Oceanographical-driven dispersal and environmental variation explain genetic structure in an upwelling coastal ecosystem.

The seascape comprises multiple environmental variables that interact with species biology to determine patterns of spatial genetic variation. The environment imposes spatially variable selective forces together with homogenizing and diverging drivers that facilitate or restrict dispersal, which is a complex, time-dependent process. Understanding how the seascape influences spatial patterns of genetic variation remains elusive, particularly in coastal upwelling systems. Here, we combine genome-wide SNP data, Lagrangian larval dispersal simulated over a hydrodynamic model, and ocean environmental information to quantify the relative contribution of ocean circulation and environmental heterogeneity as drivers of the spatial genetic structure of two congeneric intertidal limpets, Scurria scurra and S. araucana, along the central coast of Chile. We find that a genetic break observed in both limpet species coincides with a break in connectivity shown by the Lagrangian dispersal, suggesting that mean ocean circulation is an important seascape feature, in particular for S. scurra. For S. araucana, environmental variation appears as a better predictor of genetic structure than ocean circulation. Overall, our study shows broad patterns of seascape forcing on genetic diversity and contributes to our understanding of the complex ecological and evolutionary interactions along coastal upwelling systems.

Zooplankton variability and possible oceanographic anomalies from 1996 to 2009 on the south coast of Brazil.

The analysis of 14 years of sampling data on the zooplankton community in southern Brazil showed a tendency toward increased density and reduced species richness. This behavior could be a response to a prolonged period of negative sea surface temperature (SST) anomalies in the Pacific Ocean and the ENSO phenomenon. The persistence of the La Niña phenomenon between 2001 and 2008 was associated with a higher incidence of stress from southwest winds and a greater reach of the front of the La Plata River plume, with possible responses being lower temperatures in the summer/autumn and lower salinities in the winter/spring in the study area. Under these conditions, one response in the zooplankton community was larger copepod domains. This group was responsible for specific changes in the community, with an increase in the population of Acartia tonsa while populations of species with more thermophilic characteristics showed a decrease. It cannot be disregarded, however, that possible interactions between different abiotic and biotic forces acting in the environment may have influenced the structure of the community. It remains unknown whether a new steady state has been established in the environment or whether there has been a return to initial conditions.

Glacial meltwater input to the ocean around the Antarctic Peninsula: forcings and consequences.

The Antarctic region has experienced recent climate and environmental variations due to climate change, such as ice sheets and ice shelves loss, and changes in the production, extension, and thickness of sea-ice. These processes mainly affect the freshwater supply to the Southern Ocean and its water masses formation and export, being crucial to changes in the global climate. Here, we review the influence of the glacial freshwater input on the Antarctic Peninsula adjacent ocean. We highlight each climate process' relevance on freshwater contribution to the sea and present a current overview of how these processes are being addressed and studied. The increase of freshwater input into the ocean carries several implications on climate, regionally and globally. Due to glacier melting, the intrusion of colder and lighter water into the ocean increases the stratification of the water column, influencing the sea-ice increase and reducing ocean-atmosphere exchanges, affecting the global water cycle. This study shows the role of each hydrological cycle processes and their contributions to the regional oceanography and potentially to climate.

High levels of connectivity over large distances in the diadematid sea urchin Centrostephanus sylviae.

Most benthic marine invertebrates with sedentary benthic adult phases have planktonic larvae that permit connectivity between geographically isolated populations. Planktonic larval duration and oceanographic processes are vital to connecting populations of species inhabiting remote and distant islands. In the present study, we analyzed the population genetic structure of the sea urchin Centrostephanus sylviae, which inhabits only the Juan Fernández Archipelago and the Desventuradas islands, separated by more than 800 km. For 92 individuals collected from Robinson Crusoe and Selkirk Islands (Juan Fernández Archipelago) and San Ambrosio Island (Desventuradas Islands), 7,067 single nucleotide polymorphisms (SNPs) were obtained. The results did not show a spatial genetic structure for C. sylviae; relative high migration rates were revealed between the islands. An analysis of the water circulation pattern in the area described a predominant northward water flow with periods of inverted flow, suggesting that larvae could move in both directions. Overall, this evidence suggests that C. sylviae comprises a single large population composed of individuals separated by more than 800 km.

