Paper No. 24
Presentation Time: 9:00 AM-6:30 PM

LIVING (STAINED) BENTHIC FORAMINIFERAL ASSEMBLAGES ALONG A DEPTH TRANSECT OFF THE COAST OF SOUTHERN CALIFORNIA


PADDACK, Brendan D., Earth and Environmental Science, Indiana State University, Terre Haute, IN 47809, RATHBURN, Anthony, Earth and Environmental Systems, Indiana State University, Terre Haute, IN 47809, ZIEBIS, Wiebke, Biological Sciences Department, Univ of Southern California, Los Angeles, CA 90089, BURKETT, Ashley, Earth and Environmental Science, Indiana State University, Science Bldg 159, Terre Haute, IN 47809, PEREZ, Elena M., Natural History Museum, Cromwell Road, London, England, WILLINGHAM, Jake T., Earth and Environmental Sciences, Indiana State University, Science Building room 159, Terre Haute, IN 47809 and BEDRAVA, Steven, Earth and Environmental Systems, Indiana State University, 600 Chestnut St, Terre Haute, IN 47809, bpaddack1@gmail.com

Living (Rose Bengal stained) foraminifera (greater than 150 microns) of multicorer surface sediments (0-1 cm) collected off the coast of southern California along a depth transect (360-3000 meters) revealed differences in assemblages between sites. In order to examine foraminifera from habitats not typically sampled on productive margins, sites with coarser-grain sediments were targeted in the oxygen minimum zone. Bottom water oxygen values at these sites ranged from 0.63 ml/L at 360 meters to values of 0.47 and 0.81 ml/L at 1000 meters to 1.5 ml/L at 1500 meters. Uvigerina spp. were the most common and most abundant calcareous taxa occurring at all but one of the sites, and Bolivina spp. were found at a majority of the sites. The epifaunal species, Planulina wuellerstorfi, typically associated with higher bottom water O2 values, was one of the dominant taxa at 1000 meters. Hoeglundina elegans was also found at most of the sites. Other common species included Cassidulina spp., Pyrgo sp., and Rutherfordoides rotundata. These results indicate that, along a depth transect across what is typically considered an oxygen minimum zone, habitat heterogeneity may influence foraminiferal assemblages.