Waters During the 2009–2010 Drought Reveals Upcoming Trophic Status

Total Page:16

File Type:pdf, Size:1020Kb

Waters During the 2009–2010 Drought Reveals Upcoming Trophic Status Spatiotemporal variability in Terminos Lagoon (Mexico) waters during the 2009–2010 drought reveals upcoming trophic status shift in response to climate change Renaud Fichez, Carlos Linares, Sandrine Chifflet, Pascal Conan, Adolfo Contreras Ruiz Esparza, Lionel Denis, Pascal Douillet, Christian Grenz, Jean-François Ghiglione, Francisco Gutiérrez Mendieta, et al. To cite this version: Renaud Fichez, Carlos Linares, Sandrine Chifflet, Pascal Conan, Adolfo Contreras Ruiz Esparza, et al.. Spatiotemporal variability in Terminos Lagoon (Mexico) waters during the 2009–2010 drought reveals upcoming trophic status shift in response to climate change. Regional Environmental Change, Springer Verlag, In press, 10.1007/s10113-019-01519-2. hal-02147089 HAL Id: hal-02147089 https://hal.archives-ouvertes.fr/hal-02147089 Submitted on 4 Jun 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Regional Environmental Change https://doi.org/10.1007/s10113-019-01519-2 ORIGINAL ARTICLE Spatiotemporal variability in Terminos Lagoon (Mexico) waters – during the 2009 2010 drought reveals upcoming trophic status shift in response to climate change 1 2 1 3 4 Renaud Fichez & Carlos Linares & Sandrine Chifflet & Pascal Conan & Adolfo Contreras Ruiz Esparza & 5 & 1 & 1 & 3 & 6 & Lionel Denis Pascal Douillet Christian Grenz Jean-François Ghiglione Francisco Gutiérrez Mendieta 1 7 3 4 Montserrat Origel-Moreno & Alain Muñoz Caravaca & Mireille Pujo-Pay & Jorge Zavala-Hidalgo Received: 8 March 2018 /Accepted: 11 May 2019 Abstract The 2009–2010 El Niño was accompanied by a severe drought strongly impacting Mexico as well as Central America, the Caribbean, and the southern USA. The present work aims at assessing how such a major climatic event impacted the hydrological typology of transitional waters in Terminos Lagoon, one of the largest shallow tropical lagoons fringing the Gulf of Mexico. Spatiotemporal inter-comparison of hydrological conditions was conducted by pairing a reference multiparametric dataset (14 hydrological parameters versus 34 sampling stations) averaged over the October 2008 to July 2010 period with each sampling occurrence dataset and running Principal Component Analyses (PCA), setting the reference-survey dataset as active variables and each sampling occurrence dataset as non-active (supplementary) variables. It revealed that the exceptional deficit in freshwater supply to the lagoon during the 2009–2010 El Niño drastically reduced hydrological diversity and lowered the trophic status of the lagoon. Short-term shifts in environmental status are common in transitional waters and responsible for temporary shifts in community structure but climate change projections show a significant long-term decrease in the freshwater discharge at the regional scale that will impact Terminos Lagoon as well as other coastal lagoons of Mexico and Central America. When combined with sea level rise, such a decrease will result in a long-term shift in hydrological conditions with a subsequent increase in salinity and a decrease in the diversity of environmental conditions affecting trophic status, will have a long-term impact on the biota. Keywords Coastal lagoon . Hydrology . Trophic status . El Niño . Global change . Climate change, Mexico Editor: Erika Coppola * Renaud Fichez Christian Grenz [email protected] [email protected] Jean-François Ghiglione Carlos Linares [email protected] [email protected] Francisco Gutiérrez Mendieta Sandrine Chifflet [email protected] [email protected] Montserrat Origel-Moreno Pascal Conan [email protected] [email protected] Alain Muñoz Caravaca Adolfo Contreras Ruiz Esparza [email protected] [email protected] Mireille Pujo-Pay [email protected] Lionel Denis [email protected] Jorge Zavala-Hidalgo [email protected] Pascal Douillet [email protected] Extended author information available on the last page of the article R. Fichez et al. Introduction effect relationship, regardless of what spatiotemporal variabil- ity has to teach us about the flexibility of tropical transitional Littoral regions accommodate a broad range of coastal sys- systems and about the most probable scenarios at stake in tems with heterogeneous water bodies often referred to as terms of environmental response to global change. Such a lack “transitional waters” characterized by strong variability in sa- of information on the distribution