Respuestas del mesozooplancton a condiciones oceanográficas en diferentes escalas en Bahía Salinas, Pacífico Norte de Costa Rica, durante 2011-2013 / Mesozooplankton responses to oceanographic conditions across different scales in Salinas Bay, Northern Pacific coast of Costa Rica during 2011-2013

Introducción: El Pacífico Norte de Costa Rica se caracteriza por presentar una variación de la temperatura subsuperficial del mar (TSSM) modulada por vientos superficiales de componente este, con variaciones estacionales e intra-estacional. La TSSM es fundamental para las interacciones de la interfase océano-atmósfera y de gran influencia en los procesos biológicos marinos. Los estudios de zooplancton en el Pacífico Norte son escasos y se han enfocado en la composición, abundancia y biomasa de macro y mesozooplanctonen en Bahía Culebra. No se han realizado trabajos sobre zooplancton al norte del Golfo de Papagayo. Objetivo: Analizar la variación del zooplancton de Bahía Salinas a diferentes escalas como respuesta a condiciones oceanográficas-atmosféricas. Métodos: durante algunos meses de los años 2011, 2012 y 2013, el mesozooplancton fue muestreado en siete estaciones siguiendo un gradiente costero-oceánico para determinar su abundancia, biomasa y composición de la comunidad. Se realizaron lances de CTD en cada estación, y se recopilaron datos horarios de la TSSM desde junio de 2003 a diciembre de 2017. Resultados: La temperatura superficial anual en Bahía Salinas es menor en diciembre-abril con un mínimo secundario en julio y mayor en mayo-junio, y agosto-octubre. Los eventos fríos, neutros y cálidos determinados por anomalías en la TSSM, presentaron una distribución de la temperatura en la columna de agua con estratificación horizontal, de mezcla vertical y homogénea, respectivamente. La distribución espacial del zooplancton no presentó diferencias significativas y la variación del promedio total de abundancia y biomasa mostró un comportamiento similar durante el período de estudio, con menor variación en el primer año en comparación con el segundo, siendo los copépodos la categoría predominante para todas las fechas. A escala estacional no se observó un patrón general de variación entre estación seca y lluviosa y, copépodos y otros grupos del zooplancton fueron las categorías que presentaron diferencias. A escala intra-estacional la abundancia y biomasa presentaron una relación inversa con la TSSM y se vieron afectadas de manera diferencial. Los copépodos y zooplancton gelatinoso se diferenciaron en todos los eventos. Conclusiones: El zooplancton de Bahía de Salinas responde de manera diferencial en las diferentes escalas a las condiciones climáticas que afectan la TSSM de la región. La clasificación de las fechas de muestreo en eventos permite caracterizar diferentes perfiles en la columna de agua, así como permite definer patrones de variación para el mesozooplancton, que refleja la adaptación a corto plazo en función de la variación de las condiciones ambientales. El conocimiento generado ayuda a comprender mejor los fenómenos oceanográficos y su efecto sobre las poblaciones de plancton y la biota en general, especialmente en el escenario de cambio climático y las manifestaciones modernas de su impacto, p. e. la acidificación oceánica y pérdida de biodiversidad marina.

