Variación espacio-temporal del ensamblaje de peces criptobentónicos y conspicuos en dos áreas naturales protegidas, Bahía de los Ángeles y Huatulco

Spatial and temporal variation of the assemblage of cryptobenthic and conspicuous reef fish in two protected natural areas, Bahía delos Ángeles and Huatulco

Rodrigo Daniel Chiriboga Ortega (2023, [Tesis de maestría])

Los peces arrecifales desempeñan roles ecológicos muy importantes manteniendo la salud de los arrecifes siendo limpiadores, recicladores de materia orgánica y además fuente de alimento entre eslabones de la cadena trófica. El presente trabajo busca describir el ensamblaje de peces arrecifales crípticos y conspicuos, y evaluar los patrones espaciales y temporales del ensamblaje de peces arrecifales en Bahía de Los Ángeles, Baja California (BLA) y el Parque Nacional Huatulco (PNH), Oaxaca. Utilizamos dos métodos de muestreo censos visuales y estaciones cerradas. Para evaluar a los peces conspicuos, se realizaron censos visuales empleando transectos de banda de 20x4 m. Para cuantificar la biodiversidad de peces crípticos, se realizaron estaciones cerradas (0.4 m2 ) en donde se utilizó aceite de clavo como anestésico para recolectar los peces arrecifales criptobentónicos (PACr). Las dos metodologías se realizaron en dos gradientes de profundidad (somero; < 5 m y profundo; > 5 m) y en dos estaciones (cálida y fría). Se realizaron curvas de acumulación de especies y un análisis del número efectivo de especies para describir la riqueza y diversidad de cada zona de estudio. Finalmente, para determinar patrones espacio temporales se realizaron análisis nMDS, PERMANOVAS y SIMPER. La riqueza total fue de 43 especies para BLA y 62 para el PNH representando el 80% y 79% del promedio de los estimadores no paramétricos respectivamente. Se aumentó el número de especies registradas a 94 para BLA y 209 para el PNH utilizando las estaciones cerradas. Se observaron diferencias significativas entre estaciones y profundidad en el ensamblaje de PACs de BLA, pero no para los PACr. En el PNH se observaron diferencias significativas para la riqueza y abundancia de los PACr y variación temporal de la biomasa de los PACs. En conclusión se demostró que el uso de métodos de muestreo complementarios mejora la calidad de los inventarios de especies y permite detectar variaciones espacio temporales en la estructura de la comunidad íctica.

Reef fishes perform important ecological roles in maintaining reef health by cleaning and recycling organic material, and by providing a source of food between trophic linkages. The thesis describes cryptic and conspicuous reef fish assemblages and estimates their spatial and temporal patterns of in two sites, Bahía de Los Ángeles (BLA) in the state of Baja California and Huatulco National Park (PNH), in the state of Oaxaca. We used two sampling methods: visual census using SCUBA (band transects of 4x20m) for conspicuous reef fish (PAC) and enclosed stations (0.4 m2) using clove oil to anesthetize and collect the cryptobenthic reef fish (PACr). Sampling was conducted at two depth strata (shallow; < 5 m and deep; > 5m) and during two seasons (warm and cold). We used species accumulation curves and analysis of effective number of species to describe the richness and diversity of reef fish. Finally, nMDS, PERMANOVAS and SIMPER were performed to determine spatial and temporal patterns. The total species richness was 43 species for BLA and 62 species for the PNH, representing 80% and 79%, respectively, of the average of the non-parametric estimators. The number of species increased to 94 for BLA and 209 for PNH using enclosed stations. Significant differences between seasons and depth strata were found for the PACs assemblage at the BLA site, but not for the PACr assemblage. At the PNH site, significant differences were found for the richness and abundance of the PACr assemblage for depth as well as for the seasonal variation of the biomass of the PACs assemblage. In conclusion we demonstrated that the use of complementary sampling methods improves the quality of species inventories and allows for the detection of both spatial and temporal variations in the structure of the reef fish community.

diversidad, peces arrecifales, criptobentónico, biomasa, espacio-temporal biodiversity, reef fishes, cryptobenthic, biomass, spatial-temporal CIENCIAS AGROPECUARIAS Y BIOTECNOLOGÍA CIENCIAS AGRARIAS PECES Y FAUNA SILVESTRE DINÁMICA DE LAS POBLACIONES DINÁMICA DE LAS POBLACIONES

Effects of geostrophic kinetic energy on the distribution of mesopelagic fish larvae in the southern Gulf of California in summer/fall stratified seasons

FERNANDO CONTRERAS CATALA (2016, [Artículo])

