From Wikipedia,
the free encyclopedia.
Broadly defined, geobiology
is an
interdisciplinary field of
scientific research that
explores interactions between the
biosphere and
lithosphere or
atmosphere. Investigators from
numerous fields are involved in
geobiologic research, including,
but not limited to, such
disciplines as:
paleontology,
microbiology,
mineralogy,
biochemistry,
sedimentology,
genetics,
physiology,
geochemistry (organic and
inorganic), and
atmospheric science. One major
subdiscipline of geobiology is
geomicrobiology, an area of study
that focuses on investigating the
interactions between
microbes and
minerals. Another related area
of research is
astrobiology, an
interdisciplinary field that uses
a combination of geobiological and
planetary science data to
establish a context for the search
for life on other
planets.
One example of geobiological
research in a modern context is
the study of
bacteria that "breathe" metals
such as
manganese and
uranium. These organisms use
metals as terminal
electron acceptors in the same
way that humans use
oxygen. These processes hold
promise as tools for
environmental
bioremediation.
Geobiology also includes
investigations of biosphere/geosphere/atmosphere
interactions throughout Earth's
history, as preserved in the
sedimentary rock record. One
example of such an interaction is
the introduction of oxygen into
the atmosphere by
photosynthetic bacteria. This
oxygenation of Earth's early
atmosphere may have resulted in
the precipitation of banded
iron formations.