Introduction: The North Pacific of Costa Rica is characterized by presenting a variation of the subsurface temperature of the sea (SSST) modulated by surface winds with east component, with seasonal and intra-seasonal variations. The SSST is fundamental for the interactions of the ocean-atmosphere interface and influence marine biological processes. Zooplankton studies in the North Pacific are scarce and have been focused on the composition, abundance and biomass of macro and mesozooplankton in Culebra Bay. No works on zooplankton has been carried out northward of Papagayo Gulf. Objective: To analyze the variation of the zooplankton in Bahía Salinas at different scales in response to oceanographic-atmospheric conditions. Methods: during 2011, 2012 and 2013, mesozooplankton was collected in seven stations following a coastal-ocean gradient to determine abundance, biomass, and community composition. CTD casts were also carried out in each station. Hourly data of the Sea Subsurface Temperature (SSST) were obtained from June 2003 to December 2017. Results: The annual surface temperature in Bahía Salinas was lower in December-April with a secondary minimum in July and higher in May-June and August-November. The cold, neutral and warm events determined by anomalies in the SSST, presented a distribution of the temperature in the water column with horizontal stratification, vertical mixture and homogeneous, respectively. The spatial distribution of zooplankton did not show significant differences and the variation of the total average abundance and biomass showed a similar behavior during the study period, with less variation in the first year compared to the second one, being the copepods the predominant category for all the dates. On a seasonal scale, a general pattern of variation between dry and rainy seasons was not observed, and copepods and others zooplankton groups were the categories that presented differences. On an intra-seasonal scale, abundance and biomass showed an inverse relationship with SST. Copepods and gelatinous zooplankton (GZ) were differentiated in all events. Conclusions: The zooplankton of Bahía Salinas respond differentially at different scales to the climatic conditions that affect the SSST of the region. The classification of the sampling dates into events allows characterizing different profiles in the water column it also allows to define the variation patterns for mesozooplankton that reflects short-term adaptation as a function of variation in environmental conditions. These findings help to understand how oceanographic processes determine plankton community composition and biota in general. This is relevant in times of climate change and the manifestation of its impact through processes such as ocean acidification and loss of marine biodiversity.

Simulación de oleaje en los alrededores de la Isla del Coco, Costa Rica / Numerical simulation of wave field around Cocos Island, Costa Rica

Introducción: La Isla del Coco por su ubicación en el océano Pacífico y en aguas profundas, periódicamente arriban olas energéticas que se originan en el Océano del Sur. La isla actúa como un abrigo disipando parte de la energía de las olas que llegan a la costa pacífica de Costa Rica. Objetivo: El objetivo del trabajo es caracterizar las condiciones generales del oleaje a través de la simulación numérica del oleaje en el Pacífico Tropical del Este (PTE), con especial interés en la Isla del Coco. Métodos: Las olas se propagan con el modelo espectral de oleaje WAVEWATCH III. Se usa en el modelo una malla no estructurada. Se utilizan dos años (2007-2008) de datos históricos de oleaje como condiciones de frontera obtenidos de reanálisis con el modelo WAVEWATCH generado por el Instituto Francés para la Investigación del Mar (IFREMER por sus siglas en francés). Se obtienen mapas anuales y estacionales y series temporales de la altura significante de la ola, periodo y dirección asociado al pico del espectro de energía. Resultados: Los resultados mostrados son similares a otros estudios previos de simulación y observación. El campo de oleaje es caracterizado por periodos largos y dirección desde suroeste en promedio. Las condiciones de oleaje sobre la isla obedecen a los sistemas extratropicales de ambos hemisferios y a procesos locales en el PTE. Conclusiones: El modelo de olas WAVEWATCH III mostró que representa las condiciones típicas de oleaje en los alrededores de la Isla del Coco. Es el primer trabajo de simulación de oleaje aplicando una malla no convencional en la zona económica exclusiva de Costa Rica. El estudio sirve como base para extenderse a otras áreas específicas de la costa.

Introduction: Periodically energetic waves, originated in the Southern Ocean, arrive to Cocos Island, because of its location in the Pacific Ocean and in deep waters. The island acts as a shelter dissipating part of the energy of the waves that reach the Pacific coast of Costa Rica. Objetive: The objective of the work is to characterize the general conditions of the swell through the numerical simulation of the swell in the Eastern Tropical Pacific (ETP), with special interest in Cocos Island. Methods: The waves are propagated with the WAVEWATCH III wave spectral model. An unstructured mesh is used in the model. Two years (2007-2008) of hindcast data are used as boundary conditions obtained from reanalysis with the WAVEWATCH model, generated by the French Institute for Marine Research (IFREMER for its acronym in French). Annual and seasonal maps and time series of significant wave height, peak period and peak wave direction are obtained. Results: The results shown are similar to other previous simulation and observation studies. The mean wave field is characterized by long periods from southwest direction. The wave conditions on the island obey the extratropical systems of both hemispheres and local processes in the PTE. Conclusions: The WAVEWATCH III wave model showed that it represents the typical wave conditions in the surroundings of Cocos Island. It is the first wave simulation work applying an unconventional mesh in the exclusive economic zone of Costa Rica. The study serves as a basis for extending to other specific areas of the coast.