and temporal variability of linity as well as in most environmental parameters of natural environmental parameters is especially critical for coastal or anthropogenic origin which are driven by the balance be- tropical systems of emerging and developing countries where tween marine and freshwater inputs (Elliott and McLusky the potential threat of global change is increasingly acknowl- 2002; McLusky and Elliott 2007). Response of transitional edged as a key parameter detrimentally impacting sustainable waters to ongoing climate change has risen to the highest level development. This is even more salient for the Mesoamerican of economic and political priority, resulting in a growing de- region (Central America and Southern Mexico), which is con- mand for the accurate scientific expertise essential for the sidered to be the most prominent tropical climate change hot- definition; implementation; and control of ecologically, so- spot worldwide (Giorgi 2006) and which is increasingly vul- cially, and economically effective management plans. This is nerable to extreme climatic events (Hidalgo et al. 2013; especially true in the Terminos Lagoon area, on the southern Vázquez-González et al. 2014). Gulf coast of Mexico, which has been singled out as being The present study was conducted on the very large and vulnerable to climate change (Magrin et al. 2007), potentially shallow coastal Terminos Lagoon during a time period includ- exposed by the end of the twenty-first century to a drastic ing the 2009–2010 El Niño Southern Oscillation positive decrease in river discharge from the Usumacinta-Grijalva anomaly when Mexico experienced the most severe drought River (Kemp et al. 2016), and subject to general sea level rise since 1941 (Baringer et al. 2010). Its objectives, based on a 2- in the range 0.5 to 1 m (Magrin et al. 2007;Rahmstorf2012). year hydrological survey, aimed to (i) apply a data treatment Here, as in all other transitional water systems, a proper as- allowing for temporal intercomparison of typology ap- sessment of spatiotemporal variability must be considered as a proaches; (ii) analyze what such an intercomparison could prerequisite to the scientific establishment of cause to effect reveal in terms of seasonal cycling and climate change in the relationships between global change and shifts in environmen- specific context of the severe 2009–2010 El Niño–related tal conditions. However, spatiotemporal variability issues drought period; and (iii) assess potential long-term environ- have often been overlooked in environmental studies, raising mental alteration in Terminos Lagoon in the context of climate the risk of drawing insufficiently supported scientific interpre- change projection scenarios. tation and of misguiding environmental policies toward inef- ficient management action plans (Lucena-Moya et al. 2012). Extracting comprehensive information from multiparametric Material and methods environmental databases remains a challenge and environmetric approaches based on multivariate data ordina- Study site and environmental conditions tion have been proven to be a rigorous and integrative way of assessing spatial and temporal variability of transitional waters The selection of Terminos Lagoon as a focus site for the study (Fichez et al. 2010;Shinetal.2013). The approach developed of tropical coastal lagoon transitional waters arose logically in the present study specifically focuses on the physico- from its exceptional status as one of the largest shallow sys- chemical and biogeochemical indicators of water quality that tems in the Gulf of Mexico, where conservation policies con- are commonly measured in environmental status assessments. flicted with anthropogenic pressure (Grenz et al. 2017). Establishing a multiparametric characterization of transitional Moreover, Terminos Lagoon benefited from a significant sci- waters has been identified as a key integrative diagnostic ap- entific background and has been the recent object of renewed proach that is still strongly lacking in environmental manage- interest from the scientific community leading to its selection ment (Poikane et al. 2014). Recent concerns about delineating as a “pilot site” within the framework of the Global environmental status categories for transitional waters have Environment Facility (GEF) Program on the Gulf of largely focused on intercomparison between distinct systems, Mexico-Large Marine Ecosystem (GoM-LME) (García-Ríos to the detriment of the preliminary assessment of internal spa- et al.
