The analysis of ceramic fragments from the site of Puerto Nuevo (1000-500 AC), on the south coast of Peru, reveals a diversified ceramic production and possible long distance interaction networks for ceramics along the coast during the first half of the first millennium before our era. Macroscopic analysis with a hand-held digital low power microscope of fresh cross-sections conducted by Alejandro Rey de Castro allowed classifying the ceramics in different paste groups as well as identifying atypical ceramics. Petrographic analysis conducted by Isabelle Druc on 120 ceramic thin sections of these fragments helped refine this classification into six compositional groups, providing more details on the production and provenance of the wares. Comparison with 30 thin sections of clay-tiles collected in the lower and middle valley of the Ica and Pisco Rivers and on the littoral between the two rivers, showed that a majority of ceramics was manufacturedwith local sediments without much sorting. Different resource areas were exploited around Puerto Nuevo, on the littoral and in the Lower and Middle Ica and Pisco valleys. Based on these results, we propose the existence of severalcommunities of potters working in the Puerto Nuevo region. One (or more) of these communities must have used coastal sandy clays with no need to ad temper, another mined inland clay deposits with natural inclusions of charophyte algae, and other(s) used materials rich in granodioritic rock fragments. Thirteen atypical ceramics were singled out based on different composition, texture, or firing, suggesting other production modes. Their composition, however, still suggests a coastal provenance, indicating that the interaction network extended along the coast, rather than with the highlands. / El análisis de fragmentos de vasijas de cerámica del sitio de Puerto Nuevo (1000 a 500 a.C.), en la costa sur del Perú, revela la existencia de una producción diversificada y la probable existencia de redes de intercambio a larga distancia de vasijas de cerámica a lo largo de la costa durante la primera mitad del primer milenio antes de nuestra era. El examen macroscópico con lupa digital sobre cortes frescos realizado por Alejandro Rey de Castro permitió agrupar inicialmente los fragmentos en diferentes grupos de pasta, así como identificar varios fragmentos atípicos. A partir del análisis petrográfico de 120 láminas delgadas de estas cerámicas, Isabelle Druc refinó esta agrupación inicial en seis grupos de composición que brindan informaciones más detalladas sobre la producción y la procedencia de las vasijas de cerámica de las cuales provienen estos fragmentos. El análisis petrográfico de estas 120 láminas delgadas de fragmentos de cerámicas con 30 láminas delgadas de muestras de arcilla de los valles bajo y medio de los ríos Ica y Pisco, y del área de litoral entre lasdesembocaduras de ambos evidencia que la mayoría de las vasijas de cerámica estudiadas fueron producidas con sedimentos locales sin mucha selección granulométrica. Diversas fuentes de materias primas fueron explotadas, tanto en el área de litoral alrededor de Puerto Nuevo, como en los valles bajo y medio de los ríos Ica y Pisco. A partir de estos resultados, proponemos la existencia de varias comunidades de alfareros que trabajaban en la región de Puerto Nuevo —al menos, una caracterizada por el uso de una arcilla arenosa a la que no se agregaba temperante; otra, por el uso de una arcilla rica en algas carofitas; y otra a la que se le agregaba un temperante granodiorítico—. Trece fragmentos de vasijas de cerámica petrográficamente atípicos —con una composición, textura o cocción distintas a las de los grupos identificados para Puerto Nuevo— sugieren la existencia de otros modos de producción, mientras que el hecho de que en todos estos casos la composición sea de tipos costeños podría indicar la existencia de redes de intercambio de vasijas de cerámica preferentemente a lo largo de la costa, en lugar de entre la costa y la sierra.

