Difference between revisions of "Stratigraphic and geographic distribution of fossils"

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In essence, paleontologic analysis is based on knowing the distribution of fossil species in time and space. All fossil species persisted for a limited geologic duration and were restricted in habitat to specific [[Paleoenvironmental analysis|paleoenvironments]] characterized by a range of ecological parameters such as temperature, salinity, dissolved oxygen, and food availability. Because several important parameters vary somewhat systematically with water depth in marine environments, [[benthic]] fossils commonly are used to estimate [[paleobathymetry]] for basin modeling and [[sequence stratigraphy]].  
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In essence, paleontologic analysis is based on knowing the distribution of fossil species in time and space. All fossil species persisted for a limited geologic duration and were restricted in habitat to specific [[Paleoenvironmental analysis|paleoenvironments]] characterized by a range of ecological parameters such as temperature, salinity, dissolved oxygen, and food availability. Because several important parameters vary somewhat systematically with water depth in marine environments, benthic fossils (remains of bottom-dwelling organisms) commonly are used to estimate [[paleobathymetry]] for basin modeling and [[sequence stratigraphy]].  
  
 
==See also==
 
==See also==

Revision as of 14:53, 25 April 2014

Exploring for Oil and Gas Traps
Series Treatise in Petroleum Geology
Part Predicting the occurrence of oil and gas traps
Chapter Applied paleontology
Author Robert L. Fleisher, H. Richard Lane
Link Web page
Store AAPG Store

In essence, paleontologic analysis is based on knowing the distribution of fossil species in time and space. All fossil species persisted for a limited geologic duration and were restricted in habitat to specific paleoenvironments characterized by a range of ecological parameters such as temperature, salinity, dissolved oxygen, and food availability. Because several important parameters vary somewhat systematically with water depth in marine environments, benthic fossils (remains of bottom-dwelling organisms) commonly are used to estimate paleobathymetry for basin modeling and sequence stratigraphy.

See also

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Stratigraphic and geographic distribution of fossils
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