Vanadyl 3-nor C 30 DPEP: Indicator of depositional environment of a lacustrine sediment

Details Vanadyl 3-nor C 30 DPEP: Indicator of depositional environment of a lacustrine sediment Vanadyl 3-nor C 30 DPEP: Indicator of depositional environment of a lacustrine sediment

Jan 1991

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1991gecoa..55..389s&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 55, Issue 1, pp.389-395

Computer Science

3

Scientific paper

Vanadyl 3-nor C 30 DPEP (Fig. 1) was first isolated as the nickel complex by Fookes (1983) and is presumably formed from chlorophyll during early diagenesis. Porphyrin analyses of the extracts from the Bucomazi Formation, Onshore Cabinda, West Africa, show that the concentration of 3-nor C 30 DPEP increases systematically relative to C 32 DPEP with depth. This systematic change is not due to maturity and has been interpreted to indicate that the pH of the depositional environment of Bucomazi Formation increased with time. Superimposed on this pH change was change in oxicity, which is indicated by the change in porphyrin ratio.

Affiliated with

Also associated with

No associations

Rating

Vanadyl 3-nor C 30 DPEP: Indicator of depositional environment of a lacustrine sediment does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Vanadyl 3-nor C 30 DPEP: Indicator of depositional environment of a lacustrine sediment, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Vanadyl 3-nor C 30 DPEP: Indicator of depositional environment of a lacustrine sediment will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-1895356