Preparing for, coping with and bouncing back after shocks. A nuanced resilience assessment for smallholder farms and farmers in Northern Ghana

Mirja Michalscheck Fred Kizito Carl Timler Jeroen Groot (2023, [Artículo])

Whole-Farm Model Health Shock CIENCIAS AGROPECUARIAS Y BIOTECNOLOGÍA SUSTAINABLE INTENSIFICATION VULNERABILITY SMALLHOLDERS LANDSCAPE TECHNOLOGY

Hot Extremes and Climatological Drought Indicators in the Transitional Semiarid-Subtropical Region of Sinaloa, Northwest Mexico

OMAR LLANES CARDENAS OSCAR GERARDO GUTIERREZ RUACHO Iván Hernández Romano ENRIQUE TROYO DIEGUEZ (2022, [Artículo])

"The main goal of this study was to explore the historical and recent spatial concurrence between the frequency (F), duration (D) and intensity (I) of hot extremes (HEs) and the frequency and evolution of meteorological drought in the region of Sinaloa. Based on the values of daily maximum temperatura (Tmax) and precipitation obtained from CLImate COMputing for the interval April–October of a historical period (1963–2000) and a recent period (1982–2014), the HE and the standardized precipitation index (SPI) were calculated on one-month (SPI-1) and four-month (SPI-4) timescales. Spearman rank correlation coefficients (Sr) were used to obtain the significant concurrences (SCs) between HEs and SPI-1, and HEs and SPI-4. El Quelite weather station showed the highest historical SCs between HEs and SPI-1 (−0.66≤Sr≤−0.57). Jaina is the only station that showed SCs with all four indicators of HEs and SPI-4 (−0.47≤Sr≤−0.34). In this study, the concurrence between HEs and SPI-1, and HEs and SPI-4 was determined for the first time. These are phenomena that can decrease the crop yield, particularly for rainfed crops such as maize, sesame and sorghum in the region commonly known as “the breadbasket of Mexico."

frequency and evolution of meteorological droughts, the breadbasket of Mexico, Sinaloa CIENCIAS FÍSICO MATEMÁTICAS Y CIENCIAS DE LA TIERRA CIENCIAS DE LA TIERRA Y DEL ESPACIO CLIMATOLOGÍA CLIMATOLOGÍA REGIONAL CLIMATOLOGÍA REGIONAL

Metals pollution in El Limón lagoon, Chiapas, Mexico

MARIA TERESA LEAL ASCENCIO SAUL MIRANDA ALONSO Elena María Otazo Sanchez Francisco Prieto García (2009, [Artículo])

La laguna El Limón, en el municipio de Reforma, Chiapas, México, ha presentado mortandad masiva de peces, lo que llevó a realizar un estudio más profundo que determinara el grado de contaminación de la laguna, así como las causas posibles de los eventos. Los resultados muestran que en los sedimentos de la laguna las concentraciones promedio de Zn, Ni, Cr, Cd y Cu rebasan los límites recomendados en Canadá y Estados Unidos para evitar la aparición de efectos biológicos nocivos en especies acuáticas. Es de especial mención la acumulación de Zn, que presenta una concentración máxima de 1360 mg/kg, presumiblemente asociada al uso de este metal como catalizador en una planta procesadora de gas. Si bien las descargas industriales que vierten a la laguna cumplen con los estándares establecidos en México para metales, esto no ha sido suficiente para evitar su acumulación en los sedimentos, lo cual demuestra que las normas existentes para las descargas de aguas residual industrial deben aumentar sus restricciones y tomar en cuenta el tipo de cuerpo receptor al que vierten. En el caso del uso de agua residual o contaminada para riego, la acumulación puede darse en los suelos agrícolas, pasando eventualmente a los cultivos, lo que tampoco es deseable.

Lagunas Contaminación del agua Metales Zinc INGENIERÍA Y TECNOLOGÍA

Calidad del agua de un lago urbano en la Ciudad de México (2015-abril 2017)

Ana Cecilia Tomasini Ortiz MERCEDES ESPERANZA RAMIREZ CAMPEROS Lina Cardoso (2017, [Memoria de congreso])

El lago urbano estudiado, está situado al oeste de la Ciudad de México. La problemática de la eutrofización del lago se agudizó y el lago presentó algunas características del estado de hipertrofía por su someridad y circulación limitada, falta de estratificación, regímenes de nutrientes y oxígeno no balanceado y productividad muy alta, tomando como parámetro concentraciones de Clorofila a. Por tal motivo, después de haber monitoreado el lago durante 2015 y hasta marzo de 2015, se adaptó una planta piloto de coagulación-floculación alimentada con agua del mismo lago para el retiro de algas.

