Dante Cicchetti’s remarkable contributions to the field of developmental psychopathology include the advancement of key principles such as the interplay of typical and atypical development, multifinality and equifinality, the dynamic processes of resilience, and the integration of multiple levels of analysis into developmental theories. In this paper we assert that person-centered data analytic methods are particularly well-suited to advancing these tenets of developmental psychopathology. We illustrate their utility with a brief novel empirical study focused on underlying patterns of childhood neuroendocrine regulation and prospective links with emerging adult functioning. Results indicate that a childhood neuroendocrine profile marked by high diurnal cortisol paired with low diurnal DHEA was uniquely associated with more adaptive functioning in emerging adulthood. We discuss these findings, and person-centered methods more broadly, within the future of developmental psychopathology.

Pedro Alvares Cabral's ships left Portugal on 9 March 1500 en route for the territory that he first named Terra de Vera Cruz and that later came to be known as Brazil. On the 22 March they called at the island of São Nicolau [Caminha, 1500], one of the northernmost islands of the Cape Verde group; this was about forty years after the discovery of the archipelago in 1460-62 [Albuquerque, 1991]. It is known that Vasco da Gama had stopped at the island of Santiago in 1498 on his voyage to India, and also in 1499 on the return journey. Straight after the discovery of Brazil Cabral sailed for India and on the way back also dropped anchor at Santiago. Indeed, our archipelago, which is situated off Cape Verde in Senegal (the place from which it appears to take its name), was to become an important stopover point for maritime traffic between Europe, Asia and the Americas in the fifteenth and sixteenth centuries, both to allow crews to rest and to take on water, wood and some food supplies. It also became important as a holding point for slaves (a large number of whom came from around thirty Guinean ethnic groups and subgroups). They were dispatched from Santiago, known then as Cape Verde island, to territories such as Brazil from the early sixteenth century onwards, since these territories, which had only recently been discovered and were little known, needed people to work and populate them.

Sozaboy's language is what I call "rotten English," a mixture of Nigerian pidgin English, broken English and occasional flashes of good, even idiomatic English. This language is disordered and disorderly. Born of a mediocre education and severely limited opportunities, it borrows words, patterns and images freely from the mother-tongue and finds expressions in a very limited English vocabulary. To its speakers, it has the advantage of having no rules and no syntax. It thrives on lawlessness, and is part of the dislocated and discordant society in which Sozaboy must live, move and have not his being. (K. S.-W.)

The mode of growth of authigenic, lath-shaped illitic particles has been investigated using field emission scanning electron microscopy (FESEM) and high resolution transmission electron microscopy (HRTEM). Two types of clay lath have been identified: overgrowths on platelets of illite or illite-smectite and discrete particles. Both are neoformed and show a slight increase in abundance with depth over the 70 m depth interval sampled. Interpretation of lattice fringe data is not unambiguous but indicates that the clay is either illite or illite-smectite with R1 structure. The formation of discrete particles of authigenic illite, or even R1 illite-smectite, is compatible with present burial depths and a regional geothermal gradient of approximately 40°C/km. This illite also differs from many previous reported occurrences of authigenic illite in mudrocks in that it appears to have formed, without being preceded by progressive illitization of illite-smectite.

How define tolerance? Tolerance consists in abstaining from intervening in the actions and opinions of other persons when these opinions or actions appear disagreeable, frankly unpleasant or morally reprehensible to us. But each will feel that there exists a real difference between that which is disagreeable or unpleasant and that which is morally repugnant. To respect this intuition, I would propose to distinguish between a narrow sense of tolerance - I tolerate that which appears displeasing or disagreeable to me, but I do not tolerate that which I judge to be morally wrong - and a broad sense in which I tolerate even that which I disapprove of morally. If we adopt the narrow sense, we have at our disposal a first answer to the question of knowing how far to tolerate: I tolerate that which relates to displeasure or to annoyance, but not that which I believe to be wrong.

Additional well-crystallized kaolin from Washington County, Georgia, has been supplied to the Clay Minerals Society Source Clay Repository to replace the exhausted supply of KGa-1. This kaolin is called KGa-1B and is from a geographic location and stratigraphic position close to where KGa-1 was collected. Slight mineralogical and chemical differences are observed between KGa-1 and KGa-1B. KGa-1B crude appears slightly better crystalline than KGa-1, and it has a slightly higher titania content than KGa-1. The Al2O3, SiO2, Fe2O3, alkali, and alkaline earth contents appear similar for both samples. KGa-1 has a slightly coarser particle size than KGa-1B crude. More intensive post-depositional alteration may have cleansed and crystallized the KGa-1B material to a slightly greater degree than the KGa-1 material.

