Low-temperature magnetic remanence and hysteresis measurements on sediment core GeoB4901-8 from the Niger deep-sea fan

Low-temperature (LT) magnetic remanence and hysteresis measurements, in the range 300-5 K, were combined with energy dispersive spectroscopy (EDS) in order to characterize the magnetic inventory of strongly diagenetically altered sediments originating from the Niger deep-sea fan. We demonstrate the possibility of distinguishing between different compositions of members of the magnetite-ulvöspinel and ilmenite-hematite solid solution series on a set of five representative samples, two from the upper suboxic and three from the lower sulfidic anoxic zone of gravity core GeoB 4901. Highly sensitive LT magnetic measurements were performed on magnetic extracts resulting in large differences in the magnetic behavior between samples from the different layers. This emphasizes that both Fe-Ti oxide phases occur in different proportions in the two geochemical environments. Most prominent are variations in the coercivity sensitive parameter coercive field (BC). At room-temperature (RT) hysteresis loops for all extracts are narrow and yield low coercivities (6-13 mT). With decreasing temperature the loops become more pronounced and wider. At 5 K an approximately 5-fold increase in BC for the suboxic samples contrasts a 20-25-fold increase for the samples from the anoxic zone. We demonstrate that this distinct increase in BC at LT corresponds to the increasing proportion of the Ti-rich hemoilmenite phase, while Fe-rich (titano-)magnetite dominates the magnetic signal at RT. This trend is also seen in the room-temperature saturation isothermal remanent magnetization (RT-SIRM) cycles: suboxic samples show remanence curves dominated by Fe-rich mineral phases while anoxic samples display curves clearly dominated by Ti-rich particles. We show that the EDS intensity ratios of the characteristic Fe Kalpha and Ti Kalpha lines of the Fe-Ti oxides may be used to differentiate between members of the magnetite-ulvöspinel and ilmenite-hematite solid solution series. Furthermore it is possible to calculate an approximate composition for each grain if the intensity ratios of natural particles are linked to well-known standards. Thus, element spectra with high Fe/Ti intensity ratios were found to be rather typical of titanomagnetite while low Fe/Ti ratios are indicative of hemoilmenite. The EDS analyses confirm the LT magnetic results, Fe-rich magnetic phases dominate in the upper suboxic environment whereas Ti-rich magnetic phases comprise the majority of particles in the lower anoxic domain: The mineral assemblage of the upper suboxic environments is composed of magnetite (~19%), titanomagnetite (~62%), hemoilmenite (~17%) and ~2% other particles. In the lower anoxic sediments, reductive diagenetic alteration has resulted in more extensive depletion of the (titano-)magnetite phase, resulting in a relative enrichment of the hemoilmenite phase (~66%). In these strongly anoxic sediments stoichiometric magnetite is barely preserved and only ~5% titanomagnetite was detected. The remaining ~28% comprises Ti-rich particles such as pseudobrookite or rutile.

(Table 2) Composition of the deapest pore fluids from ODP Holes 168-1030B and 168-1031A

On the eastern flank of the Juan de Fuca Ridge, reaction between upwelling basement fluid and sediment alters hydrothermal fluxes of Ca, SiO2(aq), SO4, PO4, NH4, and alkalinity. We used the Global Implicit Multicomponent Reactive Transport (GIMRT) code to model the processes occurring in the sediment column (diagenesis, sediment burial, fluid advection, and multicomponent diffusion) and to estimate net seafloor fluxes of solutes. Within the sediment section, the reactions controlling the concentrations of the solutes listed above are organic matter degradation via SO4 reduction, dissolution of amorphous silica, reductive dissolution of amorphous Fe(III)-(hydr)oxide, and precipitation of calcite, carbonate fluorapatite, and amorphous Fe(II)-sulfide. Rates of specific discharge estimated from pore-water Mg profiles are 2 to 3 mm/yr. At this site the basement hydrothermal system is a source of NH4, SiO2(aq), and Ca, and a sink of SO4, PO4, and alkalinity. Reaction within the sediment column increases the hydrothermal sources of NH4 and SiO2(aq), increases the hydrothermal sinks of SO4 and PO4, and decreases the hydrothermal source of Ca. Reaction within the sediment column has a spatially variable effect on the hydrothermal flux of alkalinity. Because the model we used was capable of simulating the observed pore-water chemistry by using mechanistic descriptions of the biogeochemical processes occurring in the sediment column, it could be used to examine the physical controls on hydrothermal fluxes of solutes in this setting. Two series of simulations in which we varied fluid flow rate (1 to 100 mm/yr) and sediment thickness (10 to 100 m) predict that given the reactions modeled in this study, the sediment section will contribute most significantly to fluxes of SO4 and NH4 at slow flow rates and intermediate sediment thickness and to fluxes of SiO2(aq) at slow flow rates and large sediment thickness. Reaction within the sediment section could approximately double the hydrothermal sink of PO4 over a range of flow rates and sediment thickness, and could slightly decrease (by

