A nutritional intervention study with hydrolyzed collagen in pre-pubertal Spanish children: influence on bone modeling biomarkers

Aim: The aim of the study was to investigate the influence of dietary intake of commercial hydrolyzed collagen (Gelatine Royal ®) on bone remodeling in pre-pubertal children. Methods: A randomized double-blind study was carried out in 60 children (9.42 ± 1.31 years) divided into three groups according to the amount of partially hydrolyzed collagen taken daily for 4 months: placebo (G-I, n = 18), collagen (G-II, n = 20) and collagen + calcium (G-III, n = 22) groups. Analyses of the following biochemical markers were carried out: total and bone alkaline phosphatase (tALP and bALP), osteocalcin, tartrate-resistant acid phosphatase (TRAP), type I collagen carboxy terminal telopeptide, lipids, calcium, 25-hydroxyvitamin D, insulin-like growth factor 1 (IGF-1), thyroid-stimulating hormone, free thyroxin and intact parathormone. Results: There was a significantly greater increase in serum IGF-1 in G-III than in G II (p < 0.01) or G-I (p < 0.05) during the study period, and a significantly greater increase in plasma tALP in G-III than in G-I (p < 0.05). Serum bALP behavior significantly (p < 0.05) differed between G-II (increase) and G-I (decrease). Plasma TRAP behavior significantly differed between G-II and G-I (p < 0.01) and between G-III and G-II (p < 0.05). Conclusion: Daily dietary intake of hydrolyzed collagen seems to have a potential role in enhancing bone remodeling at key stages of growth and development.

Cholinergic regulation of bone.

Bone remodeling is regulated by the two branches of the autonomic nervous system: the adrenergic and the cholinergic branches. Adrenergic activity favors bone loss, whereas cholinergic activity has been recently shown to favor bone mass accrual. In vitro studies have reported that cholinergic activity induces proliferation and differentiation of bone cells. In vivo studies have shown that the inhibition of cholinergic activity favors bone loss, whereas its stimulation favors bone mass accrual. Clinical studies have shown that bone density is associated with the function of many cholinergic-regulated tissues such as the hypothalamus, salivary glands, lacrimal glands and langerhans cells, suggesting a common mechanism of control. Altogether, these observations and linked findings are of great significance since they improve our understanding of bone physiology. These discoveries have been successfully used recently to investigate new promising therapies for bone diseases based on cholinergic stimulation. Here, we review the current understanding of the cholinergic activity and its association with bone health.

The Fresh Frozen Bone Allograft (FFBA) to reconstruc the atrophic maxilla: evaluation of the clinical and histological viability at six and nine months in the maxillary sinus

This work aimed to analyze clinically and histologically the allogen bone graft behavior at 6 and 9 months. A leukoderm, female, 55 years old patient sought dental care for oral rehabilitation with dental implants and implant supported fixed prosthesis in the maxilla. Bilateral sinus lifting procedure were performed in a same patient, the analysis were made after 6 and 9 months, respectively. At 6 months, there was lack of a better bone remodeling in the region, associated to the presence of fibrous connective tissue within the collected tissue, showing us that this is not the best stage of tissue maturation to place dental implants. The 9 months period showed an improvement, with a more organized bone tissue surrounding particles of homogenous bone, what possibly had increased implant stability at the time of surgery. There is no doubt about the increase of clinical applications of FFBA, but there are no studies available regarding the standardization of time to load implants inserted in allografts. So papers with long-term monitoring are necessary to eliminate questions that still remain to be answered.

Implantes tipo plataforma modificada: revisión de literatura

The purpose of this revision was to explore the concept of Platform Switching in implantology and its acting in the clinical practice. The concept of platform switching will be considered together with a revision of pertinent literature, with the purpose of providing guidelines based on scientific evidences. The following databases were used: Pubmed, Library Cochrane and ISI in the last 17 years. The inclusion approaches were: clinical articles, laboratorials and of revision on the topic, in English language. 41 articles were selected, using the describers "platform switching dental implants", "platform shifting and dental implants", "expanded platform dental implant". In accordance with this revision, implant them platform switching they present a rate of more favorable bony remodeling that you implant them conventional. This fact seems to be resulting of a group of biological factors and mechanics. The concept of platform switching has important relevance in the aesthetic area.

