Biogenic and abiogenic graphite in minerals and rocks of the early earth

Research output: Chapter in Book/Report/Conference proceedingChapter

Abstract

Minerals and rocks older than 3.7 billion years in age have attracted investigators looking to find evidence for traces of life. However, ancient rocks are heavily metamorphosed, leaving only graphitized organic matter. In addition, abiogenic graphite is ubiquitous in ancient rocks, creating difficulties for researchers seeking to claim true traces of life. Previous investigations searching for traces of life, based in Jack Hills (Australia), Akilia and Isua (Greenland), and Nuvvuagittuq (Canada), are summarized in this chapter. Graphite accompanied by low δ13C values was found at all these localities. However, whether or not this graphite has a biogenic origin is the subject of debate. Rocks from the >3.7 Ga Isua supracrustal belt provide robust evidence of traces of life in the form of well-preserved sedimentation features of reduced carbon accompanied by low δ13C values. The occurrence of graphite with low d13C values in ancient rocks cannot be used to indicate the presence of a microbial biosphere on the early Earth unless the age of the carbonaceous material is confirmed as the same age of host rock sedimentation.

Original languageEnglish
Title of host publicationAstrobiology
Subtitle of host publicationFrom the Origins of Life to the Search for Extraterrestrial Intelligence
PublisherSpringer Singapore
Pages209-227
Number of pages19
ISBN (Electronic)9789811336393
ISBN (Print)9789811336386
DOIs
Publication statusPublished - 2019 Jan 1

Keywords

  • Archean
  • Biogenic graphite
  • Biosphere
  • Early earth
  • STEM

ASJC Scopus subject areas

  • Agricultural and Biological Sciences(all)
  • Physics and Astronomy(all)
  • Immunology and Microbiology(all)
  • Earth and Planetary Sciences(all)

Fingerprint Dive into the research topics of 'Biogenic and abiogenic graphite in minerals and rocks of the early earth'. Together they form a unique fingerprint.

Cite this