ABSTRACT The present study aimed to evaluate the ecology considering distribution, abundance, population structure, and fecundity of the marine diplostraceans Penilia avirostris and Pseudevadne tergestina in the Veracruz Reef System National Park, southwest Gulf of Mexico. Surface samples were collected with a 300 μm mesh plankton net at 26 sampling sites in June, August, October (2011), May (2012) and June (2013). Temperature, salinity, and dissolved oxygen were measured in situ. The temperature range was 26.53 ± 0.41 and 29.29 ± 0.27°C, salinity between 33.43 ± 0.49 and 35.91 ± 0.09, and dissolved oxygen between 2.92 ± 0.08 and 6.56 ± 0.08 mg L-1. P. avirostris and P. tergestina presented the highest density, with 2200 ind 100 m-3 in June and 5980 ind 100 m-3 in October, respectively. Four stages were determined in P. avirostris. In P. tergestina, there were five instars, with males in August and October. The size of parthenogenic females of P. avirostris was 773.4 ± 20.08 μm. In P. tergestina, it was 637.6 ± 49.28 μm. The number of embryos in P. avirostris was 2 to 7, and in P. tergestina, 2 to 8 embryos. The correlations between body length and the number of embryos in both species were statistically significant under the potential model (r > 0.68 for both species, P < 0.001). The transects with the highest abundance were the northern and the southern zones because they are far from the influence of the Jamapa River. The density of these crustaceans is related to optimal temperature, salinity, and dissolved oxygen values. The low proportions obtained from gamogenic individuals of P. avirostris and P. tergestina suggest that in tropical and subtropical regions, gamogenesis is not crucial for the life cycle of these organisms.

Abstract: The Port of Veracruz, Mexico was artificially built at the beginning of the 21st century, dredging the sea floor and removing reefs to allow the entry of large ships, which led to a growth in the traffic of goods and people through it, making it the largest commercial port in all of Mexico. In 1992 the Government of Mexico decreed the area of coastal reefs near the Port of Veracruz as a protected natural area with the name of the Parque Nacional Sistema Arrecifal Veracruzano (PSNSAV). In 2013, with the demand of international trade, the decision was made to expand the port, generating job growth in the area and an increase in the flow of containers and automobiles, also have a greater capacity to transport cereals, minerals and fuels. In contrast to the disagreements of the society due to the loss of protected space, the Parks polygon had to be modified. This work try to demonstrated that the construction of the port expansion began previous the presentation to the environmental authorities of the Environmental Impact Statement and the change in the protected limits with the disappearance of the Punta Gorda reefs and the dredging of Vergara Bay for the arrival of deep draft vessels. Through a systematic mapping of the scientific literature combined with satellite mapping and visual interpretation of images, and documentary analysis, we determined the damage to the reef system, which has protected species according to Mexican national regulations.

Resumen: El Puerto de Veracruz, México fue construido de manera artificial a principios del siglo XXI, dragando el suelo marino y removiendo arrecifes para permitir la entrada de buques de gran tamaño, lo que conllevó a un crecimiento en el tráfico de mercancías y personas a través de él y convirtiéndolo en el mayor puerto comercial de todo México. En 1992 el Gobierno de México decretó en la zona de arrecifes litorales cercanos al Puerto de Veracruz como un área natural protegida con el nombre de Parque Nacional Sistema Arrecifal Veracruzano (PSNSAV). En 2013, con la demanda del comercio internacional, se tomó la decisión de ampliar el puerto, generando un incremento de empleo en la zona y un aumento del flujo de contenedores y automóviles, además de tener una mayor capacidad para transportar cereales, minerales y combustibles. Frente a las disconformidades de la sociedad por la pérdida de espacio protegido, el polígono de Parques tuvo que ser modificado. Con este trabajo se demuestra que la construcción de la ampliación del puerto se inició previa autorización de las autoridades ambientales de la Manifestación de Impacto Ambiental y el cambio en los límites protegidos, lo dicho tuvo inicio con la desaparición de los arrecifes de Punta Gorda y el dragado de la Bahía de Vergara para el arribo de buques de gran calado. A través de un mapeo sistemático de la literatura científica combinado con mapeo satelital e interpretación visual de imágenes, así como el análisis documental, se determinó el daño al sistema de arrecife, el cual cuenta con especies protegidas de acuerdo a la normatividad nacional mexicana.

ABSTRACT The ecology, distribution, and taxonomy of bopyrid isopod species are often omitted from studies not systematically addressed to crustaceans. From a wider study of zooplankton in coastal and reef waters of the Mexican Caribbean Sea, two bopyrid species were collected, Probopyrinella latreuticola, attached to the branchial chamber of Latreutes fucorum andProbopyrus pandalicola parasitizing the branchial chamber of Palaemon northropi. For both parasite-host associations, these records represent a new locality and the southernmost record in the Mexican Caribbean. A map and a list of the bopyrid species belonging to Bopyridae recorded in the Mexican Caribbean are provided.

