Invasiones en montañas: ¿Cuánto hemos avanzado en los últimos 10 años y cuáles son los desafíos para los ecosistemas de los Andes?

During the last decade, there has been a great interest in understanding the process of invasion of exotic plants in the ecosystems of the Andes mountain range, because they have a high diversity endemic species and are an important source of ecosystem services. Therefore, this review aims to assess the current state of knowledge about the invasion of plants in the mountain ecosystems of the Andes mountain range. Through a systematic quantitative review that I integrate publications made in the periods 1997-2017. The aim was to identify scientific productivity during the last 10 years, the main research trends and understand how global change processes will affect the invasion process. We determined that publications per year increase linearly (R2 = 0.68), being more noticeable during the last 10 years (2008-2017). More than 50% of the publications were concentrated in studies carried out in Andean ecosystems in Chile and Argentina. The most developed themes were new reports of exotic species (18.48%) and the study of anthropic disturbances as agents promoting invasion (16.38%). Based on the research patterns, it was exemplified how the anthropic factors model the patterns of distribution of exotic species in the ecosystems of the Andes and how the patterns of global change will have implications for the redistribution patterns of the exotic species. Finally, we conclude that it is necessary to strengthen experimental studies on climate change, impact assessment and the generation of control and management protocols for exotic species

Inhibición de la activación plaquetaria por derivados de hidroquinonas

39 p.La búsqueda de nuevos compuestos antiplaquetarios es de suma importancia debido a la gran cantidad de morbimortalidad que presentan las enfermedades cardiovasculares donde sus procesos patológicos se asocian con la actividad de diferentes linajes celulares, como ocurre con las plaquetas. Las plaquetas son claves en la hemostasia, es por esto por lo que la alteración de su función o la activación de este componente sanguíneo por un proceso patológico pueden provocar diferentes afecciones dependiendo de a qué nivel o en que sitio se esté afectando. En esta revisión bibliográfica se reclutó información sobre los principales compuestos derivados de hidroquinonas con actividad antiplaquetaria, los cuales actúan a nivel del orgánulo mitocondrial de las plaquetas, con capacidad para ingresar a las mitocondrias y ejecutar una acción antioxidante, además de redox en la cadena transportadora de electrones, lo suficiente para inhibir la activación de las plaquetas

Going up the Andes: patterns and drivers of non-native plant invasions across latitudinal and elevational gradients

The Andes mountain range in South America has a high level of endemism and is a major source of ecosystem services. The Andes is increasingly threatened by anthropogenic disturbances that have allowed the establishment of non-native plants, mainly in the lower elevation areas. However, synergies between climate change and anthropogenic pressure are promoting the spread of non-native plants to higher elevation areas. In this article, we evaluate and identify the main non-native plants invading Andean ecosystems, and assess their taxonomic families, growth forms and distribution patterns. Based on a systematic literature review, we identified the importance of climatic and anthropogenic factors as drivers of non-native species establishment in Andean ecosystems and the main impacts of non-native plants in the Andes. We then identified research gaps across each biogeographic region in the Andes. Finally, we highlight key elements to better tackle the problem of non-native plant invasions in Andean ecosystems, including the need for a systematic monitoring of invasion patterns and spread (e.g. MIREN protocol) and a common policy agenda across international borders for the prevention and management of non-native plants in this highly vulnerable region.Fil: Fuentes Lillo, Eduardo. Universidad de Concepción; Chile. Universiteit Antwerp; BélgicaFil: Lembrechts, Jonas J.. Universiteit Antwerp; BélgicaFil: Barros, Ana Agustina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; ArgentinaFil: Aschero, Valeria. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; ArgentinaFil: Bustamante, Ramiro O.. Universidad de Chile; ChileFil: Cavieres, Lohengrin A.. Universidad de Concepción; ChileFil: Clavel, Jan. Universiteit Antwerp; BélgicaFil: Herrera, Ileana. Universidad Espíritu Santo; EcuadorFil: Jiménez, Alejandra. Universidad de Concepción; ChileFil: Tecco, Paula Andrea. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Instituto Multidisciplinario de Biología Vegetal. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Instituto Multidisciplinario de Biología Vegetal; ArgentinaFil: Hulme, Philip E.. Lincoln University.; Nueva ZelandaFil: Nuñez, Martin Andres. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigaciones en Biodiversidad y Medioambiente. Universidad Nacional del Comahue. Centro Regional Universidad Bariloche. Instituto de Investigaciones en Biodiversidad y Medioambiente; ArgentinaFil: Rozzi, Ricardo. University of North Texas; Estados UnidosFil: García, Rafael A.. Universidad de Concepción; ChileFil: Simberloff, Daniel. University of Tennessee; Estados UnidosFil: Nijs, Ivan. Universiteit Antwerp; BélgicaFil: Pauchard, Aníbal. Universidad de Concepción; Chil

