Geology Lessons - 3 - Bacteria Microfossils

Bacteria - The Fossil Record
It may seem surprising that bacteria can leave fossils at all. However, one particular group of bacteria, the cyanobacteria or "blue-green algae," have left a fossil record that extends far back into the Precambrian - the oldest cyanobacteria-like fossils known are nearly 3.5 billion years old, among the oldest fossils currently known. Cyanobacteria are larger than most bacteria, and may secrete a thick cell wall. More importantly, cyanobacteria may form large layered structures, called stromatolites (if more or less dome-shaped) or oncolites (if round). These structures form as a mat of cyanobacteria grows in an aquatic environment, trapping sediment and sometimes secreting calcium carbonate. When sectioned very thinly, fossil stromatolites may be found to contain exquisitely preserved fossil cyanobacteria and algae.
(We met a living cyanobacteria and its fossil relation from Australia in the Introduction.)
The group shows what is probably the most extreme conservatism of morphology of any organisms.

Aside from cyanobacteria, identifiable fossil bacteria are not particularly widespread. However, under certain chemical conditions, bacterial cells can be replaced with minerals, notably pyrite or siderite (iron carbonate), forming replicas of the once-living cells, or pseudomorphs. Some bacteria secrete iron-coated sheaths that sometimes fossilize. Others may bore into shells or rocks and form microscopic canals within the shell; such bacteria are referred to as endolithic, and their borings can be recognized all through the Phanerozoic. Bacteria have also been found in amber -- fossilized tree resin -- and in mummified tissues. It is also sometimes possible to infer the presence of disease-causing bacteria from fossil bones that show signs of having been infected when the animal was alive. Perhaps most amazing are the fossils left by magnetobacteria -- a group of bacteria which form tiny, nanometer-sized crystals of magnetite (iron oxide) inside their cells. Magnetite crystals identifiable as bacterial products have been found in rocks as old as two billion years -- at a size of a few hundred millionths of a meter, these hold the record for the smallest fossils.

Endolithic Bacteria:


This is an electron micrograph taken using the UCMP Environmental Scanning Electron Microscope. It shows an extreme close-up of a bryozoan from Bahia de Animas, Baja California, Mexico. The calcareous shell of the bryozoan is perforated with a network of channels and tunnels, made by bacteria that bore into such shells. Such trace fossils have been found all through the last 600 million years of the fossil record, and add a new dimension to the study of the history of bacterial life.

Next time, the cyanobacteria, our friends. They even have their own website.

Need to know more: Here comes a discussion of bacteria.
OO OO OO OO OO OO OO!!!!!!