Lagos Zonas urbanas Eutroficación Calidad del agua INGENIERÍA Y TECNOLOGÍA

El proyecto de creación del Estado del Centro, 1870

The project to create the State of the Center, 1870

EVELIN MARES CENTENO (2022, [Artículo])

El 21 de julio de 1870 los principales vecinos de la ciudad de León y el cabildo emprendieron las gestiones necesarias para crear una nueva entidad federativa que llevaría el nombre de Estado del Centro, la cual estaría compuesta por ayuntamientos de los estados de Jalisco y Guanajuato. A pe sar de que se trató de un proyecto político que se llevó a cabo en un momento en el que se estaba reconfigurando la geografía política del país, y de que contaba con los requisitos que solicitaba la Constitución de 1857, no logró consolidarse. Sin embargo, su estudio permite acercarse a conocer el proceso de configuración política del territorio.

On July 21, 1870, the main residents of the city of León and the council, undertook the necessary steps to create a new federal entity that would bear the name of the State of the Center, which would be composed of municipalities of the states of Jalisco and Guanajuato. Despite the fact that it was a political project that was carried out at a time when the

political geography of the country was being reconfigured, and that it had the requirements requested by the 1857 Constitution, it failed to consolidate. However, its study allows us to get closer to knowing the process of political configuration of the territory.

CIENCIAS SOCIALES León, Guanajuato, México Ayuntamiento Lagos Territorio Florencio Antillón, 1830-1903 León, Guanajuato, México Municipalities Lagos Territory Florencio Antillón, 1830-1903

Worldwide selection footprints for drought and heat in bread wheat (Triticum aestivum L.)

Ana Luisa Gómez Espejo Carolina Sansaloni Juan Burgueño Fernando Henrique Toledo Adalberto Benavides-Mendoza M. Humberto Reyes-Valdés (2022, [Artículo])

Genome–Environment Associations Climatic Variables Hormonal Elicitors CIENCIAS AGROPECUARIAS Y BIOTECNOLOGÍA ADAPTATION DROUGHT STRESS HEAT STRESS LANDRACES TRITICUM AESTIVUM

Landscape and micronutrient fertilizer effect on agro-fortified wheat and teff grain nutrient concentration in western Amhara

Tilahun Amede Elizabeth Bailey Abdul Wahab Mossa Dereje Tirfessa MESFIN KEBEDE DESTA Getachew Agegnehu Tesfaye Shiferaw Sida Stephan Haefele R. Murray Lark Martin Broadley Samuel Gameda (2023, [Artículo])

Agronomic biofortification, encompassing the use of mineral and organic nutrient resources which improve micronutrient concentrations in staple crops is a potential strategy to promote the production of and access to micronutrient-dense foods at the farm level. However, the heterogeneity of smallholder farming landscapes presents challenges on implementing agronomic biofortification. Here, we test the effects of zinc (Zn)- and selenium (Se)-containing fertilizer on micronutrient concentrations of wheat (Triticum aestivum L.) and teff (Eragrostis tef (Zucc.) Trotter) grown under different landscape positions and with different micronutrient fertilizer application methods in the western Amhara region of Ethiopia. Field experiments were established in three landscape positions at three sites, with five treatments falling into three broad categories: (1) nitrogen (N) fertilizer rate; (2) micronutrient fertilizer application method; (3) sole or co-application of Zn and Se fertilizer. Treatments were replicated across five farms per landscape position and over two cropping seasons (2018 and 2019). Grain Zn concentration ranged from 26.6 to 36.4 mg kg−1 in wheat and 28.5–31.2 mg kg−1 in teff. Grain Se concentration ranged from 0.02 to 0.59 mg kg−1 in wheat while larger concentrations of between 1.01 and 1.55 mg kg−1 were attained in teff. Larger concentrations of Zn and Se were consistently attained when a foliar fertilizer was applied. Application of ⅓ nitrogen (N) yielded significantly larger grain Se concentration in wheat compared to a recommended N application rate. A moderate landscape effect on grain Zn concentration was observed in wheat but not in teff. In contrast, strong evidence of a landscape effect was observed for wheat and teff grain Se concentration. There was no evidence for any interaction of the treatment contrasts with landscape position except in teff, where an interaction effect between landscape position and Se application was observed. Our findings indicate an effect of Zn, Se, N, landscape position, and its interaction effect with Se on grain micronutrient concentrations. Agronomic biofortification of wheat and teff with micronutrient fertilizers is influenced by landscape position, the micronutrient fertilizer application method and N fertilizer management. The complexity of smallholder environmental settings and different farmer socio-economic opportunities calls for the optimization of nutritional agronomy landscape trials. Targeted application of micronutrient fertilizers across a landscape gradient is therefore required in ongoing agronomic biofortification interventions, in addition to the micronutrient fertilizer application method and the N fertilizer management strategy.