Recommended publications
  • Risk Analysis by Overtopping During an Upstream Landslide in Peñitas
    https://doi.org/10.5194/nhess-2019-191 Preprint. Discussion started: 9 July 2019 c Author(s) 2019. CC BY 4.0 License. 1 Case Study: Risk Analysis by Overtopping During an Upstream 2 Landslide in Peñitas Dam, Mexico 3 Humberto J.F. Marengo1, Alvaro A. Aldama2 4 1Engineering Institute, UNAM, Mexico. 5 2 Independent Consultant, Cuernavaca, Mexico. 6 Correspondence to: Humberto Marengo ([email protected]) 7 Abstract. This research presents the procedure for risk assessment and reliability analysis to dam 8 overtopping (Peñitas) located downstream of a landslide dam. For the analysis are used six statistical 9 variables and their uncertainties, peak flood of the upstream dam, are evaluated with empirical formulas. 10 Highest water levels of the dam break event were computed using reservoir routing with an explicit 11 equation developed by authors. Afterward, overtopping risk analysis of Peñitas Dam was assessed for 12 different stages of excavation of the natural dam that were made for solve the problem. A sensitivity 13 analysis of duration of dam break is made, and also is calculated the possible upper elevation of Peñitas 14 dam, finding that is a recommended practice measurement in similar further cases. A methodology to do 15 an orderly and consistently analysis of risk is proposed to solve similar situations. 16 17 1. Introduction. Rain season on 2007 was very severe in the South-east part of Mexico and produced 18 during September and October higher flood until that date in Tabasco State. On 4 November 2007, took 19 place a landslide on Grijalva River, the second in the country with an extension of 80 Ha.
    [Show full text]
  • FLOODS GLIDE No
    Appeal N° MDRMX002 MEXICO: FLOODS GLIDE no. FL-2007-000200-MEX Operations Update n°1 14 November 2007 Period covered by this Operations Update: 6 November to 13 November 2007; Appeal target: CHF 1,208,000 (USD 1,042,278 or EUR 722,056); Appeal coverage: 98% <click here to go directly to the updated donor response report, or here to link to contact details > Appeal history: • This Emergency Appeal was initially launched on a preliminary basis on 6 November 2007 for CHF 1,208,000 (USD 1,042,278 or EUR 722,056) for four months to assist 40,000 beneficiaries. • Disaster Relief Emergency Fund (DREF): CHF 200,000 (USD 173,563 or EUR 119,546) was initially allocated from the Federation’s DREF to support the National Society’s response. • Due to bilateral contributions from the Swiss Red Cross, this Operations Update n°1 includes a new objective The city of Villahermosa in Tabasco is still where 2,000 families will receive flooded. Source: International Federation cleaning kits and 3,600 children school kits. Summary: Since the onset of the emergency in the states of Tabasco and Chiapas, the Mexican Red Cross (MRC) activated its national response system, coordinated with local authorities, provided information for the Federation’s Disaster Management Information System (DMIS) and has been working arduously to provide relief aid to the affected population. The MRC headquarters in Mexico, F.D. dispatched a Rapid Intervention Unit (RIU) consisting of specialized personnel in disaster response, rescue equipment and vehicles. The National Rescue Director was deployed to Tabasco and led the operation with support from the Tabasco state delegate.