As ocean temperatures increase, so does the need for accurate, regular, and widespread temperature data. This is especially important for researchers studying corals, which can be pushed over their bleaching thresholds by small, sustained changes in water temperature. Satellite data products offer longitudinal estimates of sea surface temperature (SST) taken at regular intervals without the ongoing costs and geospatial limits associated with underwater temperature loggers. However, previous work indicates satellite data are sometimes characterized by significant temperature biases, particularly in stratified coastal waters. Here, we compared the foundation sea surface temperature (fSST) estimated from a highly processed, gridded satellite data set (GHRSST MUR L4 Global SST) to in situ temperature (IST) data collected from coral reef habitats in the top 20 m of the water column at 19 sites in Panama. Comparisons between Pacific and Caribbean coasts and between upwelling and non-upwelling seasons provide a robust test of the utility of this product to estimate subsurface temperatures. The mean differences between fSST and IST show that MUR fSST accurately reflects temperatures at shallow (<9 m) depths on the Caribbean coast (mean bias ≤0.55°C ± standard error (SE) 0.01°C) and during the non-upwelling season on the Pacific coast (mean bias ≤0.26°C ± SE 0.03°C). MUR fSST poorly reflects IST during the Pacific upwelling season, especially at sites 12 m and deeper. In such cases, 66% of satellite estimates deviated from ISTs by >1°C. Our findings underscore how highly processed SST data products should be ground-truthed before being used as a substitute for IST, especially in upwelling areas.

Abstract Introduction: Echinoderms are strictly aquatic animals and one of the groups of marine invertebrates whose ecological importance is crucial for the environments where they inhabit. The most outstanding characteristic is their pentaradial symmetry. These organisms can be distributed in a wide variety of oceanic environments, and are not exclusive inhabitants of reef formations. A total of 1 539 species have been registered, of which 717 belong to the Pacific and 60 of them have been registered for El Salvador. Objective: The objective of the work was to record the richness and density of echinoderm species in rocky reefs of Punta Amapala (La Unión). Methods: The sampling was conducted in five sites, two of them at 3 m of depth and three at 6 m. For this, snorkeling and autonomous diving were used, covering two band transects of 30 x 1 m. Within the transects, the identification (richness) and counting (abundance) of the organisms was carried out. Results: The species that presented the highest density at 3 m reefs was Echinometra vanbrunti (0.83 indv/m2), followed by the ophiuroid Ophiocomella alexandri (0.16 indv/m2) and Ophiocoma aethiops (0.16 indv/m2). And at the 6 m reefs were Ophiothela mirabilis (0.83 indv/m2), Ophionereis annulata (0.21 indv/m2), Ophiothrix rudis (0.08 indv/m2) and Ophiocomella alexandri (0.01 indv/m2). Conclusions: These organisms fulfill various ecological roles, such as being bioindicators of water quality by tolerating certain changes in physicochemical conditions and fulfilling the role of macrofauna hosts due to the cavities formed by some sea urchins. That is why sampling efforts must increase in these areas to monitor the quality and health of the rocky reefs, whose role is key, as they are, together with Los Cóbanos, the largest in the country.

Resumen Introducción: Los equinodermos son animales estrictamente acuáticos y de los grupos de invertebrados marinos cuya importancia ecológica es crucial para los ambientes en donde habitan. La característica más destacada es su simetría pentarradial. Estos organismos pueden distribuirse en una amplia variedad de ambientes oceánicos, y no ser exclusivamente habitantes de las formaciones arrecifales. Se han registrado el total de 1 539 especies, de las cuales 717 pertenecen a Pacífico y 60 de ellas se han registrado en El Salvador. Objetivo: El objetivo del trabajo fue registrar la riqueza y densidad de especies de equinodermos en arrecifes rocosos de Punta Amapala (La Unión). Métodos: El muestreo fue llevado a cabo en cinco sitios, dos a 3 m de profundidad y tres a 6 m. Para esto, se utilizó snorkeling y buceo autónomo, recorriendo dos transectos de banda de 30 x 1 m. Dentro de los transectos, se realizó la identificación (riqueza) y contabilización (abundancia) de los organismos. Resultados: La especie que presentó mayor densidad en los arrecifes de 3 m fue Echinometra vanbrunti (0.83 indv/m2), seguido por el ofiuroideo Ophiocomella alexandri (0.16 indv/m2) y Ophiocoma aethiops (0.16 indv/m2). Y en los arrecifes a 6 m fueron Ophiothela mirabilis (0.83 indv/m2), Ophionereis annulata (0.21 indv/m2), Ophiothrix rudis (0.08 indv/m2) y Ophiocomella alexandri (0.01 indv/m2). Conclusiones: Estos organismos, cumplen con diversos roles ecológicos, como ser bioindicadores de calidad de agua al tolerar ciertos cambios en las condiciones físico-químicas, así como cumplir el papel de hospederos de macrofauna por las cavidades que forman algunos erizos. Es por ello que los esfuerzos de muestreo deben incrementarse en estas zonas para monitorear la calidad y salud de los arrecifes rocosos, cuyo papel es clave, por ser junto con Los Cóbanos, los de mayor extensión en el país.

