Resiliencia en crestas de arrecifes coralinos del este del golfo de Batabanó, Cuba, y factores determinantes probables

RESUMEN Se comparó el grado de resiliencia de seis crestas arrecifales del este del golfo de Batabanó, Cuba. Tres fueron del norte del golfo de Cazones (Tramo Norte) y las restantes, del oeste de Cayo Largo (Tramo Sur). Las del primer tramo fueron las de faro Cazones, Norte de la cresta de cayo Diego Pérez y de faro Diego Pérez. Las otras tres fueron las de cayo Rico, arrecifes Los Ballenatos y arrecifes Hijos de Los Ballenatos. Se emplearon los indicadores biológicos del Protocolo AGRRA. El Tramo Norte presentó las crestas más resilientes, sobre todo la de faro Cazones. Las del Tramo Sur no exhibieron resiliencia. Fueron varios e interrelacionados, los factores aparentemente más determinantes en la resiliencia. Entre estos, cuatro se consideraron como fuerzas motrices: resguardo contra el oleaje, circulación habitual giratoria ciclónica en la ensenada de Cazones, entrada de nutrientes provenientes tanto de la ciénaga de Zapata como de aguas profundas, y abundancia del erizo herbívoro Diadema antillarum. Los demás factores, desencadenados por los anteriores y también interrelacionados, fueron, al parecer la menor afectación por oleaje y sedimentos, estabilización de fragmentos vivos de coral, índices favorables de macroalgas bentónicas, cierta retención de nutrientes y plancton, más alimentación heterotrófica de los corales, mayor auto reclutamiento de corales y del erizo Diadema; mejores condiciones para el asentamiento y viabilidad de los reclutas, y para el recapamiento de corales; mayor crecimiento y recuperación de los corales y mejores condiciones térmicas contra el blanqueamiento de corales ABSTRACT The degree of resilience of six reef crest sites was compared at the east of the Gulf of Batabano, Cuba. Three of them were located north of the Gulf of Cazones (Northern Stretch), while the remaining ones were west of Cayo Largo (Southern Stretch). Those of the Northern Stretch were “Faro Cazones”, north of the crest of cayo Diego Pérez and “Faro Diego Pérez”. The remaining sites were those of the cayo Rico, Los Ballenatos reefs, and Hijos de Los Ballenatos reefs. The AGRRA biological indicators were applied. The Northern Stretch presented the most resilient crests, mainly that of “Faro Cazones”. Those of the Southern Stretch did not reveal signs of resilience. Several interrelated factors were apparently more linked to resilience. Four of them were considered as driving forces: shelter from waves, usual cyclonic revolving water circulation in the Ensenada de Cazones, nutrient input from the Zapata swamp and deep water, and the abundance of the herbivore sea urchin Diadema antillarum. Triggered by these driving forces, the remaining factors apparently were less effect of waves and sediments, stabilization of live coral fragments, favorable benthic macro-algae indices, some retention of nutrient and plankton, increased coral heterotrophic feeding; better conditions for recruit settlement and viability, and for coral re-sheeting; faster coral growth and recuperation and better thermal conditions against coral bleaching.

Morphometric study and length-weight relationship of Therapon jarbua, Forsskal

The different morphometric characters of Therapon jarbua showed a linear relationship and uniformity in the various biometric measurements whereas the length-weight relationship showed a curvilinear graph. The studies also indicate that there is no significant difference, in the morphometric characters and length-weight relationship between the males and females. Ponderal index values for males and females was found to fluctuate between 1.3 to 1.5 for most of their life times with the peaks and crests appearing at different lengths for males and females.

