M.J. Kraus
University of Colorado, Boulder, Boulder, CO
Activity
2021
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AN EARLIEST EOCENE CONGLOMERATE IN THE BIGHORN BASIN, WYOMING, AND POSSIBLE RELATIONSHIP TO THE PALEOCENE-EOCENE THERMAL MAXIMUM
130 D13. Recent Advances in Paleoclimatology/PaleoceanographyTuesday, 12 October 20218:00 AM - 12:00 PMD137
2014
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ALLUVIAL RESPONSE TO CLIMATE CHANGE INTERPRETED FROM PALEOSOLS ACROSS THE PALEOCENE-EOCENE THERMAL MAXIMUM, BIGHORN BASIN, WYOMING
T6 Soil Development: Its Role in Geological ProcessesSunday, 19 October 20148:00 AM - 12:00 PM213
2013
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BIOTURBATION IS THE MAJOR PROCESS IN THE EVOLUTION OF SOILS AND LANDSCAPES––EVIDENCE FROM MODERN AND DEEP TIME
272 Special Session: Accomplishments, Challenges, and Frontiers in Soil Geomorphology: In Memory of Donald L. JohnsonTuesday, 29 October 20131:00 PM - 5:00 PMMile High Ballroom 3C
2012
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PALEOHYDROLOGIC RESPONSE TO CONTINENTAL WARMING: PALEOSOLS ACROSS THE PALEOCENE-EOCENE THERMAL MAXIMUM, BIGHORN BASIN, WYOMING
T147 Terrestrial Proxies of Paleoclimate and Paleoenvironment in Deep TimeTuesday, 6 November 20128:00 AM - 12:00 PM202AB
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RESOLVING INCONSISTENCIES AMONG PETM CIES IN THE SE BIGHORN BASIN, WYOMING: AN ALLOCHTHONOUS CARBON HYPOTHESIS
157 Geochemistry (Posters)Tuesday, 6 November 20129:00 AM - 6:00 PMHall B
2011
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NEOGENE DRAINAGE RATES IN THE BIGHORN BASIN FROM JAROSITE 40Ar/39Ar CHRONOMETRY; A HYDROLOGIC ANALOG FOR MERIDIANI PLANUM, MARS
T284 Terrestrial Analogs in Solar System StudiesWednesday, 12 October 20111:30 PM - 5:30 PMRoom L100H-J
2010
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BIOTIC AND SEDIMENTARY CHANGE DURING THE PALEOCENE-EOCENE THERMAL MAXIMUM IN WESTERN NORTH AMERICA
T288 Cenozoic Terrestrial Environmental Change in North America: From Paleosols to PaleobotanyWednesday, 3 November 20101:30 PM - 5:30 PMRoom 607
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SEDIMENTARY RESPONSE TO CLIMATE CHANGE DURING THE PALEOCENE-EOCENE THERMAL MAXIMUM, SOUTHEASTERN BIGHORN BASIN, WY
T190 Cenozoic Terrestrial Environmental Change in North America: From Paleosols to Paleobotany (Posters)Tuesday, 2 November 20108:00 AM - 6:00 PMHall D
2008
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Revised Ichnopedofabric Indices That Semiquantitatively Analyzes the Degree of Pedogenic Modification: Recognizing the Effects of Subaerial Exposure on Continental and Marine Deposits
T210 Leaving Traces—Making Marks II: In Honor of H. Allen CurranMonday, 6 October 20081:30 PM - 5:30 PM
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PALEOPRECIPITATION TRENDS ACROSS THE PALEOCENE-EOCENE THERMAL MAXIMUM OF CABIN FORK, BIGHORN BASIN, WYOMING
5 Paleontology/Sedimentology/Stratigraphy (Posters)Wednesday, 19 March 20088:00 AM - 12:00 PM
2007
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ABRUPT PALEOENVIRONMENTAL CHANGE DURING THE PALEOCENE-EOCENE THERMAL MAXIMUM IN THE BIGHORN BASIN, WYOMING
T70 Evidence for Paleoenvironmental Change during the Paleogene from the Interior Basins of Western North AmericaMonday, 29 October 20078:00 AM - 12:00 PM
