Status of the Petroleum Pollution in the Wider Caribbean Sea
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Ficha Informativa De Los Humedales De Ramsar (FIR)
Ficha Informativa de los Humedales de Ramsar (FIR) 1. Nombre y dirección del compilador de la Ficha: PARA USO INTERNO DE LA OFICINA DE RAMSAR. Biol. Giberth Gordillo Morales Biol.. Leticia Cruz Paredes DD MM YY Consejo Estatal de Protección al Ambiente Gobierno del Estado de Veracruz. Río Tecolutla No. 20 segundo piso, Designation date Site Reference Number Col. Cuauhtémoc C.P. 91060 Xalapa, Veracruz Tel. (228) 8123568 y 8123981 [email protected] 2. Fecha en que la Ficha se llenó: 30 de mayo de 2005 3. País: México 4. Nombre del sitio Ramsar: Laguna de Tamiahua 5. Mapa del sitio incluido: a) versión impresa (necesaria para inscribir el sitio en la Lista de Ramsar): sí X -o- no b) formato digital (electrónico) (optativo): sí X -o- no 6. Coordenadas geográficas (latitud / longitud): 020° 57’ 36”N / 097° 18’ 41’’W 7. Ubicación general: La Laguna de Tamiahua se localiza en los llanos costeros del norte del Estado de Veracruz, es compartida por los municipios de Ozuluama, Tamalín, Tamiahua, Tampico Alto y Tuxpan. Las localidades importantes más cercanas son Tamiahua, Naranjos, Tuxpan y Tampico; esta última perteneciente al Estado de Tamaulipas. Con base en el censo de población y vivienda del año 2000 (INEGI 2002), el municipio de Ozuluama cuenta con una población de 25,978, Tamalín 11,670 hab., Tamiahua 27,398 hab., Tampico Alto 13,604 hab., Tuxpan 127,622 hab. La Laguna de Tamiahua se encuentra en la región marina prioritaria de México, Pueblo Viejo-Tamiahua y en la región terrestre prioritaria Laguna de Tamiahua (CONABIO, 2002). -
Andrea RAZ-GUZMÁN1*, Leticia HUIDOBRO2, and Virginia PADILLA3
ACTA ICHTHYOLOGICA ET PISCATORIA (2018) 48 (4): 341–362 DOI: 10.3750/AIEP/02451 AN UPDATED CHECKLIST AND CHARACTERISATION OF THE ICHTHYOFAUNA (ELASMOBRANCHII AND ACTINOPTERYGII) OF THE LAGUNA DE TAMIAHUA, VERACRUZ, MEXICO Andrea RAZ-GUZMÁN1*, Leticia HUIDOBRO2, and Virginia PADILLA3 1 Posgrado en Ciencias del Mar y Limnología, Universidad Nacional Autónoma de México, Ciudad de México 2 Instituto Nacional de Pesca y Acuacultura, SAGARPA, Ciudad de México 3 Facultad de Ciencias, Universidad Nacional Autónoma de México, Ciudad de México Raz-Guzmán A., Huidobro L., Padilla V. 2018. An updated checklist and characterisation of the ichthyofauna (Elasmobranchii and Actinopterygii) of the Laguna de Tamiahua, Veracruz, Mexico. Acta Ichthyol. Piscat. 48 (4): 341–362. Background. Laguna de Tamiahua is ecologically and economically important as a nursery area that favours the recruitment of species that sustain traditional fisheries. It has been studied previously, though not throughout its whole area, and considering the variety of habitats that sustain these fisheries, as well as an increase in population growth that impacts the system. The objectives of this study were to present an updated list of fish species, data on special status, new records, commercial importance, dominance, density, ecotic position, and the spatial and temporal distribution of species in the lagoon, together with a comparison of Tamiahua with 14 other Gulf of Mexico lagoons. Materials and methods. Fish were collected in August and December 1996 with a Renfro beam net and an otter trawl from different habitats throughout the lagoon. The species were identified, classified in relation to special status, new records, commercial importance, density, dominance, ecotic position, and spatial distribution patterns. -
Venezuela Location Geography Food