Abstract Introduction: The sea urchin Diadema mexicanum, due to its bioerosion activity, is considered of ecological importance. This phenomenon could negatively or positively affect coral reef ecosystems. The bioerosion process varies according to the abundance and size of the sea urchin. Objective: Juvenile organisms possess different metabolic needs compared to adults, so knowing their stomach content according to size allows us to quantify the selection of substrate bioeroded. Methods: To determine this, D. mexicanum individuals were collected in 12 sites from January 2009 to September 2010 along the Eastern Tropical Pacific coast. The stomach content was categorized in Carbonated Fraction (CF), Non-Carbonated Fraction (NCF), and Organic Matter (OM). Stomach content was analyzed according to a) juvenile (< 2.5 cm) or adult (> 2.5 cm) stage and b) locality. Results: Juveniles presented the following stomach content average percentages: 20.7 % OM, 12 % NCF and 67.9 % CF; and adults: 11.4 % OM, 14.8 % NCF and 73.8 % CF. Based on a Wilcoxon test and a Kendall linear regression, the following results were obtained. The carbonated fraction in the stomach increased by 0.47 units on average for every cm of growth (p < 0.05). OM consumed by D. mexicanum increases only 0.05 units for every cm of growth (p < 0.05). We found a difference of stomach content depending on the site (p < 0.05) and life stage (p < 0.05). Localities like Huatulco and Coco presented significant differences that could be related to local oceanographic conditions. Conclusions: We relate these changes of the stomach fractions to the necessity of the juvenile sea urchins for nutrients to maintain their growth. The amount of OM is crucial for the development of early stages, meaning that there is a difference in substrate selection associated with growth.

Resumen Introducción: El erizo de mar Diadema mexicanum, por su actividad de bioerosión, es considerado de importancia ecológica. Este fenómeno podría afectar negativa o positivamente a los ecosistemas de arrecifes de coral. El proceso de bioerosión varía según la abundancia y el tamaño del erizo de mar. Objetivo: Los organismos juveniles poseen diferentes necesidades metabólicas en comparación con los adultos, por lo que conocer el contenido estomacal según el tamaño, nos permite cuantificar la selección de sustrato bioerosionado. Métodos: Para determinar esto, se recolectaron individuos de D. mexicanum en 12 sitios desde enero de 2009 hasta septiembre de 2010 a lo largo de la costa del Pacífico Tropical Oriental. El contenido estomacal se clasificó en Fracción Carbonatada (FC), Fracción No Carbonatada (NCF) y Materia Orgánica (MO). El contenido estomacal se analizó según a) estadio juvenil (< 3 cm) o adulto (> 3 cm) y b) localidad. Resultados: Los juveniles presentaron los siguientes porcentajes promedio del contenido estomacal: 20.7 % OM, 12 % NCF y 67.9 % CF; y adultos: 11.4 % OM, 14.8 % NCF y 73.8 % CF. Con base en una prueba de Wilcoxon y una regresión lineal de Kendall, se obtuvieron los siguientes resultados. La fracción carbonatada en el estómago aumentó en promedio 0.47 unidades por cada cm de crecimiento (p < 0.05). La MO consumida por D. mexicanum aumenta solo 0.05 unidades por cada cm de crecimiento (p < 0.05). Encontramos una diferencia en el contenido estomacal según el sitio (p < 0.05) y el estadio de vida (P < 0.05). Localidades como Huatulco y Coco presentaron diferencias significativas que podrían estar relacionadas con las condiciones oceanográficas locales. Conclusiones: Relacionamos estos cambios de la composición porcentual del contenido estomacal con la necesidad de los erizos de mar juveniles de nutrientes para mantener su crecimiento. La cantidad de MO es crucial para el desarrollo de las primeras etapas, lo que significa que existe una diferencia en la selección de sustrato asociada con el crecimiento.