Biogeochemical processes in anoxic sediment from Lake Plußsee, Germany

In anoxic environments, volatile methylated sulfides like methanethiol (MT) and dimethyl sulfide (DMS) link the pools of inorganic and organic carbon with the sulfur cycle. However, direct formation of methylated sulfides from reduction of dissolved inorganic carbon has previously not been demonstrated. When studying the effect of temperature on hydrogenotrophic microbial activity, we observed formation of DMS in anoxic sediment of Lake Plußsee at 55 °C. Subsequent experiments strongly suggested that the formation of DMS involves fixation of bicarbonate via a reductive pathway in analogy to methanogenesis and engages methylation of MT. DMS formation was enhanced by addition of bicarbonate and further increased when both bicarbonate and H2 were supplemented. Inhibition of DMS formation by 2-bromoethanesulfonate points to the involvement of methanogens. Compared to the accumulation of DMS, MT showed the opposite trend but there was no apparent 1:1 stoichiometric ratio between both compounds. Both DMS and MT had negative d13C values of -62 per mil and -55 per mil, respectively. Labeling with NaH**13CO3 showed more rapid incorporation of bicarbonate into DMS than into MT. The stable carbon isotopic evidence implies that bicarbonate was fixed via a reductive pathway of methanogenesis, and the generated methyl coenzyme M became the methyl donor for MT methylation. Neither DMS nor MT accumulation were stimulated by addition of the methyl-group donors methanol and syringic acid or by the methyl-group acceptor hydrogen sulphide. The source of MT was further investigated in a H2**35S labeling experiment, which demonstrated a microbially-mediated process of hydrogen sulfide methylation to MT that accounted for only <10% of the accumulation rates of DMS. Therefore, the major source of the 13C-depleted MT was neither bicarbonate nor methoxylated aromatic compounds. Other possibilities for isotopically depleted MT, such as other organic precursors like methionine, are discussed. This DMS-forming pathway may be relevant for anoxic environments such as hydrothermally influenced sediments and fluids and sulfate-methane transition zones in marine sediments.

(Table 1) Concentration of iron, DIP and silicic acid in water samples taken during Nathaniel B. Palmer cruises NBP06-01 and NBP06-08 (CORSACS I+II), Ross Sea

The Ross Sea polynya is among the most productive regions in the Southern Ocean and may constitute a significant oceanic CO2 sink. Based on results from several field studies, this region has been considered seasonally iron limited, whereby a "winter reserve" of dissolved iron (dFe) is progressively depleted during the growing season to low concentrations (~0.1 nM) that limit phytoplankton growth in the austral summer (December-February). Here we report new iron data for the Ross Sea polynya during austral summer 2005-2006 (27 December-22 January) and the following austral spring 2006 (16 November-3 December). The summer 2005-2006 data show generally low dFe concentrations in polynya surface waters (0.10 ± 0.05 nM in upper 40 m, n = 175), consistent with previous observations. Surprisingly, our spring 2006 data reveal similar low surface dFe concentrations in the polynya (0.06 ± 0.04 nM in upper 40 m, n = 69), in association with relatively high rates of primary production (~170-260 mmol C/m**2/d). These results indicate that the winter reserve dFe may be consumed relatively early in the growing season, such that polynya surface waters can become "iron limited" as early as November; i.e., the seasonal depletion of dFe is not necessarily gradual. Satellite observations reveal significant biomass accumulation in the polynya during summer 2006-2007, implying significant sources of "new" dFe to surface waters during this period. Possible sources of this new dFe include episodic vertical exchange, lateral advection, aerosol input, and reductive dissolution of particulate iron.

