Changes

==Distribution of palynomorph types==

==Distribution of palynomorph types==

Whittaker et al.<ref name=ch17r95>Whittaker, M. F., Giles, M., R., Cannon, S., J., C., 1992, Palynological review of the Brent Group, UK sector, North Sea, in Morton, A., C., Haszeldine, R., S., Giles, M., R., Brown, S., eds., Geology of the Brent Group: Geological Society Special Publication 61, p. 169–202.</ref> provide an industrial example in the [[Brent Group]] (Jurassic), [[North Sea]], in which the distribution of palynomorph types is used to infer the depositional environments and extent of delta [[Depocenter#Sediment_supply_rate_and_facies_patterns|progradation]] during brief intervals of the Jurassic. [[:file:applied-paleontology_fig17-19.png|Figure 3]] illustrates the nonmarine (fluvial and marsh), lagoon, barrier, and marine environments and the interpreted sediment transport direction (large arrow) during one time interval. This information can help identify regions of greater potential for fluvial reservoir sands.

Whittaker et al.<ref name=ch17r95>Whittaker, M. F., Giles, M. R., Cannon, S. J. C., 1992, Palynological review of the Brent Group, UK sector, North Sea, in Morton, A., C., Haszeldine, R., S., Giles, M., R., Brown, S., eds., Geology of the Brent Group: Geological Society Special Publication 61, p. 169–202.</ref> provide an industrial example in the [[Brent Group]] (Jurassic), [[North Sea]], in which the distribution of palynomorph types is used to infer the depositional environments and extent of delta [[Depocenter#Sediment_supply_rate_and_facies_patterns|progradation]] during brief intervals of the Jurassic. [[:file:applied-paleontology_fig17-19.png|Figure 3]] illustrates the nonmarine (fluvial and marsh), lagoon, barrier, and marine environments and the interpreted sediment transport direction (large arrow) during one time interval. This information can help identify regions of greater potential for fluvial reservoir sands.

Oboh<ref name=ch17r67>Oboh, F., E., 1992, Multivariate statistical analysis of palyno debris from the Middle Miocene of the Niger Delta and their environmental significance: Palaios, vol. 7, p. 559–573., 10., 2307/3514869</ref> develops a paleoenvironmental model of Middle Miocene reservoir units from the Niger Delta, which uses palynomorphs and organic matter to interpret more precisely the depositional environments. This improves the understanding of the lateral continuity of the reservoir and its susceptibility to diagenetic changes.

Oboh<ref name=ch17r67>Oboh, F. E., 1992, Multivariate statistical analysis of palyno debris from the Middle Miocene of the Niger Delta and their environmental significance: Palaios, vol. 7, p. 559–573., 10., 2307/3514869</ref> develops a paleoenvironmental model of Middle Miocene reservoir units from the Niger Delta, which uses palynomorphs and organic matter to interpret more precisely the depositional environments. This improves the understanding of the lateral continuity of the reservoir and its susceptibility to diagenetic changes.

 

==Integrated paleoenvironmental interpretation==

==Integrated paleoenvironmental interpretation==