Paleoceanography and paleolimnology of petroleum source rocks
Journal Article
·
· AAPG Bulletin (American Association of Petroleum Geologists); (USA)
OSTI ID:5901201
- Indiana Univ., Bloomington (USA)
Sedimentary strata containing greater than 0.5 wt. % organic carbon are unusual in both modern and ancient depositional settings. Rates of primary production (photosynthesis), recycling (decompositional efficiency), and sediment accumulation (clastic dilution) are the principal factors determining organic carbon contents of sediments and sedimentary rocks. Clastic dilution is the dominant factor in all aquatic environments when sediment accumulation rates are above about 100 mg/cm{sup 2}/yr or sedimentation rates are above about 300 m/10{sup 6}/yr. Enhanced primary productivity associated with upwelling is the dominant control on burial and preservation of organic matter in modern marine environments, but benthic anoxia related to restricted circulation may be the dominant factor in many modern lakes and most ancient epicontinental seas. During transportation and sedimentation in marine and lacustrine environments, organic detritus can by oxidized to carbon dioxide or incorporated into new biomass by bacterial communities that sequentially transfer electrons from organic matter to oxygen, nitrate, iron (Fe{sup 3+}), manganese (Mn{sup 4+}), sulfate, and carbon dioxide. Zonation of early diagenetic minerals results from progressive changes in the composition of pore water and sediment as organic matter is buried to depths of about 10 m. Mineralic and stable isotopic (carbon and sulfur) compositions of diagenetic carbonates and iron sulfides reflect depth-related bacterial and redox zones. Data bearing on these processes contribute to development of comprehensive basin models because they can be used to reconstruct changes in salinity and oxygen content of bottom water.
- OSTI ID:
- 5901201
- Journal Information:
- AAPG Bulletin (American Association of Petroleum Geologists); (USA), Journal Name: AAPG Bulletin (American Association of Petroleum Geologists); (USA) Vol. 74:11; ISSN AABUD; ISSN 0149-1423
- Country of Publication:
- United States
- Language:
- English
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·
Wed Mar 31 23:00:00 EST 1982
· Am. J. Sci.; (United States)
·
OSTI ID:5137265
Relationship between sedimentation rate and total organic carbon content in ancient marine sediments
Journal Article
·
Sun Jan 31 23:00:00 EST 1982
· Am. Assoc. Pet. Geol., Bull.; (United States)
·
OSTI ID:5324615
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Thesis/Dissertation
·
Tue Dec 31 23:00:00 EST 1991
·
OSTI ID:6645133
Related Subjects
02 PETROLEUM
020200* -- Petroleum-- Reserves
Geology
& Exploration
58 GEOSCIENCES
580000 -- Geosciences
CARBON
CARBONATE ROCKS
CHALCOGENIDES
CHEMICAL REACTIONS
DEPOSITION
DIAGENESIS
ELEMENTS
ENERGY SOURCE DEVELOPMENT
GEOLOGIC DEPOSITS
GEOLOGIC STRUCTURES
IRON COMPOUNDS
IRON SULFIDES
MANGANESE
MATURATION
METALS
MINERAL RESOURCES
NONMETALS
ORGANIC MATTER
ORIGIN
OXIDATION
PETROLEUM DEPOSITS
PRODUCTION
RESOURCES
ROCKS
SALINITY
SEDIMENTARY BASINS
SEDIMENTARY ROCKS
SEDIMENTATION
SEDIMENTS
SOURCE ROCKS
SULFIDES
SULFUR COMPOUNDS
TRANSITION ELEMENT COMPOUNDS
TRANSITION ELEMENTS
020200* -- Petroleum-- Reserves
Geology
& Exploration
58 GEOSCIENCES
580000 -- Geosciences
CARBON
CARBONATE ROCKS
CHALCOGENIDES
CHEMICAL REACTIONS
DEPOSITION
DIAGENESIS
ELEMENTS
ENERGY SOURCE DEVELOPMENT
GEOLOGIC DEPOSITS
GEOLOGIC STRUCTURES
IRON COMPOUNDS
IRON SULFIDES
MANGANESE
MATURATION
METALS
MINERAL RESOURCES
NONMETALS
ORGANIC MATTER
ORIGIN
OXIDATION
PETROLEUM DEPOSITS
PRODUCTION
RESOURCES
ROCKS
SALINITY
SEDIMENTARY BASINS
SEDIMENTARY ROCKS
SEDIMENTATION
SEDIMENTS
SOURCE ROCKS
SULFIDES
SULFUR COMPOUNDS
TRANSITION ELEMENT COMPOUNDS
TRANSITION ELEMENTS