Presentación [del libro "Simulación del comportamiento óseo. Aplicación al diseño de implantes"]

La aplicación de los fundamentos, métodos y herramientas básicas de la Mecánica del Daño Continuo a un modelo de comportamiento biológico como es la remodelación ósea supone un mutuo enriquecimiento y las posibilidades de generalización o ampliación de las disciplinas involucradas. Así surge la idea de reparación que, termodinámicamente sería imposible en un sistema mecánico puro aislado pero que aparece como conveniente y posible en un sistema simulado como mecánico pero en realidad acoplado y, por tanto, con entradas energéticas adicionales como es la energía metabólica en este caso. El grupo que dirige el profesor Doblaré, a quien tuve la oportunidad de facilitar sus primeros pasos en la investigación, tesis doctoral incluída, es conocido en el ámbito de la Mecánica Computacional donde ha venido trabajando en distintos campos desde fundamentos de los Métodos Numéricos hasta aplicaciones en la dinámica, fractura y fatiga, optimización estructural y, últimamente la Biomecánica. Por ello es para mí una doble satisfacción presentar este informe a la Academia de Ingeniería ya que a la difusión de la investigación en un área de enorme futuro en la que muchos de nuestros grupos actuales de investigación se verán inmersos en los próximos años, se une la confirmación de las esperanzas puestas en la inteligencia y capacidad de trabajo de una joven promesa hoy brillante realidad.

Aplicación exitosa de PRP y parches de fibrina en un caso clínico de un equino deportivo

Resumen Los equinos deportivos, son víctimas de frecuentes heridas en la región distal de los miembros y de fracturas articulares. La medicina regenerativa es un campo emergente el cual utiliza métodos alternativos para diferentes lesiones de difícil resolución con tratamiento convencional. Existen antecedentes que utilizan parches de fibrina (PF) en la reparación de heridas cutáneas y plasma rico en plaquetas (PRP) en lesiones osteoarticulares. Este trabajo tuvo por objetivo evaluar la aplicación de PRP sobre una fractura de tercer carpiano del miembro anterior derecho y la aplicación de PF en una herida de 54 cm² en la región metatarsiana del miembro posterior izquierdo de un equino Sangre Pura de Carrera (SPC). Se realizó una única aplicación PRP mediante artrocentesis intercarpiana. Sobre la herida cutánea, se realizaron 3 aplicaciones (1 por semana) de PF. Un mes post-aplicación de PRP el equino ya no evidenciaba claudicación, no manifestaba dolor ni inflamación articular y no rechazaba el apoyo. A nivel radiográfico, se observó consolidación de la línea de fractura, con remodelación ósea. A su vez, luego de la tercera aplicación de PF (3 semanas), la superficie de la herida se redujo dos tercios del tamaño original y a las 8 semanas se logró su completa resolución

Remodelación del patio.

Las Unidades de Evaluación se presentan como alternativa a las pruebas de rendimiento o exámenes. Una Unidad de Evaluación tiene tres partes esenciales: el escenario, las tareas y los inventarios de corrección. El 'escenario' es el estímulo, la situación significativa del contexto que se utiliza para movilizar los conocimientos; se utiliza un formato verbal (texto escrito) y otro no verbal (imágenes, tablas, gráficos, cuadros, etc.) que se extraen de cualquier fuente documental. Las 'tareas' permiten conocer, mediante la movilización de los conocimientos, cuál es la competencia alcanzada en el uso de procesos cognitivos, afectivos, sociales y funcionales, y el nivel de logro de los aprendizajes. Para que la información contenida sea completa (saber, hacer y querer) la Unidad de Evaluación debe incluir tareas que valoren aprendizajes receptivos, productivos y valorativos. El proceso de evaluación concluye con la corrección de tareas, realizada por el propio alumno o por el profesorado. Con carácter general, las tareas utilizadas en las Unidades de Evaluación se definen con diferentes formatos de respuesta y criterios de corrección. Esta Unidad de Evaluación se presenta como un modelo de evaluación competencial, en ningún caso pretende ser algo más que una ejemplificación que estimule la creación de materiales para la evaluación de las competencias básicas de los propios docentes. Elaborada por la Oficina de Evaluación de la Junta de Comunidades de Castilla-La Mancha para su aplicación en las pruebas de acceso a los Ciclos Formativos de Grado Medio en la convocatoria de junio de 2009

Residuos motivados por obra de remodelación interior en distintas tipologías de vivienda.