Venezuela Location Venezuela, officially the Republic of Venezuela, is a republic (1995 est. pop. 21,005,000), 352,143 sq mi. (912,050 sq. km), in the northern part of South America. With the Caribbean Sea in the north, Venezuela has a coastline of 1,750 long. It is bordered on the south by Brazil, on the west and southwest by Colombia, and on the east by Guyana. Dependencies include Margarita Island, Tortuga Island, and many smaller island groups in the Caribbean. Caracas is the capital and also the largest city in Venezuela. Geography Venezuela, a third larger than Texas, occupies most of the northern coast of South America on the Caribbean Sea. Mountain systems break Venezuela into four distinct areas: (1) the Maracaibo lowlands; (2) the mountainous region in the north and northwest; (3) the Orinoco basin, with the llanos (vast grass-covered plains) on its northern border and great forest areas in the south and southeast, and (4) the Guiana Highlands, south of the Orinoco, accounting for nearly half the national territory. Food The food in Venezuela is generally easy and flavorful. Caracas, the capital of Venezuela, claims to have a greater variety of restaurants than any other South American city, and it would certainly be a pleasure to try and prove it, even if you failed. Venezuelan cooking has European, indigenous, and African roots – a heterodox cuisine formed over the centuries by immigrants. Some of the native dishes include: Page 1 of 7 - Pabellon - stewed and shredded meat accompanied by rice, black beans, and baban -Hallaca - a traditional Christmas dish. -
Temporal and Spatial Fluctuations of Sea Surface Temperature and Chlorophyll a Levels Due to Atmospheric Forcing in a Tropical Coastal Lagoon
Ciencias Marinas (2016), 42(1): 49–65 http://dx.doi.org/10.7773/cm.v42i1.2551 C M Temporal and spatial fluctuations of sea surface temperature and chlorophyll a levels due to atmospheric forcing in a tropical coastal lagoon Fluctuaciones espaciales y temporales de la temperatura superficial del mar y las concentraciones de clorofila a debido a forzamientos atmosféricos en una laguna costera tropical José de Jesús Salas-Pérez*, Carlos González-Gándara Facultad de Ciencias Biológicas y Agropecuarias, Universidad Veracruzana, km 7.5 Carretera Tuxpan-Tampico, Tuxpan, Veracruz, CP 92860, México. * Corresponding author. E-mail: [email protected] ABSTRACT. The temporal and spatial fluctuations of sea surface temperature (SST) and chlorophyll a (Chla) levels due to atmospheric forcing in Mexico’s third largest tropical coastal lagoon (Tamiahua Lagoon), located in the western Gulf of Mexico, was examined from July 2002 to May 2012. The main hypothesis of this study is that SST and Chla levels are modulated by the exchange of heat fluxes from the atmosphere and by rainfall (river runoff). The atmosphere supplies heat (555.05 ± 42.31 W m–2) to Tamiahua Lagoon, which implies that the temperature of the lagoon over the period analyzed (~27 ºC) was higher than normal in the coastal zone. Precipitation regulates Chla levels during the rainy season because the cross-correlation values were high (r > 0.61) and the phase lag of the rainy season with the Chla time series was typically 0 to –1 month. El Niño/Southern Oscillation phases affected the rainfall patterns and, thus, Chla concentrations in the lagoon. -
Monocotyledons and Gymnosperms of Puerto Rico and the Virgin Islands
