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The Evidence for Evolution02:55

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Genetic variations accumulating within populations over generations give rise to biological evolution. Evolutionary changes can result in the formation of novel varieties and entire new species. These changes are responsible for the diverse forms of life inhabiting the planet. The evidence for evolution suggests that all living organisms descended from common ancestors.
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Convergent Evolution01:54

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Evolution shapes the features of organisms over time, ensuring that they are suited for the environments in which they live. Sometimes, selection pressure leads to the rise of similar but unrelated adaptations in organisms with no recent common ancestors, a process known as convergent evolution.
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Group polarization is the strengthening of an original group attitude following the discussion of views within a group (Teger & Pruitt, 1967). That is, if a group initially favors a viewpoint, after discussion the group consensus is likely a stronger endorsement of the viewpoint. Conversely, if the group was initially opposed to a viewpoint, group discussion would likely lead to stronger opposition.
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The endosymbiont theory is the most widely accepted theory of eukaryotic evolution; however, its progression is still somewhat debated. According to the nucleus-first hypothesis, the ancestral prokaryote first evolved a membrane to enclose DNA and form the nucleus. Conversely, the mitochondria-first hypothesis suggests that the nucleus was formed after endosymbiosis of mitochondria.
Contrary to the endosymbiont theory, the eukaryote-first hypothesis proposes that the simpler prokaryotic and...
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John H. Renwick first coined the term “synteny” in 1971, which refers to the genes present on the same chromosomes, even if they are not genetically linked. The species with common ancestry tend to show conserved syntenic regions. Therefore, the concept of synteny is nowadays used to describe the evolutionary relationship between species.
Around 80 million years ago, the human and mice lineages diverged from the common ancestor. During the course of evolution, the ancestral...
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Video Experimental Relacionado

Updated: Feb 8, 2026

Competitive Homing Assays to Study Gut-tropic T Cell Migration
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Evolución sincrónica de la temperatura tropical y polar en el Eoceno

Marlow J Cramwinckel1, Matthew Huber2, Ilja J Kocken3

  • 1Department of Earth Sciences, Faculty of Geoscience, Utrecht University, Utrecht, The Netherlands. m.j.cramwinckel@uu.nl.

Nature
|July 4, 2018
PubMed
Resumen

La reconstrucción de los climas del Eoceno con alto dióxido de carbono atmosférico (CO2) ayuda a predecir el cambio climático futuro. Este estudio revela cambios paralelos de temperatura en los océanos tropicales y profundos, impulsados por los gases de efecto invernadero, no por la circulación oceánica.

Área de la Ciencia:

  • Paleoclimatología
  • Modelado del clima
  • Geoquímica

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Sus antecedentes:

  • Comprender los climas cálidos del pasado con alto CO2 atmosférico es vital para las proyecciones futuras del cambio climático.
  • La época del Eoceno (hace 56-34 millones de años) fue la más cálida en 66 millones de años, pero los datos de temperatura tropical continua son escasos.
  • Estudios anteriores establecieron el calor polar del Eoceno, destacando la necesidad de registros de temperatura tropical para cuantificar la evolución del clima global.