End-to-end validation of EPS / MetOp GOME-2 trace gas data

Within the next decade, the improved version 2 of Global Ozone Monitoring Experiment (GOME-2), a ultraviolet-visible spectrometer dedicated to the observation of key atmospheric trace species from space, will be launched successively on board three EUMETSAT Polar System (EPS) MetOp satellites. Starting with the launch of MetOp-1 scheduled for summer 2006, the GOME-2 series will extend till 2020 the global monitoring of atmospheric composition pioneered with ERS-2 GOME-1 since 1995 and enhanced with Envisat SCIAMACHY since 2002 and EOS-Aura OMI since 2004. For more than a decade, an international pool of scientific teams active in ground-and space-based ultraviolet-visible remote sensing have contributed to the successful post-launch validation of trace gas data products and the associated maturation of retrieval algorithms for the latter satellites, ensuring that geophysical data products are/become reliable and accurate enough for intended research and applications. Building on this experience, this consortium plans now to develop and carry out appropriate validation of a list of GOME-2 trace gas column data of both tropospheric and stratospheric relevance: nitrogen dioxide (NO 2), ozone (O 3), bromine monoxide (BrO), chlorine dioxide (OClO), formaldehyde (HCHO), and sulphur dioxide (SO 2). The proposed investigation will combine four complementary approaches resulting in an end-to-end validation of expected column data products.

Synthese und Charakterisierung zylindrischer Poly(2-oxazolin)bürsten als Nanocarrier für Drug Delivery Systeme

