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There have been five major extinction events throughout geological history, resulting in the elimination of biodiversity, followed by a rebound of species that adapted to the new conditions. In the current geological epoch, the Holocene, there is a sixth extinction event in progress. This mass extinction has been attributed to human activities and is thus provisionally called the Anthropocene. In 2019 the human population reached 7.7 billion people and is projected to comprise 10 billion by...
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An ecological disturbance is a temporary disruption in the environment resulting from abiotic, biotic, or anthropogenic factors, causing a pronounced change in an ecosystem. The impact of an ecological disturbance, which can depend on its intensity, frequency, and spatial distribution, plays a significant role in shaping the species diversity within the ecosystem.
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Small population sizes put a species at extreme risk of extinction due to a lack of variation, and a consequent decrease in adaptability. This weakens the chances of survival under pressures such as climate change, competition from other species, or new diseases. Large populations are more likely to survive pressures such as these, as such populations are more likely to harbor individuals that have genetic variants that are adaptive under new stresses. Small populations are much less...
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Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
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Ecological succession is influenced by the processes of facilitation, inhibition, and toleration. Facilitation occurs when early successional species create more favorable ecological conditions for subsequent species, such as enhanced nutrient, water, or light availability. In contrast, inhibition happens when early successional species create unfavorable ecological conditions for potential successive species, such as limiting resource availability. In some cases, later successional species...
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The Sulfur Cycle01:22

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Sulfur, an important element in the chemical makeup of proteins, is recycled through the atmosphere and aquatic and terrestrial environments. Found in the atmosphere as sulfur dioxide (SO2), sulfur is released by decaying organisms, weathered rocks, geothermal vents, volcanos, and burning fossil fuels. It is deposited into the ecosystem, cycled through the biotic community, and either released back into the atmosphere as gas or deposited in marine sediment for long-term storage and eventual...
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¿Qué puso en llamas a Siberia?

Gabriela Schaepman-Strub1, Jin-Soo Kim2

  • 1Department of Evolutionary Biology and Environmental Studies, University of Zürich, Zürich, Switzerland.

Science (New York, N.Y.)
|December 1, 2022
PubMed
Resumen

Los incendios extremos del Ártico ocurrieron entre 2019 y 2021. Estos eventos fueron impulsados por el cambio de las corrientes de aire y el derretimiento de la nieve más temprano de lo habitual, que impactó en la región del Ártico.

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Área de la Ciencia:

  • Ciencias del medio ambiente en el Ártico
  • Ciencias atmosféricas
  • Investigación sobre el cambio climático

Sus antecedentes:

  • La región ártica está experimentando rápidos cambios ambientales.
  • Los incendios forestales son una perturbación significativa en los ecosistemas del Ártico.
  • Comprender las causas de los incendios extremos es crucial.

Objetivo del estudio:

  • Investigar los factores principales que contribuyen a los incendios extremos del Ártico de 2019 a 2021.
  • Para analizar el papel de la circulación atmosférica y los patrones de deshielo.

Principales métodos:

  • Análisis de los datos meteorológicos, incluidos los patrones de las corrientes de aire.
  • Examen del tiempo y la extensión del derretimiento de la nieve mediante imágenes satelitales.
  • Análisis de la correlación entre las variables climáticas y la aparición de incendios.

Principales resultados:

  • Los patrones cambiantes de corriente de aire se identificaron como un factor clave.
  • El deshielo temprano aumentó significativamente la disponibilidad de combustible y el riesgo de incendio.
  • Se estableció un fuerte vínculo entre estos factores y la actividad de incendios extremos.

Conclusiones:

  • Los cambios atmosféricos y criosféricos son críticos para modular los regímenes de fuego del Ártico.
  • Los hallazgos ponen de relieve la vulnerabilidad del Ártico a los eventos extremos provocados por el clima.
  • El futuro riesgo de incendios en el Ártico puede aumentar debido a los cambios climáticos en curso.