SMITHSONIAN INSTITUTION Contributions from the United States National Herbarium Volume 52: 1-415 Monocotyledons and Gymnosperms of Puerto Rico and the Virgin Islands Editors Pedro Acevedo-Rodríguez and Mark T. Strong Department of Botany National Museum of Natural History Washington, DC 2005 ABSTRACT Acevedo-Rodríguez, Pedro and Mark T. Strong. Monocots and Gymnosperms of Puerto Rico and the Virgin Islands. Contributions from the United States National Herbarium, volume 52: 415 pages (including 65 figures). The present treatment constitutes an updated revision for the monocotyledon and gymnosperm flora (excluding Orchidaceae and Poaceae) for the biogeographical region of Puerto Rico (including all islets and islands) and the Virgin Islands. With this contribution, we fill the last major gap in the flora of this region, since the dicotyledons have been previously revised. This volume recognizes 33 families, 118 genera, and 349 species of Monocots (excluding the Orchidaceae and Poaceae) and three families, three genera, and six species of gymnosperms. The Poaceae with an estimated 89 genera and 265 species, will be published in a separate volume at a later date. When Ackerman’s (1995) treatment of orchids (65 genera and 145 species) and the Poaceae are added to our account of monocots, the new total rises to 35 families, 272 genera and 759 species. The differences in number from Britton’s and Wilson’s (1926) treatment is attributed to changes in families, generic and species concepts, recent introductions, naturalization of introduced species and cultivars, exclusion of cultivated plants, misdeterminations, and discoveries of new taxa or new distributional records during the last seven decades. -
Lemna Obscura Releasing Analyze Under Spectral Signature at the Maracaibo´S Lake, Venezuela
Lemna obscura releasing analyze under spectral signature at the Maracaibo´s lake, Venezuela. Gustavo Morillo-Díaz1. Fernando Miralles-Wilhem2. Gerardo Aldana1. Giovanny Royero3. Alberto Trujillo1. Eugen Wildermar2. 1. Universidad del Zulia, Centro de Investigación del Agua. Maracaibo, Venezuela 2. Florida International University. Miami, USA. 3. Universidad del Zulia, Laboratorio de Geodesia Física y Satelital, Maracaibo, Venezuela. ABSTRACT The Maracaibo’s Lake is a basin located in the western side of Venezuela and supports an important agricultural and industrial activity. This basin is a core of the petroleum industry since the 20th century. Oil activities had develop a ecological disorder, which a sign of primary manifestation were a cultural eutrophication process related to the phytoplankton blooms in the middles 70’s, and more recently, since 2004 an extensive covered area of Lemna obscura . It seems that change in the hydrological cycles and input of pollutants are the reasons of this macrophyte appearance. In this research, the spectral signature of Lemna obscura is evaluated using MODIS images from 2000 to 2010. Other program as ENVI 4.3 has been considerate to correlate hydrological data with Lemna obscura bloom. Spectral signature appearance of Lemna obscura could be a consequence and indicates changes in the hydrological and ecological features in Maracaibo´s Lake. Key words: Maracaibo’s Lake, Lemna obscura, Spectral signature INTRODUCTION Maracaibo´s lake shorelines have been historically, a primary support for the development of human activities as fishery, in which societies have established cities built infrastructure and found a natural resources. These actions have impact environmental cost that it has accelerated and intensified in recent decades (Hernandez et al, 2003). -
No.784-15/11/24 to the Members Dear Sirs, Venezuela – Oil Stains
