Storm Events in
Geological Record - a Lecture from 92 MYA
Nebrigic, Dragana
D.1, Boyan K. Vakarelov1 (1) The
The ongoing debate on greenhouse effect
and modern global warming strengthen interest for abrupt warming events in the
geological past. Cenomanian-Turonian greenhouse
interval is related to a broad- scale global warming which peaked in the basal Turonian and led to major changes in oceanic environments.
Siliciclastic-carbonate-bentonitic unit, deposited during Cenomanian-Turonian transgression, the Eagle Ford Formation
of Texas, has been a focus of study over several decades, due at least in part
to the hydrocarbon resources generated from it. However, its upper lower Turonian Kamp Ranch unit
(“member”) (Collignoceras woolgariZone)
has never been adequately described probably due to the insignificant thickness
of the unit, laterally discontinues, and poorly exposed. It represents a
locally prominent sequence of alternating dark gray to grayish black, noncalcareous , laminated shales
and silty shales interbedded with a distinctive, ledge-forming well-indurated light brown to grayish orange coquinoid,
shell hash limestone, calcarenite, which makes
prominent marker beds within the outcrops and occur approximately 30 m below
the Eagle Ford-Austin Chalk contact. Average thickness of the entire unit
varies from 0.03-1.5 m. A recent investigation of four Kamp
Ranch exposures in
AAPG Search and Discover Article #90063©2007 AAPG Annual Convention, Long Beach, California