A procedência dos dados consiste no conjunto de metadados que possibilita identificar as fontes e os processos de transformação aplicados aos dados, desde a criação até o estado atual desses dados. Existem diversas motivações para se incorporar a procedência ao processo de integração, tais como avaliar a qualidade dos dados das fontes heterogêneas, realizar processos de auditoria dos dados e de atribuição de autoria aos proprietários dos dados e reproduzir decisões de integração. Nesta dissertação é proposto o MPPI, um modelo de procedência para subsidiar processos de integração. O modelo enfoca sistemas nos quais as fontes de dados podem ser atualizadas somente pelos seus proprietários, impossibilitando que a integração retifique eventuais conflitos de dados diretamente nessas fontes. O principal requisito do MPPI é que ele ofereça suporte ao tratamento de todas as decisões de integração realizadas em processos anteriores, de forma que essas decisões possam ser reaplicadas automaticamente em processos de integração subsequentes. O modelo MPPI possui quatro características. A primeira delas consiste no mapeamento da procedência dos dados em operações de cópia, edição, inserção e remoção, e no armazenamento dessas operações em um repositório de operações. A segunda característica é o tratamento de operações de sobreposição, por meio da proposta das políticas blind, restrict, undo e redo. A terceira característica consiste na identificação de anomalias decorrentes do fato de que fontes de dados autônomas podem alterar os seus dados entre processos de integração, e na proposta de quatro tipos de validação das operações frente a essas anomalias: validação completa, da origem, do destino, ou nenhuma. A quarta característica consiste na reaplicação de operações, por meio da proposta dos métodos VRS (do inglês Validate and Reapply in Separate) e VRT (do inglês Validate and Reapply in Tandem) e da reordenação segura do repositório, os quais garantem que todas as decisões de integração tomadas pelo usuário em processos de integração anteriores sejam resolvidas automaticamente e da mesma forma em processos de integração subsequentes. A validação do modelo MPPI foi realizada por meio de testes de desempenho que investigaram o tratamento de operações de sobreposição, o método VRT e a reordenação segura, considerando como base as demais características do modelo. Os resultados obtidos mostraram a viabilidade de implementação das políticas propostas para tratamento de operações de sobreposição em sistemas de integração reais. Os resultados também mostraram que o método VRT proporcionou ganhos de desempenho significativos frente à coleta quando o objetivo é restabelecer resultados de processos de integração que já foram executados pelo menos uma vez. O ganho médio de desempenho do método VRT foi de pelo menos 93%. Ademais, os testes também mostraram que reordenar as operações antes da reaplicação pode melhorar ainda mais o desempenho do método VRT / Data provenance is the set of metadata that allows for the identification of sources and transformations applied to data, since its creation to its current state. There are several advantages of incorporating data provenance into data integration processes, such as to estimate data quality and data reliability, to perform data audit, to establish the copyright and ownership of data, and to reproduce data integration decisions. In this master\'s thesis, we propose the MPPI, a novel data provenance model that supports data integration processes. The model focuses on systems in which only owners can update their data sources, i.e., the integration process cannot correct the sources according to integration decisions. The main goal of the MPPI model is to handle decisions taken by the user in previous integration processes, so they can be automatically reapplied in subsequent integration processes. The MPPI model introduces the following properties. It is based on mapping provenance data into operations of copy, edit, insert and remove, which are stored in an operation repository. It also provides four techniques to handle overlapping operations: blind, restrict, undo and redo. Furthermore, it identifies anomalies generated by sources that are updated between two data integration processes and proposes four validation approaches to avoid these anomalies: full validation, source validation, target validation and no validation. Moreover, it introduces two methods that perform the reapplication of operations according to decisions taken by the user, called the VRS (Validate and Reapply in Separate) and the VRT (Validate and Reapply in Tandem) methods, in addition to extending the VRT method with the safe reordering optimization. The MPPI model was validated through performance tests that investigated overlapping operations, the VRT method and the safe reordering optimization. The tests showed that the techniques proposed to handle overlapping operations are feasible to be applied to real integration systems. The results also demonstrated that the VRT method provided significant performance gains over data gathering when the goal is to reestablish previous integration results. The performance gains were of at least 93%. Furthermore, the performance results also showed that reordering the operations before the reapplication process can improve even more the performance of the VRT method

[pt] Muitos experimentos científicos são elaborados como fluxos de tarefas computacionais, que podem ser implementados através do uso de linguagens de programação. Na área de bioinformática é muito comum o uso de scripts ad-hoc para construir fluxos de tarefas. Os Sistemas de Gerência de Workflow Científico (SGWC) surgiram como uma alternativa a estes scripts. Uma das funcionalidades desses sistemas que têm recebido bastante atenção pela comunidade científica é a captura automática de dados de proveniência. Estes permitem averiguar quais foram os recursos e parâmetros utilizados na geração dos resultados, dentre muitas outras informações indispensáveis para a validação e publicação de um experimento. Neste trabalho foram levantados alguns desafios na área de proveniência de dados em SGWCs, como por exemplo (i) a heterogeneidade de formas de representação dos dados nos diferentes sistemas, dificultando a compreensão e a interoperabilidade; (ii) o armazenamento de dados consumidos e produzidos e (iii) a reprodutibilidade de uma execução específica. Estes desafios motivaram a elaboração de um esquema conceitual de proveniência de dados para a representação de workflows. Foi implementada também uma extensão em um SGWC específico (BioSide) para incluir dados de proveniência e armazená-los utilizando o esquema conceitual proposto. Foram priorizados neste trabalho alguns requisitos comumente encontrados em workflows de Bioinformática. / [en] Many scientific experiments are designed as computational workflows, which can be implemented using traditional programming languages. In the Bioinformatics domain ad-hoc scripts are often used to build workflows. Scientific Workflow Management Systems (SWMS) have emerged as an alternative to those scripts. One particular SWMS feature that has received much attention by the scientific community is the automatic capture of provenance data. These allow users to track which resources and parameters were used to obtain the results, among many other required information to validate and publish an experiment. In the present work we have elicited some data provenance challenges in the SWMS context, such as (i) the heterogeneity of data representation schemes that hinders the understanding and interoperability; (ii) the storage of consumed and produced data and (iii) the reproducibility of a specific execution. These challenges have motivated the proposal of a data provenance conceptual scheme for workflow representation. We have implemented an extension of a particular SWMS system (Bioside) to include provenance data and store them using the proposed conceptual scheme. We have focused on some requirements commonly found in bioinformatics workflows.