RESUMEN Numerosos autores han interpretado el margen pacífico colombiano como sucesivas acreciones de terrenos oceánicos, con la generación de cuencas de antearco bajo un régimen tectónico compresivo-transpresivo vigente durante el Cretácico tardío-Mioceno. Existe nueva información adquirida en la última década, consistente en nuevas secciones sísmicas y geológicas reprocesadas, además de información de pozos y columnas estratigráficas. En el presente trabajo se analiza esta nueva información y se hace notar que no presenta coherencia con los modelos de sucesivas acreciones de terrenos oceánicos propuestos a la fecha. Los nuevos datos sugieren que, entre el Cretácico tardío y el Eoceno Medio-tardío, las cuencas costa adentro (onshore basins) estuvieron regidas por una extensa plataforma marina, con crecimiento de carbonatos arrecifales hacia el final de ese periodo. Coetáneo a la sedimentación del Cretácico tardío, se presentó magmatismo efusivo, principalmente basáltico. A partir del Oligoceno, la evolución de las cuencas estuvo dominada por procesos diferentes durante tres periodos. Primero, en el Oligoceno-Mioceno temprano, en la cuenca Tumaco y subcuenca San Juan ocurrió un evento transtensional acompañado del emplazamiento de cuerpos ígneos hacia sus bordes orientales, con la generación de estructuras de pilares tectónicos, fosas tectónicas y fallas tipo dominó. En tanto, la subcuenca Atrato presentó hacia su límite sur deformación con fallas inversas locales concentradas en su flanco oriental. Segundo, durante el Mioceno Medio-tardío se levantó el flanco occidental de la cuenca Tumaco, mientras que en la subcuenca San Juan tuvo lugar deformación transpresiva dada por la interacción del sistema de fallas San Juan y Garrapatas. Tercero, durante el Pleistoceno, en la subcuenca Atrato se generó el anticlinal de Baudó asociado a un régimen transpresional. Los resultados aquí expuestos sugieren que no hay evidencia de acreción de terrenos oceánicos en las cuencas estudiadas; tampoco se observan los efectos generados por la presencia de un sistema de subducción durante el Cretácico tardío-Eoceno Medio. Esto abre la posibilidad de que el sistema de subducción en el margen pacífico colombiano haya comenzado en el Oligoceno temprano.

ABSTRACT Several authors have interpreted the Colombian Pacific margin as a succession of oceanic terrane accretions, with generation of forearc basins under a compressive-transpressive tectonic regime during the Late Cretaceous-Miocene. New data acquired in the last decade, consisting of reprocessed seismic lines, geological cross-sections, stratigraphic data from wells, and new stratigraphic columns, are analyzed in this study. We suggest that the proposed models of successive terrane accretions are not supported by the new data; rather, the onshore basins were likely controlled by a marine platform from the Late Cretaceous to the Middle-Late Eocene, with reef growth to the end of this period. In the Late Cretaceous, contemporary to the sedimentation stage, effusive magmatism, mainly basaltic, also occurred. Since Oligocene time, the basins were affected by three different tectonic processes. First, during the Oligocene-Early Miocene, an extensional-transtensional event occurred in the Tumaco Basin and San Juan Sub-basin, which produced horst and graben structures and domino faults, along with the emplacement of igneous bodies in the eastern flank of the basins. The Atrato Sub-basin was affected by local reverse faulting towards its eastern edge. Second, during the Mid-Late Miocene, the western side of the Tumaco Basin was uplifted, and transpressive deformation occurred in the San Juan Sub-basin as evidenced by the San Juan and Garrapatas fault systems. Finally, in the Atrato Sub-basin, a transpressional regime is evidenced by the Baudó anticline. Our results suggest there is no evidence of oceanic terrane accretions in the abovementioned basins during the Late Cretaceous-Middle Eocene. Furthermore, we do not see evidence of a subduction system during that period. We conclude that subduction in western Colombia could have begun during the Early Oligocene instead.

Abstract “For more than two decades, the Philippine government has protected the giant clams (Bivalvia: Cardiidae: Tridacninae) from exploitation and trade. However, there still is lack of information on the impact of these protective measures in conserving the species richness and density, especially in Palawan, the country’s last stronghold of these reef-associated bivalves. Hence, to assess the species richness and density of giant clams in Palawan, we conducted 57 photo-transect surveys in six sites covering 12,325 m 2. Out of these transect, 15 measured 5 × 25 m and the rest measured 5 × 50 m. For historical trends in the population of giant clams in Palawan, we used six published papers obtained from online platforms, 13 reports, and five undergraduate theses archived in local libraries. Information derived from recent field surveys indicated high variations in species richness (2 to 5 species) and densities (0.1 to > 3.6 ind.100 m -2). Historical data starting from 1984, including recent fieldwork, indicated very low densities and a declining trend. The current status suggests that giant clam populations’ viability and the reefs’ health are threatened. Effective mechanisms are needed to safeguard and enhance the remaining giant clam populations.” decades Bivalvia (Bivalvia Cardiidae Tridacninae trade However Palawan countrys country s reefassociated reef associated bivalves Hence phototransect photo transect 12325 12 325 12,32 2 1 platforms reports libraries ( 0.1 01 0 (0. 36 3 6 3. ind100 ind 100 ind.10 . -2) 1984 fieldwork trend populations reefs threatened populations. 1232 32 12,3 0. (0 ind10 10 ind.1 -2 198 123 12, ind1 ind. - 19

