The
biosphere is the global sum of all
ecosystems. It can also be termed as the zone of
life on
Earth, a closed system (apart from solar and cosmic radiator and heat from the interior of the Earth), and largely self-regulating. By the most general
biophysiological definition, the biosphere is the global
ecological system integrating all living beings and their relationships, including their interaction with the elements of the
lithosphere,
geosphere,
hydrosphere, and
atmosphere. The biosphere is postulated to have
evolved, beginning with a process of
biopoesis (life created naturally from non-living matter such as simple organic compounds) or
biogenesis (life created from living matter), at least some 3.5 billion years ago. The earliest evidence for
life on Earth includes
biogenic graphite found in 3.7 billion-year-old
metasedimentary rocks from
Western Greenland and
microbial mat fossils found in 3.48 billion-year-old
sandstone from
Western Australia. More recently, in 2015, "remains of
biotic life" were found in 4.1 billion-year-old rocks in Western Australia. According to one of the researchers, "If life arose relatively quickly on Earth ... then it could be common in the
universe."