Early Life on Earth: The Ancient Fossil Record

2004 ◽  
pp. 287-316 ◽  
Author(s):  
Frances Westall
2006 ◽  
Vol 5 (4) ◽  
pp. 333-342 ◽  
Author(s):  
David Wacey ◽  
Nicola McLoughlin ◽  
Owen R. Green ◽  
John Parnell ◽  
Crispin A. Stoakes ◽  
...  

The recognition and understanding of the early fossil record on Earth is vital to the success of missions searching for life on other planets. Despite this, the evidence for life on Earth before ~3.0 Ga remains controversial. The discovery of new windows of preservation in the rock record more than 3.0 Ga would therefore be helpful to enhance our understanding of the context for the earliest life on Earth. Here we report one such discovery, a ~3.4 Ga sandstone at the base of the Strelley Pool Formation from the Pilbara of Western Australia, in which micrometre-sized tubular structures preserve putative evidence of biogenicity. Detailed geological mapping and petrography reveals the depositional and early diagenetic history of the host sandstone. We demonstrate that the depositional environment was conducive to life and that sandstone clasts containing putative biological structures can be protected from later metamorphic events, preserving earlier biological signals. We conclude from this that sandstones have an exciting taphonomic potential both on early Earth and beyond.


2007 ◽  
Vol 158 (3-4) ◽  
pp. 198-227 ◽  
Author(s):  
Abigail C. Allwood ◽  
Malcolm R. Walter ◽  
Ian W. Burch ◽  
Balz S. Kamber

1998 ◽  
Vol 4 ◽  
pp. 255-285 ◽  
Author(s):  
Emily A. Cobabe

The exploration of chemosynthetic communities in the geologic record over the last ten years has generated a series of sedimentological, tectonic and geochemical criteria that help define a continuum of environments from hot hydrothermal vents to nearshore geothermal deposits. Many of these studies have used stable isotope geochemistry to uncover a depleted carbon signature that characterizes most fossil chemosynthetically derived deposits. Isotope geochemistry (carbon, nitrogen and sulfur) as been an important thread in the story of the discovery of modern chemosynthetic communities, as well, adding to understanding of the biogeochemistry of these ecosystems. With increasing awareness of the prominence of these communities, not just as a biological novelty, but as a fundamental component of life on Earth (and perhaps elsewhere), the drive to develop geochemical proxies for chemosynthetic taxa in the fossil record intensifies. Increased ability to recognize these communities provides access to a second tier of paleobiological questions, including ideas of evolutionary history and selective advantage.


2011 ◽  
Vol 59 (10) ◽  
pp. 1093-1106 ◽  
Author(s):  
Frances Westall ◽  
Frédéric Foucher ◽  
Barbara Cavalazzi ◽  
Sjoukje T. de Vries ◽  
Wouter Nijman ◽  
...  
Keyword(s):  

2016 ◽  
Vol 18 (30) ◽  
pp. 20033-20046 ◽  
Author(s):  
Sankar Chatterjee

Submarine hydrothermal vents are generally considered as the likely habitats for the origin and evolution of early life on Earth.


1991 ◽  
Vol 9 (1) ◽  
pp. 51-66 ◽  
Author(s):  
Eleanora Iberall Robbins ◽  
Arthur S. Iberall
Keyword(s):  

1987 ◽  
Vol 18 ◽  
pp. 1-19
Author(s):  
Jere H. Lipps

Perhaps two of the most important groups of fossils are the prokaryotes and protists, both single-celled organisms. They are not spectacular fossils and so may be less interesting to students than the more complicated metazoans and metaphytes, yet these two groups not only dominate life on Earth today, but they contribute enormously to our understanding of Earth and life history. Prokaryotes dominated the fossil record of Earth from 3.5 to nearly .5 billion years ago (Knoll, 1985). For the last 1.5 billion years, protists have been an important element in marine and probably other ecosystems.


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