Archives

Geobiology: May 2013


The Antarctic continental ice cap came into existence during the Oligocene epoch, some 33.6 million years ago, according to data from an international expedition led by the Andalusian Institute of Earth Sciences (IACT)--a Spanish National Research Council-University of Granada joint centre. These findings, based on information contained in ice sediments from different depths, have recently been published in the journal Science.

The widespread disappearance of stromatolites, the earliest visible manifestation of life on Earth, may have been driven by single-celled organisms called foraminifera.

Please join us for the NAI Early Earth Focus Group Workshop Without Walls on "The Hadean Earth-Moon System". The workshop is aimed at providing the most up-to-date science on the first billion years' history of the Earth-Moon system, from solar system formation at 4.567 Ga to the widespread preservation of crustal rocks at 3.5 Ga to evidence for life preserved within those rocks.