Changes

In [[:file:applied-paleontology_fig17-18.png|Figure 2]], species inhabiting high-oxygen environments (e.g., shelf depth) are small, prolate forms; those in low-oxygen environments (e.g., basin depths) are large, lanceolate forms.

In [[:file:applied-paleontology_fig17-18.png|Figure 2]], species inhabiting high-oxygen environments (e.g., shelf depth) are small, prolate forms; those in low-oxygen environments (e.g., basin depths) are large, lanceolate forms.

[[file:applied-paleontology_fig17-19.png|left|thumb|{{figure number|3}}. Copyright: Whittaker et al., 1992; courtesy Geological Society.]]

[[file:applied-paleontology_fig17-19.png|left|300px|thumb|{{figure number|3}}Nonmarine (fluvial and marsh), lagoon, barrier, and marine environments and the interpreted sediment transport direction (large arrow) during one time interval. Copyright: Whittaker et al., 1992; courtesy Geological Society.]]

==Distribution of palynomorph types==

==Distribution of palynomorph types==