A tentative determination of upwelling influence on the paleo-surficial marine water reservoir effect in southeastern Brazil.

Previous work has suggested that seasonal and inter-annual upwelling of deep, cold, radiocarbon depleted waters from the South Atlantic has caused variations in the reservoir effect (R) through time along the southern coast of Brazil. This work aims to examine the possible upwelling influence on the paleo-reservoir age of Brazilian surficial coastal waters based on paired terrestrial/marine samples obtained from archaeological remains. On the Brazilian coast there are hundreds of shell-middens built up by an ancient culture that lived between 6500 to 1500 years ago, but there are few located on open coast with a known upwelling influence. Three archaeological sites located in a large headland in Arraial do Cabo and Ilha de Cabo Frio, southeastern coast of Brazil with open ocean conditions and a well-known strong and large upwelling of the Malvinas/Falkland current were chosen for this study. The 14C age differences between carbonized seed and marine samples varied from 281 ± 44 to 1083 ± 51 14C yr. There are also significant age differences between carbonized seed samples (977 14C yr) and marine samples (200 and 228 14C yr) from the same archaeological layer that cannot be explained by a reservoir effect or an old-wood effect for charcoal. Therefore the present data from the southeastern Brazilian coast are inconclusive for identifying an upwelling effect on R. To do so it would be necessary to more precisely define the present-pre-bomb R in upwelling regions and to analyze paired marine/terrestrial samples that are contemporaneous beyond doubt.

Roteiros Paleo-Geológicos no Barlavento Algarvio

Dissertação mestr., Biologia e Geologia - Educação, Universidade do Algarve, 2007

A percepção da ordem e a consciência do tempo em Mari no período Paleo-Babilónico (séc. XIX- XVIII a. C.)

O presente estudo tem como objectivo estudar as questões do tempo e da ordem no reino de Mari. A análise destas questões evidencia dois aspectos importantes: por um lado, a convergência de duas culturas distintas – uma cultura acádica, tipicamente mesopotâmica, e uma cultura amorrita, mais ocidental – num mesmo espaço e, por outro lado, a importância do reino de Mari como um estudo de caso que retrata, por vezes com grande pormenor, a influência da penetração dos povos nómadas nas terras da Mesopotâmia e as suas repercussões nos vários domínios da vida pública. Estudar a ordem implica compreender a organização do mundo e da sociedade, bem como a relação entre as esferas humana e celeste. Estudar o tempo implica, por sua vez, entender como o homem se posiciona no espaço, como entende a sua história e o seu destino. Uma análise focada nestes dois temas permitir-nos-á, pois, compreender qual era o verdadeiro sentido da vida e do mundo para o homem de Mari. Como veremos, para o mariota, a vida assentava numa intensa dinâmica na qual a família detinha o papel principal: era ela que o enquadrava na sociedade, que lhe permitia participar nos destinos da vida pública e receber as devidas honras após a morte. Nesta perspectiva, a família e os laços de sangue adquiriam um papel preponderante em vários domínios da vida humana. Eram os laços consanguíneos que imperavam aquando da escolha de aliados e partidários. Por outro lado, o culto do parentesco impunha uma visão da história segundo a qual o tempo passado se afirmava como o grande modelo teórico das acções desenvolvidas no quotidiano (no presente). Paralelamente à família, o homem de Mari acreditava que no mundo divino residia a sua verdadeira esperança de levar uma vida feliz. A imagem de uma teocracia, onde homem e deus partilhavam o mesmo destino, é transversal a todo o pensamento e acção do homem de Mari. Nesta tese, propomos desenvolver um estudo de conjunto, uma análise transversal que abranja todos os aspectos da vida social e humana: a religião, a política, a cultura e a sociedade

Miniature Carvings in the Canadian Dorset Culture: the Paleo-Eskimo Belief System

En este estudio, intento resumir los debates relacionados con la última cultura paleoesquimal de Canadá Ártica y la de Groenlandia, y llamar la atención sobre las analogías culturales desde Asia, además de crear un cuadro complejo sobre el chamanismo y el culto al oso de los Dorset. Los temas como el origen del arte de los Dorset, la transición Pre-Dorset-Dorset, y los contactos entre los Dorset y los Thule son relevantes para reconstruir el sistema de creencias de los Dorset. Sin embargo, la totalidad del sistema de creencias de los paleoesquimales no se puede comprender sobre la base de los hallazgos arqueológicosy las analogías etnográficas remotas.