The thesis addresses the problem of capturing and tracking multi-user interpretations of 3D spatial datasets. These interpretations are completed after the end of the visualization pipeline to identify and extract features of interest, and are subjective to human intuition and knowledge. Users may also assess regions of these interpretations. Consequently, the thesis proposes a provenance-enabled interpretation pipeline. It adopts and extends the W3C PROV data model, producing a provenance model for visual interpretations. This was implemented for seismic imaging interpretation in a proof-of-concept prototype architecture and application. Accumulation of users' interpretations and annotations are captured by the provenance model in a fine-grained form. The captured provenance information can be utilised to filter data. The work of this thesis was evaluated in three parts. First, a usability evaluation by geoscientists was conducted by postgraduate students in the field of geoscience to illustrate the system's ability in allowing users to amend others' interpretations and trace the history of amendments. Second, a conceptual evaluation of this research was approached by interviewing domain experts. The importance of this research to the industry was assured. Interviewees perceived and shared potential implementations of this work in the workflow of seismic interpretation. Limitations and concerns of the work were highlighted. Third, a performance evaluation was conducted to illustrate the behaviour of the architecture on commodity machines as well as on a multi-node parallel database, such that a new functionality in fine-grained provenance can be implemented simply but with an acceptable performance in realistic visualization tasks. The measures suggested that the current implementation achieved an acceptable performance in comparison to conventional methods. The proposed provenance model in an interpretation pipeline is believed to be a promising shift in methods of data management and storage which can record and preserve interpretations by users as a result of visualization. The approach and software development in this thesis represented a step in this direction.

The Numidian Flysch Formation is a regionally extensive series of deep marine sandstones and mudstones which crop out in Spain, Morocco, Algeria, Tunisia, Sicily, and southern mainland Italy. The formation is dated as Oligocene to mid Miocene and represents an approximately linear series of submarine fans characterised by a quartz rich petrofacies. Their unique regional extent is nearly twice the length of the Angolan margin although issues surrounding provenance and basin context have hampered understanding. The Numidian Flysch Formation was deposited into the Maghrebian Flysch Basin (MFB) which was a foreland basin remnant of the neo-Tethys ocean in the western portion of the present day Mediterranean Basin. The basin was bordered to the north by an active margin which consisted of a southward verging accretionary prism, underlain by European crustal blocks which rode above northwards subducting oceanic crust. To the south, the African margin formed a passive-margin to the basin.The huge amount of geophysical and outcrop data which is becoming increasingly available suggests that submarine slope systems are more complex than previously thought, including topographically complex slopes, a wide variety of density flow types, and flow transformations. This thesis aims to review the sedimentology of the Numidian Flysch Formation in Sicily and Tunisia in light of these developments. Constraining the provenance and basin context of the formation is therefore of paramount importance, and this is also addressed.Commonly used evidence for the provenance of Numidian Flysch sandstones include its quartz rich petrology, an Eburnian and Pan-African age detrital zircon suite, its structural position within the foreland fold and thrust belt, and complex palaeocurrent orientations. when reviewd in their entirety and placed in context of other basin successions, the Numidian Flysch is constrained to a depositional location in the south of the basin, with polycyclic sediment sourced from African basement. The Numidian Flysch Formation is therefore a 'passive margin' sequence as opposed to a flysch sensu stricto. The timing of Numidian Flysch deposition is also coincidental with uplift of the Atlas chain in North Africa, during a period of significantly wetter conditions. A switch from carbonate to clastic deposition results from these conditions, and the Numidian Flysch Formation is considered an offshore extension of this regional sedimentation.Characterisation of outcrops in Sicily and Tunisia shows remarkably similar lithofacies and depositional elements. Sinuous upper slope channel complexes are entrenched within slope deposits to a depth of 100 m and occur within channel systems up to 5.7 km in width. They are filled predominantly with massive ungraded sandstones interpreted to aggrade through quasi-steady turbidity currents, interbedded with normally graded turbidites. Channel elements are subseismic in scale, are nested within complexes and show sinuosity. Coupled with lateral offset stacking, this strongly affects the architecture and facies heterogeneity of channel complexes. When compared to globally reviewed data, the thickness of channel elements as shown through their frequency distribution also suggests a fundamental control upon the degree of slope incision which is as yet unconstrained.In lower slope settings, channel complexes stack aggradationally with a width of over 1000 m. They are also predominantly filled with massive sandstones in fining upwards cycles, and show heterogeneous margins and large scale slumping. In central Sicily, large channel complexes are overlain by a stacked lobe complex, in turn overlain by a channel lobe transition zone. This progression coupled with palaeocurrent variability suggests intraslope deformation strongly impacts transiting flows through changes in flow capacity. Salt tectonics, present in Algeria and Tunisia is a possible forcing mechanism.Taken in context, the sections in Sicily record a proximal to distal palaeogeographic trend which is reconstructed towards the north/northeast once well constrained tectonic rotations are taken into account. Given regional similarities, controls upon slope architecture are interpreted to be similar throughout the basin, and deposits in Sicily therefore provide a good analogue for the remainder of the basin. These results therefore allow for a better constrained fan architecture, along with the allogenic controls upon them. Given the continental extent of this formation, the Numidian Flysch Formation provides a unique opportunity to study controls upon fan architecture once provenance and intraslope topography is factored in.