SoilTemp: a global database of near-surface temperature

Current analyses and predictions of spatially-explicit patterns and processes in ecology most often rely on climate data interpolated from standardized weather stations. This interpolated climate data represents long-term average thermal conditions at coarse spatial resolutions only. Hence, many climate-forcing factors that operate at fine spatiotemporal resolutions are overlooked. This is particularly important in relation to effects of observation height (e.g. vegetation, snow and soil characteristics) and in habitats varying in their exposure to radiation, moisture and wind (e.g. topography, radiative forcing, or cold-air pooling). Since organisms living close to the ground relate more strongly to these microclimatic conditions than to free-air temperatures, microclimatic ground and near-surface data are needed to provide realistic forecasts of the fate of such organisms under anthropogenic climate change, as well as of the functioning of the ecosystems they live in. To fill this critical gap, we highlight a call for temperature time series submissions to SoilTemp, a geospatial database initiative compiling soil and near-surface temperature data from all over the world. Currently this database contains time series from 7538 temperature sensors from 51 countries across all key biomes. The database will pave the way towards an improved global understanding of microclimate and bridge the gap between the available climate data and the climate at fine spatiotemporal resolutions relevant to most organisms and ecosystem processes.Additional co-authors: Stuart W. Smith, Robert G. Björk, Lena Muffler, Simone Cesarz, Felix Gottschall, Amanda Ratier Backes, Joseph Okello, Josef Urban, Roman Plichta, Martin Svátek, Shyam S. Phartyal, Sonja Wipf, Nico Eisenhauer, Mihai Pușcaș, Pavel Dan Turtureanu, Andrej Varlagin, Romina D. Dimarco, Krystal Randall, Ellen Dorrepaal, Keith Larson, Josefine Walz, Luca Vitale, Miroslav Svoboda, Rebecca Finger Higgens, Aud H. Halbritter, Salvatore R. Curasi, Ian Klupar, Austin Koontz, William D. Pearse, Elizabeth Simpson, Michael Stemkovski, Bente Jessen Graae, Mia Vedel Sørensen, Toke T. Høye, M. Rosa Fernández Calzado, Juan Lorite, Michele Carbognani, Marcello Tomaselli, T'ai G.W. Forte, Alessandro Petraglia, Stef Haesen, Ben Somers, Koenraad Van Meerbeek, Mats P. Björkman, Kristoffer Hylander, Sonia Merinero, Mana Gharun, Nina Buchmann, Jiri Dolezal, Radim Matula, Andrew D. Thomas, Joseph J. Bailey, Dany Ghosn, George Kazakis, Miguel Angel de Pablo, Julia Kemppinen, Pekka Niittynen, Lisa Rew, Tim Seipel, Christian Larson, James D.M. Speed, Jonas Ardö, Nicoletta Cannone, Mauro Guglielmin, Francesco Malfasi, Maaike Y. Bader, Rafaella Canessa, Angela Stanisci, Juergen Kreyling, Jonas Schmeddes, Laurenz Teuber, Valeria Aschero, Marek Čiliak, František Máliš, Pallieter De Smedt, Sanne Govaert, Camille Meeussen, Pieter Vangansbeke, Khatuna Gigauri, Andrea Lamprecht, Harald Pauli, Klaus Steinbauer, Manuela Winkler, Masahito Ueyama, Martin A. Nuñez, Tudor‐Mihai Ursu, Sylvia Haider, Ronja E.M. Wedegärtner, Marko Smiljanic, Mario Trouillier, Martin Wilmking, Jan Altman, Josef Brůna, Lucia Hederová, Martin Macek, Matěj Man, Jan Wild, Pascal Vittoz, Meelis Pärtel, Peter Barančok, Róbert Kanka, Jozef Kollár, Andrej Palaj, Agustina Barros, Ana Clara Mazzolari, Marijn Bauters, Pascal Boeckx, José Luis Benito Alonso, Shengwei Zong, Valter Di Cecco, Zuzana Sitková, Katja Tielbörger, Liesbeth van den Brink, Robert Weigel, Jürgen Homeier, C. Johan Dahlberg, Sergiy Medinets, Volodymyr Medinets, Hans J. De Boeck, Miguel Portillo‐Estrada, Lore T. Verryckt, Ann Milbau, Gergana N. Daskalova, Haydn J.D. Thomas, Isla H. Myers‐Smith, Benjamin Blonder, Jörg G. Stephan, Patrice Descombes, Florian Zellweger, Esther R. Frei, Bernard Heinesch, Christopher Andrews, Jan Dick, Lukas Siebicke, Adrian Rocha, Rebecca A. Senior, Christian Rixen, Juan J. Jimenez, Julia Boike, Aníbal Pauchard, Thomas Scholten, Brett Scheffers, David Klinges, Edmund W. Basham, Jian Zhang, Zhaochen Zhang, Charly Géron, Fatih Fazlioglu, Onur Candan, Jhonatan Sallo Bravo, Filip Hrbacek, Kamil Laska, Edoardo Cremonese, Peter Haase, Fernando E. Moyano, Christian Rossi, and Ivan Nij