El medio ambiente es cada vez, un tema de más actualidad. Un tema que ya está preocupando, incluso a los que antes no le daban importancia. En nuestro ámbito, el de la construcción, este tema también se plantea, ya que en nuestra actividad cotidiana nos encontramos con residuos de construcción, tanto durante el proceso edificatorio en sí mismo, como a posteriori, en demolición, bien sea total o parcial, rehabilitación o reforma. Nos topamos con residuos y no sabemos qué hacer con ellos, surgen varias preguntas: ¿Cómo los tratamos? ¿Los reciclamos? ¿Qué fin se le pueden dar? ¿O directamente van a vertedero o a incinerar? Quería estudiar este tema, pero a la vez quería que no fuese solo teórico sino que lo combinara con algo real, algo que en nuestra profesión sea habitual, entonces me planteo la siguiente pregunta: ¿Qué tipo, material y cantidad de residuos de construcción sacaríamos si aplicáramos unas reformas a distintas viviendas, según su programa de necesidades? Y básicamente, este estudio es la respuesta a dicha pregunta. Junto a los tutores, hemos elegido tres tipologías diferentes de vivienda, todas ellas ya construidas y existentes actualmente. Y después de un estudio de necesidades (bien sea sobre accesibilidad, conciliación de la vida familiar y profesional, movilidad, estética o nuevas tendencias...) según las características de dichas viviendas y de sus usuarios; se le han aplicado una supuesta reforma, obteniendo así unos datos, una información de residuos de construcción y demolición (RCDs) reales, que nos pueden tocar a cualquiera en nuestra labor profesional diaria. Y a partir de ellos, estudiamos la clasificación, el fin, el tratamiento etc. de estos.

The River And The Sea: Fieldwork In Human Ecology And Ethnobiology.

This article is a commentary on the experiences that motivated my decision to become a human ecologist and ethnobiologist. These experiences include the pleasure of studying and of having the sense of being within nature, as well as the curiosity towards understanding the world and minds of local people. In particular, such understanding could be driven by addressing the challenging questions that originate in the interactions of such individuals with their natural surroundings. I have been particularly interested in the sea and the riverine forests that are inhabited by coastal or riverine small-scale fishers. Sharing the distinctive world of these fishers enjoyably incited my curiosity and challenged me to understand why fishers and their families 'do as they do' for their livelihoods including their beliefs. This challenge involved understanding the rationality (or the arguments or views) that underlies the decisions these individuals make in their interaction with nature. This curiosity was fundamental to my career choice, as were a number of reading interests. These reading interests included political economy and philosophy; evolution and sociobiology; evolutionary, human, and cultural ecology; cultural transmission; fisheries; local knowledge; ecological economics; and, naturally, ethnobiology.

Embryonic, Larval, and Juvenile Development of the Sea Biscuit Clypeaster subdepressus (Echinodermata: Clypeasteroida)