Geochemistry of recent sediments of the East African continental margin, Arabian Sea

Chemical analyses have been carried out on 40 samples from the sediment surface and 210 samples from cores that were taken from the edge of the African continental block at the Arabian Sea (coasts of Somalia and Kenya, from Cape Guardafui to Mombasa) on the occasion of the Indian Ocean Expedition of the German research vessel "Meteor" during the years 1964/65. The carbonate content shows its maximum on the northern part of the continental shelf of Africa, where fossil reef debris furnish the detritic portion of carbonate. In the southern part of the continental shelf of Africa the portion of carbonate is low, as it is heavily diluted by the non-carbonatic detritus. It is also in the deep-sea that a lower carbonate content is encountered below the calcite compensation depth. Trace elements in the carbonates: On the shelf and in its vicinity Sr and Mg are enriched. The enrichment has been brought about by the portion of reef debris, as this latter contains aragonite (enrichment of Sr) as well as high-magnesium calcite. The greatest part of the slope contains carbonates that are poor in trace elements and mainly made up of foraminifera (and of coccoliths). Below the carbonate compensation depth another enrichment of Mg takes place in the carbonates, which is probably due to a selective dissolution of calcite in comparison to dolomite. The iron and manganese contents of the carbonates are high (iron higher in coast proximity, manganese higher in the depth), but not genuine, as they come about in the course of the extraction of the carbonates as a result of the dissolution of authigenic Mn-Fe-minerals. Non-carbonatic portion of the sediments: In coast proximity an enrichment of quartz comes about. Within the quartz-rich zone it is the elements V, Cr, Fe, Ti, and B that have been enriched in the non-carbonatic components. This enrichment must be attributed to an elevated content of heavy minerals. In the case of Ti and Fe the preliminary enrichment brought about by processes of lateritisation on the continent plays a certain role. Toward the deep-sea an enrichment of the elements Mn Ni, Cu, and Zn takes place; these enrichments must be explained by authigenic Mn-Fe-minerals. Within the Mn-rich zone a belt running parallel to the coast stands out that shows an increased Mn-enrichment. However, this increase in enrichment does not apply to the elements Ni, Cu, and Zn. It is probable that this latter increased enrichment comes about as a result of the migration of manganese to the sediment surface. (Within the sediments there prevail reductive conditions, in the presence of which Mn is capable of migration, whereas at the sediment surface its precipitation comes about under oxidizing conditions). The quantity of organic matter mainly is dependent on grain size and on the rate of sedimentation. On the shelf an impoverishment of organic matter is to be encountered, as the sediments are coarse-grained. In the depth the impoverishment must be explained on the strength of a small rate of sedimentation. Between those two ranges organic substance is enriched. P and N show an enrichment in comparison to Corg with this applying all the more the smaller the absolute quantity of Corg is. In this particular case one has to do with an enrichment coming about during the diagenetic processes of organic matter. A comparison with the sediments from the Indian and Pakistani continental border in Arabian Sea shows as follows: on the African continental border the coarse detrital material has been transported farther out to deep-sea, which has something to do with the greater inclination of the surface of sedimentation. Carbonate is found in greater abundance on the African side. Its chemical composition is influenced by reef-debris which is missing by Indian-Pakistani side. The content of organic matter is lower on the African side. Contrary to that, the enrichments of N and P compared to organic matter are of an equal order of magnitude on both sides of the Arabian Sea.

Porewater and solid-phase phosphorus geochemistry in surface sediments of sediment core GeoB9510-3, GeoB9518-4 and GeoB9519-6

Despite intensive research on the different domains of the marine phosphorus (P) cycle during the last decades, frequently discussed open questions still exist especially on controlling factors for the benthic behaviour of P and its general distribution in sediment-pore water systems. Steady state or the internal balance of all relevant physical and (bio)geochemical processes are amongst the key issues. In this study we present and discuss an extended data set from surface sediments recovered from three locations on the NW African continental slope. Pore water data and results from sequential sediment extractions give clear evidence to the well-known close relationship between the benthic cycles of P and iron. Accordingly, most of the dissolved phosphate must have been released by microbially catalyzed reductive dissolution of iron (oxhydr)oxides. However, rates of release and association of P and iron, respectively, are not directly represented in profiles of element specific sediment compositions. Results from steady-state based transport-reaction modelling suggest that particle mixing due to active bioturbation, or rather a physical net downward transport of P associated to iron (oxyhydr)oxides, is an essential process for the balance of the inspected benthic cycles. This study emphasizes the importance of balancing analytical data for a comprehensive understanding of all processes involved in biogeochemical cycles.

