Petrologia do magmatismo tardi-brasiliano no Maciço São José de Campestre(RN/PB), com ênfase no Plúton Alcalino Caxexa

The area studied is located on the north-easternmost portion of the Borborema Province, on the so-called São José de Campestre Massif, States of RN and PB, Northeast Brazil. Field relations and petrographic, geochemical and isotope data permitted the separation of five suites of plutonic rocks: alkali-feldspar granite (Caxexa Pluton), which constitutes the main subject of this dissertation, amphibole-biotite granite (Cabeçudo Pluton), biotite microgranite, gabbronorite to monzonite (Basic to Intermediate Suite) and aluminous granitoid. The Caxexa Pluton is laterally associated to the Remígio Pocinhos Shear Zone, with its emplacement along the mylonitic contact between the gneissic basement and the micashists. This pluton corresponds to a syntectonic intrusion elongated in the N-S direction, with about 50 km2 of outcropping surface. It is composed exclusively of alkali-feldspar granites, having clinopyroxene (aegirine-augite and hedenbergite), andradite-rich garnet, sphene and magnetite. It is classified geochemically as high silica rocks (>70 % wt), metaluminous to slightly peraluminous (normative corindon < 1%), with high total alkalis (>10% wt), Sr, iron number (#Fe=90-98) and agpaitic index (0.86-1.00), and positive europium anomaly. The Cabeçudo Pluton is composed of porphyritic rocks, commonly containing basic to intermediate magmatic enclaves often with mingling and mixing textures. Petrographically, it presents k-feldspar and plagioclase phenocrysts as the essential minerals, besides the accessories amphibole, biotite, sphene and magnetite. It is metaluminous and shows characteristics transitional between the calc-alkaline and alkaline series (or monzonitic subalkaline). Its REE content is greater than those ones of the Caxexa Pluton and biotite microgranite, and all spectra have negative europium anomalies. The biotite microgranites occur mainly on the central and eastern portion of the mapped area, as dykes and sheets with decimetric thickness, hosted principally in orthogneisses and micashists. Their field relationships as regards the Caxexa and Cabeçudo plutons suggested that they are late-tectonic intrusions. They are typically biotite granites, having also sphene, amphibole, allanite, opaques and zircon in the accessory assemblage. Geochemically they can be distinguished from the porphyritic types because the biotite microgranites are more evolved, peraluminous, and have more fractionated REE spectra. The Basic to Intermediate rocks form a volumetrically expressive elliptical, kilometric scale body on the Southeast, as well as sheets in micashists. They are classified as gabbronorites to monzonites, with the two pyroxenes and biotite, besides subordinated amounts of amphibole, sphene, ilmenite and allanite. These rocks do not show a well-defined geochemical trend, however they may possibly represent a monzonitic (shoshonitic) series. Their REE spectra have negative europium anomalies and REE contents greater than the other suites. The aluminous granitoids are volumetrically restricted, and have been observed in close association with migmatised micashists bordering the gabbronorite pluton. They are composed of almandine-rich garnet, andalusite, biotite and muscovite, and are akin to the peraluminous suites. Rb-Sr (whole rock) and Sm-Nd (whole-rock and mineral) isotopes furnished a minimum estimate of the crystallization (578±14 Ma) and the final resetting age of the Rb-Sr system (536±4 Ma) in the Caxexa Pluton. The aluminous granitoid has a Sm-Nd garnet age similar to that one of the Caxexa Pluton, that is 574±67 Ma. The strong interaction of shear bands and pegmatite dykes favoured the opening of the Rb-Sr system for the Caxexa Pluton and biotite microgranite. The amphibole-plagioclase geothermometer and the Al-in amphibole geobarometer indicate minimum conditions of 560°C and 7 kbar for the Cabeçudo Pluton, 730°C and 6 kbar for the microgranite and 743°C and 5 kbar for the basic to intermediate suite. The Zr saturation geothermometer reveals temperatures of respectively 855°C, 812°C and 957°C for those suites, whereas the Caxexa Pluton shows temperatures of around 757°C. The Caxexa, Cabeçudo and microgranites suites crystallized under high fO2 (presence of magnetite). On the other hand, the occurrence of ilmenite suggests less oxidant conditions in the basic to intermediate suite. Field relations demonstrate the intrusive character of the granitoids into a tectonically relatively stable continental crust. This is corroborated by petrographic and geochemical data, which suggest a late- or post-collisional tectonic context. It follows that the generation and emplacement of those granitoid suites is related to the latest events of the Brasiliano orogeny. Finally, the relationships between eNd (600 Ma), TDM (Nd) and initial Sr isotope ratio (ISr) do not permit to define the precise sources of the granitoids. Nevertheless, trace element modelling and isotopic comparisons suggest the participation of the metasomatised mantle in the generation of these suites, probably modified by different degrees of crustal contamination. In this way, a metasomatised mantle would not be a particular characteristic of the Neoproterozoic lithosphere, but a remarkable feature of this portion of the Borborema Province since Archaean and Paleoproterozoic times.