A TAXONOMIC REVIEW OF TYLOTOTRITON VERRUCOSUS ANDERSON (AMPHIBIA, CAUDATA, SALAMANDRIDAE)

Generally it has not been recognized that salamanders of two distinctive color morphs currently are assigned to Tylototriton verrucosus Anderson. One form is uniformly dark brown dorsally, with bright orange coloration confined to the ventral edge of the tail; the other has a dark brown to black dorsal ground color with orange dorsolateral warts, an orange vertebral crest, and orange lateral and medial crests on the head. In addition, the limbs and ventrolateral surfaces of the second form have a variable pattern of orange coloration. The brown form occurs in northeastern India, Nepal, northern Burma, Bhutan, northern Thailand, the type locality in extreme western Yunnan, and perhaps in northern Vietnam. The orange-patterned form occurs only in western Yunnan Province, People's Republic of China. The two forms appear to be allopatric but occur close together in the area of the type locality near the Burma border in western Yunnan. There is no evidence of color intergradation in specimens from this region. Analyses of morphometric and meristic characters, however, suggest the possibility of limited genetic exchange between adjacent populations of brown and orange-patterned forms in western Yunnan. The genetic and taxonomic relationships between the two forms is not fully resolved. However, these two highly distinctive forms obviously have evolved along independent trajectories and merit taxonomic recognition. We therefore propose to restrict the concept of Tylototriton verrucosus to the brown form and designate a neotype for that purpose, and we describe a new species to receive the orange-patterned form.

Report of Prionospio complex (Annelida: Polychaeta: Spionidae) from China's waters, with description of a new species

Nine species of Prionospio complex are recorded front China's waters, including one new species and six newly recorded species. Prionospio (Prionospio) pacifica sp. nov., is characterized by having first and forth pairs of branchiae pinnate, second and third pairs of apinnate, ventral crest on Setiger 9 and dorsal crests on Setigers 10-25. Apoprionospio kirrae (Wilson, 1990), Prionospio (Aquilaspio) convexa Imajima, 1990, Prionospio (Minuspio) multibranchiata Berkeley, 1927, Prionospio (Prionospio) bocki Soderstrom, 1920, Prionospio (Prionospio) dubia Maciolek, 1985 and Prionospio (Prionospio) paradisea Imajima, 1990 are recorded for the first time from China's waters.

New records of Paraprionospio (Annelida: Spionidae) from Chinese waters, with the description of a new species

Paraprionospio pinnata (Ehlers, 1901), a poorly known and potentially cosmopolitan polychaete, was examined from museum specimens and from collections in Jiaozhou Bay, the Yellow Sea. New observations indicate that previous Chinese records of P. pinnata are doubtful, and that Chinese waters contain at least three valid species of Paraprionospio, two are known and one is new. Paraprionospio inaequibranchia (Caullery, 1914) and Paraprionospio coora Wilson, 1990, previously misidentified as P. pinnata, are reported from Chinese waters for the first time. Paraprionospio crist'ata. new species, is characterized by having brown pigment patches on the prostomium, ventral crests on chaetigers 9 and 10, dorsal crests on the middle part of the body (from chaetigers 21-23, not beyond chaetiger 29). thin filaments on chaetiger 3, and bifoliate branchial lamellae.

The effect of differences in methodology among some recent applications of shearing quotients.

A shearing quotient (SQ) is a way of quantitatively representing the Phase I shearing edges on a molar tooth. Ordinary or phylogenetic least squares regression is fit to data on log molar length (independent variable) and log sum of measured shearing crests (dependent variable). The derived linear equation is used to generate an 'expected' shearing crest length from molar length of included individuals or taxa. Following conversion of all variables to real space, the expected value is subtracted from the observed value for each individual or taxon. The result is then divided by the expected value and multiplied by 100. SQs have long been the metric of choice for assessing dietary adaptations in fossil primates. Not all studies using SQ have used the same tooth position or crests, nor have all computed regression equations using the same approach. Here we focus on re-analyzing the data of one recent study to investigate the magnitude of effects of variation in 1) shearing crest inclusion, and 2) details of the regression setup. We assess the significance of these effects by the degree to which they improve or degrade the association between computed SQs and diet categories. Though altering regression parameters for SQ calculation has a visible effect on plots, numerous iterations of statistical analyses vary surprisingly little in the success of the resulting variables for assigning taxa to dietary preference. This is promising for the comparability of patterns (if not casewise values) in SQ between studies. We suggest that differences in apparent dietary fidelity of recent studies are attributable principally to tooth position examined.