Abstract Herpyllobiid copepods are highly transformed mesoparasites that infect marine benthic polychaete annelids. The genus Herpyllobius Steenstrup and Lütken, 1861, the most diverse in the family, was known to infect exclusively polychaetes of the family Polynoidae, but it was recently reported also on another family. Species of Herpyllobius have been reported mainly from cold latitudes including Arctic and Antarctic areas, except for two subtropical species. During the taxonomic examination of flabelligerid polychaetes collected from a Western Australian coral reef system, a mesoparasitic copepod was found infecting a specimen of Lamispina horsti (Haswell, 1892). The copepod represents an undescribed species of Herpyllobius. The new species, Herpyllobius paulayi n. sp. belongs to a group of congeneric species (Group III) lacking intergenital processes or sclerotized dots. It diverges from the other species in this group by its possession of a unique combination of characters: 1) a globose ectosoma with pilose surface; 2) elongate, thick cylindrical egg sacs with +10 egg rows; 3) endosoma discoid, short, with two lateral, asymmetrical flattened processes and a medial lobe; 4) it attaches to the host prostomium; and 5) it infects a non-polynoid subtropical polychaete species. annelids Lütken 1861 Polynoidae areas system Haswell, Haswell (Haswell 1892. 1892 . 1892) n sp Group III dots characters 1 surface 2 elongate 10 +1 rows 3 discoid short lateral lobe 4 prostomium 5 nonpolynoid non polynoid 186 189 + 18

Abstract One of the major paradigms in ecology is the understanding of processes and patterns related to the structure of biological communities. Reef ecosystems, with their high productivity, habitat heterogeneity, and fish diversity provide a model for studying these processes. We sampled four sites three times during the season associated with the California Current and two times associated with the North Equatorial Current using video-transects on the coast of Zihuatanejo, Guerrero, Mexico to determine the relationship between the habitat characteristics and the structure of the fish assemblage. We recorded a total of 26 families and 54 species and estimated fish richness and abundance. In addition to measuring local water variables such as temperature (°C), salinity (PPT), pH and dissolved oxygen (O2%), we determined habitat heterogeneity by processing photographs of the substrate and calculated rugosity using the tape chain. Oxygen and temperature were the variables associated to sea water conditions that differentiated the sampled sites. The fish community structure presented high correlations with temperature, salinity, and dissolved oxygen, followed by the heterogeneity components such as rugosity and substrate diversity. Our results showed that seasonal changes in water conditions and physical components in the coast of Zihuatanejo promotes changes in the fish community. communities ecosystems productivity videotransects video transects Guerrero assemblage 2 5 abundance °C, C °C , (°C) PPT, PPT (PPT) O2%, O2 O O2% (O2%) chain (°C (PPT (O2% (O2 (O

Resumen Uno de los principales paradigmas en ecología es el entendimiento de procesos y patrones relacionados con la estructura de las comunidades biológicas. Los ecosistemas de arrecifes, con su alta productividad, heterogeneidad de hábitat y diversidad de peces, proporcionan un modelo para estudiar estos procesos. Muestreamos cuatro sitios tres veces durante la temporada asociada a la Corriente de California y dos veces asociada a la Corriente Ecuatorial Norte utilizando video-transectos en la costa de Zihuatanejo, Guerrero, México para determinar la relación entre las características del hábitat y la estructura de la comunidad de peces. Registramos un total de 26 familias y 54 especies, y estimamos la riqueza y abundancia de peces. Además de medir variables locales del agua como temperatura (°C), salinidad (PPT), pH y oxígeno disuelto (O2%), determinamos la heterogeneidad del hábitat procesando fotografías del sustrato y calculamos la rugosidad usando una cadena. El oxígeno y la temperatura fueron las variables asociadas a las condiciones del agua de mar que diferenciaron los sitios muestreados. La estructura de la comunidad de peces presentó altas correlaciones con la temperatura, salinidad y oxígeno disuelto, seguido por los componentes de la heterogeneidad como rugosidad y diversidad del sustrato. Nuestros resultados mostraron que los cambios estacionales en las condiciones del agua y los componentes físicos en la costa de Zihuatanejo promueven cambios en la estructura de la comunidad de peces. biológicas arrecifes productividad videotransectos video transectos Guerrero 2 5 especies °C, C °C , (°C) PPT, PPT (PPT) O2%, O2 O O2% (O2%) cadena muestreados (°C (PPT (O2% (O2 (O