"Uma dádiva das marés": os estudos sobre manguezais da cientista Marta Vannucci em sua trajetória internacional, 1969-1989 / "A gift of the tides: "studies of mangroves by the scientist Marta Vannucci in her international trajectory, 1969-1989

Resumo Marta Vannucci é considerada uma das mais importantes cientistas brasileiras. O artigo explora a trajetória internacional da pesquisadora, destacando sua atuação na Organização das Nações Unidas para a Educação, a Ciência e a Cultura (Unesco) no âmbito do projeto regional sobre mangues na Ásia e no Pacífico. Produto da sua atuação nesse programa, a autora publicou Os manguezais e nós, que é objeto de análise crítica neste artigo.

Abstract Marta Vannucci is held to be one of Brazil's most important scientists. Her international trajectory is explored, highlighting her work with the United Nations Educational, Scientific and Cultural Organization (Unesco) in the ambit of the regional project on mangroves in Asia and the Pacific. As a result of her work for this program, Vannucci published The mangroves and us, which is the object of critical analysis in this article.

Salinity and stable oxygen isotope relationship in the Southwestern Atlantic: constraints to paleoclimate reconstructions.

Stable isotopes have been widely used in the literature both to discuss current ocean circulation processes, as well as to reconstitute paleoceanographic parameters. The distribution of oxygen and deuterium stable isotopes in seawater (δ18Osw and δDsw) at the Western Tropical South Atlantic border was investigated to better understand the main fractionation processes of these isotopes and establish a regional salinity and δ18Osw relation to improve the paleoceanographic knowledge in the region. This study was conducted during a quasi-synoptic oceanographic cruise in which 98 discrete seawater samples were collected in the core of the main water masses for stable isotope analysis. A strong correlation between δ18Osw and δD was found, which made it possible to extrapolate the results for δ18Osw to δD. Although it was not possible to distinguish the water masses based only on their isotopic signatures, the water masses had a strong salinity and δ18Osw relation, and compared with previous studies, a seasonal pattern was observed. Paleosalinity differences of up to 0.2 psu between Summer and Winter are reported. Considering the limitations of the current techniques to seasonally separate the samples for the paleoceanographic studies, an intermediate Mixing Line for the Tropical South Atlantic (SSS = 1.942* δ18Osw + 34.56) was proposed to reduce the estimated errors associated with these seasonal variations.

The impact of fishing on a highly vulnerable ecosystem, the case of Juan Fernández Ridge ecosystem.

The Juan Fernández Ridge (JFRE) is a vulnerable marine ecosystem (VME) located off the coast of central Chile formed by the Juan Fernández Archipelago and a group of seamounts. This ecosystem has unique biological and oceanographic features, characterized by: small geographical units, high degree of endemism with a high degree of connectivity within the system. Two fleets have historically operated in this system: a long term coastal artisanal fishery associated with the Islands, focused mainly on lobster, and a mainland based industrial demersal finfish fishery operating on the seamounts which is currently considered overexploited. The management of these fisheries has been based on a classical single-species approach to determine output controls (industrial fleet) and a mixed management system with formal and informal components (artisanal fleet). There has been growing interest in increasing the exploitation of fisheries, and modernization of the fishing fleet already operating in the JFRE. Under this scenario of increased levels of fishing exploitation and the high level of interrelation of species it might be necessary to understand the impact of these fisheries from a holistic perspective based on a ecosystem-based modeling approach. To address these challenges we developed an Atlantis end-to-end model was configured for this ecosystem. The implemented model has a high degree of skill in representing the observed trends and fluctuations of the JFRE. The model shows that the industrial fishing has a localized impact and the artisanal fisheries have a relatively low impact on the ecosystem, mainly via the lobster fishery. The model indicates that the depletion of large sized lobster has leads to an increase in the population of sea urchins. Although this increase is not sufficient, as yet, to cause substantial flow-on effects to other groups, caution is advised in case extra pressure leads the ecosystem towards a regime shift.