Effects of geostrophic kinetic energy flux on the three-dimensional distribution of fish larvae of mesopelagic species (Vinciguerria lucetia, Diogenichthys laternatus, Benthosema panamense and Triphoturus mexicanus) in the southern Gulf of California during summer and fall seasons of stronger stratification were analyzed. The greatest larval abundance was found at sampling stations in geostrophic kinetic energy-poor areas (&lt;7.5 J/m3), where the distribution of the dominant species tended to be stratified. Larvae of V. lucetia (average abundance of 318 larvae/10m2) and B. panamense (174 larvae/10m2) were mostly located in and above the pycnocline (typically ∼ 40 m depth). In contrast, larvae of D. laternatus (60 larvae/10m2) were mainly located in and below the pycnocline. On the other hand, in sampling stations from geostrophic kinetic energy-rich areas (&gt; 21 J/m3), where mesoscale eddies were present, the larvae of the dominant species had low abundance and were spread more evenly through the water column, in spite of the water column stratification. For example, in a cyclonic eddy, V. lucetia larvae (34 larvae/10m2) extended their distribution to, at least, the limit of sampling 200 m depth below the pycnocline, while D. laternatus larvae (29 larvae/10m2) were found right up to the surface, both probably as a consequence mixing and secondary circulation in the eddy. Results showed that the level of the geostrophic kinetic energy flux affects the abundance and the three-dimensional distribution of mesopelagic fish larvae during the seasons of stronger stratification, indicating that areas with low geostrophic kinetic energy may be advantageous for feeding and development of mesopelagic fish larvae because of greater water column stability. © 2016 Contreras-Catala 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, autumn, Benthosema panamense, Diogenichthys laternatus, environmental factor, environmental parameters, fish, geographic distribution, geostrophic kinetic energy, hydrography, larva, nonhuman, population abundance, population dispersion, pop CIENCIAS FÍSICO MATEMÁTICAS Y CIENCIAS DE LA TIERRA CIENCIAS DE LA TIERRA Y DEL ESPACIO OCEANOGRAFÍA OCEANOGRAFÍA

Maintenance of Coastal Surface Blooms by Surface Temperature Stratification and Wind Drift

MARY CARMEN RUIZ DE LA TORRE (2013, [Artículo])

Algae blooms are an increasingly recurrent phenomenon of potentially socio-economic impact in coastal waters globally and in the coastal upwelling region off northern Baja California, Mexico. In coastal upwelling areas the diurnal wind pattern is directed towards the coast during the day. We regularly found positive Near Surface Temperature Stratification (NSTS), the resulting density stratification is expected to reduce the frictional coupling of the surface layer from deeper waters and allow for its more efficient wind transport. We propose that the net transport of the top layer of approximately 2.7 kilometers per day towards the coast helps maintain surface blooms of slow growing dinoflagellate such as Lingulodinium polyedrum. We measured: near surface stratification with a free-rising CTD profiler, trajectories of drifter buoys with attached thermographs, wind speed and direction, velocity profiles via an Acoustic Doppler Current Profiler, Chlorophyll and cell concentration from water samples and vertical migration using sediment traps. The ADCP and drifter data agree and show noticeable current shear within the first meters of the surface where temperature stratification and high cell densities of L. polyedrum were found during the day. Drifters with 1m depth drogue moved towards the shore, whereas drifters at 3 and 5 m depth showed trajectories parallel or away from shore. A small part of the surface population migrated down to the sea floor during night thus reducing horizontal dispersion. The persistent transport of the surface bloom population towards shore should help maintain the bloom in favorable environmental conditions with high nutrients, but also increasing the potential socioeconomic impact of the blooms. The coast wise transport is not limited to blooms but includes all dissolved and particulate constituents in surface waters. © 2013 Ruiz-de la Torre et al.

chlorophyll, algal bloom, article, cell count, cell density, coastal waters, controlled study, dinoflagellate, Lingulodinium polyedrum, meteorological phenomena, Mexico, near surface temperature stratification, nonhuman, nutrient concentration, popul CIENCIAS FÍSICO MATEMÁTICAS Y CIENCIAS DE LA TIERRA CIENCIAS DE LA TIERRA Y DEL ESPACIO OCEANOGRAFÍA OCEANOGRAFÍA

Freshwater exchanges and surface salinity in the Colombian basin, Caribbean Sea

Emilio Beier (2017, [Artículo])

Despite the heavy regional rainfall and considerable discharge of many rivers into the Colombian Basin, there have been few detailed studies about the dilution of Caribbean Surface Water and the variability of salinity in the southwestern Caribbean. An analysis of the precipitation, evaporation and runoff in relation to the climate variability demonstrates that although the salt balance in the Colombian Basin overall is in equilibrium, the area south of 12N is an important dilution sub-basin. In the southwest of the basin, in the region of the Panama-Colombia Gyre, Caribbean Sea Water is diluted by precipitation and runoff year round, while in the northeast, off La Guajira, its salinity increases from December to May by upwelling. At the interannual scale, continental runoff is related to El Niño Southern Oscillation, and precipitation and evaporation south of 12°N are related to the Caribbean Low Level Jet. During El Niño years the maximum salinification occurs in the dry season (December-February) while in La Niña years the maximum dilution (or freshening), reaching La Guajira Coastal Zone, occurs in the wet season (September-November). © 2017 Beier 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.

