Laura Speir
University of Missouri, Columbia, MO
Activity
2024
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WHO DISSOLVES, WHO DIES, WHO TELLS YOUR STORY: DISENTANGLING SELECTIVE BIASES IN EXTRACTION METHODS FOR CAMBRIAN SMALL SHELLY FAUNAS
T65 Future Leaders in PaleontologySunday, 22 September 20241:30 PM - 5:30 PM207A
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DISENTANGLING REDOX ENVIRONMENTS AND SMALL SHELLY FAUNAL OCCURRENCES FROM THE NORMALLY FOSSILIFEROUS MERNMERNA FORMATION OF SOUTH AUSTRALIA
26 Emerging Voices in PaleontologyTuesday, 23 April 20248:00 AM - 12:00 PMFiji Ballroom, Oasis CC
2023
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WHERE HAVE ALL THE SMALL SHELLY FAUNAS GONE? A MULTI-PROXY APPROACH TO UNDERSTANDING THE ABSENCE OF FOSSILS FROM THE TYPICALLY FOSSILIFEROUS MERNMERNA FORMATION OF SOUTHERN AUSTRALIA
T81 Laws of the Grave: Advances in Taphonomy across the Paleontologic RecordMonday, 16 October 20238:00 AM - 12:00 PM301 / 302
2022
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UNDERSTANDING LGBTQ+ EXPERIENCES ACROSS THE GEOSCIENCES THROUGH A TARGETED SURVEY: INITIAL FINDINGS AND RESULTS
T206 Institutional and Grassroots Efforts Promoting Diversity, Equity, and Inclusion in the Scientific Workplace (Posters)Tuesday, 11 October 20222:00 PM - 6:00 PMExhibit Hall F
2021
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SMALL SHELLY FAUNAS AND REPEATED PHOSPHATIC HARDGROUNDS FROM THE LOWER CAMBRIAN, WIRRAPOWIE LIMESTONE, IKARA-FLINDERS RANGES, SOUTH AUSTRALIA
T142 Stratigraphy, Stasis, and Shales ITuesday, 12 October 20218:00 AM - 12:00 PME143/E144
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UNDERSTANDING LGBTQ+ EXPERIENCES ACROSS THE GEOSCIENCES THROUGH A TARGETED SURVEY
89 D44. Recent Advances in Geoscience and Public Policy (Posters)Monday, 11 October 20219:00 AM - 1:00 PMExhibit Hall A
2020
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PALEOENVIRONMENTAL AND TAPHONOMIC IMPLICATIONS FOR LOWER CAMBRIAN PHOSPHATIC HARDGROUNDS FROM SOUTH AUSTRALIA
T113 Trends and Patterns in Neoproterozoic–Cambrian Biodiversity and Evolutionary Originations IIWednesday, 28 October 202010:00 AM - 12:00 PMMeeting Rooms
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PROGRESS MADE AND OUTSTANDING ISSUES REGARDING LGBTQ+ DIVERSITY IN THE GEOSCIENCES
T169 Incorporating Identities to Advance Diversity throughout Geoscience Disciplines IIWednesday, 28 October 20205:30 PM - 8:00 PMMeeting Rooms
2019
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AN APATITE FOR ORDOVICIAN TEMPERATURE TRENDS: USING δ18OPHOS DATA DERIVED FROM CONODONTS TO UNDERSTAND ORDOVICIAN CLIMATE AND BIODIVERSIFICATION
T88 Integrated Biostratigraphy and Chemostratigraphy Using Conodonts—North American Pander Society Annual MeetingMonday, 23 September 20198:00 AM - 12:00 PMRoom 227ABC, North Building
2017
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HIGH-RESOLUTION CONODONT BIOSTRATIGRAPHY OF THE EARLY CARBONIFEROUS, TOURNAISIAN STAGE, CHESTNUT RIDGE SECTION IN SOUTHWEST MISSOURI
T52 Undergraduate Research Talks: The Next Step in Student Research ProjectsSunday, 22 October 20171:30 PM - 5:30 PMChelan 5