Influence of oceanographic and meteorological events on the quantity and quality of marine debris along an estuarine gradient.

The influence of three meteorological/oceanographic conditions - frontal systems (FS), high riverine discharges (HRD) and regular weather conditions (RWC) - over the quantity (Overall Abundance and Richness of types) and quality (composition and most probable source) of marine debris was assessed in sand beaches along three sectors (internal, I; median, M; and external, E) of an estuarine gradient. The highest overall abundance and richness of types were observed in HRD (I and E), while the lowest were observed in RWC (I and M). The external sector showed lowest abundance in FS. Greatest numbers of "domestic" and "sewage related debris" were observed under HRD (I > E > M). Greatest numbers of "fisheries" items were observed in HRD (I and E). For "unknown" sourced items, there was no indication of a single condition with smaller quantities (E > I = M). Results suggest that adopting oceanographical and meteorological conditions for analysis have the potential to detect temporal variations.

Variation in species diversity of deep-water megafauna assemblages in the Caribbean across depth and ecoregions.

Diversity patterns of the deep-sea megafauna in the Caribbean Basin and the Guiana ecoregion were analyzed in order to test the hypothesis of species richness variation as a function of depth and the hypothesis of non-differences between ecoregions by analyzing spatial patterns of five taxa and a merged assemblage. Collections of five taxa (corals, sea stars, sea urchins, sea lilies and gastropods) were obtained from seven oceanographic expeditions aboard the R/V Pillsbury at 310 stations between 60 and 7500 m depth. Data were sorted according to depth zones and ecoregions and were analyzed in order to estimate species richness, changes in species composition and distinction of ß-diversity by species turnover or by nestedness. The observed patterns of diversity were consistent between taxa and their assemblage: Species richness increased from the continental shelf (60-200 m deep) to the slope (200-2000 m deep), followed by a decrease at the continental rise-abyssal zone. We detected marked changes in species composition according to depth ranges. Changes in species composition in relation to ecoregions were also detected. In general, the Caribbean Basin lacks important physical barriers, causing high deep-sea ecosystem connectivity; however, variation in composition could be related to changes in environmental conditions associated with productivity and/or continental influences.

The Eastern Tropical Pacific coral population connectivity and the role of the Eastern Pacific Barrier.

Long-distance dispersal is believed to strongly influence coral reef population dynamics across the Tropical Pacific. However, the spatial scale and strength at which populations are potentially connected by dispersal remains uncertain. To determine the patterns in connectivity between the Eastern (ETP) and Central Tropical Pacific (CTP) ecoregions, we used a biophysical model incorporating ocean currents and larval biology to quantify the seascape-wide dispersal potential among all population. We quantified the likelihood and determined the oceanographic conditions that enable the dispersal of coral larvae across the Eastern Pacific Barrier (EP-Barrier) and identified the main connectivity pathways and their conservation value for dominant reef-building corals. Overall, we found that coral assemblages within the CTP and ETP are weakly connected through dispersal. Although the EP-Barrier isolates the ETP from the CTP ecoregion, we found evidence that the EP-Barrier may be breached, in both directions, by rare dispersal events. These rare events could explain the evolutionary genetic similarity among populations of pocilloporids in the ecoregions. Moreover, the ETP may function as a stronger source rather than a destination, providing potential recruits to CTP populations. We also show evidence for a connectivity loop in the ETP, which may positively influence long-term population persistence in the region. Coral conservation and management communities should consider eight-key stepping stone ecoregions when developing strategies to preserve the long-distance connectivity potential across the ETP and CTP.