Inspiriert durch natürlich vorkommende Peptide, sind Poly(2-oxazoline) vielversprechende Kandidaten für Anwendungen in Bereichen des kontrollierten Wirkstoff- bzw. Gentransportes, wie die moderne Biomedizin dies fordert. Da Polyoxazoline als strukturisomere Amide von natürlichen Polypeptiden aufgefasst werden können, zeigen diese synthetischen Polymere in direktem Vergleich erhebliche Vorteile etwa hinsichtlich Zytotoxizät und Effizienz, was wesentlich dazu beitragen kann, aktuelle Hürden biomedizinischer Fragestellungen hinsichtlich Transport und Targeting zu überwinden. Darüber hinaus sollten zylindrische Polymerbürsten aufgrund ihrer molekularen, architekturbedingten Formanisotropie und jüngsten Ergebnissen insbesondere zur formabhängigen Endozytose sehr aussichtsreiche Kandidaten für den Einsatz zum Wirkstofftransport sein.rnrnDie vorliegende Arbeit widmete sich deshalb der Synthese und Charakterisierung von biokompatiblen zylindrischen Poly(2-oxazolin)bürsten als potentielle Nanotransporter von Wirkstoffen, Biomolekülen oder genetischem Material. Als Monomer wurde zunächst 2-Isopropyloxazolin gewählt, da das Polymer eine Phasenübergangstemperatur von 37 °C besitzt, was für Konjugatsynthesen wie auch diverse biomedizinische Applikationen interessant sein kann. Durch terminierende Methacrylamid Funktionalisierung der lebenden kationischen Oxazolinpolymerisation bzw. nachfolgende Endgruppen Transferreaktionen sind Makromonomere im Bereich 1000-5000 g/mol zugänglich. Erstmals gelang es so 2-Oxazolin basierte, hochmolekulare zylindrische Bürsten mit Konturlängen im Bereich von 250 nm mittels „Grafting Through“ Technik in freier radikalischer Polymerisation herzustellen.rnrnAusgehend von der entwickelten Syntheseroute konnten so neben Homo- und Blockcopolymerbürsten von 2-Ethyl-2-oxazolin und 2-Isopropyl-2-oxazolin auch Bürstenmoleküle aus statistischen Copolymeren von 2-Ethyl-2-oxazolin und unsubstituiertem 2-Oxazolin hergestellt werden. Während letztere die Einführung kationischer Gruppen durch selektivere Abspaltmethoden der Formylreste erlauben und so etwa DNA/RNA Komplexierungen ermöglichen können, bietet andererseits der in dieser Arbeit erstmalig demonstrierte Einsatz Azid-funktionalisierter Initiatoren zur kationischen Oxazolinpolymerisation unter Beibehaltung aller anderen sonstigen Reaktionsschritte auch die Möglichkeit der Synthese Azid-Endgruppen-funktionalisierter Makromonomere. Die „Grafting Through“ Methodik der freien radikalischen Makromonomer Polymerisation ist selbst bei diesen funktionalisierten Systemen von großem Vorteil, erlaubt sie auch hier den Zugang zu hochmolekularen Substraten mit einem Pfropfungs- bzw. Funktionalisierungsgrad von 100 %, da jede Seitenkette dieser zylindrischen Bürsten die aussenliegende, und damit sterisch leichter zugängliche funktionale Gruppe trägt. Dabei gelang es die Syntheseroute so zu gestalten, dass es möglich war alle vorgestellten Polymerbürsten mittels statischer und dynamischer Lichtstreuung hinsichtlich absoluter Molmasse und molekularer Dimension zu charakterisieren.rnIn weitereren Reaktionen konnten dann reaktive Fluoreszenzfarbstoffe mit Hilfe kupferfreier 1,3 dipolarerer Addition (kupferfreie „Click-Chemie“) an die Azid-funktionalisierten Polymerbürsten angebunden werden, so dass eine wesentliche Voraussetzung für die Detektion in in vivo und in vitro Experimenten erfüllt werden kann. Darüber hinaus gelingt die quantitative polymeranaloge Umsetzung der Azid- zu Aminogruppen durch eine polymeranalog geführte Reduktion nach Staudinger; damit können an diesen Systemen auch etablierte Konjugationstechniken an Aminogruppen durchgeführt werden. Zudem erlauben die Aminogruppen-haltigen Polymerbürsten durch Protonierung schon bei physiologischem pH die Komplexierung von DNA oder RNA. rnrnErste Lichtstreumessungen in Blutserum zeigen im Falle der kationischen Aminogruppen tragenden Polymerbürsten zwar Aggregation, was aber durch entsprechende Umsetzung nach Konjugation wahrscheinlich unterdrückt werden kann, zeigen doch die entsprechenden Precursorpolymerbürsten mit Azidgruppen in Serum keinerlei Aggregation.rnrnZellaufnahmestudien in dendritische Zellen zeigen nur im Falle einer Azid-funktionalisierten Poly(2-isopropyl-2-oxazolin)bürste eine unspezifische Aufnahme. Die hydrophileren Poly(2-oxazolin)bürsten weise keine unspezifische Aufnahme auf, was eine wichtige Anfoderung für die Verwendung als Polymercarrier in der Krebsimmuntherapie ist.rn

The (2 + 1)-d U (1) quantum link model masquerading as deconfined criticality

The (2 + 1)-d U(1) quantum link model is a gauge theory, amenable to quantum simulation, with a spontaneously broken SO(2) symmetry emerging at a quantum phase transition. Its low-energy physics is described by a (2 + 1)-d RP(1) effective field theory, perturbed by an SO(2) breaking operator, which prevents the interpretation of the emergent pseudo-Goldstone boson as a dual photon. At the quantum phase transition, the model mimics some features of deconfined quantum criticality, but remains linearly confining. Deconfinement only sets in at high temperature.

Comparative morphology among representatives of main taxa of Scaphopoda and basal protobranch Bivalvia (Mollusca)