    [Show full text]
  • Processional Ceremonies in the Formative Period Chiapas Central Depression, Chiapas, Mexico
    Processional Ceremonies in the Formative Period Chiapas Central Depression, Chiapas, Mexico Timothy D. Sullivan Processional ceremonies figured Clark 2001; Inomata 2014: 19-20), and prominently in Mesoamerican religious creating what Eric Wolf referred to as practices at the time of European contact, structural power (Wolf 1990: 586, 590-591; and continue in different guises today. The 1999: 5-15). Wolf describes structural power organization of architecture, and sometimes as “the power manifest in relationships that of sculptures, within the earliest not only operates in settings and domains, Mesoamerican political centers supports the but also organizes and orchestrates the idea that processional ceremonies date to at settings themselves, and that specifies the least the inception of polities in this area. direction and distribution of energy flows” These ceremonies provided much more than (1999:5). the ideological legitimization of leadership Over the course of the Middle roles; they served an essential function to Formative period in Mesoamerica (Table 1), insure the cosmic balance and the survival the Chiapas Central Depression, an of the community. The prehispanic ethnically Zoque area (Lowe 1977, 1999), Mesoamerican world view did not saw the foundation of a number of new distinguish between what most political centers, each of which was centered contemporary people would view as on a large scale ceremonial zone, pragmatic adaptive techniques designed to appropriate for staging processional rituals. increase production, and belief-based The organization of large-scale rituals had a practices designed to venerate or pacify strong effect on the relation between rulers cosmological forces and entities. The idea and subjects, and architectural evidence that these ceremonies were less important to indicates that this relational structure survival than the construction of irrigation changed from the Middle Formative through systems or the manufacture of stone tools the Terminal Formative periods.
    [Show full text]
  • Flood Severity Along the Usumacinta River, Mexico: Identifying the Anthropogenic Signature of Tropical Forest Conversion
    Journal of Hydrology X 10 (2021) 100072 Contents lists available at ScienceDirect Journal of Hydrology X journal homepage: www.sciencedirect.com/journal/journal-of-hydrology-x Research papers Flood severity along the Usumacinta River, Mexico: Identifying the anthropogenic signature of tropical forest conversion Alexander J Horton a,*, Anja Nygren b, Miguel A Diaz-Perera c, Matti Kummu a,* a Water & Development Research Group, Aalto University, Espoo, Finland b Development Studies, University of Helsinki, Helsinki, Finland c El Colegio de la Frontera Sur-Unidad Villahermosa, Villahermosa, Tabasco, Mexico ARTICLE INFO ABSTRACT Keywords: Anthropogenic activities are altering flood frequency-magnitude distributions along many of the world’s large Deforestation rivers. Yet isolating the impact of any single factor amongst the multitudes of competing anthropogenic drivers is Flooding a persistent challenge. The Usumacinta River in southeastern Mexico provides an opportunity to study the Hydrological modelling anthropogenic driver of tropical forest conversion in isolation, as the long meteorological and discharge records Flow regime capture the river’s response to large-scale agricultural expansion without interference from development ac­ Stormflow Watershed management tivities such as dams or channel modifications. We analyse continuous daily time series of precipitation, tem­ perature, and discharge to identify long-term trends, and employ a novel approach to disentangle the signal of deforestation by normalising daily discharges by 90-day
    [Show full text]
  • Laguna De Terminos/Rio Candelaria Delta Core: Conditions of Sustainable Urban Occupation in the Interior of the Yucatan Peninsula
    Laguna de Terminos/Rio Candelaria Delta Core: Conditions of Sustainable Urban Occupation in the Interior of the Yucatan Peninsula By: Joel D. Gunn, William J. Folan, John W. Day, Jr., and Betty B. Faust Gunn, Joel D., William J Folan, John W. Day, Jr., and Betty B. Faust. Lagoon Terms / Rio Candelaria Core : Conditions of Sustainable Urban Occupation in the Interior of the Yucatan Peninsula . Estudios de cultura maya [online]. 2012, vol.39, p. 67-97. Made available courtesy of the Universidad Nacional Autónoma de México: http://www.scielo.org.mx/scielo.php?script=sci_abstract&pid=S0185- 25742012000100003&lng=es&nrm=iso&tlng=en***Reprinted with permission. No further reproduction is authorized without written permission from Universidad Nacional Autónoma de México. This version of the document is not the version of record. Figures and/or pictures may be missing from this format of the document.*** Keywords: anthropology | oceanography | climate | Maya civilization | Yucatan Peninsula | Mexico Table of Contents Laguna de Terminos/Rio Candelaria Delta Core: Conditions of Sustainable Urban Occupation in the Interior of the Yucatan Peninsula ...................................................................... 3 Abstract ........................................................................................................................... 3 Abstracto ......................................................................................................................... 3 Introduction ....................................................................................................................
