Traces of Ancient Life in Oceanic Basalt Preserved as Iron-Mineralized Ultrastructures: Implications for Detecting Extraterrestrial Biosignatures-Reference-Cited by-同舟云学术

Traces of Ancient Life in Oceanic Basalt Preserved as Iron-Mineralized Ultrastructures: Implications for Detecting Extraterrestrial Biosignatures

Published:2023-07-01 Issue:7 Volume:23 Page:769-785
ISSN:1531-1074
Container-title:Astrobiology
language:en
Short-container-title:Astrobiology

Author:

Qu Yuangao¹^ORCID,Yin Zongjun²,Kustatscher Evelyn³⁴⁵^ORCID,Nützel Alexander⁴⁵⁶,Peckmann Jörn⁷^ORCID,Vajda Vivi⁸,Ivarsson Magnus⁸

Affiliation:

1. Institute of Deep-Sea Science and Engineering, Chinese Academy of Sciences, Sanya, China.

2. State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing, China.

3. Museum of Nature South Tyrol, Bozen/Bolzano, Italy.

4. Department für Geo- und Umweltwissenschaften, Paläontologie und Geobiologie, Ludwig-Maximilians-Universität, München, Germany.

5. SNSB-Bayerische Staatssammlung für Paläontologie und Geobiologie, München, Germany.

6. GeoBio-Center, Ludwig-Maximilians-Universität München, München, Germany.

7. Institute für Geologie, Centrum für Erdsystemforschung und Nachhaltigkeit, Universität Hamburg, Hamburg, Germany.

8. Department of Paleobiology, Swedish Museum of Natural History, Stockholm, Sweden.

Publisher

Mary Ann Liebert Inc

Subject

Space and Planetary Science,Agricultural and Biological Sciences (miscellaneous)

Link

https://www.liebertpub.com/doi/pdf/10.1089/ast.2022.0075

Reference101 articles.

1. Raman spectroscopy of alpha-FeOOH (goethite) near antiferromagnetic to paramagnetic phase transition

2. How to obtain a reliable structural characterization of polished graphitized carbons by Raman microspectroscopy

3. Extending the applicability of the Raman carbonaceous-material geothermometer using data from contact metamorphic rocks

4. Multiple sulfur isotope constraints on microbial sulfate reduction below an Archean seafloor hydrothermal system

5. Iron and sulfide oxidation within the basaltic ocean crust: implications for chemolithoautotrophic microbial biomass production