective brain? -- Facial EMG – Investigating the interplay of facial muscles and emotions.

Description / Table of Contents: Chapter 1: A Sea Of Microbes: What’s So Special About Marine Microbiology -- Part I: Diversity And Evolution Of Marine Microorganisms -- Chapter 2: Survival In A Sea Of Gradients: Bacterial And Archaeal Foraging In A Heterogeneous Ocean -- Chapter 3: Marine Cyanobacteria -- Chapter 4: Marine Protists: A Hitchhiker’s Guide To Their Role In The Marine Microbiome -- Chapter 5: Marine Fungi -- Chapter 6: Marine Viruses: Agents Of Chaos, Promoters Of Order -- Chapter 7: Evolutionary Genomics Of Marine Bacteria And Archaea -- Part II: Marine Habitats -- Chapter 8: Towards A Global Perspective Of The Marine Microbiome -- Chapter 9: The Pelagic Light-Dependent Microbiome -- Chapter 10: Microbial Inhabitants Of The Dark Ocean -- Chapter 11: The Subsurface And Oceanic Crust Prokaryotes -- Chapter 12: The Microbiome Of Coastal Sediments -- Chapter 13: Symbiosis In The Ocean Microbiome -- Chapter 14: Marine Extreme Habitats -- Part III: Marine Microbiome From Genomes To Phenomes: Biogeochemical Cycles, Networks, Fluxes, And Interaction -- Chapter 15: Marine Biogeochemical Cycles -- Chapter 16: A Holistic Approach For The Study Of The Role Of Microorganisms In The Marine Ecosystem -- Chapter 17: The Hidden Treasure: Marine Microbiome As Repository Of Bioactive Compounds -- Chapter 18: Ocean Restoration And The Strategic Plan Of The Marine Microbiome. .

Description / Table of Contents: Chapter1. Introduction to Indian Late Cretaceous-Early Palaeocene Microbiota from the Deccan Intertrappean Beds of the Chhindwara District, Madhya Pradesh, India -- Chapter 2. Historical Background of Late Cretaceous-Early Palaeocene Microbiotic Assemblages from the Deccan Intertrappean Beds of the Chhindwara District, Madhya Pradesh, India -- Chapter 3. Geology and Stratigraphy of Microbiota-Bearing Deccan Intertrappean Beds of the Chhindwara District, Madhya Pradesh, India -- Chapter 4. Indian Late Cretaceous-Early Palaeocene Deccan Microbiota from Chhindwara District, Madhya Pradesh: Systematic Studies -- Chapter 5 Palaeoecological and Palaeoenvironmental Implications of the Cretaceous-Palaeogene Microbiota-Bearing Deccan Intertrappean beds of the Chhindwara District, Madhya Pradesh, India -- Chapter 6. Palaeobiogeographical Implications of Late Cretaceous-Early Palaeocene Microbiota from the Deccan Intertrappean beds of the Chhhindwara District, Madhya Pradesh, India.

Description / Table of Contents: Introduction: Transport and mobility situations of African cities -- Part 1: Urban form, accessibility and travel demand -- Urban form, accessibility and travel demand in African cities: An introduction -- Urban form and access to public transport in Accra, Ghana -- Disparities in public transport coverage and bus service quality in Algiers -- An Analysis of transportation demand Patterns in Ghana -- Part 2: Transport poverty, equity and inclusion -- Transport poverty and social divisions in African cities: An introduction -- Mobility regimes and equity in urban transport: Examining women’s mobility experiences in Accra -- Community severance in urban Africa -- Transport poverty, distance covered to access to basic infrastructures and modal choice in urban areas in Cameroon -- Conceptualizing an urban transport framework for enhanced residential quality of life in Sub-Saharan Africa: Case study of Ghana and Namibia -- Part 3: Public transport policy and governance -- Public transport policy and governance in African cities: An introduction -- Bus rapid transit implementation in African cities: The case for a more incremental reform approach -- Pricing transport services in urban Ghana – The politics and socio-spatial conflicts between transport operators and the state -- Safe, inclusive public transport in Africa - Challenges and opportunities identified in Ghana and Namibia -- Part 4: Non-motorized transport and traffic safety -- Non-motorized transport and traffic safety in African cities: An introduction -- Planning for walkability in Johannesburg -- Exploring barriers and prospects of bicycle transportation: A case study of a Ghanaian University campus -- The provision of NMT in the City of Lusaka: An analysis of policy and practice -- The future of non-motorized transport in Urban Africa -- Part 5: ICT, platforms and new technologies -- ICTs, digital platform mobility services, and transport de-carbonization in African cities: An introduction -- Opportunities and challenges for addressing personal safety concerns on public transport through ICTs in South African cities -- Smart mobility in urban Africa: Geography of diffusion, user characteristics and emerging impacts of digital platform/app-based mobility services -- e-Quantum leap: Planning for electric minibus taxis in sub-Saharan Africa’s paratransit system -- Conclusion: What futures for transport and mobility in African cities?

Description / Table of Contents: Preface -- Chapter 1 Fundamentals of Adsorption -- Chapter 2 Methods of Synthesis of Magnetic Adsorbents -- Chapter 3 Magnetic Biosorbents and their Application in Water Remediation -- Chapter 4 Lignocellulosic Wastes as Precursor of carbonaceous magnetic adsorbents of organic and inorganic pollutants adsorption -- Chapter 5 Magnetic Biochar Fibers for Copper Removal -- Chapter 6 Treatment of Landfill Leachate with Magnetic Adsorbents -- Chapter 7 Removal of Emerging Pollutants and Toxic Metals using Magnetic Adsorbents -- Chapter 8 Magnetically Modified Biological Materials for Dyes Removal -- Chapter 9 Regeneration of magnetic adsorbents saturated by organic pollutants using advanced oxidation technologies -- Chapter 10 Magnetic Nanofibers for Contaminants Removal from Water -- Chapter 11 Magnetic solid phase-based sorbents for isolation/pre-concentration and removal of pesticides -- Chapter 12 Characterization and application of Fe-magnetic materials and nanomaterials for application in the aqueous matrices decontamination -- Chapter 13 Advanced Magnetic Adsorbents Prepared from Emulsion Template for Water Treatment -- Chapter 14 Chitosan Based Magnetic Adsorbents -- Chapter 15 Methods used for performance enhancement of iron based magnetic adsorbents in water systems.

Description / Table of Contents: Abstract The Palaeozoic Era ends with the c. 47-million-year-long Permian Period. This was a major juncture in Earth history when the vast Pangean supercontinent continued its assembly and the global biota suffered the most extensive biotic decimation of the Phanerozoic, the end-Permian mass extinction. It was also the time of accumulation of vast mineral and energy deposits, notably of salt and petroleum. The temporal ordering of geological and biotic events during Permian time is, therefore, critical to the interpretation of some unique and pivotal events in Earth history. This temporal ordering is based mostly on the Permian timescale, which has been developed and refined for nearly two centuries. This book reviews the history of the development of the Permian chronostratigraphic scale. It also includes comprehensive analyses of Permian radioisotopic ages, magnetostratigraphy, isotope-based correlations, and timescale-relevant marine and non-marine biostratigraphy and biochronology.

Description / Table of Contents: Over the last decades, the rate of near-surface warming in the Arctic is at least double than elsewhere on our planet (Arctic amplification). However, the relative contribution of different feedback processes to Arctic amplification is a topic of ongoing research, including the role of aerosol and clouds. Lidar systems are well-suited for the investigation of aerosol and optically-thin clouds as they provide vertically-resolved information on fine temporal scales. Global aerosol models fail to converge on the sign of the Arctic aerosol radiative effect (ARE). In the first part of this work, the optical and microphysical properties of Arctic aerosol were characterized at case study level in order to assess the short-wave (SW) ARE. A long-range transport episode was first investigated. Geometrically similar aerosol layers were captured over three locations. Although the aerosol size distribution was different between Fram Strait(bi-modal) and Ny-Ålesund (fine mono-modal), the atmospheric column ARE was similar. The latter was related to the domination of accumulation mode aerosol. Over both locations top of the atmosphere (TOA) warming was accompanied by surface cooling. Subsequently, the sensitivity of ARE was investigated with respect to different aerosol and spring-time ambient conditions. A 10% change in the single-scattering albedo (SSA) induced higher ARE perturbations compared to a 30% change in the aerosol extinction coefficient. With respect to ambient conditions, the ARETOA was more sensitive to solar elevation changes compared to AREsur f ace. Over dark surfaces the ARE profile was exclusively negative, while over bright surfaces a negative to positive shift occurred above the aerosol layers. Consequently, the sign of ARE can be highly sensitive in spring since this season is characterized by transitional surface albedo conditions. As the inversion of the aerosol microphysics is an ill-posed problem, the inferred aerosol size distribution of a low-tropospheric event was compared to the in-situ measured distribution. Both techniques revealed a bi-modal distribution, with good agreement in the total volume concentration. However, in terms of SSA a disagreement was found, with the lidar inversion indicating highly scattering particles and the in-situ measurements pointing to absorbing particles. The discrepancies could stem from assumptions in the inversion (e.g. wavelength-independent refractive index) and errors in the conversion of the in-situ measured light attenuation into absorption. Another source of discrepancy might be related to an incomplete capture of fine particles in the in-situ sensors. The disagreement in the most critical parameter for the Arctic ARE necessitates further exploration in the frame of aerosol closure experiments. Care must be taken in ARE modelling studies, which may use either the in-situ or lidar-derived SSA as input. Reliable characterization of cirrus geometrical and optical properties is necessary for improving their radiative estimates. In this respect, the detection of sub-visible cirrus is of special importance. The total cloud radiative effect (CRE) can be negatively biased, should only the optically-thin and opaque cirrus contributions are considered. To this end, a cirrus retrieval scheme was developed aiming at increased sensitivity to thin clouds. The cirrus detection was based on the wavelet covariance transform (WCT) method, extended by dynamic thresholds. The dynamic WCT exhibited high sensitivity to faint and thin cirrus layers (less than 200 m) that were partly or completely undetected by the existing static method. The optical characterization scheme extended the Klett–Fernald retrieval by an iterative lidar ratio (LR) determination (constrained Klett). The iterative process was constrained by a reference value, which indicated the aerosol concentration beneath the cirrus cloud. Contrary to existing approaches, the aerosol-free assumption was not adopted, but the aerosol conditions were approximated by an initial guess. The inherent uncertainties of the constrained Klett were higher for optically-thinner cirrus, but an overall good agreement was found with two established retrievals. Additionally, existing approaches, which rely on aerosol-free assumptions, presented increased accuracy when the proposed reference value was adopted. The constrained Klett retrieved reliably the optical properties in all cirrus regimes, including upper sub-visible cirrus with COD down to 0.02. Cirrus is the only cloud type capable of inducing TOA cooling or heating at daytime. Over the Arctic, however, the properties and CRE of cirrus are under-explored. In the final part of this work, long-term cirrus geometrical and optical properties were investigated for the first time over an Arctic site (Ny-Ålesund). To this end, the newly developed retrieval scheme was employed. Cirrus layers over Ny-Ålesund seemed to be more absorbing in the visible spectral region compared to lower latitudes and comprise relatively more spherical ice particles. Such meridional differences could be related to discrepancies in absolute humidity and ice nucleation mechanisms. The COD tended to decline for less spherical and smaller ice particles probably due to reduced water vapor deposition on the particle surface. The cirrus optical properties presented weak dependence on ambient temperature and wind conditions. Over the 10 years of the analysis, no clear temporal trend was found and the seasonal cycle was not pronounced. However, winter cirrus appeared under colder conditions and stronger winds. Moreover, they were optically-thicker, less absorbing and consisted of relatively more spherical ice particles. A positive CREnet was primarily revealed for a broad range of representative cloud properties and ambient conditions. Only for high COD (above 10) and over tundra a negative CREnet was estimated, which did not hold true over snow/ice surfaces. Consequently, the COD in combination with the surface albedo seem to play the most critical role in determining the CRE sign over the high European Arctic.