Repositorio Nacional

El estudio de la dispersión de materia flotante en el océano es fundamental para abordar problemas contemporáneos, como la contaminación por desechos y la distribución de nutrientes. Sin embargo, la distribución superficial horizontal no captura completamente la complejidad del problema, ya que muchos contaminantes, incluidos los plásticos, tienden a hundirse debido a la desintegración o a la adhesión de materiales que alteran su densidad. Este estudio se centra en la dispersión horizontal y vertical de trazadores pasivos en un océano turbulento impulsado por el viento. Se utilizan partículas sintéticas que son advectadas por un modelo Lagrangiano resolviendo la trayectoria de cada partícula mediante un método Runge-Kutta de 4 ◦ orden. Se exploran cuatro mecanismos de dispersión: (i) corrientes geostróficas a gran escala según el modelo clásico de Stommel, (ii) velocidad de Ekman, (iii) difusividad turbulenta debida a movimientos de submesoescala (simulados con una caminata aleatoria), y (iv) efectos inerciales relacionados con el tamaño y la flotabilidad del trazador. El estudio se divide en dos partes: primero, se examina la dispersión horizontal en superficie, y después se aborda el caso tridimensional mediante la inmersión de trazadores por bombeo de Ekman. Los principales resultados son: 1) con la deriva superficial de Ekman, las partículas convergen hacia una región alrededor del centro del giro de Stommel; sin embargo, dicha convergencia disminuye a medida que aumentan los efectos de la turbulencia; 2) considerando los efectos inerciales, aumentar la flotabilidad o el tamaño de las partículas provoca una convergencia mayor que la producida por la deriva de Ekman; 3) al incluir la velocidad vertical negativa, una baja difusividad turbulenta permite que los trazadores alcancen mayores profundidades porque permanecen más tiempo en regiones de mayor hundimiento.

The study of floating material dispersion in the ocean is crucial for addressing contemporary issues such as waste pollution and nutrient distribution. However, the horizontal surface distribution does not fully capture the complexity of the problem. Many pollutants, including plastics, tend to sink due to the disintegration or adhesion of materials altering their density. This study focuses on the horizontal and vertical dispersion of passive tracers in a turbulent, wind-driven ocean. Synthetic particles are advected using a Lagrangian model, with each particle’s trajectory solved using a fourth-order Runge-Kutta method. Four dispersion mechanisms are explored: (i) large-scale geostrophic currents based on the Stommel’s classical model, (ii) Ekman velocity, (iii) turbulent diffusivity due to submesoscale motions (simulated with a random walk), and (iv) inertial effects related to the tracer’s size and buoyancy. The study is divided into two parts: first, horizontal dispersion at the surface is examined, and then the three-dimensional scenario is addressed by immersing tracers through Ekman pumping. The key findings are as follows: 1) with surface Ekman drift, particles converge around the center of the Stommel gyre; however, this convergence decreases as turbulence effects increase; 2) considering inertial effects, increasing buoyancy or particle size results in greater convergence than that caused by Ekman drift; 3) when the vertical velocity is included, a low turbulent diffusivity allows tracers to reach greater depths because they remain longer times in regions of greater sinking.

circulación de Stommel, deriva de Ekman, partículas inerciales, dispersión de partículas, bombeo de Ekman Stommel circulation, Ekman drift, inertial particles, particle dispersion, Ekman pumping CIENCIAS FÍSICO MATEMÁTICAS Y CIENCIAS DE LA TIERRA CIENCIAS DE LA TIERRA Y DEL ESPACIO OCEANOGRAFÍA OCEANOGRAFÍA FÍSICA (VE R 5603 .04) OCEANOGRAFÍA FÍSICA (VE R 5603 .04)

Expansión poblacional reciente en la historia evolutiva de la anchoveta de California Engraulis mordax

Recent population expansion in the evolutionary history of the Californian anchovy Engraulis mordax

NOE DIAZ VILORIA LAURA SANCHEZ VELASCO RICARDO PEREZ ENRIQUEZ (2012, [Artículo])

"La anchoveta de California Engraulis mordax, es una especie templada que pudo haber pasado por un proceso de disyunción poblacional, debido al proceso postglacial de calentamiento del agua alrededor de la punta de la península de Baja California, hace unos 10,000 años. Se realizó un análisis genético para probar la hipótesis nula de homogeneidad genética entre el Golfo de California, México y el sur de California, EUA y si este era el caso, estimar el tiempo de surgimiento de haplotipos en términos de coalescencia. Se analizaron en total 80 secuencias de la región control hipervariable (ADNmt) de E. mordax, capturadas en la región central del Golfo de California (n = 40) y el sur de California (n = 40). A pesar del gran número de haplotipos únicos, no se observó diferenciación genética significativa entre localidades (FST = –0.0025, p = 0.686). Una distribución unimodal en la frecuencia del número de diferencias entre haplotipos indica un modelo de expansión rápida en el tamaño poblacional, que basado en una tasa mutacional de 3.6% por millón de años para la región control, indicó un tiempo de diferenciación nucleotídica relativamente reciente de aproximadamente 61,000 años. Este periodo de tiempo corresponde al Pleistoceno tardío, después de la formación de la península de Baja California, sugiriendo expansiones poblacionales en cada una de las localidades, seguidas del último episodio de glaciación, el cual quizás contribuyó a la migración de esta especie de afinidad templada entre las dos localidades y a su homogenización genética. Sin embargo este único evento reciente de flujo genético en la historia evolutiva de la especie, no explica por sí solo los patrones de distribución encontrados en las frecuencias de diferencias nucleotídicas."