(Tables 1,2) Polar bear (Ursus maritimus), beluga whale (Delphinapterus leucas) and ringed seal (Pusa hispida) liver microsomal protein content and EROD activity

The present study assessed and compared the oxidative and reductive biotransformation of brominated flame retardants, including established polybrominated diphenyl ethers (PBDEs) and emerging decabromodiphenyl ethane (DBDPE) using an in vitro system based on liver microsomes from various arctic marine-feeding mammals: polar bear (Ursus maritimus), beluga whale (Delphinapterus leucas), and ringed seal (Pusa hispida), and in laboratory rat as a mammalian model species. Greater depletion of fully brominated BDE209 (14-25% of 30pmol) and DBDPE (44-74% of 90pmol) occurred in individuals from all species relative to depletion of lower brominated PBDEs (BDEs 99,100, and 154; 0-3% of 30pmol). No evidence of simply debrominated metabolites was observed. Investigation of phenolic metabolites in rat and polar bear revealed formation of two phenolic, likely multiply debrominated, DBDPE metabolites in polar bear and one phenolic BDE154 metabolite in polar bear and rat microsomes. For BDE209 and DBDPE, observed metabolite concentrations were low to nondetectable, despite substantial parent depletion. These findings suggested possible underestimation of the ecosystem burden of total-BDE209, as well as its transformation products, and a need for research to identify and characterize the persistence and toxicity of major BDE209 metabolites. Similar cause for concern may exist regarding DBDPE, given similarities of physicochemical and environmental behavior to BDE209, current evidence of biotransformation, and increasing use of DBDPE as a replacement for BDE209.

An Oka principle for equivariant isomorphisms

Let G be a reductive complex Lie group acting holomorphically on normal Stein spaces X and Y, which are locally G-biholomorphic over a common categorical quotient Q. When is there a global G-biholomorphism X → Y? If the actions of G on X and Y are what we, with justification, call generic, we prove that the obstruction to solving this local-to-global problem is topological and provide sufficient conditions for it to vanish. Our main tool is the equivariant version of Grauert's Oka principle due to Heinzner and Kutzschebauch. We prove that X and Y are G-biholomorphic if X is K-contractible, where K is a maximal compact subgroup of G, or if X and Y are smooth and there is a G-diffeomorphism ψ : X → Y over Q, which is holomorphic when restricted to each fibre of the quotient map X → Q. We prove a similar theorem when ψ is only a G-homeomorphism, but with an assumption about its action on G-finite functions. When G is abelian, we obtain stronger theorems. Our results can be interpreted as instances of the Oka principle for sections of the sheaf of G-biholomorphisms from X to Y over Q. This sheaf can be badly singular, even for a low-dimensional representation of SL2(ℂ). Our work is in part motivated by the linearisation problem for actions on ℂn. It follows from one of our main results that a holomorphic G-action on ℂn, which is locally G-biholomorphic over a common quotient to a generic linear action, is linearisable.

Ocean Acidification Affects Redox-Balance and Ion-Homeostasis in the Life-Cycle Stages of Emiliania huxleyi

Ocean Acidification (OA) has been shown to affect photosynthesis and calcification in the coccolithophore Emiliania huxleyi, a cosmopolitan calcifier that significantly contributes to the regulation of the biological carbon pumps. Its non-calcifying, haploid life-cycle stage was found to be relatively unaffected by OA with respect to biomass production. Deeper insights into physiological key processes and their dependence on environmental factors are lacking, but are required to understand and possibly estimate the dynamics of carbon cycling in present and future oceans. Therefore, calcifying diploid and non-calcifying haploid cells were acclimated to present and future CO2 partial pressures (pCO2; 38.5 Pa vs. 101.3 Pa CO2) under low and high light (50 vs. 300 µmol photons/m**2 /s). Comparative microarray-based transcriptome profiling was used to screen for the underlying cellular processes and allowed to follow up interpretations derived from physiological data. In the diplont, the observed increases in biomass production under OA are likely caused by stimulated production of glycoconjugates and lipids. The observed lowered calcification under OA can be attributed to impaired signal-transduction and ion-transport. The haplont utilizes distinct genes and metabolic pathways, reflecting the stage-specific usage of certain portions of the genome. With respect to functionality and energy-dependence, however, the transcriptomic OA-responses resemble those of the diplont. In both life-cycle stages, OA affects the cellular redox-state as a master regulator and thereby causes a metabolic shift from oxidative towards reductive pathways, which involves a reconstellation of carbon flux networks within and across compartments. Whereas signal transduction and ion-homeostasis appear equally OA-sensitive under both light intensities, the effects on carbon metabolism and light physiology are clearly modulated by light availability. These interactive effects can be attributed to the influence of OA and light on the redox equilibria of NAD and NADP, which function as major sensors for energization and stress. This generic mode of action of OA may therefore provoke similar cell-physiological responses in other protists.