Self-diffusion coefficients of H2O molecules in Na-rich hectorite gel were measured by 'H nuclear magnetic resonance (NMR), Spin-echo pulse sequences with magnetic field gradient pulses for the translational diffusion measurement were applied to the hectorite gel at the Larmor frequency of 20 MHz. Effects of clay fraction (0-51.2 wt. %) and temperature (20.0-60.3°C) were studied. The results show: (1) Phenomenologically, the self-diffusion coefficient, D, of 1H2O in the clay gel is expressed by the normalized diffusivity, D/D0 = exp(−0.0257w), where D0 is the water self-diffusivity in bulk water at temperature and w is the weight fraction of the hectorite (wt. %). (2) The activation energy of H2O diffusivity in the hectorite gel is nearly equal to that in bulk water. Hence, the normalized diffusivity, D/D0, obeys a temperature-independent curve. (3) The exponential dependence of D/D0 on w for w <30 wt. % is explained by a random-walk model, in which free or unbound H2O molecules migrate in the geometrically complex and tortuous pore structure of randomly scattered clay-mineral grains.

Weathering of spodumene in a lateritized pegmatite in Western Australia was studied by investigating in situ samples by electron-beam techniques. The spodumene had mostly altered to smectite. However, some non-crystalline material adjacent to smectite and intermixed with smectite was also observed. No crystallographic orientation between spodumene and smectite was observed by high resolution techniques. The spodumene dissolved to produce etch pits similar to those observed on hornblende grains. The etch pits were almost completely filled with smectite. Most of the Li in the spodumene was lost during its weathering to smectite.

The Chinese are probably the most particular people in the world when it comes to their names. As the Chinese proverb says, “worse than being born under a bad star is to receive a bad name.” For this reason it is difficult, if not impossible, to evaluate the role of name signs in China without a certain knowledge of the Chinese tradition regarding the attribution of names. A legal Chinese name is made up of a family name, monosyllabic with some exceptions, followed by a monosyllabic or disyllabic first name. Theoretically, the 50,000 characters that make up the Chinese lexicon are potential choices for the composition of a first name. Due to the great number of homophones included in the Chinese language, it is difficult to identify the graphic form of a Chinese name by its pronunciation alone. Hence the custom of specifying the characters by writing them in the air or by indicating their signification, or even by simply presenting a calling card.

Does Seoul, a city of eight million inhabitants, one of the planet's ten megalopolises, still have shamans? Can there be a place for shamanism in a country like South Korea, which is striving to be modern? Can shamanism survive at all in a country where the successes of Christianity have been celebrated by Westerners? Can it adapt itself to religious pluralism? What is shamanism's role in the urban setting? How does the fast pace of urban life affect its rituals? How is shamanism presented in the mass media? Is it beginning to emerge from the centuries-long ostracism imposed on it by official ideologies?

These questions will be explored in this article on the basis of data gathered on-site in the city of Seoul between the years 1982 and 1991. We will attempt not only to highlight several important facts but to grasp the overall process of transformation that the city is imposing on shamans and shamanism.

