Cretaceous/Tertiary boundary event, El Kef Tunesia: a foraminiferal response
Conference
·
· Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6613894
The Cretaceous/Tertiary boundary extinction event affected benthic communities less than planktonic faunas. Only 9% of benthic species comprising 20% in relative abundance of the total population became extinct, but most species declined in abundance. Only one species, Gavelinella eriksdalensis rapidly increased in abundance through the Danian and Loxostomum and Alabamian dorsoplanata are common in the boundary clay. Two further extinction events of lesser magnitude are observed in the upper A. mayaroensis Zone where 2% of the species go extinct, or 9% of the population, and in the Globigerina engubina Zone where also 2% of the species go extinct or 4% of the population. Significant species abundance changes also accompany these extinction events. Similar stepwise extinction events are also observed in the planktonic foraminifers. Benthic foraminifers indicate that the C/T boundary event was accompanied by a shallowing environment from middle slope to outer shelf. Reducing conditions prevailed during deposition of the boundary clay as suggested by the abundance of pyrite. The authors study of the El Kef section suggests that the observed population turnovers in benthic and planktonic communities could be explained by a sea level fall and/or geotectonically induced changes in oceanic circulation accompanied by temperature and salinity fluctuations. Although they cannot rule out the possibility of impact induced extinction events, have found no evidence of microtektite-like spherules in the boundary clay.
- Research Organization:
- Princeton Univ., NJ (USA)
- OSTI ID:
- 6613894
- Report Number(s):
- CONF-8510489-
- Conference Information:
- Journal Name: Geol. Soc. Am., Abstr. Programs; (United States) Journal Volume: 17
- Country of Publication:
- United States
- Language:
- English
Similar Records
Cretaceous/Tertiary boundary in the North Pacific: planktonic foraminiferal results from deep sea drilling site 577, Shatsky Rise
Late Cretaceous stepwise mass extinction of planktonic foraminifera
Selective extinction and survival across the Cretaceous/Tertiary boundary in the northern Atlantic Coastal Plain
Conference
·
Mon Dec 31 23:00:00 EST 1984
· Geol. Soc. Am., Abstr. Programs; (United States)
·
OSTI ID:6595378
Late Cretaceous stepwise mass extinction of planktonic foraminifera
Conference
·
Mon Dec 31 23:00:00 EST 1984
· Geol. Soc. Am., Abstr. Programs; (United States)
·
OSTI ID:6646197
Selective extinction and survival across the Cretaceous/Tertiary boundary in the northern Atlantic Coastal Plain
Journal Article
·
Tue Oct 01 00:00:00 EDT 1991
· Geology; (United States)
·
OSTI ID:5996741
Related Subjects
58 GEOSCIENCES
580100* -- Geology & Hydrology-- (-1989)
ANIMALS
AQUATIC ORGANISMS
ASIA
BENTHOS
BIOLOGICAL EXTINCTION
CENOZOIC ERA
CHALCOGENIDES
CLAYS
CRETACEOUS PERIOD
DEVELOPING COUNTRIES
FORAMINIFERA
FOSSILS
GEOLOGIC AGES
GEOLOGIC HISTORY
INDONESIA
INVERTEBRATES
IRON COMPOUNDS
IRON SULFIDES
ISLANDS
LEVELS
MESOZOIC ERA
MICROORGANISMS
MINERALS
PALEONTOLOGY
PLANKTON
POPULATION DYNAMICS
PROTOZOA
PYRITE
ROCKS
SARCODINA
SEA LEVEL
SEDIMENTARY ROCKS
SULFIDE MINERALS
SULFIDES
SULFUR COMPOUNDS
TERTIARY PERIOD
TRANSITION ELEMENT COMPOUNDS
580100* -- Geology & Hydrology-- (-1989)
ANIMALS
AQUATIC ORGANISMS
ASIA
BENTHOS
BIOLOGICAL EXTINCTION
CENOZOIC ERA
CHALCOGENIDES
CLAYS
CRETACEOUS PERIOD
DEVELOPING COUNTRIES
FORAMINIFERA
FOSSILS
GEOLOGIC AGES
GEOLOGIC HISTORY
INDONESIA
INVERTEBRATES
IRON COMPOUNDS
IRON SULFIDES
ISLANDS
LEVELS
MESOZOIC ERA
MICROORGANISMS
MINERALS
PALEONTOLOGY
PLANKTON
POPULATION DYNAMICS
PROTOZOA
PYRITE
ROCKS
SARCODINA
SEA LEVEL
SEDIMENTARY ROCKS
SULFIDE MINERALS
SULFIDES
SULFUR COMPOUNDS
TERTIARY PERIOD
TRANSITION ELEMENT COMPOUNDS