Research Article| September 01, 1997 Biological mediation of stochastic peritidal carbonate accumulation Bruce H. Wilkinson; Bruce H. Wilkinson 1Department of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109-1063 Search for other works by this author on: GSW Google Scholar Carl N. Drummond; Carl N. Drummond 2Department of Geosciences, Indiana-Purdue University Fort Wayne, Fort Wayne, Indiana 46805-1499 Search for other works by this author on: GSW Google Scholar Nathaniel W. Diedrich; Nathaniel W. Diedrich 1Department of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109-1063 Search for other works by this author on: GSW Google Scholar Edward D. Rothman Edward D. Rothman 3Department of Statistics, University of Michigan, Ann Arbor, Michigan 48109-1027 Search for other works by this author on: GSW Google Scholar Author and Article Information Bruce H. Wilkinson 1Department of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109-1063 Carl N. Drummond 2Department of Geosciences, Indiana-Purdue University Fort Wayne, Fort Wayne, Indiana 46805-1499 Nathaniel W. Diedrich 1Department of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109-1063 Edward D. Rothman 3Department of Statistics, University of Michigan, Ann Arbor, Michigan 48109-1027 Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1997) 25 (9): 847–850. https://doi.org/10.1130/0091-7613(1997)025<0847:BMOSPC>2.3.CO;2 Article history First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Bruce H. Wilkinson, Carl N. Drummond, Nathaniel W. Diedrich, Edward D. Rothman; Biological mediation of stochastic peritidal carbonate accumulation. Geology 1997;; 25 (9): 847–850. doi: https://doi.org/10.1130/0091-7613(1997)025<0847:BMOSPC>2.3.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Exponential thickness frequencies of peritidal carbonate units in the Lower Ordovician Kindblade and West Spring Creek Formations at Ardmore, Oklahoma, are readily interpreted in a context of probabilities of upsection transition from one lithology to another. These largely reflect Poisson (random) processes of deposition from suspended load, traction load, and microbialitic accumulation. Although grainy to muddy particulate and cyanobacterial elements exhibit nearly equal ranges of unit thickness, carbonate generation and/or entrapment via algally mediated processes was less likely to lapse and therefore led to lower probability of transition to some other sediment type. The mean thickness of microbially bound units is roughly double those from the physical transport and deposition of particulate material. Greater persistence of algal accumulation probably related to intrinsically higher biologically induced rates of carbonate precipitation and/or binding by cyanobacteria. Stratigraphic intervals between successive occurrences of suspended load, traction load, and microbial units are also closely approximated by exponential frequency distributions for which regression slopes define probabilities of upsection recurrence of a particular sediment type. Values for grainy and algal carbonates are similar and are nearly twice that of muddy suspended-load units. Although biological processes resulted in significantly lower transition probabilities for thrombolitic bioherms and cryptalgal laminites, spatial dominance of carbonate mud across the region led to higher rates of stratigraphic recurrence and a volumetric dominance of muddy lithologies in the Ardmore sequence. Poissonian distributions of unit stratigraphic duration and recurrence suggest a significant component of haphazard variation in the type and amount of accumulated carbonate sediment. If deposition was influenced by extrabasinal forcing, such control must have been nearly random in both secular and spatial dimensions of water depth change. Stratigraphic durations and recurrences in this sequence more closely reflect the inherently stochastic nature of carbonate accumulation in epicratonic platformal settings than any influence of rhythmic eustatic forcing. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.