A synthetic octahedral-site-vacancy-free annite sample and its progressive oxidation, induced by heating in air, were studied by powder X-ray diffraction (pXRD), Mössbauer spectroscopy, nuclear reaction analysis (NRA), Raman spectroscopy, X-ray fluorescence (XRF) spectroscopy, gas chromatography (GC), thermogravimetric analysis (TGA), differential thermal analysis (DTA), scanning electron microscopy (SEM), and size-fraction separation methods. For a set heating time and as temperature is increased, the sample first evolves along an annite-oxyannite join, until all H is lost via the oxybiotite reaction (Fe2+ + OH− ⇌ Fe3+ + O2− + H↑). It then evolves along an oxyannite-ferrioxyannite join, where ideal ferrioxyannite, KFe3+8/3□1/3AlSi3O12, is defined as the product resulting from complete oxidation of ideal oxyannite, KFe3+2Fe2+AlSi3O12, via the vacancy mechanism (3 Fe2+ ⇌ 2 Fe3+ + [6]□ + Fe↑). A pillaring collapse transition is observed as a collapse of c near the point where ${\text{Fe}}^{2+}\text{/Fe}=\raisebox{1ex}{$1$}\!\left/ \!\raisebox{-1ex}{$3$}\right.$ and all OH groups are predicted and observed to be lost. Quantitative analyses of H, using NRA, GC, and Raman spectroscopy, corroborate this interpretation and, in combination with accurate ferric/ferrous ratios from Mössbauer spectroscopy and lattice parameter determinations, allow a clear distinction to be made between vacancy-free and vacancy-bearing annite. The amount of Fe in ancillary Fe oxide phases produced by the vacancy mechanism is measured by Mössbauer spectroscopy to be 11.3(5)% of total Fe, in agreement with both the theoretical prediction of 1/9 = 11.1% and the observed TGA weight gain. The initiation of Fe oxide formation near the point of completion of the oxybiotite reaction (${\text{Fe}}^{2+}\text{/Fe}=\raisebox{1ex}{$1$}\!\left/ \!\raisebox{-1ex}{$3$}\right.$) is corroborated by pXRD, TGA, Raman spectroscopy, and appearance of an Fe oxide hyperfine field sextet in the Mössbauer spectra. The region of Fe oxide formation is shown to coincide with a region of octahedral site vacancy formation, using a new Mössbauer spectral signature of vacancies that consists of a component at 2.2 mm/s in the [6]Fe3+ quadrupole splitting distribution (QSD). The crystal chemical behaviors of annite-oxyannite and of oxyannite-ferrioxyannite are best contrasted and compared to the behaviors of other layer-silicate series in terms of b vs. [D] (average octahedral cation to O bond length). This also leads to a diagnostic test for the presence of octahedral site vacancies in hydrothermally synthesized annite, based on a graph of b vs. Fe2+/Fe. The implications of the observed sequence of thermal oxidation reactions for the thermodynamic relevance of the oxybiotite and vacancy reactions in hydrothermal syntheses are examined and it is concluded that the oxybiotite reaction is the relevant reaction in the single-phase stability field of annite, at high hydrogen fugacity and using ideal starting cation stoichiometry. The vacancy reaction is only relevant in a multi-phase field, at lower hydrogen fugacity, that includes an Fe oxide equilibrium phase (magnetite) that can effectively compete for Fe, or when using non-ideal starting cation stoichiometries.

Clay mineralogy and whole-rock chemistry of the borate-bearing layers of the Hisarcik and Esbey mines were examined. The Hisarcik clays occur as laminated or unlaminated clay layers with sharp contacts. Unlaminated layers contain quartz derived from metamorphic rocks and carbonate fragments in a clay matrix, and are interpreted as reworked tuffs deposited in playa-lake environments. An important feature is that the unlaminated clays contain little MgO (3–15 wt. %) as compared with the laminated clays (15–30 wt. %). As previous studies have shown, the clay fraction of the studied profile contains predominantly Li-bearing saponite, and accounts for 60–90 wt. % of the clay fraction (<2 μm). Illite in the clay fraction varies from 0 to 67 wt. % and the average illite percentage never exceeds 40 wt. %. Chlorite is scarce (2–5 wt. %). Illite-smectite interstratified clays (illite at 70%, smectite at 30%) were only found in low concentrations in the laminated clay layers of the upper limestone unit (above the borate zone), where illite-2M of detrital origin is also present. The Esbey clays occur interstratified with colemanite layers and envelope colemanite nodules. Calcite is the major mineral of the clays whereas quartz, plagioclase, feldspar, colemanite, and cahnite are minor components. The MgO contents vary between 4.70–13.95 wt. % in the clays interstratified with colemanite layers, between 7.24–11.89 wt. % in the enveloping clays, and between 10.27–21.25 wt. % in clays located above the colemanite zone. The composition of the clay fraction (<2 μm) in all samples is similar. Smectite represents between 40–90 wt. % of the clay fraction in the upper portion of the stratigraphic profile and decreases towards the lower part of the stratigraphic profile. Smectite always occurs with illite which may vary from 20 to 90 wt. % of the clay fraction, and a small amount of kaolinite and chlorite. Illite-2M polytype is abundant. The d(060)-reflection position suggests that the smectite minerals from the Hisarcik and Esbey colemanite mines contain both dioctahedral and trioctahedral smectites to form a transitional zone. These smectites are a product of a magnesium-rich alkaline playa-lake environment.

