Oncolites are sedimentary structures composed of oncoids, which are layered structures formed by the growth of one or more species of microorganisms,[1] usually containing cyanobacteria.[2] Oncolites are very similar to stromatolites, but, instead of forming columns, they form approximately spherical structures.[3] The oncoids often form around a central nucleus, such as a shell fragment,[4] and a calcium carbonate structure is deposited by encrusting microbes. Oncolites are indicators of warm waters in the photic zone, but are also known in contemporary freshwater environments.[5] These structures rarely exceed 10 cm in diameter.
Oncolites may have either a porostromate or spongiostromate texture. Most oncolites are spongiostromate, having no recognisable cellular texture or microstructure. Porostromate oncolites are mostly unknown during the Precambrian; since the Eocene they have mostly been confined to freshwater environments.[6]
Distribution
The appearance of recent or near-recent freshwater oncoids has been documented in two rivers in Bavaria: the Alz, whose source is the Chiemsee, and the Moosach, near Freising.[7][8][9] Modern oncoids also grow in some springs in Atacama Desert in South America. In one particular case a system of oncoids have been observed interface between Salar de Antofalla and an adjacent wetland.[10]
^Gutschick, R. C.; Perry, T. G. (1959). "Sappington (Kinderhookian) Sponges and Their Environment". Journal of Paleontology. 33 (6): 977–985. JSTOR1300833.
^Hägele, Daniela (2007). Morphogenese, Wachstum und Ökologie der modernen Süßwasser-Onkoide der Alz (Thesis). Ludwig-Maximilians-Universität München. doi:10.5282/edoc.8314.
^E. Rott (1994), "Der Algenaufwuchs in der Oberen Alz (Oberbayern)"(Online-Version; pdf-Datei; 7,6 MB), Berichte des Naturwissenschaftlich-medizinischen Vereins in Innsbruck (in German), vol. 81, Innsbruck, pp. 229–253