How did the evolution of oxygenic photosynthesis influence the temporal and spatial development of the microbial iron cycle on ancient Earth?-Reference-Cited by-同舟云学术

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How did the evolution of oxygenic photosynthesis influence the temporal and spatial development of the microbial iron cycle on ancient Earth?

Published:2019-08 Issue: Volume:140 Page:154-166
ISSN:0891-5849
Container-title:Free Radical Biology and Medicine
language:en
Short-container-title:Free Radical Biology and Medicine

Author:

Schad Manuel,Konhauser Kurt O.,Sánchez-Baracaldo Patricia,Kappler Andreas,Bryce Casey

Funder

German Research Foundation

Natural Sciences and Engineering Research Council of Canada

Royal Society University Research Fellowship

Publisher

Elsevier BV

Subject

Physiology (medical),Biochemistry

Reference221 articles.

1. U-rich Archaean sea-floor sediments from Greenland – indications of > 3700 Ma oxygenic photosynthesis;Rosing;Earth Planet. Sci. Lett.,2004

2. The Paleoproterozoic snowball Earth: a climate disaster triggered by the evolution of oxygenic photosynthesis;Kopp;Proc. Natl. Acad. Sci.,2005

3. 13C-depleted carbon microparticles in > 3700-Ma sea-floor sedimentary rocks from West Greenland;Rosing;Science,1999

4. Questioning the evidence for Earth's oldest fossils;Brasier;Nature,2002

5. Metasomatic origin of quartz-pyroxene rock, Akilia, Greenland, and implications for Earth's earliest life;Fedo;Science,2002

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