Where: Lindi, Tanzania (10.1° S, 39.6° E: paleocoordinates 29.2° S, 29.2° E)
• coordinate stated in text
When: Lindi Formation (Kilwa Group), Early/Lower Turonian (93.5 - 89.3 Ma)
Environment/lithology: offshore; lithified, silty sandstone
•(e.g., bedding angle shifts, convoluted lamination, folded bedding) is abundant in the intervals 38.40–79.07 m and 95.70 m to the bottom of the hole (Fig. 6), and suggests relatively common processes of sediment liquidization before significant compaction took place. The intensity of stratigraphic disruption of these sediments is difficult to evaluate, since in 2007 no other holes were drilled close to TDP Site 22 that allowed examination of the lateral extension of the soft deformation. This issue, along with the driving causes of the sediment deformation, will be analyzed in future TDP expeditions. Ammonite and inoceramid debris are visible at 20.05 m and 26.90 m, respectively, and small bioclasts and bioturbation
•mottling occur sporadically.
Size class: microfossils
Preservation: original calcite, replaced with calcite
Collected by Tanzania Drilling Project Expedition in 2007; reposited in the USNM
Collection methods: core, smear slide,
Primary reference: Á J. Berrocoso, K. G. MacLeod, B. T. Huber, J. A. Lees, I. Wendler, P. R. Bown, A. K. Mweneinda, C. I. Londoño, and J. M. Singano. 2010. Lithostratigraphy, biostratigraphy and chemostratigraphy of Upper Cretaceous sediments from southern Tanzania: Tanzania drilling project sites 21-26. Journal of African Earth Sciences 57:47-69 [M. Uhen/L. Petruny]more details
Purpose of describing collection: biostratigraphic analysis
PaleoDB collection 179875: authorized by Mark Uhen, entered by Loren Petruny on 03.07.2016
Creative Commons license: CC BY (attribution)
Taxonomic list
Coccolithophyceae | |
Eprolithus moratus Stover 1966 | |
Foraminifera | |
Whiteinella archaeocretacea Pessagno 1967 |