Paper No. 14
Presentation Time: 9:00 AM-6:30 PM
PRELIMINARY FORAM BIOSTRATIGRAPHY AND ORGANIC BIOMARKER PALEOTEMPERATURE RESULTS FROM SITE U1396, IODP EXP. 340
FRAASS, Andrew, Department of Geoscience, University of Massachusetts - Amherst, Amherst, MA 01375, CASTAÑEDA, Isla, Department of Geosciences, University of Massachusetts, 611 N. Pleasant St, Morrill Science Building, Amherst, MA 01003, PHU, Victoria, Department of Geosciences, University of Massachusetts - Amherst, 611 North Pleasant Street, Amherst, MA 01003, LECKIE, R. Mark, Department of Geosciences, Univ of Massachusetts, 611 North Pleasant Street, Amherst, MA 01003 and EXP, 340 Science Party, Integrated Ocean Drilling Program, USIO Science Services, TAMU, 1000 Discovery Drive, College Station, TX 77845, afraass@geo.umass.edu
During the Pliocene major changes in global climate and oceanography occurred due to closure of the Central American Seaway (CAS) and the intensification of Northern Hemisphere glaciations. Currently, many outstanding questions remain regarding the re-organization of oceanic circulation during this time. Here, we apply a multiproxy approach to examine sediments from Site U1396 from IODP Expedition 340 (Lesser Antilles Volcanism and Landslides), situated in the eastern Caribbean, which presently falls under in the influence of the North Equatorial Current. This site presents an excellent opportunity to test both the new tropical planktic foraminiferal biostratigraphic calibration of Wade
et al., 2011 and to investigate the temperature of the past ~4.52 myr from the Montserrat region. After correlating Holes A and C, planktic results largely corroborate the order of bioevents from Wade
et al., 2011, however secondary marker species
Globorotalia flexuosa, Gr. crassaformis, and
Gr. pertenuis have lowest occurrences that extend below their expected First Appearance datums, while
Globigerinoides extremus and
Pulleniatina primalis were found to have anomalously high ranges reflecting regional influences. Sedimentation rates derived from this revised Hole U1396-A and -C biostratigraphy show the same trend as shipboard work: faster sedimentation in the lower Pliocene, slowing towards the Holocene.
Two organic geochemical paleothermometers, the Uk’37 Index and TEXH86, were utilized to examine Plio-Pleistocene SST variability. While the Uk’37 Index is at unity in many samples and is thus somewhat insensitive to temperature change at this tropical site, the TEXH86 record displays more variability. A significant cooling is noted in TEXH86 SST at ~4.1 Ma based on the preliminary age model, coinciding with significant changes in foraminiferal abundance, which may be related to changes in ocean circulation associated with an important transition in the closure of the central American Seaway (e.g., Steph et al., 2010). Overall, application of organic geochemical paleothermometers appears to be a promising technique for examining the Pliocene SST evolution of the Caribbean, particularly since these proxies are not influenced by salinity to the extent observed in d18O or Mg/Ca ratios of foraminifera.