"The Californian anchovy Engraulis mordax, a temperate species, may have undergone a process of population disjunction from experiencing post-glacial water heating processes around the tip of the Baja California Peninsula, Mexico about 10,000 b.p. A genetic analysis was performed to test the null hypothesis of genetic homogeneity between the Gulf of California and Southern California, U. S. A., and if this is the case, to estimate the time of haplotype emergence in terms of coalescence. A total of 80 sequences of the mtDNA hypervariable control region of E. mordax captured in the central Gulf of California (n = 40) and Southern California (n = 40) were analyzed. In spite of the large number of private haplotypes, no significant genetic differentiation among sites (FST = –0.0025, p = 0.686) was observed. An unimodal distribution of mismatch frequency between haplotypes indicated a model of rapid expansion in population size that, based on a mutation rate of 3.6% per million years in the control region, indicates a relatively recent nucleotide differentiation

time of approximately 61,000 years. This time period corresponds to the late Pleistocene, suggesting population expansions at each locality, followed by the last episode of glaciation, which may have contributed to migration of this temperate-affinity species between two locations and the genetic homogenization. However this unique recent event of gene flow in the evolutionary history of species does not explain by itself the mismatch distribution patterns found."

ADN mitocondrial, expansión poblacional reciente, flujo genético, región control, reloj molecular. Control region, gene flow, mitochondrial DNA, molecular clock, recent population expansion. BIOLOGÍA Y QUÍMICA CIENCIAS DE LA VIDA BIOLOGÍA ANIMAL (ZOOLOGÍA) ZOOLOGÍA MARINA ZOOLOGÍA MARINA

Gamma-diversity partitioning of gobiid fishes (Teleostei: Gobiidae) ensemble along of Eastern Tropical Pacific: Biological inventory, latitudinal variation and species turnover

OMAR VALENCIA MENDEZ (2018, [Artículo])

Gobies are the most diverse marine fish family. Here, we analysed the gamma-diversity (γ-diversity) partitioning of gobiid fishes to evaluate the additive and multiplicative components of α and β-diversity, species replacement and species loss and gain, at four spatial scales: sample units, ecoregions, provinces and realms. The richness of gobies from the realm Eastern Tropical Pacific (ETP) is represented by 87 species. Along latitudinal and longitudinal gradients, we found that the γ-diversity is explained by the β-diversity at both spatial scales, ecoregions and provinces. At the ecoregion scale, species are diverse in the north (Cortezian ecoregion) and south (Panama Bight ecoregion) and between insular and coastal ecoregions. At the province scale, we found that the species turnover between the warm temperate Northeast Pacific (WTNP), Tropical East Pacific (TEaP) and the Galapagos Islands (Gala) was high, and the species nestedness was low. At the ecoregion scale, historical factors, and phylogenetic factors have influenced the hotspots of gobiid fish biodiversity, particularly in the Cortezian, Panama Bight and Cocos Island ecoregions, where species turnover is high across both latitudinal and longitudinal gradients. At the provincial level, we found that the contributions of the β-diversity from north to south, in the WTNP, TEaP and Gala were high, as result of the high number of unique species. Species turnover was also high at this scale, with a low contribution from species nestedness that was probably due to the low species/gene flow within the provinces. These results highlight the importance and successful inclusion of a cryptobenthic fish component in ecological and biogeographical studies. © 2018 Valencia-Méndez et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

Article, biodiversity, biogeographic region, biogeography, gene flow, goby fish, nonhuman, phylogeny, species distribution, species diversity, taxonomic identification, teleost, animal, animal dispersal, fish, Pacific Ocean, phylogeography, Animal Di CIENCIAS AGROPECUARIAS Y BIOTECNOLOGÍA CIENCIAS AGRARIAS PECES Y FAUNA SILVESTRE PECES Y FAUNA SILVESTRE

Dipole-wind interactions under gap wind jet conditions in the Gulf of Tehuantepec, Mexico: A surface drifter and satellite database analysis

MAURO WILFRIDO SANTIAGO GARCIA (2019, [Artículo])

Gap wind jets (Tehuano winds) trigger supersquirts of colder water and mesoscale asymmetric dipoles in the Gulf of Tehuantepec (GT). However, the effects of successive gap wind jets on dipoles and their effects inside eddies have not yet been studied. Based on the wind fields, geostrophic currents, and surface drifter dispersion, this research documented three dipoles triggered and modified by Tehuano winds. Once a dipole develops, successive gap wind jets strengthen the vortices, and the anticyclonic eddy migrates southwestward while the cyclonic eddy is maintained on the east side of the GT. During the wind relaxation stage, the cyclonic eddy may propagate westward, but due to the subsequent re-intensification of the Tehuano winds, the vortex could break down, as was suggested by surface drifter dispersion pattern and geostrophic field data. The effect of the Tehuano winds was evaluating via eddy-Ekman pumping. Under Tehuano wind conditions, Ekman downwelling (upwelling) inside the anticyclonic (cyclonic) eddies may reach ~ -2.0 (0.5) m d-1 and decrease as the wind weakens. In the absence of Tehuano winds, Ekman downwelling inside the anticyclonic eddy was ~ 0.1 (-0.1) m d-1. The asymmetry of downwelling and upwelling inside eddies during Tehuano wind events may be associated with Tehuano wind forcing. © 2019 Santiago-García et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

article, dipole, leisure, Mexico, cold, ecosystem, factual database, geographic mapping, hurricane, Mexico, satellite imagery, season, water flow, wind, sea water, Cold Temperature, Cyclonic Storms, Databases, Factual, Ecosystem, Geographic Mapping, CIENCIAS FÍSICO MATEMÁTICAS Y CIENCIAS DE LA TIERRA CIENCIAS DE LA TIERRA Y DEL ESPACIO OCEANOGRAFÍA OCEANOGRAFÍA