Indiana University-Purdue University Indianapolis (IUPUI) / The outwash deposits of the Eel River paleo meltwater channel in DeKalb and Allen Counties, Indiana predominantly originated from the Erie Lobe of the Laurentide Ice Sheet, but do contain some sediment from the Saginaw Lobe. This determination helps clarify the ice dynamics and Last Glacial Maximum sediment depostional history in northeastern Indiana, which is complicated because of the interactions between the Erie and Saginaw Lobes. Outwash deposits were analyzed from IGS core SC0802 in the Eel River paleo meltwater channel, which intersects the previously identified Huntertown Formation. The core includes 29.2 m of deposits underlain by the hard glacial till of the Trafalgar formation. Mean grain size, sediment skewness, lithology, magnetic susceptibility, and quantitative X-ray diffraction were used to evaluate the provenance of the outwash deposits. Representative samples of Erie Lobe and Saginaw Lobe deposits were analyzed to develop end member provenance signatures. A weight of evidence approach was developed and revealed that deposits from 8.0-13.8 m are of mixed origin from the Erie and Saginaw Lobes, whereas the 0-8.0 and 13.8-29.2 m deposits are Erie Lobe in origin. Cluster analysis and discriminant function analysis supported the findings of this approach. These findings suggests that the Eel River paleo meltwater channel was formed as an outwash channel, and that the adjacent Huntertown Formation does not appear to have been directly deposited by the Saginaw Lobe. The sediments of Saginaw origin from ~8-14 m in the Eel River paleo meltwater channel were likely transported from an upgradient source. The sediments from this zone have a larger mean grain size indicating deposition occurred during higher meltwater discharge, such as the release of meltwater from the drainage of proglacial or subglacial lake(s) associated with the disintegration of the Saginaw Lobe, thus resulting in the mixing of Saginaw Lobe deposits with Erie Lobe deposits. However, the majority of the sediment in the Eel River paleo channel near SC0802 is Erie Lobe in origin. Based on the provenance and depositional sequence at SC0802, the Saginaw Lobe disintegrated prior to the Erie Lobe retreat from the Wabash moraine around 16-17 cal ka.

Indiana University-Purdue University Indianapolis (IUPUI) / Reproducible computing and research are of great importance for scientific investigation in any discipline. This thesis presents a general approach to provenance in the context of workflows for widely used script languages. Our solution is based on system integration, and is demonstrated by integrating MATLAB with VisTrails, an open source scientific workflow system. The integrated VisTrails-MATLAB system supports reproducible computing with truly prospective and retrospective provenance at multiple granularity levels as scientists choose for their scripts, and at the same time, is very easy to use.