CIENCIAS AGROPECUARIAS Y BIOTECNOLOGÍA BIOFORTIFICATION LANDSCAPE SELENIUM ZINC WHEAT

Estructura del basamento de la Cuenca Farallón al Sur del Golfo de California, mediante la interpretación de datos potenciales y sísmicos

Basement structure of the Farallon Basin at the south of the Gulf of California, through the interpretation of seismic and potential field data

Marco Antonio Bartens Olortegui (2013, [Tesis de maestría])

El Golfo de California es un rift continental activo con apertura oblicua y desplazamiento lateral derecho y es uno de los pocos ejemplos de un rift continental en la fase inicial donde los procesos de apertura activa se pueden estudiar a lo largo de un rift completo. En este escenario, establecer el límite entre basamento continental y oceánico es clave para entender los mecanismos tectónicos que actúan en esta etapa inicial del rift. Desafortunadamente, esta también es una tarea difícil debido a la presencia de corteza oceánica de nueva creación. El objetivo de este trabajo es el de identificar, delimitar y estimar espesores de la corteza oceánica y corteza continental en la cuenca Farallón. Para ellos se utilizaron datos de sísmica de reflexión multicanal 2D de alta resolucion tomados durante la expedicion Ulloa 2006, datos de anomlías gravimetricas tomados de la base de datos de la gravedad marina global obtenida por altimetría de radar relocalizada de los satélites Geosat y ERS-1. Para su interpretación se realizó modelado gravimetrico bidimensional a lo largo de cada perfil sísmico, seguido por una inversión 3D de los datos potenciales del área de la cuenca Farallón restringidos por los perfiles sísmicos interpretados. La corteza de característica oceánica se sitúa en el centro de la cuenca y se identifica principalmente por la concavidad de sus estructuras, interpretadas como sills en las secciones sísmicas, y por la elevada magnitud de la anomalía de Bouguer en el área. La corteza continental se localiza en los margenes oeste y este de la cuenca y se reconoce por la continuidad del reflector correspondiente y el significativo decremento de la anomalía de Bouguer. Tambien se identificaron: una corteza de naturaleza volcánica en el Macizo Farallón Sur (asociado a un reflector sísmico discontinuo de gran amplitud) y dos capas sobreyacientes de sedimentos, la más profunda afectada aparentemente por intrusiones magmáticas. Las profundidades interpretadas con los modelos gravimétricos indican que se tiene una corteza oceánica delgada al centro de la cuenca, con espesores mínimos de 2.5 km en el eje sur abandonado y 3 km en el eje de la dorsal, así como una corteza continental que se va engrosando gradualmente hacia el continente.

The Gulf of California is an active continental rift with an oblique and dextral opening displacement and it is one of the few examples of an initiating continental rift where active opening processes can be studied along a complete rift. In this scenary, establishing the boundary between continental and oceanic basement holds the key to fully understand the tectonic mechanisms acting on this initial rifting stage. Unfortunately, this is also a challenging task due to the presence of oceanic crust of new creation. The aim of this work is to identify, delineate and estimate the thickness of oceanic and continental crusts in the Farallón basin. For this purpose, they were used high-resolution 2D multichannel seismic reflection data from the Ulloa’s 2006 expedition along with gravity anomaly data from the global marine gravity database obtained by repositioned radar altimetry from Geosat and ERS-1 satellites. For their interpretation, two-dimensional gravity modeling was carried out along each seismic profile, followed by 3D inversion of potential field data from the Farallón basin area as constrained by the interpreted seismic profiles. The oceanic-like crust was located at the centre of the basin and is mainly identified by the concavity of their structures, interpreted as sills in the seismic sections, and the highamplitude of the Bouguer anomaly in the area. The continental crust is located in the western and eastern margins of the basin and it is distinguished by the relevant reflector’s continuity and the significant decrease of the Bouguer anomaly. They were also identified: a volcanic crust at the south of the Farallón Massif (associated to a prominent discontinuous seismic reflector) and two overlying sedimentary layers, the deepest one apparently affected by magmatic intrusions. The interpreted depths from the gravity models indicate that there is a thin oceanic crust at the center of the basin, with minimum thicknesses of 2.5 km in the abandoned south axis and 3 km in the dorsal axis, as well as a continental crust that gradually thickens towards the continent.