Ocean structure and climate (Eastern North Atlantic): in situ measurement and remote sensing

Structure and climate of the east North Atlantic are appraised within a framework of in situ measurement and altimeter remote sensing from 0 degree - 60 degree N. Long zonal expendable bathythermograph /conductivity-temperature-depth probe sections show repeating internal structure in the North Atlantic Ocean. Drogued buoys and subsurface floats give westward speeds for eddies and wavelike structure. Records from longterm current meter deployments give the periodicity of the repeating structure. Eddy and wave characteristics of period, size or wavelength, westward propagation speed, and mean currents are derived at 20 degree N, 26 degree N, 32.5 degree N, 36 degree N and 48 degree N from in situ measurements in the Atlantic Ocean. It is shown that ocean wave and eddy-like features measured in situ correlate with altimeter structure. Interior ocean wave crests or cold dome-like temperature structures are cyclonic and have negative surface altimeter anomalies; mesoscale internal wave troughs or warm structures are anticyclonic and have positive surface height anomalies. Along the Eastern Boundary, flows and temperature climate are examined in terms of sla and North Atlantic Oscillation (NAO) Index. Longterm changes in ocean climate and circulation are derived from sla data. It is shown that longterm changes from 1992 to 2002 in the North Atlantic Current and the Subtropical Gyre transport determined from sla data correlate with winter NAO Index such that maximum flow conditions occurred in 1995 and 2000. Minimum circulation conditions occurred between 1996-1998. Years of extreme negative winter NAO Index result in enhanced poleward flow along the Eastern Boundary and anomalous winter warming along the West European Continental Slope as was measured in 1990, 1996, 1998 and 2001.

A Description of the Stationary Wave Pattern of a Marine Craft in Shallow and Intermediate Water Depths

A stationary phase model is used to study supercritical waves generated by high speed ferries. Some general relationships in terms of wave angle, propagation direction, dispersion relationship and depth wavelength relationship are explored and discussed. In particular, it is shown that the wave pattern generated by high speed craft at supercritical speeds depends mainly on the relationship of water depth and ship speed and that the wave patterns are similar in terms of location of crests and troughs for a given depth Froude number. In addition it is found that the far field wave pattern can be described adequately using a single moving point source. The theoretical model compares well with towing tank measurements and full scale data over a range of parameters and hull shapes. The paper also demonstrates that the far field wave pattern at supercritical speeds should be non-dimensionalised by water depth and not hull length unlike it is usually done for subcritical speeds.

Efeitos de um programa de exercícios específico no domicílio, em indivíduos com doença arterial coronária, na composição corporal, gordura abdominal, perfil lipídico, glicose e nível de atividade física

contribuindo para o aumento da gordura abdominal, e consequentes complicações metabólicas. O exercício físico permite quebrar este ciclo através da estimulação da lipólise e da utilização de ácidos gordos. Objetivo: Verificar os efeitos de um programa de exercícios no domicílio, em indivíduos com doença arterial coronária, na composição corporal, gordura abdominal, perfil lipídico, glicose, e nível de atividade física. Métodos: Estudo experimental composto por 20 indivíduos, aleatorizados grupo experimental (GE) e grupo de controlo (GC), ambos com 10, tendo o GE sido sujeito ao programa durante 8 semanas. Realizou-se uma avaliação inicial e final, através da bioimpedância, Tomografia Computorizada (TC) abdominal, perimetria, adipometria, análises sanguíneas e acelerómetro. Resultados: Numa análise intergrupal, verificouse uma diminuição da percentagem (%) de gordura total (GT) calculado pela adipometria (p<0.01), na prega supra-ilíaca (p=0.005), na prega abdominal horizontal (p=0.001) e vertical (p=0.003) no GE, e da % de tempo em atividades moderadas no GC (p=0.035). Após 8 semanas o GE diminuiu a %GT (p=0.008); a massa gorda (MG) (p=0.002); perímetro abaixo da última costela (p=0.037) e acima das cristas-ilíacas (p=0.021); %GT calculado (p=0.002); pregas supra-ilíaca (p=0.008), abdominal horizontal (p=0.002) e vertical (p=0.033); TC abdominal subcutâneo (p=0.031) e %de tempo em atividades vigorosas (p=0.031). O GC diminuiu a %GT (p=0.002) e MG (p=0.008); aumentou o perímetro ao nível dos grandes trocânteres (p=0.008), diminuiu o rácio cintura/anca (p=0.002), e a %de tempo em atividades moderadas (p=0.031) e vigorosas (p=0.008). Parece existir uma tendência no GE para diminuição do rácio cintura/anca, c-LDL, triglicerídeos e aumento do nível de atividade moderado. Conclusão: O programa de exercícios no domicílio demonstrou uma diminuição da gordura abdominal, alteração da composição corporal, e parece promover uma melhoria no perfil lipídico e no aumento do nível de atividade física moderado.

