Academic literature on the topic 'Macro fossil analysis'

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Journal articles on the topic "Macro fossil analysis"

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Halsall, Karen M., Vanessa M. Ellingsen, Johan Asplund, Richard HW Bradshaw, and Mikael Ohlson. "Fossil charcoal quantification using manual and image analysis approaches." Holocene 28, no. 8 (May 14, 2018): 1345–53. http://dx.doi.org/10.1177/0959683618771488.

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Charcoal particles are evidence of past fire events and macro-charcoal particles have been shown to represent local fire events. There are several methods for the preparation and quantification of macro-charcoal particles, none of which have been universally accepted as standard. Very few studies compare methodological differences and no studies to date compare quantification by mass with quantification by volume using image analysis. Using three cores taken from a peatland located in SE Norway, we compare these two established methods using a generalized linear mixed model (GLMM) and a split-plot ANOVA test. We show that charcoal volume (image analysis method) was a better predictor of charcoal mass than charcoal particle number and the same size classes of charcoal as size class distributions were not spatially and temporally correlated. Although there is still a need for a common and unifying method, our results show that quantification of charcoal particles by image analysis including size (e.g. height in mm) and area (mm2)/volume (mm3) measurements provides more significant results in cross-site or multiple-site studies than quantifications based on particle number. This has implications for the interpretation of charcoal data from regional studies that are used to model drivers of wildfire activity and environmental change in boreal–temperate landscapes during the Holocene.
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Aslani, Alireza, Mohsen Rezaee, and Seyed Mostafa Mortazavi. "Analysis of the Robustness of Australia Economy and Energy Supply/Demand Fluctuation." Present Environment and Sustainable Development 11, no. 2 (October 1, 2017): 35–48. http://dx.doi.org/10.1515/pesd-2017-0023.

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Abstract Energy has a strategic role in social and economic development of the countries. Due to the high dependency of energy supply to fossil fuels, fluctuations in prices and supply have macro/micro-economics effects for both energy exporters and importers. Therefore, understanding economic stability based on energy market changes is an important subject for policy makers and researchers. As the competitiveness of Australia products/services has high dependency on energy prices, analyzing the relationships of economics robustness with fossil fuel fluctuations is important for the policy makers and researchers. In this paper, the researchers investigate the effects of energy changes on Australian economics. In this regard, first, the impact of oil price on macro-economic parameters is discussed. After that, the main issues related to energy economics including resilience of the energy sector, energy policies, economics analysis of the energy sector, electricity markets are discussed.
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Pandita, Hita, and Gendoet Hartono. "Identification and Stratiraphic Position of Mollusk Type Locality at West Progo Stage." Journal of Geoscience, Engineering, Environment, and Technology 4, no. 2 (June 30, 2019): 76. http://dx.doi.org/10.25299/jgeet.2019.4.2.2682.

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The location of the discovery of mollusk fossils on the island of Java is spread in various places. One location is in the Kulon Progo region known as West Progo beds. However, due to the lack of studies of mollusk fossils in the Kulon Progo region, this resulted in a lack of understanding of the location of the discovery. This study was intended to re-record the location of fossil molluscs discovery in the Kulon Progo region, with the aim of contributing to the stratigraphic arrangement in Kulon Progo. Research methods include literature studies, field investigations and laboratory analysis. The literature study includes libraries of the Dutch colonial era regarding the location of the discovery of mollusk fossils. Field studies in the form of stratigraphic measurements and sampling. Laboratory investigations include petrographic observations and identification of micro and macro fossils. The results of the investigation successfully re-identified the Kembang Sokkoh and Spolong locations which are two types of locations on the West Progo beds. Based on the lithological characteristics of the two locations included in the Jonggrangan Formation, with the Lower Miocene age based on an analysis of the fossil content of the molluscs.
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Aslani, Alireza, Maryam Hamlehdar, and Reza Saeedi. "Robustness of Norway Economy and Energy Supply/Demand." International Journal of Green Computing 8, no. 2 (July 2017): 1–19. http://dx.doi.org/10.4018/ijgc.2017070101.

