|Northeastern (46th Annual) and North-Central (45th Annual) Joint Meeting (20–22 March 2011)|
|Paper No. 31-4|
|Presentation Time: 8:45 AM-9:00 AM|
LOWER TO MIDDLE MIOCENE PALYNOLOGY OF THE SHALLOW NEW JERSEY SHELF: EVIDENCE OF ICEHOUSE COOLING
MCCARTHY, Francine M.G., Department of Earth Sciences, Brock University, 500 Glenridge Ave, St Catharines, ON L2S 3A1, Canada, FMcCarthy@brocku.ca, MAHDAVI, Mehrsa, Earth Sciences, Brock University, 500 Glenridge Ave, St. Catharines, ON L2S 3A1, Canada, KOTTHOFF, Ulrich, Department of Geosciences, Hamburg University, Bundesstrasse 55, Hamburg, D-20146, Germany, and HEAD, Martin J., Earth Sciences, Brock University, 500 Glenridge Avenue, St. Catharines, ON L2S 3A1, Canada|
Marine and terrestrial palynomorphs from IODP EXP 313 Sites 27 and 29 on the New Jersey shallow shelf record the establishment of drier continental climates and cooler, more neritic surface waters during the Serravallian. The common presence of gonyaulacoid dinocysts including Apteodinium tectatum, Hystrichokolpoma rigaudiae, Tectatodinium pellitum, Pentadinium laticinctum, Reticulatosphaera actinocoronata, Dapsilidinium pseudocolligerum, Lingulodinium machaerophorum, as well as various Operculodinium, Spiniferites and Impagidinium species in Lower Serravallian and older deposits differs from the pollen-rich Upper Serravallian–Tortonian sediments in which protoperidinioid dinocysts such as Trinovantedinium, Lejeunecysta, Selenopemphix, and Brigantedinium spp. comprise a greater component of the cyst flora. This is consistent with global cooling associated with the growth of ice on Antarctica and the rapid progradation of terrigenous sediments across the New Jersey margin during the early Serravallian.
Northeastern (46th Annual) and North-Central (45th Annual) Joint Meeting (20–22 March 2011)
General Information for this Meeting
|Session No. 31|
Theory and Application in Cenozoic Paleoclimate Studies
Omni William Penn Hotel: Conference B
8:00 AM-12:00 PM, Monday, 21 March 2011
Geological Society of America Abstracts with Programs, Vol. 43, No. 1, p. 99
© Copyright 2011 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.