This study deals with detailed morphology and anatomy of 4 species of Scaphopoda and 5 species of protobranch Bivalvia. Both classes are traditionally grouped in the taxon Diasoma, which has been questioned by different methodologies, such as molecular and developmental. This study is developed under a phylogenetic methodology with the main concern in performing it in an intelligible and testable methodology. The analyzed Scaphopoda species came from the Brazilian coast and belong to the family Dentaliidae [(1) Coccodentalium carduus; (2) Paradentalium disparile] and Gadiliidae; [(3) Polyschides noronhensis, n. sp. from Fernando de Noronha Archipelago; (4) Gadila braziliensis]. These species represent the main branches of the class Scaphopoda. From protobranch bivalves, representatives of the families Solemyidae [(5) Solemya occidentalis, from Florida; S. notialis, n. sp. from S.E. Brazil], Nuculanidae [(6) Propeleda carpentieri from Florida], and Nuculidae [(7) Ennucula puelcha, from south Brazil] are included. These species represent the main branches of the basal Bivalvia. The descriptions on the anatomy of S. occidentalis and of P. carpentieri are published elsewhere. The remaining are included here, for which a complete taxonomical treatment is performed. Beyond these species, representatives of other taxa are operationally included as part of the ingroup (indices are then shared with them), as a procedure to test the morphological monophyly of Diasoma. These taxa are: two lamellibranch bivalves [(8) Barbatia - Arcidae; (9) Serratina - Tellinidae; both published elsewhere;, and Propilidium (10) Patellogastropoda, and (11) Nautilus, basal Cephalopoda, based on basal taxa. The effective outgroups are (12) Neopilina (Monoplacophora) and (13) Hanleya (Polyplacophora). The phylogenetic analysis based on morphology revealed that the taxon Diasoma is supported by 14 synapomorphies, and is separated from Cyrtosoma (Gastropoda + Cephalopoda). Although they are not the main goal of this paper, the taxa Scaphopoda and Bivalvia are supported by 8 and by 7 synapomorphies respectively. The taxon Protobranchia resulted paraphyletic. Both scaphopod orders resulted monophyletic. The obtained cladogram is: ((((Coccodentalium carduus - Paradentalium disparile) (Polyschides noronhensis - Gadila brasiliensis)) ((Solemya occidentalis - S. notialis) (Propeleda carpenteri (Ennucula puelcha (Barbatia cancellaria - Serratina capsoides))))) (Propilidium curumim - Nautilus pompilius - Lolliguncula brevis)).

Urban air pollution and chronic obstructive pulmonary disease-related emergency department visits

Background: Patients with chronic obstructive pulmonary disease (COPD) can have recurrent disease exacerbations triggered by several factors, including air pollution. Visits to the emergency respiratory department can be a direct result of short-term exposure to air pollution. The aim of this study was to investigate the relationship between the daily number of COPD emergency department visits and the daily environmental air concentrations of PM(10), SO(2), NO(2), CO and O(3) in the City of Sao Paulo, Brazil. Methods: The sample data were collected between 2001 and 2003 and are categorised by gender and age. Generalised linear Poisson regression models were adopted to control for both short-and long-term seasonal changes as well as for temperature and relative humidity. The non-linear dependencies were controlled using a natural cubic spline function. Third-degree polynomial distributed lag models were adopted to estimate both lag structures and the cumulative effects of air pollutants. Results: PM(10) and SO(2) readings showed both acute and lagged effects on COPD emergency department visits. Interquartile range increases in their concentration (28.3 mg/m(3) and 7.8 mg/m(3), respectively) were associated with a cumulative 6-day increase of 19% and 16% in COPD admissions, respectively. An effect on women was observed at lag 0, and among the elderly the lag period was noted to be longer. Increases in CO concentration showed impacts in the female and elderly groups. NO(2) and O(3) presented mild effects on the elderly and in women, respectively. Conclusion: These results indicate that air pollution affects health in a gender-and age-specific manner and should be considered a relevant risk factor that exacerbates COPD in urban environments.

Group theory and quasiprobability integrals of Wigner functions

The integral of the Wigner function of a quantum-mechanical system over a region or its boundary in the classical phase plane, is called a quasiprobability integral. Unlike a true probability integral, its value may lie outside the interval [0, 1]. It is characterized by a corresponding selfadjoint operator, to be called a region or contour operator as appropriate, which is determined by the characteristic function of that region or contour. The spectral problem is studied for commuting families of region and contour operators associated with concentric discs and circles of given radius a. Their respective eigenvalues are determined as functions of a, in terms of the Gauss-Laguerre polynomials. These polynomials provide a basis of vectors in a Hilbert space carrying the positive discrete series representation of the algebra su(1, 1) approximate to so(2, 1). The explicit relation between the spectra of operators associated with discs and circles with proportional radii, is given in terms of the discrete variable Meixner polynomials.