    [Show full text]
  • Heavy Metal Contamination and Provenance of Sediments Recovered at the Grijalva River Delta, Southern Gulf of Mexico
    J. Earth Syst. Sci. (2021) 130:88 Ó Indian Academy of Sciences https://doi.org/10.1007/s12040-021-01570-w (0123456789().,-volV)( 0123456789().,-vol V) Heavy metal contamination and provenance of sediments recovered at the Grijalva River delta, southern Gulf of Mexico 1 2, MARTHA PATRICIA AYALA-PEREZ ,JOHN SARMSTRONG-ALTRIN * 2 and MARIA LUISA MACHAIN-CASTILLO 1Posgrado en Ciencias del Mar y Limnologıa, Universidad Nacional Autonoma de Mexico, Ciudad Universitaria, 04510 Mexico City, CDMX, Mexico. 2Unidad de Procesos Oceanicos y Costeros, Instituto de Ciencias del Mar y Limnologıa, Universidad Nacional Autonoma de Mexico, Ciudad Universitaria, 04510 Mexico City, CDMX, Mexico. *Corresponding author. e-mail: [email protected] john˙[email protected] MS received 19 November 2020; revised 5 January 2021; accepted 6 January 2021 This study examines textural characteristics, carbonate, organic carbon and chemical composition of sediment samples recovered in the nearshore region (*3–19 m water depth) at the Grijalva River mouth, southern Gulf of Mexico. The aim of this study is to assess the heavy metal contamination and prove- nance variations in sediments between the dry and northers (rainy) seasons. The proportion of sand, carbonate, and organic carbon contents were abundant at sites located near to the Grijalva River mouth, principally in northers season. Silt content is dominant in the dry season, especially in the sites located away from the Grijalva River mouth. The Chemical Index (CIX) values obtained for the dry (*76–84) and northers (*75–87) seasons indicated a moderate to high intensity of weathering and a humid climate in the source area.
    [Show full text]
  • Geochronology and Landscape Evolution of the Strand-Plain of the Usumacinta and Grijalva Rivers, Southern Mexico
    Accepted Manuscript Geochronology and landscape evolution of the strand-plain of the Usumacinta and Grijalva rivers, southern Mexico Esperanza Muñoz-Salinas, Miguel Castillo, David Sanderson, Tim Kinnaird PII: S0895-9811(17)30269-9 DOI: 10.1016/j.jsames.2017.08.021 Reference: SAMES 1762 To appear in: Journal of South American Earth Sciences Received Date: 3 July 2017 Revised Date: 25 August 2017 Accepted Date: 28 August 2017 Please cite this article as: Muñoz-Salinas, E., Castillo, M., Sanderson, D., Kinnaird, T., Geochronology and landscape evolution of the strand-plain of the Usumacinta and Grijalva rivers, southern Mexico, Journal of South American Earth Sciences (2017), doi: 10.1016/j.jsames.2017.08.021. This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. ACCEPTED MANUSCRIPT 1 Geochronology and landscape evolution of the strand-plain of 2 the Usumacinta and Grijalva rivers, southern Mexico 3 4 Esperanza Muñoz-Salinas 1,* , Miguel Castillo 2, David Sanderson 3, Tim Kinnaird 4 5 6 1Instituto de Geología, Universidad Nacional Autónoma de México, UNAM, Ciudad 7 Universitaria 3000, P.C. 02510, Mexico City, Mexico. Email: [email protected], 8 telephone: +52 (55) (525) 622 4300 Ext. 109 9 10 2Instituto de Geología, Universidad Nacional MANUSCRIPTAutónoma de México, UNAM, Ciudad 11 Universitaria 3000, P.C.
