FREE BOOKS

Author's List




PREV.   NEXT  
|<   225   226   227   228   229   230   231   232   233   234   235   236   237   238   239   240   241   242   243   244   245   246   247   248   249  
250   251   252   253   254   255   256   257   258   259   260   261   262   263   264   265   266   267   268   269   270   271   272   273   274   >>   >|  
tion by different workers include brachiopods, pelecypods, cephalopods, corals, fishes and plants; and the results of the comparison of the faunas and floras of different areas where Carboniferous rocks occur are generalized in the table below. The relative value of any group of animals or plants for the correlation of distant areas must vary greatly with the varying conditions of sedimentation and with the precise definition of the zonal species and with many other factors. It is found that the subdivisions in this system demanded by palaeobotanists do not always coincide with those acknowledged by palaeozoologists; nevertheless there is general agreement as to the main divisional lines. _Breaks in the Stratigraphic Sequence._--The sequence of Carboniferous strata is not everywhere one of unbroken continuity. From central France eastward towards the Carpathians only later portions of the system are found. These generally rest upon crystalline rocks, but in places they contain evidence of the denuded surfaces of Lower Carboniferous, as in the basin of Charleroi, where the equivalent of the Millstone Grit contains fragments of chert which can only have come from the waste of the earlier limestones. This unconformity is generally found about the same horizon in the continental Culm areas, and it occurs again in the western part of the English Culm. _Tabular Statement of the Principal Subdivisions of the Carboniferous System._ +-------------+------------------------+---------------+-------------+ | | Lower Carboniferous | Upper Carboniferous | +-------------+------------------------+---------------+-------------+ | | Carboniferous | Coal Measures = | | | Limestone Series. | Terrain Houiller. | +-------------+------------------------+---------------+-------------+ | | Dinantien = | Moscovien = | Ouralien = | | | (marine pelagic, | (marine type) |(marine type)| | | including continental | | | | European | deposits in some areas)| and | and | | Development.| and | | | | | | Westphalien = | Stephanien =| | | Culm = |(continental
PREV.   NEXT  
|<   225   226   227   228   229   230   231   232   233   234   235   236   237   238   239   240   241   242   243   244   245   246   247   248   249  
250   251   252   253   254   255   256   257   258   259   260   261   262   263   264   265   266   267   268   269   270   271   272   273   274   >>   >|  



Top keywords:

Carboniferous

 

marine

 
continental
 

system

 

generally

 
plants
 

earlier

 

portions

 

fragments

 

Millstone


Carpathians

 

crystalline

 
places
 

evidence

 
equivalent
 
Charleroi
 
denuded
 

surfaces

 

occurs

 

Houiller


Dinantien

 

Moscovien

 
Terrain
 

Series

 

Measures

 

Limestone

 
Ouralien
 

pelagic

 

Development

 

Westphalien


Stephanien

 

deposits

 

including

 

European

 

horizon

 

unconformity

 

western

 
Principal
 

Subdivisions

 

System


Statement

 

Tabular

 
English
 
limestones
 

Sequence

 

correlation

 

distant

 
animals
 

precise

 

definition