Neonatal Clinical Evaluation, Blood Gas and Radiographic Assessment After Normal Birth, Vaginal Dystocia or Caesarean Section in Dogs

This study aimed to standardize signs and diagnostic criteria of respiratory function in newborn puppies delivered normally or after dystocia and caesarean operation. A total of 48 neonates were allocated into groups: eutocia (n = 20), dystocia (n = 8), caesarean (c)-section (n = 20). Neonatal health was assessed using the Apgar score and body temperature was determined at 0, 5 and 60 min after delivery. Venous blood gases (pO(2) and SO(2)) was measured immediately and 60 min after delivery, and a thoracic radiograph was made between 0 and 5 min of life. The c-section group had significantly lower Apgar scores at birth and 5 min. Hypothermia was present at 5 min in the eutocia and c-section groups, and at 60 min in all groups. The eutocia group had an irregular respiratory pattern in 78% of puppies at birth, 27.7% at 5 min and 21% at 60 min compared with 87.5%, 62.5% and 12.5% of the pups in the dystocia group where there was irregular respiratory rhythm, moderate to intense respiratory sounds with agonic episodes. The c-section group had respiratory alterations in 70%, 45% and 16% of puppies at 0, 5 and 60 min, respectively. Radiographic abnormalities were present in 17% of the pups in the eutocia group, 25% of the pups in the dystocia group and 30% of the pups in the c-section group, respectively. The c-section group had significantly lower SO(2) values at 60 min than at birth. All puppies had hypoxaemia, but a significant decrease was observed in the c-section group. Newborn puppies had tissue hypoxia and irregular respiratory pattern at birth. Caesarean-section puppies had lower vitality; however, all developed satisfactory Apgar scores at 5 min of life, regardless of the obstetric condition.

Leptogenesis, CP violation and neutrino data: what can we learn?

A detailed analytic and numerical study of baryogenesis through leptogenesis is performed in the framework of the standard model of electroweak interactions extended by the addition of three right-handed neutrinos, leading to the seesaw mechanism. We analyze the connection between GUT-motivated relations for the quark and lepton mass matrices and the possibility of obtaining a viable leptogenesis scenario. In particular, we analyze whether the constraints imposed by SO(10) GUTs can be compatible with all the available solar, atmospheric and reactor neutrino data and, simultaneously, be capable of producing the required baryon asymmetry via the leptogenesis mechanism. It is found that the Just-So(2) and SMA solar solutions lead to a viable leptogenesis even for the simplest SO(10) GUT, while the LMA, LOW and VO solar solutions would require a different hierarchy for the Dirac neutrino masses in order to generate the observed baryon asymmetry. Some implications on CP violation at low energies and on neutrinoless double beta decay are also considered. (C) 2002 Elsevier Science B.V. All rights reserved.

Estudo exploratório da qualidade do ar em escolas de educação básica, Coimbra, Portugal

OBJETIVO : Analisar a qualidade do ar em escolas de educação básica e suas condições estruturais e funcionais. MÉTODOS : Foi avaliada a qualidade do ar de 51 escolas (81 salas de aula) de educação básica da cidade de Coimbra, Portugal, tanto na parte interior das salas como na exterior, durante as quatro estações do ano, de 2010 a 2011. Foram avaliadas a temperatura (Tº), umidade relativa (Hr), concentrações de monóxido de carbono (CO), dióxido de carbono (CO 2 ), ozona (O 3 ), dióxido de nitrogênio (NO 2 ), dióxido de enxofre (SO 2 ), compostos orgânicos voláteis (COV), formaldeído e material particulado (PM 10 ), de novembro de 2010 a fevereiro de 2011 (outono/inverno) e de março de 2011 a junho de 2011 (primavera/verão). Procedeu-se ao preenchimento de uma grelha de caracterização das condições estruturais e funcionais das escolas. Aplicaram-se os testes estatísticos t- Student para amostras emparelhadas e o teste t de Wilcoxon. RESULTADOS : Em 47 escolas, as concentrações médias de CO 2 encontravam-se acima da concentração máxima de referência (984 ppm) mencionada na legislação portuguesa. Os valores máximos de concentração encontrados no interior das salas foram críticos, principalmente no outono/inverno (5.320 ppm). As concentrações médias de COV e de PM 10 no interior ultrapassaram a concentração máxima de referência legislada em algumas escolas. Não foram detetados valores relevantes (risco) de CO, formaldeído, NO 2 , SO 2 e O 3 . CONCLUSÕES : Houve maior concentração de poluentes no interior das salas, comparativamente com o exterior. A inadequada ventilação está associada à elevada concentração de CO 2 nas salas de aula.

