Active solids{,} more specifically elastic lattices embedded with polar active units{,} exhibit collective actuation when the elasto-active feedback{,} generically present in such systems{,} exceeds some critical value. The dynamics then condensates on a small fraction of the vibrational modes{,} the selection of which obeys non trivial rules rooted in the nonlinear part of the dynamics. So far{,} the complexity of the selection mechanism has limited the design of specific actuation. Here{,} we investigate numerically how localizing activity to a fraction of modes enables the selection of non-trivial collective actuation. We perform numerical simulations of an agent-based model on triangular and disordered lattices and vary the concentration and the localization of the active agents on the lattice nodes. Both contribute to the distribution of the elastic energy across the modes. We then introduce an algorithm{,} which{,} for a given fraction of active nodes{,} evolves the localization of the activity in such a way that the energy distribution on a few targeted modes is maximized – or minimized. We illustrate on a specific targeted actuation{,} how the algorithm performs as compared to manually chosen localization of the activity. While{,} in the case of the ordered lattice{,} a well-educated guess performs better than the algorithm{,} and the latter outperform the manual trials in the case of the disordered lattice. Finally{,} the analysis of the results in the case of the ordered lattice leads us to introduce a design principle based on a measure of the susceptibility of the modes to be activated along certain activation paths.

Fjords are considered biodiversity hotspots and aquatic critical zones, being extremely sensitive to climate change due to close oceanic, terrestrial, and glacial interactions. These ecosystems have received a great deal of attention in research on current and future anthropic impacts. Despite this, there is no analog in the geological record that presents icehouse-greenhouse biological and climatic changes. Here we present an analog, through a detailed taphonomic survey of the Lontras Shale Lagerstätte (Itararé Group, Paraná Basin, Brazil), related to a climatic optimum of the end of the Late Paleozoic Ice Age (Late Pennsylvanian), in which a temperate outer paleofjord with a rich well-preserved biota was installed. In the monotone layers of black shale, we find subtle variations of the dominant skeletal type, rates of fragmentation and disarticulation, and other taphonomic aspects that define distinct taphofacies. Each of them is the result of distinct time-averaging related to mass mortality events, turbidity, and depositional hiatus periods at different scales and intensities, mixing the ecologic census with short-term and long-term within-habitat assemblages. In addition, the rich paleobiota was reconstructed with autochthonous and allochthonous benthic fauna, many marine nektonic organisms, and intense continental contribution of terrestrial bioclasts, that proliferated and were exceptionally preserved by the establishment of an anoxic temperate outer fjord. The taphofacies show an evolution in a high-frequency sequence within a highstand systems tract, linked to climatic improvement. Furthermore, taphonomic detailing can be used as a comparison of deep marine and deep lacustrine taphofacies, in addition to serving as an analog for the short-time scale biological, biogeochemical, climatic, and stratigraphic changes associated with the icehouse–greenhouse transition in the past, present, and future.

Abstract Pierre Bourdieu’s theoretical contributions pave the way for studying a wide range of social spaces, such as the academia. Through using Bourdieusian fields, our objective was to investigate whether the teaching area of the Coordination for the Improvement of Higher Education Personnel (CAPES) can be considered a relatively autonomous scientific field. Therefore, this study is motivated by two research questions: 1) what is the distribution of scientific capital in the teaching area; and 2) what are the implications of this distribution on its constitution as a scientific field. By crossing data on professors of programs in the field of education with the evaluation grade assigned by Capes to each of these programs, our analysis revealed that this area does not constitute a scientific field. Differently from what happens in well-established fields, most teaching advisors come from many different scientific backgrounds and do not recognize this field’s specific intellectual production as scientific capital. Assuming that the existing disputes between professors with less and more scientific capital can generate new conformations in the area, a possible structure could be a stabilization of the subgroup of professors with greater scientific capital and its constitution as a scientific field, whose agents become increasingly aware that their cognitive structure and ideals of education/research are different from what Capes intended to homogenize with the creation of a teaching area. We believe that our results can be a reference for critical reflection on the structure of the field of teaching, which is still driven by its agents.

Este livro, organizado por Eros Moreira de Carvalho (UFRGS/CNPq), contém a tradução para o português de sete verbetes da Stanford Encyclopedia of Philosophy na área de filosofia da cognição.

{The study of sambaquis (ancient shell mounds) in conservation paleobiology is a complicated subject, especially when comparing body sizes of current and past mollusk valves to observe possible changes. There is a lack of information regarding how ancient fisher-gardeners collected these shellfish. Another obstacle is finding the hypothesis tests and data that can be used to compare current and past body sizes. To this end, we use the t-test (tt), Mann-Whitney (mw), and Bootstrap (bt) analyses to determine data scenarios for yellow clam (Amarilladesma mactroides) shells from two sambaquis units, and from two transects along the beaches of Rio Grande do Sul in southern Brazil. The study finds that the average body size of an Amarilladesma mactroides adult specimen is greater in sambaquis than the current valves across all tests (tt

Neste artigo, mapeio o terreno da discussão em torno das teorias da conspiração, destacando o problema de como defini-las, os fatores que levam à crença nas teorias da conspiração, os seus potenciais prejuízos e como devemos reagir a elas. Defendo que devemos avaliar as consequências da crença em uma teoria da conspiração para determinar se ela deve ser levada a serio ou não. Em bloco, as teorias da conspiração ameaçam a capacidade coletiva de produção de conhecimento e devemos nos preocupar com a sua difusão.

In the Southern Brazil ShelfSouthern Brazil Shelf (SBS), surface bioclastic concentrationsBioclastic concentrations are associated with putative paleo-shorelines formed where wave ravinement surfaces are probably present. From the late Last Glacial Maximum, the SBS can be considered a sediment-starved passive margin continental shelf, with its morphostructural development fairly known. There, fourteen molluscan shell samples from near shelf-break deposits (“distal shell-rich”), eleven from proximal, low depth bioclastic deposits (“proximal shell-rich”) and ten samples from sandy substrate (“shell-poor”) were evaluated for taphonomic damage accordingly to updated protocols. Multivariate statistical analysis showed significant differences between the three groups of shelly samples. Low-intensity damage states (such as natural bright and ornamentation) dominate samples from the distal shell-rich deposit, whereas the inverse occurs in the proximal deposit (samples from the shell-poor locations present an intermediate damage pattern). This pattern is consistent either with onlap/toplap and backlap shell bedShell bed formation, according to characteristics determined in the literature. The condition of these three areas may reflect degrees of exposure at the taphonomically-active zone, the magnitude of time averagingTime-averaging and duration of shell accumulation, and even the lack of shelf accommodation space, which in turn is related to glacioeustatic sea-level oscillations.