    [Show full text]
  • Trace Metals in Fresh Marine Sediments from the Southwest of the Gulf of Mexico
    Ingeniería Investigación y Tecnología, volumen XIV (número 4), octubre-diciembre 2013: 511-522 ISSN en trámite, FI-UNAM (artículo arbitrado) Cluster and Principal Components Analyses on the Contents of (Total and Sorbed) Trace Metals in Fresh Marine Sediments from the Southwest of the Gulf of Mexico Análisis de componentes principales y clusters de metales trazas (totales y sorbidos) en sedimentos marinos recientes del Suroeste del Golfo de México De Lorenz-Santos Fernando Jesús Fernández-Villagómez Georgina Facultad de Ingeniería Facultad de Ingeniería División de Ingeniería Civil y Geomática División de Ingeniería Civil y Geomática Universidad Nacional Autónoma de México Universidad Nacional Autónoma de México E-mail: [email protected] E-mail: [email protected] Cervini-Silva Javiera † Vázquez Felipe Departamento de Procesos y Tecnología Laboratorio de Fisicoquímica Marina División de Ciencias Naturales e Ingeniería Instituto de Ciencias del Mar y Limnología Universidad Autónoma Metropolitana Unidad Cuajimalpa Universidad Nacional Autónoma de México E-mail: [email protected] Information on the article: received: April 2012, reevaluated: August 2012, accepted: December 2012 Abstract The amounts of total and sorbed Al, Ba, Cr, Fe, Mn, Ni, and V present in three sediment cores from the South of the Gulf of Mexico (N1, N2, and N3) were Keywords: determined. Of the three samples studied herein (N1. N2, and N3), one of them (N2) is associated to a natural “chapopotera”. ICP/MS analyses show that • trace metals partitioning total concentrations of Al, Fe, Mn, Ba, Cr, Ni, Pb, and V for N1 and N3 were • enrichment factor -1 found to be ca. 4.2, 2.3, 206.5, 165, 91, 72, 14 and 97 mg kg , and ca.
    [Show full text]
  • VALVERDE. Chiapa De Corzo
    THE SPLENDOR OF MEXICO A Meeting Place María del Carmen Valverde Valdés* Photos this page by Elsie Montiel estled in the sultry Central Chiapas Depression on the banks of the Gran de or Grijalva River and just before the entranc e Nto the spectacular Sumidero Canyon is the city of Chiapa de Corzo. Famous for its magnificent sixteenth-century Mudéjar fountain, a few people know it for its colorful xicalpestles (lacquered and painted gourds), and even fewer know it for its para chico revelers, the m ain attraction at the fiesta of San Sebastián. 1 Also, few people are aware of the existence of a first-class archaeological site in the city, even though a round-about had to be built on the route of the Pana mer - ic an Highway to avoid going directly over one of its pyramid’s foun - dations. Most people only visit Chiapa de Corzo because the boats that go through the Sumidero Canyon leave from there, and they are not aware that its nooks and crannies and environs contain an ancient and sometimes fascinating history. The town of Chiapa has been inhabited by different groups continuously from the earliest pre-Hispanic times until today. It is one of the few places in Chiapas that has 5 This pre-Hispanic building is on private grounds. 6 Structure 32 still stands at a crossroad near the entrance to the city. 3 Photos: Elsie Montiel * Researcher at the Center for Mayan Studies of the UNAM Institute for Philological Research ( IIFL ). 74 l e i t been both an urban center and a meeting place for dif ferent cultures that have n o M e been determinant in the history of today’s Mexico.
    [Show full text]
  • Risk and Unsustainability in Villahermosa, Mexico
    Sustainable Development and Planning IX 17 RISK AND UNSUSTAINABILITY IN VILLAHERMOSA, MEXICO JOEL F. AUDEFROY Instituto Politécnico Nacional (IPN) Escuela Superior de Ingeniería y Arquitectura (ESIA-Tecamachalco), Mexico ABSTRACT The city of Villahermosa, Tabasco, Mexico is located in the basin of the Grijalva and Usumacinta rivers. In pre-Hispanic times, the watershed system was not a threat; rather, it was a system that favored human settlements and trade. Since then, throughout its history, the plain has undergone several transformations that have changed its riverbeds. Urban development plans and the design and control of water works have failed to take these changes into account, forgetting that rivers have memory and tend to return to their old channels. Historically, between 1652 and 2008 floods and disasters caused by hydrometeorological events on record totaled 67 events. In the period for which we have reliable records of hydrometeorological events, recurrent flooding has been observed, especially in the months of September, October, and November. In that context, the great flood of October 2007 cannot be seen as an isolated phenomenon. This study shows how, over time, the risk of flooding in Villahermosa has been socially constructed by human actions that undermine sustainability: the diversion of rivers, deforestation, and introduction of livestock, all of which have contributed to changing ecosystems and the hydrogeological context of the state. Despite extensive water works carried out since the 1950s, the city of Villahermosa remains highly vulnerable to catastrophic flooding. There are irregular settlements which are particularly vulnerable to flooding, due to the absence of a policy on low-income housing development.