Resumo Os sistemas costeiros abrangem uma variedade de ecótonos que são importantes para as espécies de peixes, fornecendo diversos micro-habitats e áreas para alimentação, proteção contra predação, reprodução e áreas para recrutamento. No entanto, a maioria desses sistemas enfrenta grandes ameaças de atividades humanas. Considerando os níveis crescentes de perturbação humana nos ecossistemas costeiros, a compreensão das associações peixe-habitat pode fornecer informações importantes sobre os padrões de ocorrência e distribuição de espécies em sistemas afetados pelo homem, que podem apoiar o desenvolvimento de medidas eficazes de conservação e gestão. Neste contexto, investigamos a relação entre os cavalos-marinhos (Hippocampus reidi) e a complexidade do habitat e diferentes espécies de fixação, para determinar a possível variação entre locais e entre estações do ano. Os dados foram obtidos nos recifes rochosos das baías de Guanabara (Praia da Urca) e Sepetiba (Ilha das Duas Irmãs), no sudeste do Brasil, por mergulho livre ao longo de transectos fixos. Os cavalos-marinhos foram contados, e o substrato usado por cada indivíduo foi registrado e identificado como espécie ou atribuído a um grupo morfofuncional. As praias diferiram quanto à composição e grupos morfofuncionais, embora compartilhando alguns grupos morfofuncionais. Os cavalos-marinhos foram mais frequentemente associados a substratos arborescentes/ramificados em ambos os locais, a foliáceos e maciços. A associação com algas foi particularmente encontrada na Urca, enquanto o coral Carijoa riisei na Ilha de Duas Irmãs. peixes microhabitats micro habitats alimentação predação recrutamento entanto humanas peixehabitat peixe homem gestão contexto cavalosmarinhos cavalos marinhos Hippocampus reidi fixação ano Praia Urca Irmãs, Irmãs , Irmãs) Brasil fixos contados morfofuncional morfofuncionais arborescentesramificados arborescentes ramificados maciços

Abstract Coastal systems encompass a range of ecotones that are important for fish species, providing diverse micro-habitats and grounds for foraging, protection from predation, reproduction and areas for recruitment. However, most of these systems face major threats from human activities. Considering the increasing levels of human disturbance in coastal ecosystems, understanding fish-habitat associations may provide important insights into patterns of species occurrence and distribution in human-impacted systems, which can support the development of effective conservation and management measures. In this context, we investigated the relationship between seahorses (Hippocampus reidi) and both habitat complexity and different holdfast species, to determine possible variation between locations and among seasons. Data were obtained from the rocky reefs of Guanabara (Urca Beach) and Sepetiba (Duas Irmãs Island) bays, in southeastern Brazil. Seahorses were counted, and the holdfast being used by each individual was recorded and identified to species or assigned to a morphofunctional group. The beaches differed in holdfast composition and morphofunctional groups, yet sharing some morphofunctional groups. Seahorses were more frequently associated with branching holdfasts at both sites, and also with foliaceous and massive. Association with algae were particularly found in Urca, while the coral Carijoa riisei in Duas Irmãs Island. microhabitats micro habitats foraging predation recruitment However activities ecosystems fishhabitat humanimpacted impacted measures context Hippocampus reidi seasons Urca Beach Island bays Brazil counted group groups sites massive

Abstract. Reef-forming cnidarians are essential for maintaining ecological balance. Unfortunately, coral reefs are endangered due to coral bleaching, which interrupts mutualistic symbiosis between Symbiodiniaceae algae and their coral hosts. Bleaching events result in very high coral mortality and the rapid deterioration of reef structures. Studies aimed at explaining the causes, mechanisms, and consequences of coral bleaching have been mainly conducted with anthozoans, while the impacts of thermal stress responsible for coral bleaching have been scarcely studied in hydrozoans, such as Millepora species (phylum Cnidaria, class Hydrozoa), which are the second most important reef-forming cnidarians. In the present study, the effects of thermal stress caused by the 2015-2016 El Niño on symbiont abundance, exoskeleton structure, and the biochemical composition of Millepora alcicornis were analyzed. Unbleached M. alcicornis specimens exhibited a higher abundance of Breviolum and Durisdinium species, which suggests that unbleached hydrocoral colonies might counteract thermal stress by hosting thermotolerant symbionts of the Durisdinium genus. Bleached hydrocorals exhibited lower levels of calcification than unbleached hydrocorals as well as changes in the microstructure of trabeculae and zooid pores. In contrast, thermal stress did not affect total calcium carbonate and carbohydrate content. Bleached tissues showed significantly higher levels of protein and refractory material, whereas their lipid content decreased considerably. The present study provides evidence that bleached M. alcicornis colonies suffered a decline in calcification and changes in the structure of their exoskeletons after being exposed to the 2015-2016 El Niño. The significant decrease in lipid content suggests that M. alcicornis primarily uses energy stores to maintain vital cellular processes at the expense of calcification.