Sea biscuits and sand dollars diverged from other irregular echinoids approximately 55 million years ago and rapidly dispersed to oceans worldwide. A series of morphological changes were associated with the occupation of sand beds such as flattening of the body, shortening of primary spines, multiplication of podia, and retention of the lantern of Aristotle into adulthood. To investigate the developmental basis of such morphological changes we documented the ontogeny of Clypeaster subdepressus. We obtained gametes from adult specimens by KCl injection and raised the embryos at 26 degrees C. Ciliated blastulae hatched 7.5 h after sperm entry. During gastrulation the archenteron elongated continuously while ectodermal red-pigmented cells migrated synchronously to the apical plate. Pluteus larvae began to feed in 3 d and were similar to 20 d old at metamorphosis; starved larvae died 17 d after fertilization. Postlarval juveniles had neither mouth nor anus nor plates on the aboral side, except for the remnants of larval spicules, but their bilateral symmetry became evident after the resorption of larval tissues. Ossicles of the lantern were present and organized in 5 groups. Each group had 1 tooth, 2 demipyramids, and 2 epiphyses with a rotula in between. Early appendages consisted of 15 spines, 15 podia (2 types), and 5 sphaeridia. Podial types were distributed in accordance to Loven's rule and the first podium of each ambulacrum was not encircled by the skeleton. Seven days after metamorphosis juveniles began to feed by rasping sand grains with the lantern. Juveniles survived in laboratory cultures for similar to 9 months and died with <500 mu m wide, a single open sphaeridium per ambulacrum, aboral anus, and no differentiated food grooves or petaloids. Tracking the morphogenesis of early juveniles is a necessary step to elucidate the developmental mechanisms of echinoid growth and important groundwork to clarify homologies between irregular urchins.

From Offshore to Onshore: Multiple Origins of Shallow-Water Corals from Deep-Sea Ancestors

Shallow-water tropical reefs and the deep sea represent the two most diverse marine environments. Understanding the origin and diversification of this biodiversity is a major quest in ecology and evolution. The most prominent and well-supported explanation, articulated since the first explorations of the deep sea, holds that benthic marine fauna originated in shallow, onshore environments, and diversified into deeper waters. In contrast, evidence that groups of marine organisms originated in the deep sea is limited, and the possibility that deep-water taxa have contributed to the formation of shallow-water communities remains untested with phylogenetic methods. Here we show that stylasterid corals (Cnidaria: Hydrozoa: Stylasteridae)-the second most diverse group of hard corals-originated and diversified extensively in the deep sea, and subsequently invaded shallow waters. Our phylogenetic results show that deep-water stylasterid corals have invaded the shallow-water tropics three times, with one additional invasion of the shallow-water temperate zone. Our results also show that anti-predatory innovations arose in the deep sea, but were not involved in the shallow-water invasions. These findings are the first robust evidence that an important group of tropical shallow-water marine animals evolved from deep-water ancestors.

Facies, delta(13)C, delta(15)N and C/N analyses in a late Quaternary compound estuarine fill, northern Brazil and relation to sea level

The present work integrates sedimentary facies, (14)C dating, delta(13)C, delta(15)N, and C/N with geologic and geomorphologic data available from literature. The aim was to characterize the depositional settings of a late Quaternary estuary in northeastern Marajo Island and analyze its evolution within the context of relative sea level fluctuations. The data derive from four continuous cores along a proximal-to-distal transect of a paleoestuary, previously recognized using remote sensing information. Fifteen sediment samples recorded ages ranging from 42,580 +/- 1430 to 3184 +/- 37 (14)C yr B.P. Fades analysis indicated fine- to coarse-grained sands with parallel lamination or cross stratification, massive or laminated muds and heterolithic deposits. delta(13)C (-28.1 parts per thousand to -19.7 parts per thousand, mean = -23.0 parts per thousand), delta(15)N (+ 14.8 parts per thousand to + 4.7 parts per thousand, mean = + 9.2 parts per thousand) and C/N (14.5 to 1.5, mean = 7.9) indicate mostly marine and freshwater phytoplankton sources for the organic matter. The results confirm a large late Quaternary paleoestuary in northeastern Marajo Island. The distribution of delta(13)C, delta(15)N, and C/N, together with fades associations, led to identify depositional settings related to fluvial channel, floodplain, tidal channel/tidal flat, central basin, tidal delta, and tidal inlet/sand barrier. These deposits are consistent with a wave-dominated estuary. Variations in stratigraphy and geochemistry are controlled by changes in relative sea level, revealing a main transgression from an undetermined time around 42,000 (14)C yr B.P. and 29,340 (+/- 200) (14)C yr B.P., which is synchronous to the overall drop in sea level after the last interglacial. Following this period, and probably until 9110 +/- 37 (14)C yr B.P., i.e., during a time interval encompassing two glacial episodes including the Last Glacial and the Younger Dryas, there was a pronounced drop in sea level, recorded by the development of a major erosional discontinuity due to valley re-incision. Sea level rose again until 5464 +/- 40 (14)C yr B.P, just before the main worldwide mid-Holocene transgressive peak. Mid to late Holocene coastal progradation ended the Marajo paleoestuarine history, and promoted the establishment of continental conditions throughout the island. The divergence comparing the Marajo sea level behavior with the eustatic curve allows hypothesizing that post-rifting tectonics along the Brazilian Equatorial margin influenced the sedimentary evolution of the studied paleoestuary. Considering that sedimentary facies in estuarine settings are highly variable both laterally and vertically, the present integration of facies with isotope and elemental analyses was crucial to provide a more precise interpretation of the Late Pleistocene and Holocene Marajo paleoestuary, and analyze its sea level history within the eustatic and tectonic context. (C) 2010 Elsevier B.V. All rights reserved.

