Changes

Jump to navigation Jump to search
Line 39: Line 39:  
[[file:applied-paleontology_fig17-7.png|300px|thumb|{{figure number|3}}See text for explanation.]]
 
[[file:applied-paleontology_fig17-7.png|300px|thumb|{{figure number|3}}See text for explanation.]]
   −
Silicoflagellates are another group of planktonic photosynthesizing marine protists; they commonly occur with diatoms. Silicoflagellates range in age from Cretaceous to Holocene. Although not as common as diatoms, they are useful time indicators, particularly in the late Cenozoic. As a group, they were much more abundant during the early and middle Cenozoic than today. They have been used to estimate marine paleotemperatures in the late Tertiary and Quaternary.
+
Silicoflagellates are another group of planktonic photosynthesizing marine protists; they commonly occur with diatoms. Silicoflagellates range in age from Cretaceous to Holocene. Although not as common as diatoms, they are useful time indicators, particularly in the late Cenozoic. As a group, they were much more abundant during the early and middle Cenozoic than today. They have been used to estimate marine paleotemperatures in the late [[Tertiary]] and Quaternary.
    
[[:file:applied-paleontology_fig17-7.png|Figure 3]] shows some typical silicoflagellates
 
[[:file:applied-paleontology_fig17-7.png|Figure 3]] shows some typical silicoflagellates
4,231

edits

Navigation menu