GSA Annual Meeting in Indianapolis, Indiana, USA - 2018

Paper No. 256-28
Presentation Time: 9:00 AM-6:30 PM

ABUNDANT COLONIZATION OF CALCAREOUS FORAMINIFERA, CIBICIDOIDES WUELLERSTORFI AND PYRGO, AT 4000 M (STATION M) IN THE PACIFIC OCEAN


BURKETT, Ashley M.1, RATHBURN, Anthony2, HOLZMANN, Maria3, PAWLOWSKI, Jan3 and SMITH Jr., K.L.4, (1)Boone Pickens School of Geology, Oklahoma State University, 105 Nobel Research Center, Stillwater, OK 74078-3031, (2)Department of Geological Sciences, California State University Bakersfield, 9001 Stockdale Highway, Bakersfield, CA 93311, (3)Department of Genetics and Evolution, University of Geneva, 4, Boulevard d'Yvoy, Geneva, 1205, Switzerland, (4)Monterey Bay Aquarium Research Institute, 7700 Sandholdt Road, Moss Landing, 95039

After one year on the seafloor at 4000 m water depth, five SEA3s (Seafloor Epibenthic Attachment Cubes) were colonized by ~500 foraminifera, ~80% of which were calcareous species. Although calcareous specimens are not typically abundant in sediments from this water depth in the Pacific, living calcareous epibenthic foraminifera may be more abundant near the CCD than previously thought. At such depths, the physiological requirements of building and maintaining a calcareous skeletal structure may severely impact the ability of foraminifera to be competitive. It is therefore surprising that calcareous foraminifera dominated multiple substrate experiments at Station M in the Pacific. Genetic analyses of the dominant, calcareous trochospiral epibenthic foraminiferal species, show that they cluster with Cibicidoides wuellerstorfi. Pyrgo sp., another calcareous foraminiferal species, was also abundant on the plastic mesh of the SEA3s. These results indicate that some deep-sea calcareous taxa are able to thrive under low pH conditions in modern oceans and may have implications for reconstructions of the past and future projections.