• Corpus ID: 38029620

Inherent problems of terminology : definition of terms frequently used in connection with microbial mats

@inproceedings{Bouougri2007InherentPO,
  title={Inherent problems of terminology : definition of terms frequently used in connection with microbial mats},
  author={El Hafid Bouougri and Gisela Gerdes and Hubertus Porada},
  year={2007}
}
Like all branches of the earth sciences, the study of microbial mats and the features they leave behind preserved within clastic sediments of various calibers, is rife with terminology. As terms are used over several decades, the original meanings often become more imprecise as shades of meaning are added to an initial definition. One example examined briefly here is the term ‘wrinkle mark’, discussed in greater detail in section (a) of this chapter. 
An Ichnotaxonomic Approach to Wrinkled Microbially Induced Sedimentary Structures
ABSTRACT Microbially induced sedimentary structures (MISS) are an important facet of recent paleoichnological work because of their taphonomic implications. MISS are extensively studied in terms of
Palaeoecological, sedimentological and stratigraphical insights into microbially induced sedimentary structures of the lower Cambrian successions of Iran
Micro‐organisms producing microbially induced sedimentary structures, particularly epibenthic cyanobacteria, are not facies‐dependent and could flourish in any environment if appropriate ecological
Implications of microbial mat induced sedimentary structures (MISS) in carbonate rocks: An insight from Proterozoic Rohtas Limestone and Bhander Limestone, India
  • Adrita Choudhuri
  • Environmental Science, Geography
    Journal of Earth System Science
  • 2020
A variety of microbial mat induced sedimentary structures (MISS) occur in the basal part of the Mesoproterozoic Rohtas Limestone and the Bhander Limestone, India. The combined outcrop and
Suspected microbial-induced sedimentary structures (MISS) in Furongian (Upper Cambrian; Jiangshanian, Sunwaptan) strata of the Upper Mississippi Valley
The Furongian (Upper Cambrian; Jiangshanian and Sunwaptan) Tunnel City Group (Lone Rock Formation and Mazomanie Formation), exposed in Wisconsin and Minnesota, represents a shallow-marine clastic
Flat pebbles and their edge‐wise fabric in relation to 2‐D microbial mat
Flat pebbles and edge‐wise fabric in the Mesoproterozoic Rohtas Limestone Formation (RLF) and the Chikkshelikere Limestone Member (CLM), India, generate a new insight into their formation. Simple

References

SHOWING 1-8 OF 8 REFERENCES
Restriction of a late Neoproterozoic biotope; suspect-microbial structures and trace fossils at the Vendian-Cambrian transition
Wrinkle structures are a class of oddly textured sedimentary structures that are common in Proterozoic-Cambrian marine siliciclastic strata, but uncommon in post-Ordovician subtidal marine facies.
Microbial mats in terminal Proterozoic siliciclastics; Ediacaran death masks
A variety of sedimentary structures and patterns in Proterozoic siliciclastic sedimentary rocks cannot be explained by known inorganic processes. In particular, certain bed-surface textures, and
Wrinkle structures: Microbially mediated sedimentary structures common in subtidal siliciclastic settings at the Proterozoic-Phanerozoic transition
Sedimentary structures produced by microbial activity are well known from ancient carbonate facies, but little is known about equivalent microbial structures in ancient siliciclastic facies. Wrinkle
A review of the origin and setting of tepees and their associated fabrics
Carbonate hardgrounds often occur at the surface of shallow subtidal to supratidal, lacustrine, and subaerial carbonate shelf sediments. These are commonly disrupted and brecciated when the surface
Structure of Microbial Mats and Biofilms
TLDR
This review will highlight some of the insights into the biological structure of biofilms and microbial mats, and how the structure is affected by the physical and chemical environment, species composition, and species interactions.
Geomorphology, Mineralogy and Groundwater Geochemistry as Factors of the Hydrodynamic System of the Gavish Sabkha
The purpose of this study is to contribute to the understanding of hydrodynamic and diagenetic processes in sabkhas by close observations of variations in mineralogy and brine geochemistry in the
Proterozoic metazoan body fossils. In: The Proterozoic Biosphere, A Multidisciplinary Study (Eds
  • J. Schopf and C. Klein),
  • 1992
Proterozoic metazoan body fossils
  • The Proterozoic Biosphere , A Multidisciplinary Study
  • 1992