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ICHNOFOSSILS OF ANCIENT SOIL BIOTA SHOW CHANGES IN ABUNCANCE, STRATIGRAPHIC DISTRIBUTION, AND SIZE DURING A RAPID GLOBAL-WARMING EVENT: PALEOCENE-EOCENE THERMAL MAXIMUM INTERVAL, PALEOGENE WILLWOOD FORMATION, BIGHORN BASIN, WYOMING
T76 Trace Fossils, Mass Extinctions, and Event Boundaries: Endobenthic and Fossorial Responses to Terrestrial and Extraterrestrial PerturbationsMonday, 29 October 20078:00 AM - 12:00 PM
2006
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MORPHOLOGY AND PALEOENVIRONMENTAL IMPLICATIONS OF ADHESIVE MENISCATE BURROWS (AMB), PALEOGENE WILLWOOD FORMATION AND OTHER CONTINENTAL DEPOSITS
T223 Fossil Behavior II: In Honor of Adolf SeilacherWednesday, 25 October 20061:30 PM - 5:30 PM
2005
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ABSENCE OF PRESERVED MANGANIFEROUS RHIZOLITHS WITHIN THE PETM INTERVAL AND ITS CLIMATIC IMPLICATIONS
T186 Causes and Effects of the Paleocene-Eocene Thermal Maximum and Other Paleogene Hyperthermal Events IITuesday, 18 October 20051:30 PM - 5:30 PM
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TRANSIENT DRYING DURING THE PALEOCENE-EOCENE THERMAL MAXIMUM (PETM): ANALYSIS OF PALEOSOLS IN THE BIGHORN BASIN, WYOMING
T117 Causes and Effects of the Paleocene-Eocene Thermal Maximum and Other Paleogene Hyperthermal Events IMonday, 17 October 20051:30 PM - 5:30 PM
2004
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THE OCCURRENCE AND DIVERSITY OF TRACE FOSSILS IN PALEOSOLS OF THE WILLWOOD FORMATION DURING THE PALEOCENE-EOCENE THERMAL MAXIMUM (PETM), BIGHORN BASIN, WYOMING
22 Paleontology (Posters) I: PaleoecologySunday, 7 November 20048:00 AM - 12:00 PM
Date Unknown
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IMPLICATIONS OF NEW CARBON ISOTOPE STRATIGRAPHY FOR THE PALEOCENE-EOCENE THERMAL MAXIMUM, SAND CREEK DIVIDE, BIGHORN BASIN, WYOMING
54 Stratigraphy (Posters)
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MODE OF ROOT TRACE PRESERVATION AND PALEOSOL HYDROLOGY: EXAMPLES FROM THE BIGHORN BASIN, WYOMING
155 Sediments, Clastic (Posters)
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PALEOSOL FEATURES MEDIATED BY ANCIENT SOIL BIOTA
223 Sediments, Clastic (Posters) II
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CONTROLS ON VERTICAL COLOR CHANGES IN ALLUVIAL PALEOSOLS OF THE MORRISON FORMATION, COYOTE BASIN, WYOMING
155 Sediments, Clastic (Posters)
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SIGNIFICANCE OF DIFFERENT TYPES OF TRACE FOSSILS AND ICHNOCOENOSES TO INTERPRETING PALEOHYDROLOGICAL AND PALEOENVIRONMENTAL SETTINGS OF PALEOSOLS IN THE PALEOGENE WILLWOOD FORMATION, BIGHORN BASIN, WYOMING, U.S.A
T178 Fossil Behavior (Posters): In Honor of Adolf Seilacher
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PRESERVATION OF A VEGETATED LANDSCAPE IN THE EARLIEST EOCENE, POLECAT BENCH, BIGHORN BASIN, WYOMING
53 Sediments, Clastic (Posters)
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PEDOGENIC OVERPRINTING OF CRAYFISH-BURROWED ALLUVIAL DEPOSITS IN THE PALEOGENE WILLWOOD FORMATION, BIGHORN BASIN, WYOMING
T197 Traces of Life: Micro- to Macroscopic Evidence of Past and Present Biogenic Activity and their Implications (Posters)