Spatial variability of zooplankton community structure in Colombian Caribbean waters during two seasons / Variabilidad espacial de la estructura comunitaria del zooplancton en aguas oceánicas del Caribe colombiano durante dos estaciones

Abstract Zooplankton is an important component to understand oceanographic dynamics, they are considered good indicators of environmental variability, since most species are short-lived they can be tight coupling of climate and population dynamics, and some taxa are sensitive to variables such as temperature, quality and quantity of food, oxygenation and stratification. In the Colombian Caribbean two oceanographic cruises were carried out, in order to characterize and analyze the biodiversity of the continental margin, for the periods May-June 2008 and November-December 2009. The objective of this study was to determine which oceanographic variable was the most important in the distribution of zooplankton in the oceanic waters, and how the variables structure the community. In each cruise, zooplankton samples were obtained by vertical hauls with a 1 m2 diameter conical net (200 μm mesh size). The zooplankton community structure was studied by automated image analysis (ZooImage), which combined with abundance data, allowed to calculate the slope of size spectrum, and diversity indexes of taxa and sizes. The environmental variables included temperature, salinity, oxygen and chlorophyll a of the water column, and were used to calculate the stratification with the Brunt-Vaiisala frequency; this information was complemented by satellite images of temperature, surface chlorophyll, geostrophic currents and sea level, obtained from MODIS and AQUA products. The association between environmental variables and the zooplankton community structure was determined using Spearman's correlation ranges with the Bioenv routine and a stepwise regression model, and Principal component analysis (PCA). Our results showed spatial and temporal patterns in the oceanographic conditions of the study area, such as upwelling in the Northeast region, strong stratification in the Southwest, and mesoscale activity. The abundance of zooplankton exhibited differences between the two climatic seasons and zones. Temporal differences were also evident in the size and diversity of taxa (ANOVA 2-way p <0.05). These changes were related to the moderate upwelling and the activity of mesoscale eddies. Cyclonic and anticyclonic eddies of variable size can either transport or retain zooplankton over cross-shelf and oceanic areas, thus modifying the taxonomic structure of the community. According to the Bioenv analysis, the main variables that explained the abundance and composition of zooplankton were sea level and chlorophyll a (Spearman correlation = 0.49). The stepwise regression showed that stratification, oxygen and chlorophyll a were the most important predictors of zooplankton abundance and size. Rev. Biol. Trop. 66(2): 688-708. Epub 2018 June 01.

Resumen El zooplancton es un componente importante para entender la dinámica oceanográfica, es considerado un buen indicador de la variabilidad ambiental, ya que la mayoría de las especies tienen ciclos de vida cortos, por lo que puede haber un estrecho acoplamiento entre el clima y la dinámica de la población, algunos grupos son sensibles a variables como la temperatura, calidad y cantidad de alimento, oxigenación y estratificación. En el Caribe colombiano dos cruceros oceanográficos durante Mayo-Junio 2008 y Noviembre-Diciembre 2009 fueron realizados con el fin de caracterizar y analizar la biodiversidad del margen continental del Caribe colombiano. El objetivo de este estudio fue determinar qué variable oceanográfica es la más importante en la distribución del zooplancton en las aguas oceánicas del Caribe colombiano y de qué forma estas variables estructuran la comunidad. En cada crucero se obtuvieron muestras de zooplancton mediante arrastres verticales con una red cónica de 1 m de diámetro de boca y 200 µm de ojo de malla. La estructura comunitaria del zooplancton se estudió mediante el análisis automatizado de imágenes (ZooImage) el que combinado con datos de abundancia permitió calcular la pendiente del espectro de tamaño de la comunidad e índices de diversidad de taxa y tamaños. Las variables ambientales (temperatura, salinidad, oxígeno y clorofila a de la columna de agua) se obtuvieron desde los mismos cruceros y se utilizaron para calcular la estratificación mediante la frecuencia Brunt-Vaisala. Esta información in situ se complementó con imágenes satelitales de temperatura, clorofila superficial, corrientes geostróficas y nivel del mar, obtenidas de los productos MODIS y AQUA. La asociación entre variables ambientales y la estructura comunitaria del zooplancton se determinó mediante rangos de correlación de Spearman con la rutina Bioenv y un modelo de regresión paso a paso. El análisis de componentes principales (PCA) permitió observar patrones espaciales y temporales en las condiciones oceanográficas del área de estudio, tales como surgencia en la región Nororiental, fuerte estratificación en la Suroccidental y actividad de remolinos de mesoescala. La abundancia del zooplancton mostró diferencias entre las dos estaciones climáticas y entre las zonas. Diferencias temporales también fueron evidentes en el tamaño y diversidad de taxa (ANOVA 2-vías P < 0.05). Estos cambios se relacionaron con la surgencia moderada y la actividad de los remolinos de mesoescala. Los remolinos ciclónicos y anticiclónicos de tamaño variable pueden transportar o retener el zooplancton sobre áreas cruzadas y oceánicas, modificando así la estructura taxonómica de la comunidad. Según el análisis Bioenv las principales variables que explicaron la abundancia y composición del zooplancton fueron el nivel del mar y la clorofila a (correlación de Spearman = 0.49). El modelo de regresión paso a paso mostró que la estratificación, el oxígeno y la clorofila a son los predictores mas importantes para la abundancia y el tamaño del zooplancton.

