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Anoxygenic photosynthesis is a phototrophic process that captures light energy to drive carbon fixation without producing molecular oxygen. Unlike oxygenic photosynthesis, which utilizes water as an electron donor and releases oxygen, anoxygenic phototrophs use alternative electron donors such as hydrogen sulfide (H₂S), elemental sulfur (S⁰), or thiosulfate (S₂O₃²⁻). This process is carried out by diverse groups of bacteria, including purple bacteria, green...
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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.
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Archaea, one of the three domains of life, exhibit remarkable diversity and adaptability, thriving in both extreme and moderate environments. Historically, most identified archaea have been classified into two major phyla: Euryarchaeota and Crenarchaeota. However, recent molecular studies have expanded this classification to include three additional phyla: Thaumarchaeota, Nanoarchaeota, and Korarchaeota, each exhibiting unique characteristics and ecological roles.Thaumarchaeota: Mesophiles...
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Archaea, named after the Archaean eon, represent a unique domain of life, distinct from bacteria and eukaryotes, with remarkable traits. Their cellular and molecular features, ecological adaptability, and industrial relevance highlight their importance in understanding life processes and leveraging biotechnology.Cellular and Molecular CharacteristicsA defining feature of archaea is their unique membrane composition. Archaeal membranes contain ether-linked isoprenoid lipids, which confer...
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Archaea, a domain of single-celled microorganisms, are classified into five major phyla based on genetic and biochemical characteristics: Euryarchaeota, Crenarchaeota, Thaumarchaeota, Korarchaeota, and Nanoarchaeota. Among these, the phylum Euryarchaeota is notable for its remarkable diversity in morphology, metabolism, and ecological adaptations.Morphological and Metabolic DiversityMembers of Euryarchaeota exhibit a variety of cellular shapes, including rods and cocci. Their metabolic pathways...
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Updated: Dec 21, 2025

Anaerobic Growth and Maintenance of Mammalian Cell Lines
07:15

Anaerobic Growth and Maintenance of Mammalian Cell Lines

Published on: July 21, 2018

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Anoxic ecosystems and early eukaryotes.

Susannah M Porter1, Heda Agić1, Leigh Anne Riedman1

  • 1Department of Earth Science, University of California at Santa Barbara, Santa Barbara, CA 93106, U.S.A.

Emerging Topics in Life Sciences
|May 16, 2020
PubMed
Summary
This summary is machine-generated.

Early eukaryotes may have thrived in anoxic oceans, challenging the assumption they needed oxygen. This research explores their adaptation to oxygen-poor environments during the Proterozoic Eon.

Keywords:
Proterozoicanoxicmicrobial eukaryotesorganic-walled microfossilsoxygenprotists

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Area of Science:

  • Paleobiology
  • Geochemistry
  • Microbial Ecology

Background:

  • Proterozoic oceans were largely anoxic, with oxygenated habitats limited to surface waters.
  • Eukaryotes were traditionally thought to be restricted to these oxygenated zones, hindering diversification.
  • Modern microbial eukaryotes inhabit anoxic environments, often via symbiotic relationships.

Purpose of the Study:

  • To propose that early eukaryotes were adapted to anoxic conditions, not just aerobic ones.
  • To explain the discrepancy between early eukaryotic body fossils and later sterane biomarker records.
  • To offer a new perspective on the ecological niches of early eukaryotes.

Main Methods:

  • Analysis of microfossil records in Proterozoic shales.
  • Examination of redox-proxy data from ancient marine sediments.
  • Comparison of modern anoxic eukaryote ecology with the Proterozoic fossil record.

Main Results:

  • Suggests early eukaryotes could have flourished in anoxic Proterozoic oceans.
  • Proposes anoxic adaptation explains the delayed appearance of diverse sterane biomarkers.
  • Provides a potential explanation for the disappearance of certain eukaryotic taxa when oxygen levels rose.

Conclusions:

  • Early eukaryotes may have been more widespread and diverse in anoxic environments than previously assumed.
  • The evolution and diversification of eukaryotes might not have been solely dependent on widespread oxygenation.
  • Revisiting the Proterozoic fossil and geochemical record with an anoxic adaptation hypothesis is warranted.