Un nuevo rol de los fijadores de nitrógeno en la captura de carbono en el océano 

Artículo: Los diazótrofos son contribuyentes ignorados a la exportación de carbono y nitrógeno al oceáno profundo

Autores: Sophie Bonnet, Mar Benavides, Frédéric A. C. Le Moigne, Mercedes Camps, Antoine Torremocha, Olivier Grosso, Céline Dimier, Dina Spungin, Ilana Berman-Frank, Laurence Garczarek, and Francisco M. Cornejo-Castillo

Te expandes hacia adentro y hacia afuera con cada ola salada, hasta que de repente la idea del almuerzo activa una punzada de hambre. Un rayo de luz sofoca la hambruna, y tomas un saciante bocado de dióxido de carbono acompañado de nitrógeno. Como una bacteria fotosintética fijadora de nitrógeno usas la energía del sol para convertir gas nitrógeno en nutrientes que tú y tus vecinos necesitan.

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Los impactos del calentamiento global en el almacenamiento de carbono en el suelo, la biodiversidad y el rendimiento de los cultivos

Crédito de la imagen: Dominio público (Pexels)

Artículo: La pérdida de carbono orgánico del suelo disminuye la biodiversidad, pero estimula interacciones multitróficas que promueven el metabolismo en el subsuelo.

Autores: Ye Li, Zengming Chen, Cameron Wagg, Michael J. Castellano, Nan Zhang, Weixin Ding.

Pocos problemas son tan urgentes y relevantes para el futuro de nuestra especie como el cambio climático. Cuando consideramos sus devastadores impactos, lo primero en lo que pensamos es en glaciares y osos polares. Sin embargo, una nueva investigación enfoca nuestra atención en organismos mucho más pequeños, los microorganismos, como protagonistas principales en la estabilidad del suelo y la prevención del colapso de la agricultura bajo el calentamiento global. 

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A New Role for Nitrogen Fixers in Oceanic Carbon Sequestration

Paper: Diazotrophs are overlooked contributors to carbon and nitrogen export to the deep ocean

Authors: Sophie Bonnet, Mar Benavides, Frédéric A. C. Le Moigne, Mercedes Camps, Antoine Torremocha, Olivier Grosso, Céline Dimier, Dina Spungin, Ilana Berman-Frank, Laurence Garczarek, and Francisco M. Cornejo-Castillo

You swell up and down with each salty wave, until suddenly, the thought of lunch triggers a pang of hunger. A ray of sunshine stifles the starvation, and you take a satiating bite of carbon dioxide with a side of nitrogen. As a nitrogen-fixing, photosynthetic bacterium you use energy from sunlight to convert nitrogen gas to necessary nutrients for yourself and your neighbors.

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Impacts of global warming on soil carbon storage, biodiversity, and crop yields

Image credit: Public Domain (Pexels)

Paper: Soil organic carbon loss decreases biodiversity but stimulates multitrophic interactions that promote belowground metabolism.

Authors: Ye Li, Zengming Chen, Cameron Wagg, Michael J. Castellano, Nan Zhang, Weixin Ding.

Few issues are as pressing and relevant for the future of our own species as climate change. We may think first about glaciers and polar bears when we consider its devastating impacts. However, new research brings our attention to much smaller organisms, microbes, as major players in stabilizing soils and preventing agriculture from collapsing under global warming.

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Nuevo soporte para el origen de la vida en fumarolas hidrotermales alcalinas

Imagen de la portada: Tapetes blancos floculantes dentro y alrededor de fumarolas blancas extremadamente gaseosas de alta temperatura (>100°C, 212°F) en la Fumarola Champagne. Copyright: CC BY-SA 4.0 a través de wikimedia commons.

Artículo: Chimeneas de óxidos blancos y verdes acumulan ARN en un jardín químico ferruginoso.

Autores: Vanessa Helmbrecht, Maximilian Weingart, Frieder Klein, Dieter Braun, William D. Orsi

Cuando pensamos en mundos extraterrestres, posiblemente evocamos una imágen de vastos oceános con estructuras altas verticales dispersas, como columnas o torres. Al observar imágenes de fumarolas hidrotermales alcalinas, te darás cuenta de que esos mundos extraterrestres no existen solamente en las películas de ciencia ficción. Las fumarolas hidrotermales alcalinas son ambientes marinos profundos abundantes en la Tierra hace más de 4000 millones de años, caracterizados por chimeneas blancas globulares y puntiagudas que se elevan desde el fondo del mar.  Ofrecen una combinación de condiciones químicas en las que pueden haber surgido las primeras formas de vida en la Tierra. Sin embargo, las fumarolas hidrotermales alcalinas se han considerado inhóspitas para la formación de ácidos nucleicos, las moléculas que almacenan información en todas las células vivas. Un artículo nuevo de investigadores de LMU Munich reta esta suposición al proporcionar evidencia clave para la estabilización de ácidos nucleicos en fumarolas hidrotermales alcalinas, un descubrimiento que podría hacer estos ambientes los candidatos más adecuados para el origen de la vida en la Tierra.

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Eunice Foote, the original founder of climate change dynamics

Featured Image: Artist rendition of Eunice Foote conducting research on compressed gasses. Image courtesy Carlyn Iverson, NOAA.  Featured image courtesy GNU Free Documentation License

Papers: Circumstances affecting the heat of the Sun’s rays; Understanding Eunice Foote’s 1856 experiments: heat absorption by atmospheric gases

Authors: Eunice Foote; Joseph Ortiz and Ronald Jackson

“An atmosphere of [carbon dioxide] would give our Earth a high temperature.”