Resumen. Los cnidarios formadores de arrecifes son esenciales en la ecología marina. Desafortunadamente, están amenazados por el fenómeno de blanqueamiento, el cual rompe la simbiosis mutualista entre algas de la familia Symbiodiniaceae y sus hospederos coralinos. El blanqueamiento causa un alto índice de mortalidad de corales y un rápido deterioro de las estructuras arrecifales. Los estudios dirigidos a explicar causas, mecanismos y consecuencias del blanqueamiento se han realizado principalmente con antozoos, mientras que los impactos del blanqueamiento de corales se han estudiado escasamente en especies de Millepora (phylum Cnidaria, clase Hydrozoa), que son los segundos constructores de arrecifes más importantes. En el presente estudio se analizó el efecto del estrés térmico causado por el evento El Niño 2015-2016 sobre la abundancia de simbiontes, la estructura del exoesqueleto y la composición bioquímica de Millepora alcicornis. Los especímenes sin blanquear de M. alcicornis contenían una mayor abundancia de especies de Breviolum y Durisdinium, lo que sugiere que las colonias de hidrocorales sin blanquear podrían estar contrarrestando el estrés térmico al albergar simbiontes termotolerantes del género Durisdinium. Los hidrocorales blanqueados mostraron niveles más bajos de calcificación y cambios en la microestructura de zooides y trabéculas. En contraste, el estrés térmico no modificó el contenido total de carbonato de calcio y carbohidratos en los hidrocorales. Los tejidos blanqueados mostraron niveles significativamente más altos de proteína y material refractario, mientras que su contenido de lípidos disminuyó considerablemente. El presente estudio muestra que las colonias blanqueadas de M. alcicornis sufrieron una disminución en la calcificación y cambios en la estructura de su exoesqueleto después de estar expuestas al estrés térmico provocado por el evento El Niño 2015-2016. La disminución significativa en el contenido de lípidos sugiere que M. alcicornis está utilizando sus reservas de energía principalmente para mantener sus procesos celulares vitales a expensas de la calcificación.

Resumen Introducción: Las comunidades de macroalgas marinas del Parque Nacional Guanahacabibes no han sido estudiadas desde el punto de vista cuantitativo, a pesar de la influencia que la vegetación submarina tiene sobre la estructura y el funcionamiento de los ecosistemas costeros, componente que hasta ahora ha sido subestimado en la región. Objetivo: Evaluar la variación temporal y espacial de los géneros de macroalgas en dos sitios de María La Gorda, sur del Parque Nacional de Guanahacabibes, y evaluar la salud del arrecife de acuerdo con la cobertura de los diferentes morfo-tipos de macroalgas predominantes. Metodología: El muestreo fue cuatrimestral entre febrero 2014 y marzo 2017 en Yemayá y Laberinto, mediante buceo autónomo a una profundidad de 10 m. La cobertura algal fue estimada siguiendo la metodología AGRRA. Se usaron ocho transectos de 20 m por sitio de muestreo de acuerdo con las condiciones del arrecife y la forma del fondo. Cada cinco metros se colocó un cuadrante de 25 x 25 cm. Se calculó el porcentaje de cobertura que aporta cada género y de los grupos morfofuncionales a la cobertura total. Resultados: Los géneros dominantes durante el periodo de estudio fueron: Dictyota, Lobophora y Halimeda. Las algas carnosas y calcáreas mostraron mayor cubrimiento en Laberinto (carnosas= 57.8 ±15.6; calcáreas = 8.3 ± 6.8) que en Yemayá, (carnosas = 47.3 ± 23.1; calcáreas = 8.5 ± 9.3). Las formas costrosas son más abundantes en Yemayá (17.1 ± 15.1) que en Laberinto (7.7 ± 10). El índice de las carnosas fue superior en Laberinto (225.7 ± 110.2). Conclusión: La disminución en los niveles de cobertura de algas costrosas y la dominancia de formas carnosas como Dictyota y Lobophora en la zona de estudio, evidencian el deterioro en ambos sitios, a pesar de las políticas de conservación de parques nacionales.

Abstract Introduction: The macroalgal communities of the Guanahacabibes National Park have been poorly studied from the quantitative point of view, despite the influence that underwater vegetation has on the structure and functioning of coastal ecosystems, a component that until now has been underestimated in the Cuba region. Objetive: To evaluate the temporal and spatial variation of the macroalgal genera in two sites of María La Gorda, south of the Guanahacabibes National Park, and evaluate the reef health according to the coverage of the different predominant macroalgal morphotypes. Methodology: Sampling took place quarterly between February 2014 and March 2017, in Laberinto and Yemayá by SCUBA diving at a depth of 10 m. The algal coverage was estimated following the AGRRA methodology. Eight 20 m transects per sampling site were used according to reef conditions and bottom shape. Every five meters a 25 x 25 cm square was placed. The coverage (%) contributed per genus and morpho-functional group to the total coverage found was calculated. Results: The dominant genera during the study period were: Dictyota, Lobophora and Halimeda. Fleshy and calcareous algae showed greater coverage in Laberinto (fleshy= 57.8 ± 15.6; calcareous = 8.3 ± 6.8) than in Yemayá (fleshy = 47.3 ± 23.1; calcareous = 8.5 ± 9.3). Crustose algae were more abundant in Yemayá (17.1 ± 15.1) than in Laberinto (7.7 ± 10). The fleshy index was higher in Laberinto (225.7 ± 110.2). Conclusion: The decrease in the levels of crustose algal cover, as well as the dominance of fleshy forms Dictyota and Lobophora in the study area, shows the deterioration in both sites, despite the conservation policies of national parks.

