| 2003 Seattle Annual Meeting (November 2–5, 2003) | |
| Paper No. 121-9 | |
| Presentation Time: 1:30 PM-5:30 PM | ||
YPRESIAN/LUTETIAN (Y/L) PALEOENVIRONMENTS IN SE SPAIN: INFERENCES FROM BENTHIC FORAMINIFERA | ||
|
ORTIZ, Silvia1, MOLINA, Eustoquio1, and THOMAS, Ellen2, (1) Area de Paleontología, Departamento de Ciencias de la Tierra, Universidad de Zaragoza, Zaragoza, E-5OOO9, Spain, silortiz@posta.unizar.es, (2) Earth & Environmental Sciences, Wesleyan Univ, 265 Church Street, Middletown, CT 06459-0139 Benthic foraminifera in the Fortuna section (Betic Cordillera, Southern Spain) were used to reconstruct changes in palaeoproductivity and oxygenation as part of a study to define a Global Stratotype Section and Point (GSSP) for the base of the Lutetian Stage (early/middle Eocene, ~ 49 Ma). The most common taxa in the upper-middle bathyal assemblages include Cibicidoides spp., Lenticulina spp., Osangularia spp., Clavulinoides angularis, Gaudryina spp. and Dorothia spp., and include highly fluctuating relative abundances of Globobulimina spp. (up to ~45-65%), which are in recent oceans characteristic of areas of high primary productivity and associated low oxygen conditions in bottom and/or pore waters. The Y/L boundary occurs in one of the intervals with a high relative abundance of Globobulimina spp., which is characterized by low species richness, a negative carbon isotope excursion (~-2‰) and a high relative abundance of Aragonia aragonensis. Other intervals with abundant Globobulimina spp. do not have A. aragonensis. Early Cenozoic climate is characterized by a long-term warming from mid-Paleocene to initial early Eocene, followed by cooling starting in the early middle Eocene. The Paleocene/Eocene Thermal Maximum (PETM) was a superimposed, short-lived hyperthermal event, during which deep-sea temperatures increased by 5 to 6oC, during which there was a ~3‰ negative carbon isotope excursion. Benthic foraminiferal species including A. aragonensis show short-term peaks in relative abundance just after the PETM and in the overall period between ~61.5 and 49 Ma. We suggest that the Y/L A. aragonensis peak accompanied by a negative carbon isotope excursion could be a hyperthermal event of lesser magnitude than the PETM, possibly caused by methane hydrate dissociation. Methane hydrate dissociation could have been caused by sea-level fall, and may have triggered increased activity of chemosynthetic bacteria serving as food supply for such species as A. aragonensis. | ||
|
2003 Seattle Annual Meeting (November 2–5, 2003)
| ||
| Session No. 121--Booth# 118 Paleoclimatology/Paleoceanography (Posters) I Washington State Convention and Trade Center: Hall 4-F 1:30 PM-5:30 PM, Monday, November 3, 2003 Geological Society of America Abstracts with Programs, Vol. 35, No. 6, September 2003, p. 255 | ||
© Copyright 2003 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. | ||