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Energy has a strategic role in the social and economic development of the countries all over the world. Due to the high dependency on fossil fuels, fluctuations in prices and supply have macro/micro-economics effects for both energy exporters and importers. Therefore, understanding economic stability based on energy market changes is an important subject for policy makers and researchers. Norway, as a fossil fuel export country, is a good choice for the analysis of the relationships between the economics robustness and fossil fuel economics fluctuations. While the country is one of the pioneers in the field of sustainable energy utilization, they have tried to provide a robust economic situation for the oil exports revenues. In this article, the effects of energy changes on the economy are investigated in Norway. In this regard, first, the impact of oil price on macro-economic parameters is discussed. Afterwards, the main issues related to the energy economics including resilience of the energy sector, energy policies, economics analysis of the energy sector, and the electricity markets are discussed.
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Allison, Peter A. "The role of anoxia in the decay and mineralization of proteinaceous macro-fossils." Paleobiology 14, no. 2 (1988): 139–54. http://dx.doi.org/10.1017/s009483730001188x.

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Actualistic experiments have quantified rate of anaerobic decay and associated mineralization around proteinaceous macro-organisms. Carcasses of the polychaete wormNereisand the eumalacostracansNephropsandPalaemonwere buried in airtight glass jars filled with sediment and water from marine, brackish, and lacustrine environments. Over a period of 25 weeks the contents were examined to determine the state of decay and were chemically analyzed to monitor early diagenetic mineralization (two methods for such analysis are reviewed). Decay processes were active in the experimental conditions despite anoxia and had virtually destroyed the carcasses within 25 weeks. However, decay-rate in the sulfate-reducing marine system was greater than in the methanogenic freshwater environments. Petrological and geochemical analyses of the organic remains identified discrete layers of authigenic iron monosulfide (a pyrite precursor) on the surface of the decayingNephropscuticle within weeks of initiating the experiment. Chemical analysis of decomposing flesh showed a marked increase in pore-water calcium content with time.The results clearly show that anoxia is ineffective as a long-term conservation medium in the preservation of soft-bodied fossils. However, decay-induced mineralization can be very rapid so that even a slight reduction in decay rate can lead to improved levels of fossil preservation. Traditionally, stagnation and rapid burial are considered to be the main prerequisites for the preservation of soft-bodied fossils and the formation ofKonservat-Lagerstätten. Clearly these factors are only important in that they promote early diagenetic mineralization. This is the only way to halt information loss through decay.
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Bernardová, Alexandra, and Jiří Košnar. "What do Holocene sediments in Petuniabukta, Spitsbergen reveal?" Polish Polar Research 33, no. 4 (December 1, 2012): 329–45. http://dx.doi.org/10.2478/v10183-012-0023-2.

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Abstract Studies of past vegetation from the inner fjords of the Svalbard archipelago have not previously been reported. This study assesses the potential of sediments retrieved from two sites in Petuniabukta, Billefjorden to track vegetation response to Quaternary climate change. The first sediment profile was retrieved from periodic lake on a 4 m a.s.l. marine terrace with a basal radiocarbon dated to 5 080 ± 30 BP, the second was retrieved from a de- pression in wet tundra on a 24m a.s.l. marine terrace, which upper part was dated to 9 470 ± 30 BP. The study is primarily focused on macro- and micro-fossils. Pollen grains are pres- ent in very low concentrations. Macro-fossils were represented mostly by leafs and buds of Salix species and Dryas octopetala as well as the hybrid Salix herbacea x polaris. Fossil moss remains represent an important part of arctic ecosystems. Tardigrada remains were found in the sediments in high abundance whilst eggs and exuviae of at least six species were identified. The sediments are definitely suitable for the reconstruction of past condi- tions. However, it is necessary to take care not to focus at single type of analysis, as pollen analysis appeared uninformative and more information was obtained from plant macro- fossils (mosses, vascular plants). Little attention has been given to Tardigrada in the past, as they were overlooked and the preservation in sediments is usually very low.
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Chatterjee, Elizabeth. "The Asian Anthropocene: Electricity and Fossil Developmentalism." Journal of Asian Studies 79, no. 1 (September 10, 2019): 3–24. http://dx.doi.org/10.1017/s0021911819000573.

