Loc. 9-15 [Borbon Fm]: Middle Miocene, Ecuador
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
unclassified
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Phomistochoartus corbula
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Globigerinidae
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Orbulina universa
d'Orbigny 1839
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Globigerina venezuelana
Hedberg 1937
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recombined as Dentoglobigerina venezuelana | |||||||
Nodosariata
- Polymorphinida
- Plectofrondiculariidae
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Plectofrondicularia jarvisi
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Nodosariata
- Nodosariida
- Stilostomellidae
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Stilostomella lepidula
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Buliminidae
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Bulimina mexicana
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Bulimina pagoda
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Cassidulinidae
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Ehrenbergina cf. pacifica
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Cassidulina tricamerata
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Globocassidulina subglobosa
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Rotaliidae
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Rotalia ecuadorana
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Uvigerinidae
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Uvigerina auberiana
d'Orbigny 1839
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Bolivinidae
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Bolivina pisciformis
Calloway and Morrey 1929
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Discorbinellidae
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Laticarinina pauperata
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Chilostomellidae
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Sphaeroidina bulloides
d'Orbigny 1826
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unclassified
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Cibicorbis herricki
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Globothalamea
- Rotaliida
- Discorbidae
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Hanzawaia wuellerstorfi
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Epistominella culter
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Globothalamea
- Rotaliida
- Nonionidae
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Melonis affinis
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Globothalamea
- Rotaliida
- Cibicididae
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Cibicides floridanus
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Cibicidoides haidingeri
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Coccolithophyceae
- Ceratolithaceae
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Angulolithina arca
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Coccolithophyceae
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Discoaster variabilis
Martini and Bramlette 1963
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Discoaster brouweri
Tan Sin Hok 1927
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Discoaster intercalaris
Bukry 1971
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Coccolithus pelagicus
(Wallich 1877)
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Cyclococcolithina leptoporus
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synonym of Coccolithus | |||||||
Cyclococcolithina macintyri
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synonym of Coccolithus | |||||||
Sphenolithus abies
Deflandre 1954
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unclassified
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Reticulofenestra pseudoumbilica
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Protozoa
- Spumellaria
- Sponguridae
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Spongocore puella
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synonym of Spongurus | |||||||
Protozoa
- Nassellaria
- Pterocorythidae
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Theocorythium vetulum
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Protozoa
- Nassellaria
- Eucyrtidiidae
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Stichocorys delmontensis
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see common names |
Geography
Country: | Ecuador |
Coordinates: | 1.0° North, 79.8° West (view map) |
Paleocoordinates: | 0.2° North, 76.9° West |
Basis of coordinate: | based on nearby landmark |
Geographic resolution: | outcrop |
Time
Period: | Neogene | Epoch: | Miocene |
10 m.y. bin: | Cenozoic 5 | ||
Key time interval: | Middle Miocene | ||
Age range of interval: | 15.98000 - 11.63000 m.y. ago |
Stratigraphy
Formation: | Borbon | ||||
Stratigraphic resolution: | bed | ||||
Stratigraphy comments: STRATIGRAPHIC RELATIONS: From the Borbon Fm, which is regionally overlain by the Esmeraldas Fm (Pliocene). AGE: Middle Miocene, on the basis of microfossil biostratigraphy; nannofossil zones N11-13; planktonic zones N13-N14. STRATIGRAPHIC POSITION: From unknown position within formation. |
Lithology and environment
Primary lithology: | tuffaceous unlithified argillaceous mudstone |
Includes fossils? | Y |
Lithology description: SPECIFIC LITHOLOGY: Tuffaceous clays and mudstones. LITHIFICATION: Unlithified, as stated in text. | |
Environment: | deep-water indet. |
Geology comments: ENVIRONMENT: Siliceous organisms (diatoms, radiolar- ians) are well preserved in the Miocene rocks, but the cal- careous fauna has been modified. The nannoflora and the globigerinacean assemblage are impoverished. This may re- flect dissolution of the more delicate forms before burial and suggests that these sediments were deposited at bathyal depths. |
Taphonomy
Modes of preservation: | body |
Size of fossils: | mesofossils,microfossils |
Collection methods and comments
Collection methods: | bulk,chemical,hydrochloric,sieve,field collection |
Reason for describing collection: | biostratigraphic analysis |
Collection method comments: COLLECTOR: Presumably the authors. REPOSITORY: Not stated, but presumably Princeton University, New Jersey. PREPARATION: Eighty-five gram samples were crushed and boiled with Calgon, then washed through 420-,m, 177-Am, 74-,m and 63- ,m screens. A cut of the fines was saved for nannofossils. The two largest fractions and half of the 74-gm fraction were dried, floated on CC14 and picked for foraminifera. The re- maining half of the 74-um fraction and the 63-,um fraction were decalcified with HC1 and washed again, then dried and floated on CClI, before mounting on slides for study of ra- diolarians. The flotation in this case was found to enrich radiolaria by a factor of about 30, and to raise the proportion of unbroken specimens. Nannofossils were concentrated from the fines that passed the 63-um mesh, in two steps: settling for 1.5 minutes in a 1-liter beaker separated a coarser fraction, to be discarded. The poured-off liquid was then settled in a similar beaker for 30 minutes, which settled out such nannofossils as could be handled by optical microscopy, while the ultra-fine ma- terial was discarded. Radiolaria and nannofossils were pre- pared for study as strewn slides mounted in balsam. Nan- nofossils were identified by optical phase contrast and polarized microscopy, at 1200 x. | |
Taxonomic list comments:COVERAGE: Exhaustive for foraminifera, nannofossils, and radiolarians. NOMENCLATURE: Not an authoritative publication, but with modern nomenclature and species-resolution identifications. |
Metadata
Database number: | 90852 | ||
Authorizer: | A. Hendy | Enterer: | A. Hendy |
Modifier: | A. Hendy | Research group: | marine invertebrate,micropaleontology |
Created: | 2009-08-19 13:34:46 | Last modified: | 2013-11-25 13:37:23 |
Access level: | the public | Released: | 2009-08-19 13:34:46 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
30557. | P. F. Hasson and A. G. Fischer. 1986. Observations on the Neogene of Northwestern Ecuador. Micropaleontology 32(1):32-42 [A. Hendy/A. Hendy] |