Caracterização geológica, geoquímica e geocronológica da suíte plutônica enoproterozóica da região de Serrinha, porção centro-leste do maciço São José de Campestre, sudeste do RN

The of Serrinha plutonic suite, northeastern portion of the Borborema Province (NE Brazil), is characterized by a voluminous and diversified magmatism of Neoproterozoic age, intrusive in the Archean to Paleoproterozoic gneissic-migmatitic basement of the São José de Campestre massif. Field relations and petrographic and geochemical data allowed us to individualize different lithologic types among this plutonic suite, which is represented by intermediate to mafic enclaves, porphyritic diorites, porphyritic granitoids, porphyritic granodiorites, microporphyritic granites and dykes/sheets of microgranite. The intermediate-to-mafic enclaves occur associated with porphyritic granitoids, showing mixture textures. The porphyrytic diorites occur as isolated bodies, generally associated with intermediate-to-mafic enclaves and locally as enclaves within porphyritic granites. The granodiorites represent mixing between an intermediate to mafic magma with an acidic one. The micropophyritic granites occur as isolated small bodies, generally deformed, while the microgranite dykes/sheets crosscut all the previous granitoids. A U-Pb zircon age of 576 + 3 Ma was obtained for the Serrinha granite. This age is interpreted as age of the peak of the regional ductile deformational event (D3) and of the associated the E-W Rio Jacu shear zone, which control the emplacement of the Neoproterozoic syntectonic plutons. The porphyrytic granitoids show monzogranitic composition, transitional between peraluminous and metaluminous types, typically of the high potassium subalkaline-calc-alkaline series. The intermediate-to-mafic enclaves present vary from quartz diorite to tonalite/granodiorite, with metaluminous, shoshonitic affinity. The diorites are generally quartz-monzodiorite in composition, with metaluminous, subalkaline affinity. They display coarse-grained, inequigranular, porphyrytic texture, with predominance of plagioclase phenocrystals immersed in a matrix composed of biotite and pyroxenes. The microporphyrytic granites are essentially monzogranites of fine- to medium-grained texture, whereas microgranite dikes/sheets varying from monzogranites to syenogranites, with fine to media texture, equigranular. The diversified magmatism occurring at a relatively small surface associated with shear zones, suggests lithospheric dimensions for such structures, with magma extractions from different depths within the lower crust and upper mantle. The geological, geochemical and geochronological characteristics of the Serrinha plutonic suite suggest a pos-collisional geodynamic context for the Neoproterozoic magmatism. Thermobarometric data show emplacement conditions in the range 5-6 kbar (AlTamphibole) and 730-740°C (plagioclase-amphibole) for the porphyrytic granitoids (Serrinha body) and the intermediate-to-mafic enclaves