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Much scholarship extrapolates global narratives of the Anthropocene from the “fossil capitalism” of European imperial powers. This analysis deploys the alternative lens of grid electricity—the great macro-technology of the twentieth century—to reevaluate the dynamics of the Anthropocene outside the Anglozone. Histories of Asian electrification refute the notion of any simple relationship between colonialism and fossil capitalism. Instead, they point towards a postcolonial trend of fossil developmentalism. Especially in the context of late development, energy expansion became a state-led moral project. Cutting against fossil capitalism's logic of commodification, electricity provision was increasingly conceptualized as a national good and an entitlement, even if one honored in the breach. This trend transcended the distinction between market and planned economies, and extended beyond formal democracies. The (partial) democratization of consumption brought by fossil developmentalism is the hallmark of the “Great Acceleration” in human impacts on the environment since 1950.
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Aslani, Alireza, Morteza Niknejad, and Amin Maghami. "Robustness of US Economy and Energy Supply/Demand Fluctuations." International Journal of Energy Optimization and Engineering 6, no. 4 (October 2017): 1–15. http://dx.doi.org/10.4018/ijeoe.2017100101.

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Energy has a strategic role in social and economic development of the countries. Due to the high dependency of energy supply on fossil fuels, fluctuations in prices and supply have macro/micro-economics effects for both energy exporters and importers. Therefore, understanding economic stability based on energy market changes is an important subject for policy makers and researchers. The US, as the first energy consumer in the world, is an interesting country to analyze the relationships of economics robustness with fossil fuel economic-fluctuations. While the country has one of the pioneers in domestic energy utilization, the competitiveness of the country is highly dependent on energy prices. In this paper, the researchers investigate the effects of energy changes on the economics of the US. First, the impact of oil price on macro-economic parameters is discussed. After that, the main issues related to energy economics including resilience of the energy sector, energy policies, economics analysis of the energy sector, electricity markets are discussed.
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Gilardoni, S., E. Vignati, F. Cavalli, J. P. Putaud, B. R. Larsen, M. Karl, K. Stenström, J. Genberg, S. Henne, and F. Dentener. "Better constraints on sources of carbonaceous aerosols using a combined <sup>14</sup>C – macro tracer analysis in a European rural background site." Atmospheric Chemistry and Physics Discussions 11, no. 1 (January 24, 2011): 2503–47. http://dx.doi.org/10.5194/acpd-11-2503-2011.

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Abstract. The source contributions to carbonaceous PM2.5 aerosol were investigated at a European background site at the edge of the Po Valley, in Northern Italy, during the period January–December 2007. Carbonaceous aerosol was described as the sum of eight source components: primary (1) and secondary (2) biomass burning organic carbon, biomass burning elemental carbon (3), primary (4) and secondary (5) fossil fuel burning organic carbon, fossil fuel burning elemental carbon (6), primary (7) and secondary (8) biogenic organic carbon. The concentration of each component was quantified using a set of macro tracers (organic carbon OC, elemental carbon EC, and levoglucosan), micro tracers (arabitol and mannitol), and 14C measurements. This was the first time that 14C measurements were performed on a long time series of data able to represent the entire annual cycle. This set of 6 tracers, together with assumed uncertainty ranges of the ratios of OC-to-EC, and the fraction of modern carbon in the 8 source categories, provides strong constraints to the source contributions to carbonaceous aerosol. The uncertainty of contributions was assessed with a Quasi-Monte Carlo (QMC) method accounting for the variability of OC and EC emission factors, and the uncertainty of reference fractions of modern carbon. During winter biomass burning composed 50% of the total carbon (TC) concentration, while in summer secondary biogenic OC accounted for 45% of TC. The contribution of primary biogenic aerosol particles was negligible during the entire year. Moreover, aerosol associated with fossil fuel burning represented 26% and 43% of TC in winter and summer, respectively. The comparison of source apportionment results in different urban and rural areas showed that the sampling site was mainly affected by local aerosol sources during winter and regional air masses from the nearby Po Valley in summer. This observation was further confirmed by back-trajectory analysis applying the Potential Source Contribution Function method to identify potential source regions. The contribution of secondary organic aerosol (SOA) to the organic mass (OM) was significant during the entire year. SOA accounted for 23% and 83% of OM during winter and summer, respectively. While the summer SOA was dominated by biogenic sources, winter SOA was mainly due to biomass and fossil fuel burning. This indicates that the oxidation of intermediate volatility organic compounds co-emitted with primary organics is a significant source of SOA, as suggested by recent model results and Aerosol Mass Spectrometer measurements in urban regions. Comparison with previous global model simulations, indicates a strong underestimate of wintertime primary aerosol emissions in this region.
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Gilardoni, S., E. Vignati, F. Cavalli, J. P. Putaud, B. R. Larsen, M. Karl, K. Stenström, J. Genberg, S. Henne, and F. Dentener. "Better constraints on sources of carbonaceous aerosols using a combined <sup>14</sup>C – macro tracer analysis in a European rural background site." Atmospheric Chemistry and Physics 11, no. 12 (June 20, 2011): 5685–700. http://dx.doi.org/10.5194/acp-11-5685-2011.