No.784-15/11/24 To the Members Dear Sirs, Venezuela – Oil stains within the port of Maracaibo We have obtained information about the recurring problem of oil pollution cause staining problems to hulls regularly in the Lake Maracaibo that seems to stem from micro-spills from operations at the oil installations from our correspondents, GLOBALPANDI, S.A. Please find attached their Circular. Yours faithfully, The Japan Ship Owners’ Mutual Protection & Indemnity Association Oil stains within the port of Maracaibo The Lake Maracaibo is an important loading place for the Venezuelan oil with approximately 11,000 active wells and 45,000 kilometers of underwater pipelines, where about 1.5 million barrels are exported through main terminals located at Puerto Miranda, La Salina and Bajo Grande. Staining of hulls with oil has been also a regular issue inside the lake, a problem that has increased in the last months. In the past these incidents affected only the vessels calling at the terminals run by PDVSA the oil state-owned company, but the problem has expanded recently and it is affecting now the vessels calling at the commercial port as well, commonly known as the port of Maracaibo under the administration of Bolivariana de Puertos, S.A. (Bolipuertos). In recent years there has been a recurring problem of oil pollution in the lake that seems to stem from micro-spills from operations at the oil installations. In some terminals controlled by PDVSA as La Salina for example, these frequent operational spills cause staining problems to hulls regularly. Over time that oil has accumulated at many areas of the lake and seasonal phenomena of the lake, as well as currents, heavy rain and the formation of Lemna during summer months, create large assemblies of oiled debris which sometimes can reach other non-oil installations like the commercial port of Maracaibo. -
Frictional Interactions Between Tidal Constituents in Tide-Dominated Estuaries
Ocean Sci. Discuss., https://doi.org/10.5194/os-2018-53 Manuscript under review for journal Ocean Sci. Discussion started: 3 May 2018 c Author(s) 2018. CC BY 4.0 License. Frictional interactions between tidal constituents in tide-dominated estuaries 1 2 3 1 Huayang Cai , Marco Toffolon , Hubert H. G. Savenije , Qingshu Yang , and 4 Erwan Garel 1Institute of Estuarine and Coastal Research, School of Marine Sciences, Sun Yat-sen University, Guangzhou 510275, China 2Department of Civil, Environmental and Mechanical Engineering, University of Trento, Italy 3Department of Water Management, Faculty of Civil Engineering and Geosciences, Delft University of Technology, Netherlands 4Centre for Marine and Environmental Research (CIMA), University of Algarve, Faro, Portugal Correspondence to: Erwan Garel ([email protected]) Abstract. When different tidal constituents propagate along an estuary, they interact because of the presence of nonlinear terms in the hydrodynamic equations. In particular, due to the quadratic velocity in the friction term, the effective friction experienced by both the predominant and the mi- nor tidal constituents is enhanced. We explore the underlying mechanism with a simple conceptual 5 model by utilizing Chebyshev polynomials, enabling the effect of the velocities of the tidal con- stituents to be summed in the friction term and, hence, the linearized hydrodynamic equations to be solved analytically in a closed form. An analytical model is adopted for each single tidal constituent with a correction factor to adjust the linearized friction term, accounting for the mutual interactions between the different tidal constituents by means of an iterative procedure. The proposed method 10 is applied to the Guadiana (southern Portugal-Spain border) and the Guadalquivir (Spain) estuaries for different tidal constituents (M2, S2, N2, O1, K1) imposed independently at the estuary mouth. -
Frictional Interactions Between Tidal Constituents in Tide-Dominated Estuaries
