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Title: Comparative planktonic foraminiferal aminostratigraphy of the Colombia basin and the northeast Gulf of Mexico

Conference · · AAPG Bulletin (American Association of Petroleum Geologists); (United States)
OSTI ID:5529476

The increase in the proportion of D-amino acids in fossil shells with increasing age can be used as a relative dating method as far back as the mid-Miocene. Planktonic foraminiferal biostratigraphy and mixed foraminiferal aminostratigraphy were determined for DSDP Site 502B (late Pliocene-Pleistocene) and 502A (late Miocene-Pliocene) in the Colombia basin. The aminostratigraphic analysis was conducted every 2.5-5.0 m in the Pleistocene and every 5-10 m in the Pliocene. Previously established planktonic foraminiferal datums and subzonal boundaries were used to establish the geochronology of DSDP Site 502B-502A. Sediment accumulation rates were then calculated and used to estimate the absolute age at a particular depth in each core. Aminostratigraphic analysis indicates a logarithmic increase in D-alloisoleucine/L-isoleucine (A/I) ratios with increasing age, where equilibrium is not reached until ca. 5 Ma. Using the logarithmic curve that best fits the A/I data, one can estimate the numerical age of a bulk sample given the A/I ratio. The mixed species assemblage A/I ratios from ODP Site 625B (Gulf of Mexico) and 502B are comparable from the late Pliocene-Pleistocene, which suggests that aminostratigraphic analysis of a mixed foraminiferal assemblage offers a very useful and unique opportunity to estimate ages in other Pliocene-Pleistocene sections in regions where independent geochronologic control may be lacking.

OSTI ID:
5529476
Report Number(s):
CONF-910403-; CODEN: AABUD
Journal Information:
AAPG Bulletin (American Association of Petroleum Geologists); (United States), Vol. 75:3; Conference: Annual meeting of the American Association of Petroleum Geologists (AAPG), Dallas, TX (United States), 7-10 Apr 1991; ISSN 0149-1423
Country of Publication:
United States
Language:
English