Think globally, measure locally: The MIREN standardized protocol for monitoring plant species distributions along elevation gradients

Climate change and other global change drivers threaten plant diversity in mountains worldwide. A widely documented response to such environmental modifications is for plant species to change their elevational ranges. Range shifts are often idiosyncratic and difficult to generalize, partly due to variation in sampling methods. There is thus a need for a standardized monitoring strategy that can be applied across mountain regions to assess distribution changes and community turnover of native and non-native plant species over space and time. Here, we present a conceptually intuitive and standardized protocol developed by the Mountain Invasion Research Network (MIREN) to systematically quantify global patterns of native and non-native species distributions along elevation gradients and shifts arising from interactive effects of climate change and human disturbance. Usually repeated every five years, surveys consist of 20 sample sites located at equal elevation increments along three replicate roads per sampling region. At each site, three plots extend from the side of a mountain road into surrounding natural vegetation. The protocol has been successfully used in 18 regions worldwide from 2007 to present. Analyses of one point in time already generated some salient results, and revealed region-specific elevational patterns of native plant species richness, but a globally consistent elevational decline in non-native species richness. Non-native plants were also more abundant directly adjacent to road edges, suggesting that disturbed roadsides serve as a vector for invasions into mountains. From the upcoming analyses of time series, even more exciting results can be expected, especially about range shifts. Implementing the protocol in more mountain regions globally would help to generate a more complete picture of how global change alters species distributions. This would inform conservation policy in mountain ecosystems, where some conservation policies remain poorly implemented

Global maps of soil temperature

Research in global change ecology relies heavily on global climatic grids derived from estimates of air temperature in open areas at around 2 m above the ground. These climatic grids do not reflect conditions below vegetation canopies and near the ground surface, where critical ecosystem functions occur and most terrestrial species reside. Here, we provide global maps of soil temperature and bioclimatic variables at a 1-km2 resolution for 0–5 and 5–15 cm soil depth. These maps were created by calculating the difference (i.e. offset) between in situ soil temperature measurements, based on time series from over 1200 1-km2 pixels (summarized from 8519 unique temperature sensors) across all the world\u27s major terrestrial biomes, and coarse-grained air temperature estimates from ERA5-Land (an atmospheric reanalysis by the European Centre for Medium-Range Weather Forecasts). We show that mean annual soil temperature differs markedly from the corresponding gridded air temperature, by up to 10°C (mean = 3.0 ± 2.1°C), with substantial variation across biomes and seasons. Over the year, soils in cold and/or dry biomes are substantially warmer (+3.6 ± 2.3°C) than gridded air temperature, whereas soils in warm and humid environments are on average slightly cooler (−0.7 ± 2.3°C). The observed substantial and biome-specific offsets emphasize that the projected impacts of climate and climate change on near-surface biodiversity and ecosystem functioning are inaccurately assessed when air rather than soil temperature is used, especially in cold environments. The global soil-related bioclimatic variables provided here are an important step forward for any application in ecology and related disciplines. Nevertheless, we highlight the need to fill remaining geographic gaps by collecting more in situ measurements of microclimate conditions to further enhance the spatiotemporal resolution of global soil temperature products for ecological applications