Análise Custo-Efectividade do Samário-153-EDTMP Versus Terapêutica Convencional da Dor em Doentes com Metástases Ósseas Múltiplas Dolorosas em Portugal

Introdução: O cancro da próstata é uma importante causa de morbilidade e mortalidade. Em Portugal, de acordo com um estudo publicado em 2003, a taxa de novos casos de cancro na próstata era de 53 por 100.000 homens, em 2000, com uma taxa de mortalidade padronizada pela idade de 28 por 100.000 (em 1995). As metástases ósseas múltiplas são uma das principais complicações associadas ao cancro de próstata avançado. O Samário-EDTMP mostrou ser uma alternativa segura e eficaz no tratamento paliativo da dor associada a metástases ósseas. O objectivo deste estudo económico é avaliar o custo-efectividade do tratamento da dor associada a metástases ósseas múltiplas com Samário-153-EDTMP versus terapêutica convencional da dor, no carcinoma da próstata hormono-refractário, em Portugal. Metodologia: Estudo de custo-efectividade que compara os custos directos do tratamento de doentes com múltiplas metástases ósseas dolorosas com Samário-153-EDTMP versus terapêutica convencional para a dor, na perspectiva do Sistema Nacional de Saúde, em Portugal, num horizonte temporal de quatro meses. Resultados: Os custos directos totais num período de quatro meses são 2.311,91 € para um doente tratado com Samário-153-EDTMP versus 2.450,74 € para um doente sob tratamento padrão. De acordo com o modelo, um doente tratado com Samário-153-EDTMP representa um decréscimo de custos de 138,83 €. Conclusão: O Samário-153-EDTMP é não só um método terapêutico muito eficaz mas também uma solução com custos reduzidos quando comparado à terapêutica convencional da dor, em doentes com dor devida a metástases ósseas múltiplas, em Portugal.

Representaciones de grupos y álgebras de Lie

Este proyecto cuenta con 7 subproyectos.Subproyecto: Restricciones de representaciones de cuadrado integrable.Se continuará trabajando en el problema de restringir representaciones de cuadrado integrable en un grupo de Lie a un subgrupo semisimple o la factor unipotente de un subgrupo parabólico. En particular, se continuará analizando el caso de restringir desde el grupo SO(2n,1) al subgrupo SO(2) x SO(2n-2,1) y al factor unipotente del parabólico minimal de un grupo de Lie clásico de rango uno. Subproyecto: Representación metapléctica y grupos de Heisenberg generalizados. Se estudia la restricción de la representación metapléctica a subgrupos del grupo metapléctico. Subproyecto: Álgebras de tipo H. Se estudiarán estructuras de biálgebra en las álgebras de tipo H, álgebras de Lie nilpotentes de dos etapas. Se continuará con el estudio de cuantizaciones de álgebras de tipo H. Se estudiarán propiedades geométricas de las funciones theta generalizadas que surgen de álgebras de tipo H. Subproyecto: Módulos de peso máximo. Se intenta dar una respuesta al problema de clasificación de módulos quasifinitos de peso máximo sobre ciertas álgebras de dimensión infinita. Subproyecto: Cuantización de las álgebras de tipo H. Se tratará de cuantizar las álgebras de tipo H, álgebras de Lie nilpotentes de dos etapas. Se trabajará con una definición más general de las álgebras de Heisenberg, tratando de encontrar teoremas tipo Stone-Von Neumann y generalizaciones de las funciones theta. Subproyecto: Continuación analítica de integrales de coeficientes matriciales. Se analiza la existencia de continuación holomorfa de la integral a lo largo de un grupo semisimple real de las potencias complejas de un coeficiente matricial de una representación irreducible admisible. Subproyecto: Cálculo explícito de soluciones fundamentales de operadores invariantes. Se analizan condiciones en el polinomio que define un operador diferencial k-invariante para que resulte hipoellítico. Se trata en particular el caso del grupo SO(n,1). Subproyecto 7: Generadores de Goldie. Se trata de encontrar algoritmos para el cálculo de generadores de Goldie.