The sea level conundrum: insights from paleo studies

Empirical Constraints on Future Sea Level Rise; Bern, Switzerland, 25–29 August 2008; Eustatic sea level (ESL) rise during the 21st century is perhaps the greatest threat from climate change, but its magnitude is contested. Geological records identify examples of nonlinear ice sheet response to climate forcing, suggesting a strategy for refining estimates of 21st-century sea level change. In August 2008, Past Global Changes (PAGES), International Marine Past Global Change Study (IMAGES), and the University of Bern cosponsored a workshop to address this possibility. The workshop highlighted several ways that paleoceanography studies can place limits on future sea level rise, and these are enlarged upon here.

Using paleo-climate comparisons to constrain future projections in CMIP5

We present a description of the theoretical framework and "best practice" for using the paleo-climate model component of the Coupled Model Intercomparison Project (Phase 5) (CMIP5) to constrain future projections of climate using the same models. The constraints arise from measures of skill in hindcasting paleo-climate changes from the present over 3 periods: the Last Glacial Maximum (LGM) (21 thousand years before present, ka), the mid-Holocene (MH) (6 ka) and the Last Millennium (LM) (850–1850 CE). The skill measures may be used to validate robust patterns of climate change across scenarios or to distinguish between models that have differing outcomes in future scenarios. We find that the multi-model ensemble of paleo-simulations is adequate for addressing at least some of these issues. For example, selected benchmarks for the LGM and MH are correlated to the rank of future projections of precipitation/temperature or sea ice extent to indicate that models that produce the best agreement with paleoclimate information give demonstrably different future results than the rest of the models. We also find that some comparisons, for instance associated with model variability, are strongly dependent on uncertain forcing timeseries, or show time dependent behaviour, making direct inferences for the future problematic. Overall, we demonstrate that there is a strong potential for the paleo-climate simulations to help inform the future projections and urge all the modeling groups to complete this subset of the CMIP5 runs.

Glacial-interglacial temperature change in the tropical West Pacific: a comparison of stalagmite-based paleo-thermometers

In the tropics, geochemical records from stalagmites have so far mainly been used to qualitatively reconstruct changes in precipitation, but several new methods to reconstruct past temperatures from stalagmite material have emerged recently: i) liquid–vapor homogenization of fluid inclusion water ii) noble gas concentrations in fluid inclusion water, iii) the partitioning of oxygen isotopes between fluid inclusion water and calcite, and iv) the abundance of the 13C18O16O (‘clumped’) isotopologue in calcite. We present, for the first time, a direct comparison of these four paleo-thermometers by applying them to a fossil stalagmite covering nearly two glacial–interglacial cycles (Marine Isotope Stages (MIS) 12–9) and to two modern stalagmites, all from northern Borneo. The temperature estimates from the different methods agree in most cases within errors for both the old and recent samples; reconstructed formation temperatures of the recent samples match within 2-sigma errors with measured cave temperatures. However, slight but systematic deviations are observed between noble gas and liquid–vapor homogenization temperatures. Whereas the temperature sensitivity of fluid inclusion δ18O and clumped isotopes is currently debated, we find that the calibration of Tremaine et al. (2011) for fluid inclusion δ18O and a synthetic calcite-based clumped isotope calibration (Ziegler et al., in prep.) yield temperature estimates consistent with the other methods. All methods (with the potential exception of clumped isotopes) show excellent agreement on the amplitude of glacial–interglacial temperature change, indicating temperature shifts of 4–5 °C. This amplitude is similar to the amplitude of Mg/Ca-based regional sea surface temperature records, when correcting for sea level driven changes in cave elevation. Our reconstruction of tropical temperature evolution over the time period from 440 to 320 thousand years ago (ka) adds support to the view that climate sensitivity to varying greenhouse forcing is substantial also in the deep tropics.