    [Show full text]
  • Itinerary “The Best of Chiapas” (6 Days / 5 Nights)
    Itinerary “The best of Chiapas” (6 days / 5 nights) View Video DAY 1: ZOO - SUMIDERO CANYON – CHIAPA DE CORZO – HOTEL IN TUXTLA GUTIÉRREZ We will pick you up at Tuxtla Gutierrez airport (we recommend an arrival in the morning). We begin the tour in the famous ZOO of Tuxtla which is located inside a natural reserve zone. Species of local fauna are exhibited, preserved, protected and studied in an environment similar to their natural habitat. This zoo is considered one of the best in the world of its kind. Its facilities are within a small jungle, crossed by small rivers. After our tour there (approx. 2 ½ hours) we will continue to take a two hour boat trip through the SUMIDERO CANYON, which was formed by a geological fault millions of years ago. Driving along the GRIJALVA RIVER, which runs through the Sumidero Canyon, you should expect a spectacular landscape in the midst of a fascinating rain forest. You will be able to watch some of the numerous species of animals, like crocodiles or monkeys. Following this we make a short visit to the historical town of CHIAPA DE CORZO, with the known colonial fountain and the POCHOTA TREE in the center of the town. We will have time to have a meal. In the afternoon we will go to the MARIMBA PLAZA to dance and enjoy the happy songs played live. We will then return to our Hotel in Tuxtla Gutiérrez. Hotel VIP: Camino Real www.caminoreal.com Hotel ****: Best Western Arecas www.hotelarecas.com.mx Info: If your flight arrives after 10:30 am, we will only go to the Sumidero Canyon.
    [Show full text]
  • Mexico) Petroleum Potential
    UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Brief on Reforma-Campeche's (Mexico) Petroleum Potential by Bernardo F. Grossling U.S. Geological Survey Open-file Report 79-237 This report has not been edited or reviewed for conformity with U.S. Geological Survey standards or nomenclature BRIEF ON REFORMA-CAMPECHE'S (MEXICO) PETROLEUM POTENTIAL Opportunities and Challenges for the United States For the past several months I have been endeavouring to gauge the petroleum prospects of southeastern Mexico on the basts of the published technical literature, newsmedia accounts, and critical examination of the data from a geologic point of view. The main results of this study are briefly summarized here, and will be reported in greater detail at a later date. 1) In May 1972 Petroleos Mexicanos (Pemex), the national oil company of Mexico, discovered a very important new petroleum province through two wildcat wells completed a day apart. These wells are about 50 km south­ west of the City of Villahermosa, State of Chiapas. The well Sitio Grande-1, completed May 8, 1972, found at 4,120 m depth a Middle Cretaceous dolomitic pay zone, over 200 m thick. The well Cactus-1, completed May 9, 1972, found at 3,360 m depth an Upper Cretaceous to Lower Cretaceous calcarenite to dolomitic limestone pay, about 200 m thick. Cactus-1 tested initially 1,694 barrels of oil per day and 5.7 million cubic feet of gas per day through a 8 mm choke. These were the first finds of Cretaceous oil in southeastern Mexico. 2) From the information now on the public record, it is apparent that the magnitude of the petroleum resources of the new province may be second, in the sense of a single province, only to those in the Middle East province.
    [Show full text]