Infiltração de água no solo sob escarificação e rotação de culturas

Nos solos com restrições físicas e, ou, físico-hídricas ao crescimento de raízes, aumentar o potencial de armazenagem de água por meio de melhorias na infiltração pode ser uma estratégia viável para aumento da produtividade das culturas. Nesse sentido, este trabalho teve como objetivo avaliar a infiltração de água em um Nitossolo Vermelho distrófico, com três sistemas de rotação de culturas sob semeadura direta com e sem escarificação inicial. O sistema de rotação de culturas constou de: (1) milheto/soja/sorgo/milho/sorgo (M/S/So/Mi/So), (2) milheto/soja/Brachiaria ruziziensis/milho/Brachiaria ruziziensis (M/S/B/Mi/B) e (3) milheto/soja/Brachiaria ruziziensis + mamona/milho/Brachiaria ruziziensis + mamona (M/S/B+Ma/Mi/B+Ma). A infiltração de água no solo foi avaliada em campo com anéis concêntricos instalados na superfície, a 0,10 e 0,20 m de profundidade, em 2006 e 2007. Após o primeiro ano, o manejo com escarificação inicial do solo apresentou a maior infiltração de água. A rotação Brachiaria ruziziensis + mamona proporcionou maior infiltração da água no solo. A atividade do sistema radicular das espécies nas parcelas sem escarificação inicial aumentou a velocidade de infiltração da água no solo.

Deccan volcanism linked to the Cretaceous-Tertiary boundary mass extinction: New evidence from ONGC wells in the Krishna-Godavari basin

A scientific challenge is to assess the role of Deccan volcanism in the Cretaceous-Tertiary boundary (KTB) mass extinction. Here we report on the stratigraphy and biologic effects of Deccan volcanism in eleven deep wells from the Krishna-Godavari (K-G) Basin, Andhra Pradesh, India. In these wells, two phases of Deccan volcanism record the world's largest and longest lava mega-flows interbedded in marine sediments in the K-G Basin about 1500 km from the main Deccan volcanic province. The main phase-2 eruptions (similar to 80% of total Deccan Traps) began in C29r and ended at or near the KTB, an interval that spans planktic foraminiferal zones CF1-CF2 and most of the nannofossil Micula prinsii zone, and is correlative with the rapid global warming and subsequent cooling near the end of the Maastrichtian. The mass extinction began in phase-2 preceding the first of four mega-flows. Planktic foraminifera suffered a 50% drop in species richness. Survivors suffered another 50% drop after the first mega-flow, leaving just 7 to 8 survivor species. No recovery occurred between the next three mega-flows and the mass extinction was complete with the last phase-2 mega-flow at the KTB. The mass extinction was likely the consequence of rapid and massive volcanic CO(2) and SO(2) gas emissions, leading to high continental weathering rates, global warming, cooling, acid rains, ocean acidification and a carbon crisis in the marine environment. Deccan volcanism phase-3 began in the early Danian near the C29R/C29n boundary correlative with the planktic foraminiferal zone P1a/P1b boundary and accounts for similar to 14% of the total volume of Deccan eruptions, including four of Earth's longest and largest mega-flows. No major faunal changes are observed in the intertrappeans of zone P1b, which suggests that environmental conditions remained tolerable, volcanic eruptions were less intense and/or separated by longer time intervals thus preventing runaway effects. Alternatively, early Danian assemblages evolved in adaptation to high-stress conditions in the aftermath of the mass extinction and therefore survived phase-3 volcanism. Full marine biotic recovery did not occur until after Deccan phase-3. These data suggest that the catastrophic effects of phase-2 Deccan volcanism upon the Cretaceous planktic foraminifera were a function of both the rapid and massive volcanic eruptions and the highly specialized faunal assemblages prone to extinction in a changing environment. Data from the K-G Basin indicates that Deccan phase-2 alone could have caused the KTB mass extinction and that impacts may have had secondary effects.