Three Wax Seals

3 Wax seals including: 1 seal of the Woodruff crest and 2 seals of fide et fortitude (faith and fortitude), n.d.

Scoliose idiopathique de l’adolescence : relations entre la morphologie pelvienne, l’attitude posturale et l’équilibre orthostatique selon différentes sévérités

Des anomalies dans la morphologie pelvienne, la posture du tronc et le contrôle de l’équilibre de jeunes filles atteintes de scoliose idiopathique de l’adolescence (SIA) ont souvent été l’objet d’études. Rares sont celles ayant distingué ces troubles en fonction de la sévérité de la déformation vertébrale. De plus, aucune n’a évalué à l’intérieur d’une même étude l’orientation et la distorsion pelvienne, l’asymétrie posturale et l’instabilité en position debout de sujets SIA. Une telle étude permettrait de comprendre le développement de la maladie et de mettre en évidence des facteurs de risque aidant au pronostic. L’objectif général de cette thèse est d’identifier des facteurs biomécaniques associés à la croissance osseuse, la posture et l’équilibre distinguant une SIA modérée d’une sévère. Les positions 3D de 14 repères prises sur 46 filles ayant une SIA droite (modérée et sévère) et 28 sujets témoins ont été captées pour quantifier la morphologie pelvienne et la posture. Un maintien en position debout de 64 s sur une plate-forme de force a aussi été enregistré afin d’évaluer leur équilibre. Les paramètres retenus sont les angles d’orientation pelvienne et du tronc; les distances entre la crête iliaque et S1 mesurant la distorsion pelvienne; la moyenne, l’amplitude et la vitesse du centre de pression (COP) en médiolatéral (ML) et antéropostérieur ainsi que la moyenne et l’amplitude du moment libre. Les différences entre les trois groupes (témoin, SIA modérée et SIA sévère) sont testées par des ANOVA et les relations entre l’angle de Cobb et les paramètres pelviens, posturaux ou d’équilibre, par des coefficients de corrélations. De plus, des régressions multiples exprimant l’angle de Cobb sont effectuées avec les paramètres pelviens, posturaux et d’équilibre afin de déterminer la classe de paramètres prédisant le mieux l’angle de Cobb. Aucune ANOVA n’est significative pour l’orientation pelvienne, bien que des différences de géométrie pelvienne soient notées entre les deux groupes de sujets SIA. Les SIA modérées ont un pelvis gauche moins profond que les SIA sévères et les sujets témoins, tandis que les SIA sévères ont un pelvis droit plus large d’environ 1,5 cm que celui des SIA modérées. Un coefficient de corrélation de -0,54 associe une rotation pelvienne droite à l’augmentation de la largeur de la crête iliaque. Au niveau postural, les SIA sévères démontrent des inclinaisons latérales et antérieures du tronc ainsi qu’une rotation axiale du haut du corps plus marquées que les SIA modérées. Les corrélations entre les paramètres posturaux, l’angle de Cobb et la morphologie pelvienne indiquent que l’attitude posturale est associée à la distorsion pelvienne dans tous les plans anatomiques, tandis qu’elle ne l’est que dans les plans sagittal et horizontal à l’angle de Cobb. Les différences retrouvées entre les deux groupes SIA concernant les troubles d’équilibre résultent en une augmentation de l’amplitude et de la vitesse du COPML. Une régression multiple de 0,896 est observée par l’emploi des paramètres pelviens, posturaux et d’équilibre, bien que ceux se rapportant à la distorsion pelvienne soient les mieux corrélés à l’angle de Cobb. Cette thèse permet de distinguer la morphologie pelvienne de sujets SIA sévères des modérées, soulignant la détection d’une anomalie de croissance avant que l’angle de Cobb ne soit élevé. Bien que les indices de croissance pelvienne soient davantage corrélés à ce dernier, c’est en considérant globalement la morphologie pelvienne, la posture et l’équilibre qu’une détermination précise de la sévérité d’une scoliose est réalisée. La mise en évidence de tels facteurs de prédiction de la SIA peut faciliter le pronostic d’une courbure.