Manuscript prepared for Ocean Sci. with version 5.0 of the LATEX class copernicus.cls. Date: 11 July 2018 Frictional interactions between tidal constituents in tide-dominated estuaries Huayang Cai1, Marco Toffolon2, Hubert H. G. Savenije3, Qingshu Yang1, and Erwan Garel4 1Institute of Estuarine and Coastal Research, School of Marine Sciences, Sun Yat-sen University, Guangzhou 510275, China 2Department of Civil, Environmental and Mechanical Engineering, University of Trento, Italy 3Department of Water Management, Faculty of Civil Engineering and Geosciences, Delft University of Technology, Netherlands 4Centre for Marine and Environmental Research (CIMA), University of Algarve, Faro, Portugal Correspondence to: Erwan Garel ([email protected]) Abstract. When different tidal constituents propagate along an estuary, they interact because of the presence of nonlinear terms in the hydrodynamic equations. In particular, due to the quadratic velocity in the friction term, the effective friction experienced by both the predominant and the mi- nor tidal constituents is enhanced. We explore the underlying mechanism with a simple conceptual 5 model by utilizing Chebyshev polynomials, enabling the effect of the velocities of the tidal con- stituents to be summed in the friction term and, hence, the linearized hydrodynamic equations to be solved analytically in a closed form. An analytical model is adopted for each single tidal constituent with a correction factor to adjust the linearized friction term, accounting for the mutual interactions between the different tidal constituents by means of an iterative procedure. The proposed method 10 is applied to the Guadiana (southern Portugal-Spain border) and the Guadalquivir (Spain) estuaries for different tidal constituents (M2, S2, N2, O1, K1) imposed independently at the estuary mouth. -
Tidal Currents and Mixing in the Lake Maracaibo Estuarine System*
SCI. MAR., 65 (S@. 1): 155-166 SCIENTLAMARINA 2001 AN INTERDISCIPLINARY VIEW OF THE OCEAN. J.L PUEGR~;1. ALONSO and J. ARÍSTEGUI (d.) Tidal currents and mixing in the Lake Maracaibo estuarine system* 'Dcpanamemo & Físia Facultad & Cimcias del Mar, Univasidad de Las Pllmas & Gran Canaria, CampusUnivasitwo~Tafw.35017LasPalmas&GranCanana,Spain. 3NTEVEP S. A.. Centro de investigaci6n y Apoyo Tecnológico, Fide F'cm5leos & Vcnaue1a S. A., Los Tcqua, EscadoMirandavenezaela SUMMARY: The Lake Maracaibo cstuarinc systcm is a cooscilIating coupled ocean-lakc systern connected through a par- tialiy mixed estuay. In this paper we examine thc low frcsuency movcmam (o< 0.1 cyclcs/day) in uie differmt water bod- ies within thi system. The harmonic and rorary specaal analyscs of velocity data indicatcs the importante of tidai forcing within thc whole system and its intaauion with winds and fresh warcr discbarge. ln particular, the nsults indicate thc exis- te~of dominant semi-mdy osciUarions in iak Maracáibo. kely of non-iincar tidal origin, and suggest thai vertical smififaetion plays an important dein coí~troiiingthe three-dimcnsional strucnire of tidal cmu. Key words: estuarine sysrcm, tidal forcing, non-linear phenomena, stdfication. mixing, Caribbean Sea. and current distributions with limited data sets. The existing stratification, on the other hand, wili shape Any dynamicd study of an estuarine system has the instantaneous and mean cunrents. Stratification to include both current and density distributions, will enhance lateral advection but reduce vertical simply because rhey are deeply inte~co~e~ted.The exchange. Wíth strong vertical stratificatian, for relative forcing of river discharge and tidal range, exarnpie, the upper and lower layers may be rather togefher with the effect of winds, waves, and the uncoupled, the tidal wave having quite different geomorphology of the basin, will determine the amplitudes and phases. -
