T190 Cushman Foundation Symposium: Latest Advances on Foraminiferal Research: From Paleo-Sea-Level Reconstructions and Paleoecological Interpretations to Applications to Environmental Science. A Tribute to the Extraordinary Lives of John Haynes, John Murray, and David Scott
Tuesday, 11 October 2022
1:30 PM - 5:30 PM
406
HEAVY METAL FORAMS: TEST ANALYSIS REDUX
Paper number: T190-13
Program: Technical Sessions
Time: 4:35 PM – 4:50 PM
Authors
-
Pamela Stephens Presenting AuthorDept. of Geological Sciences and Museum of Natural History, University of Colorado, Boulder, CO
-
Thomas M. MarchittoUniv of Colorado, Boulder, CO
-
Martin A. BuzasSmithsonian Institution, Washington, DC
Abstract
To better understand the role of heavy metal contamination on foraminifera, major and minor elements (including Mn, Fe, Zn, Cd, Ba, Pb, Ni, and Cu) in living Ammonia parkinsoniana shells from Copano, Mesquite, Mission, and Nueces Bays were first analyzed with ICP-MS in 2018. The preliminary results showed that A. parkinsoniana is incorporating these elements into its tests approximately proportionally to the amounts found in sediment. However, small sample sizes may have rendered some data unreliable, and specimens from Mesquite Bay, the least impacted site, disintegrated during cleaning, making re-analysis desirable.
For the current research, a larger number of “living” (stained with rose Bengal at the time of collection) A. parkinsoniana tests from the same bays were again run with ICP-MS. Both Pb and Ba compare well with the first run, and along with Zn and Cu are elevated orders of magnitude higher than in predicted pristine shell values. It is likely that the presence of excess metals contributes to the dissolution and pyritization observed in most bays. Many studies have dealt with the effects of heavy metal pollution on foraminiferal abundance and shell deformation, but this is one of the few that focuses on test analysis.
Geological Society of America Abstracts with Programs. Vol. 54, No. 6
doi: 10.1130/abs/2022AM-382007
© Copyright 2022 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.