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Abstract. The source contributions to carbonaceous PM2.5 aerosol were investigated at a European background site at the edge of the Po Valley, in Northern Italy, during the period January–December 2007. Carbonaceous aerosol was described as the sum of 8 source components: primary (1) and secondary (2) biomass burning organic carbon, biomass burning elemental carbon (3), primary (4) and secondary (5) fossil organic carbon, fossil fuel burning elemental carbon (6), primary (7) and secondary (8) biogenic organic carbon. The mass concentration of each component was quantified using a set of macro tracers (organic carbon OC, elemental carbon EC, and levoglucosan), micro tracers (arabitol and mannitol), and 14C measurements. This was the first time that 14C measurements covered a full annual cycle with daily resolution. This set of 6 tracers, together with assumed uncertainty ranges of the ratios of OC-to-EC, and the reference fraction of modern carbon in the 8 source categories, provides strong constraints to the source contributions to carbonaceous aerosol. The uncertainty of contributions was assessed with a Quasi-Monte Carlo (QMC) method accounting for the variability of OC and EC emission factors, the uncertainty of reference fractions of modern carbon, and the measurement uncertainty. During winter, biomass burning composed 64 % (±15 %) of the total carbon (TC) concentration, while in summer secondary biogenic OC accounted for 50 % (±16 %) of TC. The contribution of primary biogenic aerosol particles was negligible during the entire year. Moreover, aerosol associated with fossil sources represented 27 % (±16 %) and 41 % (±26 %) of TC in winter and summer, respectively. The contribution of secondary organic aerosol (SOA) to the organic mass (OM) was significant during the entire year. SOA accounted for 30 % (±16 %) and 85 % (±12 %) of OM during winter and summer, respectively. While the summer SOA was dominated by biogenic sources, winter SOA was mainly due to biomass burning and fossil sources. This indicates that the oxidation of semi-volatile and intermediate volatility organic compounds co-emitted with primary organics is a significant source of SOA, as suggested by recent model results and Aerosol Mass Spectrometer measurements. Comparison with previous global model simulations, indicates a strong underestimate of wintertime primary aerosol emissions in this region. The comparison of source apportionment results in different urban and rural areas showed that the sampling site was mainly affected by local aerosol sources during winter and regional air masses from the nearby Po Valley in summer. This observation was further confirmed by back-trajectory analysis applying the Potential Source Contribution Function method to identify potential source regions.
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Dissertations / Theses on the topic "Macro fossil analysis"

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Pettersson, Siri. "Makrofossilanalys som ekologiskt verktyg : En metodutvärdering." Thesis, Uppsala universitet, Institutionen för biologisk grundutbildning, 2017. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-321511.

