Sample 158156 - Upper N20r - Locality 7: Early/Lower Pliocene - Late/Upper Pliocene, East Timor

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Globorotaliidae
Neogloboquadrina pseudopima
Neogloboquadrina dutertrei (d'Orbigny 1839)
Neogloboquadrina humerosa (Takayanagi and Saito 1962)
Neogloboquadrina acostaensis (Blow 1959)
Globorotalia tumida (Brady 1877)
Hirsutella scitula (Brady 1882)
Hirsutella margaritae (Bolli and Bermudez 1965)
Menardella menardii (Parker et al. 1865)
Menardella limbata (Fornasini 1902)
Globorotalia plesiotumida (Blow and Banner 1965)
subspecies "G. tumida flexuosa" subspecies "G. tumida tumida"
Menardella sp. Bandy 1972
Menardella multicamerata
Pulleniatina obliquiloculata (Parker and Jones 1865)
Pulleniatina primalis Banner and Blow 1967
Pulleniatina praecursor Banner and Blow 1967
Globigerinidae
Globoquadrina venezuelana (Hedberg 1937)
recombined as Dentoglobigerina venezuelana
Sphaeroidinella dehiscens (Parker and Jones 1865)
subspecies "S. dehiscens immaturus"
Globigerinoides immaturus
Globigerinoides quadrilobatus
Globigerinoides sp. Cushman 1927
Globigerinoides triloba
Globigerinoides ruber (d'Orbigny 1839)
Globigerinoides obliquus Bolli 1957
Globigerinoides extremus (Bolli and Bermudez 1965)
original and current combination Globigerinoides obliquus extremus
Sphaeroidinellopsis paenedehiscens Blow 1969
Sphaeroidinellopsis seminulina (Schwager 1866)
Sphaeroidinellopsis kochi (Caudri 1934)
Orbulina bilobata
Orbulina universa d'Orbigny 1839
Globigerinoides sacculifer (Brady 1877)
recombined as Trilobatus sacculifer
see common names

Geography
Country:East Timor
Coordinates: 8.9° South, 126.4° East (view map)
Paleocoordinates:8.1° South, 128.8° East
Time
Period:Neogene Epoch:Pliocene
10 m.y. bin:Cenozoic 6
Key time interval:Early/Lower Pliocene - Late/Upper Pliocene Foram zone: Upper N20r
Age range of interval:5.33300 - 2.58000 m.y. ago
Stratigraphy
Lithology and environment
Primary lithology: chalk
Lithology description: Throughout the island, chalk and marl, in places containing tuffaceous material, form the basal part of the post-5.7 Ma succession (“Batu Putih” unit of van Bemmelen, 1949, Table 59; Carter et al.,1976, Fig. 5; but not of Charlton and Suharsono, 1990, p. 52) and are overlain by marl and mudstone with very slow sedimentation rates (Keep and Haig, 2010, Fig. 7). Foraminifera form almost all the sand fraction of the chalk and provide keys to interpreting the palaeobathymetry as well as the age. interbedded turbiditic sands and conglomerates (Viqueque Series of Grunau, 1956). The basal chalk represents pelagic carbonate ooze that accumulated at
Environment:marine indet.
Taphonomy
Modes of preservation:body
Size of fossils:microfossils
Collection methods and comments
Reason for describing collection:biostratigraphic analysis
Metadata
Database number:143244
Authorizer:M. Uhen Enterer:R. McClees-Funinan
Created:2013-04-21 15:06:51 Last modified:2013-04-21 00:06:51
Access level:the public Released:2013-04-21 15:06:51
Creative Commons license:CC BY
Reference information

Primary reference:

46117. D. Haig. 2012. Palaeobathymetric gradients across Timor during 5.7–3.3 Ma and implications for collision uplift. Palaeogeography, Palaeoclimatology, Palaeoecology (331-332)50-59 [M. Uhen/R. McClees-Funinan]