Quaternary paleoenvironments and relative sea-level changes in Marajo Island (Northern Brazil): Facies, delta(13)C, delta(15)N and C/N

The reconstruction of physical environments of Amazonian areas is of great interest to determine the dynamic evolution of the Amazon drainage basin. However. few studies have emphasized the Quaternary deposits in this region. which is mostly due to the lack of natural exposures imposed by the low topography. This work integrates facies analysis. radiocarbon dating, delta(13)C, delta(15)N, and C/N of an 124 m-thick core from an area located at the mouth of the Amazon River. northeastern Amazonia. The study records deposits up to 50.795 (14)C yr B P. in age. which formed in a variety of depositional environments including fluvial channel, tidal flat, outer estuarine basin to shallow marine. inner estuarine basin, estuarine channel and lagoon. Facies interpretation was significantly improved with the inclusion of delta(13)C, delta(15)N, and C/N analyses of organic matter extracted from the sediments The obtained values conform to a transitional. mostly estuarine paleosetting evolved during successive relative sea-level fluctuations. The results suggest fluvial deposition between 40,950 (+/- 590) and 50.795 (14)C yr B P, with a rise in relative sea level that commenced between 35,567 (+/- 649) and 39,079 (+/- 1114) (14)C yr B P. An overall transgression took place until 29,340 (+/- 340) (14)C yr B P., after which the relative sea level dropped, favoring valley rejuvenation and incision. Following this time up to 10,479 (+/- 34) (14)C yr B.P. a rise in relative sea level filled up the valley with estuarine deposits After 10.479(+/- 34) (14)C yr B.P., the estuary was replaced by a lagoon At the end of the Holocene, the coastline prograided approximately 45 km northward, replaci ng the lagoon by a lake system Despite the influence of eustatic fluctuations. regional tectonics played a significant role to create new space where these Late Pleistocene and Holocene sediments accumulated. (C) 2009 Elsevier B V All rights reserved.

Middle Pleistocene sea surface temperature in the Brazil-Malvinas Confluence Zone: Paleoceanographic implications based on planktonic foraminifera

We reconstructed Middle Pleistocene surface hydrography in the western South Atlantic based on planktonic foraminiferal assemblages, modern analog technique and Globorotalia truncatulinoides isotopic ratios of core SP1251 (38 degrees 29.7`S / 53 degrees 40.7`W / 3400 m water depth). Biostratigraphic analysis suggests that sediments were deposited between 0.3 and 0.12 Ma and therefore correlate to Marine Isotopic Stage 6 or 8. Faunal assemblage-based winter and summer SST estimates suggest that the western South Atlantic at 38 degrees S was 4-6 degrees C colder than at present, within the expected range for a glacial interval. High relative abundances of subantarctic species, particularly the dominance of Neogloboquadrina pachyderma (left), support lower than present SSTs throughout the recorded period. The oxygen isotopic composition of G. truncatulinoides suggests a northward shift of the Brazil-Malvinas Confluence Zone and of the associated mid-latitude frontal system during this Middle Pleistocene cold period, and a stronger than present influence of superficial subantarctic waters and lowering in SSTs at our core site during the recorded Middle Pleistocene glacial.