The 3.4-3.5 Ga Sao Jose do Campestre massif, NE Brazil: remnants of the oldest crust in South America

The oldest fragment of continental crust recognized in South America occurs as an isolated Archean enclave in northeastem Brazil's Borborema Province, ca. 600 Ma Brasiliano-Pan African orogenic belt. This Archean fragment, the Sao Jose do Campestre massif, is surrounded by large tracts of 2.2-2.0 Ga Paleoproterozoic gneisses and is located more than 600-1500 km from the much larger assemblages of Archean rocks found in the Sao Fransciso and Amazonian cratons, located to the south and west, respectively. Geochronological studies of the Sao Jose do Campestre massif show that its oldest rocks contain zircons with U-Pb ages up to 3.5 Ga and Sm-Nd T-DM model ages of more than 3.7 Ga, indicating that they represent reworked crust. This older nucleus is flanked by both reworked and juvenile 3.25 and 3.18 Ga rocks which arc intruded by both 3.00 and 2.69 Ga plutonic bodies. The protracted evolution the Sao Jose do Campestre massif is consistent with that of a larger continental mass as opposed to a small crustal fragment that grew in isolation. As such, the Sao Jose do Campestre massif is interpreted as representing a detached piece of an evolved craton that became entrained with younger rocks during a subsequent Paleoproterozoic accretionary-orogenic event. This hypothesis is bolstered by the presence of Paleoproterozoic gneisses that envelop the Sao Jose do Campestre massif, as well as the existence of ca. 2.0 Ga metamorphic zircon and monazite within its rocks. The occurrence of several different Archean cratonic basement inliers within the greater Paleoproterozoic crustal framework of the Borborema Province suggests that cratonic slices spalled off one or more larger Archean masses prior to the ca. 2.2-2.0 Ga Paleoproterozoic orogenic collage. A important challenge is to link these older fragments to their parent cratons. Although results are not unique, the pattern of ages and isotopic signatures observed in the Sao Jose do Campestre massif is similar to that seen in parts of the Sao Francisco Craton, and it is possible that the Sao Jose do Campestre massif is a fragment of an Archean continental fragment formed during an episode of continental breakup prior to 2200 Ma. (C) 2003 Elsevier B.V. All rights reserved.

Crustal growth in the 3.4-2.7Ga São José de Campestre Massif, Borborema Province, NE Brazil

The Archean (3.45-2.70Ga) rocks of the São José do Campestre Massif (SJCM) in the Borborema Province (NE Brazil) make up a small area (~6000km2) and are composed of granitoids and metasupracrustal rocks that define a complex magmatic and deformational history. The massif provides the opportunity to study mantle- and crustal-derived magmas generated since the Palaeoarchean. The orthogneisses of the SJCM are composed of: (1) tonalite to granodiorite with diorite enclaves (Bom Jesus gneiss, 3412±8Ma; TDM Nd model ages from 4.1 to 3.5Ga and negative epsilon Nd values); (2) biotite and ferroan-diopside monzogranite (Presidente Juscelino complex, 3356±21Ma and 3251±44Ma; TDM model ages range from 4.1 to 3.4Ga and epsilon Nd values that are slightly positive to negative); (3) hornblende tonalite to granodiorite (Brejinho complex, 3333±77Ma and 3187±8Ma; dominantly positive epsilon Nd values and TDM ages from 3.6 to 3.2Ga); (4) biotite monzogranite (São Pedro do Potengi gneiss, 3120±22Ma; TDM =3.5Ga; negative epsilon Nd value); (5) ferroan-diopside-grossular anorthosite and metagabbro (Senador Elói de Souza complex, 3033±3Ma); and (6) quartz diorite to syenogranite (São José do Campestre complex; 2685±9Ma and 2655±4Ma; negative epsilon Nd values and TDM ages from 3.9 to 3.3Ga). The orthogneisses are subalkaline to faintly alkaline, magnesian to ferroan, M- and I-type granitoids that follow either the K-enrichment or the trondhjemite trends. Each group has a subset with REE characteristics similar to Archean TTG and another that is analogous to Phanerozoic granitoids. They have negative Ta-Nb and Ti anomalies and have trace element contents of granitoids from subduction zones. Geochemical and Nd isotope data suggest that subducted oceanic crust and a depleted and metasomatised mantle wedge both acted as the magma sources. We propose a convergent tectonic model in which hybridisation of the upper mantle occurs through interactions with adakitic or trondhjemitic melts and recycling of earlier crust. The results imply that both the subducted oceanic crust and the mantle wedge played major roles in continent formation throughout successive episodes of arc accretion in Palaeo- and Mesoarchean times. The Archean rocks of the SJCM shares some similarities with the Pilbara, Kaapvaal, West African, and São Francisco cratons. However, the most reliable comparisons with the SJCM are with the neighbouring basement of the Nigeria and Cameroon shields. © 2012 Elsevier B.V.