Larval dispersal in three coral reef decapod species: Influence of larval duration on the metapopulation structure.

Most coral-associated decapod species have non-migratory adult populations and depend on their planktonic larvae for dispersal. This study examined the metapopulation structure of three decapod species with different pelagic larval duration (PLD) from twelve coral reef complexes of the Gulf of Mexico. The dispersion of larvae was analyzed through the use of a realistic numerical simulation of the Gulf of Mexico with the Hybrid Coordinate Ocean Model. To study the transport and dispersion of particles in near-surface waters, a particle-tracking subroutine was run using as input the currents from the model. The simulation consisted of the launch of 100 passive particles (virtual larvae) every 24 hours from each reef throughout five years, and tracked for as long as 210 days. Results indicated that species with a short PLD, Mithraculus sculptus (PLD 8‒13 days), had a weak connection among the reefs, but higher self-recruitment, especially on the narrow western shelf. The species with a longer PLD, Dromia erythropus (28‒30 days), had a stronger connection among neighboring reefs (< 300 km). Finally, the species with an even longer PLD, Stenopus hispidus (123‒210 days), had a wider potential distribution than the other species. Circulation on synoptic, seasonal and interannual scales had differential effects on the larval dispersal of each species. The metapopulation structure of M. sculptus and D. erythropus seemed to combine features of the non-equilibrium and the patchy models, whereas that of S. hispidus presumably fit to a patchy model. These findings support previous observations that indicate that species with longer PLD tend to occupy larger areas than species with short PLD, although recruitment of juveniles to the adult populations will also depend on other factors, such as the availability of suitable habitats and the ability to colonize them.

Contemporary and historical oceanographic processes explain genetic connectivity in a Southwestern Atlantic coral.

Understanding connectivity patterns has implications for evolutionary and ecological processes, as well as for proper conservation strategies. This study examined population genetic structure and migration patterns of the coral Mussismilia hispida, one of the main reef builders in the Southwestern Atlantic Ocean. For this, 15 sites were sampled along its entire distributional range employing 10 microsatellite loci. M. hispida was divided into five genetically differentiated populations by Structure analysis. Population structure and migration estimates are consistent with present-day oceanographic current patterns, zones of upwelling and historical sea-level changes. The Central Region and Oceanic Islands populations had the highest genetic diversity, were possibly the main sources of migrants for other populations and presented mutual migrant exchange. This mutual exchange and the high diversity of Oceanic Islands, a peripherical population, is highly interesting and unexpected, but can be explained if these sites acted as refugia in past low sea-level stance. This is the first connectivity study in the region using hyper-variable markers and a fine sampling scale along 3,500 km. These results enlighten the population dynamics of an important reef building species and shows how oceanographic processes may act as barriers to dispersal for marine species, providing valuable information for management strategies.

