246 D12. Recent Advances in Diversity, Extinction, and Origination (Posters)
Wednesday, 25 September 2024
8:00 AM - 5:30 PM
Hall D
CHANGES IN THE FUNCTIONAL DIVERSITY OF MESOZOIC MARINE GASTROPODS
Paper number: 246-6
Program: Technical Sessions
Time: 8:00 AM – 5:30 PM
Authors
-
Madeline EssMiami University, Oxford, OH
-
Roxanne M.W. BankerUniversity of Nevada, Las Vegas, NV
-
Roxanne M.W. BankerProvidence College, Providence, RI
-
Ashley DineenThe Natural History Museum, London
-
Peter D. RoopnarineCalifornia Academy of Sciences, San Francisco, CA
-
Carrie TylerUniversity of Nevada Las Vegas, Las Vegas, NV
Abstract
Here we examine functional diversity, the number and types of functions performed by organisms in a community. To assess how gastropod functional diversity may have changed across the MMR in the western Tethys, we examined how species were distributed within functional space for 5 stage time-bins: the Anisian, Carnian, Bathonian, Aptian, and Maastrichtian. Functional diversity was quantitatively assessed using a Functional Entities (FEs) approach. Species with similar traits are thought to perform similar ecosystem functions, thus, for 642 gastropod species feeding habit, motility, and tiering were classified to create unique FEs. Differences in trait composition between stages should correspond to differences in functional composition, that is relating to trophic structure, tiering, and animal-substrate interactions in benthic ecosystems. The number of FEs ranged from 5 to 16, and functional vulnerability (no. species/no. FEs) increased from 22.2 during the Anisian to 35.7 in the Aptian, as functional groups were occupied by fewer species, but declined to 20 in the Maastrichtian. Functional redundancy, the percentage of FEs with only 1 species, corresponded with species richness, a pattern we observe in other paleocommunities, suggesting that species richness may play a large role in buffering ecosystems against the loss of functional diversity. These findings support the hypothesis that metabolic and physiological escalation during the MMR prompted significant ecosystem restructuring and changes in energy transfer pathways.
Geological Society of America Abstracts with Programs. Vol. 56, No. 5
doi: 10.1130/abs/2024AM-405335
© Copyright 2024 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.