The term "stromatolite" was coined by Kalkowsky (1908) while describing coastal paleoenvironments of a Lower Triassic (Buntsandstein) epicontinental sea. Stable, finely laminated structures appeared together with massive deposits of shoaling ooid sands, and later consolidated into rocks ("Stromatolith und Oolith"). © 2011 Springer Berlin Heidelberg.
CITATION STYLE
Radtke, G., & Golubic, S. (2011). Microbial euendolithic assemblages and microborings in intertidal and shallow marine habitats: Insight in cyanobacterial speciation. Lecture Notes in Earth Sciences, 131, 233–263. https://doi.org/10.1007/978-3-642-10415-2_16
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