Abstract (EN):
Zooclasts correspond to animal-derived organic particles such as crustacean eggs, tintinnids, insect cuticles fragments and other arthropods fragments. Zoomorph subgroup is composed by animal-derived palynomorphs including foraminiferal linings, chitinozoa and scolecodonts. Due to their characteristics, it is very rare to find these organic particles in the kerogen assemblage of ancient marine sediments. The Candeeiros formation (informal unit), corresponds to sediments of the inner part of a carbonate ramp developed in the Middle Jurassic, showed in some layers the presence of degraded remains of particulate organic matter classified as zooclasts and foraminiferal test-linings (zoomorphs). The fact that such amounts of zooclasts and zoomorphs were preserved is indicative of high zooplankton productivity and consequently high primary productivity. To allow the survival of these organisms the water column must be oxygen rich. Despite the high primary productivity, the accumulation and preservation of the organic matter in the sediments was weak as evidenced by the lower total organic carbon content (less than 0.16wt.%). © 2014 LNEG ¿ Laboratório Nacional de Geologia e Energia IP.
Language:
English
Type (Professor's evaluation):
Scientific