Corteza y gravedad: el plano del suelo como estrategia en la arquitectura contemporánea

Es, en el encuentro de los edificios con el terreno, donde el suelo como realidad se transforma en cualidad arquitectónica. La presente tesis aborda el estudio del plano del suelo, haciendo una revisión crítica de la arquitectura como mecanismo de pensamiento proyectual. Este análisis se enmarca a partir de los años sesenta, por considerar que es cuando comienza a evidenciarse la ruptura respecto a la herencia del Movimiento Moderno. Es entonces cuando la arquitectura marca un punto de inflexión, y empiezan a surgir diferentes actitudes metodológicas respecto al suelo, totalmente nuevas. Las clásicas acciones de encuentro como posar, elevar o enterrar fueron poco a poco sustituidas por otras más complejas como plegar, inclinar o esponjar. Utilizando como marco de restricción los encuentros o desencuentros del objeto arquitectónico con el terreno, se analiza el suelo como estrategia arquitectónica tratando de demostrar como su manipulación puede ser una eficaz herramienta con la que establecer relaciones específicas con el lugar. La capacidad que presenta el suelo, como elemento arquitectónico, de explorar y modificar las características de cada entorno, hacen de esta superficie una eficiente forma de contextualización. Por tanto, la manipulación del suelo que aquí se plantea, opera transcodificando los elementos específicos de cada lugar y actúa como estrategia arquitectónica que pone en relación al edificio con el contexto, modificando las particularidades formales de dicho plano. Frente a la tendencia que reduce la expresión arquitectónica a una simple apariencia formal autónoma, se plantea la manipulación del plano del suelo como mecanismo de enraizamiento con el lugar, enfatizando para ello la condición terrestre de la arquitectura. El plano del suelo es el que ata al edificio mediante la gravedad a la corteza terrestre. En realidad se trata de realzar el carácter mediador del suelo en la arquitectura, definiendo para ello el establecimiento de elementos comunes entre realidades distintas, potenciando el valor del suelo como herramienta que puede transcodificar el entorno, trasformando su datos en elementos arquitectónicos concretos. En este proceso de traducción de información, el suelo pasa de ser un objeto pasivo a ser uno operativo, convirtiéndose en parte activa de las acciones que sobre él se ejercen. La tesis tiene también como propósito demostrar cómo, la clave de la rápida evolución que el suelo como estrategia arquitectónica ha sufrido en los últimos años, mucho debe a la expansión del suelo en otras artes como en la escultura, y mas concretamente en el landart. Surgen entonces nuevas disciplinas, en las que se propone la comprensión del lugar en los proyectos desarrollando una visión integral del mundo natural, convirtiéndolo en un tejido viviente y conector que pone en relación las actividades que sustenta. También encontramos en Utzon, y sus plataformas geológicas, al precursor de la importancia que más tarde se le daría al plano del suelo en la arquitectura, ya que inicia cierta actitud crítica, que hizo avanzar hacia una arquitectura más expresiva que requería nuevos mecanismos que la relacionasen con el suelo que los soportaba, proponiendo con sus plataformas una transformación infraestructural del suelo. Con su interpretación transcultural de las estructuras espaciales arquetípicas mayas, chinas y japonesas, irá enriqueciendo el panorama arquitectónico, adquiriendo de este modo más valor el contexto que acabará por ser entendido de forma más compleja. Los proyectos de arquitectura en muchas ocasiones se han convertido en territorios propicios de especulación donde construir teoría arquitectónica. Desde este contexto se analizan cuatro estrategias de suelo a través del estudio de cuatro posiciones arquitectónicas muy significativas desde el punto de vista de la manipulación del plano del suelo, que construyen una interesante metodología proyectual con la que operar. Los casos de estudio, propuestos son; la Terminal Pasajeros (1996-2002) en Yokohama del estudio FOA, la Casa de la Música (1999-2005) de OMA en Oporto, el Memorial Judío (1998-2005) de Berlín de Peter Eisenman, y por último el Museo MAXXI (1998-2009) de Zaha Hadid en Roma. Descubrir las reglas, referencias y metodologías que cada uno nos propone, nos permite descubrir cuáles son los principales posicionamientos en relación al proyecto y su relación con el lugar. Las propuestas aquí expuestas abordan una nueva forma de entender el suelo, que hizo avanzar a la arquitectura hacia nuevos modos de encuentro con el terreno. Nos permite también establecer cuáles son las principales aportaciones arquitectónicas del suelo, como estrategia arquitectónica, que han derivado en su reformulación. Dichas contribuciones abren nuevas formas de abordar la arquitectura basadas en el movimiento y en la flexibilidad