North-Central Section - 38th Annual Meeting (April 1–2, 2004)
Paper No. 12-2
Presentation Time: 8:20 AM-8:40 AM

RESPONSES OF DEEP-SEA BENTHIC FORAMINIFERA TO SEASONAL FLUCTUATIONS IN PRODUCTIVITY OF THE SOUTHERN CALIFORNIA MARGIN

BAHLS, Amanda S.1, RATHBURN, Anthony E.2, and PÉREZ, M. Elena2, (1) Geography, Geology, and Anthropology, Indiana State University, Science Building 159, Terre Haute, IN 47809, amandabahls@yahoo.com, (2) Geography, Geology, and Anthropology, Indiana State Univ, Science Building 159, Terre Haute, IN 47809

Analyses of living (Rose Bengal stained) deep-sea benthic foraminifera collected on the Southern California margin reveal temporal and spatial changes in foraminiferal assemblages that are related to changes in sea-surface productivity. Samples were collected from two sites (water depths of 990 and 1330 m) during the months of August and October 1996. Results show that benthic foraminiferal abundances in the >63 micron fraction and increases in the densities of the 63-150 micron fraction seem to be positively related to surface productivity in this region. However, >150 micron fraction assemblage abundances of this high productivity region are not correlated with surface productivity. Opportunistic taxa, such as Nonionella fragilis, respond quickly to sea-surface productivity blooms. Based on these results, total abundances in the >63 micron fraction, comparisons between the >150 micron and >63 micron fractions, and known opportunistic species should be used in assessing paleoproductivity along productive continental margins.

North-Central Section - 38th Annual Meeting (April 1–2, 2004)
Session No. 12--Booth# 0
Paleoceanography and Paleoclimatology
Millennium Hotel St. Louis: Laclede Room
8:00 AM-12:00 PM, Friday, 2 April 2004

Geological Society of America Abstracts with Programs, Vol. 36, No. 3, p. 37

© Copyright 2004 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.