Capacidade de auto-recuperação de cursos d'água urbanos: estudo de caso : Córrego Campestre em Lins - SP

Pós-graduação em Engenharia Civil - FEIS

Monitoramento e avaliação da qualidade da água na microbacia do córrego campestre no município de Lins-SP

Pós-graduação em Engenharia Civil - FEIS

Ri-abitare il margine urbano - Strategie di riqualificazione per il social housing: un edificio residenziale "ACER" come modello di intervento

La tesi individua alcune strategie di rigenerazione urbana e di riqualificazione edilizia, al fine di ottenere una serie di linee guida per l’intervento sul patrimonio di edilizia abitativa situata nelle periferie urbane. Tali principi sono stati poi applicati ad un edificio ACER collocato nella prima periferia di Forlì, per sperimentare l’efficacia delle strategie individuate. Dalla ricerca svolta sulle strategie di intervento volte alla riqualificazione sociale delle periferie, in particolare la teoria del “Defencible space” di Jacobs, si evidenzia l’importanza di accentuare nei residenti il sentimento di territorialità, ovvero la consapevolezza di far parte di una comunità specifica insediata in un particolare spazio, alimentata attraverso la frequentazione e l’appropriazione percettivo-funzionale degli spazi pubblici. Si è deciso quindi di allargare il campo di intervento alla rigenerazione dell’interno comparto, attraverso la riorganizzazione degli spazi verdi e la dotazione di attrezzature sportive e ricreative, in modo da offrire spazi specifici per le diverse utenze (anziani, giovani, bambini) e la definizione di un programma funzionale di servizi ricreativi e spazi destinati a piccolo commercio per integrare le dotazioni carenti dell’area. Dall’analisi approfondita dell’edificio sono emerse le criticità maggiori su cui intervenire: - l’intersezione dei percorsi di accesso all’edificio - la struttura portante rigida, non modificabile - la scarsa varietà tipologica degli alloggi - l’elevato fabbisogno energetico. La riqualificazione dell’edificio ha toccato quindi differenti campi: tecnologico, funzionale, energetico e sociale; il progetto è stato strutturato come una serie di fasi successive di intervento, eventualmente realizzabili in tempi diversi, in modo da consentire il raggiungimento di diversi obiettivi di qualità, in funzione della priorità data alle diverse esigenze. Secondo quest’ottica, il primo grado di intervento, la fase 1 - riqualificazione energetica, si limita all’adeguamento dello stato attuale alle prestazioni energetiche richieste dalla normativa vigente, in assenza di adeguamenti tipologici e spaziali. La fase 2 propone la sostituzione degli impianti di riscaldamento a caldaie autonome presenti attualmente con un impianto centralizzato con pompa di calore, un intervento invasivo che rende necessaria la realizzazione di un “involucro polifunzionale” che avvolge completamente l’edificio. Questo intervento nasce da tre necessità fondamentali : - architettonica: poter ampliare verso l’esterno le superfici degli alloggi, così da intervenire sulle unità abitative rendendole più rispondenti alle necessità odierne; - statica: non dover gravare in ciò sull’edificio esistente apportando ulteriori carichi, difficilmente sopportabili dalla struttura esistente, assicurando il rispetto della normativa antisismica in vigore; - impiantistica/tecnologica: alloggiare i condotti del nuovo impianto centralizzato per il riscaldamento, raffrescamento e acs; La fase 3 è invece incentrata sull’ampliamento dell’offerta abitativa, in modo da rispondere anche a necessità legate ad utenze speciali, come utenti disabili o anziani. L’addizione di nuovi volumi si sviluppa in tre direzioni: - un volume parassita, che aderisce all’edificio nel fronte sud/est, indipendente dal punto di vista strutturale, ruotato per sfruttare al meglio l’orientamento ottimale. - un volume satellite, indipendente, connesso all’edificio esistente tramite un elemento di raccordo, e nel quale sono collocati alcuni alloggi speciali. - un’addizione in copertura, che non appoggia direttamente sul solaio di copertura esistente, ma grava sull’elemento di chiusura del’involucro realizzato nella fase 2 Completano il progetto le addizioni volumetriche a piano terra, destinate a servizi quali un centro diurno, un micronido e un bar, i quali costituiscono la traduzione alla scala dell’edificio delle strategie applicate nel progetto di comparto. Questi interventi hanno consentito di trasformare un edificio costruito negli anni ’80 in un complesso residenziale moderno, dotato spazi accessori di grande qualità, tecnologie moderne che ne garantiscono il comfort abitativo, servizi alla persona disponibili in prossimità dell’edificio.

