Dental anomalies in Richieri-Costa-Pereira syndrome

Objective. The objective of this study was to investigate the prevalence of dental anomalies in individuals with Richieri-Costa-Pereira syndrome. Study Design. A total of 13 individuals with Richieri-Costa-Pereira syndrome who were older than 8 years with at least 1 available panoramic radiograph were assessed. Dental anomalies were evaluated clinically and radiographically and classified as hyperplastic, hypoplastic, or heterotopic and as alterations of shape, number, position, and structure. Enamel alterations were classified by the DDE index. Results. All individuals exhibited anomalies, with predominance of hypoplastic disorders, mainly agenesis of mandibular incisors and second premolars and demarcated creamy-white enamel opacities primarily affecting the maxillary premolars. Conclusions. Individuals with Richieri-Costa Pereira syndrome exhibit high prevalence of tooth agenesis, especially mandibular incisors and premolars, as well as high frequency of enamel opacities. These findings are compatible with the mandibular cleft observed in all individuals and also reflect the hypoplastic characteristic of the syndrome. (Oral Surg Oral Med Oral Pathol Oral Radiol 2012;114:99-106)

Laryngeal malformation in Richieri-Costa Pereira syndrome: New findings

Laryngeal structural anomalies were described in 13 cases of Richieri-Costa Pereira syndrome, and four previously reported cases were reviewed. The 17 individuals examined had the typical laryngeal anomalies and vocal disorders previously described. The new findings are the laryngeal microweb observed in three cases and arytenoid anteriorization movement observed in 14 cases. (C) 2012 Wiley Periodicals, Inc.

Differences in habitat use of two sympatric species of Ameiva in East Costa Rica

Identifying the differences in habitat use for sympatric species is important for understanding the species preferences and the limits of population distribution. We studied the differences in the habitat use of two understudied sympatric species of Ameiva (A. festiva and A. quadrilineata) in a natural reserve of the Caribbean coast of Coast Rica. Ameiva quadrilineata showed a more restrictive habitat use pattern than A. festiva. A. quadrilineata's smaller body size may be one of the factors limiting its habitat range. Both species showed higher density in regenerated forests, while A. quadrilineata was never found in swamp forests. The air temperature and the meteorological condition at the moment of the survey also influenced the occurrence of the A. quadrilineata, while the juveniles of A. festiva were only affected by the meteorological condition. None of the studied variables seemed to affect the occurrence of A. festiva adults. The results of this study can be useful to evaluate possible changes in the species distribution patterns as a consequence of direct (i.e., deforestation) or indirect (i.e., climate change) human activities in the distribution area of these species.

Jupoata (Coleoptera, Cerambycidae, Cerambycinae): nova espécie da Costa Rica e chave para identificação das espécies

Jupoata brenesi é descrita da Costa Rica, figurada e incluída em chave para as espécies do gênero.

Novos táxons e notas sobre Cerambycidae (Coleoptera) da Costa Rica

Nova espécie descrita: Eupogonius intonsus sp. nov. de Guanacaste. Nova subespécie descrita: Eburia lanigera costaricensis subsp. nov. de Guanacaste. Novos registros: Cymatonycha meridionalis Martins & Galileo, 1995 (Puntarenas) e Nesozineus triviale Galileo & Martins, 1996 (Guanacaste). É comentada a variabilidade no colorido elitral de Eburodacrys havanensis Chevrolat, 1862.

Metabólitos secundários dos nudibrânquios Tambja stegosauriformis, Hypselodoris lajensis e Okenia zoobotryon e dos briozoários Zoobotryon verticillatum e Bugula dentata da costa do Brasil

The chemical investigation of the MeOH extract from the bryozoan B. dentata MeOH yielded tambjamines A (1), C (3), D (4), K (6), aldehyde 8 and the new tambjamine J1(9), while the extract of its predator, the nudibranch Tambja stegosauriformis, yielded tambjamines C and K, along with aldehyde 8. Furodisinin lactone (11) was isolated from the nudibranch Hypselodoris lajensis, a compound previously isolated from Dysidea sponges. The alkaloid 2,5,6-tribromo-N-methylgramine (12) was isolated from the nudibranch Okenia zoobotryon and from its prey, the bryozoan Zoobotryon verticillatum, the only source of 12 previously known.

Los manglares de la costa brasileña: revision preliminar de la literatura

Los manglares ocurren intermitentemente a lo largo del litoral brasileño desde Cabo Orange (4°21'N) en Amapá hasta la ciudad de Laguna (28°30'S). En este trabajo se sugiere la división del litoral en 7 trechos que comparten características geomorfológicas y rangos de condiciones meteorológicas similares. Estes trechos son: Litoral Guianense, Golfão Amazónico, Litoral de Ponta Coruçá a Ponta Mangues Secos, Litoral de Ponta Mangues Secos al Cabo Calcanhar, Litoral del Cabo Calcanhar al Recôncavo Baiano, Litoral Oriental y Costa Cristalina. El mayor desarrollo del manglar ocurre en los trechos Guianense y del Gofão Amazónico. Los manglares se desarrollhan por todo el litoral aún en los sectores donde la precipitación es en el orden de 500 mm/año. En las costas expuestas se desarrolla en las áreas anegadas detrás de medanos, canales, lagunas y márgenes de los estuarios, penetrando en ocasiones 30-40 km. Coloniza además las márgenes de las grandes bahías hasta los 28°30'S donde la temperatura anual es de 19.6°C y la temperatura media del mes más frío es de 15.7°C. En el trecho del Litoral Cristalino, el manglar alcanza su límite latitudinal en el estado de Santa Catarina. Rhizophora alcanza 27°53'S mientras que Avicennia continúa hasta los 28°30'S en Laguna. En la isla de Santa Catarina se encuentran manglares bien desarrollados dominados por Avicennia. Estos manglares alcanzan un porte promedio de 7.0 ± 0.4 m, tienen un DAP de 17.9 cm, densidades totales (≥ 2.5 cm) de 431 ± 93 árboles/ha y áreas basimétricas (≥ 2.5 cm) de 7.42 ± 0.80 m2/ha. Las áreas basimétricas bajas se deben al dominio de los rodales por pocos ejemplares de diámetros moderados. Debido a estas bajas densidades, la copa es rala y los bosques son extremadamente abiertos

Evolução da linha de costa e morfologia atual do Delta do Valo Grande, Litoral Sudeste do Brasil

O sistema estuarino‐lagunar de Cananéia‐Iguape, localizado no sul do Estado de São Paulo, sudeste do Brasil, encerra um complexo de canais, associados a uma planície costeira, cuja evolução data dos eventos transgressivo‐regressivos do Quaternário superior e cujos processos sedimentares recentes foram dramaticamente alterados em função da atividade antrópica, nos últimos 150 anos, determinada, basicamente, pela abertura de um canal artificial, o Valo Grande. Uma análise de documentos cartográficos, dos últimos 100 anos (Commissão Geographica e Geologica do Estado de S. Paulo, 1914; Freitas, 2005; Nascimento Jr et al., 2008), além de imagens de satélites, revela que, após a abertura do Valo Grande, houve uma enorme intensificação no processo sedimentar de parte do sistema lagunar, em função, não somente da erosão das margens do canal artificial mas, também, por conta do aumento expressivo sedimentos para o sistema estuarino‐lagunar, levando à formação de um “delta intra‐lagunar antropogênico” (“man‐made intra‐lagoonal delta”) cuja evolução e morfologia atual estão sendo investigados.