Hidrolipoclasia con solución salina hipotónica versus isotónica en adiposidad localizada

Introducción: La hidrolipoclasia es una técnica de moldeamiento corporal consistente en la infiltración de una solución en el tejido adiposo con la consiguiente aplicación de ultrasonido para producir lisis en los adipocitos y reducción del tejido adiposo en el área de tratamiento. Sin embargo, existen múltiples variaciones a la técnica, entre ellas el tipo de solución utilizada. El objetivo de este estudio fue comparar los resultados con la técnica de hidrolipoclasia en cuanto a reducción de medidas con el uso de solución salina hipotónica versus isotónica. Metodología: Estudio descriptivo de corte transversal, se analizaron historias clínicas de pacientes a los que se les realizó hidrolipoclasia entre enero de 2013 y febrero 2014 en dos centros médicos estéticos de Bogotá. Se compararon dos técnicas (utilizando solución salina isotónica versus hipotónica) en cuanto a la disminución de medidas antropométricas tomadas antes y después del tratamiento. Los datos fueron analizados mediante la comparación de medias utilizando la prueba t de Student. Resultados: Se analizaron 37 historias clínicas, 19 pacientes sometidos a hidrolipoclasia con solución salina hipotónica y 18 con isotónica. Después de la realización de un procedimiento hubo una disminución estadísticamente significativa (p: 0,000) en todas las medidas antropométricas evaluadas, siendo mayor comparativamente en los pacientes tratados con solución hipotónica en cintura, perímetro abdominal y perímetro a nivel de crestas iliacas. Los efectos secundarios incluyeron equimosis y hematomas. No se presentaron complicaciones. Conclusión: La hidrolipoclasia es segura y eficaz en el manejo de adiposidad localizada, teniendo una mayor efectividad cuando se utiliza solución salina hipotónica.