High-resolution ammonite and carbon isotope stratigraphy across the Triassic-Jurassic boundary at New York Canyon (Nevada)

The Triassic-Jurassic boundary is generally considered as one of the major extinctions in the history of Phanerozoic. The high-resolution ammonite correlations and carbon isotope marine record in the New York Canyon area allow to distinguish two negative carbon excursions across this boundary with different paleoenvironmental meanings. The Late Rhaetian negative excursion is related to the extinction and regressive phase. The Early Hettangian delta(13)C(org) negative excursion is associated with a major floristic turnover and major ammonite and radiolarian radiation. The end-Triassic extinction-Early Jurassic recovery is fully compatible with a volcanism-triggered crisis, probably related to the Central Atlantic Magmatic Province. The main environmental stress might have been generated by repeated release of SO(2) gas, heavy metals emissions, darkening, and subsequent cooling. This phase was followed by a major long-term CO(2) accumulation during the Early Hettangian with development of nutrient-rich marine waters favouring the recovery of productivity and deposition of black shales. (C) 2004 Elsevier B.V. All rights reserved.

Mineral zoning and geochemistry of epithermal polymetallic Zn-Pb-Ag-Cu-Bi mineralization at Cerro de Pasco, Peru

The large Cerro de Pasco Cordilleran base metal deposit in central Peru is located on the eastern margin of a middle Miocene diatreme-dome complex and comprises two mineralization stages. The first stage consists of a large pyrite-quartz body replacing Lower Mesozoic Pucara carbonate rocks and, to a lesser extent, diatreme breccia. This body is composed of pyrite with pyrrhotite inclusions, quartz, and black and red chalcedony (containing hypogene hematite). At the contact with the pyrite-quartz body, the diatreme breccia is altered to pyrite-quartz-sericite-pyrite. This body was, in part, replaced by pipelike pyrrhotite bodies zoned outward to carbonate-replacement Zn-Pb ores hearing Fe-rich sphalerite (up to 24 mol % Fes). The second mineralization stage is partly superimposed on the first and consists of zoned east-west-trending Cu-Ag-(Au-Zn-Pb) enargite-pyrite veins hosted in the diatreme breccia in the western part of the deposit and well-zoned Zn-Pb-(Bi-Ag-Cu) carbonate-replacement orebodies; in both cases, sphalerite is Fe poor and the inner parts of the orebodies show typically advanced argillic alteration assemblages, including aluminum phosphate Sulfate (APS) minerals. The zoned enargite-pyrite veins display mineral zoning, from a core of enargite-pyrite +/- alunite with traces of Au, through an intermediate zone of tennantite, chalcopyrite, and Bi minerals to a poorly developed Outer zone hearing sphalerite-galena +/- kaolinite. The carbonate-hosted replacement ores are controlled along N 35 degrees E, N 90 degrees E, N 120 degrees E, and N 170 degrees E faults. They form well-zoned upward-flaring pipelike orebodies with a core of famatinite-pyrite and alunite, an intermediate zone with tetrahedrite-pyrite, chalcopyrite, matildite, cuprobismutite, emplectite, and other Bi minerals accompanied by APS minerals, kaolinite, and dickite, and an outer zone composed of Fe-poor sphalerite (in the range of 0.05-3.5 mol % Fes) and galena. The outermost zone consists of hematite, magnetite, and Fe-Mn-Zn-Ca-Mg carbonates. Most of the second-stage carbonate-replacement orebodies plunge between 25 degrees and 60 degrees to the west, suggesting that the hydrothermal fluids ascended from deeper levels and that no lateral feeding from the veins to the carbonate-replacement orebodies took place. In the Venencocha and Santa Rosa areas, located 2.5 km northwest of the Cerro de Pasco open pit and in the