sea water, fresh water, Article, Caribbean, dilution, dry season, El Nino, environmental parameters, evaporation, freshwater exchange, geographic distribution, molecular weight, oscillation, precipitation, river basin, salinity, seasonal variation, s CIENCIAS FÍSICO MATEMÁTICAS Y CIENCIAS DE LA TIERRA CIENCIAS DE LA TIERRA Y DEL ESPACIO OCEANOGRAFÍA OCEANOGRAFÍA

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

Agricultura, agua y cambio climático en zonas áridas de México

SALVADOR EMILIO LLUCH COTA JUAN ALBERTO VELAZQUEZ ZAPATA César Nieto Delgado (2022, [Artículo])

"En este artículo se expone cómo a pesar de que la ciencia y la tecnología han permitido aumentar históricamente la productividad agrícola, hoy día existen grandes retos derivados del cambio climático y la crisis global de abastecimiento de agua. Se comentan algunas medidas de adaptación y manejo del recurso agua, con algunas referencias a nuestra realidad nacional, y se argumenta cómo el enfoque de Nexo, que implica la toma de decisiones sobre el uso del recurso agua de forma transectorial, representa una alternativa de adaptación al cambio climático."

Cambio climático, agricultura, agua, Nexo, adaptación Climate change, agriculture, water, nexus, adaptation CIENCIAS FÍSICO MATEMÁTICAS Y CIENCIAS DE LA TIERRA CIENCIAS DE LA TIERRA Y DEL ESPACIO CLIMATOLOGÍA CLIMATOLOGÍA REGIONAL CLIMATOLOGÍA REGIONAL

Sismograma de la estación Pico de Orizaba.

Servicio Sismológico Nacional (IGEF-UNAM) (2009, [Event])

Entrada Mayo 30, 2015 at 12:53 p.m. (GMT) / Salida Mayo 31, 2015 at 10:29 a.m. (GMT)

Estación telemática que envía su señal a la estación central localizada en el Instituto de Geofísica de la UNAM y pertenece a la red sismológica convencional.

Componente Z.

Sismología Sismología Sismología CIENCIAS FÍSICO MATEMÁTICAS Y CIENCIAS DE LA TIERRA CIENCIAS DE LA TIERRA Y DEL ESPACIO GEOFÍSICA SISMOLOGÍA Y PROSPECCIÓN SÍSMICA

Sismograma de la estación Pico de Orizaba.

Servicio Sismológico Nacional (IGEF-UNAM) (2009, [Event])

Entrada Marzo 16, 2009 at 12:22 p.m. (GMT) / Salida Marzo 17, 2009 at 12:46 p.m. (GMT)

Estación telemática que envía su señal a la estación central localizada en el Instituto de Geofísica de la UNAM y pertenece a la red sismológica convencional.

Componente Z.

Sismología Sismología Sismología CIENCIAS FÍSICO MATEMÁTICAS Y CIENCIAS DE LA TIERRA CIENCIAS DE LA TIERRA Y DEL ESPACIO GEOFÍSICA SISMOLOGÍA Y PROSPECCIÓN SÍSMICA

Sismograma de la estación Popocatépetl.

Servicio Sismológico Nacional (IGEF-UNAM) (2009, [Event])

Entrada Julio 02, 2015 at 12:12 p.m. (GMT) / Salida Julio 03, 2015 at 11:51 a.m. (GMT)

Estación telemática que envía su señal a la estación central localizada en el Instituto de Geofísica de la UNAM y pertenece a la red sismológica convencional.

Componente E-W.

Sismología Sismología Sismología CIENCIAS FÍSICO MATEMÁTICAS Y CIENCIAS DE LA TIERRA CIENCIAS DE LA TIERRA Y DEL ESPACIO GEOFÍSICA SISMOLOGÍA Y PROSPECCIÓN SÍSMICA

Sismograma de la estación Popocatépetl.

Servicio Sismológico Nacional (IGEF-UNAM) (2009, [Event])

Entrada Agosto 27, 2015 at 00:00 a.m. (GMT) / Salida Agosto 28, 2015 at 11:34 a.m. (GMT)

Estación telemática que envía su señal a la estación central localizada en el Instituto de Geofísica de la UNAM y pertenece a la red sismológica convencional.

Componente E-W.

Sismología Sismología Sismología CIENCIAS FÍSICO MATEMÁTICAS Y CIENCIAS DE LA TIERRA CIENCIAS DE LA TIERRA Y DEL ESPACIO GEOFÍSICA SISMOLOGÍA Y PROSPECCIÓN SÍSMICA