Obesidade adolescente, composição corporal e aptidão física

RESUMO: A principal razão que me levou a escolher este estágio e esta intervenção, foi o facto de gostar muito de trabalhar com jovens. Esse gosto, aliado à paixão que tenho pelo exercício e saúde, trouxe-me para um projecto que visa alterar e promover estilos de vida saudáveis em jovens obesos com idades entre os 12 e os 16 anos de idade. O estágio teve a duração de 10 meses, de Outubro de 2010 a Julho de 2011. Começamos com a definição dos protocolos a implementar e das tarefas a realizar. A primeira dessas tarefas, centrava-se no recrutamento da amostra que pretendíamos para desenvolver o estudo. Paralelamente ao projecto TOP, colaborámos também nas consultas de obesidade pediátrica no Hospital de Santa Maria, o que nos permitiu recrutar jovens que iam às consultas e incluí-los no projecto TOP. Após termos efectuado o recrutamento, começámos com as aulas práticas e teóricas. Essas aulas ocorriam na Universidade Lusófona, todos os sábados, das 10 às 12 horas. Eram sempre da nossa responsabilidade as aulas práticas, e as teóricas quando se falava de exercício. Nas aulas práticas realizavam-se circuitos, jogos tradicionais, jogos colectivos, e jogos que promovessem a competição saudável e a inter-ajuda, visto que ali todos os participantes tinham um objectivo comum. Durante o ano foram realizadas duas colónias de férias, onde organizámos outro tipo de actividades, nomeadamente mini-golf e caminhadas na zona do Jamor. Tanto as colónias de férias, como as avaliações eram da nossa inteira responsabilidade, desde a preparação, à execução e realização das mesmas. De referir que, tendo em conta os resutados obtidos, os participantes que melhoraram na sua capacidade cardiovascular apresentaram igualmente melhoras ao nível da composição corporal, nomeadamente com a diminuição do perímetro da anca e do perímetro acima das cristas ilíacas. Importa ainda referir que ocorreram melhorias significativas (p <0,05) ao nível da composição corporal, no que se refere ao perímetro da meia distância entre a grelha costal e as cristas ilíacas, no teste da flexibilidade dos membros inferiores e na força média. Os objectivos do estágio centravam-se em adquirir competências no que diz respeito a conhecer as características da população alvo tanto das consultas como do programa TOP, saber aplicar as recomendações internacionais de actividade física para adolescentes obesos, ser capaz de adaptar a prescrição de exercício às diferentes necessidades dos adolescentes, planear e colocar em prática os planos de aula da componente física do TOP, conduzir de forma autónoma uma consulta de avaliação e aconselhamento físico, interagir em contexto clínico com especialidades de outras áreas de intervenção, planear e implementar a calendarização das sessões teórico-práticas do Projecto TOP, saber colaborar com uma equipa multidisciplinar num ambiente clínico e colaborar na intervenção e elaboração de um projecto científico. Os resultados obtidos demonstram que uma replicação futura deste projecto, tendo em conta sempre limitações que possam ocorrer, por exemplo, ao nível dos protocolos e testes, pode melhorar a qualidade de vida do adolescente, com vista a um futuro adulto mais saudável.ABSTRACT: The main reason that made me decide on this internship is the fact that I enjoy working with young people. This, combined with the passion I have for exercising and health, led me to a project aiming at changing lifestyles by promoting a healthy lifestyle among obese young people aged between 12 and 16 years old. The internship lasted for 10 months, from October 2010 to July 2011. We started with the definition of protocols to implement and carry out the POT project (Pediatric Obesity Treatment). The first task focused on the recruitment of the sample we needed to conduct the study for this project. Along with the POT project, we‟ve also collaborated in clinical pediatric obesity surgery in Santa Maria Hospital, which allowed us to recruit young people who came to surgery and include them in the sample. After having carried out the recruitment, we started with the practical and theoretical lessons. These lessons took place at the Universidade Lusófona de Humanidades e Tecnologias (ULHT) every month on Saturdays from 10 to 12. It was always our responsibility to prepare and present both the physical lessons and the theoretical ones concerning advice on everyday exercising. During practical lessons, circuits, traditional games and team games were held in order to promote a healthy competition and mutual help, since all the participants had a common goal. During the year there were two holiday camps, where we did many more activities, including mini-golf and walking in the area of Jamor. In those camps, all activities and evaluation sessions were our responsibility. By analysing the results we came to the conclusion that the participants who improved their cardiovascular capacity also improved their body composition, particularly with the reduction of the hip circumference and the circumference above the iliac crests. It should also be noted that significant improvements (p <0.05) in terms of body composition occurred namely concerning the circumference of the half distance between the rib cage and the iliac crests, the test of lower limbs flexibility and average strength. The objectives of the internship were to develop the ability to understand the characteristics of the adolescents in the POT project, know how to apply international recommendations for physical activity for obese adolescents, being able to individualize the exercise prescription for the different needs of adolescents, plan and implement physical and theorical lessons, conduct an independent surgery with a physical evaluation and counseling, interact in the context of other clinical speciality areas, plan and implement the scheduling of theoretical-practical sessions, learn how to collaborate with a multidisciplinary team in a clinical setting, intervene and collaborate in the development of a scientific project. The results show that a future replication of this project, always taking into account constraints that may occur, for example, the ones concerning the protocols, the testing, can improve the quality of life of adolescents aiming to a healthier adult life.

