Australia: The Land Where Time Began

A biography of the Australian continent 

Bitter Springs Formation                                        

Eastern MacDonnell Ranges, central Australia. Dating to more than 850 million years old, the Bitter Springs Formation contains chert beds which have yielded some of our best and most diverse Proterozoic fossils. These include thirty species of microfossil, with more than a dozen cyanobacteria, a couple of chlorophycean algae, and an assortment of possible fungi, dinoflagellates, and heterotrophic bacteria.

Bitter Springs strata are exposed at the northeastern end of the Amadeus Basin, in central Australia. The formation is composed largely of dark limestone and dolomite, and contains black chalcedonic chert in fine laminated layers. The formation has yielded numerous fossils of stromatolites in addition to microfossils.

The microfossils of Bitter Springs are amazingly well-preserved. Thin sections of fossiliferous chert make it possible to view their three-dimensional morphology. This exceptional situation is the result of the fine-grained way in which the cherts formed, through chemical precipitation. However, though the fossils are morphologically preserved, infra-red spectroscopy shows that the organic materials have been geochemically altered.

The Bitter Springs microbiota was one of the earliest successful demonstrations that fossils could be found in Precambrian rocks, and along with fossils found in the Gunflint chert of Ontario, Canada, revolutionized thinking about what evidence of early life might be available to be found. J. William Schopf, who published the first extraordinary findings from this locality, attributes this revolution to four factors: widespread attempts to radiometrically date Precambrian strata; the realization that cherts might preserve delicate fossils; successful searches for biologically significant compounds in Precambrian rocks; and the use of electron microscopy.

Fossils from Bitter Springs are also important for two others reasons. First, they show that the cyanobacteria were present in morphologically modern forms, and were quite diverse from an early date. With additional evidence demonstrating that stromatolites are the products of cyanobacterial activity, it is now believed that the cyanobacteria diversified early and spread globally, becoming important players in the history of early life on Earth. The fact that recognisable forms appear in rocks nearly 1,000 million years old is a remarkable case of morphological conservatism. Perhaps cyanobacteria are simply successful in the forms they acquired early in their evolution, or perhaps they possess some mechanism of genetic stability which has caused them to remain physically unchanged since that time.

Second, and perhaps even more important, it was at Bitter Springs that the first convincing evidence of early eukaryote fossils was found. Some of the larger cells have preserved internal structures comparable to nuclei and pyrenoids, upon which basis they were assigned to the green algae. While it is possible that the inclusions are artefacts of preservation, other lines of evidence, such as molecular sequence data, have established that eukaryotic cells had evolved by this time.

Evidence for the presence of cells produced by meiosis, the basis of sexual reproduction, is found in the y-shaped stigma, marks on the walls of some cells that results from the formation of tetrads during meiosis. These cells are some of the earliest signs that sexual reproduction had already evolved in the Precambrian, about 900 million years ago.

Sources & Further reading

  • J. W. Schopf. 1968. Microflora of the Bitter Springs Formation, Late Precambrian, central Australia. Journal of Paleontology 42(3):651-688.
  • J. W. Schopf. 1992. Atlas of representative Proterozoic microfossils. Pp. 1055 - 1117 In J.W. Schopf & C. Klein (eds.) "The Proterozoic Biosphere: A Multidisciplinary Study". Cambridge Univ. Press, Cambridge.



Author: M. H. Monroe
Last Updated 25/02/2011 



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