Young Graphite in Old Rocks Challenges the Earliest Signs of Life

The team -- which includes researchers from Boston College, the Carnegie Institution of Washington, NASA's Johnson Space Center and the Naval Research Laboratory -- says new evidence from Canada's Hudson Bay region shows carbonaceous particles are millions of years younger than the rock in which they're found, pointing to the likelihood that the carbon was mixed in with the metamorphic rock later than the rock's earliest formation -- estimated to be 3.8 to 4.2 billion years ago.

The samples come from the Nuvvuagittuq Supracrustal Belt, a sedimentary banded iron formation located in the Archean Superior craton, one of Earth's ancient continental shields. Samples were subjected to a range of high-tech tests in an effort to more clearly characterize the carbon in the rock.

Traditional techniques used by scientists have involved collecting samples and crushing them into powder and then determining the bulk characteristics of carbon minerals. The new approach relies upon a variety of microscopy and spectroscopy methods to characterize intact micro-fabricated cross-sections of crystalline graphite removed from the rock samples. The results found that the carbon was very young compared to the age of these oldest rock samples ever unearthed.

"The characteristics of the poorly crystalline graphite within the samples are not consistent with the metamorphic history of the rock," said Boston College Assistant Professor of Earth and Environmental Sciences Dominic Papineau, a co-author of the report. "The carbon in the graphite is not as old as the rock. That can only ring a bell and require us to ask if we need to reconsider earlier studies."

Nearly 4,000-million years old samples from Greenland have been used to develop the dominant time line regarding the emergence of the earliest biosphere. The recent findings suggest the biosphere may have emerged millions of years later, a hypothesis that now demands a rigorous study, said Papineau.

"It could be that researchers in the field need to go back to Greenland to restudy these rocks and determine if the the carbonaceous materials are in fact as old as the metamorphosed rock itself," Papineau said.