Plan De Desarrollo Municipal 2018-2021
Plan de Desarrollo Municipal 2018-2021 P LAN DE DESARROLLO MUNICIPAL 2018-2021 ÍNDICE PRESENTACIÓN 4 MARCO JURÍDICO 6 ALINEACIÓN PROGRAMÁTICA 8 DIAGNÓSTICO 17 UBICACIÓN 17 ANTECEDENTES HISTÓRICOS 18 DIVISIÓN POLÍTICA 18 MEDIO FÍSICO NATURAL 20 HIDROLOGÍA 20 GEOLOGÍA 21 EDAFOLOGÍA 22 TOPOGRAFÍA 24 CLIMA 25 USO DE SUELO 26 FLORA Y FAUNA 26 ÁREAS NATURALES PROTEGIDAS 27 MEDIO AMBIENTE Y CONTAMINACIÓN 30 RIESGO Y VULNERABILIDAD 32 DEMOGRAFÍA 37 CRECIMIENTO POBLACIONAL 37 COMPOSICIÓN POR SEXO Y GRUPOS DE EDAD 39 ASPECTOS SOCIALES 42 EDUCACIÓN 42 SALUD 44 POBLACIÓN INDÍGENA 45 POBREZA Y PERSONAS VULNERABLES 46 ECONOMÍA 53 LA LAGUNA DE TAMIAHUA 58 DESARROLLO URBANO Y ECOLOGÍA 59 DISTRIBUCIÓN DE LA POBLACIÓN EN EL TERRITORIO 59 TRANSPORTE Y VIALIDAD 60 INFRAESTRUCTURA Y SERVICIOS PÚBLICOS 62 EQUIPAMIENTO 63 VIVIENDA 65 ESPACIOS PÚBLICOS 66 H. AYUNTAMIENTO DE TAMIAHUA 2018 – 2021 PÁGINA 0 PLAN DE DESARROLLO MUNICIPAL 2018-2021 SITIOS PATRIMONIALES 68 SEGURIDAD PÚBLICA 68 PRONÓSTICO 71 MISIÓN Y VISIÓN 72 MISIÓN 72 VISIÓN 72 VALORES 72 SUSTENTABILIDAD 72 HONESTIDAD 72 RESPETO 72 INSTITUCIONALIDAD 73 ESTRATEGIA 74 CRITERIOS DE DEMOCRACIA PARTICIPATIVA 74 EJES TRANSVERSALES 77 RESILIENCIA 77 COMPETITIVIDAD ECONÓMICA 78 EJE DE TRABAJO 1. DESARROLLO SUSTENTABLE 79 LÍNEA ESTRATÉGICA 1. MANEJO INTEGRAL DE LA LAGUNA DE TAMIAHUA 81 LÍNEA ESTRATÉGICA 2. PROMOCIÓN DE ACTIVIDADES DE TURISMO SUSTENTABLE 83 LÍNEA ESTRATÉGICA 3. DESARROLLO PORTUARIO Y AÉREO GLOBAL YAN – JA ¡ERROR! MARCADOR NO DEFINIDO. LÍNEA ESTRATÉGICA 4. GASODUCTO TRANSCÁNADA 85 LÍNEA ESTRATÉGICA 5. IMPULSO A OTRAS ACTIVIDADES ECONÓMICAS 85 EJE DE TRABAJO 2. SOCIEDAD Y TERRITORIO 86 LÍNEA ESTRATÉGICA 6. DISMINUCIÓN DE LAS DESIGUALDADES MEDIANTE EL ORDENAMIENTO TERRITORIAL 88 LÍNEA ESTRATÉGICA 7. -
MODIS Detects Oil Spills in Lake Maracaibo,Venezuela
Eos,Vol. 84, No. 33, 19 August 2003 the lava’s melting temperature at surface pres- can be lost entirely from Io or cold-trapped at Keszthelyi, L., and A. McEwen, Magmatic differentia- sure.However,for lava at 1870 K to have a stable sites,compositional evolution of evapo- tion of Io, Icarus 130, 437–448, 1997. basaltic composition (with liquidus melting rated lava residues would affect igneous Lopes, R., et al., Io in the near-infrared: NIMS results temperatures ~1400–1550 K at 1 bar),the magma phase equilibria and the temperature of subse- from the Galileo fly-bys in 1999 and 2000,J. Geo- would have to ascend rapidly from nearly phys. Res. 106, 33,053–33,078, 2001. quent eruptions.Refractory lava residues lack the Lopes-Gautier,R., et al.,A close-up look at Io in the 1,000 km deep with little cooling in transit. amounts of SiO2 and FeO in common silicate infrared: Results from Galileo’s near-infrared map- Though no record of such an eruption exists lavas (Figure 3b) and may have extraordinary ping spectrometer, Science, 288, 1201–1204, 2000. on Earth, magma may have erupted from liquidus temperatures (Figure 3c). Marchis, F., et al., High-resolution Keck adaptive nearly such depths on Earth’s moon.Alternatively, optics imaging of violent volcanic activity on Io, Io’s magmas could be heated near the surface Questions Still to be Answered Icarus 160, 124–131, 2002. by the electrical induction currents and McEwen et al., High-temperature silicate volcanism plasma currents bathing Io.Heating in a tidally The epic tour of the Jovian system by Galileo on Jupiter’s moon,Io,Science, 281, 87–90, 1998.