T172 Quantitative Paleobiology of Marine Ecosystems
Tuesday, 24 September 2019
8:00 AM - 12:00 PM
Room 227ABC, North Building
LATE TRIASSIC FAUNAL AND PALEOECOLOGICAL SUCCESSION IN NEW ZEALAND AND IMPLICATIONS FOR GLOBAL PREDATOR-PREY DYNAMICS
Paper number: T172-9
Program: Technical Sessions
Time: 10:00 AM – 10:15 AM
Authors
-
Annaka ClementNorth Dakota State University, Fargo, ND
Abstract
Here, we present preliminary results of a shallow marine macrofauna sampling effort from Norian (Oretian-Warepan, Late Triassic) volcaniclastic sedimentary deposits in South Island, New Zealand. Faunal assemblages contained lower diversity relative to lower latitude deposits in Nevada and Italy, and were typically dominated by Halobia and Monotis bivalves that rarely reach high abundances in oxic, shallow environments. Four faunal phases were recognized, as successive intervals of ecological dominance by Halobia, Manticula, various endemic brachiopods, and finally Monotis. The four taxa likely utilized a similar ecological niche (sessile epifauna), although size and generic morphological diversity increased during the stage. Monotis, in particular, underwent a dramatic taxonomic radiation that resulted in morphological characters not seen in coeval Monotis-bearing deposits elsewhere.
Norian benthic fauna from New Zealand differ from lower-latitude assemblages in their lack of mobile or infauna taxa, but similarly exhibit multiple phases of turnover. The extent to which these taxonomic shifts are driven by environmental or biological influences are further discussed.
Geological Society of America Abstracts with Programs. Vol. 51, No. 5
doi: 10.1130/abs/2019AM-340507
© Copyright 2019 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.