Harassment is often understood to be, in its paradigm form, overtly aggressive or hostile. But harassment can also occur in a more deceptive format, and can be presented as soft, neutral, innocent, or even friendly and caring. There is something fundamentally deceptive and dishonest about this kind of harassment. The overt friendliness makes these particular forms of harassment harder to spot, and therefore potentially more likely to succeed. I focus on one such instance of friendly-presenting harassment: sealioning. I argue that, despite its ostensive friendliness, sealioning is a form of harassment that has a twofold goal: there is the political goal of forestalling action, and the epistemic goal of undermining the victim's authority. I draw on Jose Medina's understanding of culpable ignorance and the existentialist notion of bad faith to flesh out the distinction between ill-willed and good-willed sealioning, and argue that the latter, despite the good will, is also harassment. I conclude by addressing the different responsibilities of the sea lion, the victim, and the onlooker. Narrowing in on these deceptive forms of harassment, I aim to contribute to the hermeneutic justice of being able to spot and name harassment as it happens.

Three different models have been reported previously to describe the kinetics of the transformation of smectite to illite (Pytte 1982; Velde and Vasseur 1992; Huang et al. 1993). In order to evaluate the general utility of these models to calculate the timing and extent of this transformation, each model was applied to four different geologic settings (Denver Basin, Gulf Coast, the Salton Sea Geothermal System, and Paris Basin) in which the ages, geothermal gradients and potassium ion activities vary markedly. The model results are compared to the measured percentages of illite in illite/smectite (I/S) and the K/Ar ages of I/S (if available) to test the utility of a given model to a particular basin.

Although individual models can be applied to study this transformation within a specific setting, none of these models was successful in simulating the transformation for all four basins. The Salton Sea was simulated best using the model by Huang et al. (1993), which incorporated an increased geothermal gradient during the last 20,000 years. These results indicate that a large fraction of illite formed due to this increased geothermal gradient, and underscores that temperature is a dominant kinetic factor in forming illite. The Denver Basin was simulated well by the models of Velde and Vasseur (1992) and Pytte (1982). The Gulf Coast was simulated very well by the model of Huang et al. (1993) using a term that terminates the transformation at 75% illite. For the Paris Basin, the results are mixed. The models can be refined by comparing the calculated and measured ages of illite such as the K/Ar ages of I/S to understand the thermal history of a particular basin. The calculated ages of illitization derived from these refined models can be used to indicate the time at which source rocks became thermally mature to form oil and gas.

Studies show that war leads to an increase in harsh parenting and a decrease in parental warmth, which in turn has a devastating impact on children’s development. However, there is insufficient research on the factors that affect parenting in post-conflict regions. In addition, most previous studies on the role of parenting in the context of war rely on self-reports, which are subject to a number of limitations. To complement existing research, the present cross-sectional study used behavioral observations of 101 mothers and their 6–12 year old children to assess parenting in post-conflict northern Uganda. The aim of the current study was to explore associations between observed maternal warmth and coercion and self-reported socioeconomic status (e.g., mother’s educational level) as well as maternal (e.g., posttraumatic stress disorder), child (e.g., externalizing problems), and social contextual factors (e.g., family violence). Results show a link between observed parenting, child characteristics, and family violence. Higher levels of children’s externalizing problems were associated with more severe maternal coercion. In addition, a negative association was found between family violence and maternal warmth. Findings are discussed in terms of their implications for prevention and intervention programs and the use of behavioral observations in post-conflict environments.

The nature and number of acid sites per unit weight on a series of materials obtained by interaction of a montmorillonite with zirconium or cerium hydrogenphosphates precipitated in situ by reaction between their precursors have been investigated.

The quantitative determination of the surface acidity has been carried out by three different methods: titration with triethanolamine in aqueous media; TG analysis of the samples after n-butylamine treatment and vacuum desorption; and chemisorption of NH3 at 239.8 K. Additional information about the nature of the surface acid sites has been obtained from the IR spectra of the samples with bases adsorbed.

Results show that the acid site density on the montmorillonite-cerium or zirconium phosphate cross-linked compounds is greater than on the parent montmorillonite and increases as the content in tetravalent metal phosphate rises throughout the different series. Also the number of acid sites for the cerium phosphate-montmorillonite materials is lower than for zirconium ones and the characteristics obtained depend on the bases used for their evaluation.

The presence of two IR adsorption bands at 1400 and 3145 cm−1, assigned to the NH4+ ion, and the absence of the 1170–1361 cm−1 bands, characteristic of the NH3 adsorbed on a Lewis site, strongly suggest the Brönsted character of the acidity of these compounds.