Indiana University-Purdue University Indianapolis (IUPUI) / Tills from major ice streams (Institute, Foundation, Academy, Recovery, and Slessor) of the Weddell Sea Embayment contain detrital zircons with distinct U-Pb age populations that can be used as a provenance tool to better understand ice stream dynamics. U-Pb ages of detrital zircons were measured in 21 samples of onshore till, erratics, and bedrock of potential source rocks, and 12 samples of offshore till. Grains were analyzed by LA-ICPMS at the University of Arizona (n=5447). Relative probability U-Pb age density plots of till in moraines along the Institute Ice Stream have dominant Grenville (1070 Ma) and secondary Ross/Pan-African peaks (560 Ma, 630 Ma). The Foundation and Academy show prominent Ross/Pan-African peaks (500-530 Ma and 615-650 Ma). The Recovery transports zircons with prominent 530 Ma and 635 Ma peaks along the southern margin, and 1610 and 1770 Ma along the northern margin. The Slessor carries zircons with prominent populations at 1710 Ma and secondary 2260-2420 Ma. U-Pb ages in zircons from offshore till samples show a general trend of fewer Mesozoic ages from west to east. The western most core, PS 1423, has dominant Jurassic populations while cores 1197 and 1278 have a high proportion of early Ross/Pan-African ages relative to Grenville ages. The similar zircon age distributions between PS 1278 and the Foundation Ice Stream tills suggest that the Foundation switched to an easterly flow path around Berkner Island (BI) at some point during the LGM. In the eastern Weddell Sea (PS 1400), there was a near absence of Proterozoic zircon age populations carried by the Slessor and northern side of the Recovery. Another unexpected find was a lack of Grenville ages in PS 1423 relative to the Institute tills. The U-Pb data in this study provides a basis for two possible LGM ice flow reconstructions. In the first, the Institute flowed west around the unnamed isolated bedrock highs, deposited tills between PS 1423 and PS 1197, providing a westerly flow path around BI for the Foundation. In the second, the Institute flows over the subglacial topography and deposited till closer to PS 1197, forcing the Foundation east around BI.

Indiana University-Purdue University Indianapolis (IUPUI) / A broad range of samples were collected from the Huron-Erie Lobe, Lake Michigan Lobe, Saginaw Lobe, and Tipton Till Plain of northern Indiana to determine the provenance of Laurentide Ice Sheet till in the Midwest U.S. during the Illinoian and Wisconsinan glaciations. U-Pb age distributions from approximately 300 detrital zircons (DZ) were used as provenance indicators for each till sample. Till from the Lake Michigan Lobe and was found to be largely homogenized. The distinct lobe DZ age distributions are the Lake Michigan Lobe till with a dominant ~1465 Ma peak, the northern Huron-Erie Lobe till with a dominant ~1060 Ma and a secondary peak at ~1450 Ma, the southern Huron-Erie Lobe till with nearly equal peaks at ~1435 Ma, ~1175 Ma, and ~1065 Ma, and the southern Saginaw Lobe till with a dominant peak at ~1095 Ma. Those four DZ age distributions were treated as endmembers in a nonlinear least-squares mixing model to calculate the contribution of each lobe to till in the Tipton Till Plain. Huron-Erie and Saginaw lobe tills were found to be the primary components of the Tipton Till Plain, and Lake Michigan Lobe till was only found in the western Tipton Till Plain. Zircons from the Saginaw Lobe till increased 39 % in the eastern Tipton Till Plain between the Illinoisan and Wisconsinan glaciations. The mixing model was also applied to relate the DZ age distributions of the lobes to bedrock within and near their flow paths. When comparing nearby bedrock to each lobe’s till, mixing model results, yield an approximate maximum transport distance between 500 and 630 kilometers for the matrix vii fraction of till in the Lake Michigan, Huron-Erie, and Saginaw lobes. Samples for the southern Huron-Erie Lobe indicate that the most of the zircon ages within the southern Huron-Erie Lobe till in Indiana were specifically entrained between Niagara County, New York and east-central Indiana. Within the model’s error, 93 – 100 % of the detrital zircons in each of the three lobes are relatable to nearby Paleozoic and Precambrian sedimentary and metamorphic bedrock formations.

Indiana University-Purdue University Indianapolis (IUPUI) / Tills for this study were analyzed from sites in East Antarctica (EA), West Antarctica (WA) and along a transect in the Ross Sea. Particle size, sand petrography, and detrital zircons were used to provide new information on the subglacial geology of Antarctica, as well as assisting in the reconstruction of Last Glacial Maximum (LGM) ice flow paths. Statistical analyses using the Kolmogorov-Smirnov (K-S test) reveal that EA and WA zircon age distributions are distinct at a P-value <0.05. This makes it possible to trace the unique signatures from EA and WA into the Ross Sea.