These words were spoken out loud in August of 1856 at the 10th annual meeting of AAAS, though not by their author. The speaker continues on to suggest that, “[if] at one period of its history the air had mixed with [carbon dioxide] a larger proportion than at present, an increased temperature…must have necessarily resulted.” This paper was the first recorded finding of the link between carbon dioxide and global warming, and was discovered by the female physicist and scientist, Eunice Foote. While these findings were remarkable on their own, she synthesized the implications to correctly state that carbon dioxide concentrations in the atmosphere both increase global warming and can explain Earth’s geologic history, specifically regarding the Devonian period1,2.  Despite being on the sidelines of science at the time because of her gender, Eunice Foote provided fundamental and groundbreaking knowledge in the field of gaseous physics. 

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Forests under (mega)fire in the Pacific Northwest

Accompaniment to the Third Pod from the Sun Episode

Featured Image: “Forests under fire” original artwork by Jace Steiner. Used with permission.

Paper: Cascadia Burning: The historic, but not historically unprecedented, 2020 wildfires in the Pacific Northwest, USA

Authors: Matthew Reilly, Aaron Zuspan, Joshua Halofsky, Crystal Raymond, Andy McEvoy, Alex Dye, Daniel Donato, John Kim, Brian Potter, Nathan Walker, Raymond Davis, Christopher Dunn, David Bell, Matthew Gregory, James Johnston, Brian Harvey, Jessica Halofsky, Becky Kerns

The natural legacy of fire in the Pacific Northwest (PNW) is complex.  The variable geography of the wet, westside temperate rain forests, to the dry, high elevation forests beyond the Cascade crest make it difficult to find a “catch-all” description of PNW forest fires.  For instance, drier forests of ponderosa pines in eastern Washington experience more frequent, low-severity fires while the temperate rain forests of western Oregon rarely see fires.  However, scientists can reconstruct historical fire regimes and identify centuries-long patterns of burning related to precipitation, temperature, and ignition frequency to define what are historical patterns and what is modern climate change.  In 2020, multiple megafires (a wildfire that burnt more than 100,000 acres of land) broke out in the typically wet parts of Oregon and Washington, burning more than 700,000 acres combined.  This event is called the 2020 Labor Day Fires, and Matthew Reilly and colleagues have revealed these fires were likely part of historical regimes and not a product of accelerated climate change.

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We’re Here Because We’re Here Because… of Chance?

A painting of many stars as in a night sky, surrounded by planets, with their orbits drawn out.

Featured image: An artist’s depiction of many, many possible planets. This image was created by the European Southern Observatory (ESO).

Paper: Tyrrell, T. Chance played a role in determining whether Earth stayed habitable. Commun Earth Environ 1, 61 (2020). https://doi.org/10.1038/s43247-020-00057-8

Have you ever stayed up at night and wondered, why am I here? Or, more broadly, why are we here, including all living things on this Earth? Don’t worry, you’re not alone, and scientists like Professor Toby Tyrrell of the University of Southampton (UK) have been trying to answer these questions using the scientific method.

His conclusion? It may have just been the luck of the draw. After all, if we weren’t here in the first place, we couldn’t wonder why we were. (Scientists call this the weak anthropic principle.)

Climate scientists often describe their models as alternate (climate) histories. Tyrrell’s 2020 paper takes this idea to its ultimate conclusion, running 100 alternate climate histories on 100,000 randomly generated planets within the habitable zone of their randomly generated stars for 3 billion years. The question he’s trying to help answer is this: how likely was it that the Earth’s climate stayed habitable for the 4 billion years between the evolution of the first prokaryotic cells and us? Was it due to some intrinsic properties of planet Earth, or of life, or was it merely chance?

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Methanotrophs: Nature’s catalytic converters

Featured image: A car exhaust pipe, by Matt Boitor on Unsplash.

Paper: Microbial methane oxidation efficiency and robustness during lake overturn

Authors: M. Zimmerman, M. Mayr, H. Bürgmann, W. Eugster, T. Steinsberger, B. Wehrli, A. Brand, D. Bouffard

If you own a car, you’re likely aware that your engine emits greenhouse gases to the atmosphere. Although we usually think of cars and other human activities as the primary source of such greenhouse gases, living ecosystems can also produce these gases through natural processes. For example, lakes are an important global source of methane, a potent greenhouse gas produced in lake sediments as organic matter decomposes. In their recent paper, Zimmerman and colleagues focus on a small but mighty team of microbes that work hard to limit the amount of methane emitted from lakes.

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The surprising effects rivers have on our atmosphere

Featured Image: Rio Bermejo meeting up with the Paraguay River, on the boarder of Formosa and Chaco Provinces.  Image by Mapio. Used with permision.

Paper: Fluvial organic carbon cycling regulated by sediment transit time and mineral protection

Authors: Marisa Repasch, Joel S. Scheingross, Niels Hovius, Maarten Lupker, Hella Wittmann, Negar Haghipour, Darren R. Gröcke, Oscar Orfeo, Timothy I. Eglinton, and Dirk Sachse

In our current era of rapid climate change, it is critical we understand how every aspect of the Earth system affects carbon cycling.  New work by Marisa Repasch and colleagues shows that rivers, under the right conditions, might be able to sequester more carbon in the sediments than released into the atmosphere. However, these findings may reveal how human impacts to rivers will likely increase the amount of carbon released to the atmosphere.

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