Delaware Reservoirs’ Drought Risk Assessment: A Paleo View

The Delaware River provides half of New York City's drinking water, is a habitat for wild trout, American shad and the federally endangered dwarf wedge mussel. It has suffered four 100‐year floods in the last seven years. A drought during the 1960s stands as a warning of the potential vulnerability of the New York City area to severe water shortages if a similar drought were to recur. The water releases from three New York City dams on the Delaware River's headwaters impact not only the reliability of the city’s water supply, but also the potential impact of floods, and the quality of the aquatic habitat in the upper river. The goal of this work is to influence the Delaware River water release policies (FFMP/OST) to further benefit river habitat and fisheries without increasing New York City's drought risk, or the flood risk to down basin residents. The Delaware water release policies are constrained by the dictates of two US Supreme Court Decrees (1931 and 1954) and the need for unanimity among four states: New York, New Jersey, Pennsylvania, and Delaware ‐‐ and New York City. Coordination of their activities and the operation under the existing decrees is provided by the Delaware River Basin Commission (DRBC). Questions such as the probability of the system approaching drought state based on the current FFMP plan and the severity of the 1960s drought are addressed using long record paleo‐reconstructions of flows. For this study, we developed reconstructed total annual flows (water year) for 3 reservoir inflows using regional tree rings going back upto 1754 (a total of 246 years). The reconstructed flows are used with a simple reservoir model to quantify droughts. We observe that the 1960s drought is by far the worst drought based on 246 years of simulations (since 1754).

Taphonomy of Bouchardia rosea (Rhynchonelliformea, Brachiopoda) shells from Ubatuba Bay, Brazil: implications for the use of taphonomic signatures in (paleo)environmental analysis

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Viés Analítico em Estudos Tafonômicos com Macroinvertebrados: Implicações (Paleo)Ambientais e (Paleo)Ecológicas

A review of recent literature shows that most taphonomic studies of Holocene and fossil macrovertebrates are not methodologically standardized. Hence, results from distinct studies are not comparable, even among researches sharing virtually identical goals, targeting the same biological group of similar age and depositional environment. The effects of the shell size in the taphonomic analysis are still poorly understood. In order to study this issue, the taphonomic signatures (articulation, valve type, fragmentation, abrasion, corrosion, edge modification, color alteration, bioerosion and encrustation) of brachiopod shells (Bouchardia rosea (Mawe)), from Ubatuba Bay in the northern coast of São Paulo State, were investigated according to the sieve sizes. In the study area, 14 collecting stations were sampled via Van Veen grab sampler, along a bathymetric gradient, ranging from 0 to 35 m of depth. Bulk samples were sieved through 8 mm, 6 mm, and 2 mm mesh sizes, yielding a total of 5.204 shells. The results indicate that, when taphonomic signatures were independently analyzed per size classes (8 mm, 6 mm, and 2 mm), the taphonomic signatures are recorded in a complex and random way. Additionally, cluster analysis showed that the similarity among the clusters vary according to the considered sieve size. Thus, the sieve size plays an important role in the distribution of taphonomic signatures in shells of distinct sizes. These results suggest that the concentration of the taphonomic analysis on one class (e.g., the largest sieve size, 8 mm) is not always the best method. Rather, the total data (all sieves included) seems more accurate in recording the whole spectrum of taphonomic processes recorded in shells of a given assemblage.

Paleo expo: uma exposição sobre a história da vida na terra para alunos do ensino fundamental

A importância do estudo da paleontologia está no seu caráter integrador, reunindo conhecimentos de várias áreas, o que pode contribuir para que os alunos do ensino básico entendam a história da vida no planeta, encarando a evolução como um processo contínuo e bem evidenciado no qual também estamos inseridos. No contexto de pequena presença do ensino da paleontologia na Educação Básica, outros espaços de educação não formal ganham força na transmissão desses conhecimentos à população e, dentre estes espaços, na área da paleontologia, encontram-se as exposições de fósseis. Estas permitem que os conhecimentos desenvolvidos na universidade e que normalmente ficam restritos ao âmbito universitário sejam levadas ao conhecimento de um grande número de alunos, contribuindo para a formação e alfabetização científica. A partir desta perspectiva, o presente estudo teve como objetivo o desenvolvimento e a avaliação de uma exposição de fósseis e réplicas para os alunos do ensino básico da rede pública das escolas de Botucatu e região. Através dessa exposição, chamada Paleo Expo, pretendeu-se que os alunos conhecessem a história da vida na Terra, tivessem contato com os principais eventos evolutivos e entendessem a evolução como um processo contínuo e bem evidenciado, contribuindo para o enriquecimento dos conhecimentos dos visitantes, aguçando a curiosidade e gerando reflexões. A exposição, destinada a alunos de sexta a oitava series do ensino fundamental, priorizou a participação ativa dos alunos e contou também com atividades complementares, que consistiram em um jogo educativo e uma apresentação de informações sobre como são realizadas as pesquisas em paleontologia. A Paleo Expo, de um modo geral, atingiu seus objetivos e os alunos se mostraram estimulados e participativos. Pode-se considerar, pelos dados coletados, que a experiência... (Resumo completo, clicar acesso eletrônico abaixo)