southern part of the deposit, respectively, advanced argillic altered dacitic domes and oxidized veins with advanced argillic alteration halos occur. The latter veins are possibly the oxidized equivalent of the second-stage enargite-pyrite veins located in the western part of the deposit. The alteration assemblage quartz-muscovite-pyrite associated with the pyrite-quartz body suggests that the first stage precipitated at slightly, acidic fin. The sulfide mineral assemblages define an evolutionary path close to the pyrite-pyrrhotite boundary and are characteristic of low-sulfidation states; they suggest that the oxidizing slightly acidic hydrothermal fluid was buffered by phyllite, shale, and carbonate host rock. However, the presence in the pyrite-quartz body of hematite within quartz suggests that, locally, the fluids were less buffered by the host rock. The mineral assemblages of the second mineralization stage are characteristic of high- to intermediate-sulfidation states. High-sulfidation states and oxidizing conditions were achieved and maintained in the cores of the second-stage orebodies, even in those replacing carbonate rocks. The observation that, in places, second-stage mineral assemblages are found in the inner and outer zones is explained in terms of the hydrothermal fluid advancing and waning. Microthermometric data from fluid inclusions in quartz indicate that the different ores of the first mineralization stage formed at similar temperatures and moderate salinities (200 degrees-275 degrees C and 0.2-6.8 wt % NaCl equiv in the pyrite-quartz body; 192 degrees-250 degrees C and 1.1-4.3 wt % NaCl equiv in the pyrrhotite bodies; and 183 degrees-212 degrees C and 3.2-4.0 wt % NaCl equiv in the Zn-Pb ores). These values are similar to those obtained for fluid inclusions in quartz and sphalerite from the second-stage ores (187 degrees-293 degrees C and 0.2-5.2 wt % NaCl equiv in the enargite-pyrite veins: 178 degrees-265 degrees C and 0.2-7.5 wt % NaCl equiv in quartz of carbonate-replacement orebodies; 168 degrees-999 degrees C and 3-11.8 wt % NaCl equiv in sphalerite of carbonate-replacement orebodies; and 245 degrees-261 degrees C and 3.2-7.7 wt % NaCl equiv in quartz from Venencocha). Oxygen and hydrogen isotope compositions oil kaolinite from carbonate-replacement orebodies (delta(18)O = 5.3-11.5%o, delta D = -82 to -114%o) and on alunite from the Venencocha and Santa Rosa areas (delta(18)O = 1.9-6.9%o, delta D = -56 to -73%o). Oxygen isotope compositions of quartz from the first and second stages have 6180 values from 9.1 to 1.7.8 per mil. Calculated fluids in equilibrium with kaolinite have delta(18)O values of 2.0 to 8.2 and delta D values of -69 to -97 per mil; values in equilibrium with alunite are -1.4 to -6.4 and -62 to -79 per mil. Sulfur isotope compositions of sulfides from both stages have a narrow range of delta(34)S values, between -3.7 and +4.2 per mil; values for sulfates from the second stage are between 4.2 and 31.2 per mil. These results define two mixing trends for the ore-forming fluids. The first trend reflects mixing between a moderately saline (similar to 10 wt % NaCl equiv) magmatic end member that had degassed (as indicated by the low delta D values) and meteoric water. The second mixing indicates condensation of magmatic vapor with HCl and SO(2) into meteoric water, which formed alunite. The hydrothermal system at Cerro de Pasco was emplaced at a shallow depth (similar to 500 m) in the epithermal and upper part of a porphyry environment. The similar temperatures and salinities obtained for the first stage and second stages, together with the stable isotope data, indicate that both stages are linked and represent successive stages of epithermal polymetallic mineralization in the upper part of a porphyry system.