Dynamic oceanography determines fine scale foraging behavior of Masked Boobies in the Gulf of Mexico.

During breeding, foraging marine birds are under biological, geographic, and temporal constraints. These contraints require foraging birds to efficiently process environmental cues derived from physical habitat features that occur at nested spatial scales. Mesoscale oceanography in particular may change rapidly within and between breeding seasons, and findings from well-studied systems that relate oceanography to seabird foraging may transfer poorly to regions with substantially different oceanographic conditions. Our objective was to examine foraging behavior of a pan-tropical seabird, the Masked Booby (Sula dactylatra), in the understudied Caribbean province, a moderately productive region driven by highly dynamic currents and fronts. We tracked 135 individuals with GPS units during May 2013, November 2013, and December 2014 at a regionally important breeding colony in the southern Gulf of Mexico. We measured foraging behavior using characteristics of foraging trips and used area restricted search as a proxy for foraging events. Among individual attributes, nest stage contributed to differences in foraging behavior whereas sex did not. Birds searched for prey at nested hierarchical scales ranging from 200 m-35 km. Large-scale coastal and shelf-slope fronts shifted position between sampling periods and overlapped geographically with overall foraging locations. At small scales (at the prey patch level), the specific relationship between environmental variables and foraging behavior was highly variable among individuals but general patterns emerged. Sea surface height anomaly and velocity of water were the strongest predictors of area restricted search behavior in random forest models, a finding that is consistent with the characterization of the Gulf of Mexico as an energetic system strongly influenced by currents and eddies. Our data may be combined with tracking efforts in the Caribbean province and across tropical regions to advance understanding of seabird sensing of the environment and serve as a baseline for anthropogenic based threats such as development, pollution, and commercial fisheries.

Changes in Microbial Plankton Assemblages Induced by Mesoscale Oceanographic Features in the Northern Gulf of Mexico.

Mesoscale circulation generated by the Loop Current in the Northern Gulf of Mexico (NGOM) delivers growth-limiting nutrients to the microbial plankton of the euphotic zone. Consequences of physicochemically driven community shifts on higher order consumers and subsequent impacts on the biological carbon pump remain poorly understood. This study evaluates microbial plankton <10 µm abundance and community structure across both cyclonic and anti-cyclonic circulation features in the NGOM using flow cytometry (SYBR Green I and autofluorescence parameters). Non-parametric multivariate hierarchical cluster analyses indicated that significant spatial variability in community structure exists such that stations that clustered together were defined as having a specific 'microbial signature' (i.e. statistically homogeneous community structure profiles based on relative abundance of microbial groups). Salinity and a combination of sea surface height anomaly and sea surface temperature were determined by distance based linear modeling to be abiotic predictor variables significantly correlated to changes in microbial signatures. Correlations between increased microbial abundance and availability of nitrogen suggest nitrogen-limitation of microbial plankton in this open ocean area. Regions of combined coastal water entrainment and mesoscale convergence corresponded to increased heterotrophic prokaryote abundance relative to autotrophic plankton. The results provide an initial assessment of how mesoscale circulation potentially influences microbial plankton abundance and community structure in the NGOM.

Phytoplankton adapt to changing ocean environments.

Model projections indicate that climate change may dramatically restructure phytoplankton communities, with cascading consequences for marine food webs. It is currently not known whether evolutionary change is likely to be able to keep pace with the rate of climate change. For simplicity, and in the absence of evidence to the contrary, most model projections assume species have fixed environmental preferences and will not adapt to changing environmental conditions on the century scale. Using 15 y of observations from Station CARIACO (Carbon Retention in a Colored Ocean), we show that most of the dominant species from a marine phytoplankton community were able to adapt their realized niches to track average increases in water temperature and irradiance, but the majority of species exhibited a fixed niche for nitrate. We do not know the extent of this adaptive capacity, so we cannot conclude that phytoplankton will be able to adapt to the changes anticipated over the next century, but community ecosystem models can no longer assume that phytoplankton cannot adapt.