sísmica de reflexión, anomalía gravimétrica, Cuenca Farallón, Golfo de California seismic reflection, gravity anomaly, Farallon Basin, Gulf of California CIENCIAS FÍSICO MATEMÁTICAS Y CIENCIAS DE LA TIERRA CIENCIAS DE LA TIERRA Y DEL ESPACIO GEOFÍSICA SISMOLOGÍA Y PROSPECCIÓN SÍSMICA SISMOLOGÍA Y PROSPECCIÓN SÍSMICA

Cell carbon content and biomass assessments of dinoflagellates and diatoms in the oceanic ecosystem of the Southern Gulf of Mexico

LORENA PATRICIA LINACRE ROJAS (2021, [Objeto de congreso])

This study assessed the cell carbon content and biomass for genera of dinoflagellates and diatoms in the oceanic ecosystem of the Southern Gulf of Mexico. Carbon content estimates were based on biovolume calculations derived from linear dimension measurements of individual cells and the approximate geometric body shape of each genus. Then, biomass assessments were performed for both groups in two gulf regions (Perdido and Coatzacoalcos) using these carbon content factors and cell abundances. After four seasonal cruises, 11,817 cells of dinoflagellates and 3,412 cells of diatoms were analyzed. Diverse body shapes and cell sizes were observed among 46 dinoflagellate genera and 37 diatom genera. Nano-cells of dinoflagellates (68% <20 μm) and micro-cells of diatoms (77% 20–200 μm, mostly 50–75 μm) were predominant. According to this cell-size structure, on average, diatoms contained 40% more carbon per cell than dinoflagellates. Contrasting carbon content estimates were observed within the genera of both microalgae. Large carbon averages (>10,000 pg C cell-1) were attributed to Gonyaulacal and some occasional genera of dinoflagellates (e.g., Pyrocystis and Noctiluca) and centric diatoms. In contrast, values up to 3 orders of magnitude lower were found for Peridinial and Gymnodinial dinoflagellates and pennate diatoms. Based on these carbon content estimates, which can be considered representative for most of this oceanic ecosystem, seasonal and regional differences were found in the biomass assessments conducted for these functional groups. Overall, dinoflagellates (mostly low-carbon Gymnodinales) had larger depth-integrated biomass than diatoms (mainly rich-carbon centric forms) within the euphotic zone. An exception to it was the late-summer cruise at the Coatzacoalcos region when a surface bloom of centric diatoms was observed in stations influenced by river runoff. This work contributes useful reference information for future ecological studies and models for understanding the biogeochemical functioning of this open-ocean ecosystem. © 2021 Linacre 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.

Carbon, biomass, Oceanic ecosystem, Southern Gulf of Mexico, Mexico CIENCIAS FÍSICO MATEMÁTICAS Y CIENCIAS DE LA TIERRA CIENCIAS DE LA TIERRA Y DEL ESPACIO OCEANOGRAFÍA OCEANOGRAFÍA

“Mexico half way of making”: Carlos Chávez and the foundation of the National Institute of Fine Arts (INBA) (1945-1947)

Ana Garduño (2023, [Artículo, Artículo])

I am focusing on the interaction between a cultural agent, Carlos Chávez, and the government elite, related to the circumstances of the enunciation of a public and official organism, INBA (The National Institute of Fine Arts), because I assume that political relations are fundamental to understand a process that endorsed the official culture as an appendage of politics. In spite of its relevance, this subject has not been studied. Based on archival documentation (at the National Archive of Mexico and the archive of INBA) I am examining the cultural policies derived from the foundation of INBA. Due to the current pandemic situation, it was not possible to consult other documental sources. I am formulating that the concept of “high culture” was at the core of a wider conflict between governmental interests and those of representative social actors, and I conclude that this obstacle would have conferred a major political and symbolical importance to the Institute, and consequently, would restrict its budget.

Carlos Chávez INBA Agentes culturales Políticas institucionales Centralización artística HUMANIDADES Y CIENCIAS DE LA CONDUCTA HUMANIDADES Y CIENCIAS DE LA CONDUCTA Foundation of the National Institute of Fine Arts in Mexico (INBA), Cultural agents Institutional policies Artistic centralization