Using remotely sensed data to support flood modelling

Recent severe flooding in the UK has highlighted the need for better information on flood risk, increasing the pressure on engineers to enhance the capabilities of computer models for flood prediction. This paper evaluates the benefits to be gained from the use of remotely sensed data to support flood modelling. The remotely sensed data available can be used either to produce high-resolution digital terrain models (DTMs) (light detection and ranging (Lidar) data), or to generate accurate inundation mapping of past flood events (airborne synthetic aperture radar (SAR) data and aerial photography). The paper reports on the modelling of real flood events that occurred at two UK sites on the rivers Severn and Ouse. At these sites a combination of remotely sensed data and recorded hydrographs was available. It is concluded first that light detection and ranging Lidar generated DTMs support the generation of considerably better models and enhance the visualisation of model results and second that flood outlines obtained from airborne SAR or aerial images help develop an appreciation of the hydraulic behaviour of important model components, and facilitate model validation. The need for further research is highlighted by a number of limitations, namely: the difficulties in obtaining an adequate representation of hydraulically important features such as embankment crests and walls; uncertainties in the validation data; and difficulties in extracting flood outlines from airborne SAR images in urban areas.

Computer modelling and estimation of recruitment patterns of non-branching coral colonies at three sites in Wakatobi Marine Park, S.E. Sulawesi, Indonesia; implications for coral reef conservation

We have studied growth and estimated recruitment of massive coral colonies at three sites, Kaledupa, Hoga and Sampela, separated by about 1.5 km in the Wakatobi Marine National Park, S.E. Sulawesi, Indonesia. There was significantly higher species richness (P<0.05), coral cover (P<0.05) and rugosity (P<0.01) at Kaledupa than at Sampela. A model for coral reef growth has been developed based on a rational polynomial function, where dx/dt is an index of coral growth with time; W is the variable (for example, coral weight, coral length or coral area), up to the power of n in the numerator and m in the denominator; a1……an and b1…bm are constants. The values for n and m represent the degree of the polynomial, and can relate to the morphology of the coral. The model was used to simulate typical coral growth curves, and tested using published data obtained by weighing coral colonies underwater in reefs on the south-west coast of Curaçao [‘Neth. J. Sea Res. 10 (1976) 285’]. The model proved an accurate fit to the data, and parameters were obtained for a number of coral species. Surface area data was obtained on over 1200 massive corals at three different sites in the Wakatobi Marine National Park, S.E. Sulawesi, Indonesia. The year of an individual's recruitment was calculated from knowledge of the growth rate modified by application of the rational polynomial model. The estimated pattern of recruitment was variable, with little numbers of massive corals settling and growing before 1950 at the heavily used site, Sampela, relative to the reef site with little or no human use, Kaledupa, and the intermediate site, Hoga. There was a significantly greater sedimentation rate at Sampela than at either Kaledupa (P<0.0001) or Hoga (P<0.0005). The relative mean abundance of fish families present at the reef crests at the three sites, determined using digital video photography, did not correlate with sedimentation rates, underwater visibility or lack of large non-branching coral colonies. Radial growth rates of three genera of non-branching corals were significantly lower at Sampela than at Kaledupa or at Hoga, and there was a high correlation (r=0.89) between radial growth rates and underwater visibility. Porites spp. was the most abundant coral over all the sites and at all depths followed by Favites (P<0.04) and Favia spp. (P<0.03). Colony ages of Porites corals were significantly lower at the 5 m reef flat on the Sampela reef than at the same depth on both other reefs (P<0.005). At Sampela, only 2.8% of corals on the 5 m reef crest are of a size to have survived from before 1950. The Scleractinian coral community of Sampela is severely impacted by depositing sediments which can lead to the suffocation of corals, whilst also decreasing light penetration resulting in decreased growth and calcification rates. The net loss of material from Sampela, if not checked, could result in the loss of this protective barrier which would be to the detriment of the sublittoral sand flats and hence the Sampela village.