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Ottakovil Formation
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Ottakovil Fm base reconstruction

Ottakovil Fm


Period: 
Cretaceous

Age Interval: 
Middle Maastrichtian (outcrop at Ariyalur area)


Province: 
E.India Cauvery Basin

Type Locality and Naming

ARIYALUR-TRICHIRAPPALLI OUTCROP: Named after Ottakovil village, Ariyalur district, TamilNadu. Type locality = 7 km North of Ariyalur town. Outskirts of Ottakovil Stream section, Ottakovil village.

[Figure 1: Geologic map of Ariyalur area]


Lithology and Thickness

Sandstone. Grey, dirty yellow to off-white, cross bedded, medium to coarse, micaceous friable sand and well cemented, fine-to medium grained sandstone (Tewari et al., 1996) and thickness is computed to 60 m (Sundaram et al., 2001).

[Figure 1: Field photos of Ottakovil Formation. Outcrop, Rip or long-shore trough, Echinoid fossil (provided by A. Nallapa Reddy and R. Nagendra)]


Lithology Pattern: 
Sandstone


Relationships and Distribution

Lower contact

Conformable onto upper surface of Kallankurichchi Fm

Upper contact

Unconformable with fluvial Kallamedu Fm

Regional extent

Lithological exposures along the stream section from Ottakovil to Anandavadi in an eastern direction


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[79.03,12.05],[79.02,11.09],[79.35,11.03],[79.83,12.06],[79.19,12.07],[79.03,12.05]]]]}}

Fossils

In the upstream section, the sandstones are associated with echinoids, Trace fossils-Thalassinoides, Ophiomorpha. In the downstream section are echinoids, nautilus, ammonite, Alectronia/Lopha (Tewari et al, 1996) and calcareous nannoplankton (Jyotsana Rai and Ramkumar, 2007) .

Nannoplankton zone equivalent to Gansserina gansseri planktonic foraminifer zone is recorded from Ottakovil top.


Age 

Middle Maastrichtian

Age Span: 

    Beginning stage: 
Maastrichtian

    Fraction up in beginning stage: 
0.4

    Beginning date (Ma): 
69.72

    Ending stage: 
Maastrichtian

    Fraction up in the ending stage: 
0.9

    Ending date (Ma):  
66.65

Depositional setting

A relatively low energy, open marine, lower-upper shore face environment. The trace fossils indicate a marginal marine, reduced sedimentation environment of deposition. The associated ammonites are suggestive of more open marine conditions in an otherwise shallowing basin.


Depositional pattern:  


Additional Information


Compiler:  

A. Nallapa Reddy & R. Nagendra