funcional, o en la superposición de flujos de información y circulación. También plantean nuevas vías desdibujando la figura contra el fondo, y refuerzan la idea del suelo como plataforma infraestructural que ya había sido enunciada por Utzon. Se trata en definitiva de proponer la exploración de la superficie del suelo como el elemento más revelador de las formas emergentes del espacio. ABSTRACT Where the building hits the ground, it is where the latter as reality becomes architectural quality. This thesis presents the study of the ground plane, making a critical review of architecture as a mechanism of projectual thought. This analysis starts from the sixties, because it is when the break begins to be demonstrated with regard to the inheritance of the Modern Movement. It is then when architecture marks a point of inflexion, and different, completely new methodological attitudes to the ground start to emerge. The classic meeting action like place, raise or bury are gradually replaced by more complex operations such as fold, bend or fluff up. Framing it within the meetings or disagreements between architectural object and ground, we analyzed it as architectural strategy trying to show how handling can be an effective tool to establish a specific relationship with the place. The capacity ground has, as an architectural element, to explore and modify the characteristics of each environment, makes this area an efficient tool for contextualization. Therefore, the manipulation of ground that is analyzed here, operates transcoding the specifics of each place and acts as architectural strategy that relates to the building with the context, modifying the structural peculiarities of such plane. Opposite to the reductive tendency of the architectural expression to a simple formal autonomous appearance, the manipulation of the ground plane is considered as a rooting mechanism place that emphasises the earthly condition of architecture. The ground plane is the one that binds the building by gravity to the earth’s crust. In fact, it tries to study the mediating character of the ground in architecture, defining for it to establish commonalities among different realities, enhancing the value of the ground as a tool that can transcode the environment, transforming its data into specific architectural elements. In this process of translating information, the ground goes from being a liability, to become active part of the actions exerted on the object. The thesis also tries to demonstrate how the key of the rapid evolution that the ground likes architectural strategy has gone through recently, much due to its use expansion in other arts such as sculpture. New disciplines arise then, in which one proposes the local understanding in the projects, developing an integral vision of the natural world and turning it into an element linking the activities it supports. We also find in Utzon, and his geological platforms, the precursor of the importance that later would be given to the ground plane in architecture, since it initiates a certain critical attitude, which advances towards a more expressive architecture, with new mechanisms that relate to the ground that it sits in, proposing with its platforms an infrastructural transformation of the ground. With his transcultural interpretation of the spatial archetypal structures, he will enrich the architectural discourse, making the context become understood in more complex ways. Architectural projects in many cases have become territories prone to architectural theory speculation. Within this context, four strategies are analyzed through the study of four very significant architectural positions, from the point of view of handling the ground plane, and the project methodology within which to operate. The case studies analyzed are; Passenger Terminal (1996-2002) in Yokohama from FOA, The House of the music (1999-2005) the OMA in Oporto, The Jew monument (1998-2005) in Berlin the Peter Eisenman, and finally the MAXXI Museum (1998-2009) the Zaha Hadid in Rome. Discovering the rules, references and methodologies that each of those offer, it allows to discover what the main positions are regarding the building and its relationship with the place where it is located. The proposals exposed here try to shed a different light on the ground, which architecture advancing in new ways on how meet it. The crossing of the different studied positions, allows us to establish what the main contributions of ground as architectural strategy are. Such contributions open up new approaches to architecture based on movement and functional flexibility, overlapping information flow and circulation, consider new ways that blur the figure against the background, and reinforce the idea of ground as infrastructural platform, already raised by Utzon. Summarizing, it tries to propose the exploration of the ground plane as the most revealing form of spatial exploration.