Recuperare l'abitare sociale. Riqualificazione dell'edificio acer di via Wolfgang Goethe a Bologna.

Nel volume vengono proposte delle strategie di riqualificazione dell’edificio in via W. Goethe con numero civico 2-10 a Corticella zona Navile. L’edificio fa parte del quartiere PEEP realizzato a partire dagli anni ‘70 circa. L’intera area ricopre una superficie pari a 220.000 m2 di cui edificata 38.000 m2. Della superficie edificata ben 30.400 m2 è stata destinata al residenziale. A seguito delle evoluzioni economiche e sociali e alle restrizioni sempre più severe della normativa, il quartiere ha mostrato delle carenze e delle criticità: – Scarse prestazioni energetiche degli edifici con elevati costi di esercizio; – Inadeguata risposta alle azioni sismiche; – Tagli di alloggi non in grado di soddisfare l’odierna domanda; – Mancanza di efficaci spazi pubblici e di relazione; – Inefficace connessione urbana ai maggiori poli attrattivi e di circolazione. Come primo obbiettivo è stato affrontato il problema della mancanza di connessioni ciclopedonali adeguate al territorio di Corticella. Vi sono infatti alcune aree di nodale importanza che sono sprovviste di questi collegamenti rendendo difficoltoso il link tra i punti attrattivi fondamentali di Corticella e il nostro quartiere. Il progetto intende migliorare questo tipo di servizio in linea con il progetto “bike sharing & ride” promosso dalla Regione Emilia Romagna al fine di incentivare e promuovere la mobilità. Seguono poi gli interventi volti a risolvere le problematiche riscontrate nell’edificio. Interventi atti a riportare l’edificio in una condizione tale da renderlo adeguato alle necessità attuali e in grado di svolgere la sua funzione per gli anni a venire. Si tratta di strategie tecniche e parallelamente di strategie energetiche, con l’obbiettivo di definire spazi confortevoli all’interno degli alloggi. A tale fine sono state realizzate anche valutazioni sull’illuminazione naturale degli ambienti interni per valutare l’efficacia o meno del sistema utilizzato.

