Technical Program

Tuesday, August 16th, 2022

Time	Talk Title	Speaker
	BREAKFAST
8:00-8:30	Conference Welcome + Introduction
8:30-8:35	*Session: Non-Marine and Microbial Carbonates*
8:35-9:00	Keratolite-stromatolite, the earliest known invertebrate-microbial reef community	Jeong-Hyun Lee Chungnam National University
9:00-9:25	Non-Marine and Microbial Carbonates	Maija J. Raudsepp University of Alberta
9:25-9:50	Microbial Carbonates of Shaybarah Island, Central Red Sea, Saudi Arabia – A unique assemblage of Stromatolites, Polygonal Tepees and Beach Rocks	Volker Vahrenkamp King Abdullah University of Science and Technology
9:50-10:20	BREAK
10:20-10:45	Indigenous microbial communities as catalysts for early marine cements: an in vitro study	Gregor Eberli University of Miami
10:45-11:10	Microfacies and Statistical Analysis of Lower Triassic (Smithian) Microbial-Dominated Teepees and Associated Deposits in the Timpoweap Limestone, basal Moenkopi Formation, in Southwestern Utah	Sarah Naone Brigham Young University
11:10-11:35	Internal wave OMZ nutrient model for cyclical facies shoaling from cross bedded glauconitic sand to thrombolytic bank, Cambrian Trempealeau Formation, Huron County, Ohio	David L. Jeffery Marietta College
	*Session: Diagenesis*
11:40-12:05	Strain-localization during fault-controlled dolomitization; insights from integrated petrographical, geochemical, and geomechanical analyses	Cole McCormick University of Manchester
12:05-1:05	LUNCH
1:05-1:30	Decompressing the Devonian: Aquifer Characterization and Management at the Kearl Oilsands Mine	Lauren Eggie
1:30-1:55	Reassessing Dolomitization Models for the Smackover Formation, Southeastern Gulf Coast, U.S.A.	Bradford E. Prather University of Kansas
1:55-2:20	The origin and architecture of late Jurassic Arab-D dolomites: Clues from petrographic, geochemical and drone-based analysis of a well-exposed outcrop reservoir analogue, Central Saudi Arabia	Gaurav Siddharth Gairola King Abdullah University of Science and Technology
2:20-2:45	Understanding processes governing solution-collapse and subsequent diagenetic features	Eivind Block Vagle University of Manchester
2:45-3:20	BREAK
3:20-3:45	Dolomitization by Tidal-pressure-driven Chemical Cycling in Organic-Rich Carbonate Sediments	Paul A. Washington Salona Exploration LLC
3:45-4:10	Stylolites in limestones: Conduits to fluid flow?	Sreetama Aich IIT Bombay
4:10-4:35	Paleofluid flow and hydrothermal dolomitization: petrographic and geochemical evidence from foreland vs. intracratonic sedimentary basins	Ihsan Al-Aasm University of Windsor
4:35-5:00	The Role of Carbonate Sedimentology and Diagenesis in Constraining Ancient Carbonate Stratigraphic Frameworks and Pleistocene-Holocene Climate Change Records	Charlie Kerans University of Texas at Austin

Thursday, August 18th, 2022

Time	Talk Title	Speaker
	BREAKFAST
8:00-8:05	*Session: Big Data and Digital Techniques*
8:05-8:30	The Visual Display of Quantitative Geologic Data	John B. Dunham Retired
8:30-8:55	Using Decision Tree-Based Machine Learning to Predict Core-Calibrated, Shale Facies from Wireline Logs in the Duvernay Formation	Elisabeth G. Rau Baylor University
8:55-9:20	Multi-scale Satellite Observations on Whitings from Little and Great Bahama Bank, 2000-2022	R. Jude Wilber CORSAGE Research Group
9:20-9:45	The importance of borehole image logs in evaluating carbonates in the subsurface: insights from the Brazil Pre-Salt	Andrea Nolting ExxonMobil
9:45-10:20	BREAK
	*Session: Carbonate Deposition*
10:20-10:45	A Tale of Storm Deposition – Formation of South Joulter Cay, Great Bahama Bank	Juan Carlos Laya Texas A&M University
10:45-11:10	Carbonate factories and reefs response to deltas and/or global controls: Jurassic-Cretaceous giga-platform offshore Nova Scotia Canada and Baltimore Canyon Trough USA	Leslie Eliuk GeoTours Consulting
11:10-11:35	Depositional and Stratigraphic Differences in the Permian San Andres and Clearfork Formations that Cause Large Differences in Oil Production, Permian Basin, USA	Art Saller Consultant
11:35-12:00	Influence of seasonal sediment input on patch reefs and marginal fringing reefs in the Kambaniru deltaic embayment, Sumba, East Nusa Tenggara, Indonesia	John-Paul Zonnenveld University of Alberta
12:00-1:00	LUNCH
	*Session: Carbonate Deposition*
1:05-1:30	Paleoecological Response and Facies Evolution in Response to Extrinsic Drivers During the Pennsylvanian-Permian Transition, Paradox Basin, SE Utah	Stephanie J. White Baylor University
1:30-1:55	High frequency sequence stratigraphy of Pennsylvanian-Lower Permian carbonate successions of the Robledo Mountains, New Mexico, and the Carnic Alps, Austria: A record of the acme and demise of the late Paleozoic ice age	Daniel Calvo Gonzalez University of Calgary
1:55-2:20	How differential biogenic sediment production impact the stratigraphic architecture of carbonate systems: a stratigraphic forward modelling study of Miocene Llucmajor platform	Timothy O. Tella University of Potsdam
2:20-2:45	The importance of evaluating the overprint of local-scale controls on eustatically-driven sequence stratigraphic frameworks: An example from the Early Cretaceous Pettet Formation, East Texas, USA	Kelly E. Hattori University of Texas at Austin
2:45-3:20	BREAK
	*Session: Deepwater Carbonates*
3:20-3:45	Not in the shadow of the Escarpment—Reconsideration of the escarpment model for deposition of the middle Cambrian Burgess Shale and associated units adjacent to the Cathedral carbonate platform	Paul Johnston
3:45-4:10	Reinterpretations of re-sedimented deepwater carbonates: Examples from the Permian Basin, southeast New Mexico and west Texas, U.S.A.	Buddy Price University of Texas at Austin
4:10-4:35	Large-Scale Suspension, Shedding and Settling of Shallow Water Carbonate Sediment to Deep Water Settings: Findings from the Carbonate Factories of the Tropical Atlantic, Pacific and Indian Oceans	R. Jude Wilber CORSAGE Research Group
4:35-5:00	Identification of a thermal maturation high and revised maturity map of the Duvernay Formation	David “Bart” Yeates Baylor University

*Schedule is subject to change.
*Some session presenters are to be confirmed and may be subject to change.