Global maps of soil temperature

Research in global change ecology relies heavily on global climatic grids derived from estimates of air temperature in open areas at around 2 m above the ground. These climatic grids do not reflect conditions below vegetation canopies and near the ground surface, where critical ecosystem functions occur and most terrestrial species reside. Here, we provide global maps of soil temperature and bioclimatic variables at a 1-km² resolution for 0–5 and 5–15 cm soil depth. These maps were created by calculating the difference (i.e., offset) between in-situ soil temperature measurements, based on time series from over 1200 1-km² pixels (summarized from 8500 unique temperature sensors) across all the world’s major terrestrial biomes, and coarse-grained air temperature estimates from ERA5-Land (an atmospheric reanalysis by the European Centre for Medium-Range Weather Forecasts). We show that mean annual soil temperature differs markedly from the corresponding gridded air temperature, by up to 10°C (mean = 3.0 ± 2.1°C), with substantial variation across biomes and seasons. Over the year, soils in cold and/or dry biomes are substantially warmer (+3.6 ± 2.3°C) than gridded air temperature, whereas soils in warm and humid environments are on average slightly cooler (-0.7 ± 2.3°C). The observed substantial and biome-specific offsets emphasize that the projected impacts of climate and climate change on near-surface biodiversity and ecosystem functioning are inaccurately assessed when air rather than soil temperature is used, especially in cold environments. The global soil-related bioclimatic variables provided here are an important step forward for any application in ecology and related disciplines. Nevertheless, we highlight the need to fill remaining geographic gaps by collecting more in-situ measurements of microclimate conditions to further enhance the spatiotemporal resolution of global soil temperature products for ecological applications

Global maps of soil temperature.

Research in global change ecology relies heavily on global climatic grids derived from estimates of air temperature in open areas at around 2 m above the ground. These climatic grids do not reflect conditions below vegetation canopies and near the ground surface, where critical ecosystem functions occur and most terrestrial species reside. Here, we provide global maps of soil temperature and bioclimatic variables at a 1-km2 resolution for 0-5 and 5-15 cm soil depth. These maps were created by calculating the difference (i.e. offset) between in situ soil temperature measurements, based on time series from over 1200 1-km2 pixels (summarized from 8519 unique temperature sensors) across all the world's major terrestrial biomes, and coarse-grained air temperature estimates from ERA5-Land (an atmospheric reanalysis by the European Centre for Medium-Range Weather Forecasts). We show that mean annual soil temperature differs markedly from the corresponding gridded air temperature, by up to 10°C (mean = 3.0 ± 2.1°C), with substantial variation across biomes and seasons. Over the year, soils in cold and/or dry biomes are substantially warmer (+3.6 ± 2.3°C) than gridded air temperature, whereas soils in warm and humid environments are on average slightly cooler (-0.7 ± 2.3°C). The observed substantial and biome-specific offsets emphasize that the projected impacts of climate and climate change on near-surface biodiversity and ecosystem functioning are inaccurately assessed when air rather than soil temperature is used, especially in cold environments. The global soil-related bioclimatic variables provided here are an important step forward for any application in ecology and related disciplines. Nevertheless, we highlight the need to fill remaining geographic gaps by collecting more in situ measurements of microclimate conditions to further enhance the spatiotemporal resolution of global soil temperature products for ecological applications