Investigating within-canopy variation of functional traits and cellular structure of sugar maple (Acer saccharum) leaves

Patterns of increasing leaf mass per area (LMA), area-based leaf nitrogen (Narea), and carbon isotope composition (δ13C) with increasing height in the canopy have been attributed to light gradients or hydraulic limitation in tall trees. Theoretical optimal distributions of LMA and Narea that scale with light maximize canopy photosynthesis; however, sub-optimal distributions are often observed due to hydraulic constraints on leaf development. Using observational, experimental, and modeling approaches, we investigated the response of leaf functional traits (LMA, density, thickness, and leaf nitrogen), leaf carbon isotope composition (δ13C), and cellular structure to light availability, height, and leaf water potential (Ψl) in an Acer saccharum forest to tease apart the influence of light and hydraulic limitations. LMA, leaf and palisade layer thickness, and leaf density were greater at greater light availability but similar heights, highlighting the strong control of light on leaf morphology and cellular structure. Experimental shading decreased both LMA and area-based leaf nitrogen (Narea) and revealed that LMA and Narea were more strongly correlated with height earlier in the growing season and with light later in the growing season. The supply of CO2 to leaves at higher heights appeared to be constrained by stomatal sensitivity to vapor pressure deficit (VPD) or midday leaf water potential, as indicated by increasing δ13C and VPD and decreasing midday Ψl with height. Model simulations showed that daily canopy photosynthesis was biased during the early growing season when seasonality was not accounted for, and was biased throughout the growing season when vertical gradients in LMA and Narea were not accounted for. Overall, our results suggest that leaves acclimate to light soon after leaf expansion, through an accumulation of leaf carbon, thickening of palisade layers and increased LMA, and reduction in stomatal sensitivity to Ψl or VPD. This period of light acclimation in leaves appears to optimize leaf function over time, despite height-related constraints early in the growing season. Our results imply that vertical gradients in leaf functional traits and leaf acclimation to light should be incorporated in canopy function models in order to refine estimates of canopy photosynthesis.

Hypoglycin A concentrations in seeds of Acer pseudoplatanus trees growing on atypical myopathy-affected and control pastures.

BACKGROUND Hypoglycin A, found in seeds of Acer negundo, appears to cause seasonal pasture myopathy (SPM) in North America and is implicated in atypical myopathy (AM) in Europe. Acer negundo is uncommon in Europe. Thus, the potential source of hypoglycin A in Europe is unknown. HYPOTHESIS AND OBJECTIVES We hypothesized that seeds of Acer pseudoplatanus were the source of hypoglycin A in Europe. Our objective was to determine the concentration of hypoglycin A in seeds of A. pseudoplatanus trees located in pastures where previous cases of AM had occurred. ANIMALS None. METHODS University of Berne records were searched to retrospectively identify 6 farms with 10 AM cases and 11 suspected AM deaths between 2007 and 2011. During October 2012, A. pseudoplatanus seeds were collected from 2 to 6 trees per pasture on 6 AM farms (7 pastures) from trees in or close to 2 pastures on 2 control farms where AM had not been previously reported. Hypoglycin A in seeds was analyzed by GC-MS. RESULTS Acer pseudoplatanus trees were identified on all AM pastures. Hypoglycin A was detected in all A. pseudoplatanus seeds in highly variable concentrations ranging from 0.04 to 2.81 μg/mg (mean 0.69) on AM farms and 0.10 to 9.12 μg/mg (mean 1.59) on control farms. CONCLUSION AND CLINICAL IMPORTANCE Preventing horses from grazing pastures containing A. pseudoplatanus seeds during late fall and early spring might be the best means to prevent AM.

Acer californicum T. et Gr.

Dr. G. Dieck

Die Verbreitung von Eryngium campestre L., Artemisia campestris L. und Tithymalus Gerardianus Kl. u. Gcke. an der unteren Lippe

Von Dr. Julius Müller

Ueber Acer Ginale, Ceanothus und Clematis und deren Verwendung bei Gruppenpflanzungen in Gärten

Von August Schütz

[Acer pensylvanicum - Ahorn]

AR