ABSTRACT Background. The recruitment of branching corals in the eastern Pacific is poorly understood despite being of paramount importance to the dynamics of coral populations. Experimental studies provide a non-destructive means to evaluate recruitment and compare settlement materials. Goals. To study Pocillopora recruitment on PVC and terracotta tiles in Bahía Ixtapa-Zihuatanejo (Mexican Pacific). Methods. We deployed 40 square (10 x 10 x 0.5 cm) experimental (20 PVC and 20 unglazed terracotta) tiles arranged as Calcification/Accretion Units at the Islote Zacatoso reef. Results. We observed two coral recruits at the edges of terracotta tiles, presumably due to light availability, and no recruits on horizontal sides, which may have been due to siltation stress, predation, or biofouling. No recruits were found on PVC tiles. Conclusions. Our findings indicate that the coral recruitment is low in the study area and that the terracotta tiles may be a better experimental substrate than PVC tiles to assess pocilloporid coral recruitment in the Mexican Pacific; however, further studies are needed to clarify this assumption.

RESUMEN Antecedentes. El reclutamiento de corales ramificados en el Pacífico oriental tropical está poco documentado, a pesar de la importancia que tiene para entender su dinámica poblacional. Los estudios experimentales proporcionan un medio no destructivo para evaluar el reclutamiento y comparar diferentes materiales. Objetivo. Estudiar el reclutamiento de Pocillopora en placas de PVC y de terracota en Bahía Ixtapa-Zihuatanejo, en el Pacífico mexicano. Métodos. Colocamos 40 placas cuadradas (10 x 10 x 0.5 cm), 20 de PVC y 20 de terracota armadas como Unidades de Calcificación/Acreción en el arrecife Islote Zacatoso. Resultados. Observamos dos reclutas de coral en la orilla de las placas de terracota pero ninguno en los lados horizontales, posiblemente debido a la disponibilidad de luz, el estrés por sedimentación, la depredación, o el sobrecrecimiento por biota incrustante. No encontramos reclutas en ninguna de las placas de PVC. Conclusiones. Nuestros hallazgos indican que el reclutamiento coralino es bajo en la zona de estudio y que las placas de terracota pueden ser un mejor sustrato experimental que las de PVC para evaluar el reclutamiento de corales pociloporidos en el Pacífico mexicano; sin embargo, se necesitan más estudios para corroborar esta suposición.

ABSTRACT Introduction: The Caribbean is the second most polluted sea by debris in the world. Urban waste from this region goes to open dumps and 85% of its wastewater is not treated, arriving a great proportion to the beaches. The Guanahacabibes National Park is Biosphere Reserve and the sea turtles that nest on its beaches are on the Red List of threatened species, also there are fish associated with the coral reef and seabirds in the area. Objective: To determine the risk of ecological impact of debris that end on the “El Holandés” beach of the Guanahacabibes National Park on animal biota. Materials and Methods: The collected debris was quantified and classified by type, possible origin and color. The risk of its ecological impact on animal biota was determined. Results and Discussion: The areas to the east of the camp are more contaminated with the presence of marine debris. White and blue plastic predominated (mainly lids and containers); the number of fragments whose function cannot be identified is large. There is a risk that the plastic material may be swallowed by sea turtles, birds and fish by being confused with food or hinder their normal behavior. The presence of sargassum in large quantities is a source of entry of marine debris. Conclusions: The importance of carrying out the systematic collection of marine debris is corroborated, since it is risky for the life of sea turtles, fish and birds. There is a base line for a longitudinal study.

RESUMEN Introducción: El Caribe es el segundo mar más contaminado por basura del mundo. Los residuos urbanos de esta región van a basureros a cielo abierto y el 85% de sus aguas residuales no son tratadas, arribando gran parte de estas a las playas. El Parque Nacional Guanahacabibes de Cuba es Reserva de la Biosfera y las tortugas marinas que anidan en sus playas están en la Lista Roja de especies amenazadas, existiendo peces asociados al arrecife coralino y aves marinas en el área. Objetivo: Determinar el riesgo de impacto ecológico de basura recalada en la playa “El Holandés” del Parque Nacional Guanahacabibes sobre la biota animal. Materiales y Métodos: La basura recolectada se cuantificó y clasificó por tipología, posible origen y color. Se determinó el riesgo de su impacto ecológico sobre la biota animal. Resultados y Discusión: Las áreas al este del campamento están más contaminadas. Predomina plástico blanco y azul (fundamentalmente tapas y envases); el número de fragmentos cuya función no fue identificada es grande. Existe riesgo de que el material plástico sea ingerido por tortugas marinas, aves y peces al ser confundidos con alimentos u obstaculice su comportamiento normal. La presencia de sargazo en grandes cantidades es una fuente de entrada de basura marina. Conclusiones: Se corrobora la importancia de realizar la recogida sistemática de basura marina, al ser riesgosa para la vida de tortugas marinas, peces y aves. Se cuenta con una línea base para un estudio longitudinal.