Sample 158103 - N18 - Locality 1: Late/Upper Miocene, East Timor

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Globorotaliidae
Menardella sp. Bandy 1972
Menardella multicamerata
Globorotalia tumida (Brady 1877)
Hirsutella scitula (Brady 1882)
Hirsutella margaritae (Bolli and Bermudez 1965)
Menardella limbata (Fornasini 1902)
Menardella menardii (Parker et al. 1865)
Globorotalia plesiotumida (Blow and Banner 1965)
Pulleniatina obliquiloculata (Parker and Jones 1865)
Pulleniatina praecursor Banner and Blow 1967
Pulleniatina primalis Banner and Blow 1967
Neogloboquadrina pseudopima
Neogloboquadrina dutertrei (d'Orbigny 1839)
Neogloboquadrina acostaensis (Blow 1959)
Neogloboquadrina humerosa (Takayanagi and Saito 1962)
Globigerinidae
Globigerinoides sacculifer (Brady 1877)
recombined as Trilobatus sacculifer
Globigerina bulloides d'Orbigny 1826
Globigerina apertura Cushman 1918
recombined as Globoturborotalita apertura
Dentoglobigerina altispira (Cushman and Jarvis 1936)
Globoquadrina venezuelana (Hedberg 1937)
recombined as Dentoglobigerina venezuelana
Globigerinoides immaturus
Globigerinoides sp. Cushman 1927
Globigerinoides triloba
Globigerinoides extremus (Bolli and Bermudez 1965)
original and current combination Globigerinoides obliquus extremus
Globigerinoides elongatus (d'Orbigny 1826)
Globigerinoides conglobatus (Brady 1879)
Orbulina bilobata
Orbulina universa d'Orbigny 1839
Sphaeroidinellopsis paenedehiscens Blow 1969
Sphaeroidinellopsis kochi (Caudri 1934)
Sphaeroidinellopsis seminulina (Schwager 1866)
Globigerinella obesa (Bolli 1957)
Globigerinella aequilateralis (Brady 1879)
Sphaeroidinella dehiscens (Parker and Jones 1865)
Candeinidae
Candeina nitida d'Orbigny 1839
see common names

Geography
Country:East Timor
Coordinates: 8.4° South, 126.9° East (view map)
Paleocoordinates:6.5° South, 131.7° East
Time
Period:Neogene Epoch:Miocene
10 m.y. bin:Cenozoic 6
Key time interval:Late/Upper Miocene Foram zone: N18
Age range of interval:11.63000 - 5.33300 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:142383
Authorizer:M. Uhen Enterer:R. McClees-Funinan
Created:2013-04-10 12:20:23 Last modified:2013-04-09 21:20:23
Access level:the public Released:2013-04-10 12:20:23
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]