Dispute over first rocks fit for life
Earth's oldest rocks containing what scientists heralded as the earliest evidence for life are under scrutiny. The rocks in question sit on Akilia Island off the southwest coast of Greenland. The island hosts a rock exposure of dark green, almost black, mineral layers alternating with white. Geologists first identified the outcrop as containing banded iron formations: a type of sedimentary rock precipitated from seawater.
  In this week's Science, a new geochemical analysis of the Akilia Island rocks 
  claims the outcrop is not sedimentary but igneous - formed in the mantle under 
  conditions too hot to support life. "It would be like going to Hawaii and 
  seeing a lava fountain and looking for life inside that," says sedimentary 
  geologist Christopher Fedo of George Washington University, in Washington. 
Fedo and Martin 
  Whitehouse of the Swedish Museum of Natural History are casting a shadow of 
  doubt over the earlier work of Stephen Mojzsis of the University of Colorado 
  in Boulder. In 1996, Mojzsis and colleagues identified the rocks as banded iron 
  formations with cross-cuts of tonalite that indicated an age of 3.85 billion-years 
  old. To determine if evidence for life existed in these rocks, some of Earth's 
  oldest, they studied the inclusions of graphite in the Akilia outcrop and concluded 
  that the isotopic signature of the carbon came from biological origins. 
Martin Whitehouse on what he considers distinctly not banded iron formation on Akilia Island. Photo by Chris Fedo.
While Fedo and Whitehouse support analyzing graphite particles for evidence 
  of life in deep-sea sedimentary rocks, they don't believe the Akilia rocks fit 
  the sedimentary requirement. Fedo and Whitehouse identified the white quartz 
  layer as having a geochemistry strongly diluted from, but closely related to, 
  the green pyroxene in the rocks. In the banded iron formation explanation, the 
  pyroxene is considered a secondary intrusion of ultramafic igneous rock, creating 
  veins that are not related to the origin of the white quartz layer. Indeed, 
  Mojzsis says the white layers are quartz-magnetite, impossible to derive from 
  an ultramafic rock. "That would mean a chimera of bizarre geological forces 
  acting on a five-by-50-meter square area of Greenland," Mojzsis says. Fedo 
  and Whitehouse argue that the magnetite makes up only half a meter of the total 
  5 meter-thick lithology, and that the presence of magnetite may have come from 
  a metamorphic breakdown of another mineral or from hydrothermal alteration. 
  
The differences 
  might be linked to looking at a marbled cake and watching bakers argue over 
  its ingredient list. But even when the Akilia rocks are geochemically analyzed 
  the geologists come up with two separate lists. One for a marine sedimentary 
  banded iron formation and the other for a metasomatized ultramafic igneous origin. 
  But Fedo and Whitehouse are distinct in that they take into account the severe 
  deformation of the outcrop, Peter Appel of the Geological Survey of Denmark 
  and Greenland. 
"I have visited the Akilia outcrops several times and was never convinced of the sedimentary origin of the quartz-pyroxene rocks in which the carbon was found," Appel says. "On the contrary a metasomatic origin is very convincing. This is supported by field evidence in the Isua [Greenland] greenstone belt, which is probably of the same age as the Akilia supracrustals."
A helicopter view of the disputed rock 
  exposures on Akilia Island, Greenland. Photo by Chris Fedo. 
Fedo and Whitehouse began working with some 40 other researchers in 1997 to study banded iron formations in Isua. When the weather was too poor for helicopters to fly into Isua, often the scientists would opt for the shorter trip from the airport to Akilia. As they continued to return to Greenland each field season, "the Akilia story had been weighing increasingly on a number of our minds," Fedo says.
"Initially I had no intention to work on this stuff because I thought it was largely a done deal. After a couple of years of revisiting this place I was deeply concerned that the banded iron formation interpretation was wrong. Because the rock doesn't look anything like banded iron formation, at least it didn't to me," he says, adding that "It doesn't physically and it doesn't chemically."
Christina Reed
Link to:
  Science
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