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Você está em: Start > Publications > View > The presence of zooclasts and zoomorphs in the carbonate candeeiros formation (Arruda sub-basin, lusitanian basin, portugal): Paleoenvironmental evidence [Presença de zooclastos e zoomorfos na formação de Candeeiros (Sub-bacia de Arruda, Bacia Lusitânica, Portugal): Evidências paleoambientais]
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The presence of zooclasts and zoomorphs in the carbonate candeeiros formation (Arruda sub-basin, lusitanian basin, portugal): Paleoenvironmental evidence [Presença de zooclastos e zoomorfos na formação de Candeeiros (Sub-bacia de Arruda, Bacia Lusitânica, Portugal): Evidências paleoambientais]

Title
The presence of zooclasts and zoomorphs in the carbonate candeeiros formation (Arruda sub-basin, lusitanian basin, portugal): Paleoenvironmental evidence [Presença de zooclastos e zoomorfos na formação de Candeeiros (Sub-bacia de Arruda, Bacia Lusitânica, Portugal): Evidências paleoambientais]
Type
Article in International Scientific Journal
Year
2014
Authors
Goncalves, PA
(Author)
Other
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Mendonca Filho, JG
(Author)
Other
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Mendonca, JO
(Author)
Other
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Flores, D
(Author)
FCUP
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Journal
Vol. 101
Pages: 439-442
ISSN: 0873-948X
Indexing
Publicação em ISI Web of Knowledge ISI Web of Knowledge
Other information
Authenticus ID: P-00G-51W
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
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