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Approximately 50 percent of all endangered species in Scandinavia are associated with old agricultural landscapes. During the agricultural industrialization of the past century the traditional practices and methods that created these environments have been phased out. This has brought on a serious decline and fragmentation of biomes that many endangered species depend on. Knowledge of traditional agricultural landscapes and their species dynamics is needed to make well informed decisions regarding their care and restoration. One way to acquire such knowledge is to study fossil plant remnants from old agricultural contexts. In this study sub-fossil Cyperaceae achenes were analyzed in an attempt to identify them. The achenes had been preserved in three Iron Age wells (80-980 AD) at the Gilltuna settlement in central Sweden and were found during an archeological investigation in 2010. The purpose of this study was to identify the achenes to species level, make conclusions about the ecology of the surrounding landscape, and construct simple species identification key as well as evaluate archaeobotany as an ecological tool. The identification attempt resulted in 14 determined species, which were in consistency with previous landscape analyses made using ecological species distribution. The resulting identification key is a suggestion, to be expanded in the future. This method can undoubtedly provide further knowledge of prehistoric and historical biomes, but in order to draw useful conclusions the identification technique further as well as knowledge of present regional ecology must be developed, especially concerning different Cyperaceae species‟ response to different kinds of stress.
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Book chapters on the topic "Macro fossil analysis"

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Hamledar, Maryam, Reza Saeidi, and Alireza Aslani. "Analysis of the Robustness of Norway's Economy and Energy Supply/Demand Fluctuations." In Economic Dynamics of Global Energy Geopolitics, 215–41. IGI Global, 2019. http://dx.doi.org/10.4018/978-1-5225-4203-2.ch011.

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The high dependency on fossil fuels, fluctuations in prices and supply have macro/micro-economics effects for both energy exporters and importers. Therefore, understanding economic stability based on energy market changes is an important subject for policymakers and researchers. Norway, as a fossil fuel exporting country, is a good choice for the analysis of the relationships between economic robustness and fossil fuel economic fluctuations. While the country is one of the pioneers in the field of sustainable energy utilization, they have tried to provide a robust economic environment for oil export revenues. In this chapter, the impacts of energy changes on the economy are investigated in Norway. In this regard, first, the impact of oil prices on macro-economic parameters is discussed. Afterwards, the main issues related to energy economics including resilience of the energy sector, energy policies, economics analysis of the energy sector, and the electricity markets are discussed.
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"Macro Studies of FOSS Ecology." In Free and Open Source Software in Modern Data Science and Business Intelligence, 58–66. IGI Global, 2018. http://dx.doi.org/10.4018/978-1-5225-3707-6.ch002.

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The ecology of Free and Open Source Software (FOSS) is dotted by projects of every kind ranging from small desktop applications to large mission critical systems. To enable maximum visibility among the developer community, these projects are often hosted in community project management portals. The current work studies one such portal, sourceforge.net by analyzing the data of 200,000 projects and 2 million developers for the period Feb 2005 to Aug 2009. The scope of the present study includes the analysis of developer contribution. The slow growth rate of developer community and high number of single developer projects are the major findings of the present work.
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Rivadeneira, Marcelo M., and Gary C. B. Poore. "Latitudinal Gradient of Diversity of Marine Crustaceans: TOWARDS a Synthesis." In Evolution and Biogeography, 389–412. Oxford University Press, 2020. http://dx.doi.org/10.1093/oso/9780190637842.003.0015.

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The latitudinal diversity gradient (LDG) is a phenomenon acknowledged for over two centuries. The LDG of marine crustaceans has been studied often but without reaching consensus on its ultimate causative processes. We have undertaken a new synthesis to assess the generality of the LDG and evaluated how potential sampling and other biases, spatial scale, geographic regions, taxonomic aggregation, and differences between clades affect patterns. A meta-analysis of 186 datasets, encompassing 20 studies and 7 crustacean orders, revealed a strong effect size of the species richness-latitude correlation, supporting the existence of a “canonical” LDG. The effect size was sensitive to spatial scale, with studies conducted over shorter latitudinal ranges tending to show a weaker LDG. Correcting for sampling biases in the number of occurrences, taxonomic completeness and spatial heterogeneity did not affect the strength of the LDG, nor did the degree of taxonomic aggregation; effect sizes were similar at family and ordinal levels. However, between orders effect sizes varied strongly, with peracarid orders (Amphipoda, Cumacea, Isopoda) showing a weaker or inverse LDG compared with non-peracarid orders (Calanoida, Euphausiacea, Decapoda, Sessilia). Additional analyses based on a global dataset of >2 million occurrences of >13,000 species revealed patterns undetected by the meta-analysis, including: (1) the existence of a marked bi-modal LDG, with peaks of diversity in subtropical areas (Calanoidea, Decapoda, Sessilia) and in temperate areas (Amphipoda, Isopoda), (2) interhemispheric asymmetry, variable across groups and depths, and (3) ocean basin differences in the shape of the LDG, dependent on taxonomic clade. Both ecological and evolutionary processes play a part. The fossil record of Decapoda showed that its global canonical LDG can be explained by median and range of the age of genera, i.e., hotspots of diversity harbor both younger and older genera and contain a high proportion of genera originating during the Paleogene. In addition, the effect size was negatively related to family age, the LDG being stronger in older families of early Cenozoic and Mesozoic origin. Modes of larval development also played a significant part, taxa without planktonic larvae having weaker or inverse LDG compared with taxa with pelagic larvae. Because clades with direct development tend to show smaller bathymetric and latitudinal ranges than those with pelagic larvae, differences in diversification rates may be implied. Overall, our evidence suggested that the ultimate causes of the LDG are deeply tied to geographic differences in macro-evolutionary rates, i.e., greater rates of species origin and lower rates of extinction in the tropics than in higher latitudes combined with a strong tropical niche conservatism.
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Conference papers on the topic "Macro fossil analysis"

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Maretto, Marco, Barbara Gherri, Greta Pitanti, and Francesco Scattino. "Urban Morphology and Sustainability: towards a shared design methodology." In 24th ISUF 2017 - City and Territory in the Globalization Age. Valencia: Universitat Politècnica València, 2017. http://dx.doi.org/10.4995/isuf2017.2017.5695.

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The information revolution is radically transforming the very foundation of the ‘fossil city’. A ‘virtual’ macro-urbanism will intersect with an ‘actual’ micro-urbanism, physical and concrete, determining the form of the new urban environment. Within the binomial of macro- and micro- urbanism, urban morphology identifies an interesting socio-building scale that can serve as the basic strategy for sustainable city planning in the twenty-first century. Morphology thus becomes the necessary ‘plug-in’ for registering the different ‘networks’ that characterize the contemporary city – from IT and ‘smart’ devices to energy and environmental systems - translating these networks into building practices, into ‘fabrics’, for the physical city. At this purpose an Urban Design methodology has been developed in order to combine the Urban Morphology tools with those of Sustainability giving particular attention to the topics of the comfort outdoor and the passive environmental control systems. The methodology has then been applied in the Sant Adrià De Besos Waterfront Regeneration Project in Barcelona. Neighbourhood’s size, complexity and localisation, between the sea and a large area of brown fields at the northern gateway of the Catalan capital, has set up an interesting testing bench. A sequence of consecutive steps characterizes the methodology in which morphology, architecture and sustainability intersect one another within a single design process. References Gherri B. (2015) Assessment of Daylight Performance in Buildings: Methods and Design Strategies, (WIT Press, Boston). Gherri, B. (2016) ‘Environmental Analysis Towards Low Carbon Urban Retrofitting For Public Spaces’, Proceedings of HERITAGE 2016 – 5th International Conference on Heritage and Sustainable Development,Vol. 1, p. 499-508. Marat-Mendes, T. (2013) ‘Sustainability and the study of urban form’, Urban Morphology 17, 123-4. Maretto, M. (2014) ‘Sustainable Urbanism: the role of urban morphology’, Urban Morphology 18(2), 163-74. Maretto, M. (2013) Ecocities. Il progetto urbano tra morfologia e sostenibilità (Franco Angeli, Roma).
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