The organic matter is mainly of terrestrial origin with the highest concentrations and TOC accumulation rates occurring in the middle Miocene turbiditic sequences that correspond to a major compressive event between the Philippine Mobile Belt and the Palawan, Cagayan, and Sulu Ridges. Petrographic analysis of the Eocene and lower Miocene organic matter in the Celebes Sea shows that it consists only of highly degraded terrestrial particles. This observation and the very low TOC accumulation rates indicate poor conditions for organic carbon preservation during this open-ocean phase of the Celebes Basin formation. -from Authors
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CITATION STYLE
Bertrand, P., Berner, U., & Lallier-Verges, E. (1991). Organic sedimentation in Celebes and Sulu Basins: type of organic matter and evaluation of organic carbon accumulation rates. Proc., Scientific Results, ODP, Leg 124, Celebes and Sulu Seas, 217–225. https://doi.org/10.2973/odp.proc.sr.124.155.1991