Dolomitized cells within chert of the Permian Assistencia Formation, Parana Basin, Brazil

Author(s)

Calca, Cleber P. ^[1] ; Fairchild, Thomas R. ^[1] ; Cavalazzi, Barbara ^{[2, 3]} ; Hachiro, Jorge ^[1] ; Petri, Setembrino ^[1] ; Gonzalez Huila, Manuel Fernando ^[4] ; Toma, Henrique E. ^[4] ; Araki, Koiti ^[4]

Affiliation

^[1] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, Sao Paulo, SP - Brazil

^[2] Univ Bologna, Dipartimento Sci Biol Geol & Ambientali, Via Zamboni 67, I-40126 Bologna - Italy

^[3] Univ Johannesburg, Dept Geol, Kingsway POB 524, ZA-2006 Johannesburg - South Africa

^[4] Univ Sao Paulo, Inst Quim, Ave Prof Lineu Prestes 748, Sao Paulo, SP - Brazil

• Document type: Journal article
• Source: SEDIMENTARY GEOLOGY; v. 335, p. 120-135, APR 15 2016.
• Web of Science Citations: 4

Abstract

Dolomitic microscopic structures in the form of microspheres, ``horseshoe- shaped{''} objects, and thin botryoidal crusts found within microfossiliferous chert within stromatolites of the Evaporite Bed (EB) of the Permian Assistencia Formation, Irati Subgroup, Parana Basin, Brazil, have been investigated by means of optical microscopy, X-ray fluorescence, scanning electron microscopy, Raman spectrometry and energy-dispersive X-ray spectrometry. The microspheres were identified as dolomitized coccoidal cyanobacteria based on similarity in size, spheroidal and paired hemispheroidal morphologies and colonial habit to co-occurring silicified organic walled cyanobacteria embedded within the same microfabric and rock samples. The co-occurrence of dolomite, pyrite framboids, and abundant dispersed carbonaceous material and silicified cells is consistent with a hypersaline depositional environment with abundant cyanobacterial mats and elevated Mg2+/Ca2+ ratios and reducing conditions with active anoxic microbial processes near the water-(bio)sediment interface. The abundance of extracellular polymeric substances facilitated anoxic microbial processes (sulfate reduction), providing essential conditions for possible primary microbially induced dolomitization. In most of the dolomitized cells dolomite occurs only as an external layer; in fully dolomitized cells magnesium is richest in the outermost layer. Presumably, the dolomitization process was favored by the presence of anoxic microbial degraders and negatively charged functional groups at the surface of the cyanobacterial cells. Botryoidal dolomite rims of silica-filled fenestrae formed by a similar process and inherited the botryoidal morphology of the cell as originally lining the fenestrae. Silicification interrupted the dolomitization of the largely organic biosediment, mostly by permineralization, but locally by substitution, thereby preserving not only dolomitic microspheres, but also huge numbers of structurally well-preserved organic-walled cyanobacteria and portions of microbial mat. Clearly, dolomitization began very early in the microbial mats, prior to compaction of the sediment or full obliteration of cellular remains, followed very closely by silicification thereby impeding continued degradation and providing a window onto very well-preserved Permian microbial mats. (C) 2016 Elsevier B.V. All rights reserved. (AU)