4.5 Review

Eukaryogenesis and oxygen in Earth history

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Summary: Oxygen is the ultimate oxidant on Earth, and microorganisms have evolved the ability to respire oxygen at extremely low levels, even in seemingly anoxic habitats. Recent advances in O-2 sensing and DNA/RNA sequencing technologies have revealed that microbial respiration of O-2 at nanomolar concentrations is ubiquitous and drives microbial activity. This discovery is changing our understanding of biogeochemical cycling in oxygen-limited environments.

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Changle Wang et al.

Summary: Earth's surface has undergone a prolonged oxidation process, which has had a profound impact on the biosphere. Research shows that the oxygen levels in shallow marine environments were low in the Proterozoic era and gradually increased afterwards, coinciding with the rise of complex eukaryotic ecosystems.

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Article Multidisciplinary Sciences

Intracellular bound chlorophyll residues identify 1 Gyr-old fossils as eukaryotic algae

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Summary: This study reports a new integrative methodology using synchrotron-based X-ray fluorescence and absorption to identify chlorophyll derivatives preserved in rocks from multicellular eukaryotes dating back to approximately 1 billion years ago. This discovery provides new insights into the evolution of photosynthesis and the diversification of early ecosystems.

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Summary: Based on chemical datasets and mineral characteristics, it is suggested that oxygen levels in the environment were very low approximately 150 million years before the Great Oxygenation Event (GOE), and the presence of certain redox-sensitive elements actually developed during postdepositional events.

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Site-and-branch-heterogeneous analyses of an expanded dataset favour mitochondria as sister to known Alphaproteobacteria

Sergio A. Munoz-Gomez et al.

Summary: The study determines the evolutionary relationship between mitochondria and their closest bacterial relatives, suggesting that mitochondria are sister to the Alphaproteobacteria. Understanding this relationship helps in understanding the ancestral mitochondrial symbiosis and its role in the origin of eukaryotes.

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Summary: This article examines the origin and diversification of eukaryotes in the Proterozoic Era. Through the integration of fossils, organic biomarkers, molecular clocks, phylogenies, and redox proxies, the study suggests that eukaryotes likely emerged in aerobic environments in the Proterozoic Era. The article emphasizes the importance of integrating biological and geological evidence and analyzing points of agreement and contention to gain new insights into the origin and early evolutionary history of this important group.

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Simon W. Poulton et al.

Summary: The rise of atmospheric oxygen had a significant impact on the chemistry of surficial environments and Earth's habitability. Research indicates that atmospheric oxygen levels continued to fluctuate around 2.32 billion years ago, correlating with major perturbations in ocean redox chemistry and climate. Ultimately, permanent atmospheric oxygenation was achieved around 2.22 billion years ago, about 100 million years later than previously estimated.

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The Proterozoic macrofossil Tawuia as a coenocytic eukaryote and a possible macroalga

Qing Tang et al.

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Summary: Experimental research on the decay of organelles in red and green algae suggests that chloroplasts are more resistant to decay than nuclei, while pyrenoids are unlikely to be preserved. This indicates